Abstract

Microbially induced calcite precipitation (MICP) is an environmentally conscious ground-improvement method that can enhance the engineering properties of granular soils through the precipitation of calcium carbonate (CaCO3) on soil particle surfaces and contacts. Although numerous studies have shown the ability of biocementation to improve the liquefaction resistance of loose sands, the effects of light cementation levels on undrained cyclic behaviors have remained relatively unexplored. A series of undrained monotonic and cyclic direct simple shear tests were performed to examine the effect of light biocementation (ΔVs<100  m/s and CaCO3 contents <0.9%) on the liquefaction triggering and post-triggering behavior of loose Ottawa F-65 sand subjected to varying loading magnitudes [cyclic stress ratio (CSR)=0.1 to 0.3]. Results suggest that the presence of light biocementation can significantly improve the liquefaction triggering resistance of loose sands, with log-linear increases in the number of cycles required to trigger liquefaction, which consistently correlated with cementation-induced Vs increases. Despite these remarkable pretriggering improvements, almost no improvements were observed in post-triggering strain accumulation and postcyclic reconsolidation behaviors, with Vs measurements indicating that small-strain improvements were largely erased following shearing events.

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Data Availability Statement

All data generated during the study are available from the corresponding author upon reasonable request. All measured data presented in the figures of this paper will be available through the NSF DesignSafe-CI Data Depot repository (https://www.designsafe-ci.org/data/browser/public/) under Project No. PRJ-2912.

Acknowledgments

Support for this research provided by the University of Washington and the Engineering Research Center Program of the National Science Foundation under NSF Cooperative Agreement No. EEC-1449501 is greatly appreciated. Any opinions, findings, and conclusions or recommendations expressed in this manuscript are those of the authors and do not necessarily reflect the views of the National Science Foundation. Presented SEM images were made possible by the Molecular Analysis Facility, a National Nanotechnology Coordinated Infrastructure site at the University of Washington, which is supported in part by the National Science Foundation Grant NNCI-1542101, the University of Washington, the Molecular Engineering & Science Institute, and the Clean Energy Institute. The authors appreciate insightful discussions with Professor Jason T. DeJong, which greatly improved the study. Research assistance from Dr. Scott Braswell and Lucas Lindberg are acknowledged and appreciated.

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Journal of Geotechnical and Geoenvironmental Engineering
Volume 148Issue 1January 2022

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Received: Oct 21, 2020
Accepted: Aug 20, 2021
Published online: Oct 21, 2021
Published in print: Jan 1, 2022
Discussion open until: Mar 21, 2022

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Ph.D. Student, Dept. of Civil and Environmental Engineering, Univ. of Washington, Seattle, WA 98195. ORCID: https://orcid.org/0000-0002-7436-5374. Email: [email protected]
Assistant Professor, Dept. of Civil and Environmental Engineering, Univ. of Washington, Seattle, WA 98105 (corresponding author). ORCID: https://orcid.org/0000-0002-4464-5447. Email: [email protected]
Ph.D. Student, Dept. of Civil and Environmental Engineering, Univ. of California, Davis, CA 95616. ORCID: https://orcid.org/0000-0002-5675-1554. Email: [email protected]
Assistant Professor, Dept. of Civil and Environmental Engineering, Univ. of California, Davis, CA 95616. ORCID: https://orcid.org/0000-0001-5494-497X. Email: [email protected]

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