Concentrated Loads on a Floating Ice Sheet

Abstract The safe bearing capacity of a floating ice sheet is usually determined by limiting the maximum tensile stress which occurs under the load at the bottom of the ice sheet. If the size of the load distribution is large compared to the ice thickness, the thin plate theory predicts these stress...

Full description

Bibliographic Details
Published in:Journal of Glaciology
Main Author: Nevel, D. E.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1977
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000029312
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000029312
id crcambridgeupr:10.1017/s0022143000029312
record_format openpolar
spelling crcambridgeupr:10.1017/s0022143000029312 2024-03-03T08:45:23+00:00 Concentrated Loads on a Floating Ice Sheet Nevel, D. E. 1977 http://dx.doi.org/10.1017/s0022143000029312 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000029312 en eng Cambridge University Press (CUP) Journal of Glaciology volume 19, issue 81, page 237-245 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1977 crcambridgeupr https://doi.org/10.1017/s0022143000029312 2024-02-08T08:40:37Z Abstract The safe bearing capacity of a floating ice sheet is usually determined by limiting the maximum tensile stress which occurs under the load at the bottom of the ice sheet. If the size of the load distribution is large compared to the ice thickness, the thin plate theory predicts these stresses correctly. However, if the size of the load distribution becomes small compared to the ice thickness, the plate theory overestimates the stresses. In this case the ice sheet should he treated as a three-dimensional elastic layer. Previous investigators have solved the elastic-layer problem for loads distributed over a circular area, and have limited the results to the stress at the bottom of the ice sheet directly under the center of the load. In the present paper the stresses are evaluated at any radial position, and it is shown how these stresses approach those for the plate theory as the radial position becomes large. The solutions for the stresses are presented in integral form, as well as graphs from the numerical integration. These new results are significant for the superposition of stresses when two concentrated loads act near each other. Similarly for loads distributed over a rectangular area, the plate theory will overestimate the stresses if the dimensions of the load becomes small compared to the ice thickness. For this case integral solutions are presented for the stresses, and are evaluated directly under the center of the load. Article in Journal/Newspaper Ice Sheet Journal of Glaciology Cambridge University Press Journal of Glaciology 19 81 237 245
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Nevel, D. E.
Concentrated Loads on a Floating Ice Sheet
topic_facet Earth-Surface Processes
description Abstract The safe bearing capacity of a floating ice sheet is usually determined by limiting the maximum tensile stress which occurs under the load at the bottom of the ice sheet. If the size of the load distribution is large compared to the ice thickness, the thin plate theory predicts these stresses correctly. However, if the size of the load distribution becomes small compared to the ice thickness, the plate theory overestimates the stresses. In this case the ice sheet should he treated as a three-dimensional elastic layer. Previous investigators have solved the elastic-layer problem for loads distributed over a circular area, and have limited the results to the stress at the bottom of the ice sheet directly under the center of the load. In the present paper the stresses are evaluated at any radial position, and it is shown how these stresses approach those for the plate theory as the radial position becomes large. The solutions for the stresses are presented in integral form, as well as graphs from the numerical integration. These new results are significant for the superposition of stresses when two concentrated loads act near each other. Similarly for loads distributed over a rectangular area, the plate theory will overestimate the stresses if the dimensions of the load becomes small compared to the ice thickness. For this case integral solutions are presented for the stresses, and are evaluated directly under the center of the load.
format Article in Journal/Newspaper
author Nevel, D. E.
author_facet Nevel, D. E.
author_sort Nevel, D. E.
title Concentrated Loads on a Floating Ice Sheet
title_short Concentrated Loads on a Floating Ice Sheet
title_full Concentrated Loads on a Floating Ice Sheet
title_fullStr Concentrated Loads on a Floating Ice Sheet
title_full_unstemmed Concentrated Loads on a Floating Ice Sheet
title_sort concentrated loads on a floating ice sheet
publisher Cambridge University Press (CUP)
publishDate 1977
url http://dx.doi.org/10.1017/s0022143000029312
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000029312
genre Ice Sheet
Journal of Glaciology
genre_facet Ice Sheet
Journal of Glaciology
op_source Journal of Glaciology
volume 19, issue 81, page 237-245
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000029312
container_title Journal of Glaciology
container_volume 19
container_issue 81
container_start_page 237
op_container_end_page 245
_version_ 1792500938043293696