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    Pore–Water Salinity Effect on the Compression and Hydraulic Characteristics of Saturated Saline Soils

    Source: International Journal of Geomechanics:;2025:;Volume ( 025 ):;issue: 001::page 04024326-1
    Author:
    Huayang Lei
    ,
    Weidi Zhang
    ,
    Lei Wang
    ,
    Yu Bo
    ,
    Chirun Zhan
    DOI: 10.1061/IJGNAI.GMENG-10136
    Publisher: American Society of Civil Engineers
    Abstract: Changes in the pore-water environment have an obvious effect on the physical and mechanical properties of soil. Traditional consolidation theory has not considered the influence of the hydrochemical environment on the mechanical properties of soil. In order to investigate the mechanism of chemical action on geotechnical properties, in this study, one-dimensional compression tests and scanning electron microscope tests are carried out on soils prepared with different concentrations of NaCl solution. The mechanical characteristics reveal that the compression index shows a gradual decrease with an increase in pore-water salinity, and the structural yield stress of the soil increases gradually with the increase in pore-water salinity, reaching a maximum value of 50.34 kPa with a salt content of 5%. Conversely, the change in osmotic suction has minimal impact on the rebound index. Notably, the pore-water salinity primarily affects the intrinsic compression behavior of soft clays, as evidenced by an increase in the slopes of the sedimentary compression curve before yielding higher pore-water salinity. Combined with the analysis of microscopic test results, it is found that as the osmotic suction increases and the interparticle hydration capacity decreases, the soil particles change from a dispersed state to an aggregate state, leading to an increase in mesopores, and this increase indicates that the ability of the soils to resist the external loads also increases, which means an enhancement of the structural characteristic. In addition, the coefficient of permeability of the soil decreases as the consolidation pressure increases. Chemical consolidation produced by the increase in pore salt solution concentration causes a decrease in pore ratio, resulting in a smaller coefficient of permeability, and there exists a critical value for the effect of salt on the coefficient of permeability of the soil, which is related to the structural yield stress of the soil. This research provides a theoretical basis for the settlement prediction and the safety evaluation of soft ground in coastal areas.
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      Pore–Water Salinity Effect on the Compression and Hydraulic Characteristics of Saturated Saline Soils

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4303728
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    • International Journal of Geomechanics

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    contributor authorHuayang Lei
    contributor authorWeidi Zhang
    contributor authorLei Wang
    contributor authorYu Bo
    contributor authorChirun Zhan
    date accessioned2025-04-20T09:57:27Z
    date available2025-04-20T09:57:27Z
    date copyright11/18/2024 12:00:00 AM
    date issued2025
    identifier otherIJGNAI.GMENG-10136.pdf
    identifier urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4303728
    description abstractChanges in the pore-water environment have an obvious effect on the physical and mechanical properties of soil. Traditional consolidation theory has not considered the influence of the hydrochemical environment on the mechanical properties of soil. In order to investigate the mechanism of chemical action on geotechnical properties, in this study, one-dimensional compression tests and scanning electron microscope tests are carried out on soils prepared with different concentrations of NaCl solution. The mechanical characteristics reveal that the compression index shows a gradual decrease with an increase in pore-water salinity, and the structural yield stress of the soil increases gradually with the increase in pore-water salinity, reaching a maximum value of 50.34 kPa with a salt content of 5%. Conversely, the change in osmotic suction has minimal impact on the rebound index. Notably, the pore-water salinity primarily affects the intrinsic compression behavior of soft clays, as evidenced by an increase in the slopes of the sedimentary compression curve before yielding higher pore-water salinity. Combined with the analysis of microscopic test results, it is found that as the osmotic suction increases and the interparticle hydration capacity decreases, the soil particles change from a dispersed state to an aggregate state, leading to an increase in mesopores, and this increase indicates that the ability of the soils to resist the external loads also increases, which means an enhancement of the structural characteristic. In addition, the coefficient of permeability of the soil decreases as the consolidation pressure increases. Chemical consolidation produced by the increase in pore salt solution concentration causes a decrease in pore ratio, resulting in a smaller coefficient of permeability, and there exists a critical value for the effect of salt on the coefficient of permeability of the soil, which is related to the structural yield stress of the soil. This research provides a theoretical basis for the settlement prediction and the safety evaluation of soft ground in coastal areas.
    publisherAmerican Society of Civil Engineers
    titlePore–Water Salinity Effect on the Compression and Hydraulic Characteristics of Saturated Saline Soils
    typeJournal Article
    journal volume25
    journal issue1
    journal titleInternational Journal of Geomechanics
    identifier doi10.1061/IJGNAI.GMENG-10136
    journal fristpage04024326-1
    journal lastpage04024326-9
    page9
    treeInternational Journal of Geomechanics:;2025:;Volume ( 025 ):;issue: 001
    contenttypeFulltext
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