On borehole indentor (BHI) measurements and analysis

In situ measurements on stress–indentation curves conducted with the National Research Council (NRC), Canada and the Arctic and Antarctic Research Institute (ARRI), Russia borehole indentors (BHI) are analyzed and classified. This establishes harmony with laboratory observations on stress–strain dia...

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Published in:Cold Regions Science and Technology
Main Authors: Sinha, Nirmal K., Shkhinek, Karl, Smirnov, Victor
Format: Article in Journal/Newspaper
Language:English
Published: 2012
Subjects:
Online Access:https://doi.org/10.1016/j.coldregions.2012.01.009
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spelling ftnrccanada:oai:cisti-icist.nrc-cnrc.ca:cistinparc:21268704 2023-05-15T13:54:10+02:00 On borehole indentor (BHI) measurements and analysis Sinha, Nirmal K. Shkhinek, Karl Smirnov, Victor 2012-06 text https://doi.org/10.1016/j.coldregions.2012.01.009 https://nrc-publications.canada.ca/eng/view/object/?id=03cf1b46-14b8-47de-a649-fc4ea23d54bd https://nrc-publications.canada.ca/fra/voir/objet/?id=03cf1b46-14b8-47de-a649-fc4ea23d54bd eng eng issn:0165-232X Cold Regions Science and Technology, Volume: 76-77, Publication date: 2012-06, Pages: 109–120 doi:10.1016/j.coldregions.2012.01.009 pii:S0165232X12000225 Ice strength In-situ Borehole indentor Failure classification Acoustic-emissions Microstructural analysis article 2012 ftnrccanada https://doi.org/10.1016/j.coldregions.2012.01.009 2021-09-01T06:26:35Z In situ measurements on stress–indentation curves conducted with the National Research Council (NRC), Canada and the Arctic and Antarctic Research Institute (ARRI), Russia borehole indentors (BHI) are analyzed and classified. This establishes harmony with laboratory observations on stress–strain diagrams and some compatibility with the recommendations (ISO/DIS 19906) on estimating uniaxial ice strengths from BHI strengths. The analysis is devoted mainly to consider the influence of local ice conditions and the indentation rates on the pressure–indentation curves. Simultaneous records of the acoustic emission (AE) detected by accelerometers installed on the ice surface, within 1.5 m of the indentation plate, indicated that major cracks are nucleated at the ice/plate interface. Microstructural analysis of the indented ice confirmed this important conclusion in addition to revealing recrystallization as well as healing activities in the indented ice. An attempt, with extremely limited success, has been made in applying conventional ice failure criteria for predicting the observed stress–indentation curves. Phenomenologically, however, a power-law between the indentation-rate and upper-yield strength exhibits the same rate sensitivity (about 3) usually obtained for strain-rate dependence of uniaxial strengths. Numerical solutions of the rate-sensitive indentation processes must be developed (as has successfully been achieved for uniaxial tests) on microstructure-property based mathematical (rheological) model that includes the effects of the rate-dependent kinetics of deformation, microcracking and crack-enhanced creep. Premature brittle fractures are contact problems and modeling must consider the nucleation of cracks in ice at the ice/plate contact surface. Peer reviewed: Yes NRC publication: Yes Article in Journal/Newspaper Antarc* Antarctic Arctic and Antarctic Research Institute Arctic National Research Council Canada: NRC Publications Archive Antarctic Arctic Canada Cold Regions Science and Technology 76-77 109 120
institution Open Polar
collection National Research Council Canada: NRC Publications Archive
op_collection_id ftnrccanada
language English
topic Ice strength
In-situ
Borehole indentor
Failure classification
Acoustic-emissions
Microstructural analysis
spellingShingle Ice strength
In-situ
Borehole indentor
Failure classification
Acoustic-emissions
Microstructural analysis
Sinha, Nirmal K.
Shkhinek, Karl
Smirnov, Victor
On borehole indentor (BHI) measurements and analysis
topic_facet Ice strength
In-situ
Borehole indentor
Failure classification
Acoustic-emissions
Microstructural analysis
description In situ measurements on stress–indentation curves conducted with the National Research Council (NRC), Canada and the Arctic and Antarctic Research Institute (ARRI), Russia borehole indentors (BHI) are analyzed and classified. This establishes harmony with laboratory observations on stress–strain diagrams and some compatibility with the recommendations (ISO/DIS 19906) on estimating uniaxial ice strengths from BHI strengths. The analysis is devoted mainly to consider the influence of local ice conditions and the indentation rates on the pressure–indentation curves. Simultaneous records of the acoustic emission (AE) detected by accelerometers installed on the ice surface, within 1.5 m of the indentation plate, indicated that major cracks are nucleated at the ice/plate interface. Microstructural analysis of the indented ice confirmed this important conclusion in addition to revealing recrystallization as well as healing activities in the indented ice. An attempt, with extremely limited success, has been made in applying conventional ice failure criteria for predicting the observed stress–indentation curves. Phenomenologically, however, a power-law between the indentation-rate and upper-yield strength exhibits the same rate sensitivity (about 3) usually obtained for strain-rate dependence of uniaxial strengths. Numerical solutions of the rate-sensitive indentation processes must be developed (as has successfully been achieved for uniaxial tests) on microstructure-property based mathematical (rheological) model that includes the effects of the rate-dependent kinetics of deformation, microcracking and crack-enhanced creep. Premature brittle fractures are contact problems and modeling must consider the nucleation of cracks in ice at the ice/plate contact surface. Peer reviewed: Yes NRC publication: Yes
format Article in Journal/Newspaper
author Sinha, Nirmal K.
Shkhinek, Karl
Smirnov, Victor
author_facet Sinha, Nirmal K.
Shkhinek, Karl
Smirnov, Victor
author_sort Sinha, Nirmal K.
title On borehole indentor (BHI) measurements and analysis
title_short On borehole indentor (BHI) measurements and analysis
title_full On borehole indentor (BHI) measurements and analysis
title_fullStr On borehole indentor (BHI) measurements and analysis
title_full_unstemmed On borehole indentor (BHI) measurements and analysis
title_sort on borehole indentor (bhi) measurements and analysis
publishDate 2012
url https://doi.org/10.1016/j.coldregions.2012.01.009
https://nrc-publications.canada.ca/eng/view/object/?id=03cf1b46-14b8-47de-a649-fc4ea23d54bd
https://nrc-publications.canada.ca/fra/voir/objet/?id=03cf1b46-14b8-47de-a649-fc4ea23d54bd
geographic Antarctic
Arctic
Canada
geographic_facet Antarctic
Arctic
Canada
genre Antarc*
Antarctic
Arctic and Antarctic Research Institute
Arctic
genre_facet Antarc*
Antarctic
Arctic and Antarctic Research Institute
Arctic
op_relation issn:0165-232X
Cold Regions Science and Technology, Volume: 76-77, Publication date: 2012-06, Pages: 109–120
doi:10.1016/j.coldregions.2012.01.009
pii:S0165232X12000225
op_doi https://doi.org/10.1016/j.coldregions.2012.01.009
container_title Cold Regions Science and Technology
container_volume 76-77
container_start_page 109
op_container_end_page 120
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