My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
2010-11-16_PERMIT FILE - C1996083A (28)
DRMS
>
Day Forward
>
Permit File
>
Coal
>
C1996083A
>
2010-11-16_PERMIT FILE - C1996083A (28)
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
8/24/2016 4:27:00 PM
Creation date
3/16/2011 8:24:19 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1996083A
IBM Index Class Name
Permit File
Doc Date
11/16/2010
Section_Exhibit Name
Volume IIIA Exhibit 15 Subsidence Prediction
Media Type
D
Archive
Yes
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
59
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
The occurrence of subsidence cracks on the surface may not necessarily result in <br />direct inflows into the mine when a surface drainage is disrupted. Studies by various <br />authors such as Orchar (1969, 1975) in Great Britain and Williamson (1978) in Australia <br />indicated that the subsidence cracks may be limited in depth by the development of <br />compressive stresses replacing the tensile stresses that cause surface fracturing. <br />Changes in land surface and drainage slope may affect the run-off water quality by <br />increasing the sediment load. The increase of drainage channel slope could result in an <br />elevated flow velocity and therefore, increase the erosion potential. <br />In summary, we believe that the occurrence of surface subsidence cracks comprises <br />the most important hazard to the surface drainage regime. There occurrence is predicted <br />principally within the areas where the overburden thickness does not exceed some 800 <br />feet. Such areas include: <br />o small ephemeral drainages near the outcrop <br />o mouth of Sheep Corral Gulch <br />o mouth of Dove Gulch <br />o mouth of Freeman Gulch <br />To eliminate or reduce the hazard of surface drainage disruptions would require a <br />change of the mining plans and design of protective pillars or zones of lower recovery <br />beneath these areas as discussed in Section 8.3. Alternatively, surface modifications of <br />the surface drainage and ponds could be made in cases of any occurrence of subsidence <br />cracks. Such surface modifications would not preclude a temporary disruption of the <br />existing surface run-off regime. <br />2.3 GROUND WATER <br />Total extraction (and, to a lesser extent, partial extraction) of coal seams causes <br />collapse, fracturing, bed separation and bedding plane slip in the roof strata above the <br />seam. All of these disturbances of the overlying strata can have a substantial impact on <br />• ground water if a major aquifer is within reach of the disruption. The height of the disturbed <br />- 21 - 10/00 <br />P~-o y <br /> <br />
The URL can be used to link to this page
Your browser does not support the video tag.