Shi Kun, Li Yun-mei, Lü Heng, Sun De-yong, Huang Chang-chun, Wang Yan-fei, Jin Xin
Key Laboratory of Virtual Geographic Environment Ministry of Education, Nanjing Normal University, Nanjing 210046, China.
Huan Jing Ke Xue. 2010 Mar;31(3):598-605.
To acquire the depth profile of suspended particle scattering coefficient and the mechanism of surface reflection, three different depths of Taihu Lake scattering coefficient and backscattering coefficient are obtained in Nov. 2008, respectively. And their characteristic variation with depth is studied. Profiling distribution of the slope of particulate size distribution (PSD) is computed by the attenuation coefficient. Profiling distribution of the concentration and composition of suspended particle is computed according the relationship between the scattering coefficient and the suspended particle concentration. Impact dominant factors on scattering coefficient of the depth of water are divided according to the range of refractive index. At the three depths (0, 50, 100 cm), the particle scattering, with the percentage 14%, 17%, 12% of the samples are dominated by algae, respectively. 35%, 30%, 34% of the samples are dominated by inorganic particulate matter and Non-algal organic particulate matter,and 51%, 53%, 51% of the samples are dominated by the above all. The results can be concluded as: scattering and backscattering coefficient of Taihu Lake water body changes with depth slightly. The concentration of total suspended particles is of more diversity in different lake area, but there is less difference at different depths except those samples near the inflow rivers. The main factors of scattering coefficient of most aquatic scattering in Taihu Lake had little difference at different depths, except several samples beside the inflow rivers.
为获取悬浮颗粒散射系数的深度剖面及表面反射机制,分别于2008年11月获取了太湖三个不同深度的散射系数和后向散射系数,并研究了它们随深度的特征变化。通过衰减系数计算颗粒粒径分布(PSD)斜率的剖面分布,根据散射系数与悬浮颗粒浓度的关系计算悬浮颗粒浓度和组成的剖面分布。根据折射率范围划分了影响水体深度散射系数的主导因素。在三个深度(0、50、100厘米)处,颗粒散射中分别有14%、17%、12%的样本以藻类为主;35%、30%、34%的样本以无机颗粒物和非藻类有机颗粒物为主;51%、53%、51%的样本以上述所有为主。结果表明:太湖水体的散射和后向散射系数随深度变化较小。不同湖区总悬浮颗粒浓度差异较大,但除入流河流附近的样本外,不同深度差异较小。太湖大多数水体散射系数的主要影响因素在不同深度差异不大,除了入流河流旁的几个样本。