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莱芜盆地岩溶地下水富集规律

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基于在莱芜盆地开展的水文地质调查与泉水保护工作,通过资料收集、野外地质调查、水文地质钻探及岩矿测试,对区内碳酸盐岩岩溶发育特征及富水规律进行研究.结果表明:莱芜盆地碳酸盐岩分布受构造控制明显,集中分布在盆地南部,呈单斜状产出,在盆地北缘、东缘地区零星分布;岩溶发育受地层岩性、地质构造、地下水动力条件及岩浆侵入等多因素影响;地表岩溶形态以溶沟、溶槽为主,地下岩溶以溶蚀裂隙、溶孔溶洞为主,主要发育 400 m以浅;岩溶水主要富集在多期构造断块区域、阻水断裂形成的上盘、地下水承压排泄区及莱芜矿山背斜两翼岩溶发育区.研究结果可为鲁中南缺水山区地下水资源开发与利用提供科学技术支撑.
Karst groundwater enrichment law in Laiwu Basin
[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 Basinkarstificationgroundwaterenrichment patternhydrogeololgy

李波、于大潞、王楠、毕雯雯、高帅、胥芹、王昱玮、侯芃

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山东省地质矿产勘查开发局八〇一水文地质工程地质大队,山东济南 250014

山东省地下水环境保护与修复工程技术研究中心,山东济南 250014

山东省地矿工程勘察院,山东济南 250014

山东省水工环地质工程有限公司,山东济南 250014

山东省地矿物资有限公司,山东济南 250014

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莱芜盆地 岩溶发育 地下水 富集规律 水文地质

国家自然科学基金项目山东省地质勘查项目

42202294鲁勘字201844号

2024

地质力学学报
中国地质科学院地质力学研究所

地质力学学报

CSTPCD北大核心
影响因子:0.5
ISSN:1006-6616
年,卷(期):2024.30(4)