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2018-10-19_REVISION - M1980244
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2018-10-19_REVISION - M1980244
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Last modified
1/4/2025 6:18:05 AM
Creation date
10/19/2018 4:32:23 PM
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Template:
DRMS Permit Index
Permit No
M1980244
IBM Index Class Name
Revision
Doc Date
10/19/2018
Doc Name
Adequacy Review Response
From
CC&V
To
DRMS
Type & Sequence
TR101
Email Name
TC1
Media Type
D
Archive
No
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might Piesold <br /> CONSULTING <br /> Environmental Department, Meg Burt, Senior Manager October 8, 2018 <br /> Cripple Creek and Victor Gold Mining Co. (Newmont) <br /> Runoff Curve Numbers <br /> Various NRCS (2004) runoff CNs were estimated and applied to represent the runoff potentials from the <br /> varying cover types (i.e., land and material types) present in the contributing areas. The CN values were <br /> estimated based on the following assumptions and information: <br /> • Antecedent Runoff Condition (ARC) II (i.e., average conditions). <br /> • Cover types and hydrologic conditions based on site tour observations and ground and aerial photos. <br /> • Hydrologic Soil Groups (HSG) based on information procured from the NRCS online Web Soil Survey <br /> and supplemented with site tour observations, ground and aerial photos, and soil gradations estimated <br /> by AMEC (2011). Information downloaded from the NRCS Web Soil Survey is presented in <br /> Attachment 3. <br /> CN estimates were made for the following cover types based on varying hydrologic conditions and HSGs, <br /> where applicable: <br /> • Natural ground- Herbaceous grass and oak-aspen woods <br /> • General disturbed areas(e.g., cut slopes, compacted stockpiles, etc.) and roads <br /> • Waste rock <br /> The estimated individual CN values are presented in Table 2.1, per NRCS (2004). As shown on <br /> Figure 2.4, the existing basin area to each structure was further delineated into sub-components <br /> corresponding to the applicable CN classifications presented in Table 2.1. Using the area-weighting <br /> technique, a single composite CN value was calculated per basin area. The results of this analysis for the <br /> existing EMPs are presented in Table 2.2. CC&V reviewed and approved the curve numbers presented <br /> herein. The composite CNs were applied to the hydrologic modeling to estimate the peak flows for the <br /> diversion channels and spillways and used to estimate the runoff volumes for the impoundments. In <br /> addition, direct precipitation (i.e., no losses) within the EMP impoundment footprints was accounted for in <br /> the modeling. <br /> 2.4 Hydraulic Analyses Methodologies, Inputs and Assumptions <br /> 2.4.1 General <br /> Hydraulic analyses were performed on the as-built infrastructure information provided by CC&V to <br /> estimate the existing capacities and erosion protection adequacies of the diversion channels, spillways, <br /> and EMP impoundments. The results of these analyses were compared to the results of the hydrologic <br /> analyses to evaluate adherence to the design criteria. <br /> 2.4.2 Hydraulic Analyses Methodologies <br /> The hydraulic capacity evaluations of the as-built diversion channels and spillway outlet channels were <br /> completed using Manning's equation for normal flow conditions (Chow, 1959). The as-built riprap erosion <br /> protection for longitudinal slopes less than 20 percent was evaluated using the shear stress method <br /> presented in the United States Federal Highway Administration's (FHWA, 2005) Hydraulic Engineering <br /> Circular (HEC) Number 15 based on the estimated 100-year/24-hour peak flows. The methodology <br /> proposed by Robinson et al. (1998) was used to evaluate the riprap for longitudinal slopes greater than <br /> 20 percent. <br /> The as-built spillway inlet weir capacities were evaluated using the standard trapezoidal weir equation. <br /> A discharge versus depth (head) rating curve was developed and applied to the HEC-HMS hydrologic <br /> model to evaluate the peak inflows to the impoundments, the flow routing effects within the <br /> impoundments (i.e., attenuation and lag), and the as-built spillway discharge capacities. It was assumed <br /> that each pond would be full to the spillway inlet invert elevation at the onset of the 100-year/24-hour <br /> storm event. <br /> 4 <br />
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