Karst groundwater enrichment law in Laiwu Basin

LI Bo; YU Dalu; WANG Nan; BI Wenwen; GAO Shuai; XU Qin; WANG Yuwei; HOU Peng

doi:10.12090/j.issn.1006-6616.2023166

Volume 30 Issue 4

Aug. 2024

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LI B，YU D L，WANG N，et al.，2024. Karst groundwater enrichment law in Laiwu Basin[J]. Journal of Geomechanics，30（4）：691−702 doi: 10.12090/j.issn.1006-6616.2023166

Citation:

LI B，YU D L，WANG N，et al.，2024. Karst groundwater enrichment law in Laiwu Basin[J]. Journal of Geomechanics，30（4）：691−702 doi: 10.12090/j.issn.1006-6616.2023166

Citation:

LI B，YU D L，WANG N，et al.，2024. Karst groundwater enrichment law in Laiwu Basin[J]. Journal of Geomechanics，30（4）：691−702 doi: 10.12090/j.issn.1006-6616.2023166

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Karst groundwater enrichment law in Laiwu Basin

doi: 10.12090/j.issn.1006-6616.2023166

LI Bo^{1, 2, 3
,},
YU Dalu^{1, 2, 3},
WANG Nan^{1, 2, 3
,
,},
BI Wenwen^{1, 2, 3},
GAO Shuai^{1, 2, 3},
XU Qin⁴,
WANG Yuwei^{1, 2, 3},
HOU Peng⁵

1.
801 Institute of Hydrogeology and Engineering Geology, Shandong Provincial Bureau of Geology & Mineral Resources, Jinan 250014, Shandong, China
2.
Shandong Engineering Research Center for Environmental Protection and Remediation on Groundwater, Jinan 250014, Shandong, China
3.
Shandong Provincial Geo-mineral Engineering Exploration Institute, Jinan 250014, Shandong, China
4.
Shandong Hydrogeology Engineering Geologyand Environment Geology Corporation, Jinan 250014, Shandong, China
5.
Shandong Geology and Mineral Resources Materials Corporation, Jinan 250014, Shandong, China

Funds: This research is financially supported by National Natural Science Foundation of China (Grant No. 42202294) and the Geological Exploration Project of Shandong Province (Grant No. Lukanzi (2018) 44).

More Information

Received: 2023-10-10
Revised: 2024-04-28
Accepted: 2024-04-30

Available Online: 2024-05-15

Published: 2024-08-28

Abstract

Abstract

Objective The Laiwu Basin is a typical monocline fault basin in the central and southern regions of Shandong Province. It has a complex geological structure and an uneven distribution of groundwater resources within the region. Previous researchers have conducted a large number of hydrogeological and spring water protection studies, but no relevant research has been conducted on the relationship between the development laws of fissure karst and the distribution of karst groundwater. Methods In this study, karstification and groundwater enrichment characteristics were investigated in the Laiwu Basin through research methods of data collection, field geological surveys, hydrogeological drilling, and rock and mineral testing. Results Carbonate strata are concentrated in the southern part of the Laiwu Basin, with a monoclinal structure controlled by the geological structure, which is scattered sporadically in the northern and eastern regions. Karst development is affected by many factors, such as formation lithology, geological structure, groundwater dynamic conditions, and magma intrusion. The principal surface karst features are grikes and karst valleys. In addition, the principal underground karst features were dominated by dissolution fissures and holes at 400 m depth. Karst groundwater is primarily concentrated in multistage structural fault basins, hanging walls formed by water-blocking faults, groundwater pressure discharge areas, and karst development areas on the anticlinal flank of the mine. Conclusion The karst water cycle in the Laiwu Basin has a general regularity of monoclinic basins but is influenced by multiple factors, forming karst water systems of varying sizes that are relatively independent. Significant differences were observed in the development characteristics and water abundance patterns of karsts in different regions. Fault structures and geological water-blocking areas have relatively abundant karst water, whereas the shallow karst water has a strong runoff cycle. [ Significance ] This study provides scientific and technical support for the exploitation and utilization of groundwater resources in water-scarce mountainous areas of central and southern Shandong Province.
- Laiwu Basin,
- karstification,
- groundwater,
- enrichment pattern,
- hydrogeololgy

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