The Atmospheric Pressure in Dry Region and Velocity of Infiltered Water in Ground Water Infiltration Phenomenon

Please use this identifier to cite or link to this item: http://10.1.7.192:80/jspui/handle/123456789/3881

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DC Field	Value	Language
dc.contributor.author	Parikh, Amit K.	-
dc.contributor.author	Mehta, M. N.	-
dc.contributor.author	Pradhan, V. H.	-
dc.contributor.author	Patel, K. R.	-
dc.date.accessioned	2013-05-17T06:56:40Z	-
dc.date.available	2013-05-17T06:56:40Z	-
dc.date.issued	2011	-
dc.identifier.uri	http://10.1.7.181:1900/jspui/123456789/3881	-
dc.description	International Journal of Appl. Maths and Mech Vol. 7 (13) April, 2011, Page No. 77-90	en_US
dc.description.abstract	The non-linear partial differential equation of groundwater infiltration has been solved with appropriate boundary conditions and height of water mound is obtained in form of error function. The atmospheric pressure in air of the dry region have been obtained by using height of water mound and then the velocity of infiltered water have been obtained by using of Darcy’s law. The graphical presentation is given by using MAT LAB coding.	en_US
dc.relation.ispartofseries	ITFMT003-2	en_US
dc.subject	Infiltration	en_US
dc.subject	Pressure	en_US
dc.subject	Velocity	en_US
dc.subject	Darcy’s law	en_US
dc.subject	Mathematics and Humanities Faculty Paper	-
dc.subject	Faculty Paper	-
dc.subject	Maths Faculty Paper	-
dc.subject	ITFMT003	-
dc.title	The Atmospheric Pressure in Dry Region and Velocity of Infiltered Water in Ground Water Infiltration Phenomenon	en_US
dc.type	Faculty Papers	en_US
Appears in Collections:	Faculty Papers, Mathematics and Humanities

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