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Measurement Scale Effect on Prediction of Soil Water Retention Curve and Saturated Hydraulic Conductivity

机译:测量尺度对土壤水分特征曲线预测的影响   饱和导水率

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摘要

Soil water retention curve (SWRC) and saturated hydraulic conductivity (SHC)are key hydraulic properties for unsaturated zone hydrology and groundwater. Inparticular, SWRC provides useful information on entry pore-size distribution,and SHC is required for flow and transport modeling in the hydrologic cycle.Not only the SWRC and SHC measurements are time-consuming, but also scaledependent. This means as soil column volume increases, variability of the SWRCand SHC decreases. Although prediction of the SWRC and SHC from availableparameters, such as textural data, organic matter, and bulk density have beenunder investigation for decades, up to now no research has focused on theeffect of measurement scale on the soil hydraulic properties pedotransferfunctions development. In the literature, several data mining approaches havebeen applied, such as multiple linear regression, artificial neural networks,group method of data handling. However, in this study we develop pedotransferfunctions using a novel approach called contrast pattern aided regression(CPXR) and compare it with the multiple linear regression method. For thispurpose, two databases including 210 and 213 soil samples are collected todevelop and evaluate pedotransfer functions for the SWRC and SHC, respectively,from the UNSODA database. The 10-fold cross-validation method is applied toevaluate the accuracy and reliability of the proposed regression-based models.Our results show that including measurement scale parameters, such as sampleinternal diameter and length could substantially improve the accuracy of theSWRC and SHC pedotransfer functions developed using the CPXR method, while thisis not the case when MLR is used. Moreover, the CPXR method yields remarkablymore accurate soil water retention curve and saturated hydraulic conductivitypredictions than the MLR approach.
机译:土壤保水曲线(SWRC)和饱和导水率(SHC)是非饱和区水文学和地下水的关键水力特性。特别是,SWRC提供了有关入口孔径分布的有用信息,SHC是水文循环中流量和输运模型的必要条件.SWRC和SHC的测量不仅费时,而且取决于规模。这意味着随着土壤柱体积的增加,SWRCand SHC的变异性降低。尽管数十年来一直在根据可用参数(如质地数据,有机质和堆积密度)对SWRC和SHC的预测进行研究,但到目前为止,还没有研究集中在测量尺度对土壤水力特性pedotransferfunctions发展的影响上。在文献中,已经应用了多种数据挖掘方法,例如多元线性回归,人工神经网络,数据处理的分组方法。但是,在这项研究中,我们使用一种称为对比模式辅助回归(CPXR)的新方法开发了脚踏板传递函数,并将其与多元线性回归方法进行了比较。为此,从UNSODA数据库中收集了包括210和213个土壤样品的两个数据库,分别开发和评估SWRC和SHC的脚踏传递函数。应用10倍交叉验证方法来评估所提出的基于回归的模型的准确性和可靠性。我们的结果表明,包括测量尺度参数(例如样品的内径和长度)可以显着提高开发的SWRC和SHC pedotransfer函数的准确性使用CPXR方法,而使用MLR则不是这种情况。此外,与MLR方法相比,CPXR方法可产生更精确的土壤保水曲线和饱和水力传导率预测。

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