摘要
表层岩溶带是岩溶学研究的重要部分,其结构的解译对表层岩溶带水循环特征及岩溶水调蓄功能的研究具有重要意义。利用综合物探方法(包括高密度电阻率法、自然电位法和地质雷达法),对平果市果化镇生态试验基地坡径流场的表层岩溶带空间结构特征进行了探测解译。通过对高密度电阻率数据和自然电位数据反演,获得坡径流场若干电阻率断面和极化源的空间分布特征,解译了3处强径流带发育的空间位置;通过地质雷达影像图划分了表层岩溶带发育深度。此外,坡径流场地西北侧有深部岩溶裂隙发育,向东南地势逐渐走低,岩溶裂隙也逐渐向面上扩大。研究结果表明,自然电位法是探测岩溶含水构造的有效方法,结合高密度电阻率法,可有效解译强径流带的空间发育位置,而地质雷达法可高分辨地探测表层岩溶带的发育厚度和浅部岩溶裂隙的发育情况;地质雷达法、高密度电阻率法和自然电位法的综合应用能有效探测表层岩溶带的结构特征,是解译表层岩溶带厚度和探测强径流带空间分布的有效手段。
The epikarst zone is widely distributed in the karst area of Southwest China,and it is the intersection zone of four circles(lithosphere,atmosphere,biosphere and hydrosphere).It is sensitive to environmental changes,in which rapid chemical reactions and strong karst actions are likely to take place.It records much information on short-term environmental change.It also has the function of regulating and storing karst water,and thus can effectively provide water resources for residents in karst mountainous areas.Therefore,the exploration and interpretation of the structure of epikarst zone is of great significance to the study of water cycle and the storage function of epikarst zone.In this study,comprehensive geophysical methods such as high-density resistivity method,spontaneous potential method and ground penetrating radar method have been used to explore and interpret the spatial structure characteristics of epikarst zone in slope runoff field of Guohua town ecological experiment base in Pingguo City.The high-density resistivity method can obtain the electrical structure section of slope runoff field by data inversion,and divide karst development areas by electrical structure.As an important method to interpret the development position of strong runoff belt,the spontaneous potential method can obtain the spatial position of polarization source through data inversion,and the generation of polarization source is closely related to water flow and electrochemical reaction between water and surrounding rock.With high resolution,the ground penetrating radar method is effective to interpret the development thickness of epikarst zone.The high-density resistivity method and the spontaneous potential method can be used to detect and comprehensively interpret the spatial position of the strong runoff belt in slope runoff field,and the ground penetrating radar method can be used to detect the thickness of the epikarst zone in the slope runoff field.In this study,according to the resistivity inversion cross-section and pola
作者
刘永亮
刘振宇
章程
吴秋菊
邬健强
张伟
甘伏平
韩凯
LIU Yongliang;LIU Zhenyu;ZHANG Cheng;WU Qiuju;WU Jianqiang;ZHANG Wei;GAN Fuping;HAN Kai(Institute of Karst Geology,CAGS/Key Laboratory of Karst Dynamics,MNR&GZAR,Guilin,Guangxi 541004,China;International Research Center on Karst Under the Auspices of UNESCO/National Center for International Research on Karst Dynamic System and Global Change,Guilin,Guangxi 541004,China;Geological Environment Monitoring Station of Guangxi Zhuang Autonomous Region,Nanning,Guangxi 530201,China;Wuhan Center of Geological Survey(Central South China Innovation Center for Geosciences),Wuhan,Hubei 430205,China)
出处
《中国岩溶》
CAS
CSCD
北大核心
2024年第1期209-218,共10页
Carsologica Sinica
基金
广西重点研发计划项目(桂科AB21075002)
广西重点研发项目(桂科AB23026062)
广西壮族自治区地质环境监测站项目(桂自然资函【2021】415)
中国地质科学院岩溶地质研究所基本科研业务费项目(2021007,2022002)。
关键词
地球探测与信息技术
表层岩溶带
空间结构
地质雷达
高密度电阻率
自然电位
earth exploration and information technology
epikarst zone
spatial structure
ground penetrating radar
high-density resistivity
spontaneous potential
