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加载过程中结构-冻土界面红外辐射温度场研究
引用本文:赵晓东,周国庆,别小勇.加载过程中结构-冻土界面红外辐射温度场研究[J].岩土力学,2010,31(6):1817-1821.
作者姓名:赵晓东  周国庆  别小勇
作者单位:1. 中国矿业大学,深部岩土力学与地下工程国家重点实验室,江苏,徐州,221008;中国矿业大学,建筑工程学院,江苏,徐州,221008
2. 无锡市政设计研究院,江苏,无锡,214011
基金项目:国家自然科学基金重点项目,国家科技支撑计划重点项目 
摘    要:为获取加载过程中结构-冻土界面温度场的时空分布规律,采用红外热辐射成像技术对模型桩-冻土界面上红外辐射温度场的产生、发展及其演变过程进行了试验研究。结果表明:模型桩在加载直至滑移过程中,桩-冻土界面处存在红外辐射温升现象;桩-冻土界面发生滑移前,红外热图上低温区域在密度和范围上均逐渐减小,距离冻土试样表面不同深度D处温升幅度?T和影响宽度W随时间而逐渐增加,但相同时刻?T和W随深度D的增加而减小;桩-冻土界面发生滑移后,红外热图上的高温区成带状分布,并趋于贯通,最大温升幅度?Tmax和温升影响的最大宽度Wmax随深度D的增加呈线性减小规律。研究结果可为红外热辐射成像技术应用于冻土地区结构-冻土界面温度场测试提供参考。

关 键 词:结构-冻土界面  红外辐射  温度场  分布规律
收稿时间:2008-10-15

Research on infrared radiation temperature field of fabric-frozen soil interface during loading process
ZHAO Xiao-dong,ZHOU Guo-qing,BIE Xiao-yong.Research on infrared radiation temperature field of fabric-frozen soil interface during loading process[J].Rock and Soil Mechanics,2010,31(6):1817-1821.
Authors:ZHAO Xiao-dong  ZHOU Guo-qing  BIE Xiao-yong
Institution:1. State Key Laboratory for Geomechanics and Deep Underground Engineering, China University of Mining and Technology, Xuzhou, Jiangsu 221008, China; 2. School of Architecture and Civil Engineering, China University of Mining and Technology, Xuzhou, Jiangsu 221008, China; 3. Wuxi Municipal Engineering Design Institute, Wuxi, Jiangsu 214011, China
Abstract:In order to reveal the loading temperature distribution law of fabric-frozen soil interface , the generation, development and evolution for temperature fields of model pile-frozen soil interface was investigated with infrared thermal radiation imaging technique. The results show that there exists infrared radiation temperature rising phenomenon in pile-frozen soil interface during loading process. Before the pile slides, the low temperature areas in the thermal maps decrease both in density and dimension; and the temperature rising amplitude ?T as well as influencing width W at different depths D increase along with time; while ?T and W of the same time both decrease as the depth increases. After the pile has slid, the high temperature areas present a zonal distribution and display a trend of transfixion; in addition, the maximum temperature rising ?Tmax and the maximum area width influenced Wmax present a linear decreasing trend as the depth increases. The research results will provide reference for the applying of infrared radiation technique to the interface temperature field’s test of fabric-frozen soil in frozen regions.
Keywords:interface of fabric-frozen soil  infrared radiation  temperature fields  distribution law
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