File:Newell-Article 1-Fig1.JPG
Revision as of 00:55, 9 May 2018 by Jhurley (talk | contribs) (Jhurley uploaded a new version of File:Newell-Article 1-Fig1.JPG)
Size of this preview: 550 × 599 pixels. Other resolutions: 220 × 240 pixels | 650 × 708 pixels.
Original file (650 × 708 pixels, file size: 139 KB, MIME type: image/jpeg)
Figure 1. Hydraulic gradient (typically described in units of m/m or ft/ft) is the difference in hydraulic head from Point A to Point B (ΔH) divided by the distance between them (ΔL). In unconfined aquifers, the hydraulic gradient can also be described as the slope of the water table. (Adapted from course notes developed by Dr. R.J. Mitchell, Western Washington University)
File history
Click on a date/time to view the file as it appeared at that time.
| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 01:07, 9 May 2018 | | 650 × 708 (139 KB) | Jhurley (talk | contribs) | |
| 00:56, 9 May 2018 |  | 650 × 708 (92 KB) | Jhurley (talk | contribs) | Reverted to version as of 12:33, 2 September 2016 (MDT) | |
| 00:55, 9 May 2018 |  | 550 × 599 (103 KB) | Jhurley (talk | contribs) | changed Well 2 label | |
| 18:33, 2 September 2016 |  | 650 × 708 (92 KB) | Debra Tabron (talk | contribs) | Figure 1. Hydraulic gradient (typically described in units of m/m or ft/ft) is the difference in hydraulic head from Point A to Point B (ΔH) divided by the distance between them (ΔL). In unconfined aquifers, the hydraulic gradient can also be describ... |
- You cannot overwrite this file.
File usage
The following file is a duplicate of this file (more details):
There are no pages that link to this file.
