An analysis of the characteristics of water storage structure and the practice of groundwater exploration in the basalt area of Zhangbei County, Bashang, Hebei Province

DENG Qijun; LI Wei; ZHU Qingjun; MA Xuemei; HE Jin; MA Xuejun; LUO Xuan

2020 Vol. 39, No. 12

Article Contents

Article navigation > Geological Bulletin of China > 2020 > 39(12): 1899-1907

Next Article Previous Article

DENG Qijun, LI Wei, ZHU Qingjun, MA Xuemei, HE Jin, MA Xuejun, LUO Xuan. An analysis of the characteristics of water storage structure and the practice of groundwater exploration in the basalt area of Zhangbei County, Bashang, Hebei Province[J]. Geological Bulletin of China, 2020, 39(12): 1899-1907.

Citation:

DENG Qijun, LI Wei, ZHU Qingjun, MA Xuemei, HE Jin, MA Xuejun, LUO Xuan. An analysis of the characteristics of water storage structure and the practice of groundwater exploration in the basalt area of Zhangbei County, Bashang, Hebei Province[J]. Geological Bulletin of China, 2020, 39(12): 1899-1907.

An analysis of the characteristics of water storage structure and the practice of groundwater exploration in the basalt area of Zhangbei County, Bashang, Hebei Province

Center for Hydrogeology and Environmental Geology Survey, CGS, Baoding 071051, Hebei, China

More Information

Corresponding author: HE Jin, hejing007105@126.com

Received Date: 15 August 2020

Revised Date: 20 October 2020

Publish Date: 25 December 2020

Abstract

Abstract

Zhangbei County is located in the contiguous poverty-stricken area of Yanshan Mountain-Taihang Mountain.The geological conditions of the basalt area are complex, which makes it difficult to find groundwater, and hence water-shortage villages are commonly existent.Based on field survey, theoretical analysis and analysis of typical groundwater exploration examples, the authors investigated the water storage structures types in the basalt area and their water-enrichment factors and summarized three types of water storage structures in this area, i.e., monoclinic structure, fault structure, and large holes.The monoclinal water storage structure can be subdivided into platform type, plain buried type, volcanic cone type and valley type according to the basalt exposure conditions.In terms of the influencing factors of water-enrichment, the monoclinic water storage structure is mainly related to the connectivity of basalt holes and fissures as well as the lithology and structure of the clastic rocks in basalt.The fault structure type water storage structure is greatly affected by the mechanical properties of faults and the later activity of the faults.Tensional faults and the newly active faults have good water conductivity and water enrichment capacity.The water storage space of the large hole type water storage structure is huge and hence the water-enrichment is very good.The influence factors of water enrichment are mainly related to the size and connectivity of basalt caverns.The results play a significant role for improving the success rate of finding groundwater in basalt areas so as to solve the problem of drinking water safety for water shortage people.
- Zhangbei County /
- basalt /
- water storage structures /
- groundwater exploration /
- Hebei Province

FullText(HTML)

References

[1]	刘光亚.基岩蓄水构造的理论与实践[J].河北地质学院学报, 1981, (4):28, 50-56. Google Scholar
[2]	肖楠森, 高明.论新构造运动对地下水资源分布的控制作用[J].工程勘察.1982, (4).1-6. Google Scholar
[3]	袁文波.近代地壳运动对基岩裂隙水的控制作用研究[D].南京大学硕士学位论文, 2018. Google Scholar
[4]	Kulkarni H, Deolankar S B, Lalwani A, et al.Hydrogeological framework of the Deccan basalt groundwater systems, west-central India[J].Hydrogeology Journal, 2000, 8:368-378. doi: 10.1007/s100400000079 CrossRef Google Scholar
[5]	Lau M.Hydrology of the Hawaiian Islands[M].Honolulu:University of Hawaii Press, 2006. Google Scholar
[6]	Fernandes A J, Maldaner C H, Negri F, et al.Aspects of a conceptual groundwater flow model of the Serra Geral basalt aquifer(Sao Paulo, Brazil)from physical and structural geology data[J].Hydrogeology Journal, 2016, 24(5):1199-1212. doi: 10.1007/s10040-016-1370-6 CrossRef Google Scholar
[7]	刘光亚, 谭绩文, 孙德佩.汉诺坝玄武岩的时代归属[J].河北地质学院学报, 1978, (2):32-46. Google Scholar
[8]	谭绩文, 刘亚民.汉诺坝玄武岩次生洞穴形成条件及其水文地质特征[J].河北地质学院学报, 1983, (3):23-35. Google Scholar
[9]	贾福海.中国玄武岩地下水[M].北京:地质出版社, 1993:47-62. Google Scholar
[10]	李巨芬, 李伟, 冯庆达, 等.山东临朐盆地新构造运动特征及其对地下水的控制作用[J].水文地质工程地质, 2020, 47(1):28-36. Google Scholar
[11]	莫若平, 邵显珉, 赵延庆.内蒙古锡盟地区新生代玄武岩地下水富集规律探讨[J].内蒙古煤炭经济, 2002, (6):70-72. Google Scholar
[12]	刘国兴, 冯文丽, 姜志刚, 等.玄武岩地区地下水资源富水性影响因素分析[J].水资源研究, 2010, (4):5-7. Google Scholar
[13]	曹新文, 马秀敏, 彭华, 等.山东蓬莱玄武岩覆盖区高密度电法找水效果分析[J].地球物理学进展, 2018, 33(6):2528-2534. Google Scholar
[14]	罗旋, 朱庆俊, 于蕾, 等.综合电法在张北县玄武岩孔洞水勘查中的应用[J].地质调查与研究, 2020, 43(3):251-258. Google Scholar
[15]	闫永福.冀西北坝上新构造运动[J].华北地质矿产杂志, 1998, (2):3-5. Google Scholar
[16]	王行军, 王德强, 班长勇, 等.冀西北康保、沽源一带新构造运动特征[J].地质调查与研究, 2006, (1):38-46. Google Scholar
[17]	万天丰.中国大地构造学[M].北京:地质出版社, 2011:202-246. Google Scholar
[18]	蔡华昌, 张四昌, 张振江, 等.张北地震区的断裂构造特征[J].华北地震科学, 2002, (2):1-9. Google Scholar