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| 基岩水与平原水转换关系的地球物理勘查技术探讨 | |
| 引用本文： | 武毅, 郭建强, 朱庆俊, 程旭学, 孙振洪. 基岩水与平原水转换关系的地球物理勘查技术探讨[J]. 地球学报, 2004, (3): 369-372. doi: 10.3321/j.issn:1006-3021.2004.03.016 |
| 作者姓名： | 武毅 郭建强 朱庆俊 程旭学 孙振洪 |
| 作者单位： | 中国地质大学，湖北武汉，430074; 中国地质调查局水文地质工程地质技术方法研究所，河北保定，071051;中国地质大学，湖北武汉，430074; 中国地质调查局水文地质工程地质技术方法研究所，河北保定，071051;中国地质调查局水文地质工程地质技术方法研究所，河北保定，071051;甘肃省水文地质工程地质勘查院，甘肃张掖，734000;保定市自来水总公司，河北保定，071051 |
| 基金项目： | 国土资源部2000年专项计划“西北地区水资源持续利用”项目之课题二(编号:20001030102) |
| 摘 要： | 基岩水与平原水转化关系的研究是搞清地表水与地下水转化途径、方式及流量进而进行水资源评价的一个重要内容.本文以河西走廊地区为例,分析了地球物理勘查技术对解决上述问题的可能性,同时结合该地区地质地貌特点,选用了EH-4电导率成像系统、自然电位法技术组合进行了实例勘查,取得了较好的效果,为前人的假说提供了科学依据,也为该内容的研究提供有效的手段. |
| 关 键 词： | 基岩水与平原水转化 地球物理勘查技术 实例效果 |
Geophysical Prospecting Techniques for the Interchange between Bedrock Water and Plain Water |
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| Geophysical Prospecting Techniques for the Interchange between Bedrock Water and Plain Water[J]. Acta Geoscientica Sinica, 2004, (3): 369-372. doi: 10.3321/j.issn:1006-3021.2004.03.016 | |
| Authors: | WU Yi GUO Jian-qiang ZHU Qing-jun CHENG Xu-xue SUN Zhen-hong |
| Affiliation: | China University of Geosciences, Wuhan, Hubei, 430074; Institute of Hydrogeological and Engineering Geological Technology, CGS, Baoding, Hebei, 071051;China University of Geosciences, Wuhan, Hubei, 430074; Institute of Hydrogeological and Engineering Geological Technology, CGS, Baoding, Hebei, 071051;Institute of Hydrogeological and Engineering Geological Technology, CGS, Baoding, Hebei, 071051;Gansu Institute of Hydrogeological and Engineering Geological Exploration, Zhangye, Gansu, 734000;Company of Water Supply of Baoding, Baoding, Hebei, 071051 |
| Abstract: | The interchange relationship between the bedrock groundwater and plain groundwater is an important research field in evaluating water resources. Nevertheless, none of the hypotheses on this relationship has been verified. With the Hexi Corridor as an example, this paper analyzes the possibility of using geophysical method to investigate such relationship and presents the results acquired by integrating the EH-4 electric conductivity imaging system with the natural potential method in accordance with the geological setting of this region. The good results obtained provide scientific evidence for the hypothesis of the previous workers. |
| Keywords: | interchange relationship between bedrock water and plain water geophysical technique the effect of a real case |
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