My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
2024-02-01_REVISION - M1973021 (2)
DRMS
>
Day Forward
>
Revision
>
Minerals
>
M1973021
>
2024-02-01_REVISION - M1973021 (2)
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
2/1/2024 12:43:10 PM
Creation date
2/1/2024 11:22:34 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M1973021
IBM Index Class Name
Revision
Doc Date
2/1/2024
Doc Name Note
Adequacy Response 1
Doc Name
Adequacy Review Response
From
Holcim/HDR
To
DRMS
Type & Sequence
TR9
Archive
No
Jump to thumbnail
< previous set
next set >
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
1813
PDF
Print
Pages to print
Enter page numbers and/or page ranges separated by commas. For example, 1,3,5-12.
After downloading, print the document using a PDF reader (e.g. Adobe Reader).
View images
View plain text
Geotechnical Stability Exhibit <br /> Engineering Evaluation of Highwall Design for the South Quarry of the Morrison Quarry <br /> <br /> January 2024 | 19 <br />observations of the quarry by HDR geologists, subsurface exploration parameters such as <br />recovery, RQD, and drill rate, and a comprehensive laboratory testing program. <br />The Hoek-Brown model is a non-linear shear strength model for rock that is well known in the <br />geotechnical engineering industry for quantifying the factor of safety of simplistic stress-strain <br />models of rock cuts. The generalized Hoek-Brown model relies on the Geologic Strength Index <br />(GSI), intact UCS (σci), disturbance factor (D), and the material constants mb, a, and s, where mb <br />is reliant on the material constant for intact rock mi modified for GSI. The major and minor <br />principal stresses (σ1 and σ3) are formulated within the Hoek-Brown (Hoek, et. al. 2002) model <br />via Equation 1, below. <br /> <br />σ = σ + σ (m <br />σ <br />σ + ) <br />Eq. ( 1) <br />Where the rock mass material constants mb, s, and a are given by Equations 2, 3 and 4, below. <br />m = m exp <br />− 100 <br />28 − 14 <br /> <br />Eq. ( 2) <br />= <br />1 <br />2 + <br />1 <br />6 ( <br /> ! <br />"− <br />#$ <br />) <br />Eq. ( 3) <br />= exp <br />− 100 <br />9 − 3 <br /> <br />Eq. ( 4) <br />And the disturbance factor D, constant mi for intact rock by rock group, and Geologic Strength <br />Index are found by interpretation of Figure 4, Figure 5, and Figure 6, below.
The URL can be used to link to this page
Your browser does not support the video tag.