Some channel‐storage studies and their application to the determination of infiltration
Some channel‐storage studies and their application to the determination of infiltration
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DOI：
10.1029/tr019i001p00435
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发表时间：
1938-08
期刊：
影响因子：
--
通讯作者：
W. Langbein
中科院分区：
文献类型：
--
作者：
W. Langbein
最近几次大洪水的研究结果强调了分析降雨量和由此产生的径流量之间关系的实用价值。分析是针对评估各自的价值的土壤和河道的机构处理潜在的洪水是特别相关的。如果来自非渗透水的蒸发损失可以被忽略为无关紧要的，如在冬季的长时间风暴期间，那么降雨和相关径流之间的差异可以归因于以渗透、截留和表面储存为代表的土壤影响。因此，分析中的问题是如何将降雨量与由此产生的径流量联系起来。本文描述的程序是对1937年1月俄亥俄州河洪水的降雨量和径流关系研究的结果[见文末参考文献1]。
Results of studies of recent major floods have emphasized the practical value of analyses of the relation between rainfall and resultant runoff. Analyses that are directed toward appraising the respective values of the soil and the river-channel as agencies for disposing of potential flood-waters are especially pertinent. If evaporation-losses from non-infiltrated water may be neglected as inconsequential, as during prolonged storms of winter, the difference between rainfall and the associated runoff may be ascribed to such edaphic influences represented by infiltration, interception, and surface-storage. The problem in the analyses is therefore one of correlating rainfall and resultant runoff. The procedures described in this paper resulted from studies of the rainfall and runoff relations of the Ohio River flood of January 1937 [see 1 of References at end of paper].