A prediction method for abrasion loss rate of some Egyptian carbonate rocks due to cyclic salt crystallization weathering using physico-mechanical deterioration: insights from laboratory investigations

IF 1.4 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS Acta Geodaetica et Geophysica Pub Date : 2023-02-02 DOI:10.1007/s40328-023-00401-2
Marzouk Mohamed Aly Abdelhamid, B. G. Mousa
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Abstract

Salt crystallization is the most important weathering processes that causes problems for rocks used as building stones. Therefore, assessment of the physico-mechanical properties of stones against cyclic salt crystallization is a critical issue for rock engineering applications in salty environmental conditions especially prone to abrasion. This research aims at investigating the relationship between the degradation of various physico-mechanical properties including apparent porosity, point load index, unconfined compression strength and abrasion loss rate for rocks during salt weathering process. For showing rock weathering in the salt crystallization process, five kinds of carbonate rocks were sampled from different areas of Egypt and subject to cyclic salt crystallization, up to twenty cycles. The variation rates of their physico-mechanical characteristics and abrasion loss values were calculated after each five cycles of salt weathering. The results showed that the studied rocks are suitable for use as building and decorative stones in areas prone to crystallization of salts, but attention must be paid to rocks with high porosity and low strength characteristics such as El-Minia limestone specimens. It was also found that there are strong linear correlations between the physico-mechanical degradation parameters and the abrasion loss rate of the studied rock samples at the end of the twentieth cycle of salt weathering. These relationships may be used to estimate the abrasion loss rate of the studied rock types against the cyclic salt weathering conditions and hence to make a rapid evaluation of the stone durability.

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利用物理-机械劣化预测埃及一些碳酸盐岩因循环盐结晶风化造成的磨蚀损失率的方法:实验室调查的启示
盐结晶是最重要的风化过程,会给用作建筑石材的岩石带来问题。因此,在盐碱环境条件下,尤其是在易磨损的环境条件下,评估石头的物理机械特性以防止循环盐结晶是岩石工程应用的一个关键问题。本研究旨在探究岩石在盐风化过程中各种物理力学性能(包括表观孔隙率、点荷载指数、无约束压缩强度和磨损率)退化之间的关系。为了展示盐结晶过程中的岩石风化,从埃及不同地区采集了五种碳酸盐岩样本,并对其进行了长达二十次的循环盐结晶。在每五个盐风化周期后,计算其物理机械特征的变化率和磨损值。结果表明,所研究的岩石适合在易受盐类结晶影响的地区用作建筑和装饰石材,但必须注意孔隙率高、强度低的岩石,如 El-Minia 石灰岩试样。研究还发现,在第 20 个盐风化周期结束时,所研究岩石样本的物理机械降解参数与磨蚀损失率之间存在很强的线性关系。这些关系可用来估算所研究岩石类型在循环盐风化条件下的磨损率,从而快速评估石材的耐久性。
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来源期刊
Acta Geodaetica et Geophysica
Acta Geodaetica et Geophysica GEOCHEMISTRY & GEOPHYSICS-
CiteScore
3.10
自引率
7.10%
发文量
26
期刊介绍: The journal publishes original research papers in the field of geodesy and geophysics under headings: aeronomy and space physics, electromagnetic studies, geodesy and gravimetry, geodynamics, geomathematics, rock physics, seismology, solid earth physics, history. Papers dealing with problems of the Carpathian region and its surroundings are preferred. Similarly, papers on topics traditionally covered by Hungarian geodesists and geophysicists (e.g. robust estimations, geoid, EM properties of the Earth’s crust, geomagnetic pulsations and seismological risk) are especially welcome.
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