沉淀
河口
沉积作用
地质学
圆柱
切萨皮克湾
材料科学
矿物学
沉积物
地貌学
环境科学
海洋学
几何学
数学
环境工程
标识
DOI:10.1029/jc090ic02p03249
摘要
The size and settling velocity of flocs of suspended sediments from the Chesapeake Bay were measured in laboratory experiments and in the field. The curves between floc diameter and settling velocity showed a non‐Stoke's relationship that was best described by the following: settling velocity (cm/s) = 1.73 (floc diameter, cm)0.78. Furthermore, the relationship between floc diameter and settling velocity indicated that the floe density decreased as the floes increased in size. In addition to changing density, a cylinder shape was found to be the best shape factor.
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