ABSTRACT This study investigates linkages between volume change, pore fluid drainage, shear wave velocity, and temperature of soft clays using a thermal triaxial cell equipped with bender elements, a measurement approach that has not been explored widely in past thermo-mechanical studies. Two kaolinite specimens were consolidated mechanically to a normally consolidated state and then subjected to drained and undrained heating-cooling cycles, respectively. After cooling, the specimens were subjected to further mechanical consolidation to evaluate changes in apparent preconsolidation stress. Both specimens showed net contractive thermal strains after a heating-cooling cycle and overconsolidated behavior during mechanical compression immediately after cooling. The shear wave velocity increased during drained heating, but negligible changes were observed during drained cooling, indicating permanent hardening because of thermal consolidation during the heating-cooling cycle. The shear wave velocity decreased during undrained heating because of a reduction in effective stress associated with thermal pressurization of the pore fluid but subsequently increased when drainage was permitted at elevated temperature. The shear wave velocity increased slightly during undrained cooling but decreased when drainage was permitted at room temperature. Net increases in small-strain shear modulus of 17 and 11 % after heating-cooling cycles under drained and undrained (with drainage after reaching stable temperatures) conditions, respectively, provide further evidence to the potential of thermal soil improvement of normally consolidated clays. Transient changes in shear modulus also highlight the importance of considering drainage conditions and corresponding changes in effective stress state during heating-cooling cycles.
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Rigidity index of soft remolded clays during thixotropic hardening
This paper presents results from an experimental program that measured the thixotropic behavior of several remolded soft clays with varying plasticity. Measurements were conducted at various curing times ranging from 1.0 hour to 64 days. The undrained shear strength s/sub u/ was measured using the fall cone while companion specimens were also prepared and mounted in a bender element jig for measurement of temporal changes in shear wave velocity V/sub vh/. The bender element specimens allowed for much greater frequency of repeated data collection since the measurement was nondestructive and only one specimen was needed per clay for the full curing period. Furthermore, the combination of measurements provided data at each curing period for the rigidity index I/sub R/ taken as the ratio of the small-strain shear modulus G/sub max/ to s/sub u/. Values of s/sub u/ and V/sub vh/ increased significantly with time for all the clays, especially at a higher rate for the first 2 to 4 days. The full time-series dataset of each clay enabled the evolution of I/sub R/ during thixotropic hardening, which was found to be nearly constant over time for each of the studied clays. These data shed light on analyzing the behavior of offshore infrastructure and in situ tools that remold soft clays during installation such as pipelines, embedment anchors, and full-flow penetrometers.
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- Award ID(s):
- 1640306
- PAR ID:
- 10207881
- Date Published:
- Journal Name:
- 4th International Symposium on Frontiers in Offshore Geotechnics
- Format(s):
- Medium: X
- Sponsoring Org:
- National Science Foundation
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