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C18 Coastal Aquifer Characterization based on Seismic and Resistivity Imaging Methods: a Case Study from Costa Brava, Spain

机译:C18基于地震和电阻率成像方法的沿海含水层表征:西班牙哥斯达堡的案例研究

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Coastal aquifer formations located in Northeast of Spain affected by saline intrusion has been the focus for a multi-technique geophysical study. Two aquifers are present: a shallow aquifer in the quaternary sediments and a deeper karstic aquifer. The objectives were: (1) estimate quaternary sediment thickness and characterize weathered/fractured rock (2) qualitative assessment of water degradation changes within the study area. The methodology consisted of combining and integrating seismic and resistivity imaging techniques: seismic refraction tomography (SRT), electrical resistivity tomography (ERT) and H/V microtremor technique. Three ERT and SRT coincident profiles have been acquired from sea to inland. Comparison of velocity and electrical models has allowed obtaining quaternary and weathered/fractured bedrock thickness. Electrical resistivity differences from one to another profile help mapping changes in saline intrusion. H/V technique has been suitable to obtain bedrock depth in the profile close to sea. However, strong attenuation of the microtremor signal has precluded its application in the rest of the study area. This attenuation could be related to the dissipation of seismic energy in moving fluids through a thick zone of fractured/weathered bedrock. All this information is critical in order to establish preferential water flows and groundwater degradation of the aquifers.
机译:位于西班牙东北部的沿海含水层形成受盐水侵入的焦点是多技术地球物理学研究。存在两种含水层:四季沉积物中的浅含水层和更深的岩溶含水层。目标是:(1)估计季沉积物厚度,表征风化/裂缝岩(2)定性评估研究区内的水利变化。该方法包括组合和集成地震和电阻率成像技术:地震折射断层扫描(SRT),电阻率断层扫描(ERT)和H / V MicroReRemor技术。从海上获得了三个ert和SRT巧合的概况到内陆。速度和电气模型的比较允许获得第四季和风化/破碎的基岩厚度。电阻率与另一个型材的电阻率差异有助于绘制盐水侵入的变化。 H / V技术适合于在靠近海的轮廓中获得基岩深度。然而,对微反射信号的强度衰减绝不能在研究区域的其余部分中的应用。这种衰减可能与通过粗糙的裂缝/风化基岩的厚区域散发出地震能量的耗散。所有这些信息都是至关重要的,以便建立含水层的优先水流和地下水降解。

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