Effects of high-temperature thermal treatment on the porosity of red sandstone: an NMR analysis

Acta Geophysica

article

Zhang, He¹  Sun, Qiang¹  Jia, Hailiang⁴  Dong, Zhihao⁵  Luo, Tao⁶ 

[1] College of Geology and Environment, Xi’an University of Science and Technology;Shaanxi Provincial Key Laboratory of Geological Support for Coal Green Exploitation;Geological Research Institute for Coal Green Mining, Xi’an University of Science and Technology;College of Architecture and Civil Engineering, Xi’an University of Science and Technology;School of Resources and Geosciences, China University of Mining and Technology;Shaanxi Key Laboratory of Safety and Durability of Concrete Structures, Xijing University

关键词: NMR;    T 2;    Thermal treatment;    Porosity;    Red sandstone;   

DOI  :  10.1007/s11600-020-00526-w

学科分类：地球科学(综合)

来源: Polska Akademia Nauk * Instytut Geofizyki

【 摘 要 】

High temperatures affect the physical properties of red sandstone seriously, especially the pores. Understanding its mechanism is of great significance in coal mining following underground gasification, geothermal energy utilization, and the deep burial of nuclear waste. Nuclear magnetic resonance (NMR) was used to detect pore structure characteristics, and scanning electron microscopy (SEM) and polarizing light microscopy (PLM) were used to mechanism of change. The transverse relaxation time (T2) and signal strengths of red sandstone treated at various temperatures were observed by NMR, and then, the pore situation can be obtained, and finally, the influence of temperature on the pore structure of red sandstone can be obtained. Microscopic photographs of the pores of red sandstone were obtained by SEM and PLM to assist in explaining the process of microstructural change, especially the influences of temperature on pore characteristics and grain morphology and distribution. The researches indicate that after the heat treatment of red sandstone at 25–1300 °C, the pore and strength characteristics change in well-defined stages. Before 500 °C, the pore diameters and distribution range increase, but the porosity and internal grain structure do not change significantly. At 500–1000 °C, red sandstone micropores contract, mesopores and macropores develop, and strength decreases. After 1000 °C, the grains that comprise sandstone melt and fill many of the pores, decreasing porosity. The proportion of micropores decreases, while mesopores and macropores increase. In addition, a large number of bubbly holes appear in and on the sandstone, presumably caused by gases such as CO2, and water vapor from dehydrating grains. The changes in pore and cementation states with temperature are the main factors affecting the tensile strength of red sandstone.

【 授权许可】

Unknown