Modeling and simulation of dissolved lead in groundwater influenced by porosity and seepage velocity in homogeneous formation

Authors

  • Solomon Ndubuisi Eluozo Subaka Nigeria Limited Port Harcourt Rivers State of Nigeria

Keywords:

modeling and simulation dissolved lead in ground water

Abstract

Modeling and simulation of dissolved lead in groundwater influenced by porosity and seepage velocity in homogenous formation has been developed. Porosity influence were considered in the study area as the major role of lead transport, seepage velocity are through the degree of porosity of the soil, this formation characteristics were thoroughly examined, the variables were applied to formulate a system, this system denoted with mathematical tools that developed a governing equation. These equations were derived and it generated a model to monitor the rate of dissolved lead influenced by porosity and seepage velocity in homogenous formation. The developed model was compared with the experimental values from other locations for validation. The model confirmed the fitness of both parameters, the validation of this model implies that the model should be applied to monitor the dissolved lead in the study location. The figures were found to be increasing gradually and rapidly in several locations, these are based on the influence of porosity and seepage velocity. It is recommended that risk assessment should be thoroughly done to reduce the type of pollution in the study area.

References

Georg, M., 1976. Effects of man's activities on groundwater qualityHydrological Sciences-lletin-des Sciences Hydrologiques, XXI, 4 12/1976

Schneider, H., 1964. Geohydrologie Nordwestfalens: Schmidt, Berlin-Konradshôhe.

Schwille, F., 1964. Die 'hydrologischen' Grundlagen fur die Untersuchung, Beurteilung und Sanierungvon Mineralôlkontaminationen des Untergrundes. Dt. gewàsserkdl. Mitt. 8 (1), 1-16.

Schwille, F., 1966. Die Kontamination des Untergrundes durch Mineralôl-ein hydrologisches Problem.Dt. gewàsserkdl. Mitt. 10 (6), 194-207.

Schwille, F., 1969. Hone Nitratgehalte in den Brunnenwassern der Moseltalaue zwischen Trier undKoblenz. Gas- u. Wasserf. 110 (2), 35-44.

Schwille, F., Vorreyer, C., 1969. Durch Mineralôl 'reduzierte' Grundwàsser. Gas- u. Wasserf. 110(44), 1225-1232.

Matthess, G., 1958. Geologische und hydrochemische Untersuchungen in der ôstlichen Vorderpfalz zwischen Worms und Speyer. Notizbl. hess. L.-Amt Bodenf. 86, 335-378.

Matthess, G., 1970. Beziehungen zwischen geologischem Bau und Grundwasserbewegung in Festgesteinen.Abh. hess. L.-Amt Bodenf. 58.

Matthess, G., 1972. Hydrogeologic criteria for the self-purification of polluted groundwaters. Intern. Geol. Congress 11, 296-304.

Matthess, G., 1973. Die Beschaffenheit des Grundwassers: Bomtraeger, Berlin-Stuttgart.

Matthess, G., 1974. Heavy metals as trace constituents in natural and polluted groundwaters. Geol. enMijnbouw 53 (4), 149-155.

Golwer, A., 1973. Beeinflussung des Grundwassers durch Strassen. Z. dt. Geol. Ges. 124,435-446.

Golwer, A., Knoll, K.H., Matthess, G., Schneider, W., Wallhâusser, K.H., 1972a. Mikroorganismen imUnterstrom eines Abfallplatzes. Gesundh.-Ing. 93, 142-152.

Golwer, A., Matthess, G., 1972. Die Bedeutung des Gasaustausches in der Grundluft fiir die Selbstreinigungsvorgàngein verunreinigten Grundwàssern. Z. dt. Geol. Ges. 123, 29-38.

Golwer, A., Matthess, G., Schneider, W., 1970. Selbstreinigungsvorgange im aeroben und anaerobenGrundwasserbereich. Vom Wasser 36, 64-92.

Golwer, A., Matthess, G., Schneider, W., 1972b. Contamination de l'eau souterraine par des depots dedéchets et implications pour les méthodes d'évacuation des residues. Tribune Cebedeau 25, 347,428-433.

Golwer, A., Schneider, W., 1973. Belastung des Bodens und des unterirdischen Wassers durch Strassenverkehr

World Health Organization 2007. Health risks of heavy metals from long-ange transboundary air pollution WHO Regional Office for Europe Scherfigsvej 8.

Published

2012-12-28

How to Cite

Ndubuisi Eluozo, S. . (2012). Modeling and simulation of dissolved lead in groundwater influenced by porosity and seepage velocity in homogeneous formation. Scientific Journal of Pure and Applied Sciences, 1(3), 97-104. Retrieved from http://sjournals.com/index.php/sjpas/article/view/1021

Issue

Section

Environmental Sciences

Most read articles by the same author(s)