Investigation of Statistical Relationships among Morphological Characteristics of Semi-Arid Watersheds for Using in Hydrological Models (Case Study: Neishabour Bar Watershed)

Memarian, Hadi; Amirafzali, Firozeh; Tajbakhsh, Seyed Mohammad; Akbarpour, Abolfazl

doi:10.22077/jwhr.2022.5361.1063

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	Investigation of Statistical Relationships among Morphological Characteristics of Semi-Arid Watersheds for Using in Hydrological Models (Case Study: Neishabour Bar Watershed)
Water Harvesting Research
دوره 5، شماره 1 - شماره پیاپی 7، فروردین 2022، صفحه 9-20 اصل مقاله (1.74 M)
نوع مقاله: Research Paper
شناسه دیجیتال (DOI): 10.22077/jwhr.2022.5361.1063
نویسندگان
Hadi Memarian^* ¹؛ Firozeh Amirafzali²؛ Seyed Mohammad Tajbakhsh³؛ Abolfazl Akbarpour⁴
¹Watershed Management Dept, Natural Resource faculty, University of Birjand, Birjand, Iran
²M.Sc. watershed management, University of Birjand, Birjand, Iran
³Watershed Management Dept, Natural Resource Faculty, University of Birjand, Birjand, Iran
⁴Department of Civil Engineering, University of Birjand, Birjand, Iran
چکیده
Due to the fact that ecosystems are more fragile and sensitive in arid and semi-arid regions of the world, the phenomenon of floods and the resulting damage and loss will be more severe in these areas. The subject of river canals and their morphology is one of the key topics in engineering and river management, which can be used to obtain a useful set of information about the geometric shape, bed shape, longitudinal profile, cross sections, over time. Default geometric relationships in hydrological models such as Kineros2 are based on field measurements in US watersheds and cause uncertainty in model results. Therefore, the purpose of this study is to determine the regional statistical relationships between the width and depth of the canal with the area of the upstream watersheds for employing in hydrological models such as Kineros2, and the width and depth of the canal with other basin characteristics. The data in this research are mainly topographic maps of Neishabour Bar watershed. Thus, according to topographic maps, preliminary studies were carried out to identify sub-basins. In this study, the basin is divided into 34 sub-basins that involve Lar Formation (in 16 sub-basins), and marl (in 18 sub-basins), where, 27 sub-basins in upstream are non-orchard lands. The linear and nonlinear regressions and equations were studied and evaluated using the software such as Excel, SPSS, Curve Expert, and XLSTAT. The results of correlation of physical parameters with canal width and depth, nonlinear regression analysis and analysis of variance in the relationships between canal depth/width with upstream area in the whole basin (R²=0.58 for canal depth and R²=0.14 for canal width), in upstream Lar formation, in downstream and non-orchard lands, showed a greater impact of the upstream acreage on the canal depth relative to the width (due to the higher coefficient of determination and less error). Furthermore, the separation of sub-basins in terms of geological formation and the presence of orchards had a significant effect on improving equations and reducing errors. The greater impact of the canal depth than the width from the upstream area is mostly related to successive droughts and the absence of flash floods in the area to change the canal depth, while the width of the canals has been mainly a function of human manipulations on the river bed. Stepwise linear regression analysis also showed a higher correlation between canal depth than the canal width with the physical parameters of the basin (R²=0.85 and R²=0.77, respectively).
کلیدواژه‌ها
Canal width and depth؛ Regression analysis؛ River morphology؛ Semi-arid region؛ Statistical equations؛ Regional equations؛ Watershed

مراجع
Abdollahi, Kh. (2002). Digital Elevation Models and Their Application in Hydrology, Published in Geomatics Conference (In Persian). Alizadeh, A. (2014). Principles of Applied Hydrology, Thirty-seventh Edition, Imam Reza University, Pp. 481 (In Persian). Ebisemiju, F. S. (1989). The morphology and downstream hydraulic geometry relations of alluvial stream channels in a humid tropical environment, southwestern Nigeria. IAHS-AISH publication, (187), 221-236. Ghiasi, N.Gh., Arab Khedri, M., Ghafari, A., Hatami H. (2004). Survey on the Effect of Some Morphometric Characteristics of Basins on Peak Discharge with Different Return Periods (Case Study North Albors Basins). Pajouhesh-va-sazandegi, 17(62): 2-10 (In Persian). Javan, J., Falsoleyman, M. (2006). The Necessity of Performing “Aquiferous Fields Plan” In The Arid And Semiarid Areas: Birjand A Case Study. Journal of geography and regional development, 6:27-50 (In Persian). Mahdavi, M. (2007). Applied Hydrology, Volume II, 5th Edition, University of Tehran, Pp. 437 (In Persian). Memarian, H., Balasundram, S. K., Talib, J. B., Teh Boon Sung, C., Mohd Sood, A., & Abbaspour, K. C. (2013). KINEROS2 application for land use/cover change impact analysis at the H ulu L angat B asin, M alaysia. Water and Environment Journal, 27(4), 549-560. Ministry of Energy. (1987). Instructions for physiographic studies in watersheds (In Persian). Mollaifar, I. (2013). Evaluation of KINEROS2 Model for Simulating Flood Hydrograph. Case study: Ziarat Watershed. Master Thesis, Faculty of Rangeland and Watershed Management, Gorgan University of Agricultural Sciences and Natural Resources (In Persian). Nam Avar, B. (2011). Runoff forecasting by implementing KINEROS2 model through AGWA - GIS tool (Case study: Kameh watershed). M.Sc., Faculty of Agriculture, Ferdowsi University of Mashhad (In Persian). Osterkamp, W. R., Lane, L. J., Foster, G. R. (1983). An analytical treatment of canal-morphology relations. US Government Printing Office. Poormohammadi, S., Dastorani, M.T. (2015). Assessment of Flow and Sediment Regime Properties in Arid and Semi-Arid Catchment Areas (Case Study: Lorestan Province). Geography and development, 13(39):195-210 (In Persian). Rezaei Pajand, H., Bozorgnia, A. (2002). Nonlinear regression analysis and its applications, translated, Ferdowsi University of Mashhad (In Persian). Rezaei, A., Soltani, A. (1998). Introduction to Applied Regression Analysis, Isfahan University of Technology (In Persian). Scott, N., Miller, D., Guertin, P., David, C., Goodrich. (1996). GIS for Water Resources and Watershed Management (Chapter 5). This edition published in the Taylor & Francis e-Library. Sobhani, M. (2016). Statistical study of suspended sediment trend in relation to watershed management operations using time series analysis (Case study: Neishabour watershed)" Master Thesis, Faculty of Natural Resources and Environment, Birjand University (In Persian). Woolhiser, D. A., Smith, R. E., & Goodrich, D. C. (1990). KINEROS: a kinematic runoff and erosion model: documentation and user manual.
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Investigation of Statistical Relationships among Morphological Characteristics of Semi-Arid Watersheds for Using in Hydrological Models (Case Study: Neishabour Bar Watershed)