摘要
通过自主研发的土体冻融装置,在开放系统下进行了单向冻结深厚表土试验,研究了冷端温度、含水率对土体冻胀及冻结过程中水热迁移的影响规律。结果表明:含水率影响了快速增长阶段的冻胀量和增长减缓阶段的冻胀时间。冻胀率和含水率呈良好的线性关系,开放系统下的土体冻结也可能会发生冻缩现象。
Unidirectional freezing deep overburden soil tests were carried out by soil freezing and thawing apparatus with water supply. The influences of temperature of freezing plate and water content on freezing expansion of soil and water-heat transference were researched. The results show that the water content has almost. The water content affects the frost heave amount in rapid growth stage and the frost heave time in growth slowing stage . The frost heaving rate and water content show a good linear relationship . Under open system, freezing soil may also occur cold shrink phenomenon
作者
吴东军
朱杰
李锐阳
WU Dong-jun;ZHU Jie;LI Rui-yang(School of Civil Engineering and Architecture, Anhui University of Science and Technology, Huainan 232001, China)
出处
《煤炭技术》
CAS
2018年第5期49-52,共4页
Coal Technology
基金
国家自然科学基金项目(41301074)
关键词
冷端温度
含水率
水热迁移
冻胀率
temperature of freezing plate
water content
water-heat transference
frost heave ratio