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2008-01-16_APPLICATION CORRESPONDENCE - C2008086 (3)
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2008-01-16_APPLICATION CORRESPONDENCE - C2008086 (3)
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Last modified
8/24/2016 3:21:02 PM
Creation date
2/7/2008 3:18:14 PM
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Template:
DRMS Permit Index
Permit No
C2008086
IBM Index Class Name
Application Correspondence
Doc Date
1/16/2008
Doc Name
Preliminary Draft Environmental Impact Statement/Subsidence
Media Type
D
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DRAFT <br />Measurements <br />9.0 SURFACE SUBSIDENCE MONITORING <br />Various governmental bodies may require a monitoring demonstration that the predicted <br />subsidence effects are indeed conservative and not significantly exceeded. Specifically, a <br />monitoring program over one of the initial longwall panels that will obtain subsidence data on <br />the maximum vertical subsidence (Smax), tensile (+E) and compressive (-E) horizontal strains, <br />angle of draw (a) and subsidence induced tilt (G) for this unique geologic environment. If <br />room-and-pillar panels are mined it may be necessary to measure the same subsidence effects, <br />or to demonstrate that sufficient pillars are left to prevent subsidence. <br />The Surface Subsidence Monitoring Guidelines by Abel (1982) indicate one possible monitoring <br />program that has been utilized to provide the data, when required. Figure 21. Subsidence <br />Monitoring Program indicates the location of surface monuments for flat lying terrain. The <br />rugged terrain and rapidly changing overburden depth in the Project Area will necessitate <br />panel-by-panel monument spacing modifications in the field after the locations of the initial <br />panels become available. Either monument spacing for the test panel will have to be <br />continuously changed to match overburden changes or all monuments will have to be spaced to <br />match the shallowest overburden for that panel. Considerable advances have been made since <br />the early subsidence transit and leveling monitoring programs by the NCB. The precise leveling <br />used by Collins (1977), has been replaced by Electronic Distance Measurement (EDM) and <br />more recently the Global Positioning System (GPS) has apparently increased its accuracy to the <br />point that it has been used to measure subsidence induced changes at the ground surface. <br />There is no substitute for properly constructed monuments either anchored to bedrock or at <br />sufficient depth to prevent temperature and moisture changes from impacting the . <br />measurements. <br />10.0 REFERENCES <br />Abel, Jr., J.F., 1982, Surface Subsidence Monitoring Guidelines, Phase 1 Report: U.S. Geol. <br />Survey Contract No. 14-08-001-18822, 11 p. <br />Abel, Jr., J.F. & F.T. Lee, 1984, Lithologic Controls on Subsidence: Trans. SME/AIME, v 274, p <br />2028-2034. <br />Abel, Jr., J.F., 1988, Soft rock pillar design: Intl. Jour Mining & Geological Engrg, v 6, p <br />215-248 <br />Bauer, R.A., B.B. Mehnert, D.J. van Roosendaal, P.J. DeMaris, N. Kawamura & C.J. Booth, <br />1995, Land subsidence and hydrologic changes due to longwall coal mining in Illinois: in <br />Land Subsidence Case Studies and Current Research, AEG Sp Pub 8, p 218-228. <br />Booth, C.J. and E.D. Spande, 1992, Potentiometric and aquifer property changes above <br />subsiding longwall min panels: Ground Water, v. 30, no. 3, May-June, p. 362-368. <br />Brauner, G., 1973:, Ground movements and mining damage, Pt. 2 of Subsidence due to <br />underground mining: U.S. Bureau of Mines Information Circular 8572, 53 p. <br />Page 44 of 57 <br />
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