2018
DOI: 10.1007/s00231-018-2376-5
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Damage characteristics and thermo-physical properties changes of limestone and sandstone during thermal treatment from −30 °C to 1000 °C

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Cited by 34 publications
(13 citation statements)
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“…Hence, some fitting of the properties (obtained from TPS tests) was carried out. Herein, a previous research study on limestone by Shen et al 21 provided some useful insight into the material properties since there was some agreement between the thermal properties presented in the mentioned study and TPS results obtained from this current work. On the basis of the comparison of data, (fitting) effective thermal properties, particularly for the thermal conductivity and specific heat, were developed (Table 5), which provided good agreement with the furnace test result (Fit_sim), see Figure 8.…”
Section: Numerical Investigationssupporting
confidence: 83%
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“…Hence, some fitting of the properties (obtained from TPS tests) was carried out. Herein, a previous research study on limestone by Shen et al 21 provided some useful insight into the material properties since there was some agreement between the thermal properties presented in the mentioned study and TPS results obtained from this current work. On the basis of the comparison of data, (fitting) effective thermal properties, particularly for the thermal conductivity and specific heat, were developed (Table 5), which provided good agreement with the furnace test result (Fit_sim), see Figure 8.…”
Section: Numerical Investigationssupporting
confidence: 83%
“…As the thermal properties were determined up to 423 C, the properties at higher temperatures were taken constant until 1200 C in the calculations (see Table 5). Herein, a previous research study on limestone by Shen et al 21…”
Section: Lime Plastermentioning
confidence: 99%
“…Commonly, crack propagation deviates from the boundary of crystals, and then turns to the direction of the maximum of thermal stress rapidly, which causes the fracture surface to be rough for these Griffith's cracks [60]. In addition, the evaporation process of free water, bounded water and structural water existing in the original defects (pores or voids) mainly occurs below the threshold temperature point 400 • C [61]. The water evaporation (seen in Figure 6), happened in the original defects, and provides enough deformation space and aggravates the thermal expansion of mineral particles to be persistent.…”
Section: Discussionmentioning
confidence: 99%
“…Furthermore, some hard decomposed minerals such as calcite and albite would begin to compose and even melt under elevated temperature conditions beyond 600 °C. In addition, metallic bonds such as Al-O, Na-O, K-O, and Ca-O generally fracture when the temperature increases to 600 °C because of the influence of solid mineral expansion [61].…”
Section: Discussionmentioning
confidence: 99%
“…e unfrozen water content of saturated rock decreases with the decrease of freezing temperature, which has a great influence on the strength and deformation [2]. Shen et al [3] studied the water migration and phase change of sandstone as the two core factors of freezing (20°C ⟶ −30°C) damage. Liu et al [4] concluded that the peak strength of saturated silty mudstone under uniaxial compression has a parabolic relationship with temperature, and the axial strain at peak strength has a linear relationship with temperature.…”
Section: Introductionmentioning
confidence: 99%