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Modelling and validation hysteresis in soil water retention curve using tomography of pore structure

机译:孔隙结构层析成像在土壤保水曲线中的滞后建模与验证

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摘要

Hysteresis in soil water retention curve (SWRC hysteresis) has a significant effect on soil water flow in unsaturated porous soils. The aims of the were to estimate wetting curve of the soil water retention curve based on drying curve and to study the reasons of hysteresis using tomography of pore structure. SWRC hysteresis was measured using capillarimeters for drying and wetting curves under a low soil potential. The proposed model α_(w) = 2.5, α_(d) was presented to calculate alpha of wetting curve ( α_(w) ) based on alpha of drying curve ( α_(d) ). The tomography method was used for describing the structure of porous space in the wetting and drying soils. Generally, the results of RMSE = 0.08 cm~(−1), GMER = 0.87, and Williams-Kloot test indicated that the proposed model can be used for estimation wetting curve under a low soil potential. Tomography of pore structure is a new technique used for describing the occurrence of hysteresis in SWRC.
机译:土壤保水曲线中的滞后性(SWRC滞后性)对非饱和多孔土壤中的水流具有显着影响。其目的是根据干燥曲线估算土壤保水曲线的润湿曲线,并使用孔隙结构层析成像技术研究滞后的原因。使用毛细管仪在低土壤电势下测量SWRC滞后的干燥和润湿曲线。提出了建议的模型α_(w)= 2.5,α_(d)基于干燥曲线(α_(d))的α来计算润湿曲线(α_(w))的α。层析成像方法用于描述湿润和干燥土壤中的多孔空间结构。通常,RMSE = 0.08 cm〜(-1),GMER = 0.87和Williams-Kloot试验的结果表明,该模型可用于估算低土壤电势下的湿润曲线。孔结构层析成像是一种用于描述SWRC滞后现象的新技术。

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