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Aspects of freezing process in porous material-water system Part 2. Freezing and properties of frozen porous materials

机译:多孔材料-水系统中冷冻过程的各个方面第2部分。冷冻多孔材料的冷冻和性质

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摘要

In Part 1 of this series it has been shown that ice isa strong material and adheres well with hydrophilic materials. Inthis part of the series the strengths of ice-infiltrated porous, bothunconsolidated and consolidated, materials have been reviewed.Ice-infiltrated porous materials are much stronger than theoriginal materials. The contribution of ice to strengths of frozenmaterials is higher than is expected from strengths of bulk iceitself. The disruptive pressure needed to cause damage duringfreezing of porous materials has also to be much higher, this faceseems not to have been considered in often-quoted mechanismsof frost attack. Ice infiltrates porous bodies in the form ofdendrites and in the process encapsulates still unfrozen water inmany places. During further cooling unfrozen water developshigh hydrostatic pressure capable of causing damage. Differentproposed mechanisms of frost damage have been examinedagainst the above background.
机译:在本系列的第1部分中,已经证明了冰是一种坚固的材料,并且可以很好地与亲水性材料粘合。在本系列的这一部分中,对未渗入和固结的渗冰多孔材料的强度进行了回顾。渗冰多孔材料比原始材料强得多。冰对冷冻材料强度的贡献高于散装冰自身强度的预期。在多孔材料的冻结过程中造成损坏所需的破坏压力也必须更高,似乎在经常引用的霜冻侵蚀机理中并未考虑到这一问题。冰以枝晶的形式渗入多孔体,并在此过程中将许多地方仍未冻结的水包裹起来。在进一步冷却期间,未冻结的水会形成高静水压力,从而导致损坏。针对上述背景,已经研究了不同的霜冻破坏机制。

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