Prediction model for the weathering of sandstone under ambient climate actions

机译：环境气候作用下砂岩风化的预测模型

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Detailed analyses of the weathering processes indicate that the decomposition can be attributed mainly to continuously changing temperature and moisture gradients, partly in conjunction with frost and ice formation as well as to partially arising crystallisation processes of solved salts in the stone. For the description of the deterioration process due to these main actions, which lead to a gradual failure of the grain bonding proceeding from the surface to inner parts of the cross section, an appropriate model for the weathering of sandstone is presently being developed.

机译：对风化过程的详细分析表明，分解主要归因于温度和湿度梯度的不断变化，部分归因于霜和冰的形成，以及部分溶解于石头中的盐的结晶过程。为了描述由于这些主要作用而导致的劣化过程，这些劣化作用导致从横截面的表面到内部的晶粒粘结逐渐失效，目前正在开发一种合适的砂岩风化模型。

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来源
《International PhD Symposium in Civil Engineering vol.2; 20040616-19; Delft(NL)》|2004年|P.1395-1401|共7页
会议地点 Delft(NL)
作者
Engin Kotan; Harald S. Mueller;
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作者单位

Institute of Reinforced Concrete Structures and Building Materials, University of Karlsruhe, Germany;

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原文格式 PDF
正文语种 eng
中图分类市政工程;
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Prediction model for the weathering of sandstone under ambient climate actions

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