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作 者:陈金明[1] 康天合[1] 杨永康[1] 刘宁[1] 王政华[1] 郭卫卫[1]
机构地区:[1]太原理工大学采矿工艺研究所,山西太原030024
出 处:《矿业研究与开发》2012年第6期40-42,共3页Mining Research and Development
基 金:国家自然科学基金资助项目(50474057;50974093)
摘 要:对自然含水煤样和饱水煤样进行控制压缩量的压裂对比实验,通过Rosin-Rammler模型分析煤样压裂破碎后碎块粒径分布及其与压缩量的关系。研究结果表明:自然含水煤样小粒径(小于1.25 mm)碎块量大于饱水煤样,随着压缩量的增加,自然含水煤样和饱水煤样小粒径碎块量都增加;随着压缩量的增大,自然含水煤样碎块分布趋于分散,饱水煤样碎块分布趋于集中,且饱水煤样碎块分布比自然含水煤样集中;饱水煤样碎块中位径d50比自然含水煤样碎块小。The contrast fracture experiment of natural hydrated coal sample and water - saturated coal sample under controlled compression was performed, and Rosin- Rammler model was used to analyze the particle size distribution of coal sample after being broken and its relationship with the controlled compression. The research results show that: the natural hydrated coal brought more small - size fragments ( smaller than 1.25 mm) than the water - saturated coal, both brought more and more small - size fragments coal with increase of compression ; As the compression increased, the size distribution of fractured natural hydrated coal sample displayed a disperse trend, but the size distribution of fractured water - saturated coal sample displayed a concentrated trend, as well the size distribution of fractured water- saturated coal sample was more concentrated than one of fractured natural hydrated coal sample; The median diameter d50 of fractured water - saturated coal sample small than one of fractured natural hydrated coal sample.
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