File:Newell-Article 1-Equation 1.jpg
Size of this preview: 800 × 224 pixels. Other resolutions: 320 × 89 pixels | 973 × 272 pixels.
Original file (973 × 272 pixels, file size: 58 KB, MIME type: image/jpeg)
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.
File history
Click on a date/time to view the file as it appeared at that time.
| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| 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... |
- You cannot overwrite this file.
File usage
There are no pages that link to this file.
