My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
PERMFILE52001
DRMS
>
Back File Migration
>
Permit File
>
600000
>
PERMFILE52001
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
8/24/2016 10:55:56 PM
Creation date
11/20/2007 3:09:25 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1980007
IBM Index Class Name
Permit File
Doc Date
6/2/2006
Section_Exhibit Name
Exhibit 60B Subsidence Evaluation for the South of Divide Mining Area
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
Subsidence Evaluation For <br />Exhibr7 608 South ofOivide Mining Area Page 13 <br />pillars, and unyielding chain pillars. Any surface or neaz-surface water that might be present in <br />this zone has a higher probability of being impacted than that occurring in any other areas above <br />the mining panels. <br />5 6 Angle of Major Influence <br />The angle of major influence, (l, (also called angle of influence of the point of evaluation) is <br />defined by Peng (1992, p. 11) "... as the angle between the horizontal and the line connecting <br />the inflection point and the edge of the radius of major influence." The radius of major influence <br />(r) is therefore the horizontal distance from the vertical projection of the inflection point [o the <br />point of maximum subsidence and the limit of subsidence (Figure 3). The angle of major <br />influence is used for computer modeling by the influence function method. In the B Seam <br />mining at West Elk Mine, the angle of major influence ranges (from a horizontal reference) from <br />about 70 to 80 degrees. <br />The angle of major influence may also be referenced to the vertical, as has been done for the <br />break angle and angle of draw. The angle of major influence (from a vertical reference) is <br />roughly equal to the angle of draw (Figure 3), and is therefore also predicted to range from 10 to <br />20 degrees. <br />5.7 Relation Between Dynamic and Final Subsidence Defornrations <br />Maximum dynamic tilt (change of slope) and horizontal tensile and compressive strain are <br />reportedly less above longwall mining panels than are the final tilt and strain values at panel <br />boundaries. Dynamic tilt and strain decrease, relative to final tilt and strain, as the rate of face <br />advance increases. <br /> <br />Dynamic tilt and strain reportedly decrease with increasing speed of longw=all coal eattraction <br />(Deng 1992, p. 20-21). Based on observations in a West Virginia coal mine: <br />1. Maximum dynamic tilt decreased by an average of 42 percent (from 0.0024 to 0.0014) as <br />the mining face rate of movement increased from 10 to 40 feet per day; dynamic tilt <br />therefore decreased by 14 percent as the face rate of movement increased by 30 feet per <br />day. <br />2. Maximum dynamic tensile strain decreased by an average of 22.5 percent (from 0.0031 to <br />0.0024) as the mining face velocity increased from 10 to 40 feet per day; dynamic <br />horizontal tensile strain decreased by 7.5 percent as the face increased by 30 feet per day. <br />3. Maximum dynamic compressive strain decreased by an average of 48 percent (0.0062 to <br />0.0032) as the face velocity increased from 10 to 40 feet per day; dynamic horizontal <br />compressive strain decreased by 16 percent as the face increased by 30 feet per day. <br />831-032.690 Wright Water Engineers, Inc. <br />
The URL can be used to link to this page
Your browser does not support the video tag.