Revision history of "File:Newell-Article 1-Equation 1.jpg"

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  • (cur | prev) 18:50, 2 September 2016‎ Debra Tabron (talk | contribs)‎ . . (275 bytes) (+275)‎ . . (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...)
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