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Modelling Homogeneous Deposition of Velocity Influenced by Porosity in Penetrating Unconfined Bed, Mbiama Coastal Location, Niger Delta of Nigeria

Received: 30 September 2016     Accepted: 1 March 2017     Published: 31 March 2017
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Abstract

This paper monitor the rate of homogeneous velocity in soil and water environment, several experts in different ways has developed other homogeneity of velocity outside deltaic formation, but the development model were to monitor the deposition of homogeneous velocity in the study location, this will generate monitoring of yield rate in the abstraction of ground water in the study environment, such condition were found significant to bleach the gap on monitoring and evaluation of homogeneous flow rate through predictive model, groundwater abstraction will definitely reduces abortive well through this source, the derived model will definitely monitor homogeneity of flow in design and construction of water wells, the developed concept will predict the homogeneous flow velocity in deltaic environment. The study has provided various dimensions that have generated the homogeneity of velocity through application of this derived model, experts will find this study significant in determining the homogeneous velocity of flow in deltaic formation.

Published in American Journal of Environmental Science and Engineering (Volume 1, Issue 1)
DOI 10.11648/j.ajese.20170101.14
Page(s) 22-25
Creative Commons

This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited.

Copyright

Copyright © The Author(s), 2017. Published by Science Publishing Group

Keywords

Modelling Homogeneous, Velocity, Unconfined Bed

References
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[2] Bodner, G., Loiskandl, W., Buchan, G., Kaul, H. P., 2008. Natural and management-induced dynamics of hydraulic conductivity along a cover-cropped field slope. Geoderma 146, 317-325.
[3] Chan, K. Y., Heenan, D. P., Ashley, R., 1994. Seasonal changes in surface aggregate stability under different tillage and crops. Soil and Tillage Research 28, 301-314.
[4] Kodešová, R., Kodeš, V., Žigová, A., Šimunek, J., 2006. Impact of plant roots and soil rganisms on soil micro morphology and hydraulic properties. Biologia 61, S339–S343.
[5] Kodešová, R., Kocárek, M., Kodeš, V., Šimunek, J., Kozák, J., 2008. Impact of soilicromorphological features on water flow andherbicide transport in soils. Vadose Zone Journal 7, 798–809.
[6] Kodešová, R., Vignozzi, N., Rohošková, M., Hájková, T., Kocárek, M., Pagliai, M., Kozák, J., Šimunek, J., 2009a. Impact of varying soilstructure on transport processes in different diagnostic horizons of three soil types, Journal of Contaminant Hydrology 104, 107-125.
[7] Kodešová, R., Rohošková, M., Žigová, A., 2009b. Comparison of aggregate stability within six soilprofiles under conventional tillage using various laboratory tests. Biologia 64, 550-554.
[8] Messing, I., Jarvis, N. J., 1993. Temporal variationin the hydraulic conductivity of a tiled clay soil as measured by tension infiltrometer. Journal of Soil Science 44, 11-24.
[9] Murphy, B. W., Koen, T. B., Jones, B. A., Huxedurp, L. M., 1993. Temporal variation of hydraulic properties for some soils with fragile structure. Australian Journal of Soil Research 31, 179-197.
[10] Petersen, C. T., Hansen, S., Jensen, H. E., 1997. Tillage-induced horizontal periodicity of preferential flow in the root zone. Soil Science Society of America Journal 61, 586-594.
[11] Somaratne, N. M., Smettem, K. R. J., 1993. Effect of cultivation and raindrop impact on the surface hydraulic properties of an alfisol under wheat. Soiland Tillage Research 26, 115-125.
[12] Strudley, W. M., Green, T. R., Ascough, I. I. J. C., 2008. Tillage effects on soil hydraulic properties inspace and time: State of the science. Soil and Tillage Research 99, 4-48.
[13] Suwardji, P., Eberbach, P. L., 1998. Seasonal changes of physical properties of an Oxic Paleustalf Red Kandosol) after 16 years of directdrilling or conventional cultivation. Soil and Tillage Research 49, 65-77.
[14] Yang, X. M., Wander, M. M., 1998. Temporal changes in dry aggregate size and stability. Soiland Tillage Research 49, 173-183.
[15] Eluozo, S. N. 2013 Modeling and simulation topredict nitrogen deposition influenced by the Porosity and the coefficient of inhibition in thecoastal area of Port Harcourt, Niger delta ofNigeria Health, Safety and Environment (2013) 1 (2) 29-40.
[16] Eluozo, S. N. 2014; Two Dimensional Flow Transport Modeling of Fungi and Arsenic Deposition on Lateritic and Silty Formation in Coastal Area of Aboluma, Niger Delta of Nigeria, ARPN Journal of Science and Technology March Vol. 4, No 3.
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  • APA Style

    Eluozo S. N. (2017). Modelling Homogeneous Deposition of Velocity Influenced by Porosity in Penetrating Unconfined Bed, Mbiama Coastal Location, Niger Delta of Nigeria. American Journal of Environmental Science and Engineering, 1(1), 22-25. https://doi.org/10.11648/j.ajese.20170101.14

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    ACS Style

    Eluozo S. N. Modelling Homogeneous Deposition of Velocity Influenced by Porosity in Penetrating Unconfined Bed, Mbiama Coastal Location, Niger Delta of Nigeria. Am. J. Environ. Sci. Eng. 2017, 1(1), 22-25. doi: 10.11648/j.ajese.20170101.14

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    AMA Style

    Eluozo S. N. Modelling Homogeneous Deposition of Velocity Influenced by Porosity in Penetrating Unconfined Bed, Mbiama Coastal Location, Niger Delta of Nigeria. Am J Environ Sci Eng. 2017;1(1):22-25. doi: 10.11648/j.ajese.20170101.14

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  • @article{10.11648/j.ajese.20170101.14,
      author = {Eluozo S. N.},
      title = {Modelling Homogeneous Deposition of Velocity Influenced by Porosity in Penetrating Unconfined Bed, Mbiama Coastal Location, Niger Delta of Nigeria},
      journal = {American Journal of Environmental Science and Engineering},
      volume = {1},
      number = {1},
      pages = {22-25},
      doi = {10.11648/j.ajese.20170101.14},
      url = {https://doi.org/10.11648/j.ajese.20170101.14},
      eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.ajese.20170101.14},
      abstract = {This paper monitor the rate of homogeneous velocity in soil and water environment, several experts in different ways has developed other homogeneity of velocity outside deltaic formation, but the development model were to monitor the deposition of homogeneous velocity in the study location, this will generate monitoring of yield rate in the abstraction of ground water in the study environment, such condition were found significant to bleach the gap on monitoring and evaluation of homogeneous flow rate through predictive model, groundwater abstraction will definitely reduces abortive well through this source, the derived model will definitely monitor homogeneity of flow in design and construction of water wells, the developed concept will predict the homogeneous flow velocity in deltaic environment. The study has provided various dimensions that have generated the homogeneity of velocity through application of this derived model, experts will find this study significant in determining the homogeneous velocity of flow in deltaic formation.},
     year = {2017}
    }
    

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    AB  - This paper monitor the rate of homogeneous velocity in soil and water environment, several experts in different ways has developed other homogeneity of velocity outside deltaic formation, but the development model were to monitor the deposition of homogeneous velocity in the study location, this will generate monitoring of yield rate in the abstraction of ground water in the study environment, such condition were found significant to bleach the gap on monitoring and evaluation of homogeneous flow rate through predictive model, groundwater abstraction will definitely reduces abortive well through this source, the derived model will definitely monitor homogeneity of flow in design and construction of water wells, the developed concept will predict the homogeneous flow velocity in deltaic environment. The study has provided various dimensions that have generated the homogeneity of velocity through application of this derived model, experts will find this study significant in determining the homogeneous velocity of flow in deltaic formation.
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Author Information
  • Department of Civil and Environmental Engineering, Subaka Nigeria Limited Port Harcourt, Port Harcourt, Nigeria

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