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• 18:50, 2 September 2016 Debra Tabron (talk | contribs) uploaded File:Newell-Article 1-Equation 1.jpg (In unconsolidated geologic settings (gravel, sand, silt, and clay) and highly fractured systems, the rate of groundwater movement can be expressed using Darcy’s Law. This law is a fundamental mathematical relationship in the groundwater field and can...)