基于氢氧稳定同位素的喀斯特泉水补给来源分析

毛龙富; 付舒; 刘宏; 周恩民; 岳兰; 杨丽瑞; 张净净

doi:10.3799/dqkx.2021.149

Volume 48 Issue 9

Sep. 2023

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Article Navigation > Earth Science > 2023 > 48(9): 3480-3493

Mao Longfu, Fu Shu, Liu Hong, Zhou Enmin, Yue Lan, Yang Lirui, Zhang Jingjing, 2023. Analysis of Recharge Source of Karst Spring Water Based on Stable Hydrogen and Oxygen Isotopes. Earth Science, 48(9): 3480-3493. doi: 10.3799/dqkx.2021.149

Citation:

Mao Longfu, Fu Shu, Liu Hong, Zhou Enmin, Yue Lan, Yang Lirui, Zhang Jingjing, 2023. Analysis of Recharge Source of Karst Spring Water Based on Stable Hydrogen and Oxygen Isotopes. Earth Science, 48(9): 3480-3493. doi: 10.3799/dqkx.2021.149

Citation:

Mao Longfu, Fu Shu, Liu Hong, Zhou Enmin, Yue Lan, Yang Lirui, Zhang Jingjing, 2023. Analysis of Recharge Source of Karst Spring Water Based on Stable Hydrogen and Oxygen Isotopes. Earth Science, 48(9): 3480-3493. doi: 10.3799/dqkx.2021.149

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Analysis of Recharge Source of Karst Spring Water Based on Stable Hydrogen and Oxygen Isotopes

doi: 10.3799/dqkx.2021.149

Mao Longfu^{1, 2
,
,},
Fu Shu^{1, 2},
Liu Hong^{1, 2
,
,
,},
Zhou Enmin^{1, 2},
Yue Lan³,
Yang Lirui^{1, 2},
Zhang Jingjing^{1, 2}

1.
School of Earth Sciences, Yunnan University, Kunming 650500, China
2.
International Joint Research Center for Karstology, Yunnan University, Kunming 650223, China
3.
School of Geographical Sciences, China West Normal University, Nanchong 637009, China

Received Date: 2021-07-02
Available Online: 2023-10-07
Publish Date: 2023-09-25

Abstract

Abstract

In order to explore the recharge mechanism of karst spring. Based on the data of hydrogen and oxygen stable isotopes monitored from April 2017 to December 2020 in Huanglong spring catchment monitored from April 2017 to December 2020, the models of unary linear regression, multiple linear regression, and trigonometric regression were used to explore the characteristics of hydrogen and oxygen stable isotopes, hydrology, and conductivity changes in the spring waters and their coupling relationships to reveal the process of spring recharge sources. The results show that: (1) The δD and δ¹⁸O values of spring water and river water were greater in the wet period than in the dry period, and the δD and δ¹⁸O values of cave drip water and stream water were similar to the stable isotope value of regional atmospheric precipitation, which were greater in the dry period than in the wet period. (2) The d-excess values of the spring catchment were greater in the wet period than in the dry period, and the water level, δD, δ¹⁸O and conductivity of the spring produced a seasonal coupling response to precipitation, and the recharge process of spring was influenced by the "piston effect" of the karst system and the "dilution effect" of the precipitation. (3) The seasonal characteristics of δD and δ¹⁸O of cave drips show that the drips inside the cave were larger than those near the cave entrance; the time sequence of troughs in the δD cosine function of the spring domain: stream water > cave drips > river water > spring water, and the response time to atmospheric precipitation was successively delayed. (4) The spring was recharged by the perennial mixture of infiltration of atmospheric precipitation and the weathering fissure water flowing from non-karst areas. The analyses of the characteristics of hydrogen and oxygen isotopes, hydrologic dynamics, runoff process and recharge mechanism in karst region have important reference significance for the control, management and protection of water resources in karst area.
- karst,
- springs,
- hydrogen and oxygen stable isotopes,
- recharge mechanisms,
- Huanglong spring catchment,
- hydrogeology

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References(59)

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