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2012-08-14_REVISION - M2002020 (5)
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2012-08-14_REVISION - M2002020 (5)
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Last modified
6/15/2021 2:25:43 PM
Creation date
8/20/2012 3:22:56 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M2002020
IBM Index Class Name
REVISION
Doc Date
8/14/2012
Doc Name
RESPONSE TO ADEQUACY REVIEW
From
BLUE EARTH
To
DRMS
Type & Sequence
AM1
Email Name
PSH
Media Type
D
Archive
No
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1,1104 Applegaite <br />Group, Inc. <br />Consultants for Land, Minerals and Water <br />Memorandum <br />Date: 02 -14-02 File No. 01 -101 <br />To: City of Greeley <br />From: Craig Ullman <br />Subject: Slope Stability for 2? Avenue Site <br />As requested by the City of Greeley we have performed a slope stability analysis for the 25 Ave. gravel pits. The <br />purpose of this analysis was to determine a stable slope configuration for additional mining proposed at the site and to <br />determine a proper location for the proposed slurry wall. Two cross sections were selected for the analysis. The first <br />cross section was located along the western boundary of the West Pond and the second section was along the north <br />edge of the east pond. <br />The first cross section poses several problems. The 35 Ave stormwater ditch is in close proximity to the existing <br />pond. The top width of the berm separating the stormwater ditch from the pond is currently 15 ft. A buried gas line is <br />located within this berm. A 40ft wide working platform is proposed for the construction of the slurry wall. Assuming a <br />side slope of 3:1 the platform slope will tie into the existing surface somewhere near the existing toe of slope. Soils in <br />this area consist primarily of approximately 5.5 11 of silts lying atop 50 ft of coarse alluvium. <br />The second cross section was along the border of the Cache La Poudre River. Existing pit slopes appear to vary from <br />211:1 V to 411:1 V. The stability analysis assumed all pit slopes would be brought to 311:1 V. Topographic data was not <br />available for the water surface or exact location of the river with respect to the ponds. Therefore, the water surface <br />elevation in the river was assumed to be 5 feet below the working platform for the slurry wall and the edge of water <br />was assumed to be 10 ft from the outer edge of the working platform. Borelogs in this vicinity indicate that there is a <br />thin layer (2.5 ft) of coarse alluvium lying atop of approximately 5 feet of fine alluvium or silt. The remaining depth to <br />bedrock consists of coarse alluvium. <br />From this point additional mining could be performed in one of two ways. If mining progresses in such a manner as to <br />expose a high wall of alluvium then the limits of mining will need to be offset a'sufficient•distance from the existing <br />toe of slope. The stability analysis was used to determine an acceptable distance for this setback. After completion of <br />mining the side slopes would need to be reclaimed at a specified slope. The construction condition for this scenario <br />was analyzed due to the presence of the high wall. Mining could also be performed by beginning at the existing toe and <br />mining down to bedrock at a specified slope. Both scenarios were analyzed for stability during a rapid drawdown <br />condition. This scenario assumes that the pore water pressure in the embankment remains unchanged as the reservoir is <br />drained. The minimum allowable factor of safety for all scenarios is 1.20. <br />Several assumptions were made in the stability analysis. It was assumed that the depth of remaining alluvium was 30 <br />feet. Weathered bedrock was assumed to extend 5.5 ft below the bedrock surface. All pit slopes were assumed to be <br />constructed at a slope of 311: IV. Groundwater levels were set at 10 ft below existing ground surface. Soil parameters <br />were unavailable for the site and therefore, were determined based on conservative values for similar materials. Of <br />special note, the materials used to reclaim the slopes of the original pit were placed without controlled compaction and <br />therefore the state of these materials is questionable. Very conservative assumptions were made concerning the soil <br />1499 West 120 Avenue, Suite 200 • Denver, Colorado 80234 -2728 • (303) 452 -6611 • Fax: (303) 452 -2759 <br />5441 Boeing Drive, Suite 200 • Loveland, Colorado 80538 -8855 • (970) 461 -9884 • Fax: (970) 613 -1177 <br />
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