摘要
以煤质煤岩数据和以往钻孔资料为基础,查明了云泉矿区9号煤层中高硫煤主要分布在矿区的南部,15号煤层高硫煤主要分布在矿区的东南部与北部。通过相关性分析发现,云泉矿区灰成分指数K与黄铁矿硫含量呈正相关关系,促进了黄铁矿硫的形成;而煤灰成分中Fe_(2)O_(3)的含量与全硫和硫化铁硫含量呈正相关关系。通过煤相分析发现,云泉矿区在形成的过程中经历了较为频繁的海进海退,煤中硫的含量和形态受到海水影响较大。
Based on coal quality and previous drilling data, this paper finds that the grizzle of No.9 coal seam is mainly distributed in the southern part of Yunquan mining area, and the grizzle of No.15 coal seam is mainly distributed in the southeast and north of the mining area. The ash composition index K of Yunquan mining area is positively correlated with the sulfur content of pyrite through the correlation analysis, which promotes the formation of pyrite sulfur;the content of Fe_(2)O_(3) in the coal ash composition is positively correlated with the content of total sulfur and iron sulfide sulfur. Through coal facies analysis, it is found that Yunquan mining area has experienced frequent sea transgressions and retreats during the formation process, and the content and form of sulfur in coal are greatly affected by seawater.
作者
郭强
张鹏
GUO Qiang;ZHANG Peng(Shanxi Provincial Geological and Mineral Research Institute Co.,Ltd.,Taiyuan 030001,China;Coal and Coal Measure Gas Geology Key Laboratory of Shanxi Province,Taiyuan 030001,China)
出处
《矿业安全与环保》
北大核心
2022年第6期13-18,共6页
Mining Safety & Environmental Protection
基金
国家自然科学基金项目(41902180)
中央引导地方科技发展资金项目(YDZX20201400001051)
山西省应用基础研究面上青年基金项目(201801D221045,201801D121031)。
关键词
沁水煤田
云泉矿区
高硫煤
煤中硫
赋存规律
地质成因
Qinshui Coalfield
Yunquan mining area
grizzle
sulfur in coal
occurrence regularity
geological genesis