Stochastic behavior of soil physical properties responsible for ground water recharge

机译：负责地下水补给的土壤物理性质的随机行为

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Results received recently in small experimental catchment are as follows: subsurface flow is prevalent over the major part of area and more frequent in time, active source area of watershed is very changeable affecting from antecedent soil moisture, surface flow origins above the soil cover mainly by heavy rainfalls, soil water residence time changes stochastically. Predictive ability of the model for infiltration based upon modified Green-Ampt approach was enhanced through a spatially common soil properties described as the joint probability function.

机译：最近在小型实验流域收到的结果如下：地下流在该地区的大部分地区盛行，时间上更频繁，流域的有效源区变化很大，受前期土壤水分的影响，表面流主要来自土壤覆盖层。大雨，土壤水的停留时间随机变化。通过描述为联合概率函数的空间通用土壤特性，增强了基于改进的Green-Ampt方法的入渗模型的预测能力。

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来源
《International Conference on Groundwater Research, Jun 6-8, 2000, Copenhagen, Denmark》|2000年|p.133-134|共2页
会议地点 Copenhagen Denmark
作者
V.A. Shutov;
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作者单位

Valday Branch of State Hydrological Institute, Valday, Russia;

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会议组织
原文格式 PDF
正文语种 eng
中图分类 P6;
关键词
soil properties; spatial distribution; joint frequency function; infiltration; residence time;

机译：土壤性质；空间分布;联合频率函数；浸润;停留时间;

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Stochastic behavior of soil physical properties responsible for ground water recharge

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