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Description
  • A method of velocity anisotropy analysis based on conventional ultrasonic transmission technique is proposed. Multiple transducers are used both to monitor acoustic emission and to measure velocities in different propagation directions. A sparse network of transducers located on the rock core surface allows approximation of elastic waves velocity distribution as an ellipsoidal surface. The shape and orientation of velocity ellipsoid is a measure of velocity anisotropy. A study of changes in velocity anisotropy and its orientation was performed on uniaxially loaded migmatite rock samples with distinct foliation. The velocity measurement was carried out during applying a uniaxial constant strain-rate loading. Orientation of the velocity ellipsoid corresponded to the anisotropy of rock structure up to activation of a failure plane. Prior to brittle failure, the axis of minimum velocity rotated from its initial direction normal to the foliation to a direction normal to the failure surface. The practical importance of the ellipsoid model lies in its simplicity and in its general applicability, which allows the use of measurement in a sparse sensor network. The-use of time-variable ellipsoidal velocity model led to a better localization of acoustic emission events during the sample loading when compared to the use of time-variable isotropic velocity model. The position of the failure plane determined by clustering of acoustic events foci coincided closely with observed sample failure.
  • A method of velocity anisotropy analysis based on conventional ultrasonic transmission technique is proposed. Multiple transducers are used both to monitor acoustic emission and to measure velocities in different propagation directions. A sparse network of transducers located on the rock core surface allows approximation of elastic waves velocity distribution as an ellipsoidal surface. The shape and orientation of velocity ellipsoid is a measure of velocity anisotropy. A study of changes in velocity anisotropy and its orientation was performed on uniaxially loaded migmatite rock samples with distinct foliation. The velocity measurement was carried out during applying a uniaxial constant strain-rate loading. Orientation of the velocity ellipsoid corresponded to the anisotropy of rock structure up to activation of a failure plane. Prior to brittle failure, the axis of minimum velocity rotated from its initial direction normal to the foliation to a direction normal to the failure surface. The practical importance of the ellipsoid model lies in its simplicity and in its general applicability, which allows the use of measurement in a sparse sensor network. The-use of time-variable ellipsoidal velocity model led to a better localization of acoustic emission events during the sample loading when compared to the use of time-variable isotropic velocity model. The position of the failure plane determined by clustering of acoustic events foci coincided closely with observed sample failure. (en)
Title
  • Determination of the anisotropy of elastic waves monitored by a sparse sensor network
  • Determination of the anisotropy of elastic waves monitored by a sparse sensor network (en)
skos:prefLabel
  • Determination of the anisotropy of elastic waves monitored by a sparse sensor network
  • Determination of the anisotropy of elastic waves monitored by a sparse sensor network (en)
skos:notation
  • RIV/00216208:11310/13:10188807!RIV14-GA0-11310___
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • I, P(GAP104/12/0915), Z(MSM0021620855)
http://linked.open...iv/cisloPeriodika
  • June
http://linked.open...vai/riv/dodaniDat
http://linked.open...aciTvurceVysledku
http://linked.open.../riv/druhVysledku
http://linked.open...iv/duvernostUdaju
http://linked.open...titaPredkladatele
http://linked.open...dnocenehoVysledku
  • 68944
http://linked.open...ai/riv/idVysledku
  • RIV/00216208:11310/13:10188807
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • Acoustic emission; Velocity ellipsoid; Ultrasonic transmission; Anisotropy; Seismic velocity (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • GB - Spojené království Velké Británie a Severního Irska
http://linked.open...ontrolniKodProRIV
  • [87CB2A87731A]
http://linked.open...i/riv/nazevZdroje
  • International Journal of Rock Mechanics and Minings Sciences
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...cetTvurcuVysledku
http://linked.open...vavai/riv/projekt
http://linked.open...UplatneniVysledku
http://linked.open...v/svazekPeriodika
  • 60
http://linked.open...iv/tvurceVysledku
  • Svitek, Tomáš
  • Vilhelm, Jan
  • Lokajicek, T.
  • Petruzalek, M.
  • Rudajev, V.
http://linked.open...ain/vavai/riv/wos
  • 000317802000022
http://linked.open...n/vavai/riv/zamer
issn
  • 1365-1609
number of pages
http://bibframe.org/vocab/doi
  • 10.1016/j.ijrmms.2012.12.020
http://localhost/t...ganizacniJednotka
  • 11310
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