My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
PERMFILE129948
DRMS
>
Back File Migration
>
Permit File
>
300000
>
PERMFILE129948
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
8/24/2016 10:30:54 PM
Creation date
11/25/2007 8:26:34 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981008A
IBM Index Class Name
Permit File
Doc Date
7/3/2007
Section_Exhibit Name
Section 2.04.7 Hydrology Description
Media Type
D
Archive
Yes
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
58
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
• mg/I and .39 mg/1, respectively) than during the irrigation season (6.8 mg/I, .49 mg/I and .08 mg/I, <br />respectively). These higheraverages fortheseconstituents at SW-N102 after the irrigation season <br />ended probably reflect the gradual recession of tail water discharge (hence, higher concentrations) <br />after irrigation ceases. <br />Surface water Site SW-N103 was situated in Calamity Draw about .6 miles downstream of <br />SW-N101. It was the furthest downstream monitoring site Peabody routinely monitored for water <br />quality in Calamity Draw. Monitoring for water quality at SW-N103 began in July of 1986 <br />(Attachment 2.04.7-11 (Peabody Appendix 7-9)). <br />The water type at Site SW-N103 for both seasons was a calcium magnesium sulfate (Attachment <br />2.04.7-10 (Peabody Appendix?-8)). Thiswatertypewasverysimilartowaterssampledupstream <br />in Calamity Draw at Site SW-N101. During periods of irrigation, the major ions at SW-N103 were <br />slightly lower than shown at SW-N101. This suggested that contributions to flow in Calamity Draw <br />between these sites due to irrigation tail water provided a dilution effect. <br />• Little variability between the seasons for pH was detected at SW-N103. During irrigation, pH <br />averages 7.84 and ranges from 6.84 up to 8.10 units. Afterthe irrigation season, pH averages 7.88 <br />and ranges between 7.50 and 8.06 units. <br />Similar to previously discussed surface water monitoring sites, the mean of TDS during the <br />non-irrigation season was more than double (3,135 mg/I) the mean for this constituent during the <br />irrigation period (1,371 mg/I). Again, the higher levels of the major ions in Calamity Draw at this <br />site after irrigation stops explains this trend. <br />At Site SW-N103, both TSS and FeT averaged higher during the irrigation period (57.0 mg/1 and <br />1.46 mg/I, respectively) than after irrigation has ceased (39.4 mg/I, TSS and 1.05 mg/I FeT). The <br />mean value of Fep was slightly higher (.04 mg/1) during the non-irrigation period compared to the <br />average Feo (.02 mg/I) determined for the irrigation season. As seen for all previously discussed <br />sites, MnT averaged consistently higher (1.24 mg/I) after the irrigation season ended than during <br />the irrigation period (.33 mg/I). <br />• West Lateral Irrigation Ditch -Flow and Water Quality. The West Lateral irrigation ditch is part <br />REVISED JULY 2006 2.04.7-33 <br />
The URL can be used to link to this page
Your browser does not support the video tag.