Measurements of the Volume Scattering Function and the Degree of Linear Polarization of Light Scattered by Contrasting Natural Assemblages of Marine Particles

: The light scattering properties of seawater play important roles in radiative transfer in the ocean and optically-based methods for characterizing marine suspended particles from in situ and remote sensing measurements. The recently commercialized LISST-VSF instrument is capable of providing in situ or laboratory measurements of the volume scattering function, β p ( ψ ) , and the degree of linear polarization, DoLP p ( ψ ) , associated with particle scattering. These optical quantities of natural particle assemblages have not been measured routinely in past studies. To fully realize the potential of LISST-VSF measurements, we evaluated instrument performance, and developed calibration correction functions from laboratory measurements and Mie scattering calculations for standard polystyrene beads suspended in water. The correction functions were validated with independent measurements. The improved LISST-VSF protocol was applied to measurements of β p ( ψ ) and DoLP p ( ψ ) taken on 17 natural seawater samples from coastal and offshore marine environments characterized by contrasting assemblages of suspended particles. Both β p ( ψ ) and DoLP p ( ψ ) exhibited signiﬁcant variations related to a broad range of composition and size distribution of particulate assemblages. For example, negative relational trends were observed between the particulate backscattering ratio derived from β p ( ψ ) and increasing proportions of organic particles or phytoplankton in the particulate assemblage. Our results also suggest a potential trend between the maximum values of DoLP p ( ψ ) and particle size metrics, such that a decrease in the maximum DoLP p ( ψ ) tends to be associated with particulate assemblages exhibiting a higher proportion of large-sized particles. Such results have the potential to advance optically-based applications that rely on an understanding of relationships between light scattering and particle properties of natural particulate assemblages. another independently-calibrated light scattering instrument, DAWN-EOS. Although the correction functions developed in this study are applicable only to the speciﬁc version of LISST-VSF instrument and the data processing code used in this study, our results emphasize a general need for evaluating the performance of light scattering instruments and minimizing the associated uncertainties in quantitative determinations from measurements.


Introduction
It has long been recognized that inherent light-scattering properties of natural waters are of crucial importance and have strong potential for wide-ranging applications in aquatic sciences, including oceanography. These properties are essential inputs to the radiative transfer models used to compute the ambient light fields in natural water bodies [1][2][3][4]. The variability in the light scattering properties of seawater is driven primarily by the concentration of suspended particles, particle size distribution, and composition through particle refractive index, internal structure, and shape. Hence, scattering measurements carry potentially useful information about characteristics of natural particle assemblages. For example, the scattering and backscattering coefficients of suspended particles have been shown to provide useful proxies of mass concentration of total suspended particulate matter (SPM), particulate inorganic carbon (PIC), and particulate organic carbon (POC) in the ocean [5][6][7]. Multi-angle light scattering measurements provide a means to estimate the particle size distribution [8][9][10][11], including the submicrometer size range [12][13][14]. The angular pattern of light scattering can also contain useful information about the composition of particulate assemblages, including the bulk refractive index of particles [15][16][17][18][19]. In addition, measurements of the scattering matrix that provide information about polarization effects of light scattering [15,[20][21][22][23] have the potential for identifying and discriminating different types of particles, such as phytoplankton species or minerals, which are present in complex natural assemblages [24][25][26][27][28][29][30][31][32][33][34]. Despite the potential usefulness of information provided by light scattering measurements, the complexity and variability in composition of natural particulate assemblages impose significant challenges in achieving an understanding of bulk light-scattering properties of seawater in terms of detailed compositional characteristics of particulate matter [35].
The volume scattering function, β p (ψ, λ), and the degree of linear polarization, DoLP p (ψ, λ) of light scattered by marine particles are of primary interest in this study. Here, ψ denotes the scattering angle, λ the light wavelength in vacuum, and the subscript p indicates that the quantity is associated with particles. When the subscript p is omitted, the quantity describes the scattering by the entire suspension with additive contributions from both water molecules and suspended particles. The volume scattering function, β(ψ, λ) [in units of m −1 sr −1 ], is one of the fundamental inherent optical properties (IOPs) of seawater, which describes the scattered intensity as a function of scattering angle per unit incident irradiance per unit volume of small sample of water [2]. Several light-scattering related IOPs can be derived from β(ψ, λ). For example, integrating β(ψ, λ) over all scattering directions gives the total spectral scattering coefficient, b(λ) [m −1 ]. In this integration, it is commonly assumed that light scattering by an assemblage of randomly-oriented scatterers (molecules and particles) in natural waters is azimuthally symmetric about the incident direction of light beam. When β(ψ, λ) is normalized by b(λ), the resulting scattering phase function β(ψ, λ) [sr −1 ] provides a useful indicator of the angular shape of the volume scattering function. In optical remote sensing applications based on measurements with above-water sensors (e.g., from satellites or aircraft), the spectral backscattering coefficient, b b (λ) [m −1 ], is particularly useful. This coefficient can be obtained by integrating β(ψ, λ) over the range of backward scattering angles [2].
The volume scattering function provides incomplete information, in the sense that it does not contain information about polarization effects associated with light scattering. A complete characterization of elastic incoherent interactions of light at arbitrary wavelength λ with a sample volume of seawater is provided by a 4 × 4 scattering matrix, often referred to as the phase matrix or Mueller matrix [20][21][22][23]. This matrix describes a linear transformation of irradiance and polarization of an incident beam described by a 4-component Stokes vector into the intensity and polarization of the scattered beam that is also described by its corresponding Stokes vector. β(ψ, λ) is related to the first element of the scattering matrix, p 11 (ψ, λ), and can be obtained from a measurement using unpolarized light for illumination of sample and measuring the total scattered intensity. The degree of linear polarization of scattered light, DoLP(ψ, λ), describes the proportion of linearly polarized light relative to total intensity of the scattered light beam. As described in greater detail below, for various assemblages of particles including suspended marine particles and when the incident light beam is unpolarized, this quantity can be derived from the first two elements of the scattering matrix, which requires measurements involving linear polarization [29,36,37].
Despite the relative importance of β(ψ, λ) and DoLP(ψ, λ) of seawater and the associated particulate components β p (ψ, λ) and DoLP p (ψ, λ), the ocean optics community has historically relied mostly on simplified theoretical models (such as Mie scattering theory for homogenous spheres) and a limited dataset of measurements made with custom-built light scattering instruments. For example, over the past several decades, a limited dataset of β(ψ, λ) measurements made by Petzold [38] was widely used as a standard input for the particulate scattering phase function for radiative transfer modeling in the ocean. Comprehensive determinations of the scattering matrix for natural seawater have been very scarce [39][40][41][42]. These determinations showed that the off-diagonal matrix elements for seawater are very small or negligible, indicating very small effects associated with optical activity or orientational anisotropy of seawater scatterers [37,42]. More recently, several light scattering sensors have been developed for in situ deployments or laboratory use [43][44][45][46], but to our knowledge, none of these sensors are commercially available. While measurements with these new sensors have already significantly contributed to the increase of available datasets of β(ψ, λ) (or β p (ψ, λ) which can usually be satisfactorily estimated by subtracting the contribution associated with water molecules) in various oceanic environments [44,47,48], the determinations of DoLP p (ψ, λ) for natural assemblages of marine particles remain very scarce, as indicated by the rarity of scattering matrix measurements of seawater.
Recently, a new light scattering instrument, the LISST-VSF (Sequoia Scientific, Inc., Bellevue, WA, USA), has become commercially available, and provides the capability of determining both the volume scattering function and the degree of linear polarization of scattered light at a single light wavelength (532 nm) with high angular resolution over the range~0.1 • to 155 • [49]. It is capable of both in situ and benchtop measurements on water samples. This commercial instrument is expected to enable routine measurements by different groups of investigators, so it has the potential to enhance our understanding of light scattering properties of seawater and marine particles and advance the related applications. In this study, we report on LISST-VSF measurements of β p (ψ) and DoLP p (ψ) and size and compositional characteristics for contrasting natural particulate assemblages from marine coastal and offshore environments. The particulate scattering (b p ) and backscattering (b bp ) coefficients have also been determined from measured β p (ψ).
To fully realize the potential of such quantitative determinations for seawater samples from this new instrument, we also conducted an evaluation of the LISST-VSF performance through a series of laboratory experiments using samples of National Institute of Standards and Technology (NIST) certified standard polystyrene beads ranging in diameter between 100 nm and 2 µm. These measurements were compared with theoretical simulations of light scattering by bead suspensions using Mie scattering computations. With this approach, we developed corrections to the determinations of β p (ψ) and DoLP p (ψ) from LISST-VSF measurements. A validation of the corrected measurements was performed using independent measurements of multi-angle light scattering with another instrument, the DAWN-EOS (Wyatt Technology Corporation, Santa Barbara, CA, USA).

Methods
The description of methods includes two main parts: first, a description of laboratory experiments and Mie scattering calculations for standard polystyrene beads which were carried out to evaluate the performance of the LISST-VSF instrument and develop a calibration correction; second, a description of measurements on natural assemblages of marine particles from coastal and offshore oceanic environments.

Laboratory Experiments and Mie Scattering Calculations to Evaluate LISST-VSF
In order to evaluate the LISST-VSF instrument, light scattering and beam attenuation measurements were made in the laboratory on samples of nearly monodisperse standard polystyrene spherical beads with mean nominal diameters of 100, 200, 400, 500, 700, and 2000 nm, which were suspended in water (Table 1). In addition to LISST-VSF, two other instruments were used in these experiments, a DAWN-EOS for measuring multi-angle light scattering and a dual beam UV/VIS spectrophotometer Lambda 18 (Perkin-Elmer, Inc., Waltham, MA, USA) equipped with a 15-cm integrating sphere (Labsphere, Inc., North Sutton, NH, USA) for measuring the beam attenuation coefficient of particles in suspension. The use of standard beads ensures that Mie scattering calculations for homogeneous spherical particles can be used to calculate the Mueller matrix elements for these particles to determine reference (expected) values of the volume scattering function and the degree of linear polarization. The comparison of measurements with such reference values allows for evaluation of performance of LISST-VSF instrument and formulation of calibration correction functions for improved determinations of the volume scattering function and the degree of linear polarization from this instrument. This type of approach, which combines measurements on standard well-characterized particles with accurate scattering calculations, has been previously used for the evaluation, calibration, and characterization of light scattering instruments [29,43,44,50]. Although the evaluation results presented in this study are relevant to the specific version of the LISST-VSF instrument used in our laboratory, most methodological aspects are generally applicable to evaluation of other light scattering instruments. Table 1. Information on the polystyrene bead size standards used to create laboratory sample suspensions for experiments. The nominal bead diameter (D), catalog number, and actual mean diameter D (± standard error of estimate) and standard deviation of the mean (SD) provided by the manufacturer (Thermo Fisher Scientific, Inc.) is listed. The particulate beam attenuation coefficient at light wavelength 532 nm of the master sample as determined with a spectrophotometer, c SPEC p , is listed in addition to specific dilution names and factors (e.g., DF1, DF2, etc.) of the master suspension used for LISST-VSF measurements at different PMT gain settings. The dilution factors in italic font denote the experimental data used for generation of the final correction functions CF f and BF f , and those in boldface font denote the six examples used for statistical evaluation in Table 2

Instrumentation
A LISST-VSF instrument (S/N 1475) was equipped with a custom designed 2 L sample chamber for benchtop laboratory use. This chamber effectively rejects ambient light and promotes good mixing conditions to maintain particles in suspension. For sample illumination the LISST-VSF uses a frequency-doubled YAG laser to produce a beam of light at a wavelength of 532 nm with a Gaussian beam profile of 3 mm in diameter. A single measurement takes approximately 4 s and consists of two scans of a 15-cm path within the sample, each with a different linear polarization state of the incident beam, i.e., parallel and perpendicular to the scattering plane. Scattered intensity is measured at multiple scattering angles ψ from 0.09 • to 15.17 • with 32 logarithmically-spaced ring detectors and from 14 • to 155 • with 1 • interval using a fixed axis Roving Eyeball sensor equipped with photomultiplier tubes (PMTs). For the Roving Eyeball, scattered light is split between two PMTs with a polarizing prism allowing for only parallel or perpendicularly polarized light to be detected by each PMT. To enable measurements of large dynamic range of scattered intensity with a single PMT, the laser power is dimmed by a factor of 8 for the angular range 14-63 • and returned to full power for 64-155 • . The beam attenuation coefficient, c, is also measured at light wavelength of 532 nm for the 15-cm path length of the sample.
For incoherent elastic scattering of light at a given wavelength λ by a collection of particles suspended in water, the Stokes vector of incident light beam, S i = [I i Q i U i V i ] T , where T represents the transpose operation, is transformed into the Stokes vector of scattered beam, S s (ψ), by a scattering matrix, P(ψ). For an ensemble of randomly-oriented particles exhibiting certain symmetry properties and no optical activity, the scattering matrix simplifies to 6 independent non-zero elements [20,36,51] where λ has been omitted for brevity, C is a constant factor (for a given sample, light wavelength, and measurement geometry), p 11 (ψ) represents the scattering phase function, and the reference plane is the scattering plane containing the incident and scattered directions [20,51,52]. This form provides a reasonable description of the measured scattering matrix by suspensions of randomly-oriented marine particles, including various specific types of particles present in seawater [24,29,33,36,37,42]. In the case of unpolarized incident light (i.e., Q i , U i , and V i are all zero), the volume scattering function β(ψ) equals (to within a constant factor) p 11 (ψ), and the degree of linear polarization DoLP(ψ) can be determined from [29,36,37,53] Positive values of DoLP(ψ) are for dominantly perpendicular polarization and negative values for dominantly parallel polarization. We note that this definition of DoLP(ψ) has been widely used for characterizing the inherent scattering properties of various types of particles beyond aquatic particles, such as aerosol particles and cosmic dust [30,[54][55][56][57][58].
The LISST-VSF measurements of forward scattering within the angular range 0.09-15.17 • are made with two linear polarization states of the incident beam, but with no polarization analyzers of the ring detectors. For the ring detectors, the calibrated β(ψ) in absolute units is a standard output of the manufacturer's processing software. The absolute calibration is based on the manufacturer-provided conversion from ring detector counts to physical units using radiant sensitivity of ring detectors [59,60]. Detection of scattered light within the angular range 14-155 • using the Roving Eyeball sensor employs measurements made with two linear polarization states of the incident beam and the corresponding two linear polarization states of the scattered light. The four measurement configurations allow for the determination of relative values of p 11 (ψ), p 12 (ψ), and p 22 (ψ). The calibrated β(ψ) values within the Roving Eyeball angular range are obtained by scaling the p 11 (ψ) data from the Roving Eyeball sensor. Specifically, the scattering measurements from the first angles of the Roving Eyeball sensor are forced to match the calibrated β(ψ) values from the overlapping last ring detectors. The DoLP(ψ) values are obtained from Equation (2) using p 11 (ψ) and p 12 (ψ), and are also included in the standard output of the manufacturer's processing code.
We also used a DAWN-EOS multi-angle light scattering instrument which provided independent measurements of β(ψ) and DoLP(ψ) of polystyrene beads suspended in water. These measurements were made with a sample placed in a 20 mL cylindrical glass vial. The DAWN-EOS instrument used in this study has been previously characterized and calibrated for such measurement configuration [61]. This instrument uses a diode-pumped frequency-doubled Nd-YAG laser at light wavelength 532 nm with a Gaussian beam profile of 62 µm in diameter. The interrogated sample volume is on the order of 10 nL. The incident beam can be linearly polarized both parallel and perpendicular to the scattering plane. The intensity of scattered light is measured simultaneously with eighteen photodiode detectors and no polarization analyzers, enabling measurements within a range of scattering angles from 22.5 • to 147 • . To encompass the large dynamic range of scattered intensity, three selectable gain settings are available for each detector (gain factors of 1, 21, or 101).
As the DAWN-EOS detectors have no polarization analyzers, they only measure the first parameter of Stokes vector of the scattered light, I s (ψ). Here we define I s (ψ) for the parallel polarization of the incident beam and I s⊥ (ψ) for the perpendicular polarization of the incident beam. The matrix elements p 11 (ψ) and p 12 (ψ) can be obtained (to within a constant factor) from DAWN-EOS measurements as which allows for determination of DoLP(ψ) from Equation (2). The calibration procedure described in Babin et al. [61] allows for determination of β(ψ) in absolute units. Importantly, the calibration procedure of DAWN-EOS is fundamentally different from the calibration procedure of LISST-VSF. The manufacturer's calibration of LISST-VSF is based on a nominal radiant sensitivity of ring detectors (amperes of photoelectric current per watt of optical power) traceable to the National Institute of Standards and Technology [59,60]. In contrast, the calibration of DAWN-EOS is based on measurements of light scattered at 90 • by pure toluene with the incident beam having a linear perpendicular polarization [61]. This calibration relies on the known magnitude of molecular scattering by toluene. The two different methods employed in calibration of LISST-VSF and DAWN-EOS allow for comparisons of independent estimates of β(ψ) obtained by these instruments. We also recall that the DoLP(ψ) estimates obtained with the two instruments within the common range of scattering angles are based on different polarization measurement configurations used by these instruments. A Lambda 18 spectrophotometer was used to collect independent measurements of the spectral beam attenuation coefficient, c(λ), of polystyrene beads suspended in water. These measurements were made for comparisons with the beam attenuation data obtained with LISST-VSF, and also to aid in the preparation of samples with appropriate concentrations of polystyrene beads to ensure that measurements with LISST-VSF and DAWN-EOS were made within the single scattering regime. The spectrophotometric measurements were made in the spectral range from 290 nm to 860 nm with 1 nm interval, but only data at 532 nm are used in this study. The general applicability of laboratory spectrophotometers with proper modifications to enable measurements of beam attenuation of particle suspensions, including colloidal samples, has long been recognized [62,63]. In our study, a sample of particle suspension was measured in a 1-cm quartz cuvette placed at a significant distance from the detector (~25 cm from the entrance of the integrating sphere), and field stops were aligned within the light path to reduce the size of the beam and acceptance angle of the detector to less than 1 • . This measurement geometry has been used in our previous studies of spectral beam attenuation by various particle assemblages [64,65].

Experimental Procedure
Baseline measurements of 0.2 µm filtered water were collected with all three instruments used in the experiments; LISST-VSF, DAWN-EOS, and Lambda 18 spectrophotometer. These baseline measurements were subtracted from subsequent measurements taken on particle suspensions to determine the optical properties associated with suspended particles only, i.e., the particulate volume scattering function, β p (ψ), the particulate degree of linear polarization, DoLP p (ψ), and the particulate beam attenuation coefficient, c p .
Original manufacturer's stock samples of standard polystyrene beads (100, 200, 400, 500, 700, and 2000 nm in diameter) were used to generate master samples using 0.2 µm filtered, deionized, and degassed water as a medium (with the exception of 2000 nm beads which used 0.2 µm filtered seawater). In the process of preparation of master samples, the particle concentration was optimized to ensure that spectrophotometric measurements of beam attenuation coefficient can be performed either directly or with small dilution factor (~3) on these samples over 1-cm path length with sufficiently high signal but negligible multiple scattering effects. The c p values for master samples ranged from about 18 m −1 to 58 m −1 ( Table 1).
The master sample was diluted for measurements with the LISST-VSF to avoid oversaturation of PMT detectors and multiple scattering over the longer path length (15 cm). For baseline measurements, the LISST-VSF sample chamber was filled with 1900 mL of 0.2 µm filtered water. The final samples of particle suspensions were created by addition of 20 to 100 mL of master sample to the LISST-VSF chamber. For most beads examined in our experiments, more than one particle suspension differing in terms of particle concentration was measured with LISST-VSF ( Table 1). The different particle concentrations were achieved by different dilution of master sample within LISST-VSF chamber. Owing to different dilution factors ranging from 20 to 96 (labeled as DF1, DF2, and DF3 in Table 1), the c p values of LISST-VSF samples ranged from about 0.5 m −1 to 1.8 m −1 . For a single bead size, concentration, and PMT gain, a series of LISST-VSF measurements was composed of 200 measurements taken in rapid succession (recall that a measurement refers to two scans, each with a different polarization of incident beam). This measurement series was divided into five sets of 20 measurements and one set of 100 measurements to enable manual gentle mixing of sample before each set of measurements. In addition, for the 2000 nm bead suspensions a magnetic stir bar which operated on low speed and changed direction of rotation every 30 s was used to prevent particle settling during the measurement.
Several LISST-VSF baseline measurements of 0.2 µm filtered water were collected for each experiment, i.e., for each examined bead size. However, for reasons of consistency and out of the desire to use an optimal baseline representative of the least contaminated 0.2 µm filtered water, a single baseline was used for processing of all experimental data collected for various bead sizes and concentrations except for 2000 nm sized beads which used 0.2 µm filtered seawater. This baseline was determined on the basis of finding a measurement which exhibited minimal scattering signal detected by Roving Eyeball and ring detectors and maximum directly transmitted light detected by the laser transmission sensor. We note, however, that for each PMT gain setting of the Roving Eyeball sensor a separate baseline was determined.
Measurements using the DAWN-EOS instrument were collected for 100, 200, 400, and 700 nm beads. Dilution factors of master samples for DAWN-EOS measurements were between 300 and 3000, depending on bead size. The gain settings for each detector were adjusted to the highest setting that would avoid saturation of signal with incident perpendicular polarization of light. For 400 and 700 nm bead suspensions, two different dilutions were measured. For each polarization state (i.e., perpendicular and parallel) of incident light, we acquired 1440 measurements with a sampling frequency of 8 Hz over 3 min. For a given sample, this data acquisition protocol was repeated three times. Each of these three replications was made with a different randomly-chosen orientation of sample cylindrical vial within the instrument. The sample was gently mixed between these replicate measurements. The baseline measurements of 0.2 µm filtered water were acquired using the same protocol.
As mentioned above, the optical measurements were made on sufficiently-diluted samples to ensure negligible effects of multiple scattering over a pathlength used by a given instrument. A criterion for a single scattering regime is generally defined in terms of small optical thickness of the sample, τ << 1, where τ is a product of the beam attenuation coefficient, c, and pathlength, r [51,66]. Also, a simple practical test for ensuring that multiple scattering effects are negligible is to verify a direct proportionality between the measured optical signal and the concentration of particles in suspension by conducting a series of measurements on the same sample with different dilutions [51]. Our measurements on bead samples with different dilutions showed an excellent 1:1 relationship between the LISST-VSF measurement and the bead concentration over the range of beam attenuation coefficient up to at least 2 m −1 . The single scattering regime can also be determined by the condition τ(1-g) << 1, where g is the average cosine of the scattering angle of the volume scattering function [23,66]. For the 100 nm polystyrene beads, the g value is 0.115, which yields the most restrictive condition in our study, τ << 1.13. For all bead samples measured with LISST-VSF, including all bead sizes and sample dilutions, τ was always less than about 0.3. This condition was also satisfied for samples measured with a spectrophotometer. For the measurements with DAWN-EOS, the τ values were even smaller. For the natural seawater samples examined in our study (which is described below in Section 2.2), the g values (for the total volume scattering function including the contribution by pure seawater) were about 0.9 or somewhat higher, which yields less restrictive criterion τ << 10. Our measurements of natural samples clearly satisfied this single scattering condition, as the highest value of c for the natural samples measured with LISST-VSF was about 2.6 m −1 , so τ was always less than about 0.45, given that the maximum pathlength for LISST-VSF is 17.5 cm for the scattering angle of 150 • .

Data Processing
Processing of LISST-VSF data was done with a standard processing code provided by manufacturer (version of 2013) to determine β p (ψ), DoLP p (ψ), and c p , denoted hereafter as β LISST * p (ψ), DoLP LISST * p (ψ), and c LISST * p respectively (the asterisk indicates that the variable is derived from the standard processing code without additional corrections developed in this study). Some details specific to the processing and quality control of our experimental data are provided below.
As a first step in data processing, the baseline values in raw counts were subtracted from each LISST-VSF measurement of raw counts acquired on samples of bead suspensions. To account for light attenuation along the path between the scattering volume and the detector, an attenuation correction factor was calculated using the average c LISST * p from the series of measurements and the length of the path for each scattering angle. Further, to account for the difference in sensitivity of the two Roving Eyeball PMT detectors, a factor α is used to adjust the measured counts of one PMT detector relative to the other [67]. The value of α = 0.9335 was determined by averaging all median values of α derived from each series of measurements for each bead size, particle concentration, and PMT gain. The α parameter was observed to be nearly constant over the period of experiments (~18 months, the coefficient of variation < 5%). For each series of measurements a specific scaling factor was determined to convert p 11 (ψ) in PMT counts to β LISST * p (ψ) in absolute units [m −1 sr −1 ] for scattering angles 14-155 • measured by the Roving Eyeball sensor. First, for each measurement from a given series of measurements, a scaling factor was determined by matching the PMT counts measured with Roving Eyeball sensor between 15 • and 16 • with β LISST * p (ψ) in absolute units obtained from measurements with the last two ring detectors at 13.01 • and 15.17 • . Then, using these determinations, the average scaling factor for a given series of measurements was calculated and used for further data processing. Note that this scaling was not needed for the determination of DoLP LISST * p (ψ) for the Roving Eyeball angular range, which is calculated from p 11 (ψ) and p 12 (ψ) determined in PMT counts following Equation (2).
Quality control of data was performed by removing the first set of 20 measurements (the remaining four sets with 20 measurements each were retained) and the first 20 measurements from the set of 100 measurements. We observed that this was necessary to ensure reasonable stability in the measured scattering signal. The mean and standard deviation values for each angle based on all of the 160 remaining measurements in the series were determined, and the outlying single measurements within the series were identified and rejected from subsequent analysis. Typically, 120 to 130 measurements from a given series of 200 measurements passed the quality criteria.
Example data of uncorrected β LISST * p (ψ) for 200 nm and 2000 nm bead suspensions are shown in Figure 1. The series of measurements that remained after quality control and the median values of β LISST * p (ψ) derived from the series of measurements are shown. We also note that the median values were very close to mean values for our data (<1% difference for most scattering angles). The results for 2000 nm beads show a distinct pattern with several scattering maxima and minima due to constructive and destructive interference of the scattered light from a nearly monodisperse population of beads that are large relative to the wavelength of light. The 200 nm beads are smaller than the wavelength of light leading to a more featureless shape of β LISST * p (ψ). The variability between the individual measurements is largest at very small scattering angles, i.e., approximately <4 • , where the scattering signal for submicron particles is low relative to our baseline measurements. Apart from small scattering angles, the coefficient of variation (CV) for each scattering angle calculated from a series of measurements on 200 nm beads is generally very small, ranging from~3% to <1%, with the smallest values at angles greater than 64 • where full laser power is used. The measurements of 2000 nm beads exhibit somewhat higher CV, i.e., between about 3% and 6%. The higher values of CV are observed mostly near the angles where minima of β LISST * p (ψ) occur. The DAWN-EOS measurements for four bead sizes were also used to calculate β p (ψ) and DoLP p (ψ), denoted as β DAWN p (ψ) and DoLP DAWN p (ψ). First, for each time series of 1440 measurements with DAWN-EOS, the highest 2% of data was rejected, as these data are assumed to result from sample contamination with rare, larger particles. Each set of measurements then consists of 1411 measurements of both I s (ψ) and I s⊥ (ψ) for a specific orientation of sample vial. These measurements were averaged to represent that orientation. Such results were then averaged for three vial orientations. This protocol was applied to both the sample and baseline measurements, with the exception that baseline values were calculated by averaging the lowest 5% of data. The final I s (ψ) and I s⊥ (ψ) for the beads were calculated by subtracting the average baseline from the average sample data. These particulate I s (ψ) and I s⊥ (ψ) were then used to determine p 11 (ψ) and p 12 (ψ) according to Equations (3) and (4), from which β DAWN p (ψ) [61] and DoLP DAWN p (ψ) (Equation (2)) were determined. Note that two dilutions of the master suspension for 400 and 700 nm beads were measured with DAWN-EOS and the average of the two was used to represent these bead sizes. As a final step, the determined β DAWN p (ψ) values were rescaled using relevant dilution factors to obtain final results representing the particle concentration in LISST-VSF samples and enable direct comparisons with LISST-VSF measurements. Note that such rescaling is not necessary for DoLP DAWN p (ψ). With regard to processing of data acquired with a Lambda 18 spectrophotometer, the spectral data of measured optical density OD(λ) (i.e., measurements made in the absorbance mode of the spectrophotometer) were converted (after subtraction of baseline measurement) into the particulate beam attenuation coefficient [m −1 ] using the relationship c p (λ) = ln(10) OD(λ)/0.01, where ln is the natural logarithm and 0.01 is the path length in meters. The final particulate beam attenuation coefficient obtained from spectrophotometric measurements is denoted as c SPEC p . The estimates of c LISST * p from LISST-VSF measurements were calculated with the standard manufacturer's processing code. Because each LISST-VSF measurement consists of two linear polarization states of the incident beam, the average of these two is used as the final estimate of c LISST * p . As a final step, the determined c SPEC p values were multiplied by relevant dilution factors to obtain final results representing particle concentration in LISST-VSF samples and enable direct comparisons with LISST-VSF measurements.

Determination of Correction Functions
In addition to β LISST * p (ψ), Figure 1 shows results for the 200 nm and 2000 nm polystyrene beads based on Mie scattering calculations (more details about these calculations are provided below). These results are significantly higher (nearly a factor of 2) than the measured values of β LISST * p (ψ). We assume that the Mie scattering calculations for samples of spherical polystyrene beads are sufficiently accurate to provide reference values for such samples.
In order to correct for the mismatch between the measured and reference values, a calibration correction function CF(ψ) is defined as where β REF p (ψ) is a reference volume scattering function determined according to  (5) and (6) are for the LISST-VSF light wavelength of 532 nm.
For each examined suspension of standard polystyrene beads, β Mie p (ψ) was determined from Mie scattering computations for homogeneous spherical particles. We used the Mie scattering code for homogeneous spheres of Bohren and Huffman [20], which included our modifications to account for polydispersity of the sample, i.e., to use particle size distribution as input to the code rather than just a single particle diameter as in the original code. The computations were performed assuming a relative particle size distribution (PSD) of Gaussian shape, with 300 evenly spaced size bins about the nominal mean diameter ± 3 standard deviations, as provided by the manufacturer for each bead size ( Table 1). The use of such PSDs allows us to account for the realistic, small degree of polydispersity of each sample. The Mie computations also require input of the refractive index of particles. Based on the study of Ma et al. [68] we assumed that the complex refractive index of polystyrene relative to water at 532 nm is m = 1.193 + 0.0003i, where the first component is the real part and the second component is the imaginary part of refractive index. Note that the imaginary part is very small because polystyrene is a weakly absorbing material in the examined spectral region.
Equation (6)  By combining Equations (6) and (7), β REF p (ψ) can be determined for each LISST-VSF measurement as Note that the estimates of β REF p (ψ) can vary between individual measurements because of variations in c LISST * p . Finally, by combining Equations (5) and (8), CF(ψ) can be determined for each LISST-VSF measurement as The application of this protocol to every individual measurement of β LISST * p (ψ) helps to better capture the variability between individual measurements during a given series of LISST-VSF measurements on a given sample, for example due to imperfect mixing in the 2 L sample chamber or potential electronic fluctuations in the instrument. The smaller-sized particle standards (<500 nm in diameter) appear as the best candidates for determination of CF(ψ) because they produce a relatively featureless pattern of angular scattering (see the results for 200 nm beads in Figure 1). The measurements with larger beads (500 nm to 2000 nm) were not used in these determinations because the angular scattering pattern includes multiple maxima and minima (see the results for 2000 nm beads in Figure 1), which render the comparison of β LISST * p (ψ) and β REF p (ψ) particularly sensitive to even small uncertainties in measurements or theoretical calculations. The results obtained with beads of 100, 200, and 400 nm in diameter were considered in the determinations of final correction function CF f (ψ) within four angular ranges, as described below: The CF 200 (ψ) data obtained with 200 nm beads provide the main contribution to the determination of CF f (ψ). The CF 100 (ψ) data obtained with 100 nm beads are used partially because of increased uncertainty in the PSD of these beads (CV of nominal mean diameter is 7.8%, see Table 1). The CF 400 (ψ) data obtained with 400 nm beads are also used partially and cover the backscattering angles, where these particular data are useful for correction of an apparent artifact near 130-140 • , which is rather minor but has been consistently observed with our LISST-VSF instrument for various natural particle assemblages. The calculations of CF 100 (ψ), CF 200 (ψ), and CF 400 (ψ) were made using data for particle concentrations and PMT gains which ensured sufficient signal for the ring detectors while avoiding PMT saturation of the Roving Eyeball sensor (see dilution factors in italic font in Table 1). For a given bead standard, the final values of correction function at different angles were determined as the median values of all the relevant determinations.
The final CF f (ψ) was smoothed in the angular range 2.56-155 • with a 3-point and then a 5-point moving average. In addition, CF f (ψ) within the near-forward angular range 0.09-4.96 • was set to a constant value of CF f (ψ 32 ), where ψ 32 = 15.17 • corresponds to the last ring detector. The rationale for this assumption is that the scattering signal produced by the examined beads for the first 25 rings (ψ = 0.09-4.96 • ) is comparable to the baseline, while there is good signal relative to the baseline for the last ring detector.
The final correction simply involves the multiplication of uncorrected β LISST * p (ψ) by the correction function CF f (ψ), where β LISST p (ψ) is the corrected LISST-VSF measurement of volume scattering function (note that the superscript * is removed from this symbol).
We also determined a correction function for DoLP LISST * p (ψ), where BF(ψ) quantifies a correction for potential bias in DoLP LISST * p (ψ) obtained from the standard processing code applied to LISST-VSF measurements and DoLP REF p (ψ) is a reference degree of linear polarization determined from Mie scattering calculations of the two scattering matrix elements, p Mie 11 (ψ) and p Mie 12 (ψ), for a given sample of standard beads. The results for BF 100 (ψ), BF 200 (ψ), BF 400 (ψ), and the final correction function BF f (ψ) were obtained using a procedure similar to that for CF 100 (ψ), CF 200 (ψ), CF 400 (ψ), and CF f (ψ). The correction of DoLP LISST * p (ψ) simply requires a subtraction of BF f (ψ), where DoLP LISST p (ψ) is the corrected degree of linear polarization within the range of scattering angles from 16 • to 150 • . Because the DoLP LISST * p (ψ) data output from standard processing of LISST-VSF measurements begins at ψ = 16 • , no correction for the forward scattering angles of the ring detectors (ψ < 16 • ) was determined.

Measurements and Analysis of Natural Seawater Samples
Optical measurements with the LISST-VSF and ancillary analyses of natural particle assemblages were performed on seawater samples collected between summer 2016 and spring 2017 in contrasting marine environments, namely, in open ocean waters off the coast of Southern California, nearshore ocean waters at the pier of the Scripps Institution of Oceanography (SIO Pier) in La Jolla, and the tidal estuary of the San Diego River. Overall 17 samples representing a broad range of natural particle assemblages were analyzed. Most samples (number of samples N = 11) were collected at the SIO Pier. These samples were collected during typical dry weather conditions, phytoplankton bloom events, and after heavy rain. The tidal estuary samples (N = 3) include three tidal states between low and high tide. The offshore samples (N = 3) were collected in the Santa Barbara Channel, about 8 km off San Diego Bay, and about 2 km off SIO Pier. Seawater samples were collected just beneath the sea surface using either Niskin bottles or a bucket, except for one offshore sample (off San Diego Bay) that was collected at the subsurface chlorophyll-a maximum at a depth of 18 m. All samples were analyzed in the laboratory within 24 h of sampling.
To characterize the concentration and composition of particulate matter for each sample, we determined the dry mass concentration of total suspended particulate matter, SPM [g m −3 ], mass concentration of particulate organic carbon, POC [mg m −3 ], and mass concentration of the pigment chlorophyll-a, Chla [mg m −3 ]. For these determinations, the particles were collected on glass-fiber filters (GF/F Whatman) by filtration of appropriate volumes of seawater (150-2100 mL depending on the sample). SPM was determined following a gravimetric method using pre-washed and pre-weighted filters [7,70]. The determinations of POC were made on precombusted filters with a standard CHN analysis involving high temperature combustion of sample filters [7,71,72]. Chla was determined spectrophotometrically using a Lambda 18 spectrophotometer and placing 1-cm cuvettes containing acetone extracts of the samples inside the integrating sphere. The measured absorbance values at 630, 647, 665, and 691 nm (after subtraction of acetone baseline values) were used in the calculation of Chla [73]. For each seawater sample, replicate determinations of SPM and POC were made on separate sample filters. The final SPM and POC are average values of replicate determinations. The replicates for SPM and POC agreed generally to within 15% and 10%, respectively. No replicates were taken for Chla. In addition to information about particle concentration, SPM, POC, and Chla provide useful proxies of bulk composition of particulate matter. The organic and inorganic fractions of SPM can be characterized using the ratio POC/SPM, and the contribution of phytoplankton to SPM using Chla/SPM [65]. These ratios are expressed on a [g/g] basis.
The measurements of particle size distribution (PSD) were made with a Coulter Multisizer 3 (Beckman Coulter, Brea, CA, USA) equipped with a 100 µm aperture, which allows particle counting and sizing in the range of volume-equivalent spherical diameter from 2 µm to 60 µm. Within this size range we used 300 log-spaced size bins to provide high resolution PSDs. For each experiment, 0.2 µm filtered seawater was used as a blank that was subtracted from sample measurements. Approximately 10 to 15 replicate measurements of 2 mL subsamples of each seawater sample were collected. After removing outliers, the remaining measurements were summed and divided by the total analyzed volume to produce an average density function of PSD in particle number per unit volume per width of size bin. For each sample the power function fit with a slope parameter, ζ, was determined using these PSD data over the size range 2-50 µm. In these determinations, the linear regression analysis was applied to log-transformed data, and the last size bins with very low particle counts were ignored. Although the measured PSDs often showed significant deviations from the power function fits, we use the slope parameter ζ as a particle size metric, because this is the most common parameterization of size distribution of marine particles [23,74]. Additionally, assuming spherical particles, the particle volume distributions were determined from particle number distributions for each sample. From particle volume distributions, we calculated the percentile-based particle diameters such as the median diameter, D 50 V , and the 90 th percentile diameter, D 90 V . These parameters have been shown to provide potentially useful metrics in the analysis of relationships between the optical and particle size properties in seawater [65].
Measurements and processing of data collected with LISST-VSF for natural seawater samples were made following a protocol similar to that described above for standard polystyrene bead samples. For each experiment, baseline measurements were taken on 0.2 µm filtered seawater obtained from a given seawater sample. However, a single baseline selected from the lowest measured baselines was used for data processing of all seawater samples to ensure a consistent baseline unaffected by possible variations associated with the imperfect purity of 0.2 µm filtered seawater prepared during different experiments. To ensure scattering measurements were acquired in a single-scattering regime, samples with an average c p over 3.0 m −1 were diluted using 0.2 µm filtered seawater. Dilution was necessary only for the two most turbid samples collected in the San Diego River Estuary. Between four and eight sets of 50 measurements were collected for each seawater sample with gentle hand mixing between the measurement sets, while a magnetic stir bar was on very low speed changing direction of rotation every 30 s. All results from LISST-VSF measurements for natural seawater samples shown in this paper represent the CF f (ψ)-corrected volume scattering function of particles, β LISST To determine the particulate scattering, b LISST p , and particulate backscattering, b LISST bp , coefficients, the corrected measured β LISST p (ψ) was first extrapolated in the angular range 150-180 • . The extrapolated portion of β LISST p (ψ) was obtained by fitting a specific function to the data of β LISST p (ψ) in the angular range 90-150 • . We used two methods for fitting and extrapolating β LISST p (ψ). The first method is based on a non-linear least squares best fit of the analytical function proposed by Beardsley and Zaneveld [75]. The second method is based on a linear mixing model that finds a non-negative least squares best fit for combined contributions of four end members representing shapes of volume scattering functions associated with scattering by small and large particles, as described in Zhang et al. [76].
A backscattering factor, κ, was determined for the fitted volume scattering function as was also calculated. We note that the κ values for all examined seawater samples were found to range between 1.125 and 1.138 and 1.118-1.120 for the Beardsley and Zaneveld [75] and Zhang et al. [76] methods, respectively. An example illustration of fitting and extrapolation methods for one sample collected during high tide at the San Diego River estuary is depicted in Figure 3. As seen, both the Beardsley and Zaneveld [75] and Zhang et al. [76]

Correction Functions for LISST-VSF
The results for CF 100 (ψ), CF 200 (ψ), CF 400 (ψ), and CF f (ψ) are plotted in Figure 4. The final correction function CF f (ψ) indicates that β LISST * p (ψ) is lower than β REF p (ψ) by a factor of about 2, and also exhibits some angular variability. One consistent feature in the forward scattering region, which is independent of the bead size, is a sharp increase in CF f (ψ) with a peak at ring 26 (ψ = 5.84 • ). We observed a similar but inverse feature consistently in natural seawater samples, which suggests that the behavior of the correction function at these angles is credible. Within the angular range of data from the Roving Eyeball sensor (16-150 • ), the CF f (ψ) values remain generally in the range between 1.7 and 1.9. For angles larger than 150 • , we did not obtain consistent results of the correction function for different bead sizes (not shown), so this angular range is omitted from our analysis of LISST-VSF measurements. Note also that CF 400 (ψ) differs greatly from CF 100 (ψ) and CF 200 (ψ) within the angular range between about 65 • and 120 • . This can be attributed to the uncertainty in the determinations of CF 400 (ψ) associated with a well-pronounced minimum in the volume scattering function for the 400 nm beads in this angular range. Therefore, the CF 400 (ψ) data in this angular range were not used in the determination of final CF f (ψ). The results for BF 100 (ψ), BF 200 (ψ), BF 400 (ψ), and BF f (ψ), are shown in Figure 5. As seen, BF f (ψ) is negative within the examined angular range and varies within a relatively narrow range of values between about −0.02 and −0.04. Similar to the results for CF 400 (ψ), the distinct feature of positive bias observed in the BF 400 (ψ) data around the scattering angle of 80 • can be attributed to the uncertainty associated with a minimum in the volume scattering function for the 400 nm beads in this angular range. This portion of BF 400 (ψ) data was not used in the determination of final BF f (ψ).
The performance of the final correction function CF f (ψ) within the range of scattering angles from 0.09 • to 150 • was evaluated by comparing the corrected LISST-VSF measurements of volume scattering function, β LISST p (ψ), with reference values of β REF p (ψ) for six samples of polystyrene beads (100, 200, 400, 500, 700, and 2000 nm in diameter; see the dilution factors for these samples indicated in boldface in Table 1). The beads with diameters of 500, 700, and 2000 nm were not used in the generation of the final correction function, so they provide completely independent data for evaluating the performance of CF f (ψ). The evaluation with the data for 100, 200, and 400 nm beads is also useful because the final CF f (ψ) was determined by averaging the results obtained with multiple bead sizes and concentrations of these samples, and not from a single bead size and concentration. Results of independent measurements obtained with the DAWN-EOS on four bead suspensions (100, 200, 400, and 700 nm) are also included in the evaluation analysis for additional comparisons.  (Figure 6c). This issue has been mentioned above in the context of determinations of CF f (ψ) and BF f (ψ). The agreement observed between β LISST p (ψ) and β DAWN p (ψ) lends additional credence to the determined correction function CF f (ψ) and its application to LISST-VSF measurements. Figure 7a illustrates the relationship between β LISST p (ψ) measured at all angles between 3.02 • and 150 • and β REF p (ψ) for the corresponding angles for the six bead samples. The overall agreement is quite good over a range spanning nearly 4 orders of magnitude. The regions of largest disagreement correspond to angles measured with the ring detectors, as well as angles corresponding to sharp minima or maxima in volume scattering function which are observed for the larger beads. Although the measured minima and maxima occur essentially at the same angles as predicted by Mie scattering calculations, the measured magnitude of minima or maxima can differ by a few tens of percent from the reference values. This is illustrated by plots of percent differences between the measured and reference values (Figure 7b). The oscillations and peaks (both positive and negative) in percent differences correspond to the minima and maxima in the angular patterns of volume scattering function.  Table 2 includes several statistical parameters that quantify the agreement between the data of Figure 7a. In this analysis we ignore ψ < 3.02 • due to generally low scattering signal relative to baseline for these ring detectors. The values of statistical parameters support the overall good agreement; for example, the median ratio (MR) of β LISST p (ψ) to β REF p (ψ) is very close to 1, and the median absolute percent difference (MAPD) between β LISST p (ψ) and β REF p (ψ) is only~4%. These median values indicate no overall bias in the corrected measurements of β LISST p (ψ) relative to the reference values of β REF p (ψ) and small statistical differences between β LISST p (ψ) and Table 2 also includes the statistical parameters for a subset of data presented in Figure 7a. In this subset, the forward scattering measurements with ring detectors were excluded, so the angular range is 16-150 • . The statistical parameters for this subset are generally improved compared with the dataset covering the angular range 3.02-150 • . For example, the root mean square difference (RMSD) is smaller (0.015 m −1 sr −1 vs. 0.21 m −1 sr −1 ) and the slope of linear regression is closer to 1 (0.958 vs. 0.723). The improvements in the statistical parameters after removing the ring detector data are related primarily to much larger values of volume scattering function at forward scattering angles compared with larger angles, and a tendency to negative bias in β LISST p (ψ) relative to β REF p (ψ) at forward angles. To further validate the correction of LISST-VSF measurements with the CF f (ψ) function, we performed comparisons for approximate scattering and backscattering coefficients, b p,150 and b bp,150 , respectively. The approximate scattering coefficient b p,150 was obtained by integrating the volume scattering function within the angular range from 0.09 • to 150 • . The approximate backscattering coefficient b bp,150 was obtained by the integration from 90 • to 150 • . These calculations were made for the uncorrected measured β LISST * p (ψ), CF f -corrected measured β LISST p (ψ), and reference β REF p (ψ). We also used Mie scattering calculations to estimate the underestimation of the scattering and backscattering coefficients for the examined polystyrene beads caused by the integration of β REF p (ψ) up to 150 • as opposed to 180 • . We found that the approximate scattering coefficient, b REF p,150 , can be lower by as much as 7% compared with the "true" scattering coefficient b REF p . This result was observed for 100 nm beads. For backscattering the approximate coefficient b REF bp,150 was found to be lower by as much as 24% for the 500 nm beads. Although the LISST-VSF measurements extend to 150 • rather than 180 • , the approximate coefficients are still useful for our validation exercise because most of the angular range and magnitude of total scattering and backscattering coefficients are included in the integration up to 150 • . In addition, this validation analysis includes all 20 experiments conducted in this study, and not just the six example experiments presented in Figures 6 and 7.  Table 2. , the results are shown for the angular range 3.02-150 • which includes the ring data and for the range 16-150 • without the ring data. R is the Pearson correlation coefficient and the coefficients A and B are the slope and y-intercept, respectively, determined from a type II linear regression between individual pairs of X i and Y i values where Y i represents measured values and X i reference values. The mean bias (MB) was calculated as 1/N × ∑ N i=1 (Y i −X i ) and MR represents the median ratio of Y i /X i . The root mean squared deviation, RMSD, was calculated as    Figure 11 depicts the corrected measured volume scattering function, β LISST p (ψ), and the degree of linear polarization, DoLP LISST p (ψ), for three contrasting natural assemblages of particles. The selected parameters describing the particulate and optical properties of these samples are provided in Table 3. Sample A was obtained~8 km offshore from the subsurface chlorophyll-a maximum at a depth of 18 m, sample B was collected just beneath the sea surface at SIO Pier during a calm sunny summer day, and sample C was collected~2 km inland at the San Diego River Estuary during low tide. The SPM range covers about one order of magnitude from 0.36 g m −3 for sample A to 3.18 g m −3 for sample C, which is reflected in significant range of the particulate scattering coefficient, b LISST p , from 0.36 m −1 to 2.23 m −1 . Chla was also lowest for sample A (0.75 mg m −3 ) but highest for sample B (2.5 mg m −3 ). Thus, whereas the offshore sample A represents a particle concentration that is within the range of observations in relatively clear open ocean waters, sample C is representative of more turbid coastal or nearshore waters [5,7]. Samples A and B have similarly high values of the ratio POC/SPM (0.43 and 0.47, respectively) and relatively high values of Chla/SPM (2.1 × 10 −3 and 2.2 × 10 −3 , respectively), indicating organic-dominated particulate assemblages with significant contribution of phytoplankton. In contrast, sample C has much lower values of POC/SPM (0.14) and Chla/SPM (3.8 × 10 −4 ), indicating inorganic-dominated particulate assemblage and relatively small role of phytoplankton, despite significant chlorophyll-a concentration (1.21 mg m −3 ).

Measured Light Scattering Properties of Natural Particulate Assemblages
These differences in particle properties between the three samples are responsible for the differences in the magnitude and angular shape of β LISST p (ψ) and DoLP LISST p (ψ) presented in Figure 11 and the optical parameters listed in Table 3. These optical parameters include the particulate backscattering ratio, b LISST bp , the ratio of β LISST p (45 • ) to β LISST p (135 • ), and the maximum value of DoLP LISST p (ψ) denoted as DoLP LISST p,max . This maximum value occurs at a scattering angle ψ max which is also provided in Table 3. The offshore sample A has an intermediate value of b LISST bp and the highest DoLP LISST p,max of about 0.77 associated with the smallest ψ max of 92 • . Sample B from the SIO Pier has the lowest b LISST bp of 0.008 among the three samples, suggesting a relatively steep slope of particle size distribution, relatively low bulk particle refractive index, or both [17]. This sample also shows the least steep near-forward scattering pattern (Figure 11c), which suggests a higher proportion of small particles relative to larger particles compared with the two other samples. Finally, the most turbid and least organic sample, sample C, exhibits an enhanced proportion of backscattering with the highest b LISST bp of 0.027. While this result may suggest a relatively high bulk particle refractive index [17] consistent with the lowest POC/SPM ratio among the three samples, the additional influence of particle size distribution cannot be ruled out. Sample C shows steep near-forward scattering pattern (Figure 11c), which is typically indicative of an increased proportion of large particles relative to small particles. Note that sample C also has the lowest β LISST  Table 3. General information on particle characteristics and median values of optical quantities derived from LISST-VSF measurements for the three example natural seawater samples depicted in Figure 11. Values of selected optical quantities estimated from the measurements of Petzold [38]  For comparison, Table 3 also includes the values for the selected optical parameters estimated from measurements reported by Petzold [38] for clear ocean waters (off Bahamas), coastal waters (San Diego coastal region), and turbid waters (San Diego Harbor). These measurements span a generally similar range of scattering angles as the LISST-VSF (10-180 • in 5 • increments), but are based on a spectrally broader incident beam (75 nm full width half maximum) centered at 514 nm. The estimates of particulate volume scattering function β p from Petzold's measurements were obtained by subtracting pure seawater contribution β w from the measured total β. The β w value was calculated assuming a water temperature of 15 • C and salinity of 33 PSU [77]. Although Petzold's data include measurements made in clearer waters compared with our samples, the range of values for the dimensionless parameters associated with the shape of angular scattering pattern, b LISST bp and β LISST p (45 • )/β LISST p (135 • ), is very similar. Specifically, our data for the offshore sample A are similar to Petzold's data from clear waters, sample B from the SIO Pier aligns with Petzold's data from coastal San Diego waters, and sample C from San Diego River Estuary with Petzold's data from the San Diego Harbor.
We note that the dotted lines in Figure 11 reflect some variations in β LISST p (ψ) and DoLP LISST p (ψ) between the individual measurements within a given set of measurements for each sample. For example, on the basis of the collection of 200 to 400 measurements for each of the two linear polarization states of the incident beam and the scattered light, the coefficient of variation at ψ = 90 • was 14%, 8%, and 13% for β LISST p and 20%, 13%, and 15% for DoLP LISST p for samples A, B, and C, respectively. These variations between the individual measurements that have been taken in rapid succession do not necessarily reflect the measurement precision, as they can also be associated with actual variations in the sample, for example the fluctuations in the presence of relatively rare large particles within the interrogated sample volume. Another important point is that the small negative values of DoLP LISST p observed for some individual measurements at forward scattering angles <30 • (see the 10th percentile dotted lines in Figure 11b,d,f) are not necessarily an indication of measurement uncertainty because the negative values, especially in this angular range, are physically possible for certain types of particles [30,54,56,58]. Figure 12 depicts scatter plots of the relationships between the dimensionless optical parameters, b LISST bp and DoLP LISST p,max , and the dimensionless particulate compositional properties, POC/SPM and Chla/SPM, for all 17 samples examined in this study. The overall range of POC/SPM in our dataset is 0.04 to 0.6. The presented data have been divided into three groups according to the values of POC/SPM as follows: the least organic-dominated (or the most mineral-dominated) data with POC/SPM < 0.15; the most organic-dominated data with POC/SPM > 0.3, and the intermediate data with 0.15 ≤ POC/SPM ≤ 0.3. The selected boundary values of POC/SPM for discriminating between the organic-dominated and mineral-dominated groups of data differ from those used in our previous studies [65,78], but appear to adequately reflect the patterns in the present data. In particular, the most mineral-dominated samples with POC/SPM < 0.15 form a clear cluster of data points with the highest b LISST bp (Figure 12a) and the lowest Chla/SPM (Figure 12b,d). We also note that no data were collected for POC/SPM between 0.15 and 0.2, so we will refer to all data with POC/SPM > 0.2 as highly organic because they all represent highly significant or dominant role of organic particles. . This result is consistent with the notion that mineral-dominated particulate assemblages with relatively high bulk refractive index of particles tend to have higher backscattering ratio b bp compared with organic-dominated assemblages with lower refractive index [17]. However, we also note that highly organic samples with POC/SPM > 0. and Chla/SPM for all data is strong (R = −0.85), the subset of data for highly organic samples (POC/SPM > 0.2) has also a relatively high correlation coefficient of −0.51. This is an important result, suggesting that for particulate assemblages with high organic content, the backscattering ratio b bp tends to decrease with increasing proportion of phytoplankton in the particulate assemblage. It is likely that the relationship in Figure 12b is largely driven by a decrease in the bulk particle refractive index with increasing proportion of phytoplankton in the particulate assemblage. Because this trend also holds for the subset of highly organic samples, it may indicate that live phytoplankton cells have generally lower refractive index than non-living organic particles.
In contrast to b LISST bp , the DoLP LISST p,max data show no clear relational trend and very weak correlation with POC/SPM (R = 0.31), indicating that the maximum degree of linear polarization does not provide a useful optical signature for the organic vs. inorganic content of particulate assemblages in our dataset (Figure 12c). A similar result with no correlation (R = 0.07) is observed for DoLP LISST p,max vs. Chla/SPM, indicating that varying proportion of phytoplankton in total particulate assemblage has no discernible systematic effect on the maximum degree of linear polarization (Figure 12d). We also determined that there is no significant correlation between DoLP LISST p,max and b LISST bp in our dataset (R = −0.22), as well as between ψ max and POC/SPM or Chla/SPM (R = −0.09 and 0.06, respectively). It is also of interest to note that the range of our DoLP LISST p,max data is generally consistent with the range of values reported in literature for natural seawater samples, although the reported range in some earlier studies extends to somewhat lower values, as low as about 0.4 [15,[39][40][41][42]79,80].
The assessment of potential presence of systematic effects of particle size distribution (PSD) on b LISST bp and DoLP LISST p,max is presented in Figure 13. In this assessment, we use two PSD metrics: the 90 th percentile diameter, D 90 V , derived from the particle volume distribution, and the power function slope, ζ, derived from the particle number distribution. We also tested other percentile-based diameters such as the median D 50 V but no improvements in the examined relationships were observed. Figure 13a,b shows no trend in the data of b LISST bp associated with variations in the particle size metrics, even though these metrics vary over a significant dynamic range. This is the case for the entire dataset as well as a subset of highly organic samples with POC/SPM > 0.2, which supports the interpretation of results presented in Figure 12b in terms of the role of refractive index. The data of DoLP LISST p,max vs. D 90

V
show the potential for the presence of a relational trend (Figure 13c). Although the scatter in these data points is significant and correlation is weak (R = −0.47), the lowest values of DoLP LISST p,max tend to occur along with the highest values of D 90 V . This result indicates that the decrease in the maximum degree of linear polarization tends to be associated with particulate assemblages exhibiting a higher proportion of large-sized particles. The potential usefulness of the relationship between the degree of linear polarization and particle size has been proposed for the first time in 1930 [81], and the trend observed in our data is consistent with those early results.

Concluding Remarks
Our laboratory measurements combined with Mie scattering calculations for samples of standard polystyrene beads illustrate the value of such an approach for evaluating the calibration and performance of light scattering instruments. For the specific version of LISST-VSF instrument and data processing code used in our study, we determined the calibration correction functions for improved determinations of the particulate volume scattering function β p (ψ) and the degree of linear polarization DoLP p (ψ). The required correction was found to be particularly significant for β p (ψ) (a correction factor of~1.7 to 1.9). The improved determinations of β p (ψ) and DoLP p (ψ) were validated with measurements on independent samples, and also using another independently-calibrated light scattering instrument, DAWN-EOS. Although the correction functions developed in this study are applicable only to the specific version of LISST-VSF instrument and the data processing code used in this study, our results emphasize a general need for evaluating the performance of light scattering instruments and minimizing the associated uncertainties in quantitative determinations from measurements.  Figure 12, but with optical quantities shown as a function of the particle size metrics (a,c) D 90 V , representing the diameter corresponding to the 90 th percentile of the particle volume distribution, and (b,d) ζ, the power law slope of the particle number distribution.
The improved protocol for measurements of light scattering with our LISST-VSF instrument was applied to measurements taken on 17 natural seawater samples from coastal and offshore marine environments characterized by contrasting assemblages of suspended particles. The particulate volume scattering function, degree of linear polarization, and backscattering ratio were determined from LISST-VSF measurements. For our dataset, these light scattering properties exhibit significant variations related to a broad range of measured particle properties characterizing the organic vs. inorganic composition and size distribution of particulate assemblages. For example, we observed negative relational trends between the particulate backscattering ratio and the increasing proportions of organic particles or phytoplankton in the total particulate assemblage. These proportions were parameterized in terms of the measured ratio of particulate organic carbon (POC) or chlorophyll-a (Chla) concentration to the total dry mass concentration of suspended particulate matter (SPM). The observed trends can be useful in the development of optical approaches for characterizing the composition of particulate assemblages. Our results also suggest a potential trend between the maximum degree of linear polarization of light scattered by particles and particle size metrics. Specifically, the decrease in the maximum degree of linear polarization observed at scattering angles close to 90 o tends to be associated with particulate assemblages exhibiting a higher proportion of large-sized particles.
Earlier theoretical studies have shown that changes in the angular shape and the maximum value of the degree of linear polarization depend on particle refractive index and size distribution [82,83]; however, the experimental data of the degree of linear polarization of scattered light for natural marine particle assemblages are very scarce. Our results provide a contribution to filling this gap. This type of data can also be useful for improving an understanding of the polarization properties of marine light fields including polarization of water-leaving radiance and advancing related applications, including remote sensing applications [84][85][86][87][88][89][90]. The various potential applications of angular light scattering measurements, including the polarization effects associated with light scattering by marine particles, call for further efforts in this research area.
Author Contributions: All authors made intellectual contributions to the study design and participated in the collection of experimental data. D.K. and R.A.R. processed the data and conducted Mie scattering calculations, and D.K. analyzed the results. D.K. and D.S. wrote the paper, and all authors reviewed and provided final edits in the manuscript.