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    Early Detection of Rock Movement with Time Domain Reflectometry

    Source: Journal of Geotechnical Engineering:;1994:;Volume ( 120 ):;issue: 008
    Author:
    Charles H. Dowding
    ,
    Fei‐Chiu Huang
    DOI: 10.1061/(ASCE)0733-9410(1994)120:8(1413)
    Publisher: American Society of Civil Engineers
    Abstract: Remote operation of a time domain reflectometry (TDR) system demonstrates the effectiveness of telemetric monitoring for early detection of rock movement. During field testing reported here, TDR data were related to shear deformation above a longwall caving operation using a correlation between the signature reflection coefficient and shear deformation established through laboratory measurements. A 175‐m (575 ft) long vertical coaxial TDR cable was grouted into the rock mass above the longwall coal‐mining operation and attached to the aboveground‐pulsing instrument. TDR data were then remotely acquired twice daily by an operator some 500 km away. Comparison of TDR signature changes with longwall‐face location showed that localized changes were detected four days before surface subsidence occurred when mining was still 64 m (210 ft) away. Since the mining was moving toward the cable at a rate of 10 m/day, a warning interval is expected to be larger for premined sites with lower deformation rates.
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      Early Detection of Rock Movement with Time Domain Reflectometry

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    http://yetl.yabesh.ir/yetl1/handle/yetl/21485
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    • Journal of Geotechnical Engineering

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    contributor authorCharles H. Dowding
    contributor authorFei‐Chiu Huang
    date accessioned2017-05-08T20:37:20Z
    date available2017-05-08T20:37:20Z
    date copyrightAugust 1994
    date issued1994
    identifier other%28asce%290733-9410%281994%29120%3A8%281413%29.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/21485
    description abstractRemote operation of a time domain reflectometry (TDR) system demonstrates the effectiveness of telemetric monitoring for early detection of rock movement. During field testing reported here, TDR data were related to shear deformation above a longwall caving operation using a correlation between the signature reflection coefficient and shear deformation established through laboratory measurements. A 175‐m (575 ft) long vertical coaxial TDR cable was grouted into the rock mass above the longwall coal‐mining operation and attached to the aboveground‐pulsing instrument. TDR data were then remotely acquired twice daily by an operator some 500 km away. Comparison of TDR signature changes with longwall‐face location showed that localized changes were detected four days before surface subsidence occurred when mining was still 64 m (210 ft) away. Since the mining was moving toward the cable at a rate of 10 m/day, a warning interval is expected to be larger for premined sites with lower deformation rates.
    publisherAmerican Society of Civil Engineers
    titleEarly Detection of Rock Movement with Time Domain Reflectometry
    typeJournal Paper
    journal volume120
    journal issue8
    journal titleJournal of Geotechnical Engineering
    identifier doi10.1061/(ASCE)0733-9410(1994)120:8(1413)
    treeJournal of Geotechnical Engineering:;1994:;Volume ( 120 ):;issue: 008
    contenttypeFulltext
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