A one-dimensional viscoelastic and viscoplastic constitutive approach to modeling the delayed behavior of clay and organic soils

被引:14
作者
Madaschi, Aldo [1 ,2 ]
Gajo, Alessandro [1 ]
机构
[1] Univ Trento, Dept Civil Environm & Mech Engn, I-38123 Trento, Italy
[2] Ecole Polytech Fed Lausanne, Ecole Polytech Fed Lausanne, LMS,Sch Architecture Civil & Environm Engn, Lab Soil Mech,ENAC, GC Stn 18, CH-1015 Lausanne, Switzerland
关键词
Organic soils; Primary consolidation; Secondary compression; Softclays; Viscoelasticity; Viscoplasticity; C-ALPHA/CC CONCEPT; SECONDARY COMPRESSION; STRAIN-RATE; PEAT; CONSOLIDATION; PLASTICITY;
D O I
10.1007/s11440-016-0518-9
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
Accurate modeling of the time-dependent behavior of geomaterials is of great importance in a number of engineering structures interacting with soft, highly compressible clay layers or with organic clays and peats. In this work, a uniaxial constitutive model, based on Perzyna's overstress theory and directly extendible to multiaxial stress conditions, is formulated and validated. The proposed constitutive approach essentially has three innovative aspects. The first concerns the implementation of two viscoplastic mechanisms within Perzyna's theory in order to distinguish between short-term (quasi-instantaneous) and long-term plastic responses. Similarly, elastic response is simulated by combining an instantaneous and a long-term viscous deformation mechanism. The second innovative aspect concerns the use of a bespoke logarithmic law for viscous effects, which has never been used before to simulate delayed soil behavior (as far as the authors are aware). The third concerns the model's extensive validation by simulating a number of different laboratory test results, including conventional and unconventional oedometer tests with small and large load increments/decrements and wide and narrow loading/unloading cycles, constant rates of stress and strain tests, and oedometer tests performed in a Rowe consolidation cell with measurement of pore pressure dissipation.
引用
收藏
页码:827 / 847
页数:21
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