中国煤炭地质
中國煤炭地質
중국매탄지질
COAL GEOLOGY OF CHINA
2014年
7期
25-27,32
,共4页
煤中硫%脱硫%沉积环境%白岩脚矿区%黔西煤田
煤中硫%脫硫%沉積環境%白巖腳礦區%黔西煤田
매중류%탈류%침적배경%백암각광구%검서매전
sulfur in coal%desulfurization%sedimentary environment%Baiyanjiao mine area%Qianxi coalfield
通过对黔西煤田白岩脚矿区龙潭组主要煤层进行化验分析，认为矿区煤中硫含量从低到高均有分布，垂向上自下而上逐渐降低，平面上9、14及15煤总体呈现东北部高西南部低的趋势，4煤层则表现为西南部相对较高；硫的赋存形态以硫化物硫为主，沉积环境控制了煤中硫的含量及各种形态硫的分布；9、14煤层以硫化物硫为主，脱硫效果良好，15煤层以有机硫为主，脱硫效果一般。建议在矿山开发过程中对低硫煤和高硫煤进行配采。
通過對黔西煤田白巖腳礦區龍潭組主要煤層進行化驗分析，認為礦區煤中硫含量從低到高均有分佈，垂嚮上自下而上逐漸降低，平麵上9、14及15煤總體呈現東北部高西南部低的趨勢，4煤層則錶現為西南部相對較高；硫的賦存形態以硫化物硫為主，沉積環境控製瞭煤中硫的含量及各種形態硫的分佈；9、14煤層以硫化物硫為主，脫硫效果良好，15煤層以有機硫為主，脫硫效果一般。建議在礦山開髮過程中對低硫煤和高硫煤進行配採。
통과대검서매전백암각광구룡담조주요매층진행화험분석，인위광구매중류함량종저도고균유분포，수향상자하이상축점강저，평면상9、14급15매총체정현동북부고서남부저적추세，4매층칙표현위서남부상대교고；류적부존형태이류화물류위주，침적배경공제료매중류적함량급각충형태류적분포；9、14매층이류화물류위주，탈류효과량호，15매층이유궤류위주，탈류효과일반。건의재광산개발과정중대저류매화고류매진행배채。
Through testing and analysis of Longtan Formation main coal seams in Baiyanjiao mine area, Qianxi coalfield have found a wide range of coal sulfur content distribution;vertically, gradually lowering from top to bottom;horizontally, coal Nos. 9, 14 and 15 low-ering from northeast to southwest, while coal No.4 presents relatively high in southwest. Forms of sulfur are mainly sulfide sulfur, sedi-mentary environment controlled sulfur content and every kind of sulfur form. Sulfur in coal Nos.9 and 14 is mainly sulfide sulfur with good desulfurization effect;in coal No.15 is mainly organic sulfur with common desulfurization. Proration extracting of low sulfur coal and high sulfur coal has been proposed during coalmine exploitation.
