宜昌潮水洞岩溶间歇泉动态特征及成因

郭绪磊; 陈乾龙; 黄琨; 周宏

doi:10.3799/dqkx.2020.138

Volume 45 Issue 12

Dec. 2020

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Guo Xulei, Chen Qianlong, Huang Kun, Zhou Hong, 2020. Dynamic Features and Causes of Chaoshuidong Siphonal Spring. Earth Science, 45(12): 4524-4534. doi: 10.3799/dqkx.2020.138

Citation:

Guo Xulei, Chen Qianlong, Huang Kun, Zhou Hong, 2020. Dynamic Features and Causes of Chaoshuidong Siphonal Spring. Earth Science, 45(12): 4524-4534. doi: 10.3799/dqkx.2020.138

Guo Xulei, Chen Qianlong, Huang Kun, Zhou Hong, 2020. Dynamic Features and Causes of Chaoshuidong Siphonal Spring. Earth Science, 45(12): 4524-4534. doi: 10.3799/dqkx.2020.138

Citation:

Guo Xulei, Chen Qianlong, Huang Kun, Zhou Hong, 2020. Dynamic Features and Causes of Chaoshuidong Siphonal Spring. Earth Science, 45(12): 4524-4534. doi: 10.3799/dqkx.2020.138

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Dynamic Features and Causes of Chaoshuidong Siphonal Spring

doi: 10.3799/dqkx.2020.138

Guo Xulei^{1
,
,},
Chen Qianlong²,
Huang Kun¹,
Zhou Hong^{2
,
,}

1.
School of Environmental Studies China University of Geosciences, Wuhan 430078, China
2.
Institute of Geological Survey, China University of Geosciences, Wuhan 430074, China

Received Date: 2020-04-29
Publish Date: 2020-12-15

Abstract

Abstract

The Chaoshuidong Siphonal Spring () is in Yichang City, Hubei Province, which could still regularly intermittently flows out when there is no rain. Systematic research into the flow and hydrochemical dynamics and formation mechanisms of CSS is lacked. Based on long-term hydrological and meteorological observation data and hydrochemical test data, in this paper, it analyzes and summarizes the changes in the flow, water temperature and conductivity of the CSS at different times, and also analyzes the hydrochemical characteristics of the CSS karst water system. The CSS karst water system can be divided into the local water flow system of the Shilongdong Group and the intermediate water flow system of the Tianheban Group, and its dynamic characteristics can be divided into two distinct periods of rain and rain-free periods, which reflects the rapid response of karst water system to rainfall and the control function of karst siphon pipe to the intermediate water flow system of Tianheban Group, respectively.There are many intermittent flow out of multiple unstable cycles during the rain-free period. The source of intermittent discharge groundwater was identified by ion ratio method and the analysis of hydrodynamic features as the Tianheban Group rock aquifer, and with the increasing process flow, the proportion of deep-cycle groundwater reached 97%. Finally, combined with hydrogeological condition analysis, in the paper it summarizes the conceptual pattern map of water circulation in the CSS karst water system, and the development of the siphon pipe inside the gray rock aquifer of the Tianheban Group forms the characteristics of the water circulation during the rain and rain-free periodof the CSS.
- Chaoshuidong Siphonal Spring (CSS),
- dynamic feature of spring,
- the ion ratio method,
- storage capacity,
- hydrogeology

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