id	author	title	date	pages	extension	mime	words	sentence	flesch	summary	cache	txt
ejpam-2506	Shah, Kunjan	Solution of Burger's Equation in a One-Dimensional Groundwater Recharge by Spreading Using q-Homotopy Analysis Method	2016	11	.pdf	application/pdf	4026	217	62	If the porous medium is soil, water content is same as the soil moisture. The motion of water flow through unsaturated porous media is governed by continuity equation ∂ (ρSθ ) ∂ t = −∇M , (2) where ρS is the bulk density of medium on dry weight basis, θ is the moisture content at any depth Z on a dry weight basis and M is a mass of flux of moisture at any time t ≥ 0.	cache/ejpam-2506.pdf	txt/ejpam-2506.txt