首页> 外文期刊>Journal of the Korean Fisheries Society >In situ Particle Size and Volume Concentration of Suspended Sediment in Seomjin River Estuary, Determined by an Optical Instrument, 'LISST-100'
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In situ Particle Size and Volume Concentration of Suspended Sediment in Seomjin River Estuary, Determined by an Optical Instrument, 'LISST-100'

机译:用光学仪器“ LISST-100”测定的西金河河口悬浮泥沙原位粒径和体积浓度

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摘要

In situ particle size and volume concentration of suspended sediment was measured at the mouth of Seomjin River Estuary in February 2001, using an optical instrument, 'LISST-100'. Time variation of in situ particle size and concentration shows: (1) during ebb tide, Seomjin River supplies relatively fine-grained particles with less-fluctuated, compared to during flood tide, and well-behaved concentrations following the tidal cycle; and (2) during flood tide, relatively coarse-grained particles with highly variable in size distribution and concentration flow upstream from Kwangyang Bay. This explains a poor correlation (r"=0.10) between sediment concentration and beam attenuation coefficient during flood and a high degree of correlation (r2=0.80) during ebb tide. Relatively fine grained and well defined, monotonous size distribution may promote the correlation between concentration and beam attenuation coefficient due to optical homogeneity of particles during ebb tide. Abundance of large aggregateswith time-varying size and shape distributions may be mainly responsible for variations in optical properties of the sediment during flood tide, and thus may confound the relationship between the two variables. The difference in particle sizes and shapesbetween flood and ebb tides can also be observed on SEM images.
机译:使用“ LISST-100”光学仪器,于2001年2月在西金河河口测量了悬浮颗粒的原位粒径和体积浓度。原位颗粒大小和浓度的时间变化显示:(1)在退潮期间,与洪水期间相比,首金河提供的颗粒相对细小,波动较小,并且在潮汐周期后浓度表现良好; (2)在洪潮期间,粒度分布和浓度变化较大的相对粗粒颗粒在光阳湾上游流动。这解释了洪水期间泥沙浓度与射束衰减系数之间的相关性较弱(r“ = 0.10),而在退潮期间则具有较高的相关度(r2 = 0.80)。相对细密且定义明确的单调尺寸分布可能会促进两者之间的相关性。退潮过程中颗粒的光学均匀性导致了浓度和光束衰减系数的增大,大量聚集体随时间的变化和形状分布的变化可能是造成洪流过程中沉积物光学特性变化的主要原因,因此可能混淆了两者之间的关系。两个变量,潮汐和退潮之间的颗粒大小和形状的差异也可以在SEM图像上观察到。

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