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作 者:任德贻[1] 雷加锦[1] 唐跃刚[1] 郭国莉 姚玉琴[2]
机构地区:[1]中国矿业大学北京研究生部,100083 [2]北京科技大学物构中心,100083
出 处:《煤田地质与勘探》1993年第1期27-30,共4页Coal Geology & Exploration
摘 要:应用扫描电镜、能谱仪和波谱仪测定了煤中有机硫含量。a.在镜质体有机硫含量低于0.50%的煤中,惰质体的有机硫含量与其相近。而在镜质体有机硫含量高于0.5%的煤中,惰质体的有机硫含量大多为镜质体的40%~50%。各种镜质体和惰质体的有机硫含量随其凝胶化程度增高而增加。b.聚煤古地理环境对煤中有机硫含量起决定性作用。以镜质体为例,形成于湖滨三角洲平原环境的神木煤含有机硫0.21%,形成于滨海三角洲平原环境的水城大河边煤含有机硫0.84%,形成于泻湖海湾环境的兖州晚石炭世煤含有机硫2.24%。The SEM,EDS,and WDS are used for the organic sulfur(S_o) determination in coal. 1.In low sulfur coals,while S_o content is less than 0.50%,S_o content of inertinite is similar to that of vitrinite.However,in the coals,whost S_o is more than 0.50%,the S_o of inertinite is mostly 40%~50% of that of vitrinite.S_o content incresses with their gelification degree.Meanwhile, sporinite,cutinite and alginite contain S_o more than vitrinite. 2.The palaeogeographic environment of coal accumulation evidently influence on S_o content in coal.The vitrinite of Shen-Mo coal,which accumulated in lacustrine delta plain,contain 0.21% S_o,the vitrinite in Shui — Cheng coal,which accumulated in coastal delta plain,contain 0.84% S_o,in Yan—Zhou coal,which is borne in paralic,sequence is so high as 2.24%.
分 类 号:P618.110.4[天文地球—矿床学]
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