Suspended sediment is one of most important parameters for water quality.
水体中悬浮泥沙的含量是最重要的水质参数之一。
The spring tide suspended sediment concentration is bigger than that of the neap tide.
大潮悬沙浓度大于小潮悬沙浓度。
The impact on water environment of the suspended sediment should be received more attention.
三峡库区含沙量大，泥沙对水环境的影响不容忽视。
Temporally, the suspended sediment concentrations show a neap-spring tidal cycle and seasonal fluctuations.
悬沙浓度在时间上呈现明显的大小潮周期和季节性变化。
A numerical model for simulating unsteady flow and suspended sediment transport in river networks was presented.
所有单一河流断面处的含沙量通过单一河流悬沙输运的求解方法获得。
Water spills out of the Gulf of Mexico where their suspended sediment is deposited to form the Mississippi River Delta
从墨西哥湾冲出的水流携带的悬浮式泥沙沉淀到了密西西比河三角洲中。
The channel sedimentation comes from three parts, i. e. the suspended sediment, high sediment layer, and bed load.
航道淤积由三部分构成：悬沙、推移质和底部高浓度含沙层。
Study the law and mechanism of the variations in SSC are the important parts of the dynamics of suspended sediment.
悬沙浓度变化的规律和机制是悬沙运动研究的重要组成部分。
Then, with the consideration of wind force, a storm runoff suspended sediment model in lake and reservoirs is built.
对滇池湖泊某次暴雨过程的悬移质泥沙进行了模拟计算，得到了该次暴雨径流的泥沙淤积等值线分布图。
For rivers with lower concentration of suspended sediment, effect of concentration on settling velocity is inapparent.
对于含沙浓度较低的河流，浓度对沉速的影响不显著。
Observing of Suspended Sediment Concentration is vital for management of coastal environments in coastal zone and estuaries.
水体悬浮泥沙浓度监测在海岸带环境管理中有重要的意义。
Many theories have been developed to approach the vertical profiles of suspended sediment concentration in sediment-laden flows.
近年来用于研究含沙水流中悬浮颗粒垂向浓度分布的理论已有很多。
According to ADCP data and suspended sediment concentration, suspended sediment movement in the Yangtze River Estuary is studied.
采用ADCP实测水流资料与悬沙含量实测资料相结合的方法，对长江口悬沙运动进行分析。
Variations of estuary width and slope would change the circulation structure and distributions of salinity and suspended sediment.
河口宽度与坡度的变化会改变环流结构和盐度、悬沙分布；
The application to Taiping waterway shows that the proposed model can reasonably simulate the tidal current and suspended sediment transport.
并且在模型中嵌入悬移质输运模块，从而建立了一个针对太平水道的水流泥沙数学模型。
Based on measured data of water flow obtained from ADCP and of suspended sediment, suspended sediment movement in the Yangtze River Estuary is studied.
采用ADCP实测水流资料与悬沙含量实测资料相结合的方法，对长江口悬沙运动进行分析。
The method of fractional steps is used to split vertical 2-D suspended sediment transport equation. Then two different computation schemes are presented.
利用空间概念上的分步法，对剖面二维悬移质泥沙输移方程，提出两种不同的计算格式。
The conclusion can benefit the coming research on nutrients release from sediment and suspended sediment concentration (SSC) response to the surface disturbance.
该结论能为计算太湖水体悬浮物浓度和动态内源释放提供重要的参考依据。
The key to the problem of probing the concentration of suspended sediment in water and its variation with acoustic equipment is how to calibrate the obtained data.
用声学设备探测水体中悬浮泥沙浓度及其变化的关键问题是对观测数据进行标定。
Based on the data from Datong gauging station of Yangtze River, the grain-size characteristics of suspended sediment has been studied by using regression analysis.
以大通站为例，用回归分析的方法研究了长江入海悬移质泥沙的粒度特征。
Computation shows that the "tidal pumping" effect has a significant role in the suspended sediment transport within the turbidity maximum of the Changjiang Estuary.
计算表明，潮泵效应在长江河口最大浑浊带悬沙输移中起着重要的作用。
The method of mechanism analyses and equal_area grids were used in this paper to calculate the suspended sediment flux in the typical cross sections in the study area.
本文运用目前较为成熟和可靠的机制分解法和等面积时变网格法分别对口外海滨地区典型断面的悬沙通量进行了估算，两种方法计算得到的通量结果方向一致，量级相同。
The suspended sediment concentration at the center of the turbidity maximum zone and near the sand bar tends to increase because of the sediment addition from upstream.
因上游来沙量增加，在最大浑浊带中心和河口拦门沙处悬浮泥沙浓度趋于增加。
Finally, the model is verified by the examples of analytical solution, the results show that the model can be applied in the suspended sediment model of estuary and coastal.
最后采用有解析解的算例进行了验证，结果表明该模型可以用于海岸河口的悬沙输移模拟。
Based on monitoring the sequence of suspended sediment concentration during the flood season, the configuration of the back flows of water from Yangtze River can be observed.
基于对汛期鄱阳湖悬浮泥沙浓度的连续监测，可对长江倒灌入鄱阳湖现象的形态进行观测。
Based on monitoring the sequence of suspended sediment concentration during the flood season, the configuration of the back flows of water from Yangtze River can be observed.
基于对汛期鄱阳湖悬浮泥沙浓度的连续监测，可对长江倒灌入鄱阳湖现象的形态进行观测。
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