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IUGG XXIV General Assembly July 2-13, 2007 Perugia, Italy (S) - IASPEI - International Association of Seismology and Physics of the Earth's Interior JSS009 Poster presentation 2054 Magnetotelluric study of mount ST. Helens Washington, USA: phase tensor analysis preliminary results Prof. Ray Cas School of Geosciences Monash University IAVCEI G. J. Hill, J. P. Cull, T. G. Caldwell, H. M. Bibby, W. Heise, M.K. Burgess, L.G. Mastin Our attempts to understand the processes that drive volcanism can be greatly enhanced by imaging the location and geometry of magma storage systems and by imaging the internal structure of volcanic complexes. The majority of efforts have been seismically based, using technologies adapted from petroleum and mineral exploration. Recently, however, there have been efforts to incorporate additional survey and data types, GPS and gravity successfully at Okmok, thermal and acoustic studies of Stromboli, self potential at Misti, and recently magneto-tellurics at Ruapehu. These multidisciplinary studies unequivocally add to the understanding of these volcanic systems, either by providing supporting evidence or suggesting alternative viable interpretations. We have undertaken a magnetotelluric study of Mount St. Helens a quaternary stratovolcano located in south-western Washington, USA, lying along the western front of the Cascade Range between Mt. Hood to the south and Mt. Rainier to the north, Mt. St. Helens is located in a region of transition both geologically and geophysically. Phase tensor and induction arrow analysis from 37 broadband magnetotelluric (~0.01 2000 s) sounding sites show the regional conductivity structure in a ~1000 km2 area around the volcano is 3-D at all period scales. Phase tensor analysis indicates that Mount St. Helens lies on the boundary of a large regional conductor to the north east of the volcano which begins at a depth of ~25 km and extends into the lower crust. The phase tensor analysis indicates a shallow response ( Keywords: magnetotellurics, mtsthelens
IUGG XXIV General Assembly July 2-13, 2007 Perugia, Italy (S) - IASPEI - International Association of Seismology and Physics of the Earth's Interior JSS009 Poster presentation 2055 Electric current emissions from brittle materials suffering near fracture mechanical stress Dr. Ilias Stavrakas Department of Electronics Technological Educational Institution ofAthens Panayiotis Kyriazis, Antonis Kyriazopoulos, Cimon Anastasiadis, Dimos Triantis, Filippos Vallianatos Pressure stimulated current (PSC) effects have been studied on various materials. In a number of previous presentations the applied mechanical stress has been correlated with the emitted current. In the present work current emissions are studied on a set of natural brittle materials like marble and amphibolite as well as on composite man-made materials like cement paste. Specifically, the stress was applied on the referred samples close to mechanical failure along with emitted PSC measurements. The recordings manifest that, dynamic phenomena, like macro-crack propagation and failure plane creation, result in current emissions. In these experiments despite the fact that the stress level was maintained practically constant in the vicinity of failure, significant PSC emissions of long duration were observed. The emitted PSC can be attributed to charge rearrangements due to dynamic change of the sample structure while new cracks are formed and the existing ones extend. In general, both the existence and interpretation of the PSC are consistent with the Moving Charged Dislocations (MCD) theory which relates the emitted current to crack formation and propagation and to the consequent strain variation. Strain recordings in the range near fracture support these findings since strain variations have been recorded without any change of stress. A deep and fast PSC reduction has always been recorded before fracture predicting the inevitable failure. This effect can be attributed to two coexisting causes: The former is related to the lack of any obvious triggering, i.e. stress or strain in the bulk of the material, that could lead to charge rearrangement since in this stage all the applied stress is localized at the edges of the main macro-crack that guides the failure plane. The latter is related with the observation that the failure plane limits significantly the available paths for the charges to move across the sample bulk which makes the detection of any emitted PSC even more difficult. Keywords: pressure stimulated currents, brittle materials fracture
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IUGG XXIV General Assembly July 2-13, 2007 Perugia, Italy<br />
(S) - <strong>IASPEI</strong> - International Association of Seismology and Physics of the Earth's<br />
Interior<br />
JSS009 Poster presentation 2055<br />
Electric current emissions from brittle materials suffering near fracture<br />
mechanical stress<br />
Dr. Ilias Stavrakas<br />
Department of Electronics Technological Educational Institution ofAthens<br />
Panayiotis Kyriazis, Antonis Kyriazopoulos, Cimon Anastasiadis, Dimos Triantis,<br />
Filippos Vallianatos<br />
Pressure stimulated current (PSC) effects have been studied on various materials. In a number of<br />
previous presentations the applied mechanical stress has been correlated with the emitted current. In<br />
the present work current emissions are studied on a set of natural brittle materials like marble and<br />
amphibolite as well as on composite man-made materials like cement paste. Specifically, the stress was<br />
applied on the referred samples close to mechanical failure along with emitted PSC measurements. The<br />
recordings manifest that, dynamic phenomena, like macro-crack propagation and failure plane creation,<br />
result in current emissions. In these experiments despite the fact that the stress level was maintained<br />
practically constant in the vicinity of failure, significant PSC emissions of long duration were observed.<br />
The emitted PSC can be attributed to charge rearrangements due to dynamic change of the sample<br />
structure while new cracks are formed and the existing ones extend. In general, both the existence and<br />
interpretation of the PSC are consistent with the Moving Charged Dislocations (MCD) theory which<br />
relates the emitted current to crack formation and propagation and to the consequent strain variation.<br />
Strain recordings in the range near fracture support these findings since strain variations have been<br />
recorded without any change of stress. A deep and fast PSC reduction has always been recorded before<br />
fracture predicting the inevitable failure. This effect can be attributed to two coexisting causes: The<br />
former is related to the lack of any obvious triggering, i.e. stress or strain in the bulk of the material,<br />
that could lead to charge rearrangement since in this stage all the applied stress is localized at the<br />
edges of the main macro-crack that guides the failure plane. The latter is related with the observation<br />
that the failure plane limits significantly the available paths for the charges to move across the sample<br />
bulk which makes the detection of any emitted PSC even more difficult.<br />
Keywords: pressure stimulated currents, brittle materials fracture