Effect of a Polydisperse Hydrosol on the Spectral Properties of Light Scattering by Seawater at Forfard Angles

E. B. Shybanov, M. E. Lee
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Abstract

In this paper we discuss the problem how to analyze the results of spectral volume scattering function measurements in natural waters and artificial ones. Analytical predictions and experimental proves of the remarkable changes in the properties of the light scattering at small angles after a filtration of water sample are presented. It was proposed that a certain correlations in the positions of scattering centers always exist in the water which were resulted in the volume scattering function of any natural water was strong forward peaked. Based on Mie theory the sums of scattering amplitudes and scattering radiances were calculated for a power-law particle size distribution while the maximal radius was varied. The square of the sum of the scattering amplitudes was compared with the value of the classical term. It is shown that in the “blue” a significant compensation of the effect of spatial correlation of particles occurs with an increasing of the maximum radius of particles, starting from the radius is about 0.2 μm. The contribution of the additional term decreases faster at general angles region. The spectral properties of light scattering by seawater during sequential filtration through nucleopore filters with a pore diameter of 2, 1, and 0.45 μm have been measured. The volume scattering function data at scattering angles from 6 to 90 degrees were analyzed. Water samples were taken from the surface of the Black Sea at the beginning of October. The Secchi depths are varied from 16 up to 19m. It was found that after filtration through a filter with pores diameter equaled to 1 μm, the typical deep at 30° of spectral slope of volume scattering function was appeared. Such deep becomes stronger after the next stage of filtration, when diameter of pores was equal to 0.45 µm. It is shown that the angular dependence of the exponent of the spectral slope obtained as a result of processing the experimental data is in consistent with theoretical predictions.
多分散纯溶胶对海水前角光散射光谱特性的影响
本文讨论了自然水体和人工水体中光谱体积散射函数测量结果的分析问题。对水样过滤后小角度光散射特性的显著变化进行了分析预测和实验证明。提出了水体中散射中心位置存在一定的相关性,这就导致了任何天然水体的体积散射函数都是强正向峰值。基于Mie理论,计算了变化最大半径时粒子粒径呈幂律分布时散射振幅和散射辐射的和。将散射振幅和的平方与经典项的值进行了比较。结果表明,在“蓝色”区域,粒子的最大半径从0.2 μm左右开始,随着最大半径的增大,粒子空间相关效应得到了显著的补偿。在一般角度区域,附加项的贡献减小得更快。测量了孔径分别为2、1和0.45 μm的核孔滤光片在海水中顺序过滤时光散射的光谱特性。对散射角为6 ~ 90°的体散射函数数据进行了分析。十月初从黑海表面采集了水样。塞奇的深度从16米到19米不等。通过孔径为1 μm的滤光片过滤后,出现了体积散射函数光谱斜率为30°的典型深度。当孔直径为0.45µm时,下一阶段过滤后,这种深度变得更强。结果表明,对实验数据进行处理得到的光谱斜率指数的角依赖性与理论预测是一致的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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