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PERMFILE139786
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Last modified
8/24/2016 10:42:53 PM
Creation date
11/26/2007 8:57:54 AM
Metadata
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Template:
DRMS Permit Index
Permit No
C1982056
IBM Index Class Name
Permit File
Doc Date
12/11/2001
Section_Exhibit Name
Exhibit 07f-1 Rockfall Hazards Study Norther Mining District
Media Type
D
Archive
No
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<br />1• <br /> <br /> <br />CJ <br /> <br /> <br /> <br />N <br /> <br />SubTerra, Inc. Twentymile Coal Company 5/23/99 <br />Northern Mining District Rockfall Hazards Evaluation <br />Scanline <br />(length in ft) <br /> <br />3 (440) Joint <br />Set <br /> <br />S1 Number of <br />Joints <br /> <br />14 Apparent <br />Spacing (ft) <br /> <br />31.4 Alpha <br />(degrees) <br /> <br />75 Terzaghi <br />Corrected <br />Spacing (ft) <br />8.1 <br /> S3 59 7.5 20 7.0 <br /> S4 52 8.5 15 8.2 <br />4 (420) S1 18 23.3 75 6.0 <br /> S3 49 8.6 20 8.1 <br /> S4 39 10.8 15 10.4 <br />Using true spacing, all three-set block-forming combinations of joint sets S1, S2, S3 and S4 <br />were analyzed to obtain the frequency distribution of block sizes. Experience has shown that <br />many discontinuity sets have a spacing distribution that approximates reasonably to a negative <br />exponential form (Priest and Hudson, 1976, Priest and Hudson, 1981), and this was assumed to <br />apply in this study. The negative exponential distribution is asingle-parameter distribution that is <br />completely defined by its mean, so provided the mean spacing is known, the full range of <br />probabilities can be estimated. Analysis of the bedding plane data indicated a lognormal <br />spacing distribution. Using these distributions, the potential discontinuity combinations and <br />resulting block sizes were analyzed using probabilistic modeling software. <br />Based on the analysis, a worst case block size of about 6000 cubic feet was considered <br />appropriate for Phase I rockfall hazard assessment. An 'equivalent' disk, with a diameter of 26 <br />ft, a thickness of 11 ft, and a volume of 5840 cu. ft. was used in the CRSP3 runs <br />Prior to the main hazard assessment, a number of trial runs were carried out to calibrate the <br />' CRSP3 model, and select appropriate site-specific slope surface parameters. These calibration <br />runs were carried out on sections of the slope where previous rockfalls provided a basis for <br />comparing observed and predicted behavior. <br />' Typical block sizes were determined from the boulder catalog for each calibration section. <br />These block sizes were converted to equivalent disks or cylinders for input to the CRSP3 model, <br />by setting the diameter equal to the average of the two most similar dimensions, and the <br />' thickness or lengths equal to the remaining dimension. <br />2.4 CRSP3 Parameters <br />CRSP3 requires that the surface of the modeled profile be described in terms of tangential and <br />normal (restitution) coefficients. Tables 2-2 and 2-3 show the relationship between the surface <br />' descriptions presented by Pfeiffer and Bowen (1989) for assigning tangential and normal <br />(restitution) coefficients, and inferred equivalent site conditions. Table 2~ indicates the ranges <br />for these parameters considered appropriate at the site. <br />1 <br />,• <br />' 4 PN: 9915 <br />
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