用介电弛豫谱估计土壤水分特征

N. Wagner, F. Daschner, A. Scheuermann, Moritz Schwing
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引用次数: 5

摘要

水饱和和非饱和多孔材料(如土壤)介电材料特性的频率依赖性不仅干扰了高频电磁技术的应用,而且由于水孔隙溶液和矿物相之间的相互作用的强烈贡献,也包含了材料的有价值的信息。因此,宽带高频电磁传感器技术能够估计土壤的物理化学参数,如含水量、质地、矿物学、阳离子交换容量和基质电位。在此背景下,应用多元(MV)方法从实验测定的粉质粘土的介电弛豫谱中估计土壤水特征曲线(SWCC)。将mv方法的结果与经验方程、理论模型以及一种新型的液压/电磁耦合方法的结果进行了比较。应用mv方法提供了证据,(i)土壤介电松弛行为和土壤水分特征之间的物理关系是一种重要的水力材料特性,(ii)适当的传感器技术适用于从宽带测量的介电光谱估计多孔介质的物理化学参数。
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Estimation of the Soil Water Characteristics from dielectric relaxation spectra
The frequency dependence of dielectric material properties of water saturated and unsaturated porous materials such as soil is not only disturbing in applications with high frequency electromagnetic (HF-EM) techniques but also contains valuable information of the material due to strong contributions by interactions between the aqueous pore solution and mineral phases. Hence, broadband HF-EM sensor techniques enable the estimation of soil physico-chemical parameters such as water content, texture, mineralogy, cation exchange capacity and matric potential. In this context, a multivariate (MV) approach was applied to estimate the Soil Water Characteristic Curve (SWCC) from experimentally determined dielectric relaxation spectra of a silty clay soil. The results of the MV-approach were compared with results obtained from empirical equations and theoretical models as well as a novel hydraulic/electromagnetic coupling approach. The applied MV-approach gives evidence, (i) of a physical relationship between soil dielectric relaxation behavior and soil water characteristics as an important hydraulic material property and (ii) the applicability of appropriate sensor techniques for the estimation of physico-chemical parameters of porous media from broadband measured dielectric spectra.
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