保加利亚Gorni Okol村地区Plana岩体新鲜花岗闪长岩的抗冻性评价

IF 0.2 Q4 GEOSCIENCES, MULTIDISCIPLINARY
M. Krastanov, P. Ivanov, Rosen Nankin
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引用次数: 0

摘要

本文介绍了Plana深成岩体新鲜花岗闪长岩冻结后物理力学参数的变化。进行了实验室研究以评估花岗闪长岩的性质,例如确定岩石材料的强度、密度和吸水性。在干燥和饱和状态下,共对39个不同风化等级的样品进行了密度和吸水率的测试。结果表明,水分的吸收与风化程度密切相关。根据实验室试验,建议在密度和吸水率方面降低不同风化等级的岩石材料强度。新鲜花岗闪长岩经过一定次数的冻融循环后,其强度指标也有所下降。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Evaluation of the frost resistance of fresh granodiorites from the Plana pluton in the region of the village of Gorni Okol, Bulgaria
This paper presents the changes in physical and mechanical parameters of fresh granodiorites from the Plana pluton after freezing. Laboratory studies were carried out to evaluate the properties of the granodiorites, such as determining the strength, density and water absorption of the rock material. A total of 39 samples at various weathering grades were tested at a wide range of density and water absorption values in the dry and saturated state. The results revealed that the absorption of water is highly dependent on the weathering grade. From the laboratory tests, reductions of rock material strength from various weathering grades with regard to density and water absorption are suggested. After carrying out a certain number of freeze-thaw cycles of the fresh granodiorites, their strength indicators also decrease.
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