My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
2020-04-30_HYDROLOGY - M2008017
DRMS
>
Day Forward
>
Hydrology
>
Minerals
>
M2008017
>
2020-04-30_HYDROLOGY - M2008017
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
3/15/2021 11:05:39 AM
Creation date
4/30/2020 3:11:36 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M2008017
IBM Index Class Name
Hydrology
Doc Date
4/30/2020
Doc Name Note
GW Modeling Rpt
Doc Name
Hydrology Report
From
Operator
To
DRMS
Permit Index Doc Type
Hydrology Report
Email Name
ECS
MAC
Media Type
D
Archive
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).
View images
View plain text
Derr Pit - Groundwater Modeling Report <br />January 31, 2020 Page 2 of 24 <br />McGrane Water Engineering, LLC <br />1669 Apple Valley Rd. Lyons, CO 80540 Phone: (303) 917-1247 <br />E-Mail: dennis@mcgranewater.com Web: ttp://www.mcgranewaterengineering.com <br />upgradient side and decline on the downgradient side. Water level increases to within 10 feet of <br />the surface on the upgradient side of the pit could threaten flooding of basements, and in extreme <br />cases if water levels increase closer to ground surface encourage phreatophyte (such as cattails) <br />growth. A decline in water levels on the downgradient side could reduce the aquifer saturated <br />thickness and well yields if the decline is significant compared to the pump setting depth. <br />Available Data <br />We compiled hydrogeologic data from: <br />Existing reports from the U.S. Geological Survey and Colorado Division of Water <br />Resources (see Sources below); <br />Well permit completion reports from 133 registered alluvial wells (DWR wells) available <br />from the State’s Well database located within the study area; <br />Water level data from 18 monitoring wells located around the Derr pit; and <br />Water levels measured at 15 offsite private registered wells located within a mile of the <br />site. <br />Hydrogeology <br />The hydrogeology of the SPR alluvial aquifer is described by Lindsay and Others (1998 and <br />2005), CDM (2006 and 2013) and CSU (2013). Figure 2 shows the site surficial geology by <br />Tweto, 1979). The alluvium within the model areas consists of alluvial sand and gravel (Qa) <br />adjacent to the modern SPR and Poudre River flood plains, and older terrace alluvium (Qg) <br />outside the floodplain. The alluvium thins to the northeast where the Laramie shale (Kl) <br />outcrops just outside the northeast corner of the model area. <br />Table 1 (end of report) shows compiled pertinent well data that includes: location (Colorado <br />State Plane North coordinates) depth, yield (gpm), water level when drilled, and depth to <br />bedrock calculated from geologic logs (if available). The upper portion of the Table shows the 18 <br />Derr borehole/monitoring well data. The average well depth, water level when drilled and depth <br />to bedrock are 95, 13, and 85 feet respectively. <br />The center portion of the table include 15 private DWR wells that are currently being monitored <br />by BAI that are located within 1 mile of the Derr pit. The average well depth, water level when <br />drilled and depth to bedrock are 67, 28, and 60 feet respectively. The deeper depths reflect <br />ground surface elevations that increase to the north. Well yields range from 7 to 1200 gpm. <br />The lower portion of the table contain the remaining DWR wells within the model area. The <br />average well depth, water level when drilled and depth to bedrock are 51, 19, and 58 feet <br />respectively, whereas, well yields range from 0.75 to 1400 gpm. <br />Predevelopment Water Level Contours <br />Figure 2 shows the geology and reported water levels when drilled which best represent <br />“predevelopment” or pre-mining conditions. The predevelopment water table elevation at wells, <br />and for the Poudre River (at 10 ft increments), were calculated by subtracting the depth to water
The URL can be used to link to this page
Your browser does not support the video tag.