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Soil water-retention prediction from pedotransfer functions for some Indian soils.

机译:根据部分土壤的pedotransfer函数预测土壤保水率。

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This paper discusses the development of pedotransfer functions (PTFs) and uses a multiple nonlinear regression technique to validate point and parametric PTFs for the estimation of a water-retention curve from basic soil properties such as particle-size distribution, bulk density and organic matter content. One hundred soil samples were collected at different depths from different locations in the Pavanje river basin that lies within the southern coastal region of Karnataka, India. Prediction accuracies were evaluated using the coefficient of determination (R2), root mean square error (RMSE) and mean error (ME) between measured and predicted values. Overall, both point and parametric methods predicted water contents at selected water potentials with considerable accuracy. However, prediction of the soil water-retention curve using PTFs by point estimation method was relatively more successful (best case R2=0.983) for the sampled soils. F-tests were also conducted for all cases. For one regression equation, the p-value was zero and for other equation, values were close to zero. Critical comparative analysis was carried out on the performances of the point and parametric methods. Use of the developed PTFs is suggested for the prediction of a water-retention curve for loamy sand and sandy loam soils in this area of the coastal region of southern India.
机译:本文讨论了pedotransfer函数(PTF)的发展,并使用多重非线性回归技术来验证点和参数PTF,以根据基本土壤性质(例如粒度分布,堆积密度和有机质含量)估算保水曲线。 。从位于印度卡纳塔克邦南部沿海地区的帕瓦涅河流域的不同地点,以不同深度收集了一百份土壤样品。使用确定系数(R 2 ),测量值和预测值之间的均方根误差(RMSE)和均值误差(ME)来评估预测准确性。总的来说,点和参数方法都可以在相当高的精度下预测选定水势下的水含量。然而,对于点样土壤,采用点估计法利用PTFs预测土壤保水曲线相对较为成功(最佳情况R 2 = 0.983)。还对所有情况进行了F检验。对于一个回归方程,p值为零,对于其他方程,值接近零。对点方法和参数方法的性能进行了重要的比较分析。建议使用已开发的PTF预测印度南部沿海地区该地区的壤土和砂质壤土的保水曲线。

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