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1.昆明理工大学 建筑工程学院,昆明 650500
2.西昌学院 土木与水利工程学院,四川 西昌 615000
OU Mingxi (1983-), PhD, associate professor, main research interests: special rock and soil mechanics, E-mail: 19590927@163.com.
Received:09 January 2024,
Published:25 April 2026
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欧明喜,李强,韩忠玉.泥炭土静止侧压力系数影响因素试验研究[J].土木与环境工程学报,2026,48(02):90-99.
OU Mingxi,LI Qiang,HAN Zhongyu.Experimental study on influencing factors of the coefficient of earth pressure at rest of peat soil[J].Journal of Civil and Environmental Engineering,2026,48(02):90-99.
欧明喜,李强,韩忠玉.泥炭土静止侧压力系数影响因素试验研究[J].土木与环境工程学报,2026,48(02):90-99. DOI: 10.11835/j.issn.2096-6717.2024.040.
OU Mingxi,LI Qiang,HAN Zhongyu.Experimental study on influencing factors of the coefficient of earth pressure at rest of peat soil[J].Journal of Civil and Environmental Engineering,2026,48(02):90-99. DOI: 10.11835/j.issn.2096-6717.2024.040.
静止侧压力系数
K
0
是解决岩土类工程问题的重要参数。为研究泥炭土
K
0
的影响因素和作用机理,采用
K
0
固结仪对昆明滇池泥炭土开展侧限压缩试验,系统分析了竖向应力、有机质含量和初始孔隙比对
K
0
的影响规律,并从结构性角度探讨
K
0
变化规律的形成机理。结果表明:重塑泥炭土的静止侧压力系数不是恒定常数,而是与竖向应力和有机质含量有关;加载时
K
0
随竖向应力的增加而减小,最后趋于稳定,且在较低竖向应力下
K
0
的减小趋势更显著;同一竖向应力下,有机质含量越大,
K
0
越小,整个加载过程
K
0
下降幅度越大;泥炭土结构性在加载过程中的动态变化是引起
K
0
变化的根本原因,竖向应力和有机质通过影响其结构性进而影响
K
0
,且两者间存在一定的耦合关系;重塑泥炭土稳定后
K
0
值在0.42~0.6之间,低于无机黏土,并与有机质含量存在线性负相关,基于试验结果提出了相应的拟合关系式;初始孔隙比与
K
0
值的关系较为离散。
The coefficient of earth pressure at rest
K
0
is an important parameter for geotechnical engineering. In order to study the influencing factors and mechanisms of peat soil
K
0
a
K
0
consolidation instrument was used to conduct a lateral compression test on Kunming Dianchi peat soil. The effects of vertical stress
organic matter content and initial void ratio on
K
0
were systematically analyzed
and from the structural perspective
the formation mechanism of its
K
0
change law was explored. The test results show that the coefficient of earth pressure at rest of reshaped peat soil is not a constant
but is related to the vertical stress and content of organic matter;
K
0
decreases with the increase of vertical stress during loading and finally tends to be stable. The decreasing trend of
K
0
under stress is more significant; under the same vertical stress
the greater the organic matter content of the soil sample
the smaller
K
0
and the greater the decrease in
K
0
during the entire loading process; the dynamic changes in the structural properties of peat soil during the loading process are the fundamental cause of changes in
K
0
. Vertical stress and organic matter affect
K
0
by affecting its structural properties
and there is a certain coupling relationship between the two; the
K
0
value after stabilization of reshaped peat soil is between 0.42 and 0.6
which is lower than that of inorganic clay
and has a linear negative correlation with the organic matter content. Based on the experimental results
a corresponding fitting relationship is proposed; the relationship between the initial void ratio and the
K
0
value is relatively discrete.
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