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Predicting the soil moisture retention curve, from soil particle size distribution and bulk density data using a packing density scaling factor

机译:使用填充密度缩放因子,根据土壤粒度分布和堆积密度数据预测土壤保水曲线

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A substantial number of models predicting the soil moisture characteristiccurve (SMC) from particle size distribution (PSD) data underestimate thedry range of the SMC especially in soils with high clay and organic mattercontents. In this study, we applied a continuous form of the PSD model topredict the SMC, and subsequently we developed a physically based scalingapproach to reduce the model's bias at the dry range of the SMC. The soilparticle packing density was considered as a metric of soil structure andused to define a soil particle packing scaling factor. This factor wassubsequently integrated in the conceptual SMC prediction model. The modelwas tested on 82 soils, selected from the UNSODA database. Theresults show that the scaling approach properly estimates the SMC for allsoil samples. In comparison to the original conceptual SMC model withoutscaling, the scaling approach improves the model estimations on average by30%. Improvements were particularly significant for the fine- and medium-textured soils. Since the scaling approach is parsimonious and does not relyon additional empirical parameters, we conclude that this approach may beused for estimating SMC at the larger field scale from basic soil data.
机译:从粒度分布(PSD)数据预测土壤水分特征曲线(SMC)的大量模型都低估了SMC的干燥范围,尤其是在粘土和有机物含量高的土壤中。在这项研究中,我们应用了PSD模型的连续形式来预测SMC,随后我们开发了基于物理的缩放方法,以减小模型在SMC干燥范围内的偏差。土壤颗粒堆积密度被认为是土壤结构的度量,并用于定义土壤颗粒堆积比例因子。随后将该因素整合到概念性SMC预测模型中。该模型在选自UNSODA数据库的82种土壤上进行了测试。结果表明,比例缩放方法可以正确估计所有土壤样品的SMC。与没有缩放的原始概念SMC模型相比,缩放方法将模型估计平均提高了30%。对于质地细密和中等质地的土壤,改进特别重要。由于缩放方法是简约的,并且不依赖于其他经验参数,因此我们得出结论,该方法可用于根据基本土壤数据在较大的野外规模下估计SMC。

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