Evaluation of Natural Drainage Flow Pattern, Necessary for Flood Control, Using Digitized Topographic Information: A Case Study of Bayelsa State Nigeria
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Evaluation of Natural Drainage Flow Pattern, Necessary for Flood Control, Using Digitized Topographic Information: A Case Study of Bayelsa State Nigeria

Authors: Collins C. Chiemeke

Abstract:

The need to evaluate and understand the natural drainage pattern in a flood prone, and fast developing environment is of paramount importance. This information will go a long way to help the town planners to determine the drainage pattern, road networks and areas where prominent structures are to be located. This research work was carried out with the aim of studying the Bayelsa landscape topography using digitized topographic information, and to model the natural drainage flow pattern that will aid the understanding and constructions of workable drainages. To achieve this, digitize information of elevation and coordinate points were extracted from a global imagery map. The extracted information was modeled into 3D surfaces. The result revealed that the average elevation for Bayelsa State is 12 m above sea level. The highest elevation is 28 m, and the lowest elevation 0 m, along the coastline. In Yenagoa the capital city of Bayelsa were a detail survey was carried out showed that average elevation is 15 m, the highest elevation is 25 m and lowest is 3 m above the mean sea level. The regional elevation in Bayelsa, showed a gradation decrease from the North Eastern zone to the South Western Zone. Yenagoa showed an observed elevation lineament, were low depression is flanked by high elevation that runs from the North East to the South west. Hence, future drainages in Yenagoa should be directed from the high elevation, from South East toward the North West and from the North West toward South East, to the point of convergence which is at the center that flows from South East toward the North West. Bayelsa when considered on a regional Scale, the flow pattern is from the North East to the South West, and also North South. It is recommended that in the event of any large drainage construction at municipal scale, it should be directed from North East to the South West or from North to South. Secondly, detail survey should be carried out to ascertain the local topography and the drainage pattern before the design and construction of any drainage system in any part of Bayelsa.

Keywords: Bayelsa, Digitized Topographic Information, Drainage, Flood.

Digital Object Identifier (DOI): doi.org/10.5281/zenodo.1337435

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[1] A. Ebipade, Bayelsa dep gov calls for disaster management/control units in LGAs, 2013, www.tribune.com.ng/news2013.
[2] Bayelsa State, 2013, en.wikipedia.org/wiki/Bayelsa_State
[3] C. A. Kogbe, The Cretaceous and Paleogene sediments of southern Nigeria. In: Geology of Nigeria, C.A. Kogbe, (editor), Elizabethan Press, Lagos, pp. 311-334, 1989.
[4] EnviroNews Nigeria, Sorrow Tears for Bayelsa Flood Victims, 2012, www.environewsnigeria.com.
[5] Google Earth 2014, Imagery Map, www.gooogle.com/earth/
[6] J.B Wright, D. A. Hasting, W. B. Jones, and H. R. Williams, Geology and mineral resources of West Africa, Allen and Unwin Limited, UK, 107pp, 1985.
[7] K. S. Okiongbo, and R. Douglas, Hydrogeochemical Analysis and Evaluation of Groundwater Quality in Yenagoa City and Environs, Southern Nigeria, Ife Journal of Science vol. 15, no. 2, pp210, 2013.
[8] M. U. Osakuni, and T. K. Abam, Shallow resistivity measurement for cathodic protection of pipelines in the Niger Delta. Environmental Geology. 45, 747-752, 2004.
[9] Short, K.C., and Stauble, A.J. 1967. Outline of the geology of the Niger Delta. Bull. AAPG. 51,761- 779.