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中文核心期刊

温度影响下砂岩的细观破坏及变形场的DSCM表征

Meso-failure of sandstone under temperature effects and DSCM study on deformation field

  • 摘要: 通过扫描电镜(SEM)实时在线观察研究了温度影响下砂岩的细观破坏,观察到砂岩的脆性断裂可同时发生在不同地方、不同矿物可能独立承载和裂纹分叉等现象. 温度低于100°C时,主裂纹附近有许多微裂纹和支裂纹发生;而温度超过150°C之后,表面很少出现支裂纹或二次裂纹. 随着温度的升高,砂岩的断裂韧性有先升高后降低的趋势,150°C左右是断裂韧性变化的临界温度. 随着温度的升高,砂岩的细观断裂机制有由脆性机制向延性机制转变的趋势,抵抗和协调变形的能力都得到增强. 细观尺度下砂岩的破坏机制有沿颗粒断裂、穿颗粒断裂及其混合断裂,其中沿颗粒断裂机制占主导地位,这是由于沿颗粒破坏需要消耗较少的能量,而穿颗粒断裂需消耗较多的能量. 利用数字散斑相关方法(digital speckle correlation method, DSCM)对SEM下砂岩破坏的细观变形场进行了测量,这表明利用DSCM表征岩石的局部变形场的连续式测量是可行的.

     

    Abstract: The meso-failure progress of sandstone under temperatureeffects was observed and studied in-situ through Scanning Electron Microscopy(SEM). The SEM observations under thermal-mechanical coupling effects showedthe brittle fracture on the different places, independent bearing mineralsand the bifurcated cracks in the sandstone sample. The numer of microcracksor the branch cracks near the main crack was large below the temperature of100°C and small over 150°C. Within the temperature from25°C to 300°C, the fracture toughness of sandstone increased firstly and thendecreased. There was the threshold temperature of 150°C forsandstone at meso-scale. With the rising temperature, the failutre ofsandstone will obtain the transition from brittle to ductile behavior.Sandstone failure modes were experimental observed, such as transgranular,intergranular and mixed mode. Meanwhile, the deformation field of sandstonewas measured using digital speckle correlation method (DSCM).

     

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