The inherent particulate nature of granular soils, such as sands and gravels, plays an important role in their engineering behavior. This dissertation aims to advance the fundamental understanding of the effect of fabric- and stress-induced anisotropy, and gradation on the micro- and macro-scale behavior of coarse-grained granular soils.The first portion of this dissertation addresses the direction-dependent characteristics exhibited by soils reflected in the anisotropy of their responses. Studies have shown that both the depositional processes and particle arrangements (i.e., fabric-induced anisotropy), and the stress state and history (i.e., stress-induced anisotropy) impact the anisotropic behaviors observed at the macroscopic level. Quantifying these anisotropies has been challenging, necessitating specialized geotechnical testing and imaging equipment. To overcome these challenges, a novel experimental testing setup is introduced, designed to measure shear wave velocities (VS) along different orientations and polarization planes using piezoelectric bender elements (BEs) to obtain angular distributions of VS. Subsequently, two investigations on shear wave propagation are presented, using the developed setup and Discrete Element Method (DEM) simulations, to explore the effects of fabric- and stress-induced anisotropy on the VS anisotropy. The experimental tests were performed on glass beads and angular natural sands, while the DEM simulations used spherical and rod-like clumped particles. These specimens were subjected to isotropic and one-dimensional (1D) compression. The results reveal that the angular distributions of VS and measurements obtained along different polarization planes (i.e. VS,HH, VS,HV, and VS,VH) can discern the effects of fabric and stress anisotropy. The observed trends indicate a relationship between the angular distributions of VS and of the alignment of particles and interparticle contact forces. A framework is presented based on the VS measurements along various orientations and polarization planes which is validated using the presented results. When presented in terms of the ratio of VS measurements along different orientations and polarization planes, namely the VS,HV/VS,VH and VS,HV/VS,HH ratios, and of the newly introduced Anisotropy parameter (Ae), this framework facilitates the evaluation of the stress- and fabric-induced anisotropy in soil specimens. The results also highlight the challenges in discerning the effects of stress and fabric anisotropy when both simultaneously influence the soil response.
Geosystems built on coarse-grained soils with broader gradations are typically designed and analyzed using methodologies developed for poorly-graded soils without explicit consideration of the effects of gradation, potentially leading to uncertainty in performance predictions. In the second portion of this dissertation, the effects of changes in the gradation on various aspects of monotonic and cyclic response of coarse-grained soil behavior are investigated using DEM simulations. The simulations include monotonic isotropically-consolidated drained and undrained triaxial tests, and cyclic undrained direct simple shear tests conducted on specimens with coefficients of uniformity (CU) between 1.9 and 6.4 composed of non-spherical particles. The triaxial simulation results indicate that an increase in CU leads to increases in peak shear strength, dilative volume change, rate of dilation, negative pore pressure generation, and rate of pore pressure generation. These findings are compared with established frameworks to highlight the differences in response resulting from variations in CU.
Particle-level measurements from the monotonic simulations highlight the influence of gradation on both the packing characteristics and the transmission of contact forces within the soil assembly. In particular, for the broadly graded specimens, the coarsest particles exhibit a disproportionately higher number of connections and carry significantly greater contact forces compared to the coarsest particles in poorly graded soils. The coarsest particles for the broadly graded specimen are connected to a disproportionally higher number of particles and carry disproportionally higher contact forces as compared to coarsest particles in poorly graded soils. The enhanced interlocking of the coarser particles results in greater dilation during shearing, leads to higher peak shear strengths for the more broadly graded specimens. Additionally, the particles smaller than D10 are inactive in contact force transmission, while the percentage of particles active in contact force transmission increases with an increasing CU.
During cyclic shearing, specimens with broader gradations yield lower liquefaction-triggering resistance than poorly graded specimens at similar relative densities. Conversely, the opposite trends emerge when compared at similar initial state parameters. Post-liquefaction, specimens with broader gradation accumulate shear strains at a smaller rate. A comparison is presented, examining the interpretation of grading-dependent behavior by choosing relative density or initial state parameters as the state definition for both monotonic and cyclic response, highlighting the efficacy of initial state parameter in capturing the systematic differences in the response because of changes in gradation. The improved interlocking in more broadly graded specimens results in a lower percentage of sliding contacts for both strong and weak force-carrying contacts at the initiation of liquefaction and in subsequent cycles, which is linked to the slower rate of post-liquefaction strain accumulation in well-graded specimens.
The combination of macro and micro observations, from the research efforts presented in this dissertation, highlight the influence of fabric- and stress-induced anisotropy and gradation on soil behavior through a combination of novel experimental testing and DEM simulations, and contribute to the advancements in the geotechnical site characterization, design methodologies, numerical simulation techniques, and constitutive modeling of granular soils.