碳酸盐岩上的石膏堆积

Elaine S. McGee, Victor G. Mossotti
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引用次数: 23

摘要

通过在监测地点暴露石灰石和大理石的新鲜样品,通过检查旧建筑物的蚀变壳和通过实验室实验,研究了碳酸盐岩上石膏的积累。碳酸盐岩中石膏的富集有几个因素。在污染程度高的城市环境中,大理石或石灰石不受雨水的直接冲刷,可能会积聚一层石膏外壳。如果石头是多孔的或具有不规则的表面积,地壳发育可能会增强。石膏结壳是一种地表蚀变特征;石膏晶体形成于气孔与空气的交界面,这里蒸发最剧烈。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Gypsum accumulation on carbonate stone

The accumulation of gypsum on carbonate stone has been investigated through exposure of fresh samples of limestone and marble at monitored sites, through examination of alteration crusts from old buildings and through laboratory experiments. Several factors contribute to gypsum accumulation on carbonate stone. Marble or limestone that is sheltered from direct washing by rain in an urban environment with elevated pollution levels is likely to accumulate a gypsum crust. Crust development may be enhanced if the stone is porous or has an irregular surface area. Gypsum crusts are a surficial alteration feature; gypsum crystals form at the pore opening-air interface, where evaporation is greatest.

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