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Volume 1 Issue 1
Jun.  2013
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Article Contents
Jingli Shao, Yali Cui, Yunzhang Zhao. 2013: A Study on Infiltration and Groundwater Development in the Influent Zone of the Perched Lower Yellow River. Journal of Groundwater Science and Engineering, 1(1): 46-53.
Citation: Jingli Shao, Yali Cui, Yunzhang Zhao. 2013: A Study on Infiltration and Groundwater Development in the Influent Zone of the Perched Lower Yellow River. Journal of Groundwater Science and Engineering, 1(1): 46-53.

A Study on Infiltration and Groundwater Development in the Influent Zone of the Perched Lower Yellow River

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Supported by a grant from the National Basic Research Program of China (973 Program) (No. 2010CB428804)

  • Publish Date: 2013-06-28
  • A three-dimension flow model based on the hydrogeological conditions within the influent zone of the Yellow River in Henan Province, Yuanyang, China, was set up using FEFLOW. The interaction of the Yellow River and the groundwater was simulated under various pumping scenarios. For the planned water supply area, simulation results indicate that, within 10 years’ pumping at a rate of 4.86′108m3/a, the shallow groundwater flow and infiltration from Yellow River will be stabilized . After 10 years pumping, the infiltration will increase to 3.22′108m3/a ?and take approximately 70% of the pumping water.
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  • ZHAO Y, SHAO J, YAN Z, ET AL. COMPREHENSIVE APPROACH TO GROUNDWATER SYSTEM BOUNDARIES OF AFFECTED ZONE ON DOWN-YELLOW RIVER[J]. ACTA
    Shao J, Cui Y, Zhao y. Groundwater Numerical Modeling and its Application in Affected Zone of the Down -Yellow River (Hennan section)[J]. Journal of Jilin University(Earth Science Edition), 2003, 33(1): 51-56
    Fetter, C W. Applied Hydrogeology[M]. Prentice Hall, 2001
    Zhao Y, Shao J, Yan Z, et al. Study on Reach of Infiltration to Groundwater in the Yellow River[J]. Yellow River, 2003, 25(1): 3~5
    Chen J. Introduction to groundwater modeling software system FEFLOW[J]. China Water Resources, 2009, B: 25-26
    Diersch, H J. Interactive, graphics-based finite element simulation systwm FEFLOW for modeling groundwater flow, contaminant mass and heat transport processes[M]. WASY, Berlin, 1996
    Lei W, Luo Y, and Jiao X. Advances in study on the Downstream Yellow River infiltration to groundwater[J]. Yellow River, 2009, 31(1): 61-64
    Yan Z, Zhao Y, Jiao H, et al. The geological contrl of the Yellow River Alluvial Fan on Central Plain Cities[J]. Earth Sciences Frontier, 2010, 17(16): 278-285
    Cui Y, Shao J, Zhao Y. Characteristics and Development of Groundwater Reservoirs in Affected Zone of the Lower Yellow River[J]. Journal of natural resources, 2004
    Zhang L, Li L and Gong X. Geological Problems and Countermeasure Research on the Lower Course of the Yellow River in Henan Province[J]. HENAN GEOLOGY, 19(1), 2001: 71-78
    Bear, J. Hydraulics of Groundwater[M]. McGraw-Hill, New York, 1979
    Gao H, Yang M, Hei L, et al. MODFLOW & FEFLOW Application of Domestic Groundwater Value Simulation[J]. Ground water, 2012, 34(4): 13-15
    Shao J, Zhao Y, Cui Y, et al. Groundwater resource evaluation and development in affected zone of downstreams of the Yellow River[J]. Journal of natural resources, 2003, 18(1): 1-7
    Huo S, Wang H and Peng M. Analysis on No-flow in the Lower Yellow River in 1997[J]. Yellow River, 1998, 20(1): 1~3
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