典型岩溶槽谷区土壤水和地下水氢氧稳定同位素对隧道建设的响应

邱菊; 蒋勇军; 吕同汝; 茆杨; 吴泽; 马丽娜; 汪啟容; 张彩云

doi:10.3799/dqkx.2021.008

Volume 47 Issue 2

Feb. 2022

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Qiu Ju, Jiang Yongjun, Lv Tongru, Mao Yang, Wu Ze, Ma Lina, Wang Qirong, Zhang Caiyun, 2022. Response of Stable Isotopes of Hydrogen and Oxygen in Soil Water and Groundwater to Tunnel Construction in Typical Karst trough Valley. Earth Science, 47(2): 717-728. doi: 10.3799/dqkx.2021.008

Citation:

Qiu Ju, Jiang Yongjun, Lv Tongru, Mao Yang, Wu Ze, Ma Lina, Wang Qirong, Zhang Caiyun, 2022. Response of Stable Isotopes of Hydrogen and Oxygen in Soil Water and Groundwater to Tunnel Construction in Typical Karst trough Valley. Earth Science, 47(2): 717-728. doi: 10.3799/dqkx.2021.008

Citation:

Qiu Ju, Jiang Yongjun, Lv Tongru, Mao Yang, Wu Ze, Ma Lina, Wang Qirong, Zhang Caiyun, 2022. Response of Stable Isotopes of Hydrogen and Oxygen in Soil Water and Groundwater to Tunnel Construction in Typical Karst trough Valley. Earth Science, 47(2): 717-728. doi: 10.3799/dqkx.2021.008

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Response of Stable Isotopes of Hydrogen and Oxygen in Soil Water and Groundwater to Tunnel Construction in Typical Karst trough Valley

doi: 10.3799/dqkx.2021.008

Chongqing Key Laboratory of Karst Environment, School of Geographical Sciences, Southwest University, Chongqing 400715, China

Received Date: 2021-11-01
Publish Date: 2022-02-25

Abstract

Abstract

The construction of the tunnel caused changes in the groundwater flow field, which seriously affected the process of regional water migration. Taking the karst trough of Zhongliang Mountain in Chongqing as an example, we collected precipitation, soil water, groundwater and tunnel drainage from April 2017 to April 2019. This study used stable hydrogen and oxygen isotopes to analyze the soil water and groundwater migration processes in the tunnel-affected zone and non-tunnel-affected zone, and explored the impact of tunnel construction on it.The results showed that the change of δ²H and δ¹⁸O of soil water in the tunnel-affected area was greater than that of the tunnel-affected area, and the change of groundwater δ²H and δ¹⁸O was more stable than that of the non-tunnel-affected area.Compared with the soil water and groundwater in the non-tunnel-affected area, the δ²H and δ¹⁸O of the shallow soil water in the tunnel-affected area were heavier in summer, the δ²H and δ¹⁸O of deep soil were heavier in autumn, the δ²H and δ¹⁸O of shallow karst spring water were basically heavier in all seasons, and the underground river water was δ²H and δ¹⁸O tends to be heavier in winter, and the δ²H and δ¹⁸O of water bodies in other seasons were basically lighter. The difference of meantransit time and young water fraction between the tunnel-affected zone and the non-tunnel-affected zone gradually decreased from soil water to groundwater.The meantransit time of soil water in the tunnel-affected area was 25.4 days shorter than that in the non-tunnel-affected area, the young water fraction was 13.5% higher, the meantransit time of groundwater was 16.1 days less, and the young water fraction was 3.4% higher.To sum up, the tunnel construction accelerated the water movement speed in the tunnel-affected zone to a certain extent, resulting in the reduction of retained water in the soil layer and the weakening of water mixing.
- stable hydrogen and oxygen isotopes,
- water movement,
- tunnel construction,
- Karst trough valley,
- hydrogeology

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Response of Stable Isotopes of Hydrogen and Oxygen in Soil Water and Groundwater to Tunnel Construction in Typical Karst trough Valley

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