My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
2006-08-10_REVISION - M1977306
DRMS
>
Day Forward
>
Revision
>
Minerals
>
M1977306
>
2006-08-10_REVISION - M1977306
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
6/16/2021 6:21:15 PM
Creation date
11/21/2007 8:54:28 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M1977306
IBM Index Class Name
Revision
Doc Date
8/10/2006
Doc Name
Monitoring Well map
From
Cotter Corporation
To
DRMS
Type & Sequence
TR4
Media Type
D
Archive
No
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
24
PDF
Print
Pages to print
Enter page numbers and/or page ranges separated by commas. For example, 1,3,5-12.
After downloading, print the document using a PDF reader (e.g. Adobe Reader).
View images
View plain text
~. <br />GeoScience Services <br />a = surface tension <br />tp = ankle of capillarity <br />r = pore/capillarity radius <br />h = height of capillary use <br />Figure 1 The phenomenon of capillarity <br />1263 Kingston Road <br />Grand Junction, CO 81503 <br />(970) 314-3356 <br />As illustrated in Figure 1, water will rise in a capillary tube a distance of (h) depending <br />on the radius (r) of the capillary tube. Connected pores in soil or rock are analogous to a <br />capillary tube. The smaller the radius or the finer grain the soil, the greater the height (h) <br />the water will rise in the capillary. The height of rise (h) is a measurement of the matrix <br />potential (`Ym) and represents a negative pressure compared to atmospheric pressure-- <br />hence the term soil suction. <br />
The URL can be used to link to this page
Your browser does not support the video tag.