On the Dilatancy of Fine-Grained Soils
Abstract
:1. Notation and Symbols
2. Introduction
- (i)
- at the beginning, , and the rate-dependent behaviour of a plastic clay achieves its maximum.
- (ii)
- After some cycles of constant stress amplitude, the mean effective pressure decreases while the void ratio and the preconsolidation pressure remain constant, i.e., the current OCR increases.
- (iii)
- For , the rate dependency of the clay decays sparsely and, depending on the subjected loading magnitude, the response of the material is contractant. This leads to a reduction in the effective mean stress p, resulting in a decay of the shear strength and of the barotropic stiffness.
- (iv)
- Towards higher , a significant reduction in the viscous effects is evident. We will show that, in this case, the phase transformation line (PTL) lies below the critical state line. Thus, besides contractancy, dilatant behaviour can also be observed when overpassing the PTL (similar to the behaviour of sands, widely reported in the literature [11,14,19,20]).
3. Dilatancy of Fine-Grained Soils Evaluated from Monotonic and Cyclic Triaxial Tests
3.1. Basic Postulates and Assumptions
3.2. Overconsolidation Ratio
3.3. Results for Kaolin
3.3.1. Triaxial Tests under Monotonic Loading
3.3.2. Triaxial Tests under Cyclic Loading
- In Figure 7a–d, all cycles are considered. A comparison between the figures on the left and those on the right (hence between the approaches proposed in Section 3.1) shows that the main difference is noticed at loading reversals in triaxial extension. These discrepancies are particularly noticeable when comparing Figure 7a with Figure 7d or Figure 7c with Figure 7d. Thereby, the evaluation accounting for isotropic hypoelasticity leads to dilatancy at the stress reversal points (from loading in triaxial compression to loading in triaxial extension). On the other hand, the use of transversal isotropic hypoelasticity leads to increased contractancy at stress reversals from loading in triaxial compression to loading in triaxial extension. The latter observations are in accordance with studies conducted on sand, e.g., [4], even though some data scatter can be observed in these figures. At this point, one should be aware that no data points have been omitted during these evaluations.
- On the other hand, only regular (not initial) cycles have been considered in Figure 7e,f. Hereby, the data scatter is almost absent and the aforementioned trends are even more pronounced. Hence, a correct description of the elasticity is essential for the evaluation of the dilatancy curves. Of course, as soon as a hyperelastic potential is evaluated experimentally and described mathematically for Kaolin, it makes sense to validate these evaluations again. At the moment, it may be concluded that the transversal isotropic hypoelasticity corresponds better than the isotropic hypoelasticity to the behaviour of Kaolin.
- This evaluation scheme can furthermore be verified by conducting tests with (e.g., in hollow cylinder apparatus). Thereby, intermediate small loops of unloading–reloading elastic cycles are also necessary to evaluate the portion of and should be the target of further research. Note that, in this work, instead of was used. As claimed in some works [4,9,52], the use of would reduce the scattering in the dilatancy vs. stress ratio relations for sand.
- As stated also in [40], the “elastic dilatancy” after reversals is evident, for example, in Figure 7c. Using the transversal isotropic hypoelasticity, it is eliminated, as depicted in Figure 7d. This elasticity provokes an increase in the effective mean stress, resulting in a slope to the upper left of the effective stress path [17,18,40]. It is well known that clays possess a greater elastic locus compared to sands. If the elasticity was isotropic, then the described path would be vertical with respect to the axis. Thus, we can consider the inherent anisotropy to be responsible for an even lower reduction in effective pressure after loading reversal. For sands, in contrast, after a loading reversal, the largest contractancy has been observed. Hence, the greater elastic regime of fine-grained soils cannot be overcome through the contractancy and it results in a non-vanishing mean effective pressure at cyclic mobility .This effect may be explained by the inherent anisotropy caused by specific sedimentation along a given axis. Thus, the question arises as to whether a cutting direction of the sample may be found at which the soft soil would also liquify (weak axis). This requires further research. Some authors [25,28,36] explain the non-liquefaction behaviour of clays in terms of the viscosity and its cohesive effect. Supposing this to be true, then the intensity of creep would not vanish with a higher overconsolidation ratio, as has been experimentally documented in [21,53]. On the other hand, this implies the existence of a special strain rate (loading velocity) with which the cyclic undrained shearing of a clay sample would result in liquefaction. Following our theory, this would be the case for the greatest velocity ; hence, the viscous effects would not have time to develop. The experiments presented in [17] and the discussions made in [40] hint at this phenomenon. However, further research work is required in order to shed more light and explain this phenomenon.
3.4. Results for Lower Rhine Clay
4. Constitutive Description of the State-Dependent Dilatancy for Cohesive Soils
4.1. Generalisation to Multiaxial Space
4.2. Dilatancy Rule
4.3. Incorporation of Dilatancy into a General Hypoplastic Model
4.4. Simulations with Experiments
5. Conclusions
Author Contributions
Funding
Institutional Review Board Statement
Informed Consent Statement
Data Availability Statement
Acknowledgments
Conflicts of Interest
Nomenclature
plasticity index | |
mean effective stress | |
q | deviatoric (effective) stress |
isometric effective stress invariants | |
stress ratio | |
stress ratio at the critical state | |
M | slope of the critical state line |
d | dilatancy |
stress ratio at the phase transformation line | |
(initial) overconsolidation ratio | |
total strain rate | |
elastic strain rate | |
plastic strain rate | |
volumetric strain rate | |
deviatoric strain | |
𝗘 | stiffness tensor |
components of the stiffness tensor | |
e | void ratio |
shear strain increment | |
time increment | |
N | number of cycles |
𝗤 | rotation tensor |
normal vector | |
anisotropic coefficient | |
auxiliary variables | |
compression index | |
swelling index | |
deviatoric stress amplitude | |
friction angle | |
dilatancy angle | |
flow rule | |
Y | degree of nonlinearity |
Appendix A. Approximation of the Mean Effective Pressure with Time t
Appendix B. Transversal Isotropic Hypoelasticity
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Material | |||||
---|---|---|---|---|---|
[-] | [-] | [-] | [-] | [-] | |
Kaolin | 1 *,1.8 * | ||||
Lower Rhine Clay |
Material | ||||||||||
---|---|---|---|---|---|---|---|---|---|---|
Kaolin | 0.3 | 1.8 | 0.13 | 0.05 | 1.76 | 1.0 | 0.3 | 6 | 2 | 0.8 |
LRC | 0.2 | 1.0 | 0.26 | 0.04 | 2.47 | 0.95 | 0.5 | 6 | 2 | 0.5 |
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Tafili, M.; Grandas Tavera, C.; Triantafyllidis, T.; Wichtmann, T. On the Dilatancy of Fine-Grained Soils. Geotechnics 2021, 1, 192-215. https://doi.org/10.3390/geotechnics1010010
Tafili M, Grandas Tavera C, Triantafyllidis T, Wichtmann T. On the Dilatancy of Fine-Grained Soils. Geotechnics. 2021; 1(1):192-215. https://doi.org/10.3390/geotechnics1010010
Chicago/Turabian StyleTafili, Merita, Carlos Grandas Tavera, Theodoros Triantafyllidis, and Torsten Wichtmann. 2021. "On the Dilatancy of Fine-Grained Soils" Geotechnics 1, no. 1: 192-215. https://doi.org/10.3390/geotechnics1010010
APA StyleTafili, M., Grandas Tavera, C., Triantafyllidis, T., & Wichtmann, T. (2021). On the Dilatancy of Fine-Grained Soils. Geotechnics, 1(1), 192-215. https://doi.org/10.3390/geotechnics1010010