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Tom Hatton Page 2 <br />December 9, 2010 <br />If the information you are providing to DRMS is pursuant to approach no. 4, you will need <br />to provide additional documentation to this office that specifies what water rights or other <br />permanent water source will be dedicated to the SWSP to assure that all permanent depletions <br />from either an unforeseen abandonment of the site by the Applicant or as a result of long term <br />ground water exposure after completion of mining and reclamation will be replaced so as to <br />prevent injury to other water rights. <br />This information must be provided to this office by April 30, 2011. If the requested <br />information is not provided to the Division of Water Resources, any future SWSP may limit the <br />mining operation so that additional ground water cannot be exposed, beyond that specified in <br />this SWSP. <br />Depletions <br />The exposed ground water surface area is 2.6 acres resulting in 6.00 acre-feet of evaporative <br />depletions. The aggregate production at the Wagner/Kauffman Pit #3 is projected to be 350,000 tons <br />which will consume 10.3 acre-feet of water lost with the mined product. The total estimated net <br />depletions for 2011 from this operation will be 16.3 acre-feet per year. <br />The mining operation has continuously dewatered directly back to the Big Thompson River since <br />2000. The estimated dewatering rate at the Wagner/Kauffman Pit #3 site is approximately 1000 gallons <br />per minute. As long as the pit is continuously dewatered, the water returned to the stream system <br />should be adequate to offset the depletions. Once dewatering at the site ceases the delayed depletions <br />must be addressed. <br />A stream depletion model was used to determine the timing of lagged depletions to the Big Thompson <br />River. The following parameters were used in the stream depletion model: transmissivity (T) = 50,000 gallons <br />per day per foot, specific yield (SY) = 0.2 (which is typical for an alluvial aquifer), the distance of the exposed <br />ground water to the river = 200 feet, and the location of the parallel impermeable boundary was estimated to <br />be 3,500 feet from the stream. Based on the above factors, the lagged stream depletions for the term of <br />this SWSP were estimated to be 16.3 acre-feet as shown on the attached Table 3. According to the <br />Applicant, the distance from the surface of the exposed ground water area to the Big Thompson <br />River was measured based on the down gradient extent of the exposed ground water surface <br />(nearest point). For purposes of this SWSP, the method used to measure the distance to estimate <br />the lagged depletions will be accepted, however any future SWSP must measure the distance from <br />the exposed ground water surface area to the Big Thompson River based on the centroid of the <br />exposed ground water surface. <br />Replacements <br />Replacement water for this pit will continue to be made available throughout the year from a <br />lease of 65 acre-feet of fully consumable water from the City of Loveland ("Loveland"). This lease also <br />applies to losses at another gravel pit, Kauffman Pit DRMS M 78-327. A copy of the lease associated <br />with the mining operation was provided to the State Engineer's Office with the plan request and a copy <br />of the lease is attached to this letter. The duration of the lease is from January 1, 2010 through <br />December 31, 2012. A 4 percent transit loss from Green Ridge Glade Reservoir to Wagner/Kauffman <br />Pit No. 3 has been applied to the delivery of the replacement water. <br />Under the terms of the lease, replacements can be made using a variety of water owned by <br />Lovelandtincluding, but not limited to, Windy Gap reusable effluent, Loveland Storage Reservoir water