My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
PROJ00495
CWCB
>
Loan Projects
>
Backfile
>
1-1000
>
PROJ00495
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
11/19/2009 11:17:47 AM
Creation date
10/5/2006 11:58:08 PM
Metadata
Fields
Template:
Loan Projects
Contract/PO #
C153678
Contractor Name
Lower Arkansas Water Management Association
Contract Type
Loan
Water District
67
County
Prowers
Bill Number
SB 96-124
Loan Projects - Doc Type
Feasibility Study
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
99
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
<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />LAWMA WELL DEPLETIONS <br /> <br />The ground water in the alluvial and bench aquifers in the main stem area are <br />hydraulically connected to the Arkansas River. In general, the ground water in these aquifers <br />is in transit down gradient toward the Arkansas River. These aquifers are recharged with <br />water from several sources, including precipitation, deep percolation from irrigation, and <br />leakage from the surface streams in the area. They are discharged also through several <br />phenomena, including water consumption by phreatophytes and subirrigation, discharges into <br />tributaries and drains in the area, and water consumption from well pumpage. Pumping wells <br />constructed into these aquifers intercepts the ground water as it flows toward the Arkansas <br />River. The actual depletion to the flow in the Arkansas River from this well pumping, <br />however, is typically less than the consumption of the well water because not all the ground <br />water in transit would otherwise make it to the Arkansas River. Part of this ground water is <br />consumed by phreatophytes and subirrigation, by evapotranspiration in and along the <br />tributaries and drains in the area, and by diversions from the tributaries and drains. <br /> <br />Most of the well depletions affect Colorado surface rights. Some affect the flow at the <br />Stateline, either directly or through reduced return flow from Colorado surface rights. Not all <br />flow at the Stateline is usable in Kansas, so not all depletions at the Stateline are depletions <br />to usable flow. The augmentation program formulated in this feasibility study contemplates <br />replacements for well depletions both to Colorado surface water rights and to usable Stateline <br />flow. In order to make these replacements successfully, LAWMA must have procedures for <br />calculating both types of well depletions.. <br /> <br />For the purpose of determining depletions to Colorado surface rights, LAWMA's <br />consultants have recommended the application of certain "presumptive well depletion factors" <br />to the main stem irrigation pumping in order to provide a basis for reasonable replacement, <br />yet one which is simple for application. These well depletion factors are 30 percent for <br />supplemental pumping, 50 percent for non-center pivot sole-source pumping, and 75 percent <br />for center-pivot sole-source pumping. It is noted also that these well depletion factors have <br />been suggested in connection with the augmentation plan proposed for well owners in the <br />Southeastern Colorado Water Conservancy District. Additionally, LAWMA will calculate <br />depletions for the municipal and commercial pumping that affect Colorado surface rights on <br /> <br />12 <br />
The URL can be used to link to this page
Your browser does not support the video tag.