大部分的土壤在径流高峰期仍然是冻结的。
Much of the soil is usually still frozen during peak run-off.
同时，还将保证新的建筑达到径流管理规定。
地表径流对水质的酸化有缓冲作用。
The runoff has the catabatic effect to acidification of water quality.
其次，建立地面径流水动力模型。
The model simulates storm water process over ground, which initially is dry.
第四部分，径流年际变化分析。
径流是区域水土流失的基础。
Runoff is an essential factor for regional soil and water loss.
点击这里重置即时径流表。
河川径流是一种复杂的非线性时间序列。
Stream flows are sorts of complicated nonlinear time series.
因为不产生径流，所以没有冲刷侵蚀问题。
气象变化与径流变化存在较好的对应关系。
There is a good relationship between variation of weather and runoff.
年平均径流量与汛期径流量均呈沿程递减。
Annual average runoff amount and runoff amount of flood season decreased along the river.
如果大多数选择是在最后的径流，它将获胜。
河道径流是流域水资源中最重要的组成部分。
径流量的变化主要取决于流域降水量的变化。
The Surface Runoff change main depends on precipitation change.
降雨和径流为三亚湾海域水质参数变化的控制因子。
The major control factor of water quality is precipitation and runoff.
研究了该地区河川径流与当地气候变化之间的关系；
First the relationship between streamflow and local climate change is reviewed.
在最佳混凝条件下，雨水径流浊度的去除率达99%。
Under best coagulation condition, removal of 99% for turbidity was obtained.
坡度因素代表了土壤的持水能力，对径流和地下水有影响；
Slope would change water storage capacity. Distance is used to represent the water utilization capacity.
坡面径流平均输沙率与平均剪切力之间量良好的线性关系。
The relationship between the average sediment transport rate and the a...
以地表径流形式输出该系统的水量占年均降雨量的9.4 %。
The surface runoff output is 9.4% of the average annual rainfall.
研究还表明，该方法在水文月径流时间序列的预测中同样有效。
On runoff time series forecasting, this method shows a good result, too. 3.
水文模型对径流成份的划分也可以用来研究枯期径流及基流分割。
Watershed hydrological models are also able to investigate low flow and base flow separation.
水文模型对径流成份的划分也可以用来研究枯期径流及基流分割。
Watershed hydrological models are also able to investigate low flow and base flow separation.
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