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    Durability Evolution Mechanism of MICP-Treated Calcareous Sand Exposed to Seawater Dry–Wet Cycles

    Source: Journal of Geotechnical and Geoenvironmental Engineering:;2025:;Volume ( 151 ):;issue: 008::page 04025081-1
    Author:
    Yao Xiao
    ,
    Huafeng Deng
    ,
    Wenxi Zhu
    ,
    Eleyas Assefa
    ,
    Lei Cheng
    ,
    Yu Xiong
    ,
    C. F. Lee
    DOI: 10.1061/JGGEFK.GTENG-13301
    Publisher: American Society of Civil Engineers
    Abstract: To 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.
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      Durability Evolution Mechanism of MICP-Treated Calcareous Sand Exposed to Seawater Dry–Wet Cycles

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4307438
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    • Journal of Geotechnical and Geoenvironmental Engineering

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    contributor authorYao Xiao
    contributor authorHuafeng Deng
    contributor authorWenxi Zhu
    contributor authorEleyas Assefa
    contributor authorLei Cheng
    contributor authorYu Xiong
    contributor authorC. F. Lee
    date accessioned2025-08-17T22:46:51Z
    date available2025-08-17T22:46:51Z
    date copyright8/1/2025 12:00:00 AM
    date issued2025
    identifier otherJGGEFK.GTENG-13301.pdf
    identifier urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4307438
    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.
    publisherAmerican Society of Civil Engineers
    titleDurability Evolution Mechanism of MICP-Treated Calcareous Sand Exposed to Seawater Dry–Wet Cycles
    typeJournal Article
    journal volume151
    journal issue8
    journal titleJournal of Geotechnical and Geoenvironmental Engineering
    identifier doi10.1061/JGGEFK.GTENG-13301
    journal fristpage04025081-1
    journal lastpage04025081-12
    page12
    treeJournal of Geotechnical and Geoenvironmental Engineering:;2025:;Volume ( 151 ):;issue: 008
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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