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dc.contributor.authorYao Xiao
dc.contributor.authorHuafeng Deng
dc.contributor.authorWenxi Zhu
dc.contributor.authorEleyas Assefa
dc.contributor.authorLei Cheng
dc.contributor.authorYu Xiong
dc.contributor.authorC. F. Lee
dc.date.accessioned2025-08-17T22:46:51Z
dc.date.available2025-08-17T22:46:51Z
dc.date.copyright8/1/2025 12:00:00 AM
dc.date.issued2025
dc.identifier.otherJGGEFK.GTENG-13301.pdf
dc.identifier.urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4307438
dc.description.abstractTo investigate the long-term performance evolution of microbial-induced carbonate precipitation (MICP) technology for treating calcareous sand, a 150 day dry–wet (DW) cycle test was conducted considering the actual occurrence of calcareous sand in a seawater environment. Based on the changes in physical and mechanical properties and microstructure of MICP-treated calcareous sand samples under different DW cycles, the macro- and microcharacteristics and evolution mechanism were analyzed. Under the action of the seawater DW cycle, the permeability coefficient and porosity of calcareous sand sample first decrease, then increase, and gradually stabilize. Compared with the initial state without DW cycles, the permeability coefficient increased by 54.85%, and the porosity of the sample increased from 8.90% to 11.41%. The unconfined compressive strength and initial tangent modulus of the samples exhibited a trend of first increasing, then decreasing, and finally stabilizing. The main failure mode was tensile shear failure. As the number of DW cycles increased, the shear failure phenomenon of longitudinal tensile cracks in the samples gradually decreased, indicating that their brittleness gradually weakened and ductility gradually increased. During the seawater DW cycle process, on the one hand, the infiltration and seepage of seawater led to the dissolution and detachment of cementitious materials, and the cemented characteristics between calcareous sand particles gradually became less dense and looser, and the contact mode between particles gradually changed from surface contact to point contact. The increase, expansion, and connectivity of interparticle pores as well as the increase of seawater infiltration channels resulted in frequent changes in the stress state at the contact points due to the alternating DW cycles. As a result, the pores inside the samples gradually became more interconnected, leading to a decrease in their physical and mechanical properties. The relevant research ideas and results can provide valuable reference for the long-term performance evaluation of MICP technology.
dc.publisherAmerican Society of Civil Engineers
dc.titleDurability Evolution Mechanism of MICP-Treated Calcareous Sand Exposed to Seawater Dry–Wet Cycles
dc.typeJournal Article
dc.journal.volume151
dc.journal.issue8
dc.journal.titleJournal of Geotechnical and Geoenvironmental Engineering
dc.identifier.doi10.1061/JGGEFK.GTENG-13301
dc.journal.fristpage04025081-1
dc.journal.lastpage04025081-12
dc.page12
dc.treeJournal of Geotechnical and Geoenvironmental Engineering:;2025:;Volume ( 151 ):;issue: 008
dc.contenttypeFulltext


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