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Turbidimetric Measuring of the Suspended Sediment Concentration in the Coastal Zone

机译:海岸带悬浮泥沙浓度的浊度法测量

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The construction peculiarities of the new model of turbidimeter for measurement of instantaneous values of suspended sediment concentration are described in this paper. The presence of optic negative feed back is the basic feature of this turbidimeter, which allows to eliminate practically completely the temperature instability of light source and of its electronic units. A new model of turbidimeter has given a possibillity to create a three-dimensional lattice for the investigations of suspended particle spatial shift. One turbidimeter of the lattice cell is recording continuously the background transparency of examined liquid in a real scale. It gives possibility of continuous controlling not only of the light radiation flux attenuation by suspended particles but and of a ratio between the light flux absorption in researched water column with suspended particles and the light flux absorption in "clean" water. Durign the field experiments with the help of turbidimeters new data about physical mechanisms of sediment suspension above a smooth and rippled bottom were received.
机译:本文介绍了浊度计新模型用于测量悬浮泥沙浓度瞬时值的特点。光学负反馈的存在是该浊度仪的基本特征,它实际上可以完全消除光源及其电子单元的温度不稳定性。一种新的浊度计模型已经可以创建一个三维晶格,用于研究悬浮粒子的空间位移。晶格单元的一个浊度计以真实比例连续记录所检查液体的背景透明性。它不仅可以连续控制悬浮颗粒对光通量的衰减,而且还可以连续控制所研究的带有悬浮颗粒的水柱中的光通量吸收与“清洁”水中的光通量吸收率之间的比率。在浊度计的帮助下进行了Durign现场实验,获得了有关光滑且波纹状底部上方的泥沙悬浮物物理机理的新数据。

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