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Pedotransfer Functions for the Estimation of Saturated Hydraulic Conductivity for Some Indian Sandy Soils

机译:用于估计一些印度砂土的饱和液压导电性的PEDOT转换功能

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摘要

Determination of the saturated hydraulic conductivity (k(s)) is needed in many studies and applications related to irrigation, drainage, water movement and solute transport in the soil. Although many advances are made for direct measurements of k(s), they are usually time consuming and costly. Some attempts have been made to indirectly predict the saturated hydraulic conductivity from the more easily or readily available basic soil properties. The objective of this study was to develop and validate Pedotransfer Functions (PTFs) for estimation of saturated hydraulic conductivity using multiple non-linear regression technique. One hundred and one soil samples were collected from agricultural and forest soils at different depths, at different locations in the Pavanje River basin that lies in the southern coastal region of Karnataka, India. Saturated hydraulic conductivity was measured, by variable falling head method through Permeameter in the laboratory. Prediction accuracies were evaluated using coefficient of determination, root mean square error, mean error, geometric mean error ratio and geometric standard deviation of the error ratio between measured and predicted values. The results show that, the PTFs for the estimation of saturated hydraulic conductivity could be used appropriately for the soils with loamy sand and sandy loam textures falling in this area of the coastal region of southern India.
机译:在许多与灌溉,排水,水运动和土壤中的溶质运输有关的研究和应用中需要确定饱和液压导电性(K(S))。虽然对K(S)的直接测量进行了许多进步,但它们通常是耗时和昂贵的。已经采取了一些尝试,以间接地预测饱和液压导电性,从更容易或容易获得的基础土壤性质。本研究的目的是开发和验证使用多元非线性回归技术估计饱和液压导电的网兜传递功能(PTF)。从不同深度的农业和森林土壤中收集了一百一和一种土壤样品,在帕兰杰河流域的不同地点,位于印度卡纳塔克卡南部沿海地区。通过在实验室中通过渗透率来测量饱和液压导率。使用确定系数,均误差,误差,几何误差比和测量值之间的误差比的几何标准偏差来评估预测精度。结果表明,估计饱和液压导电性的PTF可适当地用于落在印度南部沿海地区的这一领域的植物砂和砂壤土纹理的土壤。

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