HYDROLOGICAL EVALUATION IN DOHUK-SEMEL AREA

  • SARBAST ISMAEL ABDI Dept. of Soil and Water, College of Agricultural Engineering Sciences, University of Duhok, Kurdistan Region
  • KURDISTAN IDREES DAWUD Dept. of Soil and Water, College of Agricultural Engineering Sciences, University of Duhok, Kurdistan Region
  • HIVEEN MIQDAD AHMED Dept. of Soil and Water, College of Agricultural Engineering Sciences, University of Duhok, Kurdistan Region
  • MURAD-JAN MUDHAFFAR Dept. of Soil and Water, College of Agricultural Engineering Sciences, University of Duhok, Kurdistan Region
Keywords: water surplus, water deficit, Hydrology and Return period

Abstract

The study area located on the east of Duhok city, it is divided into three sub-basins: Hishkero in the east, Semel in the middle, and Gregewr in the west, it covers about 487 km2. The historical record of rainfall data in Duhok-Semel area from Seismology Directorate and Duhok Meteorological Stations were used to calculate the water balance parameters for the period 2005-2006 to 2020-2021. It receives 559.6 mm of rain during rainy months. This occurs across 58 days in the eight wet months of the year. The amount of rain in January, which averages 124.8 mm, is the most. The amount of runoff is calculated using the curve number approach and the Soil Conservation Service method (SCS), where the soil type is the most important variable. Since all of the soil in the study area belongs to the D group, that the calculated value of runoff is (259mm/Year) or (45.9%) from annual average of rainfall (563.6mm/year). From the total annual rainfall, there is a water surplus of 31.2% and a water deficit of 68.8%. According to overall calculations of the water balance components, the groundwater recharge is (-175.5 mm/year) or (0.1%) of the study area from surplus water. From rainfall prediction value according to Log person III during return period (95.2%) as probability in first two years appear that the rainfall amount will be little, but inversely rain falling will start with probability (80%)

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References

Abdulrahman, H. D., Fayyadh, M. A., & Doski, J. A. (2020). Formation and development of vertisols in selivany plain at duhok governorate, kurdistan region, iraq. Journal of duhok university, 23(2), 246-258.
Al-Kubaisi, Q.Y. (2004). Annual aridity index of type.1 and type.2 mode options climate classification. Science Journal, 45c (1): 32-40.
Al-Sudani HIZ., (2019). Estimation of water balance in Iraq using meteorological data. International Journal of Recent Engineering Science., 6(5): 8-13.
Brown, L.H., and Cochem, J., (1973). A Study at the Agromeleorblogy, 125pp.
Dara RN, Jirjees S, Fatah KK, Javadinejad S. (2021) Climatic Parameters Analysis of Koysinjaq Meteorological Station, Kurdistan Region, Northern Iraq. The Iraqi Geological Journal. Jan 28:99-109.
Das, J. and B.C. Acharya, (2003). Hydrology and assessment of lotic water quality in Cuttack city,India. Water, Air, Soil Pollut. 150: 163-175. DOI: 10.1023/a: 1026193514875.
FAO, (2003). Grazing systems and livestock production in the three northern Governorates of Iraq.
Fetter, C.W. (1980). Applied Hydrology, Charles Merril Publishing Company. A Bell and Howell Company, Columb. Ohio, 488P.
Gulcur, M. and M. S. Kettenah (1972). Forestry research, Demonstration and Training. FO: SF/ IRQ. 518 Erbil, Iraq.
Hammer, M., and Mackichan, H., (1981). Hydrology and Quality of Water Resources. Wiley Co.
Hassan, A. H. Al Kubuisi, Q. Y. (1998). Water surplus model for Basrah meteorological station, Geology of Jordan and Adjacent areas. Proceedings of the sixth Jordanian Geological conference (5-8), 207-210 p.
Hassan, H. A. and Zeki, N. A. (1982). Water availability periods and water balance parameters, AWRRC, Tech. Rep. No.160, 32p.
Hassan, H. A.; Hama Said, M. A. and Ali, D. M. (1999). Modeling water balance of Derband Gomaspan Basin, NE, Erbil, Journal of Duhok University Vol.2, No. 4.
Hossein Tabari, P. Hosseinzadeh Talaee , B. (2012). Shifteh Some'e. Spatial modelling of reference evapotranspiration using adjusted Blaney-Criddle equation in an arid environment. Pages 408-420, Received 08 Jan 2012, Accepted 24 Jul, Published online: 18 Feb 2013.
Ishaq Yaqo, (1955). Hydrogeology Semel Area – Duhok.
Ivezic, V., Bekic, D. and Žugaj, R. (2017). A review of procedures for water balance modelling. J Environ Hydrol, 25.
Jabbouri, S. T. (1988). Hydrology and watershed management, Mosul University press. P. 89-92.
Jaferim. T., Hamid. (2006). Evaluation of Hydrological study in Semel- Duhok Area. Kurdistan Region Iraq.
Jaferm. T., Hameed and Haliz S. Mohamed A., (2015). Evaluation of Water Balance Modeling Parameters for Zawita-Swaratoka Watershed. Journal of University of Duhok., Vol. 18, No.1 (Agri. and Vet. Sciences), Pp 7-18.
Jamil, A. K.; Habib, H. R. and Hama Said M. A. (1999). Hydrological and Meteorological Aspects and Water Balance in Bastora Basin, Erbil Governorate-Northern Iraq, Journal of Duhok University, Vol.2, No.2.
Jassim, S. Z. and Sisakian, V., (1978). Field guide to the geology of Salah Al-din - Shaqlawa area, Northern Iraq.
Jawad, S., and Washeed, S., (1986). A water balance and discharge predictive model for Kani Kedri springs system, north W. Iraq. Journal of Agriculture and Water Resource Research, 5(1):151–168.
Ketanah, Gangopadhyaya, and Gangopadhyay, M., (1974). Analysis Rainfall Data in II.R.I, Drainage Principles and Investigation, Wageningen, the Netherlands, 368 pp.
Kharrufa, N. S. (1985). ‘Simplified Equation for Evapotranspiration in Arid Regions’, Beiträge zur Hydrologie, Sonderheft 5.1, 39–47.
Khasback, S., (1973). A Geographical study on natural and pollution conditions, Northern Iraq. Shafeq Press.
Kosslar, J. and Read, S. J. (1974). Analyzing rainfall data. Drainage principles and application, III surveys and investigations, International Instituted for Land Resolution and Improvement. Netherland P. 14
Kottek, M. J., Grieser, C., Beck, B. Rudolf, and Rubel, F., 2006.World Map of Köppen- Geiger Climate Classification updated, Meteorol, Z., 15, 259-263.4
KRI. 2018. Demographic Survey. KRSO_IOM_UNFPA_Demographic_Survey_Kurdistan_Region_of_Iraq. pdf. book. © International Organization for Migration (IOM), 2018.
Maidment, D., (1993). Handbool of Hydrology. New York.
Markus, K., Juregen G., Christof B., Bruno R., and Franz R., (2006). World Map of the Köppen-Geiger climate classification updated. Meteorologische Zeitschrift, Vol. 15, No. 3, 259-263 (June), DOI: 10.1127/0941-2948/2006/0130.
Mather, J. R., (1974). Climatology fundamentals and applications, McGraw-Hill Book Co., New York.412 P.
Muhemmed Ali Fayadh (2010). mineralogical Study of Semel area.
Parsons, Donald A. (1955). Coshocton-type runoff samplers: U.S. Dept. Agriculture, ARS-41-2, 10 p.
Rudić, D., Đurović, N.: Odvodnjavanje. Izdavač: Poljoprivredni fakultet, Beograd, (2006).
Showap, G., Frifrevt, R., Admister, T., and Barniz, K., (1984). Engineering of Soil and Water Conservation.
Subedi, A and Chavez JL. (2015). Crop evapotranspiration (ET) estimation models: A review and discussion of the applicability and limitations of ET method. Journal of Agriculture Science, 7(6).
Taufiq, J.M. and J. Domas (1977). The regional geological mapping of Dohuk-Ain Zala area. State Organization for Minerals Library Reports, Baghdad, Iraq, no. 837.
Toma, J.J., (2012). Water quality index for assessment of water quality of Duhok Lake, Kurdistan region of Iraq. J. Adv. Lab. Res. Bio, 3(2), pp.142-147.
Veronica L. Webster & Jery Stedinger. (2007). Log-Pearson Type 3 Distribution and Its Application in Flood Frequency Analysis. II: Parameter Estimation Methods. Journal of Hydrologic Engineering 12(5)DOI: 10.1061/(ASCE)1084-0699(2007)12:5(492)
Published
2023-09-25
How to Cite
ABDI, S. I., DAWUD, K. I., AHMED , H. M., & MUDHAFFAR, M.-J. (2023). HYDROLOGICAL EVALUATION IN DOHUK-SEMEL AREA. Journal of Duhok University, 26(2), 1-11. https://doi.org/10.26682/ajuod.2023.26.2.1
Section
Agriculture and Veterinary Science