Figure 14From: Lie group analysis and similarity solutions for hydro-magnetic Maxwell fluid through a porous mediumVariation of the dimensionless velocity distribution along the y -axis with t for different values of magmatic velocity V 0 ( U 0 = 2; y = 0; m 0 = m 1 = m 2 = 2; k = 0.05; R = 0.5; λ = 50; m = 0.5; M = 0.5).Back to article page