My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
PERMFILE106678
DRMS
>
Back File Migration
>
Permit File
>
100000
>
PERMFILE106678
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
8/24/2016 9:59:19 PM
Creation date
11/24/2007 2:05:50 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1980007
IBM Index Class Name
Revision
Doc Date
6/13/2005
Doc Name
Exhibit 60D 2004 Geologic Hazard Field Observations for the South of Divide Mining Area
Type & Sequence
PR10
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.
/
53
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
2004 Geologic Hazard Field Observations <br />South of Divide Mining Area <br />CJ <br />7.0 SUBSIDENCE PREDICTION BASED ON PAST LONGWALL MINING <br />Coalmine subsidence, as defined in this report, is the local downwazd displacement <br />(downwarping) of the ground surface and underlying rocks above the mined coal under the <br />influence of gravity. This report includes only a brief summary, see Exhibits 60 and 60B, dated <br />November 2004 for greater detail. Subsidence above longwall mining panels can be divided into <br />four zones, which conceptually chazacterize the subsidence processes occurring from the mine <br />workings to the surface: 1) caved zone, 2) fractured zone, 3) continuous deformation zone, and 4) <br />neaz-surface zone. The continuous deformation and near-surface zones are usually combined, so <br />that the zones aze reduced to three (the continuous deformation and near-surface zones will also <br />be evaluated together in this report). <br />Subsidence causes the overburden material above longwall mining panels to: 1) cave into rubble <br />for the first 2 to 5 coal extraction thicknesses (2 to St) above the mine floor (caved zone); 2) <br />fracture for the next 10 to 20t (fracture zone); and 3) deform downwazd (down warp) as <br />• continuous, multiple layers (or plates) from the limit of the fracture zone to the ground surface <br />(continuous deformation and neaz-surface zone). <br />• <br />7.1 Vertical and Horizontal Displacement, Tilt, Curvature, and Horizontal Strain. <br />Differential vertical lowering of the ground surface causes vertical displacement (S), horizontal <br />displacement (S b), tilt (NI), curvature (C), and horizontal strain (E). Vertical displacement (also <br />called subsidence), tilt, and strain aze the main subsidence pazameters used in most subsidence <br />studies, and therefore, these will be the ones discussed in this report. <br />Vertical displacement, tilt, and horizontal strain predictions for the South of Divide mining area <br />are determined from the baseline data obtained from subsidence measurements above the 1NW, <br />2NW, and 3NW mining panels at West Elk Mine (Table 1). The basic subsidence parameters aze <br />then adjusted to geologic and topographic conditions in the areas where mining is planned. The <br />subsidence pazameters, projected for the South of Divide mining azea, are listed below. <br />831-032.621 Wright Water Engineers, Inc. Page 12 <br />November 2004 <br />
The URL can be used to link to this page
Your browser does not support the video tag.