Determining the Effectiveness of a Navigable Ice Boom.
The performance of a navigable ice boom was studied by monitoring the progression of the leading edge of the unconsolidated ice cover over a reach of the St. Marys River directly downstream of the boom. Ice and hydraulic data were obtained for four winters from 1975-76 through 1978-79 for the St. Ma...
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ftdtic:ADA162926 2023-05-15T16:37:11+02:00 Determining the Effectiveness of a Navigable Ice Boom. Perham,Roscoe E COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER NH 1985-10 text/html http://www.dtic.mil/docs/citations/ADA162926 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA162926 en eng http://www.dtic.mil/docs/citations/ADA162926 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Snow Ice and Permafrost Civil Engineering *ICE *BOOMS(EQUIPMENT) CONTROL THICKNESS SHIPS CONTROL SYSTEMS OPENING(PROCESS) WINTER NAVIGATION MODEL TESTS RELEASE LEADING EDGES COVERINGS RIVERS CHANNELS(WATERWAYS) HYDRAULIC EQUIPMENT DOWNSTREAM FLOW MICHIGAN Saint Marys River(Michigan) Text 1985 ftdtic 2016-02-21T01:20:08Z The performance of a navigable ice boom was studied by monitoring the progression of the leading edge of the unconsolidated ice cover over a reach of the St. Marys River directly downstream of the boom. Ice and hydraulic data were obtained for four winters from 1975-76 through 1978-79 for the St. Marys River at Sault Ste. Marie, Michigan. The ice cover progression rate was highest in early winter. The unconsolidated ice cover in the channel was estimated to have a thickness of at least 0.91 m and a porosity of 30%. During early winter the ice discharge per vessel passage averaged approximately 5500 cu m. for the four years. Model tests for this site had indicated that without an ice control structure of any type, an ice release of 63,000 cu m per ship passage could be expected; with an ice boom the release would be 12,300 cu m per ship passage. If a 100% effective boom releases no ice at all, then the measured rate indicates that the boom is 92% effective. On-site observations and time-lapse movies provided partial verification. Ice flowed down the ship track and through the navigation opening fairly often. Occasionally ice came over the boom in response to ship movements and natural causes. Keywords: Ice booms; Ice control; Winter navigation. Text Ice permafrost Defense Technical Information Center: DTIC Technical Reports database St. Marys River ENVELOPE(-55.839,-55.839,52.312,52.312) |
institution |
Open Polar |
collection |
Defense Technical Information Center: DTIC Technical Reports database |
op_collection_id |
ftdtic |
language |
English |
topic |
Snow Ice and Permafrost Civil Engineering *ICE *BOOMS(EQUIPMENT) CONTROL THICKNESS SHIPS CONTROL SYSTEMS OPENING(PROCESS) WINTER NAVIGATION MODEL TESTS RELEASE LEADING EDGES COVERINGS RIVERS CHANNELS(WATERWAYS) HYDRAULIC EQUIPMENT DOWNSTREAM FLOW MICHIGAN Saint Marys River(Michigan) |
spellingShingle |
Snow Ice and Permafrost Civil Engineering *ICE *BOOMS(EQUIPMENT) CONTROL THICKNESS SHIPS CONTROL SYSTEMS OPENING(PROCESS) WINTER NAVIGATION MODEL TESTS RELEASE LEADING EDGES COVERINGS RIVERS CHANNELS(WATERWAYS) HYDRAULIC EQUIPMENT DOWNSTREAM FLOW MICHIGAN Saint Marys River(Michigan) Perham,Roscoe E Determining the Effectiveness of a Navigable Ice Boom. |
topic_facet |
Snow Ice and Permafrost Civil Engineering *ICE *BOOMS(EQUIPMENT) CONTROL THICKNESS SHIPS CONTROL SYSTEMS OPENING(PROCESS) WINTER NAVIGATION MODEL TESTS RELEASE LEADING EDGES COVERINGS RIVERS CHANNELS(WATERWAYS) HYDRAULIC EQUIPMENT DOWNSTREAM FLOW MICHIGAN Saint Marys River(Michigan) |
description |
The performance of a navigable ice boom was studied by monitoring the progression of the leading edge of the unconsolidated ice cover over a reach of the St. Marys River directly downstream of the boom. Ice and hydraulic data were obtained for four winters from 1975-76 through 1978-79 for the St. Marys River at Sault Ste. Marie, Michigan. The ice cover progression rate was highest in early winter. The unconsolidated ice cover in the channel was estimated to have a thickness of at least 0.91 m and a porosity of 30%. During early winter the ice discharge per vessel passage averaged approximately 5500 cu m. for the four years. Model tests for this site had indicated that without an ice control structure of any type, an ice release of 63,000 cu m per ship passage could be expected; with an ice boom the release would be 12,300 cu m per ship passage. If a 100% effective boom releases no ice at all, then the measured rate indicates that the boom is 92% effective. On-site observations and time-lapse movies provided partial verification. Ice flowed down the ship track and through the navigation opening fairly often. Occasionally ice came over the boom in response to ship movements and natural causes. Keywords: Ice booms; Ice control; Winter navigation. |
author2 |
COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER NH |
format |
Text |
author |
Perham,Roscoe E |
author_facet |
Perham,Roscoe E |
author_sort |
Perham,Roscoe E |
title |
Determining the Effectiveness of a Navigable Ice Boom. |
title_short |
Determining the Effectiveness of a Navigable Ice Boom. |
title_full |
Determining the Effectiveness of a Navigable Ice Boom. |
title_fullStr |
Determining the Effectiveness of a Navigable Ice Boom. |
title_full_unstemmed |
Determining the Effectiveness of a Navigable Ice Boom. |
title_sort |
determining the effectiveness of a navigable ice boom. |
publishDate |
1985 |
url |
http://www.dtic.mil/docs/citations/ADA162926 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA162926 |
long_lat |
ENVELOPE(-55.839,-55.839,52.312,52.312) |
geographic |
St. Marys River |
geographic_facet |
St. Marys River |
genre |
Ice permafrost |
genre_facet |
Ice permafrost |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/ADA162926 |
op_rights |
APPROVED FOR PUBLIC RELEASE |
_version_ |
1766027479201349632 |