晋城矿区综采放顶煤工作面顶煤冒放性分析

根据晋城煤业集团综采放顶煤开采实际情况,从影响顶煤冒放性的煤体裂隙、开采工艺和支架与围岩关系3个方面进行分析,对综放工作面的布置、采放比、放煤步距、支架架型与工作阻力提出了建议.     

汽油机瞬态排放间接检测的实践(Ⅰ)

瞬态排放间接检测是对汽油机在汽车加速-滑行组合、节气门加速开启-关闭等瞬态工况下进行法规性检测、获得其排放状况的基本手段之一．讨论了汽油机瞬态排放间接检测的有关基础,主要内容有:建立能够方便实现瞬态工况的工程化措施;分析采用五组分排放分析仪检测汽油机瞬态排放信号将导致畸变的原因;设置瞬态排放特征参数——符号时间序列分析的Shannon熵．     

河南省某金矿床地质特征及找矿方向研究

某金矿床赋存于太华群龙潭沟组地层中，金矿床严格受断裂构造控制．通过对此金矿床地质特征的研究，系统总结了该矿床的控矿因素和找矿标志，并指明了矿区今后的找矿方向．     

建筑火灾事故的混沌特性及其控制方法研究

针对火灾事故的严峻形势,在建筑火灾事故特性进行分析的基础上,应用混沌理论对建筑火灾事故的混沌特性及控制方法进行了初步探讨,并初步建立建筑火灾事故混沌特性分析模型,对预防和控制建筑火灾事故的发生具有指导意义.图3,参8.     

柴达木盆地西部第三系碳酸盐岩层的古生物特征

柴达木盆地西部第三系的碳酸盐岩层中发现有藻类、介形虫、有孔虫、腹足类、多毛类等化石.除藻类外各种生物的数量都比较少.生物具有个体小,壳体构造简单,多样性低等特点.所有生物都属于广盐性生物.根据该区古生物特征分析和与其它地区的对比,认为当时该区生物生长于内陆半咸化湖至咸化湖环境,而不是海相或海陆过渡相环境.参11.     

冲击破煤过程中能量耗散的理论分析

介绍了能量在冲击式破煤过程中的产生、传递和耗散过程以及能量最终的分布范围;运用应力波的方法分析了应力波在煤体中传播过程,并得出能量在衰减过程中衰减率的计算方法;还分析了剥落厚度的计算方法,并得出正弦应力波在煤体中传播时的冲劈厚度和最大煤块尺寸的关系;根据冲击规律和能量的传递特征对能量的传递过程进行了分析,并求出冲击消耗能量和最小散逸能之间的关系,指出了要使煤块破碎必须满足冲击消耗能量要大于最小散逸能。     

煤与生物质共超临界水催化气化制氢的实验研究

在压力为20～25MPa、停留时间为15～30s、：NaOH添加量(质量分数)为0．1％、反应器外壁温度为650℃的条件下，对煤与生物质的模型化合物羧甲基纤维素钠(CMC)在超临界水环境中的催化气化制氢性能进行了研究，探讨了物料浓度、压力以及停留时间对煤与CMC共气化制氢的影响．实验结果表明：煤与CMC二共超临界水催化气化制氢的主要气体产物是H2、CO2和CH4，H2的体积分数可高达60％以上；增加物料浓度、升高压力有利于提高产氢率，但延长停留时间不利于氢气的制取．     

The fate of injectant coal in blast furnaces: The origin of extractable materials of high molecular mass in blast furnace carryover dusts

The aim of the work was to investigate the fate of injectant coal in blast furnaces and the origin of extractable materials in blast furnace carryover dusts. Two sets of samples including injectant coal and the corresponding carryover dusts from a full sized blast furnace and a pilot scale rig have been examined. The samples were extracted using 1-methyl-2-pyrrolidinone (NMP) solvent and the extracts studied by size exclusion chromatography (SEC). The blast furnace carryover dust extracts contained high molecular weight carbonaceous material, of apparent mass corresponding to 10⁷?10⁸ u, by polystyrene calibration. In contrast, the feed coke and char prepared in a wire mesh reactor under high temperature conditions did not give any extractable material. Meanwhile, controlled combustion experiments in a high-pressure wire mesh reactor suggest that the extent of combustion of injectant coal in the blast furnace tuyeres and raceways is limited by time of exposure and very low oxygen concentration. It is thus likely that the extractable, soot-like material in the blast furnace dust originated in tars is released by the injectant coal. Our results suggest that the unburned tars were thermally altered during the upward path within the furnace, giving rise to the formation of heavy molecular weight (soot-like) materials.     

Influence of overpressure on coalbed methane reservoir in south Qinshui basin

In theory, from the high temperature and pressure during the coal generating gas to the present low temperature and pressure of coalbed methane reservoir, the accumulation of coalbed methane was from oversaturated to undersaturated. The gas content of the coalbed methane reservoir in the south Qinshui basin was 12-35.7 m3/t. According to the isotherm and measured gas content of No. 3 coal, the adsorbed gas content in some wells was highly saturated and oversaturated, which was hard to theoretically understand. In addition, there were no thermogenic and biogenic gases at the late stage in the south Qinshui basin. This article proposed that the overpressure was the main reason for the present high saturation of the coalbed methane reservoir. In early Cretaceous, the coalbed methane reservoir was characterized by overpressure and high saturation caused by gas generation from coal measure source rocks. In late Cretaceous, the coalbed methane reservoir was rapidly uplifted, and with the temperature and pressure decreasing, the pressure condition of adsorbed gas changed from overpressure to normal-under pressure, which resulted in the high saturation and gas content in the present coalbed methane reservoir.     

黑龙江省煤炭城市地质灾害及防治对策

论述了黑龙江省煤炭城市地质灾害的类型、成因及危害 ;并针对目前地质灾害现状提出了相应的防治对策 .