Welcome to Open Science
Contact Us
Home Books Journals Submission Open Science Join Us News
Determining the Hydraulic Geometry Parameters of Seyhan River
Current Issue
Volume 2, 2015
Issue 4 (July)
Pages: 77-84   |   Vol. 2, No. 4, July 2015   |   Follow on         
Paper in PDF Downloads: 71   Since Aug. 28, 2015 Views: 2007   Since Aug. 28, 2015
Authors
[1]
M. Ishak Yuce, Civil Engineering Department, University of Gaziantep, Gaziantep, Turkey.
[2]
Musa Esit, Civil Engineering Department, University of Gaziantep, Gaziantep, Turkey; Civil Engineering Department, University of Adıyaman, Adıyaman, Turkey.
[3]
Abdullah Muratoglu, Civil Engineering Department, University of Batman, Batman, Turkey.
Abstract
Cross-section of rivers vary by time due to the dynamic structure of hydraulic geometry. The hydraulic geometry parameters of rivers including the width, depth and velocity are related to its discharge as simple power functions at a given cross-section. The characteristics of a river can be determined by using the hydraulic geometry parameters. The aim of this study is to determine the downstream and at-a-station hydraulic geometry parameters of Seyhan River. The hydraulic geometry parameters are estimated by employing the daily discharge values and the cross-sectional data of seven flow measurement stations located on the main river and its tributaries. The results of the analyses show that both the summation of the exponents and the multiplication of the coefficients are almost unity. These outcomes are expected to be helpful in developing water resources projects the basin.
Keywords
River Geometry, Downstream Hydraulic Geometry, At-a-Station Hydraulic Geometry, Seyhan River, Power Functions
Reference
[1]
Campell, D., Campell, S., 2008. Introduction to regression and data analysis. StatLap Workshop Series, 1-15.
[2]
Chong, S.E. 1970. The width, depth and velocity of Sungei Kimla, Perak. Geographica, 6, 72-63.
[3]
De Rose, R. C., Stewardson, M. J., Harman, C., 2008. Downstream hydraulic geometry of rivers in Victoria, Australia. Geomorphology 99, 302-316.
[4]
Dincer, A., 2007. Relationship Between the Develop Of Water Resources and Lagoons in Lower Seyhan Plain (Lsp). Çukurova University Institute of Natural and Applied Sciences Department of Environmental Engineering. 22, pp. 72.
[5]
Fujihara Y, Tanaka K, Watanabe T, Kojırı T (2007) Assesing the impact of climate change on the water resources of the Seyhan River basin, Turkey. The final report of ICCAP, pp 89–94
[6]
Howard, A.D., 1980. Thresholds in river regimes. In: Coates, D.R., Vitek, J.D. (Eds.), Thresholds in Geomorphology. Allen Unwin, Boston, pp. 227–258.
[7]
Huang, H.Q., Nanson, G.C., 1997. Vegetation and channel variation; a case study of four small streams in southeastern Australia. Geomorphology 18, 237–249.
[8]
Lee, S. J., Julien. P. Y., 2006. Downstream Hydraulic Geometry of Alluvial Channels. Journal of Hydraulic Engineering, 132, 1347-1352.
[9]
Leopold, L. B. and Maddock, T. 1953. The hydraulic geometry of stream channels and some physiographic implications, U.S. Geological Survey Professional Paper, 252.
[10]
Muratoglu, A., Yuce, I. M., 2011. Determination of the Downstream Hydraulic Geometry Parameters of Tigris River. Proceedings of International Conference on Sediment transport Modeling in Hydrological Watersheds and Rivers, İstanbul, Turkey pp. 557-562
[11]
Nanson, G.C., Nanson, R.A, Huang, H.Q., 2010. The hydraulic geometry of narrow and deep channels; evidence for flow optimization and controlled peatland growth. Geomorphology 117, 143-154.
[12]
Nanson, G. C., Pietsch,T.J., 2011. Bankfull hydraulic geometry; the role of in-channel vegetation and downstream declining discharges in the anabranching and distributary channels of the Gwydir distributive fluvial system, southeastern Australia. Geomorphology 129, 152-165.
[13]
Park, C.C., 1977. World-wide variations in hydraulic geometry exponents of stream channels: an analysis and some observations. Journal of Hydrology 33, 133–146.
[14]
Rhoads, B.L., 1991. A continuously varying parameter model of downstream hydraulic geometry. Water Resources Research 27, 1865–1872.
[15]
Singh, V.P. 2003. On the theories of hydraulic geometry, International Journal of Sediment Research, 18, 196-218.
[16]
Stewardson, M., 2005. Hydraulic geometry of stream reaches, Journal of hydrology, 306, 97-111.
[17]
Topraksu, 1974. Seyhan Watershed Lands. Earthy General Manager of Publications, (in Turkish: Seyhan Havzası Toprakları. Topraksu Genel Müdürlüğü Yayınları Raporlar Serisi) 286. Report series 70. Ankara.
[18]
Turkish Ministry of Environment and Urbanization, 2011. Strategic Steps to Adapt to Climate Change in Seyhan River Basin 11, pp. 41.
[19]
Turkman, K. F., Scotto, M. G, and Bermudez, P. de Z., 2014 Non-Linear Time Series: Extreme Events and Integer Value Problems, Springer, ISBN-13: 978-3319070278
Open Science Scholarly Journals
Open Science is a peer-reviewed platform, the journals of which cover a wide range of academic disciplines and serve the world's research and scholarly communities. Upon acceptance, Open Science Journals will be immediately and permanently free for everyone to read and download.
CONTACT US
Office Address:
228 Park Ave., S#45956, New York, NY 10003
Phone: +(001)(347)535 0661
E-mail:
LET'S GET IN TOUCH
Name
E-mail
Subject
Message
SEND MASSAGE
Copyright © 2013-, Open Science Publishers - All Rights Reserved