My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
7431
CWCB
>
UCREFRP
>
Public
>
7431
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
7/14/2009 5:02:30 PM
Creation date
5/22/2009 6:10:09 PM
Metadata
Fields
Template:
UCREFRP
UCREFRP Catalog Number
7431
Author
Colorado River Salinity Program Coordinator.
Title
Salinity Update.
USFW Year
1989.
USFW - Doc Type
Denver, Colorado.
Copyright Material
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).
Show annotations
View images
View plain text
High salinity concentrations <br />result from two general processes: <br />salt loading and salt concentration. <br />Salt loading increases the amount of <br />salt added to a given amount of <br />water, and salt concentration <br />decreases the amount of dilution <br />water available for a given amount <br />of salt. <br />Specifically, salt loading in the <br />Colorado River system results in the <br />addition of mineral salts from <br />natural and manmade sources. Salt <br />concentration results in the rise in <br />salinity through beneficial <br />consumptive use of waters and <br />associated streamflow dr iletions in <br />the Basin that concentrate the salt <br />burden into a lesser volume of <br />water. Generally, the application of <br />irrigation water results in increased <br />salt loading because of salt leaching <br />and the concentrating effects of <br />consumptive use. The total salt <br />concentration in the river fluctuates <br />annually with the overall Basin <br />water supply. <br />A <br />t <br />I <br />M <br />P <br />r <br />T <br />f <br />D <br />a <br />m <br />M <br />9 <br />The Colorado River, at its <br />headwaters in the mountains of <br />north-central Colorado, has a <br />salinity (dissolved minerals) <br />concentration of only about <br />50 mg/L (milligrams per liter). The <br />salinity concentrations <br />progressively increase as the river <br />flows downstream as a result of <br />water diversion, evaporation from <br />reservoirs, and salt contributions <br />from a variety of sources. Recent <br />record-high flows have flushed and <br />filled the major reservoirs, resulting <br />in significantly lower salinity levels <br />at Imperial Dam - from an annual <br />average of 826 mg/L in 1982 to <br />621 mg/L (provisional) in 1987. <br />Without control measures, however, <br />the concentration is projected to <br />increase, following the overall rising <br />trend shown in figure 2, possibly <br />reaching a level of 966 mg/L* at <br />Imperial Dam by about 2010. <br />* The current projection is from 1988 <br />Evaluation of Salinity Control Programs <br />in the Colorado River Basin. <br />1000 ................................... <br />WO/Controls <br />950 ............................::.' <br />900 Standard <br />850 ..............."............I. <br /> <br />800 J ......... Al .... <br />750 ....................................... <br />700 ...... .................................... <br />650 .... :' ...................................... <br />600 <br />L 1985 1990 1995 2000 2005 2010 2015 2020 <br />Years <br />Figure 2. - Salinity projections with and without further controls 10/88.
The URL can be used to link to this page
Your browser does not support the video tag.