The variation of creep strain with the number of freeze-thaw cycles.

<p><b>(a)</b> Intact rock specimens. <b>(b)</b> Slow-slow fissures.</p>

محفوظ في:
التفاصيل البيبلوغرافية
المؤلف الرئيسي: Dengke Yang (842532) (author)
مؤلفون آخرون: Xiaoxiao Duan (3610763) (author), Keyan Cheng (21368031) (author), Lijun Xie (520423) (author), Yongjun Song (6320696) (author)
منشور في: 2025
الموضوعات:
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_version_ 1852020395894374400
author Dengke Yang (842532)
author2 Xiaoxiao Duan (3610763)
Keyan Cheng (21368031)
Lijun Xie (520423)
Yongjun Song (6320696)
author2_role author
author
author
author
author_facet Dengke Yang (842532)
Xiaoxiao Duan (3610763)
Keyan Cheng (21368031)
Lijun Xie (520423)
Yongjun Song (6320696)
author_role author
dc.creator.none.fl_str_mv Dengke Yang (842532)
Xiaoxiao Duan (3610763)
Keyan Cheng (21368031)
Lijun Xie (520423)
Yongjun Song (6320696)
dc.date.none.fl_str_mv 2025-05-15T14:55:14Z
dc.identifier.none.fl_str_mv 10.1371/journal.pone.0320194.g006
dc.relation.none.fl_str_mv https://figshare.com/articles/figure/The_variation_of_creep_strain_with_the_number_of_freeze-thaw_cycles_/29074926
dc.rights.none.fl_str_mv CC BY 4.0
info:eu-repo/semantics/openAccess
dc.subject.none.fl_str_mv Biophysics
Medicine
Physiology
Biotechnology
Evolutionary Biology
Developmental Biology
Space Science
Environmental Sciences not elsewhere classified
Biological Sciences not elsewhere classified
greater fracture angles
rock &# 8217
open rock masses
thaw cycle frequency
greater strain generation
double fractured rock
fracture angle affects
rock mass engineering
thaw cycles exert
fractured rock samples
considering different freeze
fractured rock
fracture angle
rock samples
thaw cycles
fracture orientations
engineering design
different pre
rock varies
thaw frequencies
thaw conditions
axial strain
term strength
significant influence
safety construction
risk assessment
results reveal
rapid decrease
pronounced increases
prolonged loading
increasing trend
increasing freeze
guiding significance
failure mode
experimental tests
creep strains
creep phenomena
creep failure
creep characteristics
creep behavior
cold regions
dc.title.none.fl_str_mv The variation of creep strain with the number of freeze-thaw cycles.
dc.type.none.fl_str_mv Image
Figure
info:eu-repo/semantics/publishedVersion
image
description <p><b>(a)</b> Intact rock specimens. <b>(b)</b> Slow-slow fissures.</p>
eu_rights_str_mv openAccess
id Manara_a46d0cfbf4f066f3dfd0efd86c3c2dc0
identifier_str_mv 10.1371/journal.pone.0320194.g006
network_acronym_str Manara
network_name_str ManaraRepo
oai_identifier_str oai:figshare.com:article/29074926
publishDate 2025
repository.mail.fl_str_mv
repository.name.fl_str_mv
repository_id_str
rights_invalid_str_mv CC BY 4.0
spelling The variation of creep strain with the number of freeze-thaw cycles.Dengke Yang (842532)Xiaoxiao Duan (3610763)Keyan Cheng (21368031)Lijun Xie (520423)Yongjun Song (6320696)BiophysicsMedicinePhysiologyBiotechnologyEvolutionary BiologyDevelopmental BiologySpace ScienceEnvironmental Sciences not elsewhere classifiedBiological Sciences not elsewhere classifiedgreater fracture anglesrock &# 8217open rock massesthaw cycle frequencygreater strain generationdouble fractured rockfracture angle affectsrock mass engineeringthaw cycles exertfractured rock samplesconsidering different freezefractured rockfracture anglerock samplesthaw cyclesfracture orientationsengineering designdifferent prerock variesthaw frequenciesthaw conditionsaxial strainterm strengthsignificant influencesafety constructionrisk assessmentresults revealrapid decreasepronounced increasesprolonged loadingincreasing trendincreasing freezeguiding significancefailure modeexperimental testscreep strainscreep phenomenacreep failurecreep characteristicscreep behaviorcold regions<p><b>(a)</b> Intact rock specimens. <b>(b)</b> Slow-slow fissures.</p>2025-05-15T14:55:14ZImageFigureinfo:eu-repo/semantics/publishedVersionimage10.1371/journal.pone.0320194.g006https://figshare.com/articles/figure/The_variation_of_creep_strain_with_the_number_of_freeze-thaw_cycles_/29074926CC BY 4.0info:eu-repo/semantics/openAccessoai:figshare.com:article/290749262025-05-15T14:55:14Z
spellingShingle The variation of creep strain with the number of freeze-thaw cycles.
Dengke Yang (842532)
Biophysics
Medicine
Physiology
Biotechnology
Evolutionary Biology
Developmental Biology
Space Science
Environmental Sciences not elsewhere classified
Biological Sciences not elsewhere classified
greater fracture angles
rock &# 8217
open rock masses
thaw cycle frequency
greater strain generation
double fractured rock
fracture angle affects
rock mass engineering
thaw cycles exert
fractured rock samples
considering different freeze
fractured rock
fracture angle
rock samples
thaw cycles
fracture orientations
engineering design
different pre
rock varies
thaw frequencies
thaw conditions
axial strain
term strength
significant influence
safety construction
risk assessment
results reveal
rapid decrease
pronounced increases
prolonged loading
increasing trend
increasing freeze
guiding significance
failure mode
experimental tests
creep strains
creep phenomena
creep failure
creep characteristics
creep behavior
cold regions
status_str publishedVersion
title The variation of creep strain with the number of freeze-thaw cycles.
title_full The variation of creep strain with the number of freeze-thaw cycles.
title_fullStr The variation of creep strain with the number of freeze-thaw cycles.
title_full_unstemmed The variation of creep strain with the number of freeze-thaw cycles.
title_short The variation of creep strain with the number of freeze-thaw cycles.
title_sort The variation of creep strain with the number of freeze-thaw cycles.
topic Biophysics
Medicine
Physiology
Biotechnology
Evolutionary Biology
Developmental Biology
Space Science
Environmental Sciences not elsewhere classified
Biological Sciences not elsewhere classified
greater fracture angles
rock &# 8217
open rock masses
thaw cycle frequency
greater strain generation
double fractured rock
fracture angle affects
rock mass engineering
thaw cycles exert
fractured rock samples
considering different freeze
fractured rock
fracture angle
rock samples
thaw cycles
fracture orientations
engineering design
different pre
rock varies
thaw frequencies
thaw conditions
axial strain
term strength
significant influence
safety construction
risk assessment
results reveal
rapid decrease
pronounced increases
prolonged loading
increasing trend
increasing freeze
guiding significance
failure mode
experimental tests
creep strains
creep phenomena
creep failure
creep characteristics
creep behavior
cold regions