4.5 Article

Influence of Temperature on the Microstructure Deterioration of Sandstone

Journal

ENERGIES
Volume 11, Issue 7, Pages -

Publisher

MDPI
DOI: 10.3390/en11071753

Keywords

sandstone; microstructure deterioration; X-ray diffraction (XRD); thermo-gravimetric analyses (TGA); scanning electron microscopy (SEM)

Categories

Funding

  1. National Natural Science Foundation of China [41772333, 51774231]
  2. National Key Basic Research and Development Program of China (973 Program) [2015CB251600]
  3. Foundation from State Key Laboratory for Geo-Mechanics and Deep Underground Engineering, China University of Mining Technology [SKLGDUEK1813]

Ask authors/readers for more resources

Macroscopic properties of sandstone are commonly attributed to the degradation of its microstructure during heating treatment processes. However, few previous studies have focused on comprehensive observations on how the microstructure of sandstone changes with temperature. In this study, a kind of sandstone containing quartz, albite, calcite, and laumontite (little), was collected from Linyi (Shandong Province, China) to observe the microstructure degradation changes with temperature by X-ray diffraction (XRD), Scanning electron microscopy (SEM) and thermo-gravimetric analyses (TGA). Firstly, 10 groups of sandstone samples were heated from 25 degrees C to 900 degrees C. Then, some core micro-parameters including lattice constant, full width at half maximum (FWHM), micro-strain, dislocation density, TGA curve changes and failure characteristic of the mineral were analyzed comprehensively. Finally, the underlying mechanism causing the microscopic thermal damage at different temperature intervals was also discussed. The results showed that: (1) quartz, the framework component of this sandstone, underwent an alpha- to beta-phase change over the temperature range from 400 degrees C to 600 degrees C. This phenomenon caused the lattice constant, micro-strain, dislocation density and TGA curve to decrease sharply during this interval, leading to the microstructure deterioration of sandstone; (2) calcite underwent a decomposition reaction between 600 degrees C and 800 degrees C, and resulted in the XRD pattern peak, lattice constant, micro-strain and TGA curve dropping continuously. It destroyed further the internal microstructure of sandstone and produced numerous inter-granular cracks around quartz crystals; (3) further examination found that the decomposition reactions of minerals presented non-synchronized characteristics due to the different sensitivities of minerals to temperature, which led to thermal stress, thermal fracturing of minerals, and thermal reactions happening in different temperature intervals.

Authors

I am an author on this paper
Click your name to claim this paper and add it to your profile.

Reviews

Primary Rating

4.5
Not enough ratings

Secondary Ratings

Novelty
-
Significance
-
Scientific rigor
-
Rate this paper

Recommended

No Data Available
No Data Available