Phase transition properties and rheological model of soft clay in South China Sea in steady rheological tests

被引:0
作者
Liu Jie-feng [1 ]
Li Sa [1 ]
Duan Gui-juan [2 ]
Wang Yi-lin [1 ]
机构
[1] Tianjin Univ, Sch Civil Engn, Tianjin 300350, Peoples R China
[2] Huadong Engn Corp Ltd, Hangzhou 311100, Zhejiang, Peoples R China
基金
中国国家自然科学基金;
关键词
soft clay in South China Sea; phase transition; water content; temperature; rheological model; FINE; STRENGTH; MUDFLOWS; SOILS;
D O I
10.16285/j.rsm.2022.0170
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
Study on the phase transition properties and rheological model of submarine sediments during rheological testing is of great significance to the safety assessment for submarine structures. Using the soft clay in South China Sea, five group samples with different water contents were prepared, and a series of rheological tests under different temperature was carried out using the MCR302 rheometer. The results show that shear stress increases rapidly then increases slowly with increasing shear rate, while apparent viscosity decreases rapidly then decreases slowly. The shear stress and apparent viscosity decrease with increase in water content, and they increase with decrease in temperature. Phase transition happens in soft clay during shearing and can be divided into static and dynamic yield stresses, and the models for static and dynamic yield stresses were established on the basis of experimental results. In addition, Dual-Bingham rheological model considering effects of water content and temperature for soft clay from South China Sea was established, and the efficiency of model was verified. The results of this paper can provide basic model for the numerical analysis of submarine structure stability in South China Sea.
引用
收藏
页码:341 / 349
页数:9
相关论文
共 22 条
[1]  
Bingham E.G., 1922, FLUIDITY PLASTICITY
[2]   Strength of fine-grained soils at the solid-fluid transition [J].
Boukpeti, N. ;
White, D. J. ;
Randolph, M. F. ;
Low, H. E. .
GEOTECHNIQUE, 2012, 62 (03) :213-226
[3]   ON THE BEHAVIOR OF FINE MUD SUSPENSIONS [J].
COUSSOT, P ;
PIAU, JM .
RHEOLOGICA ACTA, 1994, 33 (03) :175-184
[4]  
Fan N, 2019, ROCK SOIL MECH, V40, P413, DOI 10.16285/j.rsm.2016.2916
[5]  
Fan N, 2018, ROCK SOIL MECH, V39, P3195, DOI 10.16285/j.rsm.2016.1227
[6]  
[郭兴森 Guo Xingsen], 2019, [岩土工程学报, Chinese Journal of Geotechnical Engineering], V41, P161
[7]  
HERSCHEL W H, 1926, P AM SOC TEST PROC
[8]   A laboratory study of rheological properties of mudflows in Hangzhou Bay, China [J].
Huang, Zhenhua ;
Aode, Huhe .
INTERNATIONAL JOURNAL OF SEDIMENT RESEARCH, 2009, 24 (04) :410-424
[9]   Rheological properties of fine-grained sediment: the roles of texture and mineralogy [J].
Jeong, Sueng Won ;
Locat, Jacques ;
Leroueil, Serge ;
Malet, Jean-Philippe .
CANADIAN GEOTECHNICAL JOURNAL, 2010, 47 (10) :1085-1100
[10]   Applicability of power law for describing the rheology of soils of different origins and characteristics [J].
Jeong, Sueng Won ;
Leroueil, Serge ;
Locat, Jacques .
CANADIAN GEOTECHNICAL JOURNAL, 2009, 46 (09) :1011-1023