A study of vertical exchange between surface water and groundwater around the banks of Baiyangdian Lake

LI Gang; MA Baiheng; ZHOU Yangxiao; ZHAO Kai; YOU Bing; LI Muzi; DONG Huijun; LI Haitao

doi:10.16030/j.cnki.issn.1000-3665.202008004

2021 Vol. 48, No. 4

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LI Gang, MA Baiheng, ZHOU Yangxiao, ZHAO Kai, YOU Bing, LI Muzi, DONG Huijun, LI Haitao. A study of vertical exchange between surface water and groundwater around the banks of Baiyangdian Lake[J]. Hydrogeology & Engineering Geology, 2021, 48(4): 48-54. doi: 10.16030/j.cnki.issn.1000-3665.202008004

Citation:

LI Gang, MA Baiheng, ZHOU Yangxiao, ZHAO Kai, YOU Bing, LI Muzi, DONG Huijun, LI Haitao. A study of vertical exchange between surface water and groundwater around the banks of Baiyangdian Lake[J]. Hydrogeology & Engineering Geology, 2021, 48(4): 48-54. doi: 10.16030/j.cnki.issn.1000-3665.202008004

A study of vertical exchange between surface water and groundwater around the banks of Baiyangdian Lake

1.
China Institute of Geo-Environment Monitoring, Beijing　100081, China
2.
Hebei Key Laboratory of Geological Resources and Environmental Monitoring and Protection, Shijiazhuang, Hebei　050021, China
3.
IHE Delft Institute for Water Education, Delft, South Holland　2611AX, Netherlands
4.
Hydrological Engineering and Geological Prospecting Institute of Hebei Province, Shijiazhuang, Hebei　050021, China

More Information

Corresponding author: LI Haitao, liht@cigem.cn

Received Date: 18 August 2020

Revised Date: 16 December 2020

Publish Date: 15 July 2021

Abstract

Abstract

Interaction between surface water and groundwater has always been a hot topic in hydrogeological researches. Previous studies focused on the hyporheic zone of rivers, but the hypolentic zone of lakes with relatively static water bodies was seldom examined. The Baiyangdian Wetlands is taken as a pilot area in this study, and a monitoring system of water table and temperature is set up. The vertical interaction fluxes between surface water and groundwater is quantified by using a heat tracing method. According to the Darcy’s Law, the vertical coefficient of permeability is calculated inversely. Based on the heat tracing method and the Darcy’s Law, a way of quantifying vertical interaction between surface water and groundwater is summarized. The results show that infiltration from surface water to groundwater around the banks of the Baiyangdian Wetlands is dominant in the interaction procedure. The total infiltration velocity from surface water to groundwater during the monitoring period ranges from 0.2 to 1.1 cm/d, and the vertical hydraulic conductivity, from 0.038 to 0.912 m/d. The conclusions in this paper can provide data support for strategy of water diversion and protection of eco-environment in the Baiyangdian Wetlands.
- Baiyangdian Lake /
- hypolentic zone /
- exchange between surface water and groundwater /
- heat tracing method /
- Darcy’s Law

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References

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