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PERMFILE112504
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PERMFILE112504
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Entry Properties
Last modified
8/24/2016 10:08:51 PM
Creation date
11/24/2007 9:34:24 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981012
IBM Index Class Name
Permit File
Doc Date
12/11/2001
Section_Exhibit Name
EXHIBIT 24 SUBSIDENCE CONTROL PLAN
Media Type
D
Archive
No
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<br />l <br />3ff <br /> 0 <br /> 10 <br />9 10 <br />i <br /> <br />a ~ <br />~ .lo <br /> SO <br />E eo <br />K <br /> ,p <br /> <br /> <br />O <br /> ~ <br />i f00 <br />SURFACE SUBSIDENCE <br />/Flnfl face pofltlon <br />i <br /> ~ ~ Rsfltl al <br /> funfltlenef <br /> <br /> Subfltlencf pr0}Ils <br /> ~, when ffcf ft <br /> , <br /> <br /> <br />, Infl fubfltl <br />proflla ZI dayf <br />alter fief flop <br /> <br /> <br />Z.0 tS 1.0 05 0 0.6 1.0 1.f TA <br />~~, ~ Race atlvfef <br />t7ep t h <br />,: ~ Hlf. f17 Naldud rubrldetKa Ixoak (IZ). Coutury U.K. Nuional Cwl Bond. <br />~' <br />~' wrfea point and reduces to 2 to 3% if the face has passed the critical <br />width. The rate of face advance determines the time needed to pass <br />;~, through the critical width. As long as the face is still within the critical <br />width, further wbsidence is expected. <br />However, Brauner (13), citing Russian data, stated that in addition to <br />the tare of advance and size of critical area, the duration of surface <br />subsidence depends on strata conditions, depth o[ extraction, kinds of <br />packings, and previous extraction and that it ranges from several days Io <br />' several ycafx. The duration is longer fur (hick-bedded or stronger uvcr- <br />• burden, for greater depths, and for complete caving. For a small extrao• <br />•. lion area of a relatively mobile overburden mined in a very short time, the <br />rate of subsidence ie proportional to the difference between the final <br />subsidence S and the instantaneous subsidence S,: <br />~t ~ c(S - S,) <br />I, , <br />4 <br />I <br />the solution of which is <br />(9.2.1) <br />S,/S ~ C ~ 1 - e-~ (9.2.2) <br />whero C is a time factor and c is a constant characteristic of the strata. A <br />typical C curve for soft strata is illustrated in Fig. 9.2.g. <br />In the United States, earlier studies (10, ll) showed that subsidence <br /> <br />r 1 <br />LJ <br />L <br />
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