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2023-02-08_REVISION - M2003016 (2)
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2023-02-08_REVISION - M2003016 (2)
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Entry Properties
Last modified
2/9/2023 10:48:46 PM
Creation date
2/9/2023 8:36:06 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M2003016
IBM Index Class Name
Revision
Doc Date
2/8/2023
Doc Name
Request For Succession Of Operator
From
City and County of Broomfield
To
DRMS
Type & Sequence
SO4
Email Name
ECS
MAC
SMS
AWA
Media Type
D
Archive
No
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Mr. Brennan Middleton <br /> September 30,2022 <br /> Page 3 <br /> The stability of structures within 200 feet of the proposed mining limits was evaluated at the two(2)most critical <br /> representative sections under anticipated loading conditions as discussed below. The GALENA computer program was <br /> used for the analysis. The method for selecting the critical failure surface for each analyzed loading condition was the <br /> following. The Simplified Bishop's Method of Analysis was used to find the critical failure surface by randomly searching <br /> 27,001 trial failure circles over a broad range of the slope surface and at the structure in question to evaluate the lowest <br /> FOS. Both static stability under anticipated mining conditions and seismic stability under peak ground acceleration loads <br /> were performed. Seismic loading was obtained from the U.S.G.S. Unified Hazard Tool attached to this report. Review of <br /> the Hazard Tool indicated a maximum horizontal acceleration of 0.0896g with a return period of 2,475 years for the site. <br /> The two(2)most critical cross section locations were selected and analyzed as described below. <br /> ► South Section: This section is on the south side of the previously mined mine cell where the underdrain is—30 <br /> feet from the mine highwall. This section considers a 22-foot tall highwall at a point where the mine limit is <br /> approximately 20 feet from the slung wall.The high wall slope 3h:1v. The overburden is modelled at 6-feet <br /> thick overlying 16-feet of sand and gravel. The top foot of the claystone was modelled at residual strength <br /> reflecting the weathered nature at the top of the claystone. Unweathered claystone was modelled below the top <br /> foot. Groundwater was modelled at a depth of 4-feet exterior to the slurry wall. Loading due to traffic along <br /> County Road 20 was simulated with a 500 pound per square foot(psf)surcharge at the road. <br /> ► Southeast Section:This section is on the southeast side of the previously mined mine cell where a concrete <br /> ditch is approximately—39 feet from the mine highwall. This section considers a 28-foot tall highwall mined at a <br /> slope of 3h:1 v. The original mine cell was mined to within approximately 12-feet of the slurry wall and <br /> approximately 1-foot of fill was placed over the top of the slurry wall. A boring at the site indicates the depth to <br /> bedrock in this area is approximately 44-feet. However,site surveys and observations indicate the cell was not <br /> mined to bedrock in this area. The overburden (including the 1-foot of fill)is modelled at 6-feet thick overlying <br /> 38-feet of sand and gravel. The top foot of the claystone was modelled at residual strength reflecting the <br /> weathered nature at the top of the claystone. Unweathered claystone was modelled below the top foot. <br /> Groundwater was modelled at a depth of 4-feet exterior to the slurry wall. Loading due to traffic along County <br /> Road 20 was simulated with a 500 psf surcharge at the road. <br /> MATERIAL PROPERTIES <br /> The material index and engineering strengths assumed in this slope stability report are discussed below. <br /> Overburden <br /> The strength properties for the in-situ overburden were based on our experience at similar sites and engineering <br /> judgment;the following parameters have been used to model the overburden. <br /> Unit Weight Cohesion C'psf Friction Angle 0'° <br /> c <br /> 105 50 26 <br /> Alluvial Sand and Gravel <br /> The sand and gravel is generally a fine to medium-grained sand overlying a fine to coarse grained sand that is typically <br /> medium dense and locally gravelly. The alluvial sand and gravel unit was modeled as follows: <br /> Unit Weight Cohesion C'psf Friction Angle 0'° <br /> c <br /> 120 0 1 35 <br />
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