摘要
本文首次较为系统地研究了不同变质程度的煤,在低角区和中角区的X射线衍射特点。指出随着变质程度的提高,16×10-(10)m峰和(002)峰强度逐渐增高,而γ带强度降低,低变质煤未见16×10-(10)m峰,高变质煤中γ带不明显;随着变质程度提高,16×10-(10)m峰、γ带峰、(002)峰的晶面间距均减小,16×10-(10)m峰减小幅度较大,(002)峰减小幅度较少。基于以上分析,对其形成机理进行了初步探讨。图6,参7。
Based on the samples of different metamorphic types of coals,the authors had made an X-ray scattering investigation of coals at middle and low angles. The results show that the intensities of the (002) peak and the 16×10-10m peak were increased,but the γ belt decreased,as the raise of metamorphic degree of coals;and that the interlayer distances of the 16×10-10m peak,the γ belt and the (002) peak were all decreased as the raise of metamorphic degree of coals. Based upon it,the forming mechanism was suggested.6figs.,7refs.
出处
《湘潭矿业学院学报》
1996年第4期62-66,共5页
Journal of Xiangtan Mining Institute
关键词
煤结构
X-射线衍射
煤
变质程度
coal structure
X-ray diffraction
the metamorphic degree of coals