My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
2005-04-12_GENERAL DOCUMENTS - M1999002
DRMS
>
Day Forward
>
General Documents
>
Minerals
>
M1999002
>
2005-04-12_GENERAL DOCUMENTS - M1999002
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
8/24/2016 3:16:11 PM
Creation date
4/14/2008 10:07:21 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M1999002
IBM Index Class Name
GENERAL DOCUMENTS
Doc Date
4/12/2005
Doc Name
Major modification
From
US Environmental Protection Agenty
To
American Soda L.L.P.
Email Name
CBM
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.
/
77
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
of we1120-12 as a test installation for TDR. Consistent with the failure of the past installations and the <br />ongoing test of TDR post-mining applicability, American Soda proposes to eliminate the requirement for <br />installation of TDR in each well at the time of construction. <br />It is not certain that the TDR system would be functional even in the more limited post-mining <br />application. Therefore, and to prevent a continual revision of permit conditions, American Soda will <br />develop a plan for future TDR installations only if the test proves that post-mining TDR monitoring is <br />viable. The original Subsidence Monitoring Plan (Appendix J, dated December 23, 1999) has been <br />revised to reflect this approach. EPA proposes to replace the original document with the revised August <br />2004 Subsidence Monitoring Plan as Appendix J. <br />b) Borehole Geophysics -Gamma Logs: Gamma logging is a common technique used to identify <br />geologic formations and the depth at which they occur. Gamma logs essentially read the radioactive <br />signature of the surrounding formation and record the depth at which it occurs. Because each formation <br />has a characteristic signature, gamma logging could potentially be used to determine if subsidence occurs <br />by comparing a baseline gamma log (e.g, conducted at the time of well construction) against later gamma <br />logs (during operations) to evaluate whether baseline formation depths have changed. <br />A gamma log is currently required as part of the geophysical logging completed at the time of <br />well drilling. The existing subsidence monitoring plan also requires a gamma log to be run at each well <br />in service after achieving individual well production levels of 85,000 tons, 150,000 tons, and.after <br />retirement for the purpose of determining if subsurface subsidence has occurred. The subsidence <br />monitoring plan also requires a gamma log to be run if TDR monitoring indicates that subsidence of 6 <br />inches or more has occurred at the Mahogany Zone. <br />Gamma logs run to date in wells have provided limited value. The well bores are subject to <br />mineral and metals buildup (scaling) during the solution mining process. This scaling affects the ability <br />to run and interpret gamma logs, effectively masking the radioactive gamma signature of the formations. <br />The degree of interference from scaling is somewhat variable, but because the gamma log method does <br />not produce consistent data, it is not considered reliable as a means to identify or evaluate subsurface <br />subsidence. <br />Consideration has been given to continuing the gamma logging gamma logging and install <br />radioactive markers in the well bore (7-inch casing) pipe thread at certain locations in the well (e.g., near <br />the A-groove, B-groove, and crown pillar). This option could only apply to new well construction and <br />would not resolve the issue with existing wells. This approach would improve the ability to consistently <br />identify the radioactive markers themselves but would not provide complete formation logging for <br />subsidence monitoring. If movement is indicated by this method, it could provide a relative indication of <br />where the movement occurred but would not provide precise depth or travel information for the event. <br />Further, if casing breaks occur as the result of thermal expansion and contraction, a shift in marker <br />location would not necessarily be related to formation subsidence. This method does not provide a direct <br />measurement of or link to whether subsidence has occurred. Radioactive markers have also been known <br />to dislodge from a well bore and this does create some concerns regarding waste management and <br />liability. Additionally, there is a perception issue associated with the potential for one of the markers to <br />come in contact with food-grade product. At this time, American Soda is not proposing to utilize this <br />technique in new well construction. <br />FINAL Addendum to SOB For Modification No. 9, UIC Area Permit No. C030858-00000 Page 3 of 29 <br />
The URL can be used to link to this page
Your browser does not support the video tag.