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Evaluation of Ground Penetrating Radar and Vertical Electrical Sounding Methods to Determine Soil Horizons and Bedrock at the Locality Dehtafe

机译:对探地雷达和垂直电测深方法的评估,以确定局部水平的土壤层和基岩

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摘要

Recently, geophysical methods have been widely used in many fields including pedology. Two of them, ground penetrating radar (GPR) and vertical electrical sounding (VES) were employed at the Dehtafe experimental site with the aim to evaluate their application in the Cambisol and Stagnosol soil types and crystalline bedrock survey in Czech conditions. These measurements were complemented by the classical soil survey using a gouge auger. As a result, interpreted soil and rock environment profiles wereobtained, with the identification of boundaries of Bg, C, and R soil horizons and bedrock at various degrees of weathering. The interpretation of measurement records demonstrated suitability of the VES and GPR method application, using GPR for imaging the soil profile and the top of bedrock, while the VES method gave better results in imaging greater depths. The research demonstrated advantages of the geophysical methods such as instancy, continuous imaging, and no disturbance of the subsurface. In spite of needing classical survey data for interpretation of the results obtained by the geophysical methods, their usage can bring better quality to the soil profile imaging.
机译:近来,地球物理方法已经广泛地用于许多领域,包括心理学。 Dehtafe实验场使用了其中的两个,即探地雷达(GPR)和垂直电测深(VES),目的是评估它们在捷克条件下的Cambisol和Stagnosol土壤类型以及结晶基岩测量中的应用。这些测量通过使用凿钻的经典土壤调查得到补充。结果,获得了解释的土壤和岩石环境概况,并确定了在不同风化程度下Bg,C和R土壤层和基岩的边界。测量记录的解释证明了VES和GPR方法应用的适用性,使用GPR对土壤剖面和基岩顶部进行成像,而VES方法在对更大深度进行成像时效果更好。研究证明了地球物理方法的优势,例如即时,连续成像以及对地下没有干扰。尽管需要经典的调查数据来解释通过地球物理方法获得的结果,但是它们的使用可以为土壤剖面成像带来更好的质量。

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