fine-sediment load 细悬移质
bed sediment load 沉积底沙
sediment load distribution 泥沙分布
suspended sediment load 悬移质 ; 悬移质泥沙
river sediment load 河流输沙量
snow sediment load 融雪输沙量
flow sediment load 水流含沙量
The CaCO3 content has no distinct change trend vertically,ranging from 2.3% ~ 3.3%, with average 2.7 % in sediment core 0306,changed with the runoff amount and sediment load of Huang River.
3、南黄海0306柱状样碳酸钙含量介于2.3% ~ 3.3%之间,平均含量2.7%,在垂向分布上变化趋势不明显,与黄河多年径流量和输沙量变化有关。
参考来源 - 黄、东海泥质区沉积物部分金属元素赋存形态研究·2,447,543篇论文数据，部分数据来源于NoteExpress
The variations of runoff and sediment load of the basin are caused mainly by human activities.
流域内水沙变化主要是人类活动引起。
The released flow from reservoirs carries less sediment load of bed material than pre? dam periods.
建坝后水库下泄水流挟带的床沙质含沙量减少，坝下游河床出现冲刷。
According to the spectrum analysis, the sediment load also fluctuated at the periodicity of 3a and 10a.
根据功率谱分析，入海泥沙还存在着3年和10年左右的周期性波动。
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