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  <front>
    <journal-meta>
<journal-id journal-id-type="publisher">AMT</journal-id>
<journal-title-group>
<journal-title>Atmospheric Measurement Techniques</journal-title>
<abbrev-journal-title abbrev-type="publisher">AMT</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Atmos. Meas. Tech.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1867-8548</issn>
<publisher><publisher-name>Copernicus GmbH</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>

    <article-meta>
      <article-id pub-id-type="doi">10.5194/amt-8-2463-2015</article-id><title-group><article-title>Validation of the poke-flow technique combined with simulations of fluid flow for determining viscosities in samples with small volumes and high viscosities</article-title>
      </title-group><?xmltex \runningtitle{Validation of the poke-flow technique combined with simulations
of fluid flow}?><?xmltex \runningauthor{J.~W.~Grayson et al.}?>
      <contrib-group>
        <contrib contrib-type="author" corresp="no" rid="aff1 aff3">
          <name><surname>Grayson</surname><given-names>J. W.</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff1 aff3">
          <name><surname>Song</surname><given-names>M.</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff2">
          <name><surname>Sellier</surname><given-names>M.</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="yes" rid="aff1">
          <name><surname>Bertram</surname><given-names>A. K.</given-names></name>
          <email>bertram@chem.ubc.ca</email>
        <ext-link>https://orcid.org/0000-0002-5621-2323</ext-link></contrib>
        <aff id="aff1"><label>1</label><institution>Department of Chemistry, University of British Columbia, Vancouver,
BC V6T 1Z1, Canada</institution>
        </aff>
        <aff id="aff2"><label>2</label><institution>Department of Mechanical Engineering,
University of Canterbury, Christchurch 8140, New Zealand</institution>
        </aff>
        <aff id="aff3"><label>*</label><institution>These authors contributed equally to this work.</institution>
        </aff>
      </contrib-group>
      <author-notes><corresp id="corr1">A. K. Bertram (bertram@chem.ubc.ca)</corresp></author-notes><pub-date><day>16</day><month>June</month><year>2015</year></pub-date>
      
      <volume>8</volume>
      <issue>6</issue>
      <fpage>2463</fpage><lpage>2472</lpage>
      <history>
        <date date-type="received"><day>21</day><month>November</month><year>2014</year></date>
           <date date-type="rev-request"><day>23</day><month>January</month><year>2015</year></date>
           <date date-type="rev-recd"><day>8</day><month>May</month><year>2015</year></date>
           <date date-type="accepted"><day>22</day><month>May</month><year>2015</year></date>
      </history>
      <permissions>
<license license-type="open-access">
<license-p>This work is licensed under a Creative Commons Attribution 3.0 Unported License. To view a copy of this license, visit <ext-link ext-link-type="uri" xlink:href="http://creativecommons.org/licenses/by/3.0/">http://creativecommons.org/licenses/by/3.0/</ext-link></license-p>
</license>
</permissions><self-uri xlink:href="https://amt.copernicus.org/articles/8/2463/2015/amt-8-2463-2015.html">This article is available from https://amt.copernicus.org/articles/8/2463/2015/amt-8-2463-2015.html</self-uri>
<self-uri xlink:href="https://amt.copernicus.org/articles/8/2463/2015/amt-8-2463-2015.pdf">The full text article is available as a PDF file from https://amt.copernicus.org/articles/8/2463/2015/amt-8-2463-2015.pdf</self-uri>


      <abstract>
    <p>Viscosity in particles consisting of secondary organic material (SOM) has
recently become an area of research focus, since information on viscosity is
needed to predict the environmental impacts of SOM particles. Recently
<xref ref-type="bibr" rid="bib1.bibx33" id="normal.1"/> developed a poke-flow technique that was combined
with simulations of fluid flow to constrain the viscosities of SOM samples of
1–5 mg mass, roughly the maximum that may be collected from environmental
chambers or flow tubes on a reasonable timescale. The current manuscript
expands on the initial validation experiments carried out by Renbaum-Wolff et
al. First, the poke-flow technique combined with simulations of fluid flow
was used to determine the viscosity of sucrose–water particles over a
relatively wide range of relative humidities (RHs). The lower and upper
limits of viscosity at 59 % RH were 1.0 <inline-formula><mml:math display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">1</mml:mn></mml:msup></mml:math></inline-formula> and
1.6 <inline-formula><mml:math display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">4</mml:mn></mml:msup></mml:math></inline-formula> Pa s, whilst at 37 % RH the corresponding values
were 7.2 <inline-formula><mml:math display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">4</mml:mn></mml:msup></mml:math></inline-formula> and 4.7 <inline-formula><mml:math display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">6</mml:mn></mml:msup></mml:math></inline-formula> Pa s, respectively.
The results are in good agreement with recent measurements by
<xref ref-type="bibr" rid="bib1.bibx31" id="normal.2"/> and <xref ref-type="bibr" rid="bib1.bibx30" id="normal.3"/>. Second, the approach was used
to determine the viscosity of two polybutene standards. The simulated lower
and upper limits of viscosity for standard #1 was 2.0 <inline-formula><mml:math display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msup></mml:math></inline-formula> and
1.2 <inline-formula><mml:math display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">4</mml:mn></mml:msup></mml:math></inline-formula> Pa s, whilst for standard #2 the corresponding
values were 3.1 <inline-formula><mml:math display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msup></mml:math></inline-formula> and 2.4 <inline-formula><mml:math display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">4</mml:mn></mml:msup></mml:math></inline-formula> Pa s. These
values are in good agreement with values reported by the manufacturer. The
results for both the sucrose–water particles and the polybutene standards
show that the poke-flow technique combined with simulations of fluid flow is
capable of providing both lower and upper limits of viscosity that are
consistent with literature or measured values when the viscosity of the
particles are in the range of
<inline-formula><mml:math display="inline"><mml:mo>≈</mml:mo></mml:math></inline-formula> 5 <inline-formula><mml:math display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msup></mml:math></inline-formula> to <inline-formula><mml:math display="inline"><mml:mo>≈</mml:mo></mml:math></inline-formula> 3 <inline-formula><mml:math display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">6</mml:mn></mml:msup></mml:math></inline-formula> Pa s.</p>
  </abstract>
    </article-meta>
  </front>
<body>
      

<sec id="Ch1.S1" sec-type="intro">
  <title>Introduction</title>
      <p>Particles consisting of secondary organic material (SOM) are abundant in the
atmosphere and, depending upon location, typically account for 20–80 %
of the mass of atmospheric aerosol particles <xref ref-type="bibr" rid="bib1.bibx15 bib1.bibx11" id="paren.4"/>. These SOM particles can affect the Earth's climate directly
by scattering and/or absorbing solar radiation and indirectly by acting as
ice and liquid cloud droplet nuclei <xref ref-type="bibr" rid="bib1.bibx42 bib1.bibx24 bib1.bibx48" id="paren.5"/>. In addition, SOM particles can influence air quality and human
health <xref ref-type="bibr" rid="bib1.bibx9 bib1.bibx1" id="paren.6"/>.</p>
      <p>Knowledge of diffusion rates of organics within SOM particles is important
for determining rates of particle growth, rates of heterogeneous reactions
and long-range transport of pollutants <xref ref-type="bibr" rid="bib1.bibx18 bib1.bibx35 bib1.bibx40 bib1.bibx19 bib1.bibx28 bib1.bibx36 bib1.bibx39 bib1.bibx51 bib1.bibx41 bib1.bibx52" id="paren.7"/>. For
example, <xref ref-type="bibr" rid="bib1.bibx35" id="normal.8"/> showed that the size distribution and number
concentrations of ultrafine aerosol particles, which are important for the
aerosol direct and indirect effect on climate, depend on diffusion within
particles. <xref ref-type="bibr" rid="bib1.bibx39" id="normal.9"/> showed that predictions of the total mass
of SOM particles in urban environments are sensitive to diffusion
coefficients of organics in the SOM material, and <xref ref-type="bibr" rid="bib1.bibx40" id="normal.10"/>
showed the chemical aging of semisolid SOM can depend on the rate of
molecular diffusion of organics within the particle. In addition,
<xref ref-type="bibr" rid="bib1.bibx51" id="normal.11"/> demonstrated that transportation of polycyclic
aromatic hydrocarbons (PAHs) in the atmosphere can depend on diffusion rates
in particles.</p>
      <p>Diffusion rates of organics in SOM particles can be estimated using viscosity
measurements and the Stokes–Einstein relation, and, as such, measurements of
viscosity in SOM particles have recently become an area of research focus.
The viscosity, <inline-formula><mml:math display="inline"><mml:mi mathvariant="italic">η</mml:mi></mml:math></inline-formula>, of SOM may span multiple orders of magnitude, from
10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">3</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula> to <inline-formula><mml:math display="inline"><mml:mo>&gt;</mml:mo></mml:math></inline-formula> 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mn>12</mml:mn></mml:msup></mml:math></inline-formula> Pa s, across the ambient relative
humidity (RH)
range in the atmosphere through the uptake and release of water
<xref ref-type="bibr" rid="bib1.bibx18 bib1.bibx19 bib1.bibx33" id="paren.12"/>. Measuring such a
wide range of viscosities presents a challenge, made more difficult by the
small, milligram, scale of SOM samples typically collected in the atmosphere
or chambers used to simulate atmospheric conditions. Currently, there is no
commercially available technique capable of quantifying the viscosity of SOM
samples across the entire viscosity range important in the atmosphere.
However, a few techniques have recently been developed, each of which is
capable of covering at least part of the range of interest.</p>
      <p><xref ref-type="bibr" rid="bib1.bibx34" id="normal.13"/> developed a bead-mobility technique, which can
determine the viscosities of SOM samples with masses between 1 and 5 mg and
viscosities between 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">3</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula> and 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">3</mml:mn></mml:msup></mml:math></inline-formula> Pa s. This technique consists of
determining the speed of circulation of micrometer-sized beads within a
particle as a shear stress is applied to the particle. In a subsequent paper,
<xref ref-type="bibr" rid="bib1.bibx33" id="normal.14"/> developed a poke-flow technique that was combined
with simulations of fluid flow to constrain the viscosities of SOM samples of
1–5 mg mass. The technique consisted of generating a hole in a
supermicron-sized SOM particle suspended on a surface and determining a characteristic
time taken for the hole to close. Simulations of fluid flow were subsequently
performed to determine limits for the viscosity of the particle, based upon
the time taken for the hole at its centre to close.
<xref ref-type="bibr" rid="bib1.bibx33" id="normal.15"/> demonstrated that measured upper limits of
viscosity were consistent with literature values up to at least
10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">4</mml:mn></mml:msup></mml:math></inline-formula> Pa s.</p>
      <p><xref ref-type="bibr" rid="bib1.bibx30" id="normal.16"/> used holographic optical tweezers to coalesce two
suspended particles with a combined volume of <inline-formula><mml:math display="inline"><mml:mo>&lt;</mml:mo></mml:math></inline-formula> 500 femtolitres. By
measuring the time taken for the resulting particle to relax to a spherical
shape, viscosities of sucrose–water or sucrose–salt-water particles were
quantified across the range of 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">3</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula>–10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">9</mml:mn></mml:msup></mml:math></inline-formula> Pa s. Subsequently, <xref ref-type="bibr" rid="bib1.bibx29" id="normal.17"/>
further outlined the application of optical tweezers for
rheological measurements. In a similar vein, <xref ref-type="bibr" rid="bib1.bibx27" id="normal.18"/> used
scanning electron microscopy images to determine the viscosity of secondary
organic aerosols by studying the time taken for multiple particles to
coalesce. <xref ref-type="bibr" rid="bib1.bibx8" id="normal.19"/> observed the behaviour of molecular rotors
using fluorescence lifetime imaging microscopy to determine the viscosity of
sodium chloride and sucrose–water particles. In addition, <xref ref-type="bibr" rid="bib1.bibx16" id="normal.20"/>
estimated some limits to viscosities of particles from the extent to which
material collected in the centreline of an impactor spreads under high
airflow.</p>
      <p>In the paper by <xref ref-type="bibr" rid="bib1.bibx33" id="normal.21"/>, only a preliminary validation of
the poke-flow technique combined with simulations of fluid flow was carried
out for viscosities <inline-formula><mml:math display="inline"><mml:mo>&lt;</mml:mo></mml:math></inline-formula> 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">8</mml:mn></mml:msup></mml:math></inline-formula> Pa s due to the lack of suitable standards
for validation at the time of publication. Specifically, Renbaum-Wolff et al.
used sucrose–water particles over a narrow range of RHs to
validate the approach for viscosities <inline-formula><mml:math display="inline"><mml:mo>&lt;</mml:mo></mml:math></inline-formula> 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">8</mml:mn></mml:msup></mml:math></inline-formula> Pa s. In addition, as
mentioned above, for viscosities <inline-formula><mml:math display="inline"><mml:mo>&lt;</mml:mo></mml:math></inline-formula> 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">8</mml:mn></mml:msup></mml:math></inline-formula> Pa s, the authors only showed
that the approach was able to provide upper limits to the viscosity of the
particles. No attempt was made to determine lower limits to the particle
viscosity using the poke-flow technique combined with simulations of fluid
flow when the viscosity was <inline-formula><mml:math display="inline"><mml:mo>&lt;</mml:mo></mml:math></inline-formula> 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">8</mml:mn></mml:msup></mml:math></inline-formula> Pa s.</p>
      <p>In the following study we expand on the initial validation and characterization of
the poke-flow technique combined with simulations of fluid flow. First, the
approach is used to determine the viscosity of sucrose–water particles over a
wider range of RHs than previously done by
<xref ref-type="bibr" rid="bib1.bibx33" id="normal.22"/>. These results are compared to recent results
published by <xref ref-type="bibr" rid="bib1.bibx30" id="normal.23"/>, who reported viscosities of sucrose–water
particles ranging from 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">3</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula> to 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">9</mml:mn></mml:msup></mml:math></inline-formula> Pa s, and <xref ref-type="bibr" rid="bib1.bibx31" id="normal.24"/>,
who measured a viscosity of 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">3</mml:mn></mml:msup></mml:math></inline-formula> Pa s at 54 % RH using a rotational
controlled stress rheometer. Second, the approach was used to determine the
viscosity of two polybutene standards, and the results were compared with
viscosities measured by the manufacturer using a commercially available
viscometer. The results for both the sucrose–water particles and the
polybutene standards show that this approach is capable of providing both lower
and upper limits of viscosity that are consistent with literature or measured
values for particles of material that range in viscosity from
<inline-formula><mml:math display="inline"><mml:mo>≈</mml:mo></mml:math></inline-formula> 5 <inline-formula><mml:math display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msup></mml:math></inline-formula> to <inline-formula><mml:math display="inline"><mml:mo>≈</mml:mo></mml:math></inline-formula> 3 <inline-formula><mml:math display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">6</mml:mn></mml:msup></mml:math></inline-formula> Pa s.</p>
</sec>
<sec id="Ch1.S2">
  <title>Materials and methods</title>
<sec id="Ch1.S2.SS1">
  <title>Poke-flow technique</title>
      <p>The qualitative method of poking a particle to determine the particle phase
(i.e. solid/semisolid vs. liquid) was introduced by <xref ref-type="bibr" rid="bib1.bibx25" id="normal.25"/>.
This approach was expanded upon by <xref ref-type="bibr" rid="bib1.bibx33" id="normal.26"/> by quantifying
flow rates after poking and determining viscosities from simulations of flow.
Figure 1 illustrates schematically the experimental setup for the poke-flow
measurements. First supermicron particles of interest (either particles
containing sucrose–water or polybutene standards) were deposited on a
hydrophobic glass substrate (18 mm diameter) (Hampton Research, Canada). The
glass substrate was then mounted onto a custom-made flow cell, similar to
those described previously <xref ref-type="bibr" rid="bib1.bibx17 bib1.bibx43 bib1.bibx50" id="paren.27"/> but
with a small hole added at the top through which a needle could be inserted
<xref ref-type="bibr" rid="bib1.bibx33" id="paren.28"/>. RH within the cell was controlled through the use
of humidified ultrapure N<inline-formula><mml:math display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> gas, a stream of which was flowed continuously
through the cell. Gas flow was maintained at 1200 sccm for all experiments.
The dew point temperature of the humidified N<inline-formula><mml:math display="inline"><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:math></inline-formula> gas was measured at the
outflow of the cell using a hygrometer with a chilled-mirror sensor (General
Eastern, Canada). The hygrometer was calibrated prior to experiments being
performed by determining the deliquescence relative humidity (DRH) of
ammonium sulfate particles and comparing the observed DRH value to that in
the literature (<inline-formula><mml:math display="inline"><mml:mo>≈</mml:mo></mml:math></inline-formula> 80.3 % RH at 20 <inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>C). The uncertainty
(1<inline-formula><mml:math display="inline"><mml:mi mathvariant="italic">σ</mml:mi></mml:math></inline-formula>) of the hygrometer was <inline-formula><mml:math display="inline"><mml:mo>±</mml:mo></mml:math></inline-formula>0.5 at 80.3 % RH after
calibration. The temperature of the sample was measured directly below the
flow cell using a thermocouple. Particles were monitored during experiments
using a reflectance optical microscope (Zeiss Axio Observer, 40<inline-formula><mml:math display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula>
objective) and recorded using a CCD camera.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F1"><caption><p>Schematic representation of poke-flow experimental setup.</p></caption>
          <?xmltex \igopts{width=241.848425pt}?><graphic xlink:href="amt-2014-379-f01.png"/>

        </fig>

      <p>Two different types of needles were used for experiments. For particles of
low viscosity, a sterilized sharp needle (0.9 mm <inline-formula><mml:math display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 40 mm)
(Becton-Dickson, USA) was used. However, at higher viscosity particles stuck
to the needle and as a result were removed from the substrate. As such, a
second set of needles was used (RS-6063, Roboz Surgical Instrument Co., USA),
which were coated with a hydrophobic Dursan coating (SilcoTek, USA) to prevent
material sticking to the needles. The needles were mounted to a
micromanipulator (Narishige, model MO-202U, Japan) and inserted through the
hole at the top of the flow cell. The effect of the presence of the hole at
the top of the flow cell upon RH in the cell was determined to be minimal by
studying the DRH of ammonium sulfate and
potassium carbonate particles with the hole open and the hole closed. The DRH
of ammonium sulfate particles differed by <inline-formula><mml:math display="inline"><mml:mo>&lt;</mml:mo></mml:math></inline-formula> 0.2 at 80 % RH, whilst the
DRH of potassium carbonate particles differed by <inline-formula><mml:math display="inline"><mml:mo>&lt;</mml:mo></mml:math></inline-formula> 0.4 at 43 % RH. The
micromanipulator was used to move the needle in the <inline-formula><mml:math display="inline"><mml:mi>x</mml:mi></mml:math></inline-formula>, <inline-formula><mml:math display="inline"><mml:mi>y</mml:mi></mml:math></inline-formula>, and <inline-formula><mml:math display="inline"><mml:mi>z</mml:mi></mml:math></inline-formula> axes.</p>
      <p>For a given experiment, the tip of the needle was aligned vertically above
the centre of a particle and then moved down in the <inline-formula><mml:math display="inline"><mml:mi>z</mml:mi></mml:math></inline-formula> direction, first
penetrating the particle at the peak of its spherical cap geometry and
subsequently coming in contact with the substrate beneath. After the needle
was removed, the material of the particle was present in a non-equilibrium
half-torus geometry and began to flow in order to minimize the surface
energy of the system. Eventually the hole at the centre of the half torus
completely closed, and the particle returned to its original spherical cap
morphology.</p>
      <p>Analysis of optical images captured during each experiment was performed
using Zen software (Zeiss). The hole at the centre of the half torus was
traced and the area of the hole calculated. An equivalent area diameter of
the hole was calculated via the relationship <inline-formula><mml:math display="inline"><mml:mrow><mml:mi>d</mml:mi><mml:mo>=</mml:mo><mml:mo>(</mml:mo><mml:mn mathvariant="normal">4</mml:mn><mml:mi>A</mml:mi><mml:mo>/</mml:mo><mml:mi mathvariant="italic">π</mml:mi><mml:msup><mml:mo>)</mml:mo><mml:mrow><mml:mn mathvariant="normal">1</mml:mn><mml:mo>/</mml:mo><mml:mn mathvariant="normal">2</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>, where <inline-formula><mml:math display="inline"><mml:mi>d</mml:mi></mml:math></inline-formula> is
the equivalent area diameter of a hole of area, <inline-formula><mml:math display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula> <xref ref-type="bibr" rid="bib1.bibx32" id="paren.29"/>. The
experimental flow time, termed <inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi mathvariant="italic">τ</mml:mi><mml:mtext>exp, flow</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>, was assigned as the
time taken for the equivalent area diameter to decrease to 50 % of its
original value. This definition of experimental flow time was chosen as it
allows experimental flow time of more viscous particles, the holes of which
may not fully close on a laboratory timescale, to be measured.</p>
      <p>In some of the experiments, a point around the inner edge of the half torus
appeared to be pinned to the hydrophobic surface. This behaviour may suggest
that in some cases the needle scratched the surface. Particles that exhibited
this pinning behaviour were excluded from analysis in order to avoid
influencing the results. Pinning affected <inline-formula><mml:math display="inline"><mml:mo>&lt;</mml:mo></mml:math></inline-formula> 20 % of all the particles
that formed a torus geometry after poking.</p>
      <p>Sucrose–water particles were produced on siliconized hydrophobic glass
substrates using a nebulizer (Meinhard; product no. TR-50-A1). First sucrose
(Sigma-Aldrich, purity <inline-formula><mml:math display="inline"><mml:mo>&gt;</mml:mo></mml:math></inline-formula> 99.5 %) was combined with high-purity water
(Millipore, 18.2 M<inline-formula><mml:math display="inline"><mml:mi mathvariant="normal">Ω</mml:mi></mml:math></inline-formula> cm) to produce an aqueous solution. The solution
was then nebulized to produce submicron-sized particles, which subsequently
coagulated on the substrate to form supermicron-sized particles,
25–60 <inline-formula><mml:math display="inline"><mml:mi mathvariant="normal">µ</mml:mi></mml:math></inline-formula>m in diameter. In the sucrose–water experiments, particles
were allowed to equilibrate at a given RH for 30–60 min prior to being
poked, which, given their size and approximate viscosity, was sufficient time
for the particles to have a water content in equilibrium with that of the gas
flowing through the cell (Shiraiwa,  2011; Price et al.,  2014).</p>
      <p>Particles consisting of polybutene standards (N450000 and N2700000; Cannon
Instrument Company, USA) were prepared on hydrophobic glass substrates using
a pipette. The samples were heated to 60–70 <inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>C over <inline-formula><mml:math display="inline"><mml:mo>≈</mml:mo></mml:math></inline-formula> 30 min to aid the production of particles by reducing the viscosity of the
material, with material being picked up on a pipette tip and the pipette
being “flicked” towards the substrate, resulting in particles being formed
on the substrate. After particle production, the particles were allowed to
equilibrate at dry (<inline-formula><mml:math display="inline"><mml:mo>&lt;</mml:mo></mml:math></inline-formula> 0.5 % RH) conditions at room temperature for
60 min. Particles consisting of polybutene standards that were poked ranged
in diameter from 40 to 70 <inline-formula><mml:math display="inline"><mml:mi mathvariant="normal">µ</mml:mi></mml:math></inline-formula>m.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F2"><caption><p>Details of half-torus model used to simulate the flow in
experiments: <bold>(a)</bold> top view, where <inline-formula><mml:math display="inline"><mml:mi>R</mml:mi></mml:math></inline-formula> and <inline-formula><mml:math display="inline"><mml:mi>r</mml:mi></mml:math></inline-formula> are the notations used
here to describe the dimensions of a half-torus geometry; <bold>(b)</bold> side
view, where surface 1 represents the air–fluid interface, and surface 2
represents the fluid–substrate interface.</p></caption>
          <?xmltex \igopts{width=241.848425pt}?><graphic xlink:href="amt-2014-379-f02.png"/>

        </fig>

      <?xmltex \floatpos{t}?><fig id="Ch1.F3" specific-use="star"><caption><p>Optical images of sucrose–water particles poked at RHs of
<bold>(a)</bold> 48.8, <bold>(b)</bold> 52.7, and <bold>(c)</bold> 58.8 % recorded
during typical poke-flow experiments. Images a1, b1, and c1 correspond to the
particles before they are poked. Images a2, b2, and c2 correspond to the
first frame post-poke (i.e. the first frame after the needle has been
removed). Images a3, b3, and c3 correspond to images of the experimental flow
time, <inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi mathvariant="italic">τ</mml:mi><mml:mtext>exp, flow</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>, the point at which the equivalent area
diameter of the hole at the centre of the particle has decreased to 50 %
of its original size. Images a4, b4, and c4 correspond to the final frame
recorded, at which point each particle has re-attained its original spherical
cap geometry. Scale bar: 20 <inline-formula><mml:math display="inline"><mml:mi mathvariant="normal">µ</mml:mi></mml:math></inline-formula>m.</p></caption>
          <?xmltex \igopts{width=398.338583pt}?><graphic xlink:href="amt-2014-379-f03.png"/>

        </fig>

      <?xmltex \floatpos{t}?><fig id="Ch1.F4" specific-use="star"><caption><p><bold>(a)</bold> <inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi mathvariant="italic">τ</mml:mi><mml:mtext>exp, flow</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> as a function of RH for
individual sucrose–water particles. <bold>(b)</bold> Calculated viscosities for
the individual sucrose–water particles in <bold>(a)</bold>, where red bars
represent the calculated lower and upper limits of viscosity. <bold>(c)</bold>
Lower and upper limits of viscosity for the particles shown in <bold>(b)</bold>,
grouped by RH. The error bars on the <inline-formula><mml:math display="inline"><mml:mi>x</mml:mi></mml:math></inline-formula> axis represent the range of RHs at
which particles in the group were poked. Lower and upper limits of viscosity
were determined for each particle via simulation, with the bottom of a bar on
the <inline-formula><mml:math display="inline"><mml:mi>y</mml:mi></mml:math></inline-formula> axis representing the lowest lower limit of viscosity for any of the
particles in the group, and the top of the bar representing the highest upper
limit of viscosity for any of the particles in the group. Literature values
<xref ref-type="bibr" rid="bib1.bibx45 bib1.bibx31 bib1.bibx30" id="paren.30"/> are provided for
comparison, with error bars representing 1<inline-formula><mml:math display="inline"><mml:mi mathvariant="italic">σ</mml:mi></mml:math></inline-formula> for Power et al. and
95 % confidence intervals for Quintas et al.</p></caption>
          <?xmltex \igopts{width=406.874409pt}?><graphic xlink:href="amt-2014-379-f04.png"/>

        </fig>

</sec>
<sec id="Ch1.S2.SS2">
  <title>Simulations of fluid flow</title>
      <p>Flow in the poke-flow experiments was simulated using the laminar two-phase
flow, moving mesh mode within the micro-fluidics module of COMSOL (version
4.3a), a finite-element analysis software package. The Navier–Stokes
equation, including surface tension, is used to describe the transport of
mass and momentum, whilst the arbitrary Lagrangian–Eularian (ALE) method is
used to track the evolution of the fluid over time as it flows to attain a
spherical cap geometry and thus minimize the surface energy of the system.
Simulations were performed with a mesh that consisted of <inline-formula><mml:math display="inline"><mml:mo>≈</mml:mo></mml:math></inline-formula> 5800
elements and had a mesh spacing of 3.92–337 nm.</p>
      <p>A top view of the half-torus geometry used to simulate the experimental
observations is shown in Fig. 2a, where the dotted line is at the midpoint
between the inner and outer edges of the ring of material forming the torus.
The initial radius of the hole at the centre of the half torus is denoted as
<inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi>R</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>–<inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi>r</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>, where <inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi>R</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> represents the distance from the centre of the hole
to the midpoint of the ring of material that creates the torus, whilst <inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi>r</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>
represents the radius of the ring of material. The half torus had two
distinct surfaces (Fig. 2b). Surface 1 represents the air–fluid interface,
which was allowed to undergo free deformation in all dimensions. Surface 2 is
the fluid–substrate interface, which was allowed to undergo free deformation
in the horizontal <inline-formula><mml:math display="inline"><mml:mi>x</mml:mi></mml:math></inline-formula>–<inline-formula><mml:math display="inline"><mml:mi>y</mml:mi></mml:math></inline-formula> plane, but not in the vertical, <inline-formula><mml:math display="inline"><mml:mi>z</mml:mi></mml:math></inline-formula>, direction. In
the simulations, the size of the hole in the half-torus geometry decreases in
an axi-symmetric manner. The time taken for <inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi>R</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>–<inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi>r</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> to decrease to
50 % of the initial value was assigned <inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi mathvariant="italic">τ</mml:mi><mml:mtext>model, flow</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>.</p>

<?xmltex \floatpos{t}?><table-wrap id="Ch1.T1" specific-use="star"><caption><p>Experimental parameters used when simulating flow with COMSOL for
the sucrose–water experiments.</p></caption><oasis:table frame="topbot"><oasis:tgroup cols="5">
     <oasis:colspec colnum="1" colname="col1" align="justify" colwidth="85.358268pt"/>
     <oasis:colspec colnum="2" colname="col2" align="left"/>
     <oasis:colspec colnum="3" colname="col3" align="left"/>
     <oasis:colspec colnum="4" colname="col4" align="left"/>
     <oasis:colspec colnum="5" colname="col5" align="justify" colwidth="142.26378pt"/>
     <oasis:thead>
       <oasis:row>  
         <oasis:entry colname="col1"/>  
         <oasis:entry colname="col2">Surface tension</oasis:entry>  
         <oasis:entry colname="col3">Slip length</oasis:entry>  
         <oasis:entry colname="col4">Density</oasis:entry>  
         <oasis:entry colname="col5">Contact angle</oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">  
         <oasis:entry colname="col1"/>  
         <oasis:entry colname="col2">(mN m<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula>)</oasis:entry>  
         <oasis:entry colname="col3">(m)</oasis:entry>  
         <oasis:entry colname="col4">(kg m<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">3</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula>)</oasis:entry>  
         <oasis:entry colname="col5">(<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>)</oasis:entry>
       </oasis:row>
     </oasis:thead>
     <oasis:tbody>
       <oasis:row>  
         <oasis:entry colname="col1">Range of values</oasis:entry>  
         <oasis:entry colname="col2">57.2–75.15<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">a</mml:mi></mml:msup></mml:math></inline-formula></oasis:entry>  
         <oasis:entry colname="col3">5 <inline-formula><mml:math display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">9</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula>–</oasis:entry>  
         <oasis:entry colname="col4">1490–</oasis:entry>  
         <oasis:entry colname="col5">94.8–102.2<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">d</mml:mi></mml:msup></mml:math></inline-formula></oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">  
         <oasis:entry colname="col1"/>  
         <oasis:entry colname="col2"/>  
         <oasis:entry colname="col3">1 <inline-formula><mml:math display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:msup><mml:mn mathvariant="normal">5</mml:mn><mml:mi mathvariant="normal">b</mml:mi></mml:msup></mml:mrow></mml:msup></mml:math></inline-formula></oasis:entry>  
         <oasis:entry colname="col4">1520<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">c</mml:mi></mml:msup></mml:math></inline-formula></oasis:entry>  
         <oasis:entry colname="col5"/>
       </oasis:row>
       <oasis:row rowsep="1">  
         <oasis:entry colname="col1">Value used to calculate lower limit of viscosity</oasis:entry>  
         <oasis:entry colname="col2">57.2</oasis:entry>  
         <oasis:entry colname="col3">5 <inline-formula><mml:math display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">9</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula></oasis:entry>  
         <oasis:entry colname="col4">1500</oasis:entry>  
         <oasis:entry colname="col5">94.8 for particles of (<inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi>R</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>–<inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi>r</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub><mml:mo>)</mml:mo><mml:mo>/</mml:mo><mml:msub><mml:mi>r</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub><mml:mo>&lt;</mml:mo><mml:mn mathvariant="normal">2</mml:mn></mml:mrow></mml:math></inline-formula> 102.2 for particles of (<inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi>R</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>–<inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi>r</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub><mml:mo>)</mml:mo><mml:mo>/</mml:mo><mml:msub><mml:mi>r</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math display="inline"><mml:mo>&gt;</mml:mo></mml:math></inline-formula> 2</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1">Value used to calculate upper limit of viscosity</oasis:entry>  
         <oasis:entry colname="col2">75.15</oasis:entry>  
         <oasis:entry colname="col3">1 <inline-formula><mml:math display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">5</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula></oasis:entry>  
         <oasis:entry colname="col4">1500</oasis:entry>  
         <oasis:entry colname="col5">102.2 for particles of (<inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi>R</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>–<inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi>r</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub><mml:mo>)</mml:mo><mml:mo>/</mml:mo><mml:msub><mml:mi>r</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math display="inline"><mml:mo>&lt;</mml:mo></mml:math></inline-formula> 2 94.8 for particles of (<inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi>R</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>–<inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi>r</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub><mml:mo>)</mml:mo><mml:mo>/</mml:mo><mml:msub><mml:mi>r</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math display="inline"><mml:mo>&gt;</mml:mo></mml:math></inline-formula> 2</oasis:entry>
       </oasis:row>
     </oasis:tbody>
   </oasis:tgroup></oasis:table><table-wrap-foot><p><inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">a</mml:mi></mml:msup></mml:math></inline-formula> <xref ref-type="bibr" rid="bib1.bibx30" id="normal.31"/>, <xref ref-type="bibr" rid="bib1.bibx22" id="normal.32"/>.
<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">b</mml:mi></mml:msup></mml:math></inline-formula> This range is based on experimental measurements of the slip
length of water and organic compounds on hydrophobic surfaces
<xref ref-type="bibr" rid="bib1.bibx38 bib1.bibx6 bib1.bibx49 bib1.bibx2 bib1.bibx7 bib1.bibx47 bib1.bibx4 bib1.bibx12 bib1.bibx14 bib1.bibx26 bib1.bibx5 bib1.bibx13 bib1.bibx53 bib1.bibx21" id="paren.33"/>.
<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">c</mml:mi></mml:msup></mml:math></inline-formula> <xref ref-type="bibr" rid="bib1.bibx54 bib1.bibx46" id="normal.34"/>. A density of 910 kg m<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">3</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula> was used for all simulations as density was found to have no effect
on simulated viscosities. <inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">d</mml:mi></mml:msup></mml:math></inline-formula> Contact angles were determined by
photographing a series of five sucrose–water particles, each on a separate
hydrophobic slide. The contact angle was measured at the particle–substrate
interface of both the right and left edges of the particle using ImageJ
software. The mean contact angle was determined to be 98.5 <inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>, and
the lower and upper limits of contact angle were determined to be 94.8 and
102.2 <inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> (98.5 <inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> <inline-formula><mml:math display="inline"><mml:mo>±</mml:mo></mml:math></inline-formula> 1 <inline-formula><mml:math display="inline"><mml:mi mathvariant="italic">σ</mml:mi></mml:math></inline-formula>). The relationship between
the simulated viscosity of a particle and its contact angle is dependent upon
the dimensions of the particle, more specifically the value of the ratio
(<inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi>R</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>–<inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi>r</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub><mml:mo>)</mml:mo><mml:mo>/</mml:mo><mml:msub><mml:mi>r</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>. The lower limit of contact angle gave rise to the
lower limit of viscosity for particles where (<inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi>R</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>–<inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi>r</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub><mml:mo>)</mml:mo><mml:mo>/</mml:mo><mml:msub><mml:mi>r</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math display="inline"><mml:mo>&gt;</mml:mo></mml:math></inline-formula> 2,
whilst the upper limit of contact angle gave rise to the upper limit of
viscosity for particles where (<inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi>R</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>–<inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi>r</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub><mml:mo>)</mml:mo><mml:mo>/</mml:mo><mml:msub><mml:mi>r</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math display="inline"><mml:mo>&lt;</mml:mo></mml:math></inline-formula> 2.</p></table-wrap-foot></table-wrap>

<?xmltex \floatpos{t}?><table-wrap id="Ch1.T2" specific-use="star"><caption><p>Experimental parameters used when simulating flow with COMSOL for
experiments using polybutene standards.</p></caption><oasis:table frame="topbot"><?xmltex \begin{scaleboxenv}{.85}[.85]?><oasis:tgroup cols="6">
     <oasis:colspec colnum="1" colname="col1" align="justify" colwidth="85.358268pt"/>
     <oasis:colspec colnum="2" colname="col2" align="left"/>
     <oasis:colspec colnum="3" colname="col3" align="left"/>
     <oasis:colspec colnum="4" colname="col4" align="left"/>
     <oasis:colspec colnum="5" colname="col5" align="justify" colwidth="142.26378pt"/>
     <oasis:colspec colnum="6" colname="col6" align="justify" colwidth="142.26378pt"/>
     <oasis:thead>
       <oasis:row>  
         <oasis:entry colname="col1"/>  
         <oasis:entry colname="col2">Surface tension</oasis:entry>  
         <oasis:entry colname="col3">Slip length</oasis:entry>  
         <oasis:entry colname="col4">Density</oasis:entry>  
         <oasis:entry namest="col5" nameend="col6" align="center">Contact angle (<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>) </oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">  
         <oasis:entry colname="col1"/>  
         <oasis:entry colname="col2">(mN m<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula>)</oasis:entry>  
         <oasis:entry colname="col3">(m)</oasis:entry>  
         <oasis:entry colname="col4">(kg m<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">3</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula>)</oasis:entry>  
         <oasis:entry colname="col5">Standard #1 (N450000)</oasis:entry>  
         <oasis:entry colname="col6">Standard <inline-formula><mml:math display="inline"><mml:mrow><mml:mi mathvariant="italic">#</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:mrow></mml:math></inline-formula> (N2700000)</oasis:entry>
       </oasis:row>
     </oasis:thead>
     <oasis:tbody>
       <oasis:row>  
         <oasis:entry colname="col1">Range of values</oasis:entry>  
         <oasis:entry colname="col2">25–50<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">a</mml:mi></mml:msup></mml:math></inline-formula></oasis:entry>  
         <oasis:entry colname="col3">5 <inline-formula><mml:math display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">9</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula>–</oasis:entry>  
         <oasis:entry colname="col4">910–</oasis:entry>  
         <oasis:entry colname="col5">53.6–</oasis:entry>  
         <oasis:entry colname="col6">48.8–</oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">  
         <oasis:entry colname="col1"/>  
         <oasis:entry colname="col2"/>  
         <oasis:entry colname="col3">1 <inline-formula><mml:math display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:msup><mml:mn mathvariant="normal">5</mml:mn><mml:mi mathvariant="normal">b</mml:mi></mml:msup></mml:mrow></mml:msup></mml:math></inline-formula></oasis:entry>  
         <oasis:entry colname="col4">913<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">c</mml:mi></mml:msup></mml:math></inline-formula></oasis:entry>  
         <oasis:entry colname="col5">66.4<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">d</mml:mi></mml:msup></mml:math></inline-formula></oasis:entry>  
         <oasis:entry colname="col6">57.4<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">d</mml:mi></mml:msup></mml:math></inline-formula></oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">  
         <oasis:entry colname="col1">Value used to calculate lower limit of viscosity</oasis:entry>  
         <oasis:entry colname="col2">25</oasis:entry>  
         <oasis:entry colname="col3">5 <inline-formula><mml:math display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">9</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula></oasis:entry>  
         <oasis:entry colname="col4">910</oasis:entry>  
         <oasis:entry colname="col5">53.6 for particles of (<inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi>R</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>–<inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi>r</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub><mml:mo>)</mml:mo><mml:mo>/</mml:mo><mml:msub><mml:mi>r</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math display="inline"><mml:mo>&lt;</mml:mo></mml:math></inline-formula> 2 66.4 for particles of (<inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi>R</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>–<inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi>r</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub><mml:mo>)</mml:mo><mml:mo>/</mml:mo><mml:msub><mml:mi>r</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math display="inline"><mml:mo>&lt;</mml:mo></mml:math></inline-formula> 2</oasis:entry>  
         <oasis:entry colname="col6">48.8 for particles of (<inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi>R</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>–<inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi>r</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub><mml:mo>)</mml:mo><mml:mo>/</mml:mo><mml:msub><mml:mi>r</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math display="inline"><mml:mo>&lt;</mml:mo></mml:math></inline-formula> 2 57.4 for particles of (<inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi>R</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>–<inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi>r</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub><mml:mo>)</mml:mo><mml:mo>/</mml:mo><mml:msub><mml:mi>r</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math display="inline"><mml:mo>&gt;</mml:mo></mml:math></inline-formula> 2</oasis:entry>
       </oasis:row>
       <oasis:row>  
         <oasis:entry colname="col1">Value used to calculate upper limit of viscosity</oasis:entry>  
         <oasis:entry colname="col2">50</oasis:entry>  
         <oasis:entry colname="col3">1 <inline-formula><mml:math display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">5</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula></oasis:entry>  
         <oasis:entry colname="col4">910</oasis:entry>  
         <oasis:entry colname="col5">66.4 for particles of (<inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi>R</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>–<inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi>r</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub><mml:mo>)</mml:mo><mml:mo>/</mml:mo><mml:msub><mml:mi>r</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math display="inline"><mml:mo>&lt;</mml:mo></mml:math></inline-formula> 2 53.6 for particles of (<inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi>R</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>–<inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi>r</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub><mml:mo>)</mml:mo><mml:mo>/</mml:mo><mml:msub><mml:mi>r</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math display="inline"><mml:mo>&gt;</mml:mo></mml:math></inline-formula> 2</oasis:entry>  
         <oasis:entry colname="col6">53.6 for particles of (<inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi>R</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>–<inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi>r</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub><mml:mo>)</mml:mo><mml:mo>/</mml:mo><mml:msub><mml:mi>r</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math display="inline"><mml:mo>&lt;</mml:mo></mml:math></inline-formula> 2 66.4 for particles of (<inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi>R</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>–<inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi>r</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub><mml:mo>)</mml:mo><mml:mo>/</mml:mo><mml:msub><mml:mi>r</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math display="inline"><mml:mo>&gt;</mml:mo></mml:math></inline-formula> 2</oasis:entry>
       </oasis:row>
     </oasis:tbody>
   </oasis:tgroup><?xmltex \end{scaleboxenv}?></oasis:table><?xmltex \begin{scaleboxenv}{.85}[.85]?><table-wrap-foot><p><?xmltex \hack{\vspace{2mm}}?><inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">a</mml:mi></mml:msup></mml:math></inline-formula> Five studies have examined the surface tension of the
polybutene, with the reported values ranging from 29 to 34.3 mN m<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula>
<xref ref-type="bibr" rid="bib1.bibx37 bib1.bibx10 bib1.bibx20 bib1.bibx3 bib1.bibx23" id="paren.35"/>. As the polybutene standards studied here are unlikely to
differ much from those studied elsewhere, a conservative value of 25 mN m<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula> has been used as the lower limit of surface tension.
<xref ref-type="bibr" rid="bib1.bibx3" id="normal.36"/> studied three different polybutene resins of differing
viscosities. Measured surface tension values suggested a direct, though weak,
relationship between surface tension and viscosity (surface tension increased
from 29.3 to 30.0 mN m<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula> as the viscosity of the resins increased from 4
to 16.4 Pa s). As the resins studied by <xref ref-type="bibr" rid="bib1.bibx3" id="normal.37"/> were 2 orders
of magnitude less viscous than those measured herein, a conservative upper
estimate of 50 mN m<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula> has been used in simulations for the surface
tension of the polybutene standards. <inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">b</mml:mi></mml:msup></mml:math></inline-formula> This range is based on
experimental measurements of the slip length of water and organic compounds
on hydrophobic surfaces <xref ref-type="bibr" rid="bib1.bibx38 bib1.bibx6 bib1.bibx49 bib1.bibx2 bib1.bibx7 bib1.bibx47 bib1.bibx4 bib1.bibx12 bib1.bibx14 bib1.bibx26 bib1.bibx5 bib1.bibx13 bib1.bibx53 bib1.bibx21" id="paren.38"/>. <inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">c</mml:mi></mml:msup></mml:math></inline-formula> Measured by Cannon Instrument Company. A
density of 910 kg m<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">3</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula> was used for all simulations as density was found
to have no effect on simulated viscosities. <inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mi mathvariant="normal">d</mml:mi></mml:msup></mml:math></inline-formula> Contact angles
were determined as for sucrose–water particles (Table 1). For standard #1
(N450000) the lower and upper limits of contact angle were determined to be
53.6 and 66.4 <inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> (i.e. 60.0 <inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> <inline-formula><mml:math display="inline"><mml:mo>±</mml:mo></mml:math></inline-formula> 1<inline-formula><mml:math display="inline"><mml:mi mathvariant="italic">σ</mml:mi></mml:math></inline-formula>), whilst for
standard #2 (N2700000) the lower and upper limits of contact angle were
determined to be 48.8 and 57.4 <inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> (i.e.
53.1 <inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> <inline-formula><mml:math display="inline"><mml:mo>±</mml:mo></mml:math></inline-formula> 1<inline-formula><mml:math display="inline"><mml:mi mathvariant="italic">σ</mml:mi></mml:math></inline-formula>)</p></table-wrap-foot><?xmltex \end{scaleboxenv}?></table-wrap>

      <p>The values of certain physical properties could be defined for a given
simulation. The dimensions <inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi>R</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> and <inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi>r</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>, and the equilibrium contact angle
were determined from measurements, and the values of surface tension
(Surface 1, Fig. 2b), slip length (which describes the interaction at
Surface 2 in Fig. 2b), and the density of the material were determined based
on literature values. These values are detailed in Tables 1 and 2. For each
particle that was poked and formed a half-torus geometry, and was not
significantly influenced by scratches (determined visually, as discussed
above), lower and upper limits of viscosity were determined via simulations.
The dimensions of the particle (<inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi>R</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> and <inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi>r</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>) were used, as were the
relevant parameters in Table 1 (for particles of sucrose–water) or Table 2
(for particles of polybutene standards). Values from row 2 of Tables 1 and 2
were used for simulations of the lower limit of viscosity for a particle,
whilst values from row 3 of Tables 1 and 2 were used for simulations of its
upper limit of viscosity. The viscosity used in the simulations of a particle
was varied until <inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi mathvariant="italic">τ</mml:mi><mml:mtext>model, flow</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> agreed with the particles
<inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi mathvariant="italic">τ</mml:mi><mml:mtext>exp, flow</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> (to within 1 %).</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F5" specific-use="star"><caption><p>Optical images of particles of polybutene standards, <bold>(a)</bold>
standard #1 (N450000) and <bold>(b)</bold> standard #2 (N2700000), being poked
at 0 % RH recorded during typical poke-flow experiments. Images a1 and b1
correspond to particles prior to poking. Images a2 and b2 correspond to the
first frame post-poke (i.e. the first frame after the needle has been
removed). Images a3 and b3 correspond to images of the experimental flow
time, <inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi mathvariant="italic">τ</mml:mi><mml:mtext>exp, flow</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>, the point at which the equivalent area
diameter of the hole at the centre of the torus has decreased to 50 % of
its original size. Images a4 and b4 correspond to the final frame recorded of
each particle, at which point each particle has re-attained its original
spherical cap geometry. Size bar: 20 <inline-formula><mml:math display="inline"><mml:mi mathvariant="normal">µ</mml:mi></mml:math></inline-formula>m.</p></caption>
          <?xmltex \igopts{width=398.338583pt}?><graphic xlink:href="amt-2014-379-f05.png"/>

        </fig>

      <?xmltex \floatpos{t}?><fig id="Ch1.F6"><caption><p>Viscosity as a function of temperature for experiments with the
polybutene standards. Results from standard #1 (N450000) are in black, whilst
results from standard #2 (N2700000) are in red. Symbols represent values
measured by Cannon Instrument Company using a manual capillary viscometer.
Bars represent viscosities determined herein. For the bar that represents
each standard the bottom of the bar represents the lowest lower limit of
viscosity of all the particles examined, whilst the top of the bar represents
the highest upper limit of viscosity of all of the particles examined.</p></caption>
          <?xmltex \igopts{width=241.848425pt}?><graphic xlink:href="amt-2014-379-f06.png"/>

        </fig>

      <p>A proportion (<inline-formula><mml:math display="inline"><mml:mo>≈</mml:mo></mml:math></inline-formula> 30 %) of the sucrose–water particles that were
poked had dimensions where <inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi>r</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub><mml:mo>/</mml:mo><mml:msub><mml:mi>R</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math display="inline"><mml:mo>&gt;</mml:mo></mml:math></inline-formula> <inline-formula><mml:math display="inline"><mml:mo>≈</mml:mo></mml:math></inline-formula> 0.4. Simulations of the
lower limit of viscosity for many of these particles gave rise to a
non-physical geometry whereby the inner edge of the half torus geometry
appeared jagged and wavy – a phenomenon not observed during experiments.
Further study of this phenomenon revealed that this was the result of the
stretching of the mesh elements at the moving front of the particle, and use
of a finer mesh did not prevent this from occurring. As such, all
sucrose–water particles of dimensions <inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi>r</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub><mml:mo>/</mml:mo><mml:msub><mml:mi>R</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math display="inline"><mml:mo>&gt;</mml:mo></mml:math></inline-formula> <inline-formula><mml:math display="inline"><mml:mo>≈</mml:mo></mml:math></inline-formula> 0.4 were
removed from the study. No particles of the polybutene standard fell into
this size range.</p>
</sec>
</sec>
<sec id="Ch1.S3">
  <title>Results and discussion</title>
<sec id="Ch1.S3.SS1">
  <title>Sucrose–water particles</title>
      <p>Shown in Fig. 3 are examples of optical images of sucrose–water particles at
48.8, 52.7, and 58.8 % RH recorded during typical poke-flow experiments.
Prior to being poked the particles may be described geometrically as a
spherical cap (Fig. 3a1, b1 and c1). Just after being poked the geometry of
the particles can be described as a half torus – a ring of material with a
hole at its centre (Fig. 3a2, b2, and c2), which is energetically
unfavourable compared to that of a spherical cap. For the particles in
Fig. 3, <inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi mathvariant="italic">τ</mml:mi><mml:mtext>exp, flow</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> was determined to be 11.25, 3.75, and 1.25 s at
48.8, 52.7, and 58.8 % RH, respectively (Fig. 3a3, b3, and c3). Following
<inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi mathvariant="italic">τ</mml:mi><mml:mtext>exp, flow</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> the material continued to flow, and eventually
re-attained its initial, energetically favourable, spherical cap geometry
(Fig. 3a4, b4, and c4).</p>
      <p>The <inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi mathvariant="italic">τ</mml:mi><mml:mtext>exp, flow</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> values of each of the individual sucrose–water
particles poked and analysed is shown in Fig. 4a. Experimental flow times
increased from <inline-formula><mml:math display="inline"><mml:mo>≈</mml:mo></mml:math></inline-formula> 150 ms at 59 % RH to <inline-formula><mml:math display="inline"><mml:mo>≈</mml:mo></mml:math></inline-formula> 40 min at
37 % RH. The millisecond time resolution of the camera precluded
experiments being performed at RH <inline-formula><mml:math display="inline"><mml:mo>&gt;</mml:mo></mml:math></inline-formula> 60 % as the closure time for the
sucrose–water particles was too fast to measure. Lower and upper limits of
viscosity were determined for each individual particle using their dimensions
and <inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi mathvariant="italic">τ</mml:mi><mml:mtext>exp, flow</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> (Fig. 4b). Between 59 and 36 % RH,
the viscosities for individual sucrose–water particles range from
1.0 <inline-formula><mml:math display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">1</mml:mn></mml:msup></mml:math></inline-formula> to 6.6 <inline-formula><mml:math display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">6</mml:mn></mml:msup></mml:math></inline-formula> Pa s, with the upper limit of
viscosity for a given particle being a factor of 16 to a factor of 140 larger
than the corresponding lower limit of viscosity, with the uncertainty mainly
due to the value of the physical properties used during simulations.</p>
      <p>In Fig. 4c, the viscosities of individual particles are grouped by RH, and
previously reported values of the viscosity of sucrose–water particles are
included for comparison <xref ref-type="bibr" rid="bib1.bibx45 bib1.bibx31 bib1.bibx30" id="paren.39"/>.
Viscosities have been determined by grouping particles based upon RH, with
lower and upper limits of viscosity from particles in the group reported. The
lower and upper limits of viscosity of the group of particles poked at
<inline-formula><mml:math display="inline"><mml:mo>≈</mml:mo></mml:math></inline-formula> 59 % RH are 1.0 <inline-formula><mml:math display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">1</mml:mn></mml:msup></mml:math></inline-formula> and
1.6 <inline-formula><mml:math display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">4</mml:mn></mml:msup></mml:math></inline-formula> Pa s, whilst at 37 % RH the corresponding values
are 7.2 <inline-formula><mml:math display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">4</mml:mn></mml:msup></mml:math></inline-formula> and 4.7 <inline-formula><mml:math display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">6</mml:mn></mml:msup></mml:math></inline-formula> Pa s, respectively. As
shown in Fig. 4c, the results are in good agreement with
<xref ref-type="bibr" rid="bib1.bibx31" id="normal.40"/>, who measured a viscosity of 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">3</mml:mn></mml:msup></mml:math></inline-formula> Pa s at 54 %
RH using a rotational controlled stress rheometer, and with <?xmltex \hack{\mbox\bgroup}?><xref ref-type="bibr" rid="bib1.bibx30" id="normal.41"/><?xmltex \hack{\egroup}?>,
who recently reported mean measured viscosities of
<inline-formula><mml:math display="inline"><mml:mo>≈</mml:mo></mml:math></inline-formula> 5 <inline-formula><mml:math display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msup></mml:math></inline-formula> to <inline-formula><mml:math display="inline"><mml:mo>≈</mml:mo></mml:math></inline-formula> 3 <inline-formula><mml:math display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">6</mml:mn></mml:msup></mml:math></inline-formula> Pa s
between 60 and 37 % RH using holographic optical tweezers.</p>
</sec>
<sec id="Ch1.S3.SS2">
  <title>Particles of polybutene standards</title>
      <p>Figure 5 shows examples of optical images of particles of the polybutene
standards recorded during poke-flow experiments at 0 % RH. As for
sucrose–water particles, the geometry of the particles of standard solution
could be described as a spherical cap prior to being poked (Fig. 5a1 and b1)
and a half-torus after being poked (Fig. 5a2 and b2). Upon removal of the
needle the material flowed, with the size of the hole at the centre of the
half-torus geometry decreasing over time. For the particles in Fig. 5,
<inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi mathvariant="italic">τ</mml:mi><mml:mtext>exp, flow</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> was determined to be 2.50 and 6.00 s, respectively
(Fig. 5a3 and b3). The particle continued to flow after <inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi mathvariant="italic">τ</mml:mi><mml:mtext>exp,
flow</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> and eventually re-attained its initial, energetically favourable,
spherical cap geometry (Fig. 5a4 and b4). The mean experimental flow times,
<inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi mathvariant="italic">τ</mml:mi><mml:mtext>exp, flow</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>, were 2.79 s (<inline-formula><mml:math display="inline"><mml:mrow><mml:mi mathvariant="italic">σ</mml:mi><mml:mo>=</mml:mo><mml:mn>0.39</mml:mn></mml:mrow></mml:math></inline-formula>) for the lower
viscosity standard #1 and 7.86 s (<inline-formula><mml:math display="inline"><mml:mrow><mml:mi mathvariant="italic">σ</mml:mi><mml:mo>=</mml:mo><mml:mn>1.65</mml:mn></mml:mrow></mml:math></inline-formula>) for the higher
viscosity standard #2.</p>
      <p>As done in the sucrose–water experiments, <inline-formula><mml:math display="inline"><mml:mrow><mml:msub><mml:mi mathvariant="italic">τ</mml:mi><mml:mtext>exp, flow</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> values from
individual particles were converted into viscosities using simulations. To
determine upper and lower limits for the viscosities of the standards, we
took the upper and lower limits of the viscosities determined from the
individual particles. Using this approach and the parameters listed in
Table 2, the simulated lower and upper limits of viscosity for the particles
poked were 2.0 <inline-formula><mml:math display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msup></mml:math></inline-formula> and 1.2 <inline-formula><mml:math display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">4</mml:mn></mml:msup></mml:math></inline-formula> Pa s for
standard #1 (N450000), and 3.1 <inline-formula><mml:math display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msup></mml:math></inline-formula> and
2.4 <inline-formula><mml:math display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">4</mml:mn></mml:msup></mml:math></inline-formula> Pa s for standard #2 (N2700000). These values are in
good agreement with value reported by the manufacturer, Cannon Instrument
Company (see Fig. 6).</p>
</sec>
</sec>
<sec id="Ch1.S4" sec-type="conclusions">
  <title>Summary</title>
      <p>The poke-flow technique combined with simulations of fluid flow provides the
advantage of being able to measure viscosities of samples that are both
highly viscous and available only in small sample volumes. The combination of
these characteristics provides a challenge that is beyond the reach of
current commercially available viscometers. In <xref ref-type="bibr" rid="bib1.bibx33" id="normal.42"/>,
only a preliminary validation of the poke-flow technique combined with
simulations of fluid flow was carried out for viscosities up to
10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">4</mml:mn></mml:msup></mml:math></inline-formula> Pa s, due to the lack of suitable standards for validation at the
time of publication. The current manuscript expands on the initial validation
experiments by <xref ref-type="bibr" rid="bib1.bibx33" id="normal.43"/>. First, the approach was used to
determine the viscosity of sucrose–water particles over a wider range of
RHs than previously done by <xref ref-type="bibr" rid="bib1.bibx33" id="normal.44"/>. The
lower and upper limits of viscosity at <inline-formula><mml:math display="inline"><mml:mo>≈</mml:mo></mml:math></inline-formula> 59 % RH were
1.0 <inline-formula><mml:math display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">1</mml:mn></mml:msup></mml:math></inline-formula> and 1.6 <inline-formula><mml:math display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">4</mml:mn></mml:msup></mml:math></inline-formula> Pa s, whilst at 37 % RH
the corresponding values were 7.2 <inline-formula><mml:math display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">4</mml:mn></mml:msup></mml:math></inline-formula> and
4.7 <inline-formula><mml:math display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">6</mml:mn></mml:msup></mml:math></inline-formula> Pa s, respectively. The results are in good agreement
with <xref ref-type="bibr" rid="bib1.bibx31" id="normal.45"/>, who measured a viscosity of 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">3</mml:mn></mml:msup></mml:math></inline-formula> Pa s at
54 % RH using a rotational controlled stress rheometer, and with
<xref ref-type="bibr" rid="bib1.bibx30" id="normal.46"/>, who recently reported that measured mean viscosities of
<inline-formula><mml:math display="inline"><mml:mo>≈</mml:mo></mml:math></inline-formula> 5 <inline-formula><mml:math display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msup></mml:math></inline-formula> to <inline-formula><mml:math display="inline"><mml:mo>≈</mml:mo></mml:math></inline-formula> 3 <inline-formula><mml:math display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">6</mml:mn></mml:msup></mml:math></inline-formula> Pa s
between 60 and 37 % RH using holographic optical tweezers.</p>
      <p>Second, the approach was used to determine the viscosity of two polybutene
standards. The simulated lower and upper limits of viscosity for standard #1
was 2.0 <inline-formula><mml:math display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msup></mml:math></inline-formula> and 1.6 <inline-formula><mml:math display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">4</mml:mn></mml:msup></mml:math></inline-formula> Pa s, and for standard
#2 1.6 <inline-formula><mml:math display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msup></mml:math></inline-formula> and 2.6 <inline-formula><mml:math display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">4</mml:mn></mml:msup></mml:math></inline-formula> Pa s. These values are
in good agreement with values reported by Cannon Instrument Company (see
Fig. 6).</p>
      <p>The results for both the sucrose–water particles and the polybutene standards
show the poke-flow technique combined with simulations of fluid flow is
capable of providing both lower and upper limits of viscosity that are
consistent with literature or measured values when the viscosity is in the
range of <inline-formula><mml:math display="inline"><mml:mo>≈</mml:mo></mml:math></inline-formula> 5 <inline-formula><mml:math display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msup></mml:math></inline-formula> to
<inline-formula><mml:math display="inline"><mml:mo>≈</mml:mo></mml:math></inline-formula> 3 <inline-formula><mml:math display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<inline-formula><mml:math display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">6</mml:mn></mml:msup></mml:math></inline-formula> Pa s. This covers an important part of the
range of viscosities of secondary organic material generated in environmental
chambers. For example, this range of viscosities has been measured at
atmospherically relevant RHs for both the water-soluble fraction of the SOM
produced via the ozonolysis of <inline-formula><mml:math display="inline"><mml:mi mathvariant="italic">α</mml:mi></mml:math></inline-formula>-pinene <xref ref-type="bibr" rid="bib1.bibx33" id="paren.47"/>
and the total SOM produced via that of isoprene <xref ref-type="bibr" rid="bib1.bibx44" id="paren.48"/>.
In addition, this technique has several advantages, including being low in
cost and the experimental setup affording compatibility with cascade
impactors for particle collection.</p>
      <p><?xmltex \hack{\newpage}?>Whilst the poke-flow technique combined with simulations of fluid flow gives
good agreement with measured values, the upper limit of viscosity for a given
particle is typically a factor of 16–140 larger than the corresponding lower
limit of viscosity. Thus, the limits of viscosity determined using this
approach are wide. The largest source of uncertainty in the approach is the
values of surface tension and slip length used in the simulations.
Constraining these values could lead to a reduction in the uncertainty of the
measurements.</p>
</sec>

      
      </body>
    <back><ack><title>Acknowledgements</title><p>We thank the Natural Science and Engineering Research Council of Canada for
funding and the Laboratory for Advanced Spectroscopy and Imaging Research
facility at the University of British Columbia for use of the microscope used
in these experiments. <?xmltex \hack{\newline}?><?xmltex \hack{\newline}?> Edited by: F. Pope</p></ack><ref-list>
    <title>References</title>

      <ref id="bib1.bibx1"><label>Baltensperger et al.(2008)Baltensperger, Dommen, Alfarra, Duplissy,
Gaeggeler, Metzger, Facchini, Decesari, Finessi, Reinnig, Schott, Warnke,
HOFFMANN, Klatzer, Puxbaum, Geiser, Savi, Lang, Kalberer, and
Geiser</label><mixed-citation>
Baltensperger, U., Dommen, J., Alfarra, M. R., Duplissy, J., Gaeggeler, K.,
Metzger, A., Facchini, M. C., Decesari, S., Finessi, E., Reinnig, C., Schott,
M., Warnke, J., HOFFMANN, T., Klatzer, B., Puxbaum, H., Geiser, M., Savi, M.,
Lang, D., Kalberer, M., and Geiser, T.: Combined Determination of the
Chemical Composition and of Health Effects of Secondary Organic Aerosols: The
POLYSOA Project, J. Aerosol. Med. Pulm. Drug. Deliv., 21, 145–154,
2008.</mixed-citation></ref>
      <ref id="bib1.bibx2"><label>Baudry et al.(2001)Baudry, Charlaix, Tonck, and
Mazuyer</label><mixed-citation>
Baudry, J., Charlaix, E., Tonck, A., and Mazuyer, D.: Experimental Evidence
for a Large Slip Effect at a Nonwetting Fluid-Solid Interface, Langmuir, 17,
5232–5236,  2001.</mixed-citation></ref>
      <ref id="bib1.bibx3"><label>Blunk and Wilkes(2001)</label><mixed-citation>Blunk, R. and Wilkes, J. O.: Surface-tension-driven flows of coatings:
Bondline readout formation – Springer, J. Coating. Tech., 73, 63–71, <ext-link xlink:href="http://dx.doi.org/10.1007/Bf02698025" ext-link-type="DOI">10.1007/Bf02698025</ext-link>, 2001.</mixed-citation></ref>
      <ref id="bib1.bibx4"><label>Cheng and Giordano(2002)</label><mixed-citation>Cheng, J. T. and Giordano, N.: Fluid flow through nanometer-scale channels,
Phys. Rev. E., 65, 031206, <ext-link xlink:href="http://dx.doi.org/10.1103/PhysRevE.65.031206" ext-link-type="DOI">10.1103/PhysRevE.65.031206</ext-link>, 2002.</mixed-citation></ref>
      <ref id="bib1.bibx5"><label>Choi and Kim(2006)</label><mixed-citation>Choi, C.-H. and Kim, C.-J.: Large Slip of Aqueous Liquid Flow over a
Nanoengineered Superhydrophobic Surface, Phys. Rev. Lett., 96,
066001, <ext-link xlink:href="http://dx.doi.org/10.1103/PhysRevLett.96.066001" ext-link-type="DOI">10.1103/PhysRevLett.96.066001</ext-link>, 2006.</mixed-citation></ref>
      <ref id="bib1.bibx6"><label>Churaev et al.(1984)Churaev, Sobolev, and Somov</label><mixed-citation>
Churaev, N. V., Sobolev, V. D., and Somov, A. N.: Slippage of liquids over
lyophobic solid surfaces, J. Coll. Inter. Sci., 97,
574–581,  1984.</mixed-citation></ref>
      <ref id="bib1.bibx7"><label>Craig et al.(2001)Craig, Neto, and Williams</label><mixed-citation>Craig, V. S., Neto, C., and Williams, D. R.: Shear-dependent boundary slip
in
an aqueous Newtonian liquid., Phys. Rev. Lett., 87, 054504, <ext-link xlink:href="http://dx.doi.org/10.1103/Physrevlett.87.054504" ext-link-type="DOI">10.1103/Physrevlett.87.054504</ext-link>, 2001.</mixed-citation></ref>
      <ref id="bib1.bibx8"><label>Hosny et al.(2013)Hosny, Fitzgerald, Tong, Kalberer, Kuimova, and
Pope</label><mixed-citation>Hosny, N. A., Fitzgerald, C., Tong, C., Kalberer, M., Kuimova, M. K., and
Pope,
F. D.: Fluorescent lifetime imaging of atmospheric aerosols: a direct probe
of aerosol viscosity, Faraday Discuss., 165, 343–356,
<ext-link xlink:href="http://dx.doi.org/10.1039/c3fd00041a" ext-link-type="DOI">10.1039/c3fd00041a</ext-link>, 2013.</mixed-citation></ref>
      <ref id="bib1.bibx9"><label>Jang et al.(2006)Jang, Ghio, and Cao</label><mixed-citation>
Jang, M., Ghio, A. J., and Cao, G.: Exposure of BEAS-2B cells to secondary
organic aerosol coated on magnetic nanoparticles., Chem. Res.
Toxicol., 19, 1044–1050,  2006.</mixed-citation></ref>
      <ref id="bib1.bibx10"><label>Jeong and Moffatt(1992)</label><mixed-citation>
Jeong, J. T. and Moffatt, H. K.: Free-surface cusps associated with flow at
low Reynolds number, J. Fluid Mechan., 241, 1–22, 1992.</mixed-citation></ref>
      <ref id="bib1.bibx11"><label>Jimenez et al.(2009)Jimenez, Canagaratna, Donahue, Prevot, Zhang,
Kroll, DeCarlo, Allan, Coe, Ng, Aiken, Docherty, Ulbrich, Grieshop, Robinson,
Duplissy, Smith, Wilson, Lanz, Hueglin, Sun, Tian, Laaksonen, Raatikainen,
Rautiainen, Vaattovaara, Ehn, Kulmala, Tomlinson, Collins, Cubison, Dunlea,
Huffman, Onasch, Alfarra, Williams, Bower, Kondo, Schneider, Drewnick,
Borrmann, Weimer, Demerjian, Salcedo, Cottrell, Griffin, Takami, Miyoshi,
Hatakeyama, Shimono, Sun, Zhang, Dzepina, Kimmel, Sueper, Jayne, Herndon,
Trimborn, Williams, Wood, Middlebrook, Kolb, Baltensperger, and
Worsnop</label><mixed-citation>
Jimenez, J. L., Canagaratna, M. R., Donahue, N. M., Prevot, A. S. H., Zhang,
Q., Kroll, J. H., DeCarlo, P. F., Allan, J. D., Coe, H., Ng, N. L., Aiken,
A. C., Docherty, K. S., Ulbrich, I. M., Grieshop, A. P., Robinson, A. L.,
Duplissy, J., Smith, J. D., Wilson, K. R., Lanz, V. A., Hueglin, C., Sun,
Y. L., Tian, J., Laaksonen, A., Raatikainen, T., Rautiainen, J., Vaattovaara,
P., Ehn, M., Kulmala, M., Tomlinson, J. M., Collins, D. R., Cubison, M. J.,
Dunlea, E. J., Huffman, J. A., Onasch, T. B., Alfarra, M. R., Williams,
P. I., Bower, K., Kondo, Y., Schneider, J., Drewnick, F., Borrmann, S.,
Weimer, S., Demerjian, K., Salcedo, D., Cottrell, L., Griffin, R., Takami,
A., Miyoshi, T., Hatakeyama, S., Shimono, A., Sun, J. Y., Zhang, Y. M.,
Dzepina, K., Kimmel, J. R., Sueper, D., Jayne, J. T., Herndon, S. C.,
Trimborn, A. M., Williams, L. R., Wood, E. C., Middlebrook, A. M., Kolb,
C. E., Baltensperger, U., and Worsnop, D. R.: Evolution of organic aerosols
in the atmosphere., Science (New York, N.Y.), 326, 1525–1529,
2009.</mixed-citation></ref>
      <ref id="bib1.bibx12"><label>Jin et al.(2004)Jin, Huang, Park, Yoo, and Breuer</label><mixed-citation>
Jin, S., Huang, P., Park, J., Yoo, J. Y., and Breuer, K. S.: Near-surface
velocimetry using evanescent wave illumination, Experim. Fluids, 37,
825–833,  2004.</mixed-citation></ref>
      <ref id="bib1.bibx13"><label>Joly et al.(2006)Joly, Ybert, and Bocquet</label><mixed-citation>Joly, L., Ybert, C., and Bocquet, L.: Probing the nanohydrodynamics at
liquid-solid interfaces using thermal motion, Phys. Rev. Lett., 96,
046101, <ext-link xlink:href="http://dx.doi.org/10.1103/Physrevlett.96.046101" ext-link-type="DOI">10.1103/Physrevlett.96.046101</ext-link>, 2006.</mixed-citation></ref>
      <ref id="bib1.bibx14"><label>Joseph and Tabeling(2005)</label><mixed-citation>Joseph, P. and Tabeling, P.: Direct measurement of the apparent slip
length,
Phys. Rev. E, 71, 035303, <ext-link xlink:href="http://dx.doi.org/10.1103/Physreve.71.035303" ext-link-type="DOI">10.1103/Physreve.71.035303</ext-link>, 2005.</mixed-citation></ref>
      <ref id="bib1.bibx15"><label>Kanakidou et al.(2005)Kanakidou, Seinfeld, Pandis, Barnes, Dentener,
Facchini, Van Dingenen, Ervens, Nenes, Nielsen, Swietlicki, Putaud,
Balkanski, Fuzzi, Horth, Moortgat, Winterhalter, Myhre, Tsigaridis, Vignati,
Stephanou, and Wilson</label><mixed-citation>Kanakidou, M., Seinfeld, J. H., Pandis, S. N., Barnes, I., Dentener, F. J.,
Facchini, M. C., Van Dingenen, R., Ervens, B., Nenes, A., Nielsen, C. J.,
Swietlicki, E., Putaud, J. P., Balkanski, Y., Fuzzi, S., Horth, J., Moortgat,
G. K., Winterhalter, R., Myhre, C. E. L., Tsigaridis, K., Vignati, E.,
Stephanou, E. G., and Wilson, J.: Organic aerosol and global climate
modelling: a review, Atmos. Chem. Phys., 5, 1053–1123,
<ext-link xlink:href="http://dx.doi.org/10.5194/acp-5-1053-2005" ext-link-type="DOI">10.5194/acp-5-1053-2005</ext-link>, 2005.</mixed-citation></ref>
      <ref id="bib1.bibx16"><label>Kidd et al.(2014)Kidd, Perraud, Wingen, and
Finlayson-Pitts</label><mixed-citation>Kidd, C., Perraud, V., Wingen, L. M., and Finlayson-Pitts, B. J.:
Integrating
phase and composition of secondary organic aerosol from the ozonolysis of
<inline-formula><mml:math display="inline"><mml:mi mathvariant="italic">α</mml:mi></mml:math></inline-formula>-pinene, Proc. Natl. Acad. Sci.
USA, 111, 7552–7557, 2014.</mixed-citation></ref>
      <ref id="bib1.bibx17"><label>Koop et al.(2000)Koop, Kapilashrami, Molina, and
Molina</label><mixed-citation>Koop, T., Kapilashrami, A., Molina, L. T., and Molina, M. J.: Phase
transitions of sea-salt/water mixtures at low temperatures: Implications for
ozone chemistry in the polar marine boundary layer, J. Geophys.
Res., 105, 26393, <ext-link xlink:href="http://dx.doi.org/10.1029/2000JD900413" ext-link-type="DOI">10.1029/2000JD900413</ext-link>, 2000.</mixed-citation></ref>
      <ref id="bib1.bibx18"><label>Koop et al.(2011)Koop, Bookhold, Shiraiwa, and
Pöschl</label><mixed-citation>
Koop, T., Bookhold, J., Shiraiwa, M., and Pöschl, U.: Glass transition
and
phase state of organic compounds: dependency on molecular properties and
implications for secondary organic aerosols in the atmosphere, Phys.
Chem. Chem. Phys., 13, 19238–19255,
2011.</mixed-citation></ref>
      <ref id="bib1.bibx19"><label>Kuwata and Martin(2012)</label><mixed-citation>
Kuwata, M. and Martin, S. T.: Phase of atmospheric secondary organic
material
affects its reactivity, Proc. Natl. Acad. Sci.
USA, 109, 17354–17359,
2012.</mixed-citation></ref>
      <ref id="bib1.bibx20"><label>Lewandowski and Dupuis(1994)</label><mixed-citation>
Lewandowski, F. Y. and Dupuis, D.: Dynamic measurements of surface tension
of
solutions of polyisobutylene in mixtures of polybutene oil and Decalin, J.
Non-Newton. Fluid, 52, 233–248,  1994.</mixed-citation></ref>
      <ref id="bib1.bibx21"><label>Li et al.(2014)Li, Jing, Pan, and Ahmad</label><mixed-citation>
Li, D. Y., Jing, D. L., Pan, Y. L., and Ahmad, K.: Slip Length Measurement
of
Water Flow on Graphite Surface Using Atomic Force Microscope, Adv.
Material. Res., 941–944, 1581–1584, 2014.</mixed-citation></ref>
      <ref id="bib1.bibx22"><label>MacDonald et al.(1996)MacDonald, Lanier, Swaisgood, and
Hamann</label><mixed-citation>
MacDonald, G. A., Lanier, T. C., Swaisgood, H. E., and Hamann, D. D.:
Mechanism for Stabilization of Fish Actomyosin by Sodium Lactate, J.
Agricul. Food Chem., 44, 106–112,
1996.</mixed-citation></ref>
      <ref id="bib1.bibx23"><label>Mewis and Metzner(2006)</label><mixed-citation>Mewis, J. and Metzner, A. B.: The rheological properties of suspensions of
fibres in Newtonian fluids subjected to extensional deformations, J.
Fluid Mechan., 62, 593–600, <ext-link xlink:href="http://dx.doi.org/10.1017/S0022112074000826" ext-link-type="DOI">10.1017/S0022112074000826</ext-link>, 2006.</mixed-citation></ref>
      <ref id="bib1.bibx24"><label>Murray et al.(2010)Murray, Wilson, Dobbie, Cui, Al-Jumur, Möhler,
Schnaiter, Wagner, Benz, Niemand, Saathoff, Ebert, Wagner, and
Kärcher</label><mixed-citation>
Murray, B. J., Wilson, T. W., Dobbie, S., Cui, Z., Al-Jumur, S. M. R. K.,
Möhler, O., Schnaiter, M., Wagner, R., Benz, S., Niemand, M., Saathoff,
H., Ebert, V., Wagner, S., and Kärcher, B.: Heterogeneous nucleation of
ice particles on glassy aerosols under cirrus conditions, Nat. Geosci.,
3, 233–237,  2010.</mixed-citation></ref>
      <ref id="bib1.bibx25"><label>Murray et al.(2012)Murray, Haddrell, Peppe, Davies, Reid, O'Sullivan,
Price, Kumar, Saunders, Plane, Umo, and Wilson</label><mixed-citation>Murray, B. J., Haddrell, A. E., Peppe, S., Davies, J. F., Reid, J. P.,
O'Sullivan, D., Price, H. C., Kumar, R., Saunders, R. W., Plane, J. M. C.,
Umo, N. S., and Wilson, T. W.: Glass formation and unusual hygroscopic growth
of iodic acid solution droplets with relevance for iodine mediated particle
formation in the marine boundary layer, Atmos. Chem. Phys., 12, 8575–8587,
<ext-link xlink:href="http://dx.doi.org/10.5194/acp-12-8575-2012" ext-link-type="DOI">10.5194/acp-12-8575-2012</ext-link>, 2012.</mixed-citation></ref>
      <ref id="bib1.bibx26"><label>Neto et al.(2005)Neto, Evans, Bonaccurso, Butt, and
Craig</label><mixed-citation>
Neto, C., Evans, D. R., Bonaccurso, E., Butt, H.-J., and Craig, V. S. J.:
Boundary slip in Newtonian liquids: a review of experimental studies,
Reports Prog. Phys., 68, 2859–2897, 2005.</mixed-citation></ref>
      <ref id="bib1.bibx27"><label>Pajunoja et al.(2014)Pajunoja, Malila, Hao, Joutsensaari, Lehtinen,
and Virtanen</label><mixed-citation>
Pajunoja, A., Malila, J., Hao, L., Joutsensaari, J., Lehtinen, K. E. J., and
Virtanen, A.: Estimating the Viscosity Range of SOA Particles Based on Their
Coalescence Time, Aerosol Sci. Tech., 48, i–iv, 2014.</mixed-citation></ref>
      <ref id="bib1.bibx28"><label>Perraud et al.(2012)Perraud, Bruns, Ezell, Johnson, Yu, Alexander,
Zelenyuk, Imre, Chang, Dabdub, Pankow, and Finlayson-Pitts</label><mixed-citation>
Perraud, V., Bruns, E. A., Ezell, M. J., Johnson, S. N., Yu, Y., Alexander,
M. L., Zelenyuk, A., Imre, D., Chang, W. L., Dabdub, D., Pankow, J. F., and
Finlayson-Pitts, B. J.: Nonequilibrium atmospheric secondary organic aerosol
formation and growth., Proc. Natl. Acad. Sci.
USA, 109, 2836–2841,  2012.</mixed-citation></ref>
      <ref id="bib1.bibx29"><label>Power and Reid(2014)</label><mixed-citation>Power, R. M. and Reid, J. P.: Probing the micro-rheological properties of
aerosol particles using optical tweezers, Reports  Prog. Phys.,
77, 074601, <ext-link xlink:href="http://dx.doi.org/10.1088/0034-4885/77/7/074601" ext-link-type="DOI">10.1088/0034-4885/77/7/074601</ext-link>, 2014.</mixed-citation></ref>
      <ref id="bib1.bibx30"><label>Power et al.(2013)Power, Simpson, Reid, and Hudson</label><mixed-citation>
Power, R. M., Simpson, S. H., Reid, J. P., and Hudson, A. J.: The transition
from liquid to solid-like behaviour in ultrahigh viscosity aerosol
particles, Chem. Sci., 4, 2597–2604, 2013.</mixed-citation></ref>
      <ref id="bib1.bibx31"><label>Quintas et al.(2006)Quintas, Brandão, Silva, and
Cunha</label><mixed-citation>
Quintas, M., Brandão, T. R. S., Silva, C. L. M., and Cunha, R. L.:
Rheology of supersaturated sucrose solutions, J. Food Eng., 77, 844–852,
2006.</mixed-citation></ref>
      <ref id="bib1.bibx32"><label>Reist(1992)</label><mixed-citation>
Reist, P.: Aerosol Science and Technology, McGraw-Hill Professional, New
York, NY, USA, 2 Edn., 1992.</mixed-citation></ref>
      <ref id="bib1.bibx33"><label>Renbaum-Wolff et al.(2013a)Renbaum-Wolff, Grayson,
Bateman, Kuwata, Sellier, Murray, Shilling, Martin, and
Bertram</label><mixed-citation>Renbaum-Wolff, L., Grayson, J. W., Bateman, A. P., Kuwata, M., Sellier, M.,
Murray, B. J., Shilling, J. E., Martin, S. T., and Bertram, A. K.: Viscosity
of <inline-formula><mml:math display="inline"><mml:mi mathvariant="italic">α</mml:mi></mml:math></inline-formula>-pinene secondary organic material and implications for particle
growth and reactivity., Proc. Natl. Acad. Sci.
USA, 110, 8014–8019,
2013a.</mixed-citation></ref>
      <ref id="bib1.bibx34"><label>Renbaum-Wolff et al.(2013b)Renbaum-Wolff, Grayson, and
Bertram</label><mixed-citation>Renbaum-Wolff, L., Grayson, J. W., and Bertram, A. K.: Technical Note: New
methodology for measuring viscosities in small volumes characteristic of
environmental chamber particle samples, Atmos. Chem. Phys., 13, 791–802,
<ext-link xlink:href="http://dx.doi.org/10.5194/acp-13-791-2013" ext-link-type="DOI">10.5194/acp-13-791-2013</ext-link>, 2013b.</mixed-citation></ref>
      <ref id="bib1.bibx35"><label>Riipinen et al.(2011)Riipinen, Pierce, Yli-Juuti, Nieminen,
Häkkinen, Ehn, Junninen, Lehtipalo, Petäjä, Slowik, Chang,
Shantz, Abbatt, Leaitch, Kerminen, Worsnop, Pandis, Donahue, and
Kulmala</label><mixed-citation>Riipinen, I., Pierce, J. R., Yli-Juuti, T., Nieminen, T., Häkkinen, S.,
Ehn, M., Junninen, H., Lehtipalo, K., Petäjä, T., Slowik, J., Chang,
R., Shantz, N. C., Abbatt, J., Leaitch, W. R., Kerminen, V.-M., Worsnop,
D. R., Pandis, S. N., Donahue, N. M., and Kulmala, M.: Organic condensation:
a vital link connecting aerosol formation to cloud condensation nuclei (CCN)
concentrations, Atmos. Chem. Phys., 11, 3865–3878,
<ext-link xlink:href="http://dx.doi.org/10.5194/acp-11-3865-2011" ext-link-type="DOI">10.5194/acp-11-3865-2011</ext-link>, 2011.</mixed-citation></ref>
      <ref id="bib1.bibx36"><label>Riipinen et al.(2012)Riipinen, Yli-Juuti, Pierce, Petäjä,
Worsnop, Kulmala, and Donahue</label><mixed-citation>
Riipinen, I., Yli-Juuti, T., Pierce, J. R., Petäjä, T., Worsnop,
D. R.,
Kulmala, M., and Donahue, N. M.: The contribution of organics to atmospheric
nanoparticle growth, Nat. Geosci., 5, 453–458,
2012.</mixed-citation></ref>
      <ref id="bib1.bibx37"><label>Roe(1968)</label><mixed-citation>
Roe, R.-J.: Surface tension of polymer liquids, J. Phys.
Chem., 72, 2013–2017, 1968.</mixed-citation></ref>
      <ref id="bib1.bibx38"><label>Schnell(1956)</label><mixed-citation>
Schnell, E.: Slippage of Water over Nonwettable Surfaces, J. Appl.
Phys., 10, 1149–1152, 1956.</mixed-citation></ref>
      <ref id="bib1.bibx39"><label>Shiraiwa and Seinfeld(2012)</label><mixed-citation>Shiraiwa, M. and Seinfeld, J. H.: Equilibration timescale of atmospheric
secondary organic aerosol partitioning, Geophys. Res. Lett., 39,
L24801, <ext-link xlink:href="http://dx.doi.org/10.1029/2012gl054008" ext-link-type="DOI">10.1029/2012gl054008</ext-link>, 2012.</mixed-citation></ref>
      <ref id="bib1.bibx40"><label>Shiraiwa et al.(2011)Shiraiwa, Ammann, Koop, and
Pöschl</label><mixed-citation>
Shiraiwa, M., Ammann, M., Koop, T., and Pöschl, U.: Gas uptake and
chemical aging of semisolid organic aerosol particles, Proc.
Natl. Acad. Sci. USA, 108,
11003–11008, 2011.</mixed-citation></ref>
      <ref id="bib1.bibx41"><label>Shiraiwa et al.(2013)Shiraiwa, Zuend, Bertram, and
Seinfeld</label><mixed-citation>
Shiraiwa, M., Zuend, A., Bertram, A. K., and Seinfeld, J. H.: Gas-particle
partitioning of atmospheric aerosols: interplay of physical state, non-ideal
mixing and morphology, Phys. Chem. Chem. Phys., 15,
11441–11453,  2013.</mixed-citation></ref>
      <ref id="bib1.bibx42"><label>Solomon et al.(2007)Solomon, Qin, Manning, Alley, Bernsten, Bindoff,
Chen, Chidthaisong, Gregory, GC, Heimann, Hewiston, Hoskins, Joos, Jouzel,
Kattsov, Lohmann, Matsuno, Molina, Nicholls, Overpeck, Raga, Ramaswamy, Ren,
Rusticucci, Somerville, Stocker, Whetton, Wood, and Wratt</label><mixed-citation>
Solomon, S., Qin, D., Manning, M., Alley, R. B., Bernsten, T., Bindoff,
N. L.,
Chen, Z., Chidthaisong, A., Gregory, J. M., GC, H., Heimann, M., Hewiston,
B., Hoskins, B. J., Joos, F., Jouzel, J., Kattsov, V., Lohmann, U., Matsuno,
T., Molina, M., Nicholls, N., Overpeck, J., Raga, G., Ramaswamy, V., Ren, J.,
Rusticucci, M., Somerville, R., Stocker, T. F., Whetton, P., Wood, R. A., and
Wratt, D.: Technical Summary, in: Climate Change 2007: The Physical Science
Basis. Contribution of Working Group I to the Fourth Assessment Report of the
Intergovernmental Panel on Climate Change, edited by: Solomon, S., Qin, D.,
Manning, M., Chen, Z., Marquis, M., Averyt, K. B., Tignor, M., and Miller,
H. L., Cambridge University Press, Cambridge, United Kingdom and New York,
NY, USA, 996 pp., 2007.</mixed-citation></ref>
      <ref id="bib1.bibx43"><label>Song et al.(2012)Song, Marcolli, Krieger, Zuend, and
Peter</label><mixed-citation>Song, M., Marcolli, C., Krieger, U. K., Zuend, A., and Peter, T.:
Liquid-liquid phase separation and morphology of internally mixed
dicarboxylic acids/ammonium sulfate/water particles, Atmos. Chem. Phys., 12,
2691–2712, <ext-link xlink:href="http://dx.doi.org/10.5194/acp-12-2691-2012" ext-link-type="DOI">10.5194/acp-12-2691-2012</ext-link>, 2012.</mixed-citation></ref>
      <ref id="bib1.bibx44"><label>Song et al.(2015)Song, Liu, Hanna, Martin, and
Bertram</label><mixed-citation>Song, M., Liu, P. F., Hanna, S. J., Li, Y. J., Martin, S. T., and Bertram, A.
K.: Relative humidity-dependent viscosities of isoprene-derived secondary
organic material and atmospheric implications for isoprene-dominant forests,
Atmos. Chem. Phys., 15, 5145–5159, <ext-link xlink:href="http://dx.doi.org/10.5194/acp-15-5145-2015" ext-link-type="DOI">10.5194/acp-15-5145-2015</ext-link>, 2015.
</mixed-citation></ref><?xmltex \hack{\newpage}?>
      <ref id="bib1.bibx45"><label>Swindells et al.(1958)Swindells, Snyder, Hardy, and
Golden</label><mixed-citation>
Swindells, J. F., Snyder, C. F., Hardy, R. C., and Golden, P. E.:
Viscosities
of Sucrose Solutions at Various Temperatures: Tables of Recalculated Values,
United States Department of Commerce, 1958.</mixed-citation></ref>
      <ref id="bib1.bibx46"><label>Tong et al.(2011)Tong, Reid, Bones, Luo, and Krieger</label><mixed-citation>Tong, H. J., Reid, J. P., Bones, D. L., Luo, B. P., and Krieger, U. K.:
Measurements of the timescales for the mass transfer of water in glassy
aerosol at low relative humidity and ambient temperature, Atmos. Chem.
Phys., 11, 4739–4754, <ext-link xlink:href="http://dx.doi.org/10.5194/acp-11-4739-2011" ext-link-type="DOI">10.5194/acp-11-4739-2011</ext-link>, 2011.</mixed-citation></ref>
      <ref id="bib1.bibx47"><label>Tretheway and Meinhart(2002)</label><mixed-citation>
Tretheway, D. C. and Meinhart, C. D.: Apparent fluid slip at hydrophobic
microchannel walls, Phys. Fluids, 14, L9–L12,
2002.</mixed-citation></ref>
      <ref id="bib1.bibx48"><label>Wang et al.(2012)Wang, Lambe, and Massoli</label><mixed-citation>Wang, B., Lambe, A. T., and Massoli, P.: The deposition ice nucleation and
immersion freezing potential of amorphous secondary organic aerosol: Pathways
for ice and mixed-phase cloud formation, J. Geophys. Res.,
117, D16209, <ext-link xlink:href="http://dx.doi.org/10.1029/2012JD018063" ext-link-type="DOI">10.1029/2012JD018063</ext-link>, 2012.</mixed-citation></ref>
      <ref id="bib1.bibx49"><label>Watanabe and Udagawa(1999)</label><mixed-citation>
Watanabe, K. and Udagawa, Y.: Drag reduction of Newtonian fluid in a
circular
pipe with a highly water-repellent wall, J. Fluid Mechan., 381,
225–238, 1999.</mixed-citation></ref>
      <ref id="bib1.bibx50"><label>You et al.(2012)You, Renbaum-Wolff, Carreras-Sospedra, Hanna,
Hiranuma, Kamal, Smith, Zhang, Weber, Shilling, Dabdub, Martin, and
Bertram</label><mixed-citation>
You, Y., Renbaum-Wolff, L., Carreras-Sospedra, M., Hanna, S. J., Hiranuma,
N.,
Kamal, S., Smith, M. L., Zhang, X., Weber, R. J., Shilling, J. E., Dabdub,
D., Martin, S. T., and Bertram, A. K.: Images reveal that atmospheric
particles can undergo liquid-liquid phase separations, Proc.
Natl. Acad. Sci. USA, 109,
13188–13193, 2012.</mixed-citation></ref>
      <ref id="bib1.bibx51"><label>Zelenyuk et al.(2012)Zelenyuk, Imre, Beránek, Abramson, Wilson,
and Shrivastava</label><mixed-citation>
Zelenyuk, A., Imre, D., Beránek, J., Abramson, E., Wilson, J., and
Shrivastava, M.: Synergy between secondary organic aerosols and long-range
transport of polycyclic aromatic hydrocarbons, Environ. Sci.
Technol., 46, 12459–12466,  2012.</mixed-citation></ref>
      <ref id="bib1.bibx52"><label>Zhou et al.(2013)Zhou, Shiraiwa, McWhinney, Pöschl, and
Abbatt</label><mixed-citation>
Zhou, S., Shiraiwa, M., McWhinney, R. D., Pöschl, U., and Abbatt, J.
P. D.:
Kinetic limitations in gas-particle reactions arising from slow diffusion in
secondary organic aerosol, Faraday Discuss., 165, 391–406,
2013.</mixed-citation></ref>
      <ref id="bib1.bibx53"><label>Zhu et al.(2012)Zhu, Attard, and Neto</label><mixed-citation>
Zhu, L., Attard, P., and Neto, C.: Reconciling slip measurements in
symmetric
and asymmetric systems, Langmuir, 28, 7768–7774,
2012.</mixed-citation></ref>
      <ref id="bib1.bibx54"><label>Zobrist et al.(2008)Zobrist, Marcolli, Pedernera, and
Koop</label><mixed-citation>Zobrist, B., Marcolli, C., Pedernera, D. A., and Koop, T.: Do atmospheric
aerosols form glasses?, Atmos. Chem. Phys., 8, 5221–5244,
<ext-link xlink:href="http://dx.doi.org/10.5194/acp-8-5221-2008" ext-link-type="DOI">10.5194/acp-8-5221-2008</ext-link>, 2008.</mixed-citation></ref>

  </ref-list><app-group content-type="float"><app><title/>

    </app></app-group></back>
    </article>
