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Characterization of reactive transport by 3-D electrical resistivity tomography (ERT) under unsaturated conditions

机译:在不饱和条件下通过3-D电阻层析成像(ERT)表征反应性输运

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摘要

The leaching of nitrate from intensively used arable soil is of major concern in many countries. In this study, we show how time lapse electrical resistivity tomography (ERT) can be used to characterize spatially heterogeneous processes of ion production, consumption, and transport in soils. A controlled release fertilizer was introduced into an undisturbed soil core in a laboratory lysimeter and subjected to infiltration events. The production of ions resulting from processes associated with nitrification and their transport through the soil core was observed by time lapse ERT and analysis of seepage water samples from a multicompartment sampler. ERT images show development and propagation of a high-conductivity plume from the fertilizer source zone. Molar amounts of nitrate produced in and exported from the soil core could be well reproduced by time lapse ERT using a spatial moment analysis. Furthermore, we observed that several shape measures of local breakthrough-curves (BTCs) of seepage water conductivity and nitrate derived by effluent analyses and BTCs of bulk conductivity derived by ERT are highly correlated, indicating the preservation of spatial differences of the plume breakthrough in the ERT data. Also differences between nitrate breakthrough and a conservative tracer breakthrough can be observed by ERT. However, the estimation of target ion concentrations by ERT is error bound and the smoothing algorithm of the inversion masks spatial conductivity differences. This results in difficulties reproducing spatial differences of ion source functions and variances of travel times. Despite the observed limitations, we conclude that time lapse ERT can be qualitatively and quantitatively informative with respect to processes affecting the fate of nitrate in arable soils.
机译:在许多国家中,从密集使用的耕地中浸出硝酸盐备受关注。在这项研究中,我们展示了如何使用延时电阻层析成像(ERT)来表征土壤中离子产生,消耗和运输的空间异质过程。将控释肥料引入实验室测渗仪中未受干扰的土壤芯中,并进行渗透作用。通过定时ERT和对来自多隔室采样器的渗漏水样品的分析,可以观察到与硝化过程相关的离子的产生及其通过土壤核心的迁移。 ERT图像显示了来自化肥源区的高导电羽流的发育和传播。使用空间矩分析可以通过时差ERT很好地再现土壤核心中产生和输出的硝酸盐的摩尔量。此外,我们观察到,通过流出物分析得出的渗流水电导率和硝酸盐的局部突破曲线(BTC)和通过ERT得出的体积电导率的BTC的几种形状度量高度相关,这表明保留了羽状突破在空间中的空间差异。 ERT数据。 ERT也可以观察到硝酸盐突破与保守示踪剂突破之间的差异。但是,通过ERT估算目标离子浓度受到误差的限制,反演的平滑算法掩盖了空间电导率差异。这导致难以再现离子源功能的空间差异和传播时间的差异。尽管存在观察到的限制,但我们得出结论,就影响耕地土壤硝酸盐命运的过程而言,延时ERT可以在质量和数量上提供信息。

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