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2003-08-13_REVISION - M1979191
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2003-08-13_REVISION - M1979191
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Last modified
6/16/2021 5:45:34 PM
Creation date
11/21/2007 5:37:41 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M1979191
IBM Index Class Name
Revision
Doc Date
8/13/2003
Doc Name
Technical Revision
From
Lafarge West Inc.
To
DMG
Type & Sequence
TR1
Media Type
D
Archive
No
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REPLACEMENT WATER <br />In previous renewals, .the replacements for this site have been from a combination of direct <br />replacement of 1.0 Box Elder share during the summer months and ]ease from the City of Fort <br />Collins during the winter months. Now; 5.0 Box Elder Ditch will now be diverted irifo a recharge <br />pit instead of direct replacement. Leases from the Cities of Greeley and Fort Collins will made . <br />replacements for depletions not covered by the rechazge program. <br />Structures -Used for Recharge <br />Lafarge constructed a recharge.pit,on an unrnined portion of the permitted area of the DMG . <br />boundary of the Three Bells site. The recharge pit was excavated to only the upper portion of the <br />gravel deposit and did not expose additional ground water, so no additional evaporative loss will <br />occur. Water is delivered to the rechazge pit through an existing lateral from the ditch. <br />Augmentation by Recharge. <br />The Three Bells and Kyger Properties will obtain replacements from diverting 5.0 Box Elder shares <br />into a rechazge pit. A recharge model was used to determine the timing of the lagged consumptive <br />use credit from the shazes as it reached the Poudre River. A copy of the recharge model run is <br />included in Appendix B. <br />The recharge model was developed_usirig the following assumptions to model the historic <br />consumptive use credit reaching the Cache la Poudre River. <br />• The centroid of the recharge pit is approximately .1600 feet from the Poudre River. <br />• The transmissivity was assumed as 45,000 gal/day/ft. This value was assumed to be the <br />same as the transmissivity of a pump test well in the area. Source:. Groundwater Circular <br />No. 11, Loc. B6-6Z-18dba (Appendix B). <br />• The specific yield was assumed to be 0.2, which is typical for an alluvial aquifer. <br />•, The location of the parallel impermeable boundary was assumed to be a distance of 5000 <br />feet from a live stream. Source: USGS.Depth to the Water Table in the Boulder-Fort <br />Collins=Greeley Area, Front Range Urban Corridor, Colorado. <br />Table No. 3 summarizes the water balance for the augmentation plan based on the results of the <br />recharge model run for 2003. Per the requirement by the SEO, this plan will-only use real-time_ <br />historic use credit realized by the river during the 2003 season. Table No. 3 shows the real-time <br />stream depletions from the mining operation as well as the real-time replacements made by the <br />lagged timing of the historic consumptive use credit- _ <br />Page 3 <br />
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