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Влияние темпа охлаждения на переохлаждение поровой воды в грунтах

Влияние темпа охлаждения на переохлаждение поровой воды в грунтах

Abstract

Представлены результаты исследования переохлаждения поровой воды в грунтах. Эксперименты проведены на дифференциальном сканирующем калориметре. Выявлено влияние темпа охлаждения на переохлаждение поровой воды в глинистых грунтах. Повышение темпа охлаждения вызывает увеличение переохлаждения поровой воды.

Researches results of soil water subcool in the article are presented. The experiments were conducted on differential scanning calorimeter. An influence of the freezing on porous water subcool in the clay soil was determined. Increasing of the freezing rate causes the increase of the soil water subcool.

Keywords

ГРУНТ, ПОРОВАЯ ВОДА, ЛЕД, ЗАРОДЫШЕОБРАЗОВАНИЕ, КИНЕТИКА, ТЕМП ОХЛАЖДЕНИЯ, ПЕРЕОХЛАЖДЕНИЕ, ДИСПЕРСНОСТЬ, ДИФФЕРЕНЦИАЛЬНЫЙ СКАНИРУЮЩИЙ КАЛОРИМЕТР

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selected citations
These citations are derived from selected sources.
This is an alternative to the "Influence" indicator, which also reflects the overall/total impact of an article in the research community at large, based on the underlying citation network (diachronically).
BIP!Citations provided by BIP!
popularity
This indicator reflects the "current" impact/attention (the "hype") of an article in the research community at large, based on the underlying citation network.
BIP!Popularity provided by BIP!
influence
This indicator reflects the overall/total impact of an article in the research community at large, based on the underlying citation network (diachronically).
BIP!Influence provided by BIP!
impulse
This indicator reflects the initial momentum of an article directly after its publication, based on the underlying citation network.
BIP!Impulse provided by BIP!
0
Average
Average
Average
bronze