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地基土冻胀的宏观分析
引用本文:刘鸿绪,朱广祥,尹冬岭,江守恒.地基土冻胀的宏观分析[J].冰川冻土,2003,25(3):347-350.
作者姓名:刘鸿绪  朱广祥  尹冬岭  江守恒
作者单位:黑龙江省, 寒地建筑科学研究院, 黑龙江, 哈尔滨, 150080
摘    要:通过野外原位观测发现,在北半球自然气温条件下,地表裸露、原状均质、冻胀性地基土的冻结过程中,冻结速率越大越有利于土的冻胀,即冻结速率与冻胀速率呈单值升函数规律.

关 键 词:温度梯度  冻结速率  冻胀速率  冻胀率  单值升函数  
文章编号:1000-0240(2003)03-0347-04
收稿时间:2002-09-10
修稿时间:2002年9月10日

Macrograph Analysis about Subsoil Frost Heaving
LIU Hong-xu,\ ZHU Guang-xiang,\ YIN Dong-ling,\ JIANG Shou-heng.Macrograph Analysis about Subsoil Frost Heaving[J].Journal of Glaciology and Geocryology,2003,25(3):347-350.
Authors:LIU Hong-xu  \ ZHU Guang-xiang  \ YIN Dong-ling  \ JIANG Shou-heng
Institution:Heilongjiang Cold Region Construction Science Research Institute, Harbin Heilongjiang 150080, China
Abstract:At present time, most savants consider that small freezing rate was advantageous to frost heaving. Through in situ observation, it was found that great freezing rate was more advantageous to frost heaving under natural air temperature of north hemisphere for exposed homogeneous subsoil, which is able to heave, i.e., frost-heaving rate increases with freezing rate.
Keywords:temperature gradient  freezing rate  frost-heaving rate  frost heaving ratio
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