Modelling the flow of water in stratified layers of sand

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DC Field	Value	Language
dc.contributor.author	Popoola, O. I	-
dc.contributor.author	Adegoke, J. A.	-
dc.contributor.author	Alabi, O. O.	-
dc.date.accessioned	2018-10-09T10:37:56Z	-
dc.date.available	2018-10-09T10:37:56Z	-
dc.date.issued	2011	-
dc.identifier.other	Journal of the Nigerian Association of Mathematical Physics 18, pp. 119-130	-
dc.identifier.other	ui_art_popoola_modelling_2011	-
dc.identifier.uri	http://ir.library.ui.edu.ng/handle/123456789/1362	-
dc.description.abstract	"The phenomenon of deflection of flow of water in porous media of different porosities with porosity ratio, ᵠ, is similar to fact that there is deviation in fluid flow in a pair of media of different densities. Theoretically, the relationship between preferred direction of flow of water, 0, and the sand layers of porosity ratio,ᵠ was found to be cos 0=nᵠ while experimentally it was obtained to be cos 0=1.98 In ᵠ+1.13 (0.5951≤ᵠ≤0.9634). Thereafter, when the theoretical equation was compared with the experimental result, the value of n ranging from 0 to 1 were found to be appropriate for the theoretical equation to be valid "	en_US
dc.language.iso	en	en_US
dc.title	Modelling the flow of water in stratified layers of sand	en_US
dc.type	Article	en_US
Appears in Collections:	Scholarly works

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