Relating seismic velocities, thermal cracking and permeability in Mt. Etna and Iceland basalts
and columnar basalt from Seljadur (Iceland). Measurements were made in a servo-controlled steady-state-flow permeameter at effective pressures from 5–80 MPa, during both increasing and decreasing pressure cycles. Selected samples were thermally stressed at temperatures up to 900 1C to induce thermal...
Published in: | International Journal of Rock Mechanics and Mining Sciences |
---|---|
Main Author: | |
Other Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Elsevier Science Limited
2005
|
Subjects: | |
Online Access: | http://hdl.handle.net/2122/7898 https://doi.org/10.1016/j.ijrmms.2005.05.022 |
id |
ftingv:oai:www.earth-prints.org:2122/7898 |
---|---|
record_format |
openpolar |
spelling |
ftingv:oai:www.earth-prints.org:2122/7898 2023-05-15T16:48:48+02:00 Relating seismic velocities, thermal cracking and permeability in Mt. Etna and Iceland basalts Vinciguerra, S. Vinciguerra, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia 2005 http://hdl.handle.net/2122/7898 https://doi.org/10.1016/j.ijrmms.2005.05.022 en eng Elsevier Science Limited International journal of rock mechanics and mining sciences & geomechanics abstracts /42 (2005) 0148-9062 1879-2073 http://hdl.handle.net/2122/7898 doi:10.1016/j.ijrmms.2005.05.022 restricted Physical properties Lava flows Columnar basalts Thermal cracking 04. Solid Earth::04.01. Earth Interior::04.01.04. Mineral physics and properties of rocks article 2005 ftingv https://doi.org/10.1016/j.ijrmms.2005.05.022 2022-07-29T06:06:15Z and columnar basalt from Seljadur (Iceland). Measurements were made in a servo-controlled steady-state-flow permeameter at effective pressures from 5–80 MPa, during both increasing and decreasing pressure cycles. Selected samples were thermally stressed at temperatures up to 900 1C to induce thermal crack damage. Acoustic emission output was recorded throughout each thermal stressing experiment. At low pressure (0–10 MPa), the P-wave velocity of the columnar Seljadur basalt was 5.4 km/s, while for the Etnean lava flow basalt it was only 3.0–3.5 km/s. On increasing the pressure to 80 MPa, the velocity of Etnean basalt increased by 45%–60%, whereas that of Seljadur basalt increased by less than 2%. Furthermore, the velocity of Seljadur basalt thermally stressed to 900 1C fell by about 2.0 km/s, whereas the decrease for Etnean basalt was negligible. A similar pattern was observed in the permeability data. Permeability of Etnean basalt fell from about 7.5 10 16m2 to about 1.5 10 16m2 over the pressure range 5–80 MPa, while that for Seljadur basalt varied little from its initial low value of 9 10 21m2. Again, thermal stressing significantly increased the permeability of Seljadur basalt, whilst having a negligible effect on the Etnean basalt. These results clearly indicate that the Etnean basalt contains a much higher level of crack damage than the Seljadur basalt, and hence can explain the low velocities (3–4 km/s) generally inferred from seismic tomography for the Mt. Etna volcanic edifice Published 900-910 2.3. TTC - Laboratori di chimica e fisica delle rocce JCR Journal restricted Article in Journal/Newspaper Iceland Earth-Prints (Istituto Nazionale di Geofisica e Vulcanologia) Etna ENVELOPE(-19.191,-19.191,63.706,63.706) International Journal of Rock Mechanics and Mining Sciences 42 7-8 900 910 |
institution |
Open Polar |
collection |
Earth-Prints (Istituto Nazionale di Geofisica e Vulcanologia) |
op_collection_id |
ftingv |
language |
English |
topic |
Physical properties Lava flows Columnar basalts Thermal cracking 04. Solid Earth::04.01. Earth Interior::04.01.04. Mineral physics and properties of rocks |
spellingShingle |
Physical properties Lava flows Columnar basalts Thermal cracking 04. Solid Earth::04.01. Earth Interior::04.01.04. Mineral physics and properties of rocks Vinciguerra, S. Relating seismic velocities, thermal cracking and permeability in Mt. Etna and Iceland basalts |
topic_facet |
Physical properties Lava flows Columnar basalts Thermal cracking 04. Solid Earth::04.01. Earth Interior::04.01.04. Mineral physics and properties of rocks |
description |
and columnar basalt from Seljadur (Iceland). Measurements were made in a servo-controlled steady-state-flow permeameter at effective pressures from 5–80 MPa, during both increasing and decreasing pressure cycles. Selected samples were thermally stressed at temperatures up to 900 1C to induce thermal crack damage. Acoustic emission output was recorded throughout each thermal stressing experiment. At low pressure (0–10 MPa), the P-wave velocity of the columnar Seljadur basalt was 5.4 km/s, while for the Etnean lava flow basalt it was only 3.0–3.5 km/s. On increasing the pressure to 80 MPa, the velocity of Etnean basalt increased by 45%–60%, whereas that of Seljadur basalt increased by less than 2%. Furthermore, the velocity of Seljadur basalt thermally stressed to 900 1C fell by about 2.0 km/s, whereas the decrease for Etnean basalt was negligible. A similar pattern was observed in the permeability data. Permeability of Etnean basalt fell from about 7.5 10 16m2 to about 1.5 10 16m2 over the pressure range 5–80 MPa, while that for Seljadur basalt varied little from its initial low value of 9 10 21m2. Again, thermal stressing significantly increased the permeability of Seljadur basalt, whilst having a negligible effect on the Etnean basalt. These results clearly indicate that the Etnean basalt contains a much higher level of crack damage than the Seljadur basalt, and hence can explain the low velocities (3–4 km/s) generally inferred from seismic tomography for the Mt. Etna volcanic edifice Published 900-910 2.3. TTC - Laboratori di chimica e fisica delle rocce JCR Journal restricted |
author2 |
Vinciguerra, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia |
format |
Article in Journal/Newspaper |
author |
Vinciguerra, S. |
author_facet |
Vinciguerra, S. |
author_sort |
Vinciguerra, S. |
title |
Relating seismic velocities, thermal cracking and permeability in Mt. Etna and Iceland basalts |
title_short |
Relating seismic velocities, thermal cracking and permeability in Mt. Etna and Iceland basalts |
title_full |
Relating seismic velocities, thermal cracking and permeability in Mt. Etna and Iceland basalts |
title_fullStr |
Relating seismic velocities, thermal cracking and permeability in Mt. Etna and Iceland basalts |
title_full_unstemmed |
Relating seismic velocities, thermal cracking and permeability in Mt. Etna and Iceland basalts |
title_sort |
relating seismic velocities, thermal cracking and permeability in mt. etna and iceland basalts |
publisher |
Elsevier Science Limited |
publishDate |
2005 |
url |
http://hdl.handle.net/2122/7898 https://doi.org/10.1016/j.ijrmms.2005.05.022 |
long_lat |
ENVELOPE(-19.191,-19.191,63.706,63.706) |
geographic |
Etna |
geographic_facet |
Etna |
genre |
Iceland |
genre_facet |
Iceland |
op_relation |
International journal of rock mechanics and mining sciences & geomechanics abstracts /42 (2005) 0148-9062 1879-2073 http://hdl.handle.net/2122/7898 doi:10.1016/j.ijrmms.2005.05.022 |
op_rights |
restricted |
op_doi |
https://doi.org/10.1016/j.ijrmms.2005.05.022 |
container_title |
International Journal of Rock Mechanics and Mining Sciences |
container_volume |
42 |
container_issue |
7-8 |
container_start_page |
900 |
op_container_end_page |
910 |
_version_ |
1766038899888488448 |