EFFECT OF GEOPHYSICAL PARAMETERS ON ATTENUATION OF CONTAMINANT IN FRESHWATER COASTAL AQUIFERS

Freshwater coastal aquifers can be contaminated by influx of seawater. The study investigated the effect of geophysical parameter such as seepage velocity (v) determined empirically on the mass flux (J) of contaminant through the coastal aquifers. Porosities of the grains were determined and tagged...

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Main Authors: ADEGOKE JAMES ADEYEMO, OLATUNDE I. POPOOLA, OLUDOTUN OMONIYI FALUYI
Format: Article
Language:English
Published: Alma Mater Publishing House "Vasile Alecsandri" University of Bacau 2019-03-01
Series:Journal of Engineering Studies and Research
Subjects:
Online Access:http://jesr.ub.ro/1/article/view/36
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spelling doaj-bff61d26be3e40eea10807c29ebb8da22021-10-05T15:54:24ZengAlma Mater Publishing House "Vasile Alecsandri" University of BacauJournal of Engineering Studies and Research2068-75592344-49322019-03-01251EFFECT OF GEOPHYSICAL PARAMETERS ON ATTENUATION OF CONTAMINANT IN FRESHWATER COASTAL AQUIFERSADEGOKE JAMES ADEYEMO0OLATUNDE I. POPOOLA1OLUDOTUN OMONIYI FALUYI2Department of Physics, University of Ibadan, Ibadan NigeriaDepartment of Physics, University of Ibadan, Ibadan NigeriaDepartment of Physics and Materials Science, Kwara State University, Malete Kwara State Nigeria Freshwater coastal aquifers can be contaminated by influx of seawater. The study investigated the effect of geophysical parameter such as seepage velocity (v) determined empirically on the mass flux (J) of contaminant through the coastal aquifers. Porosities of the grains were determined and tagged samples A to E. v was obtained in the experimental setup. Results showed that hydraulic gradient ranged between 3.233 to 0.317 while the corresponding values of contaminant J ranged between 0.302 to 5.381 Kgm-2s-1 within 60 to 360 seconds. Therefore, the attenuation coefficients of J decreased with increased in flow rate of fluid through the samples. http://jesr.ub.ro/1/article/view/36seepage velocityporosities, hydraulic gradientfreshwater and coastal aquifers
collection DOAJ
language English
format Article
sources DOAJ
author ADEGOKE JAMES ADEYEMO
OLATUNDE I. POPOOLA
OLUDOTUN OMONIYI FALUYI
spellingShingle ADEGOKE JAMES ADEYEMO
OLATUNDE I. POPOOLA
OLUDOTUN OMONIYI FALUYI
EFFECT OF GEOPHYSICAL PARAMETERS ON ATTENUATION OF CONTAMINANT IN FRESHWATER COASTAL AQUIFERS
Journal of Engineering Studies and Research
seepage velocity
porosities, hydraulic gradient
freshwater and coastal aquifers
author_facet ADEGOKE JAMES ADEYEMO
OLATUNDE I. POPOOLA
OLUDOTUN OMONIYI FALUYI
author_sort ADEGOKE JAMES ADEYEMO
title EFFECT OF GEOPHYSICAL PARAMETERS ON ATTENUATION OF CONTAMINANT IN FRESHWATER COASTAL AQUIFERS
title_short EFFECT OF GEOPHYSICAL PARAMETERS ON ATTENUATION OF CONTAMINANT IN FRESHWATER COASTAL AQUIFERS
title_full EFFECT OF GEOPHYSICAL PARAMETERS ON ATTENUATION OF CONTAMINANT IN FRESHWATER COASTAL AQUIFERS
title_fullStr EFFECT OF GEOPHYSICAL PARAMETERS ON ATTENUATION OF CONTAMINANT IN FRESHWATER COASTAL AQUIFERS
title_full_unstemmed EFFECT OF GEOPHYSICAL PARAMETERS ON ATTENUATION OF CONTAMINANT IN FRESHWATER COASTAL AQUIFERS
title_sort effect of geophysical parameters on attenuation of contaminant in freshwater coastal aquifers
publisher Alma Mater Publishing House "Vasile Alecsandri" University of Bacau
series Journal of Engineering Studies and Research
issn 2068-7559
2344-4932
publishDate 2019-03-01
description Freshwater coastal aquifers can be contaminated by influx of seawater. The study investigated the effect of geophysical parameter such as seepage velocity (v) determined empirically on the mass flux (J) of contaminant through the coastal aquifers. Porosities of the grains were determined and tagged samples A to E. v was obtained in the experimental setup. Results showed that hydraulic gradient ranged between 3.233 to 0.317 while the corresponding values of contaminant J ranged between 0.302 to 5.381 Kgm-2s-1 within 60 to 360 seconds. Therefore, the attenuation coefficients of J decreased with increased in flow rate of fluid through the samples.
topic seepage velocity
porosities, hydraulic gradient
freshwater and coastal aquifers
url http://jesr.ub.ro/1/article/view/36
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