Prediction of Impacts Caused by South-to-North Water Diversion on Underground Water Level in Shijiazhuang

HAN Kang-qin; LIU Jian; HAN Lei-lei; HAN Wen-ling; ZHANG Yun-xiao

Volume 2 Issue 2

Jun. 2014

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Article Navigation > Journal of Groundwater Science and Engineering > 2014 > 2(2): 27-33

HAN Kang-qin, LIU Jian, HAN Lei-lei, et al. 2014: Prediction of Impacts Caused by South-to-North Water Diversion on Underground Water Level in Shijiazhuang. Journal of Groundwater Science and Engineering, 2(2): 27-33.

Citation:

HAN Kang-qin, LIU Jian, HAN Lei-lei, et al. 2014: Prediction of Impacts Caused by South-to-North Water Diversion on Underground Water Level in Shijiazhuang. Journal of Groundwater Science and Engineering, 2(2): 27-33.

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Prediction of Impacts Caused by South-to-North Water Diversion on Underground Water Level in Shijiazhuang

1Hebei Institute of hydrological and engineering of geological survey, China2Hebei University of Geosciences,shijiazhuang, China

Publish Date: 2014-06-28

Abstract

Abstract

After implementation of the South-to-North Water Diversion Project which has attracted worldwide attentions, new surface water sources would be added and, accordingly, mining of groundwater for industrial and living water would be reduced to ease the mining pressure of the underground water and abate the decline of the water level in the depression centers of Shijiazhuang and the whole intake area. Numerical model was established in this paper to respectively calculate the underground water level in 2020 based on three schemes including mining status of underground water, urban water resource planning of South-to-North water diversion in Shijiazhuang and Hutuo River infiltration with artificial regulation and storage. It is estimated that after implementation of the South-to-North Water Diversion Project, the buried depth of groundwater of depression centers in Shijiazhuang in 2020 will increase by 28.5~41.09 m comparing with that without water supply through South-to-North water diversion
- South-to-North water diversion,
- Numerical model,
- Underground water level,
- Infiltration field,
- Artificial regulation and storage

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References(7)

References

Hebei Hydrological Engineering Geological Survey Institute of Ministry of Geology and Mineral Resources. 1994. Evaluations on urban underground water resources of Shijiazhuang.

Environmental and Hydrological Key station of Hebei Province. 1986. Observation of underground water dynamics in Shijiazhuang (Plain) (1981-1985).

Investigation and Design Institute for Water Resources and Hydropower of Hebei Province and Hebei Hydrological Engineering Geological Survey Institute of Ministry of Geology and Mineral Resources. 1997. Research on impacts caused by vertical seepage- proofing in Huabizhuang reservoir on downstream underground water.

Environmental and Hydrological Key Station of Hebei Province. 2001. Geological environment monitoring in Shijiazhuang (1996-2000).

Environmental and Hydrological Key Station of Hebei Province. 1991. Geological environment Monitoring in Shijiazhuang (1986-1990).

Geology Brigade for Hydrological and Geological Engineering of Hebei Bureau of Geology. 1965. Hydrogeological investigation for urban water supply of Shijiazhuang.

Geology Brigade for Hydrological and Geological Engineering of Hebei Bureau of Geology. 1958. 1:200 000 Comprehensive geologicalHydro- geological survey(Shijiazhuang).

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