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首页> 外文期刊>Journal of caves and karst studies: the National Speleological Society bulletin >DETERMINING GEOPHYSICAL PROPERTIES OF A NEAR-SURFACE CAVE THROUGH INTEGRATED MICROGRAVITY VERTICAL GRADIENT AND ELECTRICAL RESISTIVITY TOMOGRAPHY MEASUREMENTS
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DETERMINING GEOPHYSICAL PROPERTIES OF A NEAR-SURFACE CAVE THROUGH INTEGRATED MICROGRAVITY VERTICAL GRADIENT AND ELECTRICAL RESISTIVITY TOMOGRAPHY MEASUREMENTS

机译:通过集成的微匍匐垂直梯度和电阻率断层扫描测量确定近表面洞的地球物理性质

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摘要

Vertical-gradient microgravity and electrical-resistivity tomography geophysical surveys were performed over a shallow cave in the Italian Armetta Mountain karst area, close to the Liguria-Piedmont watershed. The aim of this study was to test the geophysical response of a known shallow cave. The shallowest portion of the cave exhibits narrow passages and, at about 30 meters below the entrance, a fossil meander linking two large chambers, the target of the geophysical survey. The integrated results of the two surveys show a clear geophysical response to the cave. The surveys exhibited high resistivity values and a negative gravity anomaly over the large cave passages. This work confirms the ability of these geophysical techniques to give the precise location of the voids, even in complex environments. The application of these techniques can be successful for site surveying where the presence of hollows may be expected.
机译:垂直梯度微痛和电阻率断层扫描地球物理调查是在意大利扶手椅喀斯特地区的浅洞内进行的,靠近利古里亚 - 皮埃蒙特流域。 本研究的目的是测试已知浅层洞穴的地球物理反应。 洞穴的最浅部分呈现狭窄的通道,并且在入口下方约30米处,一个化石蜿蜒连接两个大腔室,是地球物理调查的目标。 两种调查的综合结果显示对洞穴的明显地球物理反应。 调查在大洞穴通道上表现出高电阻率值和负重异常。 这项工作确认了这些地球物理技术的能力,即使在复杂的环境中也能提供空隙的精确位置。 这些技术的应用可以成功地对现场测量来说,可以预期空洞的存在。

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