Characterization of agricultural contaminant transport using ground-penetrating radar and electrical data

P. Sénéchal, H. Perroud, A. Bourg
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Abstract

In this on-going study, a combination of Ground Penetrating Radar (GPR) and electrical surveys is used to characterize the physico-chemical properties of soil, in particular those concerning lithology variations, water content, porosity and salinity in agricultural zones. These investigations will be completed by independent chemical analyses of soil and water. The experiments are conducted on fields of intensive corn culture (4 x 2 km) where the water table is 1.5 to 5 m deep, in a geological context of alluvial deposits. Analyses of water from various wells in the study area show high concentrations of nitrate coming from the chemical fertilizers spread on the soil surface. Globally, values increase from south to north and can be explained by the general direction of flow in the water table aquifer. In this on-going study, GPR and electrical data are recorded at two sites located along a north-south line and seasonal variations will be monitored for twelve months. Preliminary results which are presented here, give structural information concerning the subsurface and show vertical flow of mineralized water (from the surface to the aquifer) providing evidence of transport of dissolved contaminants to the water table aquifer. This study demonstrates the potential of non-destructive geophysical methods for providing information on hydric and solute transfer in the ground and monitoring soil contamination.
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利用探地雷达和电气数据表征农业污染物的运输
在这项正在进行的研究中,利用探地雷达(GPR)和电测量相结合来描述土壤的物理化学性质,特别是那些与农业地区的岩性变化、含水量、孔隙度和盐度有关的性质。这些调查将通过对土壤和水的独立化学分析来完成。实验在地下水位为1.5至5米深的玉米集约化栽培田(4 × 2公里)进行,地质环境为冲积矿床。对研究地区各口井的水进行的分析表明,土壤表面扩散的化肥中含有高浓度的硝酸盐。在全球范围内,数值从南到北增加,这可以用地下含水层的总体流动方向来解释。在这项正在进行的研究中,在沿南北线的两个地点记录了探地雷达和电数据,并将监测12个月的季节变化。这里介绍的初步结果给出了有关地下的结构信息,并显示了矿化水的垂直流动(从地表到含水层),提供了溶解污染物向地下含水层输送的证据。这项研究证明了非破坏性地球物理方法在提供地下水和溶质转移信息以及监测土壤污染方面的潜力。
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