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首页> 外文期刊>Advance journal of food science and technology >Study on the Model of Soil Water Resources Quantity in Baoding Plain
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Study on the Model of Soil Water Resources Quantity in Baoding Plain

机译:保定平原土壤水资源量模型研究

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摘要

The soil water resources has special properties, independent of surface water resources and groundwater resources. The relationship between soil water resources and soil water, the concept and characteristics of soil water resources have been analyzed and the model calculating the soil water resources quantity under the natural condition has been put forward based on the principle of water balance principle in this study. The model parameters have been focused on. Firstly, the daily precipitation has been determined based on typical year. Secondly, the surface runoff has been applied on the basis of the hydrological model of runoff yield in excess of infiltration. Thirdly, canopy interception rainfall has been concluded according to canopy interception model. Fourthly, the water quantity of infiltrated out of the assessment layer has been calculated based on the hydrological model of runoff yield at natural storage. The model has been applied to the work of soil water resources assessment of Qingyuan county in Baoding plain and the result has showed that the soil water resources quantity in mean precipitation year is 301.1485 million m~3 and its temporal distribution is consistent with the distribution of rainfall of the year.
机译:土壤水资源具有特殊的特性,与地表水资源和地下水资源无关。分析了土壤水资源与土壤水分之间的关​​系,分析了土壤水资源的概念和特征,并基于水平衡原理,提出了自然条件下土壤水资源量的计算模型。模型参数已被关注。首先,根据典型年份确定日降水量。其次,在径流产量超过入渗量的水文模型的基础上,应用了地表径流。第三,根据冠层截留模型得出了冠层截留降雨的结论。第四,根据自然储藏区径流量的水文模型,计算了从评价层渗入的水量。将该模型应用于保定平原清远县土壤水资源评价工作中,结果表明,平均降水年土壤水资源量为30114.85万m〜3,时间分布与降水量的分布一致。年的降雨量。

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