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2024-03-15_HYDROLOGY - M2016085
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2024-03-15_HYDROLOGY - M2016085
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Last modified
3/18/2024 10:27:46 AM
Creation date
3/18/2024 9:55:04 AM
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Template:
DRMS Permit Index
Permit No
M2016085
IBM Index Class Name
Hydrology
Doc Date
3/15/2024
Doc Name
Substitute Water Supply Plan
From
Division of Water Resources
To
DRMS
Email Name
BFB
JLE
Media Type
D
Archive
No
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NCCI Bennett Gravel Pit SWSP Page 2 of 5 <br /> March 15, 2024 <br /> that result from mining related exposure of groundwater. The DRMS letter identifies four approaches <br /> to satisfy this requirement. <br /> In accordance with approach nos. 1 and 3, the Applicant has indicated that a bond has been obtained <br /> for$1,077,271.00 through the DRMS for lining of this site to assure that depletions from groundwater <br /> evaporation do not occur in the unforeseen event(s) that would lead to the abandonment of the Pit. <br /> Depletions <br /> The projected depletions for the period of this SWSP consist of net evaporation from exposed <br /> groundwater surface area, water removed in the mined product and dust suppression. <br /> Evaporation <br /> The Applicant anticipates 0.85 acres of exposed surface area at the site outside of the north cell lined <br /> area. Gross annual evaporation at the gravel pit location was estimated to be 44.00 inches per year. Net <br /> evaporation is defined as gross evaporation less the consumptive use of water by vegetation that naturally <br /> occurred at the site prior to construction of the pit. The historical consumptive use was assumed to be <br /> equal to the effective precipitation, which was estimated based on the data from the Brighton NOAA <br /> weather station (record 1982-2022). The net evaporation from the exposed water surface is estimated <br /> at 2.9 acre-feet/acre, as shown in attached Table 1. <br /> Computation of evaporation under this SWSP was reduced during the ice-covered period. You have <br /> assumed the ice-covered period will occur during the month of February based on average monthly <br /> temperatures less than 32°F taken from the Brighton (record 1982-2022) NOAA weather station. However, <br /> for the purpose of this SWSP, the Applicant shall replace the net evaporation depletions from the exposed <br /> groundwater surface area that may occur during the assumed ice-covered period (the month of February) <br /> for any time that the pit is not completely covered by ice. After accounting for the ice cover month, the <br /> net evaporation from the exposed water surface is estimated at 2.34 acre-feet during this SWSP period, <br /> as shown in attached Table 1. <br /> Water Lost from Mined Product <br /> In addition to evaporation, water is lost with the mined product removed from the mine site. The <br /> applicant projects approximately 750,000 tons of product will be mined within the lined boundary. Gravel <br /> mined will be in a dewatered state and after washing, the groundwater lost with the mined product <br /> during this SWSP period is estimated at 2% by weight. The water used for washing the aggregate is <br /> projected to total 11 acre-feet during the SWSP period, as shown in attached Table 2. <br /> Dust Suppression <br /> The estimated water used for dust suppression during the SWSP period totals 9.6 acre-feet, as shown in <br /> attached Table 2. <br /> Total Consumptive Use <br /> The total consumptive use at the site during this SWSP period is 23.0 acre-feet as shown on Table 2. The <br /> total lagged depletions for this SWSP period from evaporation, operational losses and current dust <br /> suppression are 22.1 acre-feet, as shown in attached Table 2. <br /> The IDS AWAS stream depletion model was used to determine the lagged depletions from the previous <br /> evaporation and operational losses to the South Platte River. The aquifer characteristics used in the <br /> model for the alluvial well are: transmissivity (T) = 133,667 gallons per day per foot, specific yield (SY) <br /> = 0.2, the distance from the centroid of the gravel pit site to the stream = 1,136 feet, and the location <br /> of the parallel impermeable boundary was estimated to be 5,923 feet from the stream. Depletions from <br />
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