Tracing groundwater discharge into a coal mining subsidence lake in eastern China: Observations from water stable (δD and δ18O) and radon (222Rn) isotopes
Many coal mining subsidence lakes have formed in eastern China due to underground coal mining. Lacustrine groundwater discharge (LGD) is of great importance to the hydrological cycle and the eco-environment of lakes. However, LGD in coal mining area is rarely reported. In the study, we quantified gr...
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| Published in | Applied geochemistry Vol. 156; p. 105757 |
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| Main Authors | , , , , , |
| Format | Journal Article |
| Language | English |
| Published |
Elsevier Ltd
01.09.2023
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| Subjects | |
| Online Access | Get full text |
| ISSN | 0883-2927 1872-9134 |
| DOI | 10.1016/j.apgeochem.2023.105757 |
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| Abstract | Many coal mining subsidence lakes have formed in eastern China due to underground coal mining. Lacustrine groundwater discharge (LGD) is of great importance to the hydrological cycle and the eco-environment of lakes. However, LGD in coal mining area is rarely reported. In the study, we quantified groundwater discharge into a Huainan coal mining subsidence lake (China) using water stable (D and 18O) and radioactive (222Rn) isotopes. 222Rn and 18O mass balance models were used to independently estimate LGD. The lake water was sampled based on the horizontal and vertical profile sampling. The isotope depth profiles were weighted according to the lake bathymetry to obtain a representative isotope inventory by geographic information system (GIS) analysis. The LGD rates estimated from two models were comparable, and the values were 18 mm d−1 for the 18O and 14 ± 8 mm d−1 for the 222Rn. Compared with the LGD of Ammelshainer See lake (Germany), a subsidence lake formed by coal mining, the LGD in the study was larger, which may be related to the different hydrological conditions in different areas. By integrating the LGD rates from these two models, this study quantitatively analyzed the role of groundwater in maintaining the water balance in subsidence lakes, which is of great significance to water resources assessment and sustainable utilization of coal mining subsidence lakes in eastern China.
•Using radioactive and stable isotopes to estimate LGD rate of the coal mining subsidence lake.•Combining horizontal and vertical sampling improves the accuracy of radon decay loss assessment.•Isotope depth profile is weighted to obtain representative isotope inventory.•Groundwater discharge contributes a large amount of water to coal mining subsidence lakes. |
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| AbstractList | Many coal mining subsidence lakes have formed in eastern China due to underground coal mining. Lacustrine groundwater discharge (LGD) is of great importance to the hydrological cycle and the eco-environment of lakes. However, LGD in coal mining area is rarely reported. In the study, we quantified groundwater discharge into a Huainan coal mining subsidence lake (China) using water stable (D and 18O) and radioactive (222Rn) isotopes. 222Rn and 18O mass balance models were used to independently estimate LGD. The lake water was sampled based on the horizontal and vertical profile sampling. The isotope depth profiles were weighted according to the lake bathymetry to obtain a representative isotope inventory by geographic information system (GIS) analysis. The LGD rates estimated from two models were comparable, and the values were 18 mm d−1 for the 18O and 14 ± 8 mm d−1 for the 222Rn. Compared with the LGD of Ammelshainer See lake (Germany), a subsidence lake formed by coal mining, the LGD in the study was larger, which may be related to the different hydrological conditions in different areas. By integrating the LGD rates from these two models, this study quantitatively analyzed the role of groundwater in maintaining the water balance in subsidence lakes, which is of great significance to water resources assessment and sustainable utilization of coal mining subsidence lakes in eastern China.
•Using radioactive and stable isotopes to estimate LGD rate of the coal mining subsidence lake.•Combining horizontal and vertical sampling improves the accuracy of radon decay loss assessment.•Isotope depth profile is weighted to obtain representative isotope inventory.•Groundwater discharge contributes a large amount of water to coal mining subsidence lakes. Many coal mining subsidence lakes have formed in eastern China due to underground coal mining. Lacustrine groundwater discharge (LGD) is of great importance to the hydrological cycle and the eco-environment of lakes. However, LGD in coal mining area is rarely reported. In the study, we quantified groundwater discharge into a Huainan coal mining subsidence lake (China) using water stable (D and ¹⁸O) and radioactive (²²²Rn) isotopes. ²²²Rn and ¹⁸O mass balance models were used to independently estimate LGD. The lake water was sampled based on the horizontal and vertical profile sampling. The isotope depth profiles were weighted according to the lake bathymetry to obtain a representative isotope inventory by geographic information system (GIS) analysis. The LGD rates estimated from two models were comparable, and the values were 18 mm d⁻¹ for the ¹⁸O and 14 ± 8 mm d⁻¹ for the ²²²Rn. Compared with the LGD of Ammelshainer See lake (Germany), a subsidence lake formed by coal mining, the LGD in the study was larger, which may be related to the different hydrological conditions in different areas. By integrating the LGD rates from these two models, this study quantitatively analyzed the role of groundwater in maintaining the water balance in subsidence lakes, which is of great significance to water resources assessment and sustainable utilization of coal mining subsidence lakes in eastern China. |
| ArticleNumber | 105757 |
| Author | Wang, Qianqian Sadat-Noori, Mahmood Liu, Dou Jiang, Chenghong Li, Hailong Jiang, Chunlu |
| Author_xml | – sequence: 1 givenname: Chunlu surname: Jiang fullname: Jiang, Chunlu organization: School of Resources and Geosciences, China University of Mining and Technology, Xuzhou, Jiangsu, 221116, China – sequence: 2 givenname: Dou surname: Liu fullname: Liu, Dou organization: School of Resources and Environmental Engineering, Anhui University, Anhui Province Engineering Laboratory for Mine Ecological Remediation, Hefei, Anhui, 230601, China – sequence: 3 givenname: Chenghong surname: Jiang fullname: Jiang, Chenghong organization: School of Resources and Environmental Engineering, Anhui University, Anhui Province Engineering Laboratory for Mine Ecological Remediation, Hefei, Anhui, 230601, China – sequence: 4 givenname: Qianqian orcidid: 0000-0002-3022-7930 surname: Wang fullname: Wang, Qianqian email: wangqq@sustech.edu.cn organization: School of Environmental Science and Engineering, Southern University of Science and Technology, Shenzhen, Guangdong, 518055, China – sequence: 5 givenname: Mahmood surname: Sadat-Noori fullname: Sadat-Noori, Mahmood organization: Water Research Laboratory, School of Civil & Environmental Engineering, UNSW Sydney, NSW, 2052, Australia – sequence: 6 givenname: Hailong surname: Li fullname: Li, Hailong organization: School of Environmental Science and Engineering, Southern University of Science and Technology, Shenzhen, Guangdong, 518055, China |
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| SubjectTerms | 18O 222Rn China coal geochemistry geographic information systems Germany groundwater Groundwater discharge hydrologic cycle inventories Isotope inventory isotopes lakes Mining subsidence lake radon subsidence |
| Title | Tracing groundwater discharge into a coal mining subsidence lake in eastern China: Observations from water stable (δD and δ18O) and radon (222Rn) isotopes |
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