液压头
米
导水率
地下水
水文学(农业)
采样(信号处理)
岩土工程
环境科学
主管(地质)
管(容器)
地下水排放
蒙特卡罗方法
地质学
土壤科学
地下水流
含水层
地貌学
工程类
土壤水分
滤波器(信号处理)
电气工程
物理
统计
机械工程
数学
天文
作者
John E. Solder,Troy E. Gilmore,David P. Genereux,D. Kip Solomon
出处
期刊:Ground Water
[Wiley]
日期:2015-12-18
卷期号:54 (4): 588-595
被引量:25
摘要
Abstract We designed and evaluated a “tube seepage meter” for point measurements of vertical seepage rates ( q ), collecting groundwater samples, and estimating vertical hydraulic conductivity ( K ) in streambeds. Laboratory testing in artificial streambeds show that seepage rates from the tube seepage meter agreed well with expected values. Results of field testing of the tube seepage meter in a sandy‐bottom stream with a mean seepage rate of about 0.5 m/day agreed well with Darcian estimates (vertical hydraulic conductivity times head gradient) when averaged over multiple measurements. The uncertainties in q and K were evaluated with a Monte Carlo method and are typically 20% and 60%, respectively, for field data, and depend on the magnitude of the hydraulic gradient and the uncertainty in head measurements. The primary advantages of the tube seepage meter are its small footprint, concurrent and colocated assessments of q and K , and that it can also be configured as a self‐purging groundwater‐sampling device.
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