РЕЖИМ РАЗРУШЕНИЯ ЛЬДОСОДЕРЖАЩЕГО СКЛОНА ПРИ ЦИКЛАХ ЗАМОРАЖИВАНИЯ-ОТТАИВАНИЯ Study on hydro-thermal changes during freeze-thaw cycles of ice-riched debris deposits

Mengfei Qu, Huan Yu, Qijun Hu, Enxi Qiu, Xusheng Wan

Аннотация


Для изучения характера разрушения льдосодержащих склонов под влиянием циклов замораживания-оттаивания были проведены модельные испытания в холодильной камере при различном содержании льда (12%, 16% и 20%) и количестве циклов замораживания–оттаивания. Результаты показали, что с ростом содержания льда на склоне формируется “нулевая завеса”, увеличение числа циклов замораживания–оттаивания делает температуру склона более чувствительной к изменениям температуры окружающей среды, а глубина оттаивания и промерзания грунта увеличивается. Под влиянием циклов замораживания–оттаивания в горизонтальном направлении склона возникают трещины растягивающего типа, а в вертикальном направлении основным механизмом разрушения является накопление деформаций ползучести.

Полный текст статьи публикуется в английской версии журнала
«Soil Mechanics and Foundation Engineering”, vol.62, No.5


Литература


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