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首页> 外文期刊>International Journal of Coal Geology >Vitrinite reflectance property change during heating under inert conditions
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Vitrinite reflectance property change during heating under inert conditions

机译:惰性条件下加热过程中玻璃tri反射特性的变化

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The aim of the study was to determine optical properties of vitrinite, subjected to temperatures within the range of 400-1200℃ for durations of 1-7 h, in an argon atmosphere. The samples of vitrinite concentrate (Vt content 90%, R_r = 1.17%) were inserted in the furnace at room temperature and subjected to a heating rate of 60℃/min. To assess the effects of the experiment, random reflectance as well as apparent maximum and minimum reflectances of vitrinite were measured on the raw and thermally treated concentrates. Employing the method and computer programme of W.E. Kilby, the true maximum, intermediate and minimum reflectances of vitrinite as well as reflectance anisotropy and Reflectance-Indicating Surface (RIS) shapes were evaluated. Transformation of vitrinite subjected to heating is influenced more by the increase of temperature than the time applied. During the plastic stage (400-500℃), vitrinite is subjected to substantial chemical and physical alteration. It is manifested by chemical decomposition, significant mass loss and mesophase appearance. Porosity, relief, reflectance and bireflectance of the vitrinite grains increase with heating. At the temperature of 1200℃, random vitrinite reflectance reaches 6.62% with bireflectance of 3.46%. Mesophase at 1200℃ was characterised by mean reflectance equal to 9.25% and a bireflectance of 13.35%. The reflectance character of vitrinite changes from biaxial negative into biaxial positive-negative. However, the original RIS shape, resulting from the tectonic regime during the main phase of coalification, is not fully transformed until heated to 1200℃. Reflectance character of mesophase is consistently biaxial negative. The internal structure of mesophase is thought to be better organised than the internal structure of vitrinite.
机译:该研究的目的是确定在氩气气氛下,在400-1200℃的温度下,持续1-7 h的镜质体的光学性质。在室温下将玻璃质精矿样品(Vt含量为90%,R_r = 1.17%)插入炉中,并以60℃/ min的速度加热。为了评估实验的效果,对未经处理和经过热处理的精矿测量了镜质体的随机反射率以及视在最大和最小反射率。采用W.E.的方法和计算机程序Kilby评估了镜质的真实最大,中间和最小反射率,以及反射率各向异性和反射指示表面(RIS)形状。加热后的镜质体的转变受温度升高的影响大于施加时间的影响。在塑化阶段(400-500℃),镜质体会发生实质性的化学和物理变化。其表现为化学分解,明显的质量损失和中间相的出现。随着加热,镜质颗粒的孔隙率,起伏,反射率和双反射率增加。在1200℃的温度下,镜质体的随机反射率达到6.62%,双反射率为3.46%。 1200℃的中间相的特征在于平均反射率为9.25%,双反射率为13.35%。镜质石的反射特性从双轴负向变为双轴正负。但是,由于在煤化的主要阶段的构造状态而产生的原始RIS形状直到加热到1200℃才完全转变。中间相的反射特性始终是双轴负的。中间相的内部结构被认为比镜质体的内部结构更好。

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