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TDFl caUla Inswr ~~ <br /> <br />-`-- <br />' - <br />Pioloctlv/ J <br />t~ <br />Coven Sp~ohm <br /> connadoi cnUlo <br /> E.Panslvo <br /> courant i <br /> prom <br /> (a) <br /> ou•m <br /> n n <br />• <br />sunslr <br />_ <br /> ,o - > <br /> ~N <br />ti <br /> <br /> _ ~~ <br /> w - <br /> im <br />,M °-I <br /> <br /> <br />• .w <br />"" wo - <br />-_ <br />fb) MEtEnS rEEr <br />CinnP <br />n caLlo <br />FIG. 1. (a) Inslallatlon for Monitoring of Rock Deformation; and (b) Associated <br />TDR Dala for Deformation above Longwall Minc <br />was w•rillen to allow gr;lpltical analysis of large, raw data files produced by <br />high-resuhdiun digiLd veccions o('I'D It sign:dures for cables hundreds of <br />ntclcrs long. II will L•ICilil:nc Display, cumpa rival, analysis, :uul xnnnully <br />of 'fh12 w•avcfunm ronsiNing of as m:ulp as 2.5111 Bala puiuls. Arqui~inun <br />and Iranslnissiun of thrsc Iargr files via nunlew reyuin'd Ute Iclrcunuuu- <br />niattiun amlrul protuatl, NUMOb. <br />'hhe pascal study was made nl a lungwall coal tutor :n the mining Faa• <br />advanced luw:ml the prcinstallcd ctble.'I'I)IL signaltncs wcrc acquired Iwicc <br />daily and compared wish defonualion nteauacd un the surface. Subsurface <br />dcfurnlalion mc;lsund h)• ~1 ~1)IL was shmvn In he Ioc:diicd ;end pn•dumi~ <br />nalcly shearing in nahu~c. Localized changes wcrc detected at depth sonic <br />four days bcforc the rlcfurmalion was observed al the surface. <br />'this :u~l icle begins wish a dcscliptinn u( the site :end is followed by an <br />interprcudion of the results of dlc twice-daily remote polling, DGails u(Ihc <br />inst nnncnlaliun and installation procedure arc contained iu the Appendix <br />of thts p:q,cr. <br />SITE <br />Geometry of ~9iuin); <br />Old IScu Coal Company's Minc No. 2.5 is totaled in I~t anklin County near <br />Well Fraukfurl, fll. As shown iu Pig. 2, the borehole for the "Tll1L cable <br />was fuelled near a residential slnlclure west of I Icnm Koad. Location of <br />the lungwall miuc face in the curd se:un some 15') m (522 (t) below ix indiealerl <br />by the Thick, nullh-south lines identified by d;de. A schematic west-(u-call <br />cross section in Pig. 3 shows the lonsa•all face advancing westward toward <br />the verlic;tl TllR hole. "phis face advanced Toward the TDR cable a[ the <br />consuutl rdc of 111 nt/d as shown in Pig. 4 by the mnslanl slope of the plot <br />ul dlseutce between face :end cable as :I function of lime since inslallalion. <br />Inlcrsecliun of This distance versus (into rehlliunship with the zero-rlislane'e <br />line (when the mine face undercuts the cable) shows That the cable had been <br />inslalleJ fur some •1811 h ur 2(I days. Simil:u ly, irate rscctiun with the zero <br />lime line (whcu the ethic was installal) shows that Thu advancng none Clcc <br />was some 15(1 m (5(111 II) ;nv;ly from the cable. <br />Gculul:Y <br />A 7G.2-nuu (3 in.) di:uncler hole w;ts wire line cored to characterize the <br />overlying strata. Illinois Stale Geological Survey personnel (Mclutcrt cl :II. <br />1992) visu:dly lugged the core and the hole was grnphysically logged ("Geo- <br />physir:d" 1991). '1~6ese geophysical lugs Then allowed estimates of ruck <br />density, purttsity, shear modulus, Poisson's ratio, bulk modulus, and Young's <br />modulus to be computed. Inslntmcnlaliun details arc conlaincd in Appen- <br />dix I. <br />Major changes iu rock Iypc arc found in this cyclulhcnn geology, which <br />is typical in the Suulh Illinois coal basin. Por insl;mcc, as can be seen in <br />Pig. 1, curd scants al depths of :48, 107, :end I IS m arc overlain with 8, 16, <br />:uul 8 m of shales, respectively. Pnrlhernutrc. Ihcsc ch;mgcs in IilhologY <br />dcscrihcrl in Pig. 3 col relate with lucnlizcrl dcLmn:dion shown iu Pig. 5. <br />Specific nwvcntenl was dclcclcd near the 0.2 m of Iimcslone al 3(I m, U.7 <br />m of inlcrlaminalcd sillslonc ;utd s;utdstonc ^l d0 m, ;end 0.1 m o(limcslouc <br />al GG nt. <br />INTERPRETATION OF AESULTS FROM REMOTE POLLING <br />Inlcrprclaliun of ~1'avcfonus <br />Pig. 5 presents s:unplc TDK records arranged by date and lime (increasing <br />lu the right) and ilhtstrncs signature patterns Ih:n occur prior to severnncc <br />as the face approaches ;old moves past the cable (neg:rlive values inrlicalc <br />Distance past the cable).'I'hcse records show that strata nutventen( sheared <br />the c;tblc producing the Icfhvanl signal dcflcclions, called rcllccliun cocf- <br />ficicnlsmarked ;ts (a) in Pig. 5 :end measured in millithns (nip). -these <br />reflections increase in amplilurle as the lungwall face advances bcforc strata <br />nu,vcntcnl severs the cable which products the open end marked ax (b)]. <br />Additional shearing Is also dclcclcd and is nlarkcd as (c). Prccrimpcd dis- <br />rata talc <br />