کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
5787591 1641765 2017 9 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
Exfoliation microcracks in building granite. Implications for anisotropy
ترجمه فارسی عنوان
میکروارگانیک ها در ساختن گرانیت. پیامدهای آنیزوتروپیک
کلمات کلیدی
میکروکراس لایه برداری، سنگ ابعاد، ناهمسانگردی، سنگ گرانیت،
موضوعات مرتبط
مهندسی و علوم پایه علوم زمین و سیارات مهندسی ژئوتکنیک و زمین شناسی مهندسی
چکیده انگلیسی


- The splitting planes of granite are controlled by the exfoliation microcracks.
- The exfoliation microcracks condition building granite anisotropy.
- The decay of building granite is different in each splitting plane.
- The analysis of exfoliation microcracks with fluorescence microscopy allowed to study their characteristics.
- Splitting planes are the orientation that should be applied when performing laboratory tests of building granite.

Granite is found in many world heritage monuments and cities. It continues to be one of the most widely used stones in today's construction, given its abundance, uniformity and durability. Quarrymen traditionally cut this rock along its orthogonal slip planes, where splitting is easier. Ranked by ease of splitting, these planes are rift, grain and hardway. Granite is traditionally quarried along the rift plane where coplanar exfoliation microcracks coalesce developing a flat surface. This splitting surface minimizes the cost and effort of subsequent hewing. Rift plane was predominantly used on the fair face of ashlars in heritage buildings worldwide. Determining the petrographic and petrophysical behaviour of these three orthogonal splitting planes in granite is instrumental to understanding decay in ashlars and sculptures. The decay of building granite is different in each splitting plane.Alpedrete granite was the stone selected for this study based on the orientation and distribution of exfoliation microcracks and the characterisation of their implications for the anisotropy of petrophysical properties such as ultrasonic wave propagation, capillarity, air permeability, micro-roughness and surface hardness. Inter- and intracrystalline microcrack length and spacing were also measured and quantified.The findings show that the splitting planes in Alpedrete granite are determined by the orientation of exfoliation microcracks, which as a rule are generally straight and intracrystalline and determine the anisotropy of the petrophysical properties analysed.Splitting planes are the orientation that should be applied when performing laboratory tests for the petrographic and petrophysical properties of building granite.

ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Engineering Geology - Volume 220, 30 March 2017, Pages 85-93
نویسندگان
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