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Journal of Geosciences and Geomatics. 2016, 4(2), 21-28
DOI: 10.12691/JGG-4-2-1
Original Research

Morphometric Analysis of Sub- watersheds in Oguta and Environs, Southeastern Nigeria Using GIS and Remote Sensing Data

Udoka Ubong Paulinus1, , Nwankwor Godwin Ifedilichukwu1, Ahiarakwem Cosmas Ahamefula1, Opara Alex Iheanyichukwu1, Emberga Terhemba Theophilus2 and Inyang Godwin Edet1

1Department of Geosciences, Federal University of Technology, Owerri, Nigeria

2Department of Physics/Industrial Physics, Federal Polytechnic, Nekede, Owerri, Nigeria

Pub. Date: March 17, 2016
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Udoka Ubong Paulinus, Nwankwor Godwin Ifedilichukwu, Ahiarakwem Cosmas Ahamefula, Opara Alex Iheanyichukwu, Emberga Terhemba Theophilus and Inyang Godwin Edet. Morphometric Analysis of Sub- watersheds in Oguta and Environs, Southeastern Nigeria Using GIS and Remote Sensing Data. Journal of Geosciences and Geomatics. 2016; 4(2):21-28. doi: 10.12691/JGG-4-2-1

Abstract

Morphometric analysis of the sub- watersheds in Oguta area, Southeastern Nigeria using GIS processed Remote Sensing data was carried out with the objectives of evaluating their morphometric characteristics and other landuse/landcover dynamics. The present study involved the measurement of the linear, aerial and relief aspects of the dimensions of the sub-watersheds. Analysis of the landuse classification revealed that Njaba drainage basin is made up of 37.32% farmland and grassland, 27.51% forest, 20.06% bare land, and 5.28% water, while the Orashi drainage basin comprises of 30.23% farmland, 10.35% urban settlement, 20.14% forest land, 15.13% bare land and 24.14% water body. It was also revealed from the study that Njaba drainage basin has a basin length of 21.48km2 while that of Orashi drainage basin was estimated to be 29.59km2. Similarly, whereas the former has an area of 21.48 km2 the latter has an estimated area of about 29.59km2. Further morphometric analysis revealed that the bifurcation ratio of Njaba and Orashi drainage basins were estimated at 1.80 and 3.92 respectively, while their drainage densities were put at about 0.54 and 0.51 respectively. Finally, the basin relief ratios of the basins were estimated at 0.0038 and 0.00367 respectively while their form factor was given as 0.31 and 0.189 respectively. The form factor values estimated from this study revealed that the Njaba drainage basin is circular while Orashi drainage basin revealed an elongated dimension. These morphometric characteristics are key indices that are invaluable in assessing the geo-hydrological behavior of the drainage basins and their vulnerability to flooding.

Keywords

drainage basin, Oguta, basin morphometry, watershed, flood management, GIS

Copyright

Creative CommonsThis work is licensed under a Creative Commons Attribution 4.0 International License. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/

References

[1]  Waugh, D. (1996). Geography: An Integrated Approach. New York: Nelson (Chapter 6).
 
[2]  Long, Hualou. et al, 2008, Analysis of Urban-Rural Land-Use Change during 1995-2006 and Its Policy Dimensional Driving Forces in Chongqing, China. ISSN 1424-8220 © 2008 by MDPI www.mdpi.org/sensors.
 
[3]  Rastogi, R.A. and Sharma, T.C. (1976) Quantitative analysis of drainage basin characteristics. Jour. Soil and water Conservation in India, v.26 (1&4), pp.18-25.
 
[4]  Dutta, D., Sharma, J. R., &Adiga, S. (2002). Watershed characterization, prioritization, development planningand monitoring remote sensing approach, technical report ISRO- NNRMS-TR-103-2002 Bangalore: ISRO.
 
[5]  Agarwal, C.S. (1998), Study of drainage pattern through aerial data in Naugarh area of Varanasi district, U.P. Journal of Indian Society of Remote Sensing, 26: 169-175.
 
[6]  Horton R.E. (1940). An approach toward a physical interpretation of infiltration capacity. Proc. Soil Sci. Am.; 5: 399-417.
 
[7]  Horton, R.E. (1945), Erosion development of Streams and their Drainage Basins: Geol. Soc. America Bull, V.56, pp.75-370.
 
[8]  Melton M.A. (1958). Correlation structure of morphometric properties of drainage system and their controlling agents. J. Geol.; 66: 442-460.
 
[9]  Pakhmode V, Kulkarni H, Deolankar SB (2003). Hydrological drainage analysis in watershed programme planning: A case study from the Deccan basalt, India. Hydrogeol. J.; 11:595-604.
 
[10]  Gangalakunta P, Amal K, Kothiram S (2004). Drainage morphometryand its influence on landform characteristics in a basaltic terrain, Central India – a remote sensing and GIS approach. Int. J. Appl. Earth and Geoinform.; 6:1-16.
 
[11]  Strahler, A. N., 1964. Quantitative geomorphology of drainage basins and channel networks. In Chow, V.T. (ed.) Handbook of Applied Hydrology, McGraw-Hill, New York. pp 439-476.
 
[12]  Krishnamurthy J, Srinivas G, Jayaram V, Chandrasekhar MG (1996). Influence of rock type and structure in the development of drainage networks in typical hard rock terrain. ITC J, 3(4): 252-259.
 
[13]  Monanus and Inyang, F.(1975) Climate Regimes in Nigeria in Maps (ed.by G.F.K. Ofomata), 27-28, Ethiope Publishing House, Benin.
 
[14]  Uma, K.O., 1984. Water resources of owerri and environs. Unpublished MA Thesis, University of Nigeria Nsukka. World Energy Council, 2004.
 
[15]  Allen, J.R.L. (1965): “Late Quaternary Niger Delta and adjacent areas: Sedimentary Environments and Lithofacies”. Bulleting American of Petroleum Geology. Vol. 49 (5) Pp (547-600).
 
[16]  Akpokodje, E. G. (1979): “The importance of engineering geological mapping” in the development of the Niger Delta Basin. Bull. 1 in Assoc. Eng. Geol. No 19 Pp (102-108).
 
[17]  Asseez. L. O. (1976): “Review of the stratigraphy, Sedimentation and structure of the Niger- Delta in geology of Nigeria” Elizabethan Publishing Co., Lagos, Nigeria.
 
[18]  Etu-Efeotor J.O., Akpokodje E.G. (1990). Aquifer systems of the Niger Delta. J. Min. Geol. 26(2):279-285.
 
[19]  Short, K.C. and Stauble, A.J.(1967), Outline of the Geology of the Niger Delta,Am. Assoc.Bll, 51, 661-779.
 
[20]  Evamy, B.D., Haremboure, J., Kamerling, P., Knaap, W.A., Molloy, F.A., and Rowlands, P.H., 1978, Hydrocarbon habitat of Tertiary Niger Delta: American Association of Petroleum Geologists Bulletin, v. 62, p. 277-298.
 
[21]  Reyment, R.A., 1965. Aspects of the Geology of Nigeria. Ibadan University Press, Ibadan, Nigeria.
 
[22]  Doust, H., and Omatsola, E., 1990, Niger Delta, in, Edwards, J. D., and Santogrossi, P.A., eds., Divergent/passive Margin Basins, AAPG Memoir 48: Tulsa, American Association of Petroleum Geologists, p. 239-248.
 
[23]  Ananaba S.E. Onu, N.N. and Iwuagwu C.J (1993). Geophysical Study of the General Deposit n Ihiagwa, Owerri, Nigeria. Nigeria J. Mining Geol. 29(2), 95-100).
 
[24]  Odigi, M.I. And Nwadiaro, C.S., 1988, Geophysical Limnology of Lake Oguta, southeastern Nigeria. Hydrobiologia. Bulletin 22, pp113-125.
 
[25]  Ahiarakwem, C.A. And Onyekuru, S.O., 2011. A Comparative Assessment of the Physico-Chemical and Microbial Trends in Njaba River, Niger Delta Basin, Southeastern Nigeria, Journal of Water Resource and Protection, Vol. 3, pp686-693.
 
[26]  Ahiarakwem, C.A., 2006, Water quality assessment and some geochemical models of Oguta lake, southeastern Nigeria. Unpubl. Ph.D Thesis, Fed. Univ. of Tech., Owerri. 225p.
 
[27]  Jolly, J. P., 1982. A proposed method for accurately calculating sediment yields from reservoir deposition volumes. In Recent developments in the Explanation andPrediction of Erosion and Sediment Yield, Proceedings of Exeter Symposium., July 1982. IAHS Publication., 137. pp 153-161.
 
[28]  Ogunkoya, O. O., Adejuwon, J. O., and Jeje, L. K., 1984. Runoff Response to basin parameters in southwestern Nigeria. Journal of Hydrology, v.72, pp 67-84.
 
[29]  Rodda, J. C. (1969). The Flood Hydrograph. In R. J. Chorley (Ed.), Water, Earth And Man: A Synthesis Of Hydrology, Geomorphology And Socio-Economic Geography (Pp.405-418). London: Methuen.
 
[30]  Hadley, R.F. and Schumm, S.A, 1961, Sediment Sources and Drainage Basin Characteristics in Upper Chenne River Basin: US Geol.Survey Water Supply Paper 1531, Part B, pp 137-146.
 
[31]  Ajibade L.T., Ifabiyi, I.P., Iroye, K.A. and Oguntere, S. (2010) Morphometric Analysis of Ogunpe and Ogbere Drainage Basin, Ibadan, Nigeria. Ethioian Journal of Environmental Studies. Vol 3. No.1.
 
[32]  Miller, V.C.,1953, “A quantitative geomorphic study of drainage basin characteristics in the Clinch Mountain area,Varginia and Tennessee”, Columbia University, Department of Geology, ONR, Geography Branch, New York.
 
[33]  Babar, Md. (2005). “Hydrogeomorphology, Fundamental Applications and Techniques”, New India Publishing Agency, New Delhi, pp.1-259.
 
[34]  Horton, R. E. (1932). Drainage basin characteristics. Trans. Am. Geophys. Unions. 13, 350-361.
 
[35]  Gregory, K. J., and D. E. Walling. 1973. Drainage Basin Form and Process.London: Edward Arnold.
 
[36]  Mark B. Bain and Nathaniel J. Stevenson (1999), Drainage Basin, Aquatic Habitat Assessment: Common Methods, Published by American Fisheries Society.
 
[37]  Gray, D.M. (1965). Physiographic Characteristics and the Runoff Patterns: Proc.of Hydrol. Symp. No. 4, Research Watershed, National Research Council of Canada, pp 147-164.
 
[38]  Dune, T. and Leopold, L.B., 1978. Water in Environmental Planning. W.H. Freeman and Company. San Francisco, C.A.
 
[39]  Barton, D.R., Taylor, W.D., and Biette, R.M., 1978. Dimensions of Riparian Buffer Strips required to Maintain Trout Habitat in Southern Ontario Streams, North American ournal of Fisheries Management, 5, 364-378.
 
[40]  McKenney, R., Jacobsen, R. B. and Wertheimer, R. C. 1995. 'Woody vegetation and channel morphogenesis in low-gradient, gravel-bed streams in the Ozark Plateaus, Missouri and Arkansas', Geomorphology, 13, 175-198.