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DOI Prefix 10.20431 |
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Hydroelectric Production using Ab-Terki River Flow Specific Energy
Saeid Eslamian1,Nicolas R.Dalezios2,Mahboubeh Amoushahi-Khouzani3,Maryam Marani-Barzani4,Amir Gandomkar5,Morteza Khodagholi6,Foroozan Rajaei-Rizi7,Vijay P.Singh8,Shahide Dehghan9,Mohsen Ghane10,Kaveh Ostad-Ali-Askari11,Morteza Soltani12,Yohannes Yihdego13,Hossein Norouzi14,Hamid-Reza Shirvani-Dastgerdi15,Nasrin Zalaki-Badil16
2.Laboratory of Hydrology, Department of Civil Engineering, University of Thessaly, Volos, Greece & Department of Natural Resources Development and Agricultural Engineering, Agricultural University of Athens, Athens, Greece.
3.Water Engineering Department, Science and Research Branch, Islamic Azad University, Tehran, Iran.
4.Department of Geography, University of Malaya (UM) ,50603 Kuala Lumpur, Malaysia.
5.Department of Geography, Najafabad Branch, Islamic Azad University, Najafabad, Iran
6.Isfahan Center for Research of Agricultural Science and Natural Resources, Department of Climate Change & Drought, Isfahan, Iran.
7.Water Engineering Department, Shahrekord University, Shahrekord, Iran.
8.Department of Biological and Agricultural Engineering & Zachry Department of Civil Engineering, Texas A and M University, 321 Scoates Hall, 2117 TAMU, College Station, Texas 77843-2117, U.S.A.
9.Department of Civil Engineering, South Tehran Branch, Islamic Azad University, Tehran, Iran.
10.Department of Civil Engineering, Isfahan (Khorasgan) Branch, Islamic Azad University, Isfahan, Iran.
11.Department of Architectural Engineering, Shahinshahr Branch, Islamic Azad University, Shahinshahr, Iran.
12.Snowy Mountains Engineering Corporation (SMEC), Sydney, New South Wales 2060, Australia.GeoInformation Science and Earth Observation (ITC), University of Twente, the Netherlands.
13.Department of Civil Engineering, Maybod Branch, Islamic Azad University, Maybod, Yazd, Iran.
14.Department of Civil Engineering, Isfahan (Khorasgan) Branch, Islamic Azad University, Isfahan, Iran.
15.Department of Soil Science, Shahid Chamran University of Ahvaz, Ahvaz, Iran.
Citation :Saeid Eslamian,et.al, Hydroelectric Production using Ab-Terki River Flow Specific Energy International Journal of Constructive Research in Civil Engineering 2017,3(3) : 46-61
The flow duration curve (FDC) of a riveris one of the important parameters for the hydrological investigation of hydroelectric plants. Computation of the hydroelectric plant capacity and power production requires the determination of relative and cumulative frequenciesof different river discharges. Ab-Terki is one of the sub-basins of Bazoft River, located in Chaharmahal and Bakhtiari province, Iran, next to Koohrang basin. It is located between eastern longitudes of 49°54' to 50°5' and northern latitudes of 32°19' to 32°24'. Morphological conditions, sloping limestone structures, and characteristics of karstic cracks in the basin have led to the formation of large springs in the eastern and western foothills of Zardkooh Mountain. In order to determine the FDCs of Ab-Terki River,3-year daily discharge and 24-year mean monthly discharge of Gooshe-pol station were used. Then, the probabilities of discharges were analyzed using Hyfa and Rank Plot numerical codes and finally, the discharge of Ab-Terki River corresponding to 95% probability was determined.