My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
HoleInTheRiverHistoryOfGroundwater
CWCB
>
Water Supply Protection
>
DayForward
>
1-1000
>
HoleInTheRiverHistoryOfGroundwater
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
1/26/2010 4:17:39 PM
Creation date
10/8/2007 9:36:09 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8420.500
Description
South Platte River Basin Task Force
State
CO
Basin
South Platte
Date
7/12/2007
Author
Nicolai A. Kryloff
Title
Hole In the River Draft Report Submitted to SPTF
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.
/
51
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
remembered unreliable summer flows near the tu rn of the century: “T he river used to be <br />so low,” he recalled, “we could cross it with just a common pair of Sunday shoes on <br />24 <br />without getting your feet wet.” In effect, the river would si mply sink away into the vast <br />aquifer below. <br />Unbeknownst to the early settlers, huma n activity had already begun to change <br />the character of both the river and the aquifer beneath it. In the upper reaches of the South <br />Platte, heavy farmland irrigation was causing what one contemporary called a “revolution <br />25 <br />in natural conditions.” This revolution was due to seepage water, an occurrence which <br />was articulated scientifically for the first time in the valley by L.G. Carpenter, a <br />researcher at Colorado’s State Agricultura l College in Fort Collins. In 1897, Carpenter <br />posited a “filling of the subsoil” by irrigati on runoff near the vall ey. Water levels had <br />26 <br />risen in some places by forty to sixty feet, and were continuing to rise. Before irrigation <br />came to the region, spring floodwaters common ly surged down the South Platte. But <br />beginning in the 1870s, irrigation companies bu ilt reservoirs to capture and save these <br />flows. When farmers applied this storage water to their crops, a substantial volume <br />soaked into the porous soil rather than flow ing away as floodwater, evaporating, or being <br />absorbed by plants. This seepage eventually reemerged in the river downstream, causing <br />volumes in the South Platte and its tributaries to rise. Most important to irrigators, the <br />flows became increasingly re gular during late summer a nd autumn, when the river <br />historically had been lowest – and when many crops most needed water. Carpenter <br />predicted these flows would only increase, valu ing them at more than two million dollars <br />24 <br /> Statement of Charles H. Lent, 1-2. Box 26, DEC. <br />25 <br /> Statement of Charles C. Huffsmith, 16. Box 26, DEC. <br />26 <br /> L.G. Carpenter, Seepage or Return Waters from Irrigation, The State Agricultural College Experiment <br />Station, Bulletin 33 (Fort Collins: Colorado Agricultural College, January 1896), 4, 51. <br />11 <br />
The URL can be used to link to this page
Your browser does not support the video tag.