Investigating the structure of a multiple karst aquifer system and its hydrological process response using high-resolution multi-tracer data

被引:0
|
作者
Ji, Huaisong [1 ,2 ]
Chiogna, Gabriele [2 ]
Chang, Wei [3 ]
Richieri, Beatrice [2 ,4 ]
Chen, Lin [5 ]
Luo, Mingming [1 ]
Guo, Xulei [1 ]
Huang, Kun [1 ]
机构
[1] China Univ Geosci, Sch Environm Studies, Wuhan 430078, Hubei, Peoples R China
[2] Friedrich Alexander Univ Erlangen Nurnberg FAU, Dept Geog & Geosci, GeoZentrum Nordbayern, Schlossgarten 5, D-91054 Erlangen, Germany
[3] Changjiang Geotech Engn Ltd, Wuhan 430010, Hubei, Peoples R China
[4] Tech Univ Dresden, Inst Groundwater Management IGW, Bergstr 66, D-01069 Dresden, Germany
[5] Sichuan Elect Power Co Ltd, State Power Investment Corp, Chengdu 610200, Sichuan, Peoples R China
基金
中国国家自然科学基金;
关键词
Multiple karst aquifer systems; High-resolution multi-tracer; Hydrological process; Conductivity decomposition method; FLOW SYSTEMS; GROUNDWATER; SPRINGS; WATER; BEHAVIOR; RAINFALL; PATH; AREA;
D O I
10.1016/j.jhydrol.2025.133152
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
Understanding the hydrogeological structure and hydrogeochemical processes of karst aquifers is critical for groundwater management. This study innovatively integrates drilling, tracer tests, high-resolution monitoring, and multi-isotope techniques (H-3, C-14, delta D, delta O-18) to systematically characterize the spatial heterogeneity of a multiple karst aquifer system. Hydrochemical data was analyzed with the electrical conductivity decomposition method. Multivariate statistical analysis and the ions ratio are used to identify the sources and components of the spring water during storm events. The results indicate that: (1)The upper and lower aquifer systems are composed of limestone and dolomite, respectively, while the intermediate aquifer system is constituted by both limestone and dolomite. The upper and intermediate aquifer systems exhibit conduit flow regimes, whereas the lower aquifer is characterized by fracture flow. The lower aquifers (similar to 13,862-year residence time) show unique SO42-, Sr2+, F- enrichment and lighter delta D/delta O-18 signatures, reflecting prolonged water-rock interactions. (2) Comparative analyses of ion ratios during storm events in the BLD spring, demonstrate that both limestone and dolomite significantly influence the spring hydrochemistry. The hydrochemistry changes in the spring outlet are caused by dilution and mixing of recharge from limestone and dolomite aquifers, triggered by rainfall. During rainstorm events, the dolomite aquifer is the primary source of recharge. (3) The study establishes a "structure-process-evolution" conceptual model, demonstrating how multi-tracer synergy resolves hydrological complexity in heterogeneous karst systems. Our study highlights the importance of collecting and interpreting high-resolution multi-tracer datasets to unravel the dynamics of hydrological processes in complex multiple karst aquifer systems.
引用
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页数:16
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