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桂南陇瑞洼地浅层岩溶自然电场特征剖析

陈贻祥 蒋莹 覃小群 黄奇波 甘伏平 韩凯 郑智杰 贺德煌 黄德健 付昱

中国岩溶2018,Vol.37Issue(1):130-138,9.
中国岩溶2018,Vol.37Issue(1):130-138,9.DOI:10.11932/karst2017y36

桂南陇瑞洼地浅层岩溶自然电场特征剖析

Analysis of the characteristicsof self-potential anomalous in shallow karst area of Longrui valley,southern Guangxi,China

陈贻祥 1蒋莹 2覃小群 1黄奇波 1甘伏平 1韩凯 1郑智杰 1贺德煌 1黄德健 1付昱2

作者信息

  • 1. 中国地质科学院岩溶地质研究所/自然资源部、广西岩溶动力学重点实验室,广西桂林541004
  • 2. 广西壮族自治区三一○核地质大队,广西桂林541213
  • 折叠

摘要

Abstract

Under the influence of osmotic pressure,the seepage water flow filtered by depressions soil in karst valley,gradually infiltrate downward and finally discharge to karst conduits or underground river through upper karst erosion networks or karst fissures.In this process,the spontaneous polarization phenomenon or self-potential field will form by the ionic conductive materials.Therefore,the study on self-potential can be applied to explore shallow groundwater in karst valley.The study results showed that the selfpotentials banded anomalies ranging from-60~-80 mv with about 40 m wide and extending from north to south with "S" shape have been observed just near the center of Longrui karst valley.On the plane view,the self-potential gradient contours present "zero" value anomalies varying from negative to positive near the top of the karst zones.The spatialdistribution of the "zero" value anomalous zones indicates the surface differences and changes of shallow karst development.Taking Line 18 as an example,the self-potentials caused by shallow karst seepage water in Longrui valley follow thepotential function distribution,namely the self-potentials have reached the minimum and accordingly self-potential gradients vary from negative to positive with the shape of central symmetry which shows the "zero" value just near the top of the shallow karst zones (station 615).The self-potentials on either side of the minimum gradually weaken until go to zero due to the stations moving away from the karst zone.Shallow caves,dissolved-fissures and fault fractures were exposed at different depths by the hydrogeologic monitoring borehole.Thus it means that the self-potential can be used as an effective geophysical method for detecting shallow karst water.

关键词

岩溶洼地/浅层岩溶/自然电场/异常特征/探测效果

Key words

karst valley/shallow karst/self-potential method/anomalous characteristics/detection effect

分类

天文与地球科学

引用本文复制引用

陈贻祥,蒋莹,覃小群,黄奇波,甘伏平,韩凯,郑智杰,贺德煌,黄德健,付昱..桂南陇瑞洼地浅层岩溶自然电场特征剖析[J].中国岩溶,2018,37(1):130-138,9.

基金项目

国家自然科学基金项目(41572232) (41572232)

中国地质调查局项目(DD20160301) (DD20160301)

中国地质科学院基本科研项目(YYWF201640) (YYWF201640)

中国地质科学院基本科研项目(YYWF201643) (YYWF201643)

中国岩溶

OA北大核心CSCDCSTPCD

1001-4810

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