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Characterization and thermal behavior of marble from northwestern Pakistan

机译:巴基斯坦西北大理石的特征与热行为

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This research aimed to determine the physical and strength characteristics and temperature-based behavior of marble. Based on laboratory investigations, marble from northwestern Pakistan (Chitral and Khyber) was characterized as follows: (i) high water absorption (0.16%), high porosity (similar to 0.42%), low ultrasonic pulse velocity (similar to 4000 m/s), and low strength (53 +/- 4 MPa) calcite with an equigranular texture with uneven boundaries and sutured contacts and (ii) low absorption (0.05%), low porosity (0.13%), high ultrasonic pulse velocity (6200 m/s) and high strength (68 +/- 6 MPa) quartz-rich calcite having an inequigranular texture with linear boundaries and mosaic contacts. Under thermal treatment, water absorption and porosity initially decreased at 100 degrees C (calcite expansion) followed by an increase around 200 degrees C (thermal fracturing) and then by a decrease at 300 degrees C (tightening of thermal fractures). Bulk density did not show any significant change within the range of these temperatures, and the ultrasonic pulse velocity trend was generally reversed. Both compressive and tensile strengths showed an initial increase at 100 degrees C followed by a decrease at 200 degrees C and then by a low decrease at 300 degrees C. As expected, the compression strength (40 MPa-120 MPa) was found to be almost one order of magnitude larger than the tensile strength (4 MPa-12 MPa).
机译:该研究旨在确定大理石的物理和强度特征和基于温度的行为。根据实验室调查,来自巴基斯坦西北部(横滩和Khotber)的大理石的特征如下:(i)高吸水率(0.16%),高孔隙率(类似于0.42%),低超声波脉冲速度(类似于4000米/秒)和低强度(53 +/- 4MPa)方解石,带有不平坦的边界和缝合触点和(ii)低吸收(0.05%),低孔隙度(0.13%),高超声波脉冲速度(6200米/ S)和高强度(68 +/- 6 MPa)石英的方解石,具有不必要的纹理,具有线性边界和马赛克接触。在热处理下,吸水和孔隙率最初在100℃(方解石膨胀)下降低,然后增加约200℃(热压裂),然后在300摄氏度(热骨折的收紧)下降。散装密度没有显示在这些温度范围内的任何显着变化,并且超声波脉冲速度趋势通常逆转。抗压和拉伸强度均显示100℃的初始增加,然后在200℃下减少,然后在300℃下降低。如预期,发现压缩强度(40MPa-120MPa)几乎比拉伸强度(4MPa-12MPa)大的一个数量级。

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