the Creative Commons Attribution 4.0 License.

the Creative Commons Attribution 4.0 License.

# An experimental study on light scattering matrices for Chinese loess dust with different particle size distributions

### Jia Liu

### Yinuo Huo

### Jinjun Wang

### Yongming Zhang

Mineral dust suspended in the atmosphere has significant effects on radiative balance and climate change. The Chinese Loess Plateau (CLP) is generally considered one of the main sources of Asian dust aerosol. After being lifted by wind, dust particles with various size distributions can be
transported over different distances. In this study, an original loess sample
was collected from Luochuan, which is centrally located on the CLP, and two
samples with different size distributions were obtained afterwards.
“Pristine loess” was used to represent dust that only affects source
regions, part of pristine loess was milled to finer “milled loess”
that can be transported over long distances. Light scattering matrices for
these two samples were measured at 532 nm wavelength from 5 to
175^{∘} angles. Particle size distribution, refractive index,
chemical component, and microscopic appearance were also characterized for
auxiliary analyses. Experimental results showed that there are obvious
discrepancies in angular behaviors of matrix elements for pristine
loess and milled loess, and these discrepancies are different from
those for other kinds of dust with distinct size distributions. Given that
the effective radii of these two loess samples differ by more than 20 times,
it is reasonable to conclude that the difference in size distributions plays
a major role in leading to different matrices, while differences in refractive index and microstructure have relatively small contributions.
Qualitative analyses of numerical simulation results of irregular particles
also validate this conclusion. Gaussian spheres may be promising
morphological models for simulating the scattering matrix of loess but need
further quantitative verification. Finally, synthetic scattering matrices
for both pristine loess and milled loess were constructed over
0–180^{∘}, and the previous average scattering matrix for loess dust was updated. This study presents measurement results of Chinese loess dust and an updated average scattering matrix for loess, which are useful for validating existing models, developing more advanced models for optical simulations of loess dust, and helping to improve retrieval accuracy of dust aerosol properties over both source and downwind areas.

Mineral dust is a common particulate type in Earth's atmosphere, and
accounts for a high fraction of atmospheric aerosol mass loading (Tegen
and Fung, 1995). Asian dust contributes a lot to global atmospheric mineral
dust aerosol; i.e, dust emitted from East Asia alone is about 1.04×10^{7}, 2.76×10^{7}, and 5.13×10^{7} t yr^{−1} for PM_{10} (particles with aerodynamic equivalent diameter smaller than 10 µm), PM_{30}, and PM_{50}, respectively (Xuan et al., 2004). During aerosol characterization experiments (ACE-Asia), mass balance calculations indicated that 45 %–82 % of atmospheric aerosol mass at
observation sites in China was attributed to Asian dust (Zhang et al., 2003). The Chinese Loess Plateau (CLP) is usually considered one of the main sources or an important supply site of Asian dust aerosol (Han et al., 2008; Shen et al., 2016; Tsai et al., 2014; Zhang et al., 2010). Statistical analysis of dust storms influencing the Chinese mainland from 2000 to 2002 showed that about a quarter of dust storms originated from the CLP (Zhang and Gao, 2007). Source tracing of dust collected in Xi'an city revealed that these dust particles were mainly transported short distances from the CLP (Yan et al., 2015). Comparisons of chemical element ratios demonstrated that dust
particles emitted from the CLP can be transported to Korea, Japan, and the North
Pacific (Cao et al., 2008).

Because of the scattering and absorption of solar radiation, atmospheric
dust has remarkable influences on global climate change and the radiation
budget (Satheesh and Moorthy, 2005; Sokolik and Toon, 1996). Dust
particles with different sizes can be transported over different distances.
More specifically, dust particles with a size range of *r*>5 µm exist in source areas only, while particles with a size range of $\mathrm{0.1}<r<\mathrm{5}$ µm can experience airborne transportation over long distances (like about 5000 km) and even across continents from Asia to North
America (Jaffe et al., 1999; Satheesh and Moorthy, 2005). Therefore,
loess dust emitted from the CLP is expected to have important influence on the
radiation balance both at source areas and places far away from sources.

It is well known that dust particles have distinct nonspherical shapes, thus retrievals of dust aerosol properties, like optical thickness, based on Lorenz–Mie computations will lead to significant errors (Herman et al., 2005; Mishchenko et al., 2003). Optical modeling of dust particles with nonspherical shapes has been an essential subject. Dubovik et al. (2006) employed a mixture of spheroids with different axial ratios and spheres to reproduce laboratory-measured angular light scattering patterns of dust aerosols presented by Volten et al. (2001), and the best fitted shape distribution of spheroids was obtained and proposed. Subsequent studies on the retrievals of dust aerosol properties from space-based (Dubovik et al., 2011), airborne (Espinosa et al., 2019), and ground-based (Titos et al., 2019) remote sensing observations were all based on this shape distribution. However, the application of the same shape distribution of spheroids for different kinds of dust is too arbitrary (Li et al., 2019) and may not be suitable for simulating optical properties of loess dust with different size distributions. Furthermore, more precise optical models that are more complex than spheroids and similar to real dust morphology are still needed. Laboratory measurements of angular scattering patterns and basic physical features, like size distribution, refractive index, and microstructure, of loess dust with different sizes are essential and beneficial to the development of more precise models for loess dust. These models will further be useful for more accurate retrievals of dust aerosol properties over both source and downwind regions from remote sensing observations and more accurate assessments of radiative forcing at different regions.

Optical properties of dust particles vary with changes in their size
distributions. The light scattering matrix **F**, a 4×4 matrix containing
16 elements *F*_{ij} (*i*, *j*=1–4), is a fundamental optical property for
characterizing airborne dust particles and describes the depolarization or
transformation of incident light with several polarization states under the
influence of particles (Quinby-Hurt et al., 2000; Volten et al., 2001). This scattering matrix is not only sensitive to size distribution but also physical features like particle shape, microstructure, and
refractive index (Muñoz and Hovenier, 2011). Therefore, it can be
employed as a useful parameter to provide information and implications about
above features of dust particles. Based on similar operational principles,
several light scattering matrix measurement apparatuses were developed by
researchers over the past 2 decades (Liu et al., 2018; Muñoz et al., 2010; Volten et al., 2001; Wang et al., 2015). With the assistance of these apparatuses, scattering matrices for various mineral dust samples were
experimentally determined, such as loess, clay, desert dust, volcanic ash,
simulants of cosmic dust, and so on (Dabrowska et al., 2015; Escobar-Cerezo
et al., 2018; Merikallio et al., 2015; Muñoz et al., 2007, 2001). In addition, the Amsterdam Database and Amsterdam–Granada Database
were established in 2005 and 2012, respectively, to publish measured scattering matrices and necessary physical properties of mineral dust particles (Volten et al., 2005, 2006a; Muñoz et al., 2012).

Most of the published literature about experimental measurements of scattering
matrices has focused more on similarities and discrepancies between different
kinds of mineral dust or between the same kinds of dust sampled from
different sources. Furthermore, some researches paid more attention to the
effect of particle size distribution on scattering matrices. Olivine dust samples
with four size distributions were obtained using different sieves, but there
are no clear and consistent effects of size on measured scattering matrices
for olivine at both 442 and 633 nm wavelengths (Muñoz et al., 2000). Forsterite samples were produced with three size distributions using dry and wet sieving methods, and comparisons of experimental scattering matrices at 632.8 nm wavelength clearly showed the influence of size (Volten et
al., 2006b). Relative phase function is larger for large forsterite particles, *F*_{22}∕*F*_{11} is larger for small particles, $-{F}_{\mathrm{12}}/{F}_{\mathrm{11}}$ and *F*_{34}∕*F*_{11} are larger for small particles at most scattering angles but there are opposite trends for the negative branches at backscattering angles, *F*_{33}∕*F*_{11} and *F*_{44}∕*F*_{11} are larger for small particles at forward scattering angles but are smaller at backscattering angles. Two samples of palagonite with different size distributions were prepared by heating, and analyses of measured $-{F}_{\mathrm{12}}/{F}_{\mathrm{11}}$ revealed that small particles have larger $-{F}_{\mathrm{12}}/{F}_{\mathrm{11}}$ values at both 488 and 647 nm wavelengths (Dabrowska et al., 2015). Three commercial samples of Arizona Road Dust consisting of
ultrafine, fine, and medium particles were selected to investigate their
scattering matrices, results demonstrated that ultrafine particles have the
largest normalized phase function, while medium particles have the smallest
*F*_{22}∕*F*_{11} values (Wang et al., 2015). Lunar soil simulant JSC-1A particles were recovered and reused during scattering matrix measurement experiments: the recovered sample was larger than pristine sample, and comparative analyses indicated that large particles have larger relative phase function and $-{F}_{\mathrm{12}}/{F}_{\mathrm{11}}$, large particles have smaller *F*_{22}∕*F*_{11} at
forward scattering angles, and *F*_{22}∕*F*_{11} for these two samples was
nearly consistent at backscattering angles (Escobar-Cerezo et al., 2018). Experimentally determined $-{F}_{\mathrm{12}}/{F}_{\mathrm{11}}$ for meteorites illustrated
that the minimum value of $-{F}_{\mathrm{12}}/{F}_{\mathrm{11}}$ for larger particles is smaller,
and the maximum value of *F*_{12}∕*F*_{11} for larger particles is larger
(Frattin et al., 2019).

It can be concluded from above research that size distributions have
inconsistent effects on scattering matrix elements for different kinds of
dust particles and that there is no study paying attention to the effect of size
distribution on the scattering matrix for loess dust. Therefore, loess dust samples with
different size distributions were investigated in this study. An original loess
sample was collected from Luochuan, the center of the CLP, after sieving to
remove oversized particles, this “pristine loess” sample was used to represent
loess dust that is only present in source regions. Furthermore, part of
the pristine loess was ball-milled to obtain a finer “milled loess” sample
that can be transported over long distances and affect regions far away from
dust sources. Scattering matrices for the above loess samples with distinct size
distributions were measured at 532 nm with the help of a self-developed and
validated apparatus over 5–175^{∘} angles. Besides particle size distribution, other characteristics that might be changed during the milling process were also analyzed, such as chemical component, refractive index, and microscopic appearance. Discrepancies in angular behaviors of matrix elements were summarized and their reasons were discussed based on analyses of numerical simulations in the literature. Furthermore, synthetic scattering matrices were defined over 0–180^{∘}, and the previously published average scattering matrix for loess was updated.

In Sect. 2, fundamental characteristics of pristine loess and milled loess samples are shown. In Sect. 3, concise descriptions of related theory, apparatus, and methods are given. In Sect. 4, measured and synthetic scattering matrices for these two samples are plotted, reasons leading to these discrepancies in matrix elements are discussed, and the previous average scattering matrix for loess is updated. Finally, in Sect. 5 conclusions are drawn.

There are two deserts in the northern part of the Chinese Loess Plateau, and
according to the distances from these deserts, the CLP is roughly separated into
three regions: sandy loess, loess, and clayey loess (Cao et al., 2008). An original loess dust sample was collected from Loess National
Geological Park (35.76^{∘} N, 109.42^{∘} E) at Luochuan, which
is in the “loess zone” at the center of the CLP. Since this park is
the only national geological park in China that has typical loess
geomorphology, it can be considered that the sample collected represents
Chinese loess to a certain extent. Prior to laboratory investigations,
oversized particles in the original sample were removed through a 50 µm sieve. Next, the original loess sample was divided into two parts, one of which was not treated any more and was referred to as pristine loess and the other was milled by a ball miller to obtain finer particles, referred to here as milled loess. It should be noted that milled loess is the same sample as the “Luochuan loess” in Liu et al. (2019). Both of these loess dust samples were investigated through light scattering matrix measurements and auxiliary analyses of other physical characteristics of particles.

The size distributions of pristine loess and milled loess were determined by a laser particle sizer (SALD-2300; Shimadzu) using a dry measurement method, dry loess particles were injected into the measurement unit of laser particle sizer, and three independent repeated measurements were conducted for each sample. As can be seen from Fig. 1, the size of pristine loess shows a distinct bimodal distribution, and after ball-milling the particle size of milled loess becomes a unimodal distribution. From the viewpoint of atmospheric particle transportation, the majority (number fraction more than 70 %) of pristine loess particles have radii larger than 5 µm with peaks at about 3.9 and 10.7 µm, and thus this sample can be used to represent coarse dust that only affects source regions, like Xi'an city (Yan et al., 2015). On the other hand, almost all particles of the milled loess sample have radii smaller than 2 µm with a peak at about 0.55 µm and can be used as a representative of fine dust that can be transported over long distances and affect regions far away from dust sources.

SALD-2300 has 84 scattering light detectors in all, including 78 forward
detector elements, 1 side detector, and 5 back detectors. The best
fitted number size distribution and refractive index *m* can be obtained by
reproducing the measured angular distribution of light intensity based on Mie
calculations. Liu et al. (2003) revealed that Mie theory can be used to
reproduce forward scattering intensities of nonspherical particles with
moderate aspect ratios at scattering angles smaller than 20^{∘}.
Since over 70 % of the detectors of SALD-2300 are set at angles smaller
than 20^{∘}, the retrieved size distributions of nonspherical loess
dust based on Mie theory are of relatively high accuracy. During size
distribution measurements of loess samples, the retrieval ranges of the real
part Re(*m*) and imaginary part Im(*m*) of the refractive index were preset as 1.45–1.75 and 0–0.05, respectively (Volten et al., 2001). The smallest calculation steps of Re(*m*) and Im(*m*) are 0.05 and 0.01, respectively. As shown in Table 1, the optimal refractive indices are 1.65+0*i* for pristine loess and 1.70+0*i* for milled loess, and larger particles have relatively small real part of refractive index, which is similar to the results of Kinoshita (2001) and is caused by the nonspherical nature of loess dust. Retrieved refractive index of particles based on measured light intensity distribution
is a kind of optically equivalent refractive index, which is close to the
inherent refractive index of the measured particles. Based on measured size
distributions, effective radius *r*_{eff} and standard deviation *σ*_{eff} can be derived (Hansen and Travis, 1974):

where *n*(*r*)d*r* stands for number proportion of equivalent spheres whose radii vary between *r* and *r*+d*r*. Results of *r*_{eff} and *σ*_{eff} are shown in Table 1. In addition, effective size parameters ${x}_{\mathrm{eff}}=\mathrm{2}\mathit{\pi}{r}_{\mathrm{eff}}/\mathit{\lambda}$ for pristine loess and milled loess were also calculated and presented in Table 1.

Scanning electron microscope (SEM) images for pristine loess (Fig. 2a) and milled loess (Fig. 2b) are displayed in Fig. 2. Obviously, particles of these two samples exhibit various shapes, and all of the particles can be classified as having an irregular shape. Almost all particles have rough surfaces, and some particles even have sharp edges. After the milling process, there are more sub-micrometer particles in the milled loess sample, some small particles even stuck on the rough surfaces of large particles due to electrostatic forces.

During the dry milling process, nonmetal grinding balls with a 6 mm diameter
were used, the main component of which is ZrO_{2}. For the purpose of
detecting whether the chemical compositions of loess samples were changed,
the oxide compositions of samples before and after milling process, that is
the pristine loess and milled loess, were determined using a X-ray
fluorescence spectrometer (XRF-1800, Shimadzu), the detection limit of which
is 0.0001 wt %. As can be seen in Table 2, the largest change of content
occurs for SiO_{2}, but this change is less than 2.5 % and even smaller than the errors between repeat measurements for the pristine loess sample, and the change of ZrO_{2} is only about 0.03 %. It can be concluded
that the composition differences between these two samples are very small,
and that the milling process has little effect on the chemical composition of loess
samples.

## 3.1 Basic concepts about the light scattering matrix

Four Stokes parameters (*I*, *Q*, *U* and *V*) are usually used to introduce the intensity and polarization properties of light beam, and these parameters
can form a column vector, the so-called Stokes vector (Hovenier et al., 2014; Hulst and van de Hulst, 1981). If a cloud of particles is present in
light path, the incident beam will be scattered and part of light will
deviate from the original direction of propagation. When multi-scattering
plays a negligible role, the intensity and polarization state of scattered beams
can be calculated from that of the incident beam using a 4×4 light
scattering matrix **F** (Mishchenko and Yurkin, 2017):

where *λ* stands for wavelength of light, *D* is the distance between particle cloud and light detector, scattering angle *θ* is the angle
between incident and scattered beams, and the scattering plane contains both
incident and scattered beams.

Generally, **F** has 16 independent matrix elements *F*_{ij} with *i*, *j*=1–4. Two basic assumptions are commonly used to simplify the general form of the light scattering matrix. The first is that all scattering planes are equivalent for particles that have random orientations. Thus, scattering
directions can be adequately depicted by *θ*. The second assumption is that
particles and their mirror counterparts exist in the same number in a cloud
of randomly oriented particles. Based on the above random orientation and mirror
particle assumptions, the number of independent elements in the light scattering
matrix can be reduced from 16 to 6 (Mishchenko and Yurkin, 2017):

Matrix elements describe the depolarization or transformation of incident
light with several polarization states under the influence of particles (Quinby-Hurt et al., 2000). *F*_{11} describes the transformation of
incident light intensity. *F*_{12} describes the depolarization of 0 and 90^{∘} linearly polarized light relative to the scattering plane.
*F*_{22} describes the transformation of ±90^{∘} polarized incident
light to ±90^{∘} polarized scattered light and it is equal to *F*_{11} for spherical particles. *F*_{33} and *F*_{44} describe the transformation of ±45^{∘} linearly (or circularly) polarized incident light to ±45^{∘} linearly (or circularly) polarized scattered light, and these two elements are equal for spherical particles. *F*_{34} describes the transformation of circularly polarized incident light to ±45^{∘} linearly polarized scattered light. Almost all of these matrix
elements are sensitive to physical properties of particles, including size
distribution, particle shape, microstructure, and refractive index.

## 3.2 Experimental apparatus and methodology

Figure 3 shows a layout diagram of the improved scattering matrix measurement apparatus. The main improvement is that angle coverage at backscattering angles is extended to 175^{∘}, while the maximum coverage of the previous apparatus is 160^{∘} (Liu et al., 2018). The wavelength of incident beam is 532 nm, and there is a linear polarizer *P* and an electro-optic modulator (EOM) in its propagation path. Subsequently, the modulated incident light is scattered by particles in the scattering
zone, which are dispersed using an aerosol generator and are sprayed upwards
to the scattering zone through a nozzle. A photomultiplier, referred to here as the
“detector”, a 532 nm quarter-wave plate *Q*, and a polarizer *A* are fixed
on a rotation arm, the rotational center of which coincides with the center of the
aerosol nozzle. Before scattered light is detected by the detector, it
successively passes through *Q* and *A*. The dark cassette used to encapsulate the detector, *Q* and *A* in the previous apparatus, are removed, which facilitates the adjustment of orientation angles of *Q* and *A*. The detector is controlled by an electric rotary table and is able to scan scattering angles from 5 to 175^{∘}. Another photomultiplier referred to here as the “monitor” is fixed at a 30^{∘} scattering angle to record variations
in dust aerosols. The combination of an electro-optic modulator and lock-in
detector allows multiple scattering matrix elements or their sums to be
measured simultaneously. All of the matrix elements of dust samples can be
determined as functions of scattering angles with the help of various
combinations of orientation angles of the above optical elements, as shown in
Table 3, which is the same method as that of Muñoz et al. (2010).

Multiple groups of values of measurable quantities, i.e., the DC component
DC(*θ*), first harmonics *S*(*θ*), and second harmonics *C*(*θ*) of the voltage signal, are recorded at every scattering angle for each combination of optical elements. The first step of data processing is to average these recorded values and get their errors. The optical platform is surrounded by black curtains to avoid the effect of environmental stray light, and background signals need to be measured and subtracted. Fluctuations of dust aerosols can be eliminated by normalizing measurements of the detector using DC(30^{∘}) measured by the monitor. Scattering matrix elements can be extracted from preprocessed DC(*θ*), *S*(*θ*), and *C*(*θ*) according to Table 3. Subsequently, *F*_{11}(*θ*) is normalized to 1 at a 10^{∘} scattering angle, and the remaining matrix elements *F*_{ij}(*θ*) are normalized to *F*_{11}(*θ*) at the same angle. Finally, whether measurement results of scattering matrix satisfy the Cloude coherency matrix test should be examined (Hovenier and Van Der Mee, 1996). Three iterations of measurements are performed for each particle sample, the final results are the average of three groups of experiments, and the errors are also calculated, including errors during every measurement and errors for repeat measurements. Furthermore, the improved apparatus is validated using water droplets. All six measured nonzero scattering matrix elements for water droplets can be fitted well using Mie calculation results, indicating that the measurement accuracy of the apparatus is satisfactory. For more details about the measurement principles and validation methods of the apparatus, see Liu et al. (2018).

A dust generator (RBG 1000; Palas) was applied to disperse loess particles
(Liu et al., 2018). Re-aerosolized dust aerosols were transported to
scattering matrix measurement apparatus using a conductive tube and sprayed
upwards to the scattering zone through a nozzle. Some particles of each loess
sample were sprayed into vessels or sprayed onto copper grids for subsequent
size distribution measurements or SEM analyses. For reliable measurements of
the scattering matrix, experiments should be conducted under single-scattering
conditions. This requires that the number of particles in the scattering
zone is appropriate, as too many particles will result in significant multiple
scattering, while too few particles will not satisfy the two basic
assumptions mentioned above. Incident light intensity *I*_{0} and
transmitted light intensity *I* passing through particle cloud can be related
by the following equation (Mokhtari et al., 2005):

where $<s>$ stands for average number of scattering events. P(2)/P(1) $=<s>/\mathrm{2}$ is used to describe the ratio of occurrence probability of double-scattering event (the simplest form of multi-scattering) to that of the single-scattering event (Wang et al., 2015).

## 4.1 Experimentally determined scattering matrices

The measurements of $<s>/\mathrm{2}$ were conducted before the measurements of matrix elements using each orientation angle combination of the above optical elements. Measured $<s>/\mathrm{2}$ for both pristine loess and milled loess were smaller than about 0.006. In other words, the occurrence probability of the double-scattering event was about 170 times smaller than that of single-scattering event, and thus the double-scattering event can be ignored without question. For each loess sample, three independent and replicated measurements of the scattering matrix were conducted, and experimental results shown in the figures are averaged values for those three measurements. Examinations showed that measurements of loess samples satisfy the Cloude coherency matrix test at all scanned scattering angles.

Experimentally determined scattering matrix elements for both pristine
loess and milled loess are shown in Fig. 4. Only six element ratios
are plotted because the other ratios do not deviate from zero within
experimental error. Matrix element ratios for pristine loess and
milled loess present similar angular behaviors; more specifically,
angular distributions of all six nonzero matrix element ratios are limited
to narrow regions. Normalized phase functions
${F}_{\mathrm{11}}\left(\mathit{\theta}\right)/{F}_{\mathrm{11}}\left(\mathrm{10}{}^{\circ}\right)$ show strong forward scattering
peaks, and variations at backscattering directions are not obvious, which are
typical behaviors for mineral dust with irregular shapes (Muñoz et al., 2012; Volten et al., 2001). For non-polarized incident beams,
$-{F}_{\mathrm{12}}\left(\mathit{\theta}\right)/{F}_{\mathrm{11}}\left(\mathit{\theta}\right)$ is equivalent to the degree of linear
polarization. Measured angular behaviors of $-{F}_{\mathrm{12}}\left(\mathit{\theta}\right)/{F}_{\mathrm{11}}\left(\mathit{\theta}\right)$ are bell-shaped, and the largest values appear at near side-scattering directions. There are negative branches of $-{F}_{\mathrm{12}}\left(\mathit{\theta}\right)/{F}_{\mathrm{11}}\left(\mathit{\theta}\right)$ at both forward and backward scattering directions. *F*_{22}(*θ*)∕*F*_{11}(*θ*) is proof of the nonsphericity and irregularity of particles, since it is constant 1 for homogeneous spheres. Measured values of these two loess samples show that
*F*_{22}(*θ*)∕*F*_{11}(*θ*) values deviate from constant 1 at
nearly all angles scanned. The ratios *F*_{33}(*θ*)∕*F*_{11}(*θ*) and *F*_{44}(*θ*)∕*F*_{11}(*θ*) can be analyzed jointly because these two ratios are equal for particles with spherical shape. But for loess dust, *F*_{33}(*θ*)∕*F*_{11}(*θ*) values are smaller than *F*_{44}(*θ*)∕*F*_{11}(*θ*), especially at backscattering directions. The ratios *F*_{34}(*θ*)∕*F*_{11}(*θ*) show near “S-type” shapes and the maxima are obtained at about 115^{∘} angle. For scattering angles smaller than 50^{∘} and larger than 170^{∘}, values of *F*_{34}(*θ*)∕*F*_{11}(*θ*) are negative.

On the other hand, the discrepancies in matrix elements for pristine
loess and milled loess are still obvious. Compared to milled
loess, there is an enlargement of relative phase function at a 5^{∘}
scattering angle for pristine loess. The relative phase function for
pristine loess is also larger at side and back scattering angles. As for
ratio $-{F}_{\mathrm{12}}\left(\mathit{\theta}\right)/{F}_{\mathrm{11}}\left(\mathit{\theta}\right)$, small milled loess has smaller maximum values at near side scattering angles, while large pristine loess has relatively large maximum values. In contrast with ratio $-{F}_{\mathrm{12}}\left(\mathit{\theta}\right)/{F}_{\mathrm{11}}\left(\mathit{\theta}\right)$, measured *F*_{34}(*θ*)∕*F*_{11}(*θ*) has a larger maximum for the small milled loess sample. Experimentally determined *F*_{22}(*θ*)∕*F*_{11}(*θ*) values of milled loess are larger than pristine loess, especially at side and back scattering angles. It should be noted that discrepancies in measured *F*_{22}(*θ*)∕*F*_{11}(*θ*) cannot be directly used to indicate
difference of particle irregularity because optical calculations of
Gaussian spheres showed that *F*_{22}(*θ*)∕*F*_{11}(*θ*) values
are sensitive not only to particle irregularity but also to size
distribution (Liu et al., 2015). As for ratios *F*_{33}(*θ*)∕*F*_{11}(*θ*) and *F*_{44}(*θ*)∕*F*_{11}(*θ*), the
measurements for milled loess are larger than those for pristine
loess. In short, these discrepancies in scattering matrices between
pristine loess and milled loess are inconsistent with those for all
other kinds of dust with different size distributions in the literature.

In this study, several fundamental properties of loess dust samples were characterized for auxiliary analyses. As shown in Table 1, effective radii for pristine loess and milled loess are 49.40 and 2.35 µm, respectively. The real part of the refractive index for pristine loess is 1.65 and that for milled loess is 1.70. Table 2 shows that the changes in chemical components are negligible. Therefore, it is reasonable to suspect that distinctions in angular distributions of measured scattering matrix elements for two loess samples may be mainly caused by different size distributions (effective radii differ by more than 20 times), while differences in other factors such as refractive index and microstructure have relatively small contributions in leading to different scattering matrices.

Literature focused on optical modeling of irregular mineral dust was
analyzed to find reasonable explanations for the differences in scattering
matrix elements for milled loess and pristine loess samples.
Numerical simulations of Gaussian spheres showed that as effective size
parameter increases from 30 to 600, phase function *F*_{11} and
*F*_{33}∕*F*_{11} and *F*_{44}∕*F*_{11} ratios decrease, the maximum of ratio
*F*_{34}∕*F*_{11} decreases and its negative branches at forward scattering
and backscattering directions become small, the maximum of ratio
$-{F}_{\mathrm{12}}/{F}_{\mathrm{11}}$ increases, and the ratio *F*_{22}∕*F*_{11} increases,
especially at backscattering angles (Liu et al., 2015). When Gaussian
spheres become more nonspherical and irregular, phase function *F*_{11} and $-{F}_{\mathrm{12}}/{F}_{\mathrm{11}}$, *F*_{22}∕*F*_{11}, *F*_{33}∕*F*_{11} and
*F*_{44}∕*F*_{11} ratios show different trends compared with the influences of
increasing effective radius, while the *F*_{34}∕*F*_{11} ratio shows a similar
trend (Liu et al., 2015). Zubko et al. (2007) showed that as the surfaces of Gaussian particles become rougher, the ratio $-{F}_{\mathrm{12}}/{F}_{\mathrm{11}}$ tends to be larger. Simulations of agglomerated debris particles showed that while the imaginary part of refractive index varies in the range 0–0.01, the scattering matrix elements remain almost unchanged (Zubko et al., 2013). However, calculations of Gaussian particles conducted by Muinonen et al. (2007) showed that an increase in refractive index (both real and imaginary part) leads to smaller $-{F}_{\mathrm{12}}/{F}_{\mathrm{11}}$ and *F*_{22}∕*F*_{11}. In summary, different factors have different or similar effects on certain matrix elements. The discrepancies in scattering matrices for milled loess and pristine loess can be mainly interpreted from the perspective of difference of effective radii, while differences in other factors such as refractive index and microstructure have relatively small contributions, and Gaussian spheres may be promising models for simulating scattering matrix for loess dust.

In this work, a relatively good case is presented to show the effect of size distribution of loess dust on scattering matrices because effective radii of pristine loess and milled loess differ by more than 20 times. The influence of loess particle size is roughly verified through qualitative analyses of simulation results of Gaussian spheres, which deepen the understanding of this effect. For more detailed explanations, quantitative analyses are still needed based on many more optical simulations of Gaussian spheres. However, besides size distribution, physical properties such as refractive index and microstructure also play important roles in determining scattering matrices of dust particles. When the difference in particle size distributions or effective radii is relatively small, the influences of other factors may become dominant or unignorable. This may be the reason why the effect of size distribution on measured scattering matrices for olivine samples cannot be concluded clearly (Muñoz et al., 2000), and this may also be the reason why effective radii cannot be used to explain all the discrepancies in matrix elements for forsterite samples based on simulation results of Gaussian spheres (Volten et al., 2006b). Another reason may be that Gaussian spheres are not suitable models to reproduce the measured scattering matrix for forsterite dust (Volten et al., 2006b), as optical modeling of irregular mineral dust is still a challenging subject.

## 4.2 Synthetic scattering matrices

Laboratory measurements of scattering matrices only cover scattering angles
from 5 to 175^{∘}. In order to obtain a scattering matrix over 0–180^{∘}, synthetic scattering matrices *F*^{syn} are constructed by a combination of numerical simulation and extrapolation of experimental measurements (Dabrowska et al., 2015; Escobar-Cerezo et al., 2018).

Measured *F*_{11}(*θ*) values are normalized to 1 at 10^{∘},
and these relative phase functions are the same for measured and synthetic
scattering matrices for the same sample (Escobar-Cerezo et al., 2018):

where ${F}_{\mathrm{11}}^{\mathrm{syn}}\left(\mathit{\theta}\right)$ is the synthetic phase function that must fulfill the following normalized equation:

SEM images for both loess samples show that most particles have relatively
moderate aspect ratios. Therefore, Lorenz–Mie theory can be used to
calculate forward peaks of synthetic phase functions at angles smaller than
5^{∘} because for particles that have moderate aspect ratios forward peaks of synthetic phase functions mainly depend on size distributions and depend little on particle shapes (Liu et al., 2003). Refractive indices and size distributions for pristine loess and milled loess obtained from a particle sizer are used in Lorenz–Mie calculations. For the 180^{∘} scattering angle, multi-order polynomial extrapolation is used on the basis of experimentally determined relative phase functions. Following this, the calculated forward peak of the phase function and relative phase function after extrapolation are incorporated at a 5^{∘} angle to construct the synthetic phase function. Whether the synthetic phase function satisfies Eq. (7) should be checked. Otherwise, increase or decrease measured relative phase function at a 5^{∘} angle within measurement error and repeat the merging process and checking process until Eq. (7) is satisfied.

As for other matrix element ratios *F*_{ij}(*θ*)∕*F*_{11}(*θ*), a
set of constraints at 0 and 180^{∘} scattering angles
should be taken into consideration (Hovenier et al., 2014; Mishchenko
and Hovenier, 1995):

Synthetic values for ratio *F*_{22}∕*F*_{11} at a 180^{∘} angle for
pristine loess and milled loess are obtained by ninth-order polynomial extrapolations. Then *F*_{33}∕*F*_{11} and *F*_{44}∕*F*_{11} at 180^{∘} are calculated according to Eqs. (10) and (11), respectively. In addition, the right-hand (left-hand) derivative at 0^{∘} (180^{∘}) for each scattering matrix element must be 0 (Hovenier and Guirado, 2014). In Fig. 5, synthetic matrices for pristine loess and milled loess are illustrated.

Using the extrapolated value of *F*_{22}∕*F*_{11} at a 180^{∘} scattering angle,
the backscattering depolarization ratio *δ*_{L} can be calculated, which is an essential parameter for aerosol lidar observations (Mishchenko et al., 2002).

Calculated backscattering depolarization ratios for pristine loess and
milled loess are 0.21 and 0.26, respectively; milled loess has a
larger value of *δ*_{L}. Direct measurements of backscattering
depolarization ratios of Arizona Test Dust with different size distributions
at both 355 and 532 nm wavelengths also showed that *δ*_{L} values
for small particles are larger than those for large particles, and this
discrepancy is more pronounced at 532 nm (Miffre et al., 2016).

Finally, the previously published average scattering matrix for loess, which
consists of results for Hungary loess, milled Yangling loess, and milled
Luochuan loess (the latter two were sampled from the CLP), was updated using new
sample pristine loess from Luochuan by averaging synthetic matrices for
different loess samples. In other words, the differences between the average
matrix before and after the update are also the differences between pristine
loess and the other three samples, and differences among these three
samples can be found in Liu et al. (2019). As shown in Fig. 6, compared to other three samples, phase function for pristine loess has larger forward scattering peaks and smaller values in the side scattering and backscattering directions. Pristine loess has larger $-{F}_{\mathrm{12}}\left(\mathit{\theta}\right)/{F}_{\mathrm{11}}\left(\mathit{\theta}\right)$ values at near side scattering angles, has larger *F*_{22}(*θ*)∕*F*_{11}(*θ*) values at almost all scattering angles, and has smaller values of both *F*_{33}(*θ*)∕*F*_{11}(*θ*) and *F*_{44}(*θ*)∕*F*_{11}(*θ*) in
backscattering directions, when compared with the other three samples.

Asian dust contributes a lot to global atmospheric dust aerosol, and the Chinese Loess Plateau (CLP) is one of the main origins of Asian dust. Loess dust aerosols originating from the CLP are expected to potentially affect the radiation balance at both source areas and downwind areas far from sources because dust particles with different sizes can be transported over different distances. In this study, an original loess sample was collected from Luochuan, which is centrally located on the CLP. Subsequently, two loess samples with different size distributions were prepared for laboratory investigations. A pristine loess sample was used to represent loess dust that affects source regions only, and a milled loess sample that was ball-milled from pristine loess was used to represent loess dust that can be transported over long distances.
Light scattering matrices for both pristine loess and milled loess
samples at a 532 nm wavelength were measured from 5 to 175^{∘} scattering angles. Besides particle size distribution, other basic properties were also characterized, such as chemical component, refractive index, and microscopic appearance.

Even through experimentally determined angular behaviors of scattering
matrix elements for pristine loess and milled loess are similar,
there are still obvious discrepancies in matrix elements. More specifically,
for small milled loess, relative phase function ${F}_{\mathrm{11}}\left(\mathit{\theta}\right)/{F}_{\mathrm{11}}\left(\mathrm{10}{}^{\circ}\right)$ and $-{F}_{\mathrm{12}}\left(\mathit{\theta}\right)/{F}_{\mathrm{11}}\left(\mathit{\theta}\right)$ and *F*_{22}(*θ*)∕*F*_{11}(*θ*) ratios are smaller than that for coarse pristine loess, while *F*_{33}(*θ*)∕*F*_{11}(*θ*), *F*_{34}(*θ*)∕*F*_{11}(*θ*), and *F*_{44}(*θ*)∕*F*_{11}(*θ*) ratios are larger than that for coarse pristine loess. These discrepancies are unique and different from those for other kinds of
dust with distinct size distributions published in literatures. Qualitative
analyses of optical simulations of various morphological models showed that
the large difference in size distributions (effective radii differ by more
than 20 times) caused by milling process plays a major role in leading to
discrepancies in scattering matrices for these two samples, while
differences in factors such as refractive index and microstructure have
relatively small and recessive contributions. Gaussian sphere models may
have good application prospects for optical modeling of loess dust, while more
detailed quantitative verification using measured physical properties is
still needed.

Synthetic scattering matrices for both pristine loess and milled
loess were defined over 0–180^{∘} scattering angle, and the previously presented average scattering matrix for loess was updated
with the new coarse pristine loess sample included. The phase function
*F*_{11}(*θ*) in the updated average matrix has larger forward scattering
peaks and smaller values at side and backward scattering angles than that in the
previous average matrix. Compared to the previous average matrix, the updated
average matrix has larger $-{F}_{\mathrm{12}}\left(\mathit{\theta}\right)/{F}_{\mathrm{11}}\left(\mathit{\theta}\right)$ at side
scattering angles and has smaller *F*_{33}(*θ*)∕*F*_{11}(*θ*) and
*F*_{44}(*θ*)∕*F*_{11}(*θ*) at backscattering angles.
*F*_{22}(*θ*)∕*F*_{11}(*θ*) experiences the largest change between before
and after the update, having values that are enlarged at almost all scattering angles.

In this study, scattering matrices for Chinese loess samples with large differences in their size distributions are investigated. Based on all the measurements, suitable shape distributions of spheroids can be obtained, which are useful for the retrievals of airborne loess dust properties at both source and downwind areas in China or even East Asia. On the other hand, the updated average scattering matrix for loess is meaningful for the validation of exiting models and the development of more advanced morphological models suitable for loess dust, which are also useful to finally improve the retrieval accuracies of dust aerosol properties.

Fine loess dust sampled from Luochuan and Yangling, two regions of the Chinese Loess Plateau, were investigated by Liu et al. (2019). Local variations in loess dust also have obvious effects on the measured scattering matrices. It should be noted that all these samples investigated still cannot completely represent the loess in Chinese Loess Plateau and China, so one of the efforts in the future is to investigate more loess samples collected from more regions and with more size distributions. Accordingly, the average scattering matrix for loess will be updated constantly. On the other hand, the validation of existing models and the development of more advanced models through reproducing measured scattering matrices using optical simulation results are also meaningful research directions.

All the data involved in this study are available online at https://github.com/liujia93/Scattering-matrix-for-loess-dust (last access: 17 July 2020, Liu, 2020).

JL and QZ designed the experiments. JL conducted the measurements. YH drew the layout diagram. All authors discussed the results. JL wrote the manuscript.

The authors declare that they have no conflict of interest.

We are very grateful to Zidong Nie for loess dust sampling. We are also very grateful to Engineer Chao Li from Hefei Ke Jing Materials Technology Co., Ltd. for milling the dust particles.

This research has been supported by the National Natural Science Foundation of China (grant nos. U1733126 and 41675024), the National Key Research and Development Program of China (grant nos. 2016YFC0800100 and 2017YFC0805100), and the Fundamental Research Funds for Central Universities of China (grant no. WK2320000040).

This paper was edited by Alexander Kokhanovsky and reviewed by six anonymous referees.

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