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2014-02-28_HYDROLOGY - M1977522
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2014-02-28_HYDROLOGY - M1977522
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Last modified
8/24/2016 5:40:25 PM
Creation date
3/4/2014 3:47:40 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M1977522
IBM Index Class Name
HYDROLOGY
Doc Date
2/28/2014
Doc Name
Substitute water supply plan
From
Division of Water Resources
To
Parsons Water Consulting, LLC
Email Name
ECS
Media Type
D
Archive
No
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Mr. Rick Parsons, P.E. <br />L.G. Everist Combined SWSP <br />Page 4 of 10 <br />February 27, 2014 <br />The net evaporation for the Firestone Pit includes a credit of 0.60 acre -feet of consumptive use of <br />ground water associated with the partial subirrigation of the historically irrigated acreage. No other <br />phreatophyte credit was applied to the other sites. Computation of evaporation under this plan was <br />reduced during the ice covered periods. You have assumed the ice covered period to occur during the <br />months of December, January and February, based on average monthly temperatures less than 32 °F <br />taken from the Longmont 2ESE weather station for the Saint Vrain Pits and Fort Lupton 2SE station for <br />the South Platte Pits, and for December and January for the Cache La Poudre site based on the monthly <br />temperatures taken from the Greeley UNC weather station. However, for the purpose of this SWSP, the <br />Applicant shall replace the net evaporation depletions from the exposed ground water surface area that <br />may occur during the assumed ice covered period (the months of January, February and December) for <br />any time that the pits are not completely covered by ice. <br />Computation of the net evaporation during any time that the pits are not completely covered by <br />ice shall be determined as the pro -rata amount of the monthly gross evaporation rate distribution amount <br />identified in the State Engineer's General Guidelines for Substitute Supply Plans for Sand and Gravel <br />Pits, subtracting the pro -rata amount of the effective precipitation for that period. <br />The material excavated from the gravel pit areas will be washed on site. The consumptive use of <br />water associated with excavated material is dependent on the location of the material with respect to the <br />water table. According to the "General Guidelines for Substitute water Supply Plans for Sand and Gravel <br />Pits" the product moisture loss is calculated as four percent by weight of mine material excavated below <br />the ground water table and two percent by weight for the mined material excavated above water table. <br />The Applicant anticipates 2014 mining production at the Carbon Valley Resource, Rinn Valley Pit, <br />Firestone Pit and Fort Lupton Sand and Gravel to be 150,000 tons, 580,000 tons, 200,000 tons and <br />1,650,000 tons respectively. For 2015, production at these same sites are anticipated to increase to <br />200,000 tons, 580,000 tons, 450,000 and 1,800,000 tons, respectively. <br />Water used for dust control at Carbon Valley Pit, Rinn Valley Pit, Firestone Pit and Star Water <br />Resources will come from water originally pumped from the pits for dewatering. Water used for dust <br />control at the Fort Lupton Sand and Gravel was previously used from an existing alluvial well, permit no. <br />57957 -F (WDID 0205018 DI TIRRO WELL 2), located outside of the approved slurry wall on the Fort <br />Lupton Pit site. Well permit no. 57957 -F is no longer being used for dust control, as Everist has a re- <br />circulating water system at the site where reusable water is pumped from lined cells to wash material and <br />for dust control. <br />Continuous dewatering operations at Carbon Valley Pit, Rinn Valley Pit, and Firestone Pit are <br />occurring in order to facilitate dry mining conditions. This water is used for dust control at these pits, and <br />is used for concrete production at the Rinn Valley pit. All other water pumped for dewatering is returned <br />immediately to the river system. The applicant has performed a lagged water balance for these <br />operations and account for the lagged depletions which is offset by monthly net accretions. Totalizing <br />flow meters have been installed and monthly meter readings showing dewatering volumes were reported <br />on the 2012 -2013 submitted accounting. <br />A stream depletion model using the Glover method was used to calculate the lagged depletions <br />to the River. The alluvial aquifer model uses four aquifer input parameters for each site as follows: 1) X- <br />distance from centroid of the well to the river, 2) W- distance from the aquifer boundary through the well <br />to the river channel, 3) T- transmissivity of the alluvial aquifer (in gallons per foot/day) between the well <br />and the river, and 4) S- specific yield. The following parameters for each site listed in the table below <br />were used in the model: <br />TABLE E — AQUIFER CHARACTERISTICS <br />Site Name <br />T <br />X <br />W <br />S <br />Carbon Valle Pit <br />50,000 <br />2,000 <br />4,173 <br />0.2 <br />
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