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REV13688
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REV13688
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Entry Properties
Last modified
8/25/2016 1:24:48 AM
Creation date
11/21/2007 10:44:39 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981015
IBM Index Class Name
Revision
Doc Date
3/29/1994
Doc Name
Memo on Stability of Portal Bench and Highwall
From
DMG
To
STEVE RENNER
Type & Sequence
SF1
Media Type
D
Archive
No
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Memo to Steve Renner <br />Fruits Highwall Stability <br />page 5 <br />Mr. Lewicki used Yang Huang's REAME computer program, which uses <br />Bishop's method of slices for cylindrical .failure. <br />Direct Shear Parameters: <br />Fill Material: Angle of <br />(Measured) Cohesion <br />Density <br />Fill Material: Angle of <br />(Adjusted) Cohesion <br />Density <br />Internal Friction (B) = 36.8° <br />(C) = 0 psf <br />116 pcf <br />Internal Friction (B) = 41.0° <br />(C) = 0 psf <br />116 pcf <br />Results of Analysis: <br />Portal Bench Fill <br />Facial Slope Angle = 2h:ly (26.6°) <br />Static Factor of Safety = 1.77 <br />Sensitivity Analysis <br />At 8 = 37' and C =.0 psf, FS = 1.54 <br />At B = 34' and C = 50 psf, FS = 1.48 <br />1992 Analysis (Highwall) <br />During the fall of 1992 the Office of Surface Mining, Reclamation <br />& Enforcement-(OSMRS) expressed a concern regarding the stability <br />of the highwall at the Fruits mine. In response to the OSMREs <br />concern, American Shield Coal Company was directed by the Division <br />to analyze the stability highwall. Mr. Lewicki completed an <br />analysis of the highwall which relied upon empirical evidence of <br />the highwalls performance as evidenced in photography dating back <br />to 1978. Mr. Lewicki demonstrated to the Division's satisfaction <br />that the highwall had remained stable and intact from 1978 through <br />1992. The evidence demonstrated that only minor debris fall had <br />occurred, as evidenced by limited blocks of rock on the reclaimed <br />surface. Limited debris calving is characteristic of the <br />surrounding natural terrain. <br />The stability of rock faces is difficult to analyze. The intrinsic <br />strength of the actual bedrock matrix, as tested in the shear <br />apparatus, will normally withstand vertical slope angles. The <br />stability of most highwalls, however, is controlled by the rock <br />mass macro discontinuities, including faults, joints. and <br />sedimentary bedding. Few models reflect these inhomogeneities with <br />sufficient detail to accurately model the highwall mechanically. <br />
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