Fracture Toughness of Ice: A Preliminary Account of Some New Experiments

Abstract This paper describes the first results from an experiment to measure the fracture toughness of ice. Two experimental techniques have been used; fracture of pre-notched rectangular specimens in three- and four-point bending, and from the observation of the cracks which form underneath an ind...

Full description

Bibliographic Details
Published in:Journal of Glaciology
Main Authors: Goodman, D. J., Tabor, D.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1978
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000033761
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000033761
id crcambridgeupr:10.1017/s0022143000033761
record_format openpolar
spelling crcambridgeupr:10.1017/s0022143000033761 2024-04-28T08:26:46+00:00 Fracture Toughness of Ice: A Preliminary Account of Some New Experiments Goodman, D. J. Tabor, D. 1978 http://dx.doi.org/10.1017/s0022143000033761 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000033761 en eng Cambridge University Press (CUP) Journal of Glaciology volume 21, issue 85, page 651-660 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1978 crcambridgeupr https://doi.org/10.1017/s0022143000033761 2024-04-02T06:55:06Z Abstract This paper describes the first results from an experiment to measure the fracture toughness of ice. Two experimental techniques have been used; fracture of pre-notched rectangular specimens in three- and four-point bending, and from the observation of the cracks which form underneath an indenter forced into the ice surface. In the latter test the indenter behaves like a wedge. We have observed that for indenters with large interior angles the plastic zone beneath the indenter may itself behave like a wedge. Data obtained over a range of temperatures has been compared with the little other data available. We find a decrease of fracture toughness as the temperature is lowered, which is the reverse of that observed by H. W. Liu and L. W. Loop. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 21 85 651 660
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Goodman, D. J.
Tabor, D.
Fracture Toughness of Ice: A Preliminary Account of Some New Experiments
topic_facet Earth-Surface Processes
description Abstract This paper describes the first results from an experiment to measure the fracture toughness of ice. Two experimental techniques have been used; fracture of pre-notched rectangular specimens in three- and four-point bending, and from the observation of the cracks which form underneath an indenter forced into the ice surface. In the latter test the indenter behaves like a wedge. We have observed that for indenters with large interior angles the plastic zone beneath the indenter may itself behave like a wedge. Data obtained over a range of temperatures has been compared with the little other data available. We find a decrease of fracture toughness as the temperature is lowered, which is the reverse of that observed by H. W. Liu and L. W. Loop.
format Article in Journal/Newspaper
author Goodman, D. J.
Tabor, D.
author_facet Goodman, D. J.
Tabor, D.
author_sort Goodman, D. J.
title Fracture Toughness of Ice: A Preliminary Account of Some New Experiments
title_short Fracture Toughness of Ice: A Preliminary Account of Some New Experiments
title_full Fracture Toughness of Ice: A Preliminary Account of Some New Experiments
title_fullStr Fracture Toughness of Ice: A Preliminary Account of Some New Experiments
title_full_unstemmed Fracture Toughness of Ice: A Preliminary Account of Some New Experiments
title_sort fracture toughness of ice: a preliminary account of some new experiments
publisher Cambridge University Press (CUP)
publishDate 1978
url http://dx.doi.org/10.1017/s0022143000033761
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000033761
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 21, issue 85, page 651-660
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000033761
container_title Journal of Glaciology
container_volume 21
container_issue 85
container_start_page 651
op_container_end_page 660
_version_ 1797586013136093184