Investigation of crack arrest fracture toughness of laboratory-manufactured polycrystalline ice

Approximately 50% of ice mass loss from ice sheets is due to icebergs breaking off in a process called calving. Icebergs are created through the incremental growth of crevasses, which are large fractures in the ice. Crevasse propagation and iceberg calving predictions within ice sheet models conflic...

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Bibliographic Details
Main Author: Alcorn, Derek West
Other Authors: Chairperson, Graduate Committee: Edward E. Adams
Format: Thesis
Language:English
Published: Montana State University - Bozeman, College of Engineering 2021
Subjects:
Ice
Online Access:https://scholarworks.montana.edu/xmlui/handle/1/16234
id ftmontanastateu:oai:scholarworks.montana.edu:1/16234
record_format openpolar
spelling ftmontanastateu:oai:scholarworks.montana.edu:1/16234 2023-05-15T13:44:27+02:00 Investigation of crack arrest fracture toughness of laboratory-manufactured polycrystalline ice Alcorn, Derek West Chairperson, Graduate Committee: Edward E. Adams 2021 application/pdf https://scholarworks.montana.edu/xmlui/handle/1/16234 en eng Montana State University - Bozeman, College of Engineering https://scholarworks.montana.edu/xmlui/handle/1/16234 Copyright 2021 by Derek West Alcorn Icebergs Ice Fracture mechanics Forecasting Mathematical models Thesis 2021 ftmontanastateu 2023-02-25T23:40:30Z Approximately 50% of ice mass loss from ice sheets is due to icebergs breaking off in a process called calving. Icebergs are created through the incremental growth of crevasses, which are large fractures in the ice. Crevasse propagation and iceberg calving predictions within ice sheet models conflict with direct observations of crevasse processes. Current ice sheet models assume that a crevasse will propagate until it reaches a depth where the stress intensity factor at the crack tip is less than that of crack initiation, however, this is likely an oversimplification as current models over estimate crevasse depth. A more robust model would also account for the crack arrest fracture toughness, a measure of how well a material can stop an already propagating crack. Here, we calculate crack arrest fracture toughness for samples of laboratory-manufactured polycrystalline ice. These samples were created using a radial freezing technique with a reproducible grain size distribution of 0.95 mm + or - 0.28 mm analyzed by cross-polarized light. Specimens were notched and brought to failure via a short-rod fracture toughness test at controlled temperatures and a constant displacement rate in a commercial mechanical testing apparatus with an environmental chamber. The presented data agrees with short-rod fracture toughness data collected from ice cores at the Filchner- Ronne Ice Shelf in Antarctica, demonstrating quasi-stable crack growth behavior. Results show the crack arrest fracture toughness of laboratory-manufactured polycrystalline ice is approximately 25 - 50% of fracture toughness. Using the crack arrest fracture toughness determined in this study would further increase modeled crevasse depth, indicating more analysis is required. Future studies can incorporate these data to more accurately determine crevasse penetration depth and improve iceberg calving predictions within ice sheet models. Thesis Antarc* Antarctica Filchner Ronne Ice Shelf Filchner-Ronne Ice Shelf Ice Sheet Ice Shelf Ronne Ice Shelf Montana State University (MSU): ScholarWorks Ronne Ice Shelf ENVELOPE(-61.000,-61.000,-78.500,-78.500)
institution Open Polar
collection Montana State University (MSU): ScholarWorks
op_collection_id ftmontanastateu
language English
topic Icebergs
Ice
Fracture mechanics
Forecasting
Mathematical models
spellingShingle Icebergs
Ice
Fracture mechanics
Forecasting
Mathematical models
Alcorn, Derek West
Investigation of crack arrest fracture toughness of laboratory-manufactured polycrystalline ice
topic_facet Icebergs
Ice
Fracture mechanics
Forecasting
Mathematical models
description Approximately 50% of ice mass loss from ice sheets is due to icebergs breaking off in a process called calving. Icebergs are created through the incremental growth of crevasses, which are large fractures in the ice. Crevasse propagation and iceberg calving predictions within ice sheet models conflict with direct observations of crevasse processes. Current ice sheet models assume that a crevasse will propagate until it reaches a depth where the stress intensity factor at the crack tip is less than that of crack initiation, however, this is likely an oversimplification as current models over estimate crevasse depth. A more robust model would also account for the crack arrest fracture toughness, a measure of how well a material can stop an already propagating crack. Here, we calculate crack arrest fracture toughness for samples of laboratory-manufactured polycrystalline ice. These samples were created using a radial freezing technique with a reproducible grain size distribution of 0.95 mm + or - 0.28 mm analyzed by cross-polarized light. Specimens were notched and brought to failure via a short-rod fracture toughness test at controlled temperatures and a constant displacement rate in a commercial mechanical testing apparatus with an environmental chamber. The presented data agrees with short-rod fracture toughness data collected from ice cores at the Filchner- Ronne Ice Shelf in Antarctica, demonstrating quasi-stable crack growth behavior. Results show the crack arrest fracture toughness of laboratory-manufactured polycrystalline ice is approximately 25 - 50% of fracture toughness. Using the crack arrest fracture toughness determined in this study would further increase modeled crevasse depth, indicating more analysis is required. Future studies can incorporate these data to more accurately determine crevasse penetration depth and improve iceberg calving predictions within ice sheet models.
author2 Chairperson, Graduate Committee: Edward E. Adams
format Thesis
author Alcorn, Derek West
author_facet Alcorn, Derek West
author_sort Alcorn, Derek West
title Investigation of crack arrest fracture toughness of laboratory-manufactured polycrystalline ice
title_short Investigation of crack arrest fracture toughness of laboratory-manufactured polycrystalline ice
title_full Investigation of crack arrest fracture toughness of laboratory-manufactured polycrystalline ice
title_fullStr Investigation of crack arrest fracture toughness of laboratory-manufactured polycrystalline ice
title_full_unstemmed Investigation of crack arrest fracture toughness of laboratory-manufactured polycrystalline ice
title_sort investigation of crack arrest fracture toughness of laboratory-manufactured polycrystalline ice
publisher Montana State University - Bozeman, College of Engineering
publishDate 2021
url https://scholarworks.montana.edu/xmlui/handle/1/16234
long_lat ENVELOPE(-61.000,-61.000,-78.500,-78.500)
geographic Ronne Ice Shelf
geographic_facet Ronne Ice Shelf
genre Antarc*
Antarctica
Filchner Ronne Ice Shelf
Filchner-Ronne Ice Shelf
Ice Sheet
Ice Shelf
Ronne Ice Shelf
genre_facet Antarc*
Antarctica
Filchner Ronne Ice Shelf
Filchner-Ronne Ice Shelf
Ice Sheet
Ice Shelf
Ronne Ice Shelf
op_relation https://scholarworks.montana.edu/xmlui/handle/1/16234
op_rights Copyright 2021 by Derek West Alcorn
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