绥滨断陷渗出沥青体特征及成因

煤中的渗出沥青体(exsudatlnite)是1974年Teichmüller通过荧光显微镜研究命名的.是一种比较新的煤岩组分,一般认为渗出沥青体在一些生烃性能较佳的烟煤中出现.作者在研究绥滨断陷顺发勘探区煤岩特征时发现了这种新的煤岩组分.文中描述了所发现的渗出沥青体的光学特征并进行成因分析,最后结合其它方面研究进一步阐述了发现渗出沥青体的地质意义.     

源岩平均活化能影响因素浅析

对源岩平均活化能的影响因素进行了讨论。结果表明 :源岩中可溶有机质对源岩平均活化能有较大影响 ;可溶有机质的存在可以掩盖各种显微组分与平均活化能之间的关系 ;源岩中的粘土矿物的含量与平均活化能大小也有密切的相关性 ;另外 ,源岩中的有机硫含量与平均活化能呈一定的负相关关系     

40kg试验焦炉在预测焦炭质量中的应用

介绍了煤岩学的基本观点以及利用煤岩学预测焦炭质量的几种方法,阐述了40kg试验焦炉的主要参数,分析和比较了不同炉型试验焦炉的优缺点,探讨了利用40kg试验焦炉预测焦炭质量的原理.     

全岩显微组分统计方法及应用

本文对实验室全岩显微组分统计方法及应用进行了讨论。提出全岩有机质类型和丰度评价标准,能有效地评价烃源岩的优劣,并可划分出全岩有机质类型。与干酪根镜检方法相比较,具有明显的优越性,能提供更丰富的信息,而且分析速度快、节省成本、直观。     

淮北煤田任楼煤矿煤的不同显微组分热解特征

为了给任楼煤矿煤的分级利用提供理论指导,在显微组分分离的基础上,进行了各显微组分热解实验。结果表明:随着热解温度的升高,3种显微组分在400～570℃均出现明显的失重现象,壳质组在400℃左右开始热解,失重速率峰温约为450℃,失重率大;镜质组和惰质组在420℃开始热解,失重峰温约为475℃。壳质组在整个热解过程中失重率为39%,平均最大热解速率为0.95 mg/(g·min);镜质组失重率为32.5%,平均最大热解速率为0.53 mg/(g·min);惰质组失重率为29.5%,平均最大热解速率为0.49 mg/(g·min)。     

东欢坨煤矿煤层赋存一氧化碳机理

煤的吸附量与煤层的工业分析、显微煤岩分析、元素分析之间有一定的关系。根据实验室分析的东欢坨煤矿的数据资料，进而建立各个要素与吸附量之间的数学模型，只要能够准确测定煤层的工业分析、元素分析数据，就可以利用这种已建立的关系计算煤层中吸附的一氧化碳量。     

Experimental study and evaluation on hydrocarbon generation of macerals

Some typical coal and maceral samples are selected for oil and gas-generating systematic thermal simulation experiments, Rock-Eval, GC and GC-MS analyses. Results cause productivity curves of extracts and gaseous, light, liquid as well as total hydrocarbon. Effects of macerals and maturation on hydrocarbon productivities and compositions are synthetically discussed. Evaluation indexes and plan on coal-generated oil and gas in bituminous coal rank are suggested according to the data from experiments and analyses.     

Laser-induced fluorescence of macerals in relation to its hydrogen richness

On the basis of results from conventional elemental analyses and a unique technique (FAMM®; fluorescence alteration of multiple macerals), using a laser fluorescence microprobe, the fluorescence characteristics of various macerals are systematically related to hydrogen content. The amount of fluorescence from inertinite and vitrinite exponentially increases with HIC values. Although liptinite has high fluorescence and high HIC values, the relationship does not follow the same trend as defined for the other maceral groups. Because petroleum yields of a maceral mainly depend upon hydrogen richness, a correlation also exists between fluorescence, and gas to oil ratios from pyrolysis. Because individual organic entities are measured, the laser fluorescence microprobe has the benefit of accommodating heterogeneous organic matter in source rocks and enables determination of oil and gas yields of specific macerals.