Simulating weathering of basalt on Mars and Earth by thermal cycling

Physical weathering induced by heating and cooling may cause rock breakdown on Mars and Earth. We report results from parallel weathering simulations on basalt blocks exposed to diurnal cycles representing Mars-like (two simulation runs from -55 to +20 oC and -75 to +10 oC, 1-100% relative humidity,...

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Main Authors: Viles, H, Ehlmann, B, Wilson, C, Cebula, T, Page, M, Bourke, M
Format: Journal article
Language:English
Published: 2010
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author Viles, H
Ehlmann, B
Wilson, C
Cebula, T
Page, M
Bourke, M
author_facet Viles, H
Ehlmann, B
Wilson, C
Cebula, T
Page, M
Bourke, M
author_sort Viles, H
collection OXFORD
description Physical weathering induced by heating and cooling may cause rock breakdown on Mars and Earth. We report results from parallel weathering simulations on basalt blocks exposed to diurnal cycles representing Mars-like (two simulation runs from -55 to +20 oC and -75 to +10 oC, 1-100% relative humidity, 4-8 mbar pressure, CO2 atmosphere) and hot arid Earth (23-72o C, 30-100% relative humidity) conditions. Under Earth conditions, thermally pre-stressed blocks showed measurable strength declines, whilst salt pre-treated blocks showed strength gains. Under Mars-like conditions, pre-stressed blocks recorded greater or similar strength declines and salt pre-treated blocks showed more muted strength declines than under Earth conditions. The results imply that on Earth and Mars diurnal cycling of temperature alone can cause deterioration of basalt with a pre-existing stress history. The type of stress history is important, with salt pre-treatment affecting the response of thermally pre-stressed blocks under both Earth and Mars conditions. Copyright © 2010 by the American Geophysical Union.
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spelling oxford-uuid:74c9d7ca-ebe5-45b2-b447-7f5b718a4a9a2022-03-26T20:05:10ZSimulating weathering of basalt on Mars and Earth by thermal cyclingJournal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:74c9d7ca-ebe5-45b2-b447-7f5b718a4a9aEnglishSymplectic Elements at Oxford2010Viles, HEhlmann, BWilson, CCebula, TPage, MBourke, MPhysical weathering induced by heating and cooling may cause rock breakdown on Mars and Earth. We report results from parallel weathering simulations on basalt blocks exposed to diurnal cycles representing Mars-like (two simulation runs from -55 to +20 oC and -75 to +10 oC, 1-100% relative humidity, 4-8 mbar pressure, CO2 atmosphere) and hot arid Earth (23-72o C, 30-100% relative humidity) conditions. Under Earth conditions, thermally pre-stressed blocks showed measurable strength declines, whilst salt pre-treated blocks showed strength gains. Under Mars-like conditions, pre-stressed blocks recorded greater or similar strength declines and salt pre-treated blocks showed more muted strength declines than under Earth conditions. The results imply that on Earth and Mars diurnal cycling of temperature alone can cause deterioration of basalt with a pre-existing stress history. The type of stress history is important, with salt pre-treatment affecting the response of thermally pre-stressed blocks under both Earth and Mars conditions. Copyright © 2010 by the American Geophysical Union.
spellingShingle Viles, H
Ehlmann, B
Wilson, C
Cebula, T
Page, M
Bourke, M
Simulating weathering of basalt on Mars and Earth by thermal cycling
title Simulating weathering of basalt on Mars and Earth by thermal cycling
title_full Simulating weathering of basalt on Mars and Earth by thermal cycling
title_fullStr Simulating weathering of basalt on Mars and Earth by thermal cycling
title_full_unstemmed Simulating weathering of basalt on Mars and Earth by thermal cycling
title_short Simulating weathering of basalt on Mars and Earth by thermal cycling
title_sort simulating weathering of basalt on mars and earth by thermal cycling
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AT pagem simulatingweatheringofbasaltonmarsandearthbythermalcycling
AT bourkem simulatingweatheringofbasaltonmarsandearthbythermalcycling