Cloud condensation nuclei (CCN) activity analysis of low-hygroscopicity aerosols using the aerodynamic aerosol classifier (AAC)
- 1Department of Chemical and Biomolecular Engineering, University of Maryland, College Park, MD 20742, United States
- 2Department of Chemistry and Biochemistry, University of Maryland, College Park, MD 20742, United States
Correspondence: Akua A. Asa-Awuku (firstname.lastname@example.org)
The aerodynamic aerosol classifier (AAC) is a novel instrument that size-selects aerosol particles based on their mechanical mobility. So far, the application of an AAC for cloud condensation nuclei (CCN) activity analysis of aerosols has yet to be explored. Traditionally, a differential mobility analyzer (DMA) is used for aerosol classification in a CCN experimental setup. A DMA classifies particles based on their electrical mobility. Substituting the DMA with an AAC can eliminate multiple-charging artifacts as classification using an AAC does not require particle charging. In this work, we describe an AAC-based CCN experimental setup and CCN analysis method. We also discuss and develop equations to quantify the uncertainties associated with aerosol particle sizing. To do so, we extend the AAC transfer function analysis and calculate the measurement uncertainties of the aerodynamic diameter from the resolution of the AAC. The analysis framework has been packaged into a Python-based CCN Analysis Tool (PyCAT 1.0) open-source code, which is available on GitHub for public use. Results show that the AAC size-selects robustly (AAC resolution is 10.1, diffusion losses are minimal, and particle transmission is high) at larger aerodynamic diameters ( 85 nm). The size-resolved activation ratio is ideally sigmoidal since no charge corrections are required. Moreover, the uncertainties in the critical particle aerodynamic diameter at a given supersaturation can propagate through droplet activation, and the subsequent uncertainties with respect to the single-hygroscopicity parameter (κ) are reported. For a known aerosol such as sucrose, the κ derived from the critical dry aerodynamic diameter can be up to ∼ 50 % different from the theoretical κ. In this work, we do additional measurements to obtain dynamic shape factor information and convert the sucrose aerodynamic to volume equivalent diameter. The volume equivalent diameter applied to κ-Köhler theory improves the agreement between measured and theoretical κ. Given the limitations of the coupled AAC–CCN experimental setup, this setup is best used for low-hygroscopicity aerosol (κ≤0.2) CCN measurements.
Cloud condensation nuclei (CCN) activity is defined as the ability of an aerosol particle to facilitate the condensation of water vapor on its surface; the condensation occurs in supersaturated ambient conditions, resulting in the formation of droplets. The use of size-resolved aerosol number concentrations obtained with the help of counting instruments is a reliable method for determining the CCN activity of aerosols (e.g., but not limited to Petters et al., 2007; Rose et al., 2008; Moore et al., 2010; Vu et al., 2015; Zieger et al., 2017; Barati et al., 2019). Currently, the most common method for studying CCN activation uses a CCN counter (CCNC) and couples it with an aerosol classifier. CCN activity measurements have consistently improved over the past few years since the development and commercialization of the continuous-flow streamwise thermal gradient CCN chamber (CFSTGC) developed by Droplet Measurement Technologies (DMT) (Roberts and Nenes, 2005; Rose et al., 2008; Lathem and Nenes, 2011), and it is widely used. However, there are several commercially available options to size-select ultrafine particles.
An aerosol classifier size-selects and generates a monodisperse aerosol from a polydisperse aerosol population. The most widely used aerosol classifier for CCN measurements is the differential mobility analyzer (DMA) (Knutson and Whitby, 1975; Rader and McMurry, 1986; Wang and Flagan, 1990). The DMA classifies the aerosol particles based on their electrical mobility; a charge distribution is applied on the particles, which then pass through an external electrostatic field that is generated by varying the voltage difference across the DMA column. Many CCN studies use the DMA in “scanning mode” for which stepwise voltage is applied across the aerosol flow to generate monodisperse particles between ∼ 10 and 500 nm. The size-selected particles are then counted by a condensation particle counter (CPC) and a parallel CCNC to obtain the number size distributions for the total aerosol particles (condensation nuclei, CN) and activated droplets (CCN), respectively, at a constant instrument supersaturation. The aerosol CN and CCN number size distributions are then combined to calculate the size-resolved activation ratio of the aerosol at the given instrument supersaturation.
A major limitation of this method is associated with the working mechanism of the DMA. The DMA uses a neutralizer (e.g., Kr-85, soft X-ray, or Po-210) to distribute electric charge to classify the polydisperse particles. The particles may receive multiple unit charges depending on the charging efficiency of the neutralizer. As a result, the particles carrying a unit charge possess the same electrical mobility as larger particles carrying a higher integral charge. Therefore, the perceived monodisperse aerosols likely contain a mixture of different-sized particles. This issue is known and can lead to discrepancies in the size-resolved activation ratio (Moore et al., 2010). Hence, charge correction algorithms (Gunn, 1956; Fuchs, 1963; Wiedensohler, 1988) are commonly applied to resolve particle multiple-charging issues, and data correction is applied in CCN software. Multiple-charging errors can still affect the reliability and efficacy of CCN activation data.
The multiple-charging issues in electrical-mobility-based classifiers have led to the development of instruments that use particle mechanical mobility. Classifiers can measure the relaxation time in pressurized flow or free-molecular (vacuum) regimes (e.g., but not limited to Conner, 1966; Marple et al., 1991; Keskinen et al., 1992; Chein and Lundgren, 1993; Flagan, 2004). Recently, the working principle and instrumentation details for an aerodynamic aerosol classifier (AAC) were described (Tavakoli and Olfert, 2013; Tavakoli et al., 2014). The AAC does not require particle charging for size selection and does not produce multiple-charging artifacts (Yao et al., 2020). The AAC classifies particles with respect to their relaxation time and reports the aerodynamic diameter.
The AAC has been used with different instruments. Johnson et al. (2018) used the AAC in tandem with the scanning mobility particle sizer (SMPS) to characterize the transfer function of the AAC. The AAC can classify particles as large as 6 µm (Johnson et al., 2018). Furthermore, the AAC in tandem with a DMA can determine the aerosol dynamic shape factor (Tavakoli and Olfert, 2014; Barati et al., 2019; Yao et al., 2020; Tran et al., 2020) and particle effective density (Tavakoli and Olfert, 2014; L. Peng et al., 2021). Sang-Nourpour and Olfert (2019) and Tran et al. (2020) discuss methods for optical particle counter (OPC) calibration using an AAC.
In short, the AAC is increasing in popularity (e.g., but not limited to Johnson et al., 2020; Su et al., 2021; Johnson et al., 2021). However, the scientific knowledge of coupling an AAC with a CCNC is limited. One previous study (Barati et al., 2019) published results for the CCN analysis of low-hygroscopicity aerosols but did not investigate the uncertainties in AAC–CCN size-resolved measurements and CCN activity predictions. To our knowledge, the validation of AAC–CCNC coupling on CCN measurement and prediction has not been studied before, and hence the AAC–CCNC coupled system is currently not well understood. This work explains the AAC–CCNC coupling for CCN activity measurements and uncertainties associated with size selection, number size distributions, and CCN activity estimates employing the AAC transfer function.
In addition to a standardized experimental protocol for an AAC–CCNC setup, a computational tool also needs to be developed for CCN analysis. Currently, the scanning mobility CCN analysis (SMCA) (Moore et al., 2010) package is widely used to calculate the CCN activity of aerosols using their electrical-mobility-classified number size distribution data. The processed size distribution data from the SMCA can be analyzed using the Köhler theory (Köhler, 1936; Seinfeld and Pandis, 2016). SMCA has been shown to efficiently perform functions that include inversion of time series measurements to obtain size-resolved data (Wang and Flagan, 1990) and multiple-charge correction using the algorithm given by Wiedensohler (1988). SMCA works well for a variety of organic and inorganic aerosols to estimate their CCN activity (e.g., but not limited to Moore et al., 2010; Padró et al., 2012; Giordano et al., 2015; Fofie et al., 2018; Barati et al., 2019; Vu et al., 2019; Dawson et al., 2020; C. Peng et al., 2021). So far, there is no computational analysis tool for data processing or CCN analysis using their aerodynamic measurements based on an AAC–CCNC setup.
In this work we couple the AAC with the CCNC, due to the aforementioned advantages and novelty of the AAC, for CCN activity analysis. We develop and test an experimental setup and CCN analysis tool. The analysis tool was developed in Python (PyCAT 1.0, described in Sect. 2.3) and is available on GitHub for public use. In the following sections, we first describe the experimental setup to size-select and count particles. We then describe the theory and mathematical formulations used in CCN analysis of aerosols. After that, we discuss the uncertainties associated with aerodynamic size selection and the propagated error into the CCN activity analysis, as well as the impact on the subsequently derived single-hygroscopicity parameter (κ) values.
2.1 Instruments and setup
A Cambustion™ aerodynamic aerosol classifier (AAC) size-selected polydisperse aerosol. Briefly described here, the AAC contains two concentric cylindrical columns for particle selection. The schematic of a typical AAC is shown in Fig. 1. The particles are introduced into the AAC from inside the inner cylinder, and the aerosol flow is then passed into the space between the two cylinders. The particles move with axial and radial velocities because of the rotation of the cylinders. The rotational speed steps across a range of values when the AAC is operated in “scanning mode”. Each of the rotational speeds correspond to a relaxation time and aerodynamic diameter. At different speeds, the particles can hit the inner surface of the outer cylinder depending on their size. The outer cylinder has an opening through which the particles of an optimum size corresponding to a specific rotational speed can pass. Particles larger than the threshold optimum size hit the cylindrical surface before the opening, and the ones smaller than the threshold exit the classifier along with the exhaust flow. The working principle of the AAC has been described previously in extensive detail (Tavakoli and Olfert, 2013; Tavakoli et al., 2014; Johnson et al., 2018).
Figure 2 shows the experimental setup used in this study. The classified aerosol was split into two streams – the first stream was passed through a condensation particle counter (CPC, TSI 3776) to obtain total aerosol particle counts (condensation nuclei, CN), and the second stream was passed through a DMT continuous-flow streamwise thermal-gradient CCN chamber (CFSTGC, or simply CCNC; Roberts and Nenes, 2005) to obtain activated aerosol particle counts (cloud condensation nuclei, CCN). The CCNC consists of a cylindrical chamber that has internally wetted walls to maintain an approximately constant supersaturation along the CCNC column. A series of experiments was performed with sucrose at different instrument supersaturations (between 0.2 % and 0.6 %). Sucrose is a highly water-soluble, moderately hygroscopic oligomer that is an atmospherically relevant aerosol from biogenic sources (Dawson et al., 2020). The CCN properties of sucrose have been well studied and characterized (e.g., but not limited to Rosenørn et al., 2006; Petters and Kreidenweis, 2007; Xu et al., 2014; Wang et al., 2017; Dawson et al., 2020). Sucrose was selected as an appropriate choice of aerosol to benchmark the AAC–CCNC setup.
The polydisperse aerosol population was generated from an aqueous solution using a Collison atomizer. The aerosol was passed through a series of two diffusion driers (for drying to < 10 % RH) and then introduced into the AAC to generate monodisperse aerosol. The atomization method typically produces dry particles in the submicron size range. A total sample flow rate of 0.8 L min−1 was split between 0.3 and 0.5 L min−1 for the CN and CCN measurements, respectively. Additionally, a sheath flow rate of 8 L min−1 was applied to maintain a sheath-to-sample flow ratio of 10 : 1. Furthermore, the AAC was maintained at a working temperature and pressure of 21.5 ∘C and 1 atm, respectively. The CCNC instrument supersaturations were calibrated using ammonium sulfate ((NH4)2SO4) (Rose et al., 2008). The details of CCNC calibration performed using DMA-based size-resolved (NH4)2SO4 measurements from 0.2 % to 0.6 % supersaturation are provided in the Supplement.
The AAC was operated in the “step-scanning mode”. In step-scanning mode, there is a transit time and stabilization (delay) time when the AAC advances from one rotational speed set point to another. Each rotational speed is related to a corresponding size bin, and here we ran the AAC between successive size bins for 14.5 s (transit time of 9.5 s and delay time of 5 s). Increasing the stabilization interval improves the repeatability of the particle counts and reduces uncertainties due to particle diffusion at lower sizes. The measured CCN to CN activation ratio was calculated for each size-selected aerodynamic diameter. A sigmoidal fit was applied to the size-resolved activation ratio. The critical dry diameter is defined at the 50 % activation efficiency at a constant instrument supersaturation and was reported every 30 min and repeated five times for the AAC–CCN experimental setup.
2.2 CCN activation theory
The critical dry diameter and instrument supersaturation can be used in Köhler theory (Köhler, 1936; Seinfeld and Pandis, 2016) to estimate the size-independent single-hygroscopicity parameter (κ) of the aerosol species. κ of an aerosol species is calculated as follows (Petters and Kreidenweis, 2007):
In the above expression, is the critical dry diameter of the aerosol species at supersaturation S. Physically, is a threshold size for activation; particles larger than this threshold are assumed to fully activate and convert into droplets, and those smaller than the threshold remain unactivated. Mw, σw, and ρw correspond to the molar mass, surface tension, and density of water, respectively. R is the universal gas constant, and T is the average temperature inside the CCNC column. Under the Köhler theory framework, the κ of an aerosol species can be related to the molar mass (Ms), density (ρs), and van't Hoff factor (νs) of the solute (Sullivan et al., 2009; Mikhailov et al., 2013).
Equation (2) assumes complete aqueous solubility of the aerosol species. Past studies have found sucrose κ from CCN measurements (obtained from Eq. 1) in the range of 0.06–0.1 (e.g., but not limited to Xu et al., 2014; Wang et al., 2015; Ruehl et al., 2016; Wang et al., 2017; Dawson et al., 2020). Furthermore, the theoretical κ of sucrose (obtained from Eq. 2) is 0.084 and implies that the previously reported κ estimates of sucrose are in good agreement with the theoretical κ of sucrose. Therefore, the theoretical κ (from Eq. 2) can also be used to validate the sucrose κ derived from the AAC–CCNC setup.
2.3 Python-based CCN Analysis Toolkit (PyCAT 1.0)
Each step-scanning-mode time series using the AAC–CCNC setup measures 90 CN data points and 1400 CCN data points. Therefore, a computationally efficient method is required to synchronize and analyze the AAC and CCNC datasets. A computer code (Python-based CCN Analysis Toolkit, PyCAT) was developed to analyze both SMPS and AAC size-resolved CCN data for CCN activity analysis. The code is written in Python3.7 and uses the most recent version of the built-in libraries. It can perform time series data synchronization and analysis, CCN activity analysis (Sect. 2.2), and uncertainty analysis (Sect. 3). In addition, the code provides aerosol sizing properties at the point of activation and Köhler theory analysis based on user inputs. Additionally, the code is flexible and allows the user to organize and visualize the post-analysis data. An open-source code has been completely packaged with the necessary capabilities and is available on GitHub for public use. Here we demonstrate the application of PyCAT for the first time. We use PyCAT for CCN activity analysis and to quantify the uncertainties associated with aerodynamic measurements and how they manifest in the CCN activity.
The uncertainty analysis for particle size selection using the AAC in step-scanning mode has been described in detail previously (Johnson et al., 2018; Yao et al., 2020). In this section, we briefly describe the derivation of AAC uncertainty and fully describe the effects of size selection for CCN activity and single-parameter hygroscopicity uncertainty analysis.
Aerosol particles moving with an axial speed ν through the AAC column experience drag force. The drag force on a particle of an assumed spherical shape can be expressed as
where Bspherical is defined as the mechanical mobility of the spherical particle (Tavakoli and Olfert, 2014; Johnson et al., 2018; Yao et al., 2020). For a given set of AAC operating conditions, Bspherical can be determined as (Tavakoli and Olfert, 2014; Yao et al., 2020)
where μ is the dynamic viscosity of the surrounding gas, dspherical is the particle diameter under the assumption of sphericity, and Cc(dspherical) is the Cunningham slip correction factor of the particle with the diameter dspherical (described in Sect. S2 in the Supplement).
where m, ω, and r are the mass, rotational speed, and radial position of the particle, respectively. The aerosol particle relaxation time is τ=mBspherical. Using this definition, the force balance expression τ is expressed as
where r1, r2, and L denote the classifier inner radius, outer radius, and length, respectively. Qsh and Qexh are the inlet sheath flow and outlet exhaust flow, respectively. In this study, Qsh and Qexh were fixed by the CPC sample flow rate. ω is the only variable parameter in Eq. (7); it defines the set point for size selection and determines the τ* corresponding to particles of desired aerodynamic diameter.
where ρ0 is the reference density of 1000 kg m−3 and Cc(dae) is the Cunningham slip correction factor of the particle with aerodynamic diameter dae. The aerodynamic diameter of a particle is defined for a spherical particle with a density of 1000 kg m−3. A nondimensional relaxation time, , is calculated by dividing Eq. (8) by Eq. (7).
Previous studies have developed models to calculate the probability of selecting a particle passing through the AAC, otherwise known as the AAC transfer function (TF) (Tavakoli and Olfert, 2013; Johnson et al., 2018). Tavakoli and Olfert (2013) developed the AAC transfer function following the methodology from Knutson and Whitby (1975) and Stolzenburg (1988). In this work, the non-diffusing particle streamline TF theory is used to describe particle classification (Tavakoli and Olfert, 2013). The AAC TF is denoted by Ω, and for ideal non-diffusion conditions, it is defined as follows (Martinsson et al., 2001; Tavakoli and Olfert, 2013; Johnson et al., 2018):
where and such that Qa is the inlet aerosol flow, and Qs is the outlet sample flow. The AAC was operated under balanced flow conditions (Qs=Qa and Qsh=Qexh), and thus β and δ were reduced to and 0, respectively. Under the balanced flow assumption, Eq. (9) can be simplified to (Johnson et al., 2018)
The nonideal particle behavior was accounted for by incorporating a transmission efficiency (λΩ) and transfer function width factor (μΩ) in the TF (described in Sect. S2). The resulting TF for nonideal, non-diffusing, balanced flow conditions is expressed as (Johnson et al., 2018)
Figure 3 compares the theoretical TFs for ideal (Eq. 10) and nonideal (Eq. 11) particle behaviors under the balanced flow, non-diffusion AAC framework. The two transfer functions are shown for a particle aerodynamic diameter of 150 nm (τ=147.7 ns, Eq. 8).
The AAC resolution can be determined from the TF broadening relative to the set point at (or, ). The AAC resolution can be correlated with the uncertainty associated with the relaxation time or aerodynamic diameter. Particles classified by the AAC only contain a narrow range of aerodynamic diameters. The AAC resolution is expressed as and assumes the flows to be balanced, laminar, and constant (Yao et al., 2020). The AAC resolution can also be expressed in the coordinates of the aerodynamic diameter as , which forms the basis to determine the uncertainties associated with the aerodynamic diameters. Using Eq. (11), the uncertainty in relaxation time is (Yao et al., 2020)
which can further be used to derive the uncertainty associated with the corresponding aerodynamic diameter as follows:
where αc=2.33, βc=0.966, and γc=0.4985 are the Cunningham slip correction factor coefficients taken from Kim et al. (2005), and λ is the mean free path of the particles. The aerodynamic diameter can be converted to the volume equivalent diameter, which is a more accurate representation of the particle morphology and size. The volume equivalent diameter is expressed using the dynamic shape factor and aerosol density as follows:
where ρp is the particle density, Cc(dve) is the Cunningham slip correction factor for the particle with the volume equivalent diameter, dve, and χ is the size-dependent dynamic shape factor. The uncertainties in the volume equivalent diameter are quantified using the uncertainties in measured aerodynamic diameter and dynamic shape factor as follows.
The uncertainty given by Eq. (15) has a direct implication for the aerosol κ. For a given supersaturation, the uncertainty in κ is dependent on the uncertainty in the volume equivalent diameter and is expressed as
Equation (16) implies that the relative uncertainty in κ is theoretically 3 times more than that of the critical dry diameter. In Eq. (16), the can either be the critical dry electrical mobility, aerodynamic diameter, or volume equivalent diameter. In this work, the uncertainties in Eq. (16) are evaluated with respect to volume equivalent diameters derived from the measured electrical mobility and aerodynamic diameters. Another important point to note here is that since the activation diameter varies with supersaturation, the uncertainty at every activation diameter will also be different. This implies that for each measured activation diameter, the uncertainty in aerosol κ will vary and will thus depend on the uncertainty in the critical dry diameter.
The AAC–CCNC measurements of sucrose were reported at varying CCNC instrument supersaturations (0.2 % to 0.6 %). The aerosol particles classified with the AAC were counted using a CPC and CCNC. An example dataset of CN and CCN number size distributions measured at 0.39 % supersaturation is shown in Fig. 4a. The CN and CCN particle counts are plotted against the aerodynamic diameters. Error bars in the y axis denote the relative uncertainties in the CN and CCN number concentrations. The errors in CN and CCN concentrations are calculated from counting uncertainties of the CPC and CCNC, as well as uncertainties in the instrument flow rate of CPC and CCNC. Details of uncertainty estimation for the CN and CCN counts are provided in Moore et al. (2010) and are briefly described in Sect. S4. The observed relative uncertainties in the CN and CCN concentrations were < 1 % for every aerodynamic diameter, which indicates that counts are repeatable. Figure 4b shows the size-resolved activation ratio for 0.39 % supersaturation (S), where CCN(S,Dp) is the CCN measurement at the constant S and Dp divided by CN measurements at constant Dp, CN(Dp). A brief description of the sigmoidal fitting and its mathematical representation is provided in Sect. S3. The sigmoidal fit applied to the Ra is also shown in Fig. 4b. Error bars on the y axis in Fig. 4b show the uncertainties in Ra. The Ra uncertainties were calculated by propagating the uncertainties in CN and CCN number concentrations. Details of the estimation of y-axis uncertainties of Ra in Fig. 4b are also provided in Sect. S4.
In both Fig. 4a and b, the error bars along the x axis show uncertainties in aerodynamic diameters estimated using the AAC TF. The x-axis uncertainties in Fig. 4a and b decreased with increasing aerodynamic diameters. The decrease in the x-axis uncertainties can be explained using Fig. 5a, which shows the AAC TF for nonideal particle behavior. For nonideal AAC TF, the increase in the AAC resolution can be attributed to a monotonic increase in the transmission efficiency (λΩ) and transfer function width factor (μΩ) with respect to the aerodynamic diameter (Fig. 5b). Figure 5a shows that the AAC TF broadening decreases with an increase in aerodynamic diameter for a fixed sheath flow rate. This is likely due to a reduced classifier flow effect with increasing aerodynamic diameter (Johnson et al., 2018). As a result, the AAC resolution increases with increasing aerodynamic diameter. An increased resolution results in a decrease in the x-axis uncertainty with increasing particle sizes. In other words, the diffusion losses decrease with an increase in the mobility mass and aerodynamic diameter, in turn decreasing Ra uncertainties associated with AAC particle size selection and counting. From our AAC–CCNC measurements at 8 L min−1, the minimum AAC resolution was 10.1 to prevent excess transfer function broadening and improve the accuracy of the size-resolved measurements. Figure 5a is a direct result of Eq. (13) and suggests that reducing the error in size measurement reduces the magnitude of error propagation for the single-hygroscopicity parameter (κ).
a κ determined using the dry aerodynamic activation diameter in the Köhler theory framework. b Theoretical κ of sucrose determined from ideal Köhler theory = 0.084. c Volume equivalent diameter including the dynamic shape factor with the dry aerodynamic activation diameter. d κ determined using the volume equivalent activation diameter in the Köhler theory framework.
The critical dry aerodynamic diameter at 0.39 % supersaturation was approximately 130 nm. The AAC–CCNC sigmoidal fitting is similar to that applied by SMCA (Moore et al., 2010). However, the sigmoid applied to the AAC–CCNC measurements does not require the correction of multiple-charging artifacts. The critical dry aerodynamic diameter (130 nm) and S (0.39 %) were then combined using the Köhler theory framework (Sect. 2.2) to estimate the single-hygroscopicity parameter (κ) of sucrose. At 0.39 % the κ was found to be 0.041 (Eq. 1). This had a ∼ 51 % difference with respect to the theoretical κ (0.084) of sucrose. Like Fig. 4b, Fig. 6 shows the size-resolved activation ratios estimated from the measured number size distributions at five different supersaturations (0.23 %, 0.31 %, 0.39 %, 0.48 %, and 0.57 %). The uncertainties associated with the aerodynamic diameters and their corresponding activation ratios are also shown on the plot. In addition to this, the critical dry aerodynamic diameters obtained from the size-resolved activation ratios at respective supersaturations are provided. For every set of size-resolved activation data, the y-axis uncertainties increase, while the x-axis uncertainties decrease with increasing aerodynamic diameters (Table 1). κ was calculated for each supersaturation using Eq. (1), and the propagated uncertainty from the critical dry volume equivalent diameter was calculated using Eq. (16). The κ and associated uncertainties were averaged for five sets of measurements at every instrument supersaturation. Accounting for changing instrument supersaturations, the mean κ for the set of five aerodynamic measurements was 0.036 ± 0.008 (slightly < 0.041, the mean κ at 0.39 % supersaturation). The 0.036 κ value was less than previously reported sucrose κ values from electrical mobility CCN measurements (in the range of 0.06–0.1) (Xu et al., 2014; Ruehl et al., 2016; Dawson et al., 2020) and the theoretical sucrose κ (0.084). This relatively large differences between κ values are attributed to the use of the aerodynamic diameter in Eq. (1).
Aerodynamic diameters are generally overpredicted as they are based on a spherical particle with a density (ρ0) = 1000 kg m−3; this is likely true in the case of sucrose as its bulk density is 1586 kg m−3 (Guard, 1999), which is significantly larger than ρ0. In such a case, a more reliable measure of particle size is required to improve the accuracy of the AAC–CCN hygroscopicity estimates. The measured aerodynamic diameters were converted into volume equivalent diameters by accounting for the particle dynamic shape factor and true particle density (Tavakoli and Olfert, 2014). Size-resolved shape factor measurements of sucrose are described in detail in Sect. S5. Dynamic shape factor (χ) = 1 corresponds to spherical particles, and χ>1 marks a deviation of particle shape from sphericity. For sucrose particles with aerodynamic diameters between ∼ 100 and 250 nm, the size-resolved dynamic shape factor was approximately 1 and was observed to be only as high as ∼ 1.1 for particles with dae=100 nm. Table 1 provides a summary of critical dry aerodynamic diameters and their volume equivalent counterparts found in this study for CCN measurements at different supersaturations.
The κ values computed using Köhler theory from five different dry aerodynamic activation diameters and their respective volume equivalent diameters are summarized in Table 1. Physically, the volume equivalent diameter represents a spherical particle with the same mass as that of a nonspherical aerodynamic particle. However, the volume equivalent diameter accounts for the aerosol density and the deviation of the aerosol particles' shape from sphericity, and it improves the accuracy of hygroscopicity estimates. The mean sucrose κ computed from critical dry volume equivalent diameters was estimated to be 0.09 ± 0.006. The critical dry volume equivalent diameters combined with their respective critical supersaturations provided estimates of sucrose κ that are in a better agreement with the theoretical and previously reported hygroscopicity values.
This study presents the AAC–CCNC experimental setup. The presented methodology can be applied for CCN activity analysis of different aerosol species. Aerosol size selection with the AAC does not require charging of particles; thus, the AAC–CCNC coupling generates truer monodisperse aerosols, ideally produces sigmoidal activation data, and improves the accuracy of size-resolved measurements. For AAC-derived critical dry aerodynamic diameters, the sizing uncertainty is larger at low particle sizes and is reduced with an increase in particle size (Table 1). Thus, larger critical dry aerodynamic diameters are preferred with the AAC–CCNC setup so the AAC–CCNC setup is more applicable for CCN measurements of low-hygroscopicity aerosols. It should be noted that this phenomenon is reversed for electrical mobility measurements. In the DMA, this can be attributed to increased diffusion losses due to a drop in transmission efficiency for the particles larger than 100 nm. A similar observation can be made based on the findings in Fig. 5 of Johnson et al. (2018). To reiterate, the uncertainties in the electrical mobility diameter increase for larger particle sizes (Fig. 7). Table S1 provides the measure of uncertainties in aerodynamic and mobility diameters of sucrose at the same supersaturations.
An optimum range of aerodynamic diameters for CCN measurements can be suggested based on the findings of this work. There are fewer particles larger than 0.5 µm generated via Collison atomization. Therefore, atomization produces extremely low number concentrations for particles larger than 0.5 µm, which can significantly reduce the counting statistics. This suggests that ∼ 0.5 µm was a suitable upper limit of aerodynamic diameters for laboratory AAC–CCNC measurements. The lower size limit can be defined using the AAC resolution, the TF broadening, and hence the flow rates used in the experiments. The sample and sheath flow rates were set to 0.8 and 8 L min−1, respectively. Additionally, AAC TF equations (Sect. 3) indicate a lower size limit of ∼ 85 nm. The minimum measurement resolution to obtain good counting statistics corresponding to any aerodynamic diameter 85 nm was 10.1. Based on the TF analysis in this paper and the previously described CCN activity measurements (Rose et al., 2008; Moore et al., 2010), it can be inferred that AAC is useful for particle classification and size-resolved measurements for relatively larger particles in the submicron regime. Furthermore, 85 nm is a reasonable lower limit for CCN measurements of low-hygroscopicity aerosols. Low-hygroscopicity aerosols (predominantly organics with κ≤0.2; Petters and Kreidenweis, 2007; Xu et al., 2014; Vu et al., 2019; Wang et al., 2019) do not activate readily at smaller particle sizes and atmospherically relevant supersaturations (< 1 %). The laboratory number size distribution measurements for such aerosols are reliable at low to mid-range supersaturations with the AAC–CCNC setup.
The uncertainty analysis in this work shows that size-resolved aerodynamic measurements are precise. However, the accuracy of the aerosol hygroscopicity estimates from aerodynamic measurements is low; this is seen from the lack of agreement between aerodynamic-diameter-derived κ and previously reported well-accepted κ values of sucrose. The aerodynamic diameter can be converted to a volume equivalent diameter if an additional aerosol classifier is used in series with the AAC (Yao et al., 2020). We measured the size-resolved dynamic shape factor (χ) with a DMA–AAC setup to convert the aerodynamic diameters to their respective volume equivalent diameters. The volume equivalent diameter of the particles were estimated by incorporating χ and known aerosol density (Eq. 14). The aerosol hygroscopicity estimates using volume equivalent diameters in the analysis showed good agreement with previously reported sucrose hygroscopicity values.
Overall, the AAC–CCNC coupling offers a promising tool for obtaining size-resolved CCN activity measurements for challenging low-hygroscopicity organic aerosols. Using the AAC–CCNC setup, the measurements and activation properties are obtained in terms of aerodynamic diameter. However, the sole use of aerodynamic diameters should be avoided in the context of CCN activity. CCN activity depends on particle size and chemistry; aerodynamic diameters assume a constant density of 1000 kg m−3, therefore neglecting the densities of different chemical species. The use of aerodynamic diameters for CCN analysis has significant consequences for the representation of aerosols and for the estimation of hygroscopicity (κ). Future work should add the dynamic shape factor and particle density in aerodynamic-diameter-derived CCN activity analysis. The additionally known parameters improve agreement between the measured and theoretical κ values. It should also be noted that the uncertainty calculations presented in this paper solely focus on the uncertainties from changing sizing instrumentation used before the CCN counter. That is, if one uses the same CCN counter, the uncertainty in the supersaturation (from changes in the δT, flow rate, and δP) is constant. One can add additional calculations of error in supersaturations by referring to Roberts and Nenes (2005) and Rose et al. (2008). If the user intends to perform CCN measurements using the AAC and DMA, they should run the CCN measurements at the same time.
The supplement related to this article is available online at: https://doi.org/10.5194/amt-15-1007-2022-supplement.
KG designed the analysis for the AAC–CCN experimental data. AAA conceived the idea for the study and designed and developed the experimental methodology. Both authors contributed to the writing and preparation of the paper.
The contact author has declared that neither they nor their co-author has any competing interests.
Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.
We would like to acknowledge Dewansh Rastogi for assisting with the CCN measurements.
This research has been supported by the National Science Foundation (grant no. 1708337).
This paper was edited by Zamin A. Kanji and reviewed by two anonymous referees.
Barati, F., Yao, Q., and Asa-Awuku, A. A.: Insight into the Role of Water-Soluble Organic Solvents for the Cloud Condensation Nuclei Activation of Cholesterol, ACS Earth and Space Chemistry, 3, 1697–1705, 2019. a, b, c, d
Chein, H. and Lundgren, D. A.: A virtual impactor with clean air core for the generation of aerosols with narrow size distributions, Aerosol Sci. Tech., 18, 376–388, 1993. a
Conner, W. D.: An inertial-type particle separator for collecting large samples, JAPCA J. Air Waste Ma., 16, 35–38, 1966. a
Dawson, J. N., Malek, K. A., Razafindrambinina, P. N., Raymond, T. M., Dutcher, D. D., Asa-Awuku, A. A., and Freedman, M. A.: Direct Comparison of the Submicron Aerosol Hygroscopicity of Water-Soluble Sugars, ACS Earth and Space Chemistry, 4, 2215–2226, 2020. a, b, c, d, e
Flagan, R. C.: Opposed migration aerosol classifier (OMAC), Aerosol Sci. Tech., 38, 890–899, 2004. a
Fofie, E., Donahue, N., and Asa-Awuku, A.: Cloud condensation nuclei activity and droplet formation of primary and secondary organic aerosol mixtures, Aerosol Sci. Tech., 52, 242–251, 2018. a
Fuchs, N.: On the stationary charge distribution on aerosol particles in a bipolar ionic atmosphere, Geofisica pura e applicata, 56, 185–193, 1963. a
Giordano, M., Espinoza, C., and Asa-Awuku, A.: Experimentally measured morphology of biomass burning aerosol and its impacts on CCN ability, Atmos. Chem. Phys., 15, 1807–1821, https://doi.org/10.5194/acp-15-1807-2015, 2015. a
Guard, U. C.: Chemical Hazard Response Information System (CHRIS)-Hazardous Chemical Data, Commandant Instruction, Department of Transportation, Hero ID: 5208492, 16465, 1999. a
Gunn, R.: The ratio of the positive and negative light ion conductivities within a neutral aerosol space, J. Colloid Sci., 11, 661–696, 1956. a
Johnson, T. J., Irwin, M., Symonds, J. P., Olfert, J. S., and Boies, A. M.: Measuring aerosol size distributions with the aerodynamic aerosol classifier, Aerosol Sci. Tech., 52, 655–665, 2018. a, b, c, d, e, f, g, h, i, j, k, l
Johnson, T. J., Nishida, R. T., Irwin, M., Symonds, J. P., Olfert, J. S., and Boies, A. M.: Measuring the bipolar charge distribution of nanoparticles: Review of methodologies and development using the Aerodynamic Aerosol Classifier, J. Aerosol Sci., 143, 105526, https://doi.org/10.1016/j.jaerosci.2020.105526, 2020. a
Johnson, T. J., Symonds, J. P., Olfert, J. S., and Boies, A. M.: Accelerated measurements of aerosol size distributions by continuously scanning the aerodynamic aerosol classifier, Aerosol Sci. Tech., 55, 119–141, 2021. a
Keskinen, J., Pietarinen, K., and Lehtimäki, M.: Electrical low pressure impactor, J. Aerosol Sci., 23, 353–360, 1992. a
Kim, J. H., Mulholland, G. W., Kukuck, S. R., and Pui, D. Y.: Slip correction measurements of certified PSL nanoparticles using a nanometer differential mobility analyzer (nano-DMA) for Knudsen number from 0.5 to 83, J. Res. Natl. Inst. Stan., 110, 31–54, https://doi.org/10.6028/jres.110.005, 2005. a
Lathem, T. L. and Nenes, A.: Water vapor depletion in the DMT continuous-flow CCN chamber: Effects on supersaturation and droplet growth, Aerosol Sci. Tech., 45, 604–615, 2011. a
Marple, V. A., Rubow, K. L., and Behm, S. M.: A microorifice uniform deposit impactor (MOUDI): Description, calibration, and use, Aerosol Sci. Tech., 14, 434–446, 1991. a
Martinsson, B. G., Karlsson, M. N., and Frank, G.: Methodology to estimate the transfer function of individual differential mobility analyzers, Aerosol Sci. Tech., 35, 815–823, 2001. a
Mikhailov, E., Vlasenko, S., Rose, D., and Pöschl, U.: Mass-based hygroscopicity parameter interaction model and measurement of atmospheric aerosol water uptake, Atmos. Chem. Phys., 13, 717–740, https://doi.org/10.5194/acp-13-717-2013, 2013. a
Moore, R. H., Nenes, A., and Medina, J.: Scanning mobility CCN analysis – A method for fast measurements of size-resolved CCN distributions and activation kinetics, Aerosol Sci. Tech., 44, 861–871, 2010. a, b, c, d, e, f, g
Padró, L. T., Moore, R. H., Zhang, X., Rastogi, N., Weber, R. J., and Nenes, A.: Mixing state and compositional effects on CCN activity and droplet growth kinetics of size-resolved CCN in an urban environment, Atmos. Chem. Phys., 12, 10239–10255, https://doi.org/10.5194/acp-12-10239-2012, 2012. a
Peng, C., Razafindrambinina, P. N., Malek, K. A., Chen, L., Wang, W., Huang, R.-J., Zhang, Y., Ding, X., Ge, M., Wang, X., Asa-Awuku, A. A., and Tang, M.: Interactions of organosulfates with water vapor under sub- and supersaturated conditions, Atmos. Chem. Phys., 21, 7135–7148, https://doi.org/10.5194/acp-21-7135-2021, 2021. a
Peng, L., Li, L., Zhang, G., Du, X., Wang, X., Peng, P., Sheng, G., and Bi, X.: Technical note: Measurement of chemically resolved volume equivalent diameter and effective density of particles by AAC-SPAMS, Atmos. Chem. Phys., 21, 5605–5613, https://doi.org/10.5194/acp-21-5605-2021, 2021. a
Petters, M. D. and Kreidenweis, S. M.: A single parameter representation of hygroscopic growth and cloud condensation nucleus activity, Atmos. Chem. Phys., 7, 1961–1971, https://doi.org/10.5194/acp-7-1961-2007, 2007. a, b, c
Petters, M. D., Prenni, A. J., Kreidenweis, S. M., and DeMott, P. J.: On measuring the critical diameter of cloud condensation nuclei using mobility selected aerosol, Aerosol Sci. Tech., 41, 907–913, 2007. a
Rader, D. and McMurry, P.: Application of the tandem differential mobility analyzer to studies of droplet growth or evaporation, J. Aerosol Sci., 17, 771–787, 1986. a
Rose, D., Gunthe, S. S., Mikhailov, E., Frank, G. P., Dusek, U., Andreae, M. O., and Pöschl, U.: Calibration and measurement uncertainties of a continuous-flow cloud condensation nuclei counter (DMT-CCNC): CCN activation of ammonium sulfate and sodium chloride aerosol particles in theory and experiment, Atmos. Chem. Phys., 8, 1153–1179, https://doi.org/10.5194/acp-8-1153-2008, 2008. a, b, c, d, e
Rosenørn, T., Kiss, G., and Bilde, M.: Cloud droplet activation of saccharides and levoglucosan particles, Atmos. Environ., 40, 1794–1802, 2006. a
Sang-Nourpour, N. and Olfert, J. S.: Calibration of optical particle counters with an aerodynamic aerosol classifier, J. Aerosol Sci., 138, 105452, https://doi.org/10.1016/j.jaerosci.2019.105452, 2019. a
Stolzenburg, M. R.: An ultrafine aerosol size distribution measuring system, University of Minnesota, https://www.proquest.com/docview/303683946?pq-origsite=gscholar&fromopenview=true (last access: 30 July 2021), 1988. a
Su, B., Zhang, G., Zhuo, Z., Xie, Q., Du, X., Fu, Y., Wu, S., Huang, F., Bi, X., Li, X. and Li, L.: Different characteristics of individual particles from light-duty diesel vehicle at the launching and idling state by AAC-SPAMS, J. Hazard. Mater., 418, 126304, https://doi.org/10.1016/j.jhazmat.2021.126304, 2021. a
Sullivan, R. C., Moore, M. J. K., Petters, M. D., Kreidenweis, S. M., Roberts, G. C., and Prather, K. A.: Effect of chemical mixing state on the hygroscopicity and cloud nucleation properties of calcium mineral dust particles, Atmos. Chem. Phys., 9, 3303–3316, https://doi.org/10.5194/acp-9-3303-2009, 2009. a
Tavakoli, F. and Olfert, J.: An instrument for the classification of aerosols by particle relaxation time: theoretical models of the aerodynamic aerosol classifier, Aerosol Sci. Tech., 47, 916–926, 2013. a, b, c, d, e, f, g, h
Tavakoli, F. and Olfert, J. S.: Determination of particle mass, effective density, mass–mobility exponent, and dynamic shape factor using an aerodynamic aerosol classifier and a differential mobility analyzer in tandem, J. Aerosol Sci., 75, 35–42, 2014. a, b, c, d, e, f
Tavakoli, F., Symonds, J. P., and Olfert, J. S.: Generation of a monodisperse size-classified aerosol independent of particle charge, Aerosol Sci. Tech., 48, 1–4, https://doi.org/10.1080/02786826.2013.877121, 2014. a, b, c
Tran, S., Iida, K., Yashiro, K., Murashima, Y., Sakurai, H., and Olfert, J. S.: Determining the cutoff diameter and counting efficiency of optical particle counters with an aerodynamic aerosol classifier and an inkjet aerosol generator, Aerosol Sci. Tech., 54, 1335–1344, 2020. a, b
Vu, D., Short, D., Karavalakis, G., Durbin, T., and Asa-Awuku, A.: Integrating cloud condensation nuclei predictions with fast time resolved aerosol instrumentation to determine the hygroscopic properties of emissions over transient drive cycles, Aerosol Sci. Tech., 49, 1149–1159, 2015. a
Vu, D., Gao, S., Berte, T., Kacarab, M., Yao, Q., Vafai, K., and Asa-Awuku, A.: External and internal cloud condensation nuclei (CCN) mixtures: controlled laboratory studies of varying mixing states, Atmos. Meas. Tech., 12, 4277–4289, https://doi.org/10.5194/amt-12-4277-2019, 2019. a, b
Wang, J., Shilling, J. E., Liu, J., Zelenyuk, A., Bell, D. M., Petters, M. D., Thalman, R., Mei, F., Zaveri, R. A., and Zheng, G.: Cloud droplet activation of secondary organic aerosol is mainly controlled by molecular weight, not water solubility, Atmos. Chem. Phys., 19, 941–954, https://doi.org/10.5194/acp-19-941-2019, 2019. a
Wang, Z., Su, H., Wang, X., Ma, N., Wiedensohler, A., Pöschl, U., and Cheng, Y.: Scanning supersaturation condensation particle counter applied as a nano-CCN counter for size-resolved analysis of the hygroscopicity and chemical composition of nanoparticles, Atmos. Meas. Tech., 8, 2161–2172, https://doi.org/10.5194/amt-8-2161-2015, 2015. a
Wang, Z., Cheng, Y., Ma, N., Mikhailov, E., Pöschl, U., and Su, H.: Dependence of the hygroscopicity parameter κ on particle size, humidity and solute concentration: implications for laboratory experiments, field measurements and model studies, Atmos. Chem. Phys. Discuss. [preprint], https://doi.org/10.5194/acp-2017-253, in review, 2017. a, b
Xu, W., Guo, S., Gomez-Hernandez, M., Zamora, M. L., Secrest, J., Marrero-Ortiz, W., Zhang, A. L., Collins, D. R., and Zhang, R.: Cloud forming potential of oligomers relevant to secondary organic aerosols, Geophys. Res. Lett., 41, 6538–6545, 2014. a, b, c, d
Yao, Q., Asa-Awuku, A., Zangmeister, C. D., and Radney, J. G.: Comparison of three essential sub-micrometer aerosol measurements: Mass, size and shape, Aerosol Sci. Tech., 54, 1197–1209, 2020. a, b, c, d, e, f, g, h
Zieger, P., Väisänen, O., Corbin, J.C., Partridge, D.G., Bastelberger, S., Mousavi-Fard, M., Rosati, B., Gysel, M., Krieger, U.K., Leck, C. and Nenes, A.: Revising the hygroscopicity of inorganic sea salt particles, Nat. Commun., 8, 1–10, 2017. a