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与地表水的蓄水相反,水文研究过程中对降水在土壤中暂时蓄水量和蓄水时间考虑得很少。这是因为获得数据比较困难之故。现在,应用奥地利耕水试验设施进行的一系列观测,都为求某些土壤水的蓄水系数提供了可能。土壤中水的蓄存及消耗与地表水域的情况相似。当然,土壤的水力过程不易观察到。此外,
Contrary to the impoundment of surface water, little attention has been given to the temporary water storage and storage time of precipitation in the soil during hydrological research. This is because it is more difficult to obtain the data. Now, a series of observations using the Austrian tillage test facility have made it possible to find some of the soil water storage coefficients. Storage and consumption of water in soil is similar to that in surface waters. Of course, the soil’s hydraulic processes are not easily observed. In addition,