基于氚和CFCs的洞庭盆地浅层地下水年龄及循环更新研究

常致凯; 马斌; 李静; 梁杏; 付鹏宇; 曹明达; 张志鑫; 杜永昌

doi:10.3799/dqkx.2022.367

Volume 48 Issue 11

Nov. 2023

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Article Navigation > Earth Science > 2023 > 48(11): 4256-4269

Chang Zhikai, Ma Bin, Li Jing, Liang Xing, Fu Pengyu, Cao Mingda, Zhang Zhixin, Du Yongchang, 2023. Study on Age and Recycling of Shallow Groundwater Based on Tritium and CFCs in Dongting Basin. Earth Science, 48(11): 4256-4269. doi: 10.3799/dqkx.2022.367

Citation:

Chang Zhikai, Ma Bin, Li Jing, Liang Xing, Fu Pengyu, Cao Mingda, Zhang Zhixin, Du Yongchang, 2023. Study on Age and Recycling of Shallow Groundwater Based on Tritium and CFCs in Dongting Basin. Earth Science, 48(11): 4256-4269. doi: 10.3799/dqkx.2022.367

Citation:

Chang Zhikai, Ma Bin, Li Jing, Liang Xing, Fu Pengyu, Cao Mingda, Zhang Zhixin, Du Yongchang, 2023. Study on Age and Recycling of Shallow Groundwater Based on Tritium and CFCs in Dongting Basin. Earth Science, 48(11): 4256-4269. doi: 10.3799/dqkx.2022.367

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Study on Age and Recycling of Shallow Groundwater Based on Tritium and CFCs in Dongting Basin

doi: 10.3799/dqkx.2022.367

School of Environmental Studies, China University of Geosciences, Wuhan 430078, China

Received Date: 2022-06-06
Available Online: 2023-11-30
Publish Date: 2023-11-25

Abstract

Abstract

The contradiction between supply and demand of water resources in Dongting basin has become increasingly prominent. In order to evaluate the age, circulation and renewal of groundwater, 12 groups water samples of tritium (³H) and CFCs were collected from shallow groundwater in Zijiang basin of Dongting basin in 2021. The piston flow (PFM) model was used to calculate the ³H and CFCs ages of groundwater. The results show that the groundwater age in the study area gradually ages from the piedmont hilly area to the plain area. In the piedmont hilly area, the groundwater age is generally less than 40 years, the recharge ratio of fresh water was 96.36%-86.41%, the actual flow rate of groundwater is 2.18 m/d, and the groundwater circulation renewal was fast. The age of groundwater in plain area is above 50 years, the proportion of new water recharge is 37.09%, the actual groundwater flow rate is 1.2-1.59 m/d, and the infiltration flow rate is 0.000 8-0.001 2 m/d. The groundwater cycle renewal is slow. Combined with the regional hydrogeological conditions, the piedmont hilly area mainly developed local water flow system, and groundwater in the plain area belongs to the intermediate water flow system. The groundwater age in the central plain is more than 80 years, which may overlap with the regional circulation system.
- tritium,
- CFCs,
- Dongting basin,
- groundwater,
- hydrogeology

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References(72)

References

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Study on Age and Recycling of Shallow Groundwater Based on Tritium and CFCs in Dongting Basin

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