1 Department of Civil Engineering, School of Engineering and Technology, China University of Geosciences, Beijing, no. 29 Xueyuan Road, Haidian District, Beijing 100083, People's Republic of China.
2 Department of Building, Civil & Environmental Engineering, Concordia University, 1455 de Maisonneuve Blvd, W., EV6.166 Montreal, Quebec, Canada H3G 1M8.

Thermally induced deterioration behaviour of two dolomitic marbles under heating-cooling cycles.

R Soc Open Sci. 2018 Oct;5(10):180779

Authors: Zhang ZJ, Liu JB, Li B, Yang XG

Abstract

Thermally induced deterioration behaviour can cause severe weathering in marbles. Most previous studies focus on the deterioration behaviour of calcitic marbles. Relevant studies of dolomitic marbles are generally carried out under a 'high temperature and low cycling times' condition. Little attention is focused on the deterioration behaviour in dolomitic marbles when they are subjected to a large quantity of heating-cooling cycles under a 'low temperature and high cycling times' condition. This paper presents experimental investigations on the thermally induced deterioration behaviour of two Beijing dolomitic marbles (Qingbaishi Marble (QM) and Hanbaiyu Marble (HM)) under heating-cooling cycles up to 1000 cycling times. The applied temperature range is from -20°C to 60°C which is to simulate the seasonal temperature variations in Beijing city, China. Related properties such as weight loss, three-dimensional microtopography, elastic wave velocity and uniaxial compressive strength were measured at certain cycles. The results indicate that thermally induced deterioration behaviour will result in a continuous weight loss in dolomitic marble samples. Mechanical properties of those two marbles are strongly affected by heating and cooling treatments, which were reflected by the reductions of dynamic Young's modulus and uniaxial compressive strength with an increase of thermal cycles. Compared with QM, HM displays a higher level of thermally induced deterioration which should be due to the abundance of quartz mineral.

PMID: 30473828 [PubMed]