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    Chemically Induced Water Repellency and the Freeze–Thaw Durability of Soils

    Source: Journal of Cold Regions Engineering:;2020:;Volume ( 034 ):;issue: 003
    Author:
    Masrur Mahedi
    ,
    Sajjad Satvati
    ,
    Bora Cetin
    ,
    John L. Daniels
    DOI: 10.1061/(ASCE)CR.1943-5495.0000223
    Publisher: ASCE
    Abstract: Organosilane (OS) is a silicon-based coupling agent capable of producing hydrophobicity in soils. This study evaluated the applicability of OS in reducing the freeze–thaw impacts on subgrade soils. A frost-susceptible soil was treated with two different dosages (50% and 100% by weight) of 10% OS solution. The OS-treated soils were dried and incorporated into natural soil as layers of 2.5 and 5 cm thickness. The freeze–thaw performances of natural and OS-incorporated soils were then evaluated in terms of maximum frost heave, heave rate, soil moisture distribution, and temperature profile. The OS-treated soil layers decreased frost heaving by 48%–74%. The heave rate of untreated soil was 13.8 cm/day, which was decreased to 4 mm/day with an incorporation of 5 cm-thick layer of 50% OS-treated soil. A 5 cm–50% OS-treated layer was found to be more efficient compared to a 5 cm–100% OS-treated layer in improving the freeze–thaw performance of the soils.
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      Chemically Induced Water Repellency and the Freeze–Thaw Durability of Soils

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4268408
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    contributor authorMasrur Mahedi
    contributor authorSajjad Satvati
    contributor authorBora Cetin
    contributor authorJohn L. Daniels
    date accessioned2022-01-30T21:33:01Z
    date available2022-01-30T21:33:01Z
    date issued9/1/2020 12:00:00 AM
    identifier other%28ASCE%29CR.1943-5495.0000223.pdf
    identifier urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4268408
    description abstractOrganosilane (OS) is a silicon-based coupling agent capable of producing hydrophobicity in soils. This study evaluated the applicability of OS in reducing the freeze–thaw impacts on subgrade soils. A frost-susceptible soil was treated with two different dosages (50% and 100% by weight) of 10% OS solution. The OS-treated soils were dried and incorporated into natural soil as layers of 2.5 and 5 cm thickness. The freeze–thaw performances of natural and OS-incorporated soils were then evaluated in terms of maximum frost heave, heave rate, soil moisture distribution, and temperature profile. The OS-treated soil layers decreased frost heaving by 48%–74%. The heave rate of untreated soil was 13.8 cm/day, which was decreased to 4 mm/day with an incorporation of 5 cm-thick layer of 50% OS-treated soil. A 5 cm–50% OS-treated layer was found to be more efficient compared to a 5 cm–100% OS-treated layer in improving the freeze–thaw performance of the soils.
    publisherASCE
    titleChemically Induced Water Repellency and the Freeze–Thaw Durability of Soils
    typeJournal Paper
    journal volume34
    journal issue3
    journal titleJournal of Cold Regions Engineering
    identifier doi10.1061/(ASCE)CR.1943-5495.0000223
    page7
    treeJournal of Cold Regions Engineering:;2020:;Volume ( 034 ):;issue: 003
    contenttypeFulltext
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