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早期受冻对水工混凝土水化程度及孔隙结构的影响

覃源 田茜茜 晋洁 赵靖伟 吴江江 吕杲 段明翰

水力发电学报2025,Vol.44Issue(7):55-66,12.
水力发电学报2025,Vol.44Issue(7):55-66,12.DOI:10.11660/slfdxb.20250704

早期受冻对水工混凝土水化程度及孔隙结构的影响

Influence of early freezing on hydration degree and pore structure of hydraulic concrete

覃源 1田茜茜 1晋洁 2赵靖伟 3吴江江 4吕杲 5段明翰1

作者信息

  • 1. 西安理工大学 旱区水工程生态环境全国重点实验室,西安 710048
  • 2. 国网甘肃省电力公司刘家峡水电厂,甘肃 永靖 731600
  • 3. 西安理工大学 旱区水工程生态环境全国重点实验室,西安 710048||中国电建集团西北勘测设计研究院有限公司,西安 710065
  • 4. 西安理工大学 旱区水工程生态环境全国重点实验室,西安 710048||中国能源建设集团西北建设投资有限公司,西安 710024
  • 5. 中国电建集团西北勘测设计研究院有限公司,西安 710065
  • 折叠

摘要

Abstract

Climatic conditions in the alpine region are complicated and changeable.A sudden temperature drop is easy to impact the hydration degree and pore structure of fresh concrete,resulting in its early frost damage,extremely unfavorable to the development of its physical properties such as strength.To explore the damage mechanism of hydraulic concrete in early freezing conditions,this study conducts experimental tests on its mechanical properties,hydration behavior,and pore structure,by varying pre-curing time(6 h,12 h,24 h,and 48 h),freezing time(6 h,12 h,24 h,and 48 h),and freezing temperature(-1 ℃,-5 ℃,and-10 ℃).The results show that an increase in freezing time or a decrease in freezing temperature increases porosity and decreases hydration degree,while a longer pre-curing time increases hydration degree and transforms more large pores into small ones.The compressive strength of early frozen concrete is proportional to pre-curing time,and inversely proportional to freezing time or freezing temperature;its pore structure shows obvious fractal characteristics,and significant correlation exists between the hydration degree and mechanical properties.

关键词

水工混凝土/早期受冻/水化程度/孔结构/分形维数

Key words

hydraulic concrete/early freezing/degree of hydration/pore structure/fractal dimension

分类

建筑与水利

引用本文复制引用

覃源,田茜茜,晋洁,赵靖伟,吴江江,吕杲,段明翰..早期受冻对水工混凝土水化程度及孔隙结构的影响[J].水力发电学报,2025,44(7):55-66,12.

基金项目

国家自然科学基金项目(52079109 ()

52279139) ()

水力发电学报

OA北大核心

1003-1243

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