A Modified Groundwater Flow Model Using the Space Time Riemann-Liouville Fractional Derivatives Approximation

<table>Example of heterogeneous karst aquifer illustrating the duality of recharge (allogenic versus autogenic), infiltration (point versus diffuse), and porosity/flow (conduits versus matrix) [<a href="/journals/aaa/2014/498381/#B21">12</a>].</table>

Abstract and Applied Analysis

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Figure 1

Figure 1: A Modified Groundwater Flow Model Using the Space Time Riemann-Liouville Fractional Derivatives Approximation 