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Characterization of soil structure and water infiltration spatial variability using electrical resistivity tomography at decimetre scale. A study of two contrasted soil tillage modalities

机译:二手尺度电阻率断层扫描土壤结构及水渗透空间变异性的特征。两种对比土壤耕作方式的研究

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Simplification of tillage practices is often considered as a solution for reducing time constraints and costs, and also for limiting soil erosion. Simplified tillage practices adopted over several years progressively induce modifications of soil physical properties in the top soil layer at decimetric scale. The general aim of this study was to test the capacity of electrical resistivity tomography to characterize the spatial variability of soil structure, bulk density and water flow in a loamy Cambisol with two modalities of tillage (conventional tillage, no tillage). For each tillage treatment, the experiment combined: 1) a description of the soil structure profile, 2) measurements of bulk density and soil hydraulic conductivities; 3) 2D electricalresistivity tomographies measured before and after an irrigation to characterize the spatial variability of soil water fluxes. These geophysical data are correlated to the spatial variability of soil structure and hydrodynamics properties.
机译:耕作实践的简化通常被认为是减少时间限制和成本的解决方案,以及限制土壤侵蚀。在几年内采用的简化耕作实践逐步诱导减去尺度下土壤层中土壤物理性质的修饰。本研究的一般目标是测试电阻率断层扫描的能力,以表征土壤结构的空间变异性,植物密度和植物中的植物植物醇的空间变异,具有两种耕作方式(常规耕作,无耕作)。对于每种耕作处理,实验组合:1)土壤结构轮廓的描述,2)散装密度和土壤液压传导的测量; 3)2D电气耐心率断层刻录物在灌溉前后测量,以表征土壤水通量的空间变异性。这些地球物理数据与土壤结构和流体动力学特性的空间变异相关。

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