My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
2017-07-31_REVISION - M2006003
DRMS
>
Day Forward
>
Revision
>
Minerals
>
M2006003
>
2017-07-31_REVISION - M2006003
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
6/16/2021 2:23:18 PM
Creation date
8/9/2017 9:01:19 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M2006003
IBM Index Class Name
REVISION
Doc Date
7/31/2017
Doc Name
Application
From
Hall-Irwin Aggregates, LLC
To
DRMS
Type & Sequence
SO2
Email Name
ECS
WHE
Media Type
D
Archive
No
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
58
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
Mr.Jeff Gregg <br /> January 5,2006 <br /> Page 4 <br /> CIVIL RESIDURCES.LLC <br /> MATERIAL PROPERTIES <br /> Overburden <br /> The index properties for the insitu clay overburden were based on field testing data and on our engineering judgment; <br /> the following parameters have been used to model the overburden. <br /> Dry Unit Moist Unit Saturated Unit <br /> Weight(pcf) Weight(pci) Weight(pcf) Cohesion C'psi Friction Angle�'° <br /> 103 114 126 200 28 <br /> Alluvial Sand and Gravel <br /> The sand and gravel is generally medium grained sand,medium dense,poorly to well graded,and generally clean. The <br /> deposit ranges from fine to coarse sand with some silt and occasional rounded to well rounded gravels less than 2- <br /> inches in diameter. The alluvial sand and gravel has been modeled as follows: <br /> Dry Unit Moist Unit ` Saturated Unit Cohesion C'paf Friction Angie G'O <br /> Weight(pcf) Weight(pcf) Weight(pcf) <br /> 119 129 130 0 35 • <br /> Claystone Bedrock <br /> The proposed mine area is generally underlain by claystone bedrock. Claystone is generally a weak bedrock and is <br /> often prone to slope instability and the bedrock foundation strength is critical for the highwall stability. For the claystone <br /> bedrock,two potential strength conditions were considered. These strength conditions are referred to as:1)peak <br /> strength,and 2)residual strength. <br /> Peak strength is the maximum shear strength the claystone bedrock exhibits. The shear strength is made up of both <br /> cohesion(diagenetic bonding)and internal friction. Under short-term conditions for unsheared claystone,peak strength <br /> governs behavior. if a sheared surface or sheared zone is present within ciaystone as a result of faulting,slippage <br /> between beds due to folding,past shrink-swell behavior,stress relief,or from a landslide,the cohesion along the <br /> sheared surface is reduced to zero,and the angle of internal friction Is decreased,due to alignment of clay minerals <br /> parallel to the shear plane. Under these conditions a claystone exhibits its lowest strength known as residual strength. <br /> Residual strength bedrock occurs in discrete zones,parallel with the sheared surface or zone,whereas fully softened <br /> strength occurs over a broader area.Based on data from other recent jobs,and engineering judgment,we modeled the <br /> claystone as follows: <br /> Dry Unit Moist Unit Saturated Unit <br /> Weight(pct) Weight(pci) Weight(pct) Cohesion C'psi Friction Angle 0'° <br /> 116 124 134 Peak=100 Peak=28 <br /> Residual=0 Residual= 15 <br /> Soli-Bentonite Slurry <br /> The proposed slurry wall will consist of a mix of the overburden clay and imported bentonite.The resulting mix will <br /> produce a non-Newtonian fluid with some shear strength characteristics based on a reduced friction angle of the <br /> overlying clay overburden.Based on engineering judgment,we modeled the slurry wall as follows: <br /> WeightDry Unit Moist Unit <br /> (pci) Weight(pct) SWeigh Weight Unit <br /> Cohesion C'psi Friction Angle 01° <br /> NA 110 122 0 26 <br />
The URL can be used to link to this page
Your browser does not support the video tag.