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Predicting soil water retention characteristics for Vietnam Mekong Delta soils

机译:预测越南湄公河三角洲土壤水保留特性

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Soil hydraulic properties (e.g. soil water retention and hydraulic conductivity) are very important for agricultural and environmental management practices. However, the direct field or laboratory measurement of these characteristics is costly, laborious and time-consuming. Therefore, their indirect estimation from available and easily measured soil properties has received great interest. Pedotransfer functions (PTFs) are being used as a well-known indirect method for determining hydraulic properties from basic soil properties (e.g. soil texture, bulk density and organic carbon content). In this study, we derived two types of PTFs, point and pseudo-continuous functions, for estimating moisture retention characteristics of soils in the Mekong Delta of Vietnam. The data of 120 samples were collected from agricultural fields distributed over the area. The results reveal that point PTFs outperformed pseudo-continuous functions. Moreover, the plastic limit, on top of classical predictors, appears to be a promising variable to predict soil water retention, especially in the wet moisture range.
机译:土壤液压特性(例如土壤水保留和水力传导)对农业和环境管理实践非常重要。然而,这些特征的直接领域或实验室测量成本高,费力且耗时。因此,从可用和容易测量的土壤性质的间接估计得到了极大的兴趣。 PEDOT转器功能(PTF)被用作众所周知的间接方法,用于从基本土壤特性确定液压性能(例如土壤质地,散装密度和有机碳含量)。在这项研究中,我们衍生出两种类型的PTF,点和伪连续功能,用于估算越南湄公河三角洲土壤的水分保留特征。从分布在该地区的农业领域收集120个样品的数据。结果表明,点PTFS优于伪连续功能。此外,在经典预测因子顶部的塑料极限似乎是预测土壤保水的有希望的变量,特别是在湿水分范围内。

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