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Recognition of shallow karst water resources and cave potentials using thermal infrared image and terrain characteristics in semi-arid regions of Iran

机译:利用热红外图像和地形特征识别伊朗半干旱地区的浅层喀斯特水资源和洞穴潜力

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摘要

Shallow karst water resources and caves may influence land surface temperatures due to cold transfer property of rocks and evaporation from buried karst. The objective of this research was to develop a method for recognition of karst areas based on evaluating the surface characteristics that manifest itself by low land surface temperature in the satellite images. Investigation of thermal ETM+ image of the study region in Iran showed that parts of carbonate rocks that bear karst water are relatively cooler compared to areas with similar terrain conditions. Relational modeling provided useful information on spatial distribution of areas that have the potential to hold karst water resources and/or caves. Further inspection of ASTER images, along with geotechnical, geophysical and geological field surveys verified the approach. Significant correlation was found between electrical resistivity and thermal band values. The method may be used as a primary exploratory tool for shallow karst water explorations in similar areas.
机译:浅层岩溶水资源和溶洞可能会由于岩石的冷传递特性和地下岩溶的蒸发而影响地表温度。这项研究的目的是基于评估卫星图像中低地表温度所表现出的表面特征,开发一种识别喀斯特地区的方法。对伊朗研究区域的ETM +热图像进行的调查显示,与地形条件相似的地区相比,部分带有岩溶水的碳酸盐岩相对凉爽。关系建模提供了有关可能保留岩溶水资源和/或洞穴的区域空间分布的有用信息。对ASTER图像的进一步检查以及岩土,地球物理和地质野外勘测证明了该方法。发现电阻率和热带值之间存在显着的相关性。该方法可用作相似地区浅层岩溶水勘探的主要勘探工具。

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