Laserfiche WebLink
• <br />._.~. Irn Sr) 1 I it o-..r,a o-onana <br />=Ji 11 ~a[R•...Kfvi-`.: ~Ji ~:'''•'.,~ {.:.::_...,.I V o ,~ cnuw o.r.IwWq <br />nli '`. Ql(Y ~ ~ nll_»~R~ -__ Iml Iml <br />,.. <br />f <br />n „• ; + '; <br />Slaln RI d <br />._.0.. .1 9 b. ..w .r„b <br />. ., <br />.. <br />,, <br />.M~. <br />14 y` <br />:l~l ~ 1 AS1 ~ o ~ m °.r bime.ee.e.nn '^- :~u~ <br />.( :.i~l s} .rranw <br />'•r. [. <br />1111 <br />!1 •• =m <br />~ _ _ <br />. ...r .y.... ~ <br />r i <br />r ~ m..p <br />r ., . ., ~..... ~. <br />...ru-........ ~ <br />_,...r....,_:....,.. ~_.. ....., <br />y..I. ...... n. ..-.~, ..-.r I <br />.r'-2i V ~~ a 50011 Q.q..,..a~ -_- -~n --u- ~ eu.ae,ars.a~ <br />f I}S.I .3.(J <br />II ~"~ I)II N ~.' 1 JD Ill brq~,J ryn <br />~ r <br />e,a- ro <br />~~ ;: ~. <br />- I ~ I° [r Neb <br />'"rl.~i, .i' TT :nni.n...i n~-I.T...,..n., ~.-.1.s..q:..v:.....a'i.m. . <br />~•JJWJ~~ .d'li,:u..~.•,~;.......:.~.,..._i ....~r._~.~.. i...-~..... ~:.,....~.,~... ..n. .o......._ mn- -us ru- <br />~~ FIG. 0. Depths of TDR-Measured Rock-Mass Movement, Relative Locallon of <br />Longwall Face and Assoclaled Strallgraphy <br />nac <br />House g JOa <br /> Holo Location <br />^ for TDR Cablo ~ <br />< <br />\V <br />/ <br /> <br />6 <br />u 2oa <br />w 6 5 <br />> <br />\ $ 10C <br />210 205 200 195 190 <br />73 60 <br />o <br />m ~ <br /> I <br />150 II <br /> ~ 6 .la[ <br /> I <br />50 m ° za <br />• <br />FIG. 2. Hole Locallon and Mining Sile Map that Shows Underground Works, Long- <br />wall-Face Locallon, Dale, and Surface Culture <br />lance indicators, marked as (d), improve location accuracy of ntcastne- <br />ntenlx. Waveform I (May 2;t, IU:4fi) is the firs) signalurc recorded alter <br />able insLdlalion. This record serves as the benchmark against which other <br />signals arc compared. Waveforms 2 (.lone 12, IG:.lS), } (.lone 11, 7:21), ;uul <br />4 (June 13, IG:2S) wcrc rcatnled before, al, :Ind :Ifler complete sevcl:utce <br />al a depth of Gfi m (217 fl ). In a similar fashion, wave (Dons S (.tune 14. <br />I1:17), 6 (June I-0, IG:27), and 7 (Jmlc I.1, 211ah) wcrc recut ded before, <br />al, and after wmpletc severance al a depth of d8 m (158 fl). <br />Time Variation of Morcutcnl <br />• Pig. 6 compares the lime variation of the reflection signahues al Jhc <br />severance locations (depths GG m and dpi m) with surface scnlcntcnls al the <br />1416 <br />J00 <br />.loco ~soo o sao loco ,soo <br />Tlmo Sirxo Cablo InslallaE (Mms) <br />FIG. 4. Longwall Face Advance Relarlve to Cable Inslallallon In Terms o1 Dlslance <br />and Time <br />l~l)IL cable-bolt collar as mining progressed luwanl the cable. 'Che initial <br />readings provide the baseline (ur subscyucnl observations. <br />"fhc cable was installed on May 23, 1991 and polled remotely on May 28 <br />as shown in Pig. fi. There was no signalurc change between May 28 and the <br />next leading on May 29. Between May 30 and .tune 3 the sysJCm undd nut <br />be accessed due to interruption of declricll service caused by a lhunder- <br />slunu. 'I~hc su rfacc nu nnuncnts wcrc not sw vcycd bchvccn May 23 and <br />June 8. <br />As dcmonsl rated in Pig. G, dclcclion of su bsurfacc movement by TDR <br />some four days before dclcclion al Jhe su r(ace demonstrates the carly- <br />warning capability of the "1'DR system. On .tune 4, remote polling showed <br />a signalurc rc(Icchon al a depth of GG nt. This spike progressively enlarged <br />~ <br />1r~1 <br /> <br />a q~ Fnco UndmMe Cablo <br />° 9A~ <br />tore <br />