风化作用对意大利南托斯卡纳Amiata山粗面质火山岩工程地质性质的影响

IF 2.4 Q2 GEOSCIENCES, MULTIDISCIPLINARY
Enrico D’Addario, Giovanna Giorgetti, Claudia Magrini, Leonardo Disperati
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引用次数: 0

摘要

岩性和风化程度的变化影响岩石的物理力学性质。本文采用野外和室内分析相结合的方法,研究了意大利中部阿米亚塔山粗面质火山岩的风化程度与工程地质性质之间的关系。我们收集了现场的施密特锤测试数据。我们通过实验室的热分析来评估风化作用,量化了次生矿物的百分比。我们还确定了干密度(ρd),固体比重(Gs),孔隙度(n)和二维(2D)孔隙度的扫描电镜调查结果。研究结果表明,施密特锤回弹值与次生矿物含量呈负线性相关。这种相关性提供了一种定量估计岩石单轴抗压强度(UCS)随风化增加而恶化的工具。热分析是评价岩浆岩风化程度的一种定量、可重复的方法。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Weathering Effects on Engineering Geological Properties of Trachydacitic Volcanic Rocks from the Monte Amiata (Southern Tuscany, Italy)
Variability in lithology and weathering degree affects physical and mechanical properties of rocks. In this study, we investigated the relationships between weathering degree and engineering geological properties of trachydacitic volcanic rocks from Monte Amiata (central Italy) by coupling field and laboratory analyses. We collected in situ Schmidt hammer tests in the field. We evaluated weathering quantifying the percentage of secondary minerals through thermal analysis in the laboratory. We also determined dry density (ρd), specific gravity of solids (Gs), porosity (n) and two-dimensional (2D) porosity as resulted from scanning electron microscopy investigations. The results of our study indicate a negative linear correlation between Schmidt hammer rebound values and secondary mineral percentage. This correlation provides a tool to quantitatively estimate the deterioration of rock uniaxial compressive strength (UCS) as weathering increases. Moreover, thermal analysis turned out to be a quantitative and reproducible method to evaluate weathering degree of magmatic rocks.
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来源期刊
Geosciences (Switzerland)
Geosciences (Switzerland) Earth and Planetary Sciences-Earth and Planetary Sciences (all)
CiteScore
5.30
自引率
7.40%
发文量
395
审稿时长
11 weeks
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