油页岩半焦燃烧动力学研究

燃烧动力学是研究油页岩半焦颗粒燃烧特性的基础。利用热重分析仪对油页岩半焦进行了恒温燃烧实验研究,在排除外扩散影响的基础上,分析了燃烧温度、氧气浓度对油页岩半焦燃烧过程的影响。在实验范围内,氧气浓度和燃烧温度均能对油页岩半焦燃烧速率产生重要影响,更高的氧气浓度和燃烧温度可以加快油页岩半焦燃烧速率。结合实验结果,建立了考虑氧气浓度影响的油页岩半焦燃烧动力学模型,发现油页岩半焦燃烧速率与氧气浓度的0.97次方呈线性关系。模型计算结果与实验结果符合较好,为进一步研究油页岩半焦大颗粒燃烧特性提供了燃烧动力学基础。     

Pyrolysis kinetics for Green River oil shale from the saline zone

The nature of the organic and mineral reactions during the pyrolysis of Saline-zone Colorado oil shale containing large amounts of nahcolite and dawsonite has been determined. Results reported include a material-balanced Fischer assay and measurements of gas evolution rate of CH₄, C₂H_x, H₂, CO and CO₂, Stoichiometry and kinetics of the organic pyrolysis reactions are similar to oil shale from the Mahogany zone. X-ray diffraction and thermogravimetric analysis results are used to help determine the characteristics of the mineral reactions. Kinetic expressions are reported for dawsonite decomposition, and it is demonstrated that the temperature of dolomite decomposition is substantially lower than for Mahogany-zone shale because of the presence of the sodium minerals.     

油页岩过热蒸汽的干燥动力学

以油页岩颗粒作为干燥物料,以过热蒸汽和热空气分别作为干燥介质,进行了油页岩干燥实验的研究。当颗粒粒径减小时,油页岩干燥速率越大;过热蒸汽和热空气温度增大时,干燥速率也越大。对比相同条件下过热蒸汽和热空气干燥油页岩的平均干燥速率,发现当干燥介质温度超过逆转点温度时,过热蒸汽条件下的平均干燥速率大于热空气下的数值。实验得出粒径分别为9,7,5 mm的油页岩颗粒逆转点温度值分别是154,179,177℃;逆转点温度值是个变量,随颗粒粒径大小变化而变化。颗粒粒径越大时逆转点温度值越小,粒径较小时逆转点变化不大。采用薄层干燥模型对油页岩的干燥数据进行动力学模拟,可得修正Page模型(Ⅱ)干基水分比w模拟值与实验值的最大绝对偏差是12%,综合比较发现修正Page模型(Ⅱ)能较好地描述油页岩在过热蒸汽条件下的干燥过程。     

Organic geochemistry of the British Kimmeridge Clay: 1. Composition of shale oils produced from Kimmeridge sediments

A series of shale oils produced by Fischer assay of Upper Jurassic Kimmeridgian oil shales, claystones and cementstones from on-shore Britain has been analysed. Oil yields are related to lithology via the quantity of sedimentary organic matter present in each lithologic unit, and also to stratigraphic horizon for certain rich, laterally uniform and persistent units. Shale oils are dark and sulphurous, containing < 50% hydrocarbons. NSO compounds are relatively important in the chromatographically separable fractions, while aliphatic hydrocarbons are usually subordinate. Unimodal normal alkane distributions maximize around nC16, while bimodal distributions have a secondary maximum around nC29. Many alkane gas chromatograms are characterized by a prominent peak due to the nC23 alkane. Certain compositional features are of pyrolytic origin (aromatics, heterocompounds, alkenes), while others are determined by the organic sedimentary input (alkane distributions, prominent nC23 alkane). Broad similarity in geochemical parameters suggests a consistency in the composition of sedimented organic matter. Smaller-scale compositional variations are thought to result from minor fluctuations in the composition of the organic sedimentary input, for example changes in the amount of terrestrial organic detritus reaching the depocentre. Results suggest a dominantly algal or bacterial organic matter source continuously operative throughout much of the Upper Jurassic over the entire region, with a smaller, more variable magnitude contribution from terrestrial sources, probably deposited in a near-shore marine shelf-sea environment under anoxic conditions.     

Organic geochemistry of the British Kimmeridge clay: 2. Acyclic isoprenoid alkanes in Kimmeridge shale oils

The C15---C20 isoprenoid alkane composition of Kimmeridge Clay shale oils produced by Fischer assay has been examined, and compared with the isoprenoid composition of corresponding bitumens. C16 and C18 isoprenoid alkanes are generally dominant in shale oils, while pristane (C19) and phytane (C20) dominate in bitumens. A significant proportion of the phytane in many shale oils is derived from simple evaporation of free (bitumen) phytane, while free pristane contributes less to shale oil composition. Some shale oil phytane and a large proportion of pristane is kerogen-derived. Certain shale oils contain lower concentrations of isoprenoid alkanes than corresponding bitumens, suggesting that some free alkane is thermally degraded during pyrolysis. Results thus indicate three sources for shale oil isoprenoid alkanes: thermal evaporation of free alkanes (particularly for phytane), kerogen decomposition, and possibly the cracking of higher homologues for C15---C19 alkanes. Kerogen-derived isoprenoids are suggested to arise by thermal desorption of adsorbed free alkane (particularly for phytane) and from C---O and C---C bonded species (excluding phytane) via postulated clay catalysed hydrogenation of initially formed alkenes. Comparison of shale oil and bitumen pristane/phytane ratios allows groups of oil shales to be defined, dependent on source composition, organic carbon content and maturity. Shale oil pristane/phytane ratios can also help to determine depositional environments and source composition, although maturity, shale mineralogy and competing alkene-forming pyrolytic reactions may also affect the ratios.     

美国绿河油页岩中沥青热解特征及动力学

沥青是油页岩中的重要有机质,也是油页岩中油母质热解产油和气过程的重要中间产物,对其热解研究有利于加深油页岩/油母质热解理解。通过索氏萃取提取出了绿河油页岩中的沥青,并对其进行了不同升温速率下热解实验。基于热重（TGA）数据,使用Friedman法计算了沥青热解的活化能,并通过活化能分布特征,推测沥青热解可能包含三个过程。接着,使用双高斯函数对含有交叠峰的DTG曲线进行反褶积处理,分解成三个峰,依次对应每一个过程。使用最小二乘法获得了这三个过程的活化能、指前因子和反应模型通式,并将获得的通式与四类固态物质热解模型中的11种理想模型进行对比,辨识出上述三个过程均遵循n级反应模型。     

煤、油页岩和石油焦混烧特性及其动力学

为了充分利用劣质燃料油页岩和难以利用的高硫石油焦,以煤、劣质燃料油页岩及高硫燃料石油焦的混合燃料为研究对象,采用热重-差热的试验方法和差减微分法,对其混烧特性曲线和混烧特性机理进行分析,计算出试样各种燃烧特性参数及燃烧动力学参数。结果表明:煤、油页岩、石油焦的质量比为1∶6∶3的混烧试样S7的DTG曲线先后出现挥发分的析出着火燃烧峰和剩余固定碳的着火燃烧峰;煤、油页岩、石油焦的质量比为6∶3∶1的混烧试样S4的可燃特性指数及着火特性指数均大于油页岩及石油焦的值,而且混合试样的燃尽指数均大于煤及石油焦的值,同时,混合样品的综合燃烧特性指数均大于油页岩的值;试样S4的活化能最小,该混合试样的燃烧反应最容易进行。只要煤、油页岩及石油焦混合比例适当,其混合燃烧特性将优于油页岩及石油焦单独的燃烧特性。     

Kinetics of oil generation from oil shale from Liaoning province of China

The intrinsic kinetics of oil generation from 0.124 dm³ kg^?1 Chinese oil shale were determined by a non-isothermal method. Overall first-order kinetics satisfactorily represented the mechanism of kerogen decomposition. The kinetic parameters were determined as 142.8 kJ mol^?1 and 7.495 × 10⁶ s^?1 for activation energy and pre-exponential factor, respectively.     

基于气固流态化原理的油页岩干燥动力学

为了考察气固流化床干燥器能否使油页岩含水质量分数达到要求,以柳树河油页岩颗粒为原料,研究进口气体温度和颗粒直径对油页岩干燥性能的影响,采用薄层干燥模型,对油页岩干燥实验数据进行模拟,确定油页岩干燥方程和干燥速率方程,建立油页岩干燥速率特征常数和有效扩散系数之间的关联式。研究结果表明:薄层干燥模型中修正Page模型Ⅰ适合描述油页岩的干燥过程;油页岩在流化床内干燥过程主要发生在降速干燥阶段,进口气体温度越高,油页岩颗粒直径越小,所需干燥时间越短,进口气体温度为350℃时,使2.4 mm油页岩含水质量分数低于5%,所需干燥时间为2.5 min。     

Composition and kinetics of oil generation from non-isothermal oil shale retorting

Oil shale retorting has been carried out under non-isothermal conditions between 623 and 773 K and at different pressures(78 and 765 kPa). The shale oil is separated into five individual components: polar, weak polar, saturates, aromatics and olefin, using a comprehensive analytical procedure. The effects of retorting pressure and heating rate have been studied. The oil yield under high pressure (765 kPa) is ≈10% less than the oil yield under ambient pressure (78 kPa). Much of this reduced yield can be accounted for by the reduced amount of polar component formed at high pressure. Heating rates of 1.67 × 10^?2, 6.67 × 10^?2and 8.33 × 10^?2Ks^?1 have been used; a higher heating rate causes a delay in the appearance of the oil. A simplified kinetic scheme is proposed which includes the distribution of liquid products and pressure effects. The activation energies and frequency factors of generation reactions for total oil and individual components have been obtained.     

Detailed kinetic analysis of oil shale pyrolysis TGA data

There are significant resources of oil shale in the western United States, which if exploited in an environmentally responsible manner would provide secure access to transportation fuels. Understanding the kinetics of kerogen decomposition to oil is critical to designing a viable process. A dataset of thermogravimetric analysis (TGA) of the Green River oil shale is provided and two distinct data analysis approaches—advanced isoconversional method and parameter fitting are used to analyze the data. Activation energy distributions with conversion calculated using the isoconversional method (along with uncertainties) ranged between 93 and 245 kJ/mol. Root mean square errors between the model and experimental data were the lowest for the isoconversional method, but the distributed reactivity models also produced reasonable results. When using parameter fitting approaches, a number of models produce similar results making model choice difficult. Advanced isoconversional method is better in this regard, but maybe applicable to a limited number of reaction pathways. © 2011 American Institute of Chemical Engineers AIChE J, 2012     

Thermal degradation of shale oils: 1. Kinetics of vapour phase oil degradation

As vertical modified in-situ retorts (VMIS) have been scaled up and tested, the overall oil yield has declined and is generally lower than that observed in an above-ground process. This reduced oil yield could adversely affect the economics of VMIS retorting. Diminished yields are attributed to a combination of factors associated with scale-up such as in complete rubblization, wide particle size distributions (large blocks of shale), and poor flow distributions. Additionally, oil losses can occur by comparatively long exposure of the oil vapours to high temperatures, by exposure to successive condensation and revaporization of the oil as it travels down the retort, and finally by long time thermal exposure of the condensed oil retained in the bottom portion of large VMIS retorts. To study such vapour phase degradation of shale oil using oil produced from Occidental Petroleum's No. 6 VMIS retort, a tubular continuous flow reactor, with an on-line gas chromatograph for gas composition monitoring was used to study thermal degradation of shale oil under retorting conditions. Oil and a combination of gases including steam were metered into the preheater and then the vapours passed into a quartz tubular reactor where the temperature and residence time of the gaseous mixture were controlled. Complete mass balances were performed giving the weight fraction of oil converted to noncondensable hydrocarbon gases and coke. This experimental design is novel because high temperature thermal degradation of shale oil was studied for the first time under steady state flow conditions with carefully controlled residence time and temperature. A range of temperatures (425–625 °C) and residence times (2–10 s) were used in a series of factorial-designed experiments (3²) to accurately determine the effects of these variables. Results of the study showed that the addition of steam to the carrier gas did not reduce oil degradation losses but did react with the coke thereby changing the product gas composition and quantity. A first-order oil degradation rate expression was used to model the rate of oil loss. The calculated activation energy was 17.3 kcal mol^?1. Chemical analyses of the product liquids and gases confirmed previously reported findings that the oil loss indices (alkene/alkane, ethylene/ethane, naphthalene/(C₁₁ + C₁₂), and gas/coke) increase with increasing oil degradation.     

汪清油页岩燃烧反应动力学研究

采用Pyris-1TGA热重分析仪测定汪清油页岩不同升温速率(20,50,80,100℃/min)下的一组燃烧TG曲线,根据Popescu提出的一种新的多重扫描法,将不同机理函数式进行线性回归。结果表明,该油页岩燃烧反应符合三维扩散机理,从而确定了该油页岩机理函数的积分式与微分式,获得了活化能与频率因子的值。取转化率为0.1,0.2,…,0.9,将冉全印-叶素温度积分近似式与所求机理函数结合,利用迭代法求出转化率-温度的理论值。结果发现,理论TG曲线与实验曲线吻合较好,表明了所求得的油页岩燃烧机理函数的合理性。     

油页岩热解特性及其甲烷释放规律研究

为研究油页岩热解特性及热解过程中甲烷的释放规律,采用热重-傅里叶变换红外光谱（TG-FTIR）对龙口（LK）、内蒙（NM）、汪清（WQ）三个地区的典型油页岩进行热解实验,并结合固相红外（FTIR）对油页岩的官能团结构进行分析。研究结果表明,油页岩热解过程可分为四个阶段,热解反应及挥发分释放主要发生在第二阶段（400～600℃）。甲烷的析出与油页岩结构中的脂肪烃（光谱范围3000～2800 cm^-1）密切相关,脂肪烃含量越多,热解过程中释放的甲烷越多。通过对甲烷析出曲线分峰拟合及结合动力学分析,得出甲烷的生成是由一个脱吸附过程和四个化学反应共同作用的结果。     

中国油页岩开发利用现状及发展前景

简单介绍了油页岩的用途及中国油页岩开发利用的历史,总结了油页岩的干馏工艺技术和开发利用现状,展望了油页岩的发展前景。     

油页岩热解的FG-DVC模型

为研究油页岩结构与热解反应性之间的关系,在TG-FTIR分析仪上对甘肃油页岩在不同升温速率条件下（5、20、50℃·min^-1）进行了热解实验研究,对CH₄、CO、CO₂、H₂O和页岩油进行了定量分析,并采用非线性最小二乘拟合方法求解各组分析出的动力学参数,同时采用基于燃料化学结构的FG-DVC模型对各组分的析出过程进行了模拟。结果表明：油页岩的脱挥发分过程主要发生在200～600℃之间;油页岩中有机质所含官能团以脂肪烃为主;由于各官能团活性不同,导致气态产物的析出有先后顺序;由非线性最小二乘拟合方法获得的各种产物析出的活化能E分布在188～239 kJ·mol^-1之间,而指前因子A在10⁹～10¹³ s^-1之间;各产物的FG-DVC模拟结果与实验数据较为相符,这说明用FG-DVC模型来描述甘肃油页岩的热解脱挥发分过程是比较合适的。     

油页岩半焦燃烧反应活性分析

采用美国Perk in E lm er公司生产的Pyris1 TGA热重分析仪,对桦甸油页岩半焦进行燃烧特性试验研究,得到3种不同升温速率下的油页岩半焦燃烧特性曲线,并使用平均质量反应性指数和燃烧稳定性指数对半焦反应性加以评价。油页岩半焦燃烧分燃烧快速段、过渡段和燃烧慢速段3个阶段进行。随着升温速率的提高,在燃烧快速段,表观活化能为133.901 3—100.204 2 kJ/mol;在燃烧慢速段,表观活化能为146.317 1—211.409 3 kJ/mol。利用Coats-Redfern法确定了燃烧快速段反应级数为3,而燃烧慢速段则为5.5,从而得到油页岩半焦燃烧化学反应的动力学参数,为油页岩半焦的有效开发与经济利用提供了理论依据。     

程序升温下页岩油泥热解机理

采用热重分析仪,进行了桦甸和汪清页岩油泥在不同升温速率（5 ℃/min,10 ℃/min,20 ℃/min,40 ℃/min）下热失重实验,并通过瓦斯气析出情况研究页岩油泥热解机理。结果表明,页岩油泥热解分为3个阶段：第一阶段（20～180 ℃）为水分和轻质组分析出;第二阶段（180～360 ℃）重质组分稳定析出,是动力学研究的重点;第三阶段（360～600 ℃）为半焦炭化及矿物质失重过程。研究发现,催化剂K2CO3能有效降低油泥热解温度及其残渣率,而Al2O3对油泥热解催化不明显甚至起抑制作用。在页岩油泥热解过程中,生成的有机大分子侧链发生C—C键断链,生成小分子的烷烃和不饱和烃,在低压高温条件下,其断链位置倾向于碳链端部,使得小分子烃含量较多。     

Kinetics of decomposition of CaCo3 in an Australian oil shale

The kinetics of decomposition of calcium carbonate in an Australian (Julia Creek) oil shale were measured because the extent of the carbonate decomposition affects the energy balance for combustors burning either raw or spent shale. The apparent activation energy was similar to that previously reported for the decomposition of calcium carbonate in Colorado oil shale but the Julia Creek shale had rate constants which were smaller than those reported for the Colorado shale.     

油页岩地下转化工艺技术

当前对油页岩的利用存在成本高和对环境污染大的问题。Shell公司研发的油页岩地下转化工艺技术,通过现场试验具有成本低、对环境污染小和效率高的特点,具有极大的商业推广价值。