Figure 3.

Effect of the magmatic field parameter Hax on θ(η) when Grx = 0.5, Gcx = 0.1, Df = 0.2, Sr = 0.3, and ξ = 0.01.

Sibanda et al. Boundary Value Problems 2012 2012:25   doi:10.1186/1687-2770-2012-25
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