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Soil Water Modeling in South Georgia using WEPP Hydrology

机译:利用WEPP水文南格鲁吉亚土壤水建模

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Soil water is a fundamental component of any field or watershed scale water balance. A basin scale soil water model is being assembled using the runoff and water redistribution functions within the WEPP model. The model uses the runoff, infiltration,plant uptake, and water redistribution functions within WEPP to make predictions of soil water within the vadose zone. The WEPP model was evaluated using runoff and soil water data collected from South Georgia experimental plots where the effects of conservation tillage were examined. WEPP model simulations of surface runoff from the plots were within 30% of the observed annual runoff for the years used for calibration but varied considerably for the years used for model validation. In general, resultswere better for the simulations of the strip tillage system than for the conventional tillage system. Simulations of soil water in the upper profile were useful for examining seasonal patterns and for examining differences between the two tillage systems.
机译:土壤水是任何领域或流域水平的基本组成部分。使用WEPP模型中的径流和水再分配功能组装盆地缩放土壤水模型。该模型采用WEPP中的径流,渗透,植物摄取和水再分配功能,以便在散阳区内的土壤水预测。通过从南格鲁氏藻实验图中收集的径流和土壤水数据进行评估WEPP模型,其中检查了保护耕作的影响。从地块中的表面径流模拟的WEPP模型模拟是在用于校准的岁月的观察到年度径流的30%以内,但对于用于模型验证的多年而变化很大。一般来说,对于传统耕作系统,为带状耕作系统的模拟产生了更好的。上部轮廓中的土壤水模拟可用于检查季节性模式和检查两个耕作系统之间的差异。

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