File:Newell-Article 1-Equation 1.jpg
Revision as of 18:50, 2 September 2016 by Debra Tabron (talk | contribs) (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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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 be expressed this way.
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| current | 18:50, 2 September 2016 | | 973 × 272 (58 KB) | Debra Tabron (talk | contribs) | 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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