My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
WSPC03939
CWCB
>
Water Supply Protection
>
Backfile
>
16000-16999
>
WSPC03939
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
1/26/2010 11:37:05 AM
Creation date
10/9/2006 4:17:16 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8460.500
Description
Platte River Basin - Endangered Species Issues - South Platte Recovery Program
State
CO
Basin
South Platte
Water Division
1
Date
12/5/1995
Author
Matthew J Cook
Title
South Platte Agreement - Groundwater Recharge as Augmentation for Restoring Wetlands Along the Central Platte River Nebraska - Final Report
Water Supply Pro - Doc Type
Report/Study
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
45
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 />II <br /> <br />I <br />I <br />I <br />I <br />I <br />il <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 />000671 <br /> <br />Elm Creek and Rowe Sanctuary sites were very similar in general topography to <br />the Crane Meadow site. <br />An in-depth review of the Platte River Wetland Hvdroloqv Studv by <br />Wesche et. al. (1994) was performed to determine the wet meadow site most <br />suitable for augmentation with groundwater recharge. The overall hydrologic <br />compatibility of each site with regard to implementation of a recharge basin was <br />investigated. <br />The "driest" of the three sites was Elm Creek, followed by Rowe <br />Sanctuary, with the Crane Meadows site being the "wettest". The term "driest" <br />refers to the average level of groundwater below the surface. The causes of the <br />lowest water table at the Elm Creek site are two-fold. First, the Elm Creek site is <br />adjacent to a very small channel of the Platte River. Surface water from the <br />Platte historically enters this channel only during high flows. At lower flows, the <br />channel is supplied primarily by a groundwater drainage canal that intercepts a <br />small channel near its inlet, about 1.3 miles west of the site (Wesche et. al. <br />1994). Second, another groundwater drainage canal is located along the <br />southern border of this study site. Groundwater drainage canals are used in the <br />area surrounding the study site to make croplands more accessible by lowering <br />the water table. The implementation of a recharge basin near this drain would <br />result in a significant portion of the recharge water draining away from the site <br />rather than raising the groundwater level for the benefit of the wet meadow <br />vegetation. <br />The Crane Meadows site located on the Mormon Island Crane Meadows <br />Wildlife Refuge was classified as the "wettest" site by Wesche et. al.(1994). <br />This site is characterized by a large proportion of low, seasonally flooded wet <br />meadows, with some higher dry meadows, and a tree lined fringe on the natural <br />levees bordering the river. During the inspection of the Crane Meadows site, Dr. <br />Paul Currier, Deputy Director; and Plant and Wetland Ecologist for the Platte <br />River Whooping Crane Maintenance Trust, believed that the Crane Meadow site <br />was already, essentially, the type of wet meadow most preferred by the migrating <br />Whooping Crane and that implementation of a recharge basin at this location <br /> <br />13 <br />
The URL can be used to link to this page
Your browser does not support the video tag.