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Assessment models to estimate water permeability in the soil

机译:评估模型以评估土壤中的水渗透率

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摘要

Permeability of the most important components, the hydrological cycle is, and one of the most commonly-physical phenomena, that researchers agricultural and natural resources, are relative to it particular attention. Accordingly, the present study, which is aimed to evaluating of the various models Horton, Kostiakov, Philip, Green Mpt and Organization Soil Conservation of American, by using data obtained from a 38-point permeability, using the Double Ring, was established in the Forest Park in yasuj.In order to compare the performance of different models was used the measures of measurement accuracy different, including the correlation coefficient, the square root square error. Modeling results showed that, on average, is visible the maximum correlation coefficient, in model of Philip and Kostiakov (R> 90), so that, depending on the soil texture, the accuracy of models, as well as to some extent varied and in clay soils, and sandy, Philip model, and,in clay soil of loamy, Kostiakov model, were identified as a top model, while the minimum coefficient of determination in Horton model obtained in all soils (R <70). In total, the maximum correlation values were obtained in clay soils of loamy.
机译:水文循环是最重要的组成部分的渗透性,研究人员的农业和自然资源是最常见的物理现象之一,对此特别关注。因此,本研究旨在通过使用双环法从38点渗透率获得的数据评估美国的Horton,Kostiakov,Philip,Green Mpt和Organisation土壤保持的各种模型。为了比较不同模型的性能,使用了相关系数,平方根平方误差等测量精度的量度。建模结果表明,在Philip和Kostiakov(R> 90)模型中,平均而言,最大相关系数可见,因此,根据土壤质地,模型的精度以及一定程度上会有所不同。粘土模型和沙质的Philip模型以及壤土粘土的Kostiakov模型被确定为顶层模型,而Horton模型的最小测定系数在所有土壤中均得到了确定(R <70)。总的来说,最大的相关值是在壤土中获得的。

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