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滇池湖相沉积泥炭土参数测定与剪切特性研究
引用本文:阮永芬,蔡斯,李荣玉,程芸,乔文件,蔡龙. 滇池湖相沉积泥炭土参数测定与剪切特性研究[J]. 地震工程学报, 2024, 0(2): 259-268
作者姓名:阮永芬  蔡斯  李荣玉  程芸  乔文件  蔡龙
作者单位:昆明理工大学建筑工程学院, 云南 昆明 650500;云南邦众岩土工程有限公司, 云南 昆明 650500;云南建投第一勘察设计有限公司, 云南 昆明 650031;中铁二十局集团第五工程有限公司, 云南 昆明 650000
基金项目:国家自然科学基金重点项目(41931294)
摘    要:有机质含量和含水率对泥炭及泥炭质土(简称泥炭土)的力学性质及工程特性影响都很大,但现有的规范、规程及标准对高有机质含量土的含水率(ω)及有机质含量(wu)测定标准不明确,各单位测试结果差异较大。为明确高有机质含量土的ωwu测定标准,开展不同灼烧温度及灼烧时间下的测试试验。滇池湖相沉积土的场地一般都有3~5层层状分布的泥炭土,现对不同埋深的5层泥炭土进行从低至高围压下的三轴固结不排水(CU)试验,探究不同埋深及围压下其应力-应变的变化规律及演化机理。试验发现:泥炭土随围压增大应力-应变关系曲线呈现“分层”现象,最大偏应力对应的应变随深度增加而减小,线型随围压和土样埋深而发生改变,孔隙压力系数总体随着深度的增加而减小,并提出CU试验泥炭土破坏应变控制标准。以上研究进一步加深了对泥炭土力学特性的认识,也为明确ωwu的测定标准提供了试验依据。

关 键 词:泥炭及泥炭质土(简称泥炭土); 含水率; 有机质含量; 剪切特性
收稿时间:2021-12-25

Parameter determination and shear characteristics of lacustrine sedimentary peat soil in Dianchi Lake
RUAN Yongfen,CAI Si,LI Rongyu,CHENG Yun,QIAO Wenjian,CAI Long. Parameter determination and shear characteristics of lacustrine sedimentary peat soil in Dianchi Lake[J]. China Earthguake Engineering Journal, 2024, 0(2): 259-268
Authors:RUAN Yongfen  CAI Si  LI Rongyu  CHENG Yun  QIAO Wenjian  CAI Long
Affiliation:Faculty of Civil Engineering and Mechanics, Kunming University of Science and Technology, Kunming 650500 , Yunnan, China;Yunnan Bangzhong Geotechnical Engineering Co., Ltd., Kunming 650500 , Yunnan, China;Yunnan No.1 Engineering Survey and Design Co., Ltd., Kunming 650031 , Yunnan, China;No.5 Engineering Co., Ltd., China Railway 20th Bureau Group, Kunming 650000 , Yunnan, China
Abstract:Organic matter content (wu) and water content (ω) greatly influence the mechanical properties and engineering characteristics of peat and peaty soil (peat soil for short). However, the determination standards of ω and wu of soil with high organic matter content are unclear in existing codes, procedures, and standards, and the test results vary greatly among different units. To define the determination standards of ω and wu of high organic content soil, tests were performed under different burning temperatures and burning times. Generally, the site of lacustrine sedimentary soil in Dianchi Lake has 3-5 layers of peat soil. To explore the variation law and evolution mechanism of stress and strain under different buried depths and confining pressures, a series of triaxial consolidation undrained (CU) tests was performed on five layers of peat soil with different buried depths under low to high confining pressures. The test results show that the stress-strain curve of peat soil presents a “layered” phenomenon with increasing confining pressure; the strain corresponding to the maximum deviatoric stress decreases with increasing depth, and the curve shape changes with the confining pressure and buried depth of soil samples; the pore pressure coefficient decreases with increasing depth. Moreover, the control standard of failure strain of peat soil in the CU test is proposed. This research further deepens the understanding of the mechanical properties of peat soil and provides an experimental basis for determining ω and wu standards.
Keywords:peat and peaty soil (peat soil for short); water content; organic matter content; shear characteristics
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