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2020 | 139 | 2 | 102-114
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Modeling Soluble Contaminant Migration by Advection Process in Subsurface Water in the Eastern Niger Delta, Nigeria

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The advective property of an aquifer in the Eastern Niger Delta was evaluated using a conservative tracer. Tracer migration was monitored in observation boreholes at various radial distances simultaneously. Particle size distribution analysis for the sand samples collected from the boreholes in the study site revealed aquifer composition to be predominantly fine sand (silt =13.42%, fine sand = 41.76%, medium sand = 36.71% and coarse sand = 8.09%) for the 8m depth sampled. This field tracer test thus, provides a definitive data on the simultaneous transport of a soluble contaminant and allows a quantitative appraisal of the advective property of the study site. The mean velocity determined 1.212×10-3 ms-1, represents the advective velocity of groundwater carrying the dissolved tracer substance. This is an indication of how soluble components of hydrocarbon will be transported in the study area. Modeling tracer migration by advection process to estimate where and when a soluble contaminant problem can first be noticed in an environmental matrix and its application in hydrological studies is an effective tool to address problems such as sustainability and uncertainty in groundwater resource system.
Physical description
  • Department of Earth Sciences, Kogi State University, Anyigba, Nigeria
  • Department of Geology, University of Port Harcourt, Port Harcourt, Nigeria
  • Department of Geology, University of Port Harcourt, Port Harcourt, Nigeria
  • [1] R. G. Maliva, Tracer Tests. In: Aquifer characterization Techniques. Springer Hydrogeology. Springer, Cham. (2016) 403-443. DOI:
  • [2] L. Piccinini, P. Fabbri & M. Pola, Point dilution test to calculate groundwater velocity: an example in a porous aquifer in northeast Italy. Hydrological Science Journal 61(8) (2016) 1512-1523.
  • [3] S. Basirico, G. B. Crosta, P. Frattini, A. Villa & A. GODIO, Borehole flow meter logging for the accurate design and analysis of tracer tests. Groundwater 53(51) (2015) 3-9.
  • [4] W. Labaky, F. F. Devlin & R. W. Gillham, Field comparison of the point velocity probe with other groundwater velocity measurement methods. Water Resources Research 45(4) (2009) 1-9. doi: 10.1029/2008WR007066.
  • [5] M. S. Field, The Q tracer program for Tracer breakthrough curve Analysis for Karst and Fractured Rock Aquifers. Journal of Environmental Systems 23(4) (1999) 1-43.
  • [6] D. W. Chlebica & G. A. Robbins, Altering dissolved oxygen to determine flow conditions in fractured bedrock wells. Groundwater Monitoring and Remediation 33(4) (2013) 100-107.
  • [7] E. Behrens, F. U. Schwarzkopf, J. F. Lubbecke & C. W. Boning, Model simulations on the long term dispersal of 137Cs released into the Pacific Ocean off Fukushima. Environmental Research Letters 7(3) (2012) 034004. doi: 10.1088/1748-9326/7/3/034004.
  • [8] R. Testoni, R. Levizzari & M. De Salve, Tracer use for protection of water resources in nuclear sites. International Conference on Technologies and Materials for Renewable Energy, Environment and Sustainability, TMREES 15. Energy Procedia 74 (2015) 826-834.
  • [9] World Health Organization (WHO) Guideline for drinking water quality 4th edition, W.H.O. Press, Geneva Swizerland. (2011) 223-230.
  • [10] F. A. Kilpatrick & Jr. F. J. Wilson, Measurement of Time of Travel and Dispersion in Stream by Dye Tracing. Water resources Bulletin of the American Water Resources Association 22(4) (1989) 537-548.
  • [11] F. D. Giadom, E. G. Akpokodje & A. C. Tse, Determination of migration rates of contaminants in a hydrocarbon-polluted site using non-reactive tracer test in the Niger Delta, Nigeria. Environmental Earth Sciences (2015) 74(1). DOI: 10.1007/s12665-015-4094-3
  • [12] L. C. Amajor, Aquifer in the Benin Formation (Miocene-Recent), Eastern Niger Delta, Nigeria: lithosratigraphy, hydraulics and water quality. Journal of Environmental Geology 17(2) (1991) 85-101.
  • [13] P. M. Newton & L. H. Brian, A comparison of methods to determine K in a shallow coastal Aquifer. Groundwater 33(1) (1995) 49-57.
  • [14] D. R. Lee & A. J. Cherry, A field exercises on groundwater flow using Seepage meters and mini-piezometers. J. of Geol. Educ. 27(1978) 6-10
  • [15] M. T. Van Genuchten & W. J. Alves, Analytical solutions of the one-dimensional convective-dispersive solute transport equation. Techn. Bull., 1661, Washington D.C: US Department of Agriculture. (1982)
  • [16] M. I. Shutter, L. K. Deeks & M. F. Billet, Transport of conservative and reactive tracers through a naturally structured upland Podzol field lysimeter. Journal of hydrology 300(1-4): (2005) 1-19. doi: 10.1016/J.Jhydro.2004.04.026
  • [17] P. Fabbri & L. Piccinini, Assessing transmissivity from specific capacity in an alluvial aquifer in the middle Venetian plain (NE, Italy). Water Science & Technology. 67(9) (2013) 2000-2008. doi: 10.2166/Wst.2013.074
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