Design Factors for River Ice Booms Analyzed (Issleovanie Ledozashchitnykh Zapanei)

Model studies were made to determine hydraulic characteristics of structures for protecting ships wintering in rivers under conditions similar to those observed in European and Siberian rivers (ice-cover thickness up to 1.8m. and river depth to 12m.). The experiments are described, and data are math...

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Bibliographic Details
Main Author: Latyshenkov,A. M.
Other Authors: COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H
Format: Text
Language:English
Published: 1975
Subjects:
ICE
Ice
Online Access:http://www.dtic.mil/docs/citations/ADA014886
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA014886
id ftdtic:ADA014886
record_format openpolar
spelling ftdtic:ADA014886 2023-05-15T16:37:01+02:00 Design Factors for River Ice Booms Analyzed (Issleovanie Ledozashchitnykh Zapanei) Latyshenkov,A. M. COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H 1975-09 text/html http://www.dtic.mil/docs/citations/ADA014886 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA014886 en eng http://www.dtic.mil/docs/citations/ADA014886 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Snow Ice and Permafrost Civil Engineering *RIVERS *ICE PREVENTION STRESSES VELOCITY MATHEMATICAL MODELS USSR THICKNESS SHIPS WATER FLOW EXPERIMENTAL DATA DEPTH ICE PRESSURE PROTECTION TRANSLATIONS BATTLES FRICTION FLOATING BODIES BOOMS(EQUIPMENT) SIBERIA HARBOR MODELS MECHANICAL CABLES *Ice booms River ice Ice cover Text 1975 ftdtic 2016-02-20T10:12:57Z Model studies were made to determine hydraulic characteristics of structures for protecting ships wintering in rivers under conditions similar to those observed in European and Siberian rivers (ice-cover thickness up to 1.8m. and river depth to 12m.). The experiments are described, and data are mathematically analyzed. Formulas and graphs for calculating the stresses as a function of ice-cover thickness, flow speed, and width and depth of the river are suggested. The ice pressure on protective booms in a stream wider than 30 m was found to increase 85-90% due to the friction between the lower ice surface and flowing water. The friction coefficient is proportional to the ratio of ice thickness to flow depth. Trans. of Gidrotekhnicheskoe Stroitel'stvo (USSR) v15 n4 p13-19 1946. Text Ice permafrost Siberia Defense Technical Information Center: DTIC Technical Reports database
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
*RIVERS
*ICE PREVENTION
STRESSES
VELOCITY
MATHEMATICAL MODELS
USSR
THICKNESS
SHIPS
WATER FLOW
EXPERIMENTAL DATA
DEPTH
ICE
PRESSURE
PROTECTION
TRANSLATIONS
BATTLES
FRICTION
FLOATING BODIES
BOOMS(EQUIPMENT)
SIBERIA
HARBOR MODELS
MECHANICAL CABLES
*Ice booms
River ice
Ice cover
spellingShingle Snow
Ice and Permafrost
Civil Engineering
*RIVERS
*ICE PREVENTION
STRESSES
VELOCITY
MATHEMATICAL MODELS
USSR
THICKNESS
SHIPS
WATER FLOW
EXPERIMENTAL DATA
DEPTH
ICE
PRESSURE
PROTECTION
TRANSLATIONS
BATTLES
FRICTION
FLOATING BODIES
BOOMS(EQUIPMENT)
SIBERIA
HARBOR MODELS
MECHANICAL CABLES
*Ice booms
River ice
Ice cover
Latyshenkov,A. M.
Design Factors for River Ice Booms Analyzed (Issleovanie Ledozashchitnykh Zapanei)
topic_facet Snow
Ice and Permafrost
Civil Engineering
*RIVERS
*ICE PREVENTION
STRESSES
VELOCITY
MATHEMATICAL MODELS
USSR
THICKNESS
SHIPS
WATER FLOW
EXPERIMENTAL DATA
DEPTH
ICE
PRESSURE
PROTECTION
TRANSLATIONS
BATTLES
FRICTION
FLOATING BODIES
BOOMS(EQUIPMENT)
SIBERIA
HARBOR MODELS
MECHANICAL CABLES
*Ice booms
River ice
Ice cover
description Model studies were made to determine hydraulic characteristics of structures for protecting ships wintering in rivers under conditions similar to those observed in European and Siberian rivers (ice-cover thickness up to 1.8m. and river depth to 12m.). The experiments are described, and data are mathematically analyzed. Formulas and graphs for calculating the stresses as a function of ice-cover thickness, flow speed, and width and depth of the river are suggested. The ice pressure on protective booms in a stream wider than 30 m was found to increase 85-90% due to the friction between the lower ice surface and flowing water. The friction coefficient is proportional to the ratio of ice thickness to flow depth. Trans. of Gidrotekhnicheskoe Stroitel'stvo (USSR) v15 n4 p13-19 1946.
author2 COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H
format Text
author Latyshenkov,A. M.
author_facet Latyshenkov,A. M.
author_sort Latyshenkov,A. M.
title Design Factors for River Ice Booms Analyzed (Issleovanie Ledozashchitnykh Zapanei)
title_short Design Factors for River Ice Booms Analyzed (Issleovanie Ledozashchitnykh Zapanei)
title_full Design Factors for River Ice Booms Analyzed (Issleovanie Ledozashchitnykh Zapanei)
title_fullStr Design Factors for River Ice Booms Analyzed (Issleovanie Ledozashchitnykh Zapanei)
title_full_unstemmed Design Factors for River Ice Booms Analyzed (Issleovanie Ledozashchitnykh Zapanei)
title_sort design factors for river ice booms analyzed (issleovanie ledozashchitnykh zapanei)
publishDate 1975
url http://www.dtic.mil/docs/citations/ADA014886
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA014886
genre Ice
permafrost
Siberia
genre_facet Ice
permafrost
Siberia
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/ADA014886
op_rights APPROVED FOR PUBLIC RELEASE
_version_ 1766027331164438528