地表水‒地下水相互作用对砷在浅层地下水系统中运移的影响

余倩; 张宇; 董听; 吴光伟; 李平

doi:10.3799/dqkx.2022.146

Volume 48 Issue 9

Sep. 2023

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Article Navigation > Earth Science > 2023 > 48(9): 3420-3431

Yu Qian, Zhang Yu, Dong Ting, Wu Guangwei, Li Ping, 2023. Effect of Surface Water-Groundwater Interaction on Arsenic Transport in Shallow Groundwater of Jianghan Plain. Earth Science, 48(9): 3420-3431. doi: 10.3799/dqkx.2022.146

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Yu Qian, Zhang Yu, Dong Ting, Wu Guangwei, Li Ping, 2023. Effect of Surface Water-Groundwater Interaction on Arsenic Transport in Shallow Groundwater of Jianghan Plain. Earth Science, 48(9): 3420-3431. doi: 10.3799/dqkx.2022.146

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Effect of Surface Water-Groundwater Interaction on Arsenic Transport in Shallow Groundwater of Jianghan Plain

doi: 10.3799/dqkx.2022.146

Yu Qian^{1
,
,},
Zhang Yu²,
Dong Ting¹,
Wu Guangwei³,
Li Ping¹

1.
College of Resources and Environmental Science, South-Central University for Nationalities, Wuhan 430074, China
2.
Gezhouba Water Service Tianjin Co., Ltd., Tianjin 300356, China
3.
Shandong Provincial Space Ecological Restoration Center, Jinan 250014, China

Received Date: 2022-04-15
Available Online: 2023-10-07
Publish Date: 2023-09-25

Abstract

Abstract

Surface water-groundwater (SW-GW) interaction is critical for arsenic transport in shallow groundwater systems, but the role of its pattern and intensity on arsenic transport remains unclear. Field monitoring and numerical simulation were employed to identify the impact of surface water-groundwater interaction mode and intensity on arsenic transport in shallow groundwater of Shahu field site, Jianghan Plain. The results indicate that the surface water recharged into groundwater and had a relatively stronger intensity in the rainy season, which led to the higher arsenic concentration, and vice versa. The seasonal shift of surface water-groundwater interaction mode and intensity could cause the seasonal response of groundwater flow velocity and direction. It is estimated by the numerical simulation that the maximum vertical exchange mass of arsenic is 457.2 mg/d in rainy season and 191.3 mg/d in dry season and the maximum horizontal exchange mass of arsenic is 4 380.0 and 1 385.6 mg/d in rainy and dry season, respectively.
- surface water,
- groundwater,
- arsenic,
- groundwater flow model,
- Jianghan Plain,
- environmental engineering

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References(44)

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Effect of Surface Water-Groundwater Interaction on Arsenic Transport in Shallow Groundwater of Jianghan Plain

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