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Information Journal Paper

Title

INTERACTION OF GROUNDWATER AND SURFACE WATER IN MAHI_DASHT AQUIFER

Pages

  63-78

Abstract

 The Mahi-Dasht aquifer located in Kermanshah province, west part of Iran. Water resources planning, development and management of Mahi-Dasht area has become inerasably complex as many factors, such as population growth and increasing demand on existing water supplies. To overcome the water shortage and increase water supply during critical demand period, interaction of surface water and groundwater has been investigated. For these reason two models, with and without INTERACTION OF GROUNDWATER AND SURFACE WATER were developed. These conceptual models (with/without feed from river) were developed in the groundwater MODFLOW PMWIN 5.3 model. Then the groundwater level and volume of aquifer were compared. The results shows that the groundwater level increase in wells near to the river, also the aquifer volume increasing too. Too increase the groundwater level as well as the aquifer volume, it is recommend that during the wet season, the flow of river can be used as recharge of groundwater.

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  • Cite

    APA: Copy

    PORHEMAT, JAHANGIR, HEYDARIZADEH, MAJID, ABDEH KOLAHCHI, ABDOLNABI, & KARIMI, ZEYNAB. (2012). INTERACTION OF GROUNDWATER AND SURFACE WATER IN MAHI_DASHT AQUIFER. JOURNAL OF THE EARTH, 7(23), 63-78. SID. https://sid.ir/paper/193065/en

    Vancouver: Copy

    PORHEMAT JAHANGIR, HEYDARIZADEH MAJID, ABDEH KOLAHCHI ABDOLNABI, KARIMI ZEYNAB. INTERACTION OF GROUNDWATER AND SURFACE WATER IN MAHI_DASHT AQUIFER. JOURNAL OF THE EARTH[Internet]. 2012;7(23):63-78. Available from: https://sid.ir/paper/193065/en

    IEEE: Copy

    JAHANGIR PORHEMAT, MAJID HEYDARIZADEH, ABDOLNABI ABDEH KOLAHCHI, and ZEYNAB KARIMI, “INTERACTION OF GROUNDWATER AND SURFACE WATER IN MAHI_DASHT AQUIFER,” JOURNAL OF THE EARTH, vol. 7, no. 23, pp. 63–78, 2012, [Online]. Available: https://sid.ir/paper/193065/en

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