ABSTRACT
The behaviour of clostridium transport were observed not to be shown concern in the study area, the migration process were observed through most physiochemical analysis that find out the rate of concentration in water supply around the community, the alarming rate of its contamination are seriously causing hundred of ill health in the study location , most settlers
in the study area does not know their cause of ill health thus the sources of this disease, there is need for thorough evaluation of ground water supply in the study location. Lots of evaluation made previously could not produced detailed results, the application of this modelling techniques generated detailed sources of contaminant and their various rate of concentration at different depth and time, the migration process and causes of exponential and vacillation were determined from the derived model simulation values, the study is imperative because it has generated the sources thoroughly and predicted their rate of concentration under the influences of predominated porosity in the study area.
Keywords: Modelling, Simulation, Permeability, Clostridium, Transport, Coarse Formation.
[1].Kozák J., Vacek O. (1996): The mathematical model (BPS) for prediction of pesticide behaviour in soil. Rostlinná Výroba, 42: 69–76.
[2]. Poletika N.N., Jury W.A., Yates M.V. (1995): Transport of bromide, simazine, and MS-2 coliphage in a lysimeter containing undisturbed, unsaturated soil. Water Resources Research, 31: 801–810.
[3].Streck T., Poletika N.N., Jury W.A., Farmer W.J. (1995): Description of simazine transport with rate-limited, two-stage, linear and nonlinear sorption. Water Resources Research, 31: 811–822.
[4].Ko?árek M., Kodešová R., Kozák J., Drábek O., Vacek O. (2005): Chlortoluron behaviour in five varying soil types. Plant, Soil and Environment, 51: 304–309.
[5].Flury M., Leuenberger J., Studer B., Flühler H. (1995): Transport of anions and herbicides in a loamy and sandy field soil. Water Resources Research, 31: 823–835.
[6].Kamra S.K., Lennartz B., van Genuchten M.Th., Widmoser P. (2001): Evaluating non-equilibrium solute transport in small soil columns. Journal of Contaminant Hydrology, 48: 189–212.
[7].FOCUS (2000): FOCUS groundwater scenarios in the EU plant protection product review process. Report of the FOCUS Groundwater Scenarios Workgroup, EC Document Reference Sanco/321/2000, DG SANCO, EU Commission, Brussels
[8]. Jorgensen P.R., Hoffmann M., Kistrup J.P., Bryde C. (2002): Preferential flow and pesticide transport in a clay-rich till: Field, laboratory, and modeling analysis. Water Resources Research, 38 (11).
[9].Therrien R., Sudicky E.A. (1996): Three-dimensional analysis of variably-saturated flow and solute transport in discretely-fractured porous media. Journal of Contaminant Hydrology, 23: 1–44.
[10]. Gerke H.H., van Genuchten M.Th. (1996): Macroscopic representation of structural geometry for simulating water and solute movement in dual-porosity media. Advances in Water Resources, 19: 343–357.
[11]. Gerke H.H., van Genuchten M.Th. (1993): A dual-porosity model for simulating the preferential movement of water and solutes in structured porous media. Water Resources Research, 29: 305–319.
[12]. Jarvis N.J. (1994): The MACRO model. Technical description and sample simulation. Reports and dissertations 19. Department of Soil Science, Swedish University of Agricultural Science, Uppsala, Sweden.
[13]. Besien T.J., Jarvis N.J., Williams R.J. (1997): Simulation of water movement and isoproturon behaviour in a heavy clay soil using the MACRO model. Hydrology and Earth System Sciences, 4: 835–844.
[14].Šim?nek J., Jarvis N.J., van Genuchten M.Th., Gär-denäs A. (2003): Review and comparison of models for describing non-equilibrium and preferential flow and transport in the vadose zone. Journal of Hydrology, 272: 14–35.
[15].Šim?nek J., Šejna M., van Genuchten M.Th. (1998): The HYDRUS-1D software package for simulating the one-dimensional movement of water, heat and multiple solutes in variably-saturated media. Version 2.0. IGWMC-TPS-53. International Ground Water Modeling Center, Colorado. School of Mines, Golden, CO.
[16]. Kodešová R., Kozák J., Vacek O. (2004): Field and numerical study of chlorotoluron transport in the soil profile. Plant, Soil and Environment, 50: 333–338.
[17].Kodešová1, R. Kozák1, J. Šim?nek, J. Vacek O. (2005): Single and dual-permeability models of chlorotoluron transport in the soil profile Supported by the Ministry of Agriculture of the Czech Republic, Project No. QF3250. Plant soil Environ. 51, (7): 310–315.