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Deriving and validating pedotransfer functions for some calcareous soils

机译:推导和验证某些石灰质土壤的pedotransfer函数

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The unsaturated soil hydraulic properties are needed for many different applications in soil hydrology. Pedotransfer functions (PTFs) have proven to be useful to indirectly estimate these parameters from more easily obtainable soil data. Until now no studies have been conducted to derive or verify PTFs for calcareous soils, which hydraulically may not behave the same as non-calcareous soils. The objectives of this study were to assess the influence of soil CaCO_3 on the soil water retention characteristics of some calcareous soils, and to derive PTFs for these soils. Two data sets were used to derive and evaluate the established PTFs. Data set 1 containing 220 samples was employed as a calibration set for multiple linear regression. An independent data set containing 55 soil samples from a different location served to verify the derived PTFs. No significant difference in accuracy was found between the PTFs with and without CaCO_3 in terms of estimating specific soil water retention values or the van Genuchten soil hydraulic parameters. Compared with the Rosetta PTFs of Schaap et al. (2001), the derived point and parametric PTFs provided better accuracy with average RMSE values of 0.028 and 0.107cm~3cm~(-3), respectively.
机译:土壤水文学中许多不同的应用都需要非饱和土壤水力学特性。已证明,Pedotransfer函数(PTF)可用于根据更容易获得的土壤数据间接估算这些参数。到目前为止,还没有进行过研究来推导或验证钙质土壤的PTF,而钙质土壤的水力特性可能与非钙质土壤不同。这项研究的目的是评估土壤CaCO_3对某些石灰质土壤保水特性的影响,并推导这些土壤的PTF。使用两个数据集来推导和评估已建立的PTF。包含220个样本的数据集1被用作多元线性回归的校准集。一个独立的数据集包含来自不同位置的55个土壤样品,用于验证派生的PTF。在估算特定土壤保水值或van Genuchten土壤水力参数方面,在有和没有CaCO_3的PTF之间,在精度上没有发现显着差异。与Schaap等人的Rosetta PTF比较。 (2001年),派生的点和参数PTFs提供更好的准确性,分别为0.028和0.107cm〜3cm〜(-3)。

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