平煤十矿底板巷穿层钻孔瓦斯抽采模拟研究

为了降低平煤十矿己15-16-24130工作面运输巷掘进中的突出危险性,基于实际工程背景,考虑瓦斯抽采中的瓦斯运移及煤岩变形等因素,建立了瓦斯抽采气固耦合模型,并利用COMSOL Multiphysics软件对平煤十矿己15-16煤层的底板巷穿层钻孔瓦斯抽采方案进行数值模拟,研究了瓦斯抽采对于降低掘进过程中突出危险性的影响。研究结果表明:在己18煤层开挖底板巷对己15-16煤层进行穿层钻孔瓦斯抽采,瓦斯抽采180 d后,己15-16-24130工作面运输巷附近煤层残余瓦斯压力及瓦斯含量分别降至0.315 MPa和3.84 m3/t;将底板巷穿层钻孔瓦斯抽采方案进行工程应用,实测抽采后的残余瓦斯压力及瓦斯含量在0.32 MPa和3.17 m3/t,均小于平煤十矿煤与瓦斯突出防治规定的“双6”指标（残余瓦斯压力小于0.6 MPa,残余瓦斯含量小于6 m3/t）,可有效降低运输巷掘进过程中的突出危险性。     

煤与瓦斯共采在错层位巷道布置中的机理研究及应用构想

为了完善现有煤与瓦斯共采技术,创新煤与瓦斯共采方法,对错层位巷道布置下的煤与瓦斯共采系统展开研究,利用相似模拟试验,分析错层位巷道布置覆岩运动情况,预测其开采围岩裂隙发育和瓦斯运移形式,提出了创新煤与瓦斯共采技术构想。研究结果表明:采空区覆岩三带高度随接续工作面的增加而增大,相邻采空区垮落矸石压实区呈现“O-L-O”形变化,多个相邻采空区覆岩出现大“O”形圈裂隙带;相邻采空区内瓦斯可实现相互运移,大“O”形圈裂隙带内赋存大量瓦斯气体;研究提出了地面钻井抽采瓦斯、走向高位瓦斯抽采巷和外错尾巷穿层钻孔3种煤与瓦斯共采技术,比传统巷道布置情况下的煤与瓦斯共采技术在安全、经济等方面更具优势。     

不同煤层煤氧化自燃性实验分析

为研究不同煤层煤自然发火特征的异同性及规律,以淮南矿区1号、3号、6号、13号煤层为研究对象,通过自然发火实验,对不同煤层煤的自然发火期周期、煤样70℃时放热强度和R70值进行分析。研究结果表明:4个不同煤层煤样自燃性由强到弱依次为:3煤>6煤>1煤>13煤;变质程度相近的4个煤层,3煤自然发火期最短,这与煤体中硫分和水分含量高有关;13煤变质程度较高,且前期放热强度、耗氧速率增长缓慢,其自燃性较弱;4个不同煤层煤的耗氧速率、CO,CO2产生率,以及C2H4/C2H6值随煤温升高具有相似的变化规律;煤中CH4气体大量解吸出现于煤温60℃之前,煤中灰分在80~120℃开始逐渐吸热融化,解析和融化均会抑制煤氧接触并且减小煤氧反应放热总量。     

水平管内不同煤质煤尘爆炸火焰传播特性实验研究

为研究水平管道空间不同煤质煤尘爆炸火焰传播特性,选取褐煤、长焰煤、不粘煤、气煤4种煤尘,对爆炸火焰焰峰特性、火焰加速传播特性、火焰传播距离与持续时间展开研究。研究结果表明:褐煤在500 ms内焰峰的形状由尖锐向平滑再向钝化不断演变,长焰煤与不粘煤在375 ms时焰峰前端出现明显焰体分离现象,分析认为这与管体冷壁效应、空间尺度效应及空间氧气消耗直接相关;气煤在375 ms时焰峰出现大面积火焰碎纹,说明气煤爆炸火焰猛烈传播的持续时间相对较短,整体爆炸强度相对较弱;褐煤与长焰煤爆炸火焰存在2次间断性加速,分析认为这与管体空间受限、常温管壁散热、局部助燃氧气瞬间不足等因素有关;褐煤在爆炸后400～600 ms内火焰2次加速完全,火焰传播距离达740 mm,明显大于长焰煤、不粘煤与气煤,说明低变质褐煤爆炸火焰持续时间更长,火焰传播距离更远且传播更剧烈;虽然气煤火焰最远传播距离比长焰煤大30 mm,但由于气煤火焰在375 ms左右出现大片火焰碎纹,因此气煤整体的爆炸强度小于长焰煤。     

pH对煤泥水絮凝沉降的影响

选择聚合氯化铝(PAC)/阴离子型聚丙烯酰胺(PHP)、氯化钙(CaCl2)/非离子型聚丙烯酰胺(NPAM)组合与NPAM、PHP、两性离子型聚丙烯酰胺(ZPAM)作为絮凝剂,在对道清选煤厂水采筛下原生煤泥和浮选尾矿的煤泥水进行组合药剂絮凝实验的基础上,考察了pH对煤泥水絮凝沉降的影响。实验结果表明,在不同的pH下,煤泥水的絮凝效果不同:在酸性条件下,宜单独使用有机高分子絮凝剂;在中性至碱性条件下,无机凝聚剂和有机絮凝剂联合使用效果较好。     

干法煤粉磁选脱硫的试验研究

本工作首次在国内完成了干法煤粉磁选脱硫的试验,探讨了脱硫机理,简述了磁法脱硫的工艺及高梯度磁分离器(HGMS)装置。试验结果表明:最佳梯度磁场强度为0.65—0.75T,最佳煤粉颗粒度在100目—120目,脱硫率最高达70％左右,费用估计为7.5元/t煤左右。     

Fingerprinting of Gasoline and Coal Tar NAPL Volatile Hydrocarbons Dissolved in Groundwater

Accidental spills and chronic leaks of fuel oil or other hydrocarbon material (e.g., coal tar) often result in subsurface accumulation of nonaqueous phase liquid (NAPL), which can be a subsequent source of contamination in groundwater. Linking hydrocarbons in groundwater to a source NAPL has been difficult when using standard target analytes (e.g., BTEX) because of differences in partitioning properties of the analytes between the source NAPL and groundwater. Because aqueous solubility is predicted to be the controlling influence in the partitioning of hydrocarbons from NAPL to groundwater, a solubility-based approach to matching dissolved hydrocarbons in groundwater to their source NAPL has been developed and validated for two sites with commonly encountered types of NAPL contamination. Specifically, a gasoline LNAPL and a coal tar DNAPL from two separate sites (West Virginia and California) and groundwater interfaced with these NAPLs were analyzed for approximately 50 gasoline-range hydrocarbons consisting of paraffin, isoparaffin, (mono-) aromatic, naphthene, and olefin compounds (PIANO). Solubility characteristics of selected alkyl aromatic hydrocarbons from the PIANO analysis were used to identify a set of diagnostic hydrocarbons, expressed as hydrocarbon ratios, which were found to be useful in distinguishing the source(s) of hydrocarbons in groundwater. At the West Virginia site, the diagnostic ratios in a downgradient groundwater sample were similar to those of a gasoline NAPL at that site, indicating the source of hydrocarbons to the groundwater was the upgradient gasoline NAPL. The diagnostic ratios of the groundwater in contact with the gasoline NAPL and the remote groundwater were also similar, providing evidence that the diagnostic ratios were retained during transport in the aquifer. At the California site, diagnostic ratios in a cross-gradient groundwater sample differed from those of the coal tar NAPL at that site, indicating that the remote groundwater hydrocarbons did not originate from the coal tar contamination. Environmental factors such as selective degradation of specific isomers and various geological conditions (e.g., soil mineralogy, and organic content) may confound the application of this solubility-based fingerprinting approach. Thus, it is recommended that multiple diagnostic pairs be simultaneously evaluated when considering this fingerprinting approach for specific sites and product types.     

臭氧氧化—包埋菌流化床生物处理组合工艺深度处理煤气化废水

采用臭氧氧化—包埋菌流化床生物处理组合工艺对煤气化废水进行深度处理。实验结果表明：当臭氧的质量浓度20 mg/L、臭氧进气流量1.5 L/min、臭氧通气时间30 min、包埋菌流化床水力停留时间24 h时,臭氧氧化工序的COD去除率达到30.0%~40.0%,总酚去除率达到100.0%;包埋菌流化床工序的COD去除率达到60.0%以上,氨氮的去除率大于95.0%;经组合工艺处理后,出水COD<60 mg/L,ρ（氨氮）<1.0 mg/L,ρ（总酚）未检出,色度小于50倍,达到GB8978—1996《污水综合排放标准》中的一级排放标准。     

采煤塌陷地积水对土壤氮素矿化过程的影响

煤炭开采导致大面积的土地塌陷,使大量耕地出现常年积水或季节性积水,对塌陷地土壤氮素矿化过程产生一定影响。采集了某矿采煤塌陷地土壤样品,进行好气和淹水培养条件下间歇淋洗培养实验,研究了塌陷地积水对土壤氮素矿化过程的影响。经过62d的培养,40d左右氮素的矿化过程趋于稳定,淹水培养条件下土壤氮素最终累积矿化量为68.99mg/kg,约为好气培养条件的10倍,且淹水培养条件下土壤氮素矿化势可达69.472mg/kg,均矿化速率为5.210mg/(kg·d),说明淹水对土壤氮素矿化过程有显著的促进作用。将实验所得累积矿化量分别代入简单指数模型及双因子指数模型进行拟合,发现简单指数模型能有效模拟好气和淹水培养条件下土壤氮素矿化过程,并获得了2种培养条件下土壤氮素矿化过程的模型参数。     

PRB强化垂直流人工湿地系统处理煤矿废水

针对常规人工湿地系统处理高浊含氮磷的有机煤矿废水不佳的问题,采用PRB与人工湿地耦合的方法,进行砂箱模拟实验研究。实验结果表明,由无烟煤、钢渣及沸石构建的PRB强化垂直流人工湿地系统对NH4+-N、PO34--P、Mn2+、COD、SS的去除率分别达到88.84%、96.08%、98.98%、85.78%和94.00%,与常规人工湿地相比,具有处理效率高、水力负荷大、占地面积小等特点,更便于运行管理。