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A Bimodal Four-parameter Lognormal Linear Model Of Soil Water Repellency Persistence

机译:土壤憎水持久性的双峰四参数对数正态线性模型

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Soil water repellency may be characterized in terms of the delayed infiltration time of a water droplet resting on the soil surface, which is, water drop penetration time (WDPT), or repellency persistence. Such repellency persistence varies nonlinearly with soil water content (θ_g), although no models have been proposed to reproduce the variation of WDPT with θ_g in soils. Dynamic factor analysis (DFA) is used to identify two common patterns of unexplained variability in a scattered dataset of WDPT versus θ_g measurements. A four-parameter lognormal distribution was fitted to both common patterns obtained by DFA, and these were combined additively in a weighted multiple linear bimodal model. We show how such an empirical model is capable of reproducing a large variety of WDPT versus θ_g curve shapes (N = 80) both within a wide range of measured WDPTs (0-17 000 s) and for samples with organic matter content ranging from 21.7 to 80.6 g (100 g)~(-1).
机译:土壤疏水性可以通过停留在土壤表面的水滴的延迟渗透时间来表征,即水滴渗透时间(WDPT)或疏水性持久性。尽管没有提出模型来再现土壤中WDPT随θ_g的变化,但这种驱避性持久性随土壤含水量(θ_g)呈非线性变化。动态因子分析(DFA)用于在WDPT与θ_g测量值的分散数据集中识别出两种无法解释的常见变化模式。将四参数对数正态分布拟合到通过DFA获得的两种常见模式,并将它们加在一起组合在加权多重线性双峰模型中。我们展示了这样一个经验模型如何能够在宽范围的测量WDPT(0-17 000 s)以及有机物含量范围为21.7的样本中重现各种WDPT与θ_g曲线形状(N = 80)至80.6 g(100 g)〜(-1)。

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