干酪根
- 网络kerogen
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硒在干酪根中的两种不同赋存状态:TEM证据
Different occurrence of selenium in kerogen : TEM evidence
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求出各类干酪根在不同的热演化阶段的H/C与R值的回归关系式,并研究了各类干酪根的油气演化界限,讨论了本区的油气勘探前景。
For kerogen at different stages of thermal evolution are given . In addition , the limits of petroliferous evolution of kerogen and explora-tion prospect are discussed .
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Matlab优化工具箱在干酪根成烃动力学参数标定中的应用
Application of MATLAB optimization toolbox in calibration of dynamic parameters of hydrocarbon generation of kerogen
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藻干酪根X射线衍射特征及其与油气生成的关系
X-ray diffraction characteristics of algal kerogen and its relation with the generation of oil and gas
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应用显微FTIR光谱技术原位研究沉积岩中生油母质干酪根
Situ-Study on Generative Kerogen in Sedimentary Rock by FTIR-Microspectrometry Technique
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选用美国尤因塔盆地绿河页岩干酪根、南海干酪根和抚顺煤干酪根作为测定芳香度fa的样品。
The kerogens from Green River oil Shale , from Nanhai and from Fushun coal are selected as testing samples .
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干酪根的差示扫描量热法(DSC)的研究
Differential scanning colorimetry studies on kerogen
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干酪根中无机矿物对DTA热谱的影响
Influence of mineral matter on DTA thermogram of kerogen
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从TGA热分解动力学原理计算干酪根热降解成油地质时间-温度关系的方法
Calculation method of geological time-temperature relation of kerogen thermo-degradation and oil-generation by TGA thermo-degradation kinetics
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基于CAN-BUS的干酪根自动制备控制系统
Research of Kerogen Preparation Control System Based On CAN-BUS
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热分析技术在石油地质中的应用&划分未成熟干酪根类型和预测油气资源的DTG法
An application of thermal-analysis technique in petroleum geology
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干酪根结构中碳分布特征及其与生烃潜力的关系&~(13)CNMRCP/MAS与DD技术的应用
Carbon distribution of kerogen and its relationship to hydrocarbon generation potential ── an application of  ̄( 13 ) c NMR cp / mas and DD techniques
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指出反映轻烃组成的RP受烃源岩沉积环境和干酪根类型影响。
And RP , reflecting composition of light hydrocarbon , would be affected by the depositional environment and kerogen type of source rock .
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南海盆地中生代生物源以浮游生物为主,干酪根为III型,以生气为主。
Biology fountain is mainly plankton that constitutes the source rock of sea-facies in the South China Sea Basin , and kerogen type is III , which mainly generates gas .
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有机质为Ⅲ型干酪根,部分ⅡB型,镜质体反射率Ro主要集中于0.5%~1.1%。
The organic matter belongs to Type-III kerogen , partly to Type-IIB ; the vitrinite reflectance ranges from 0.5 % to 1.1 % .
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通过对加水热模拟实验中藻干酪根X射线衍射(XRD)特征的分析.探讨了其XRD谱图的演化特征、结构参数间的关系及其与油气生成的关系。
This paper presents the X-ray diffraction data of algal kerogen obtained by hydrous pyrolysis and discusses the correlation between the structural parameters of algal kerogen and the evolution of oil and gas .
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利用电子顺磁共振(EPR)技术可以简便地测定沉积有机质中干酪根的自由基。
The free radicals in kerogen of sedimentary organic matter can be easily determined by using the electron paramagnetic resonance ( EPR ) technique .
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高压地层顶部的过渡带可以用声波过渡时间、碳氢化合物指数(PI)、伊利石化程度、干酪根的结构以及镜质体反射率的变化加以确定。
The top of the anomalously pressured transition zone is identified by marked increases in sonic transit time , hydrocarbon production index ( PI ), clay diagenesis , and vitrinite reflectance .
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本文应用X射线衍射法测定干酪根的芳香度,并根据X射线衍射谱图计算干酪根的微晶参数,以研究干酪根的结构。
In this paper , the texture of kerogen is studied , using x-ray diffraction to determine the aromaticity of kerogen . According to the x-ray diffraction spectra , the microcrystalline parameter of the kerogen is calculated .
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Ⅰ型干酪根的活化能分布范围很窄,泥质岩与碳酸盐岩中主要分布于50837~53828cal/mol;
The activation energy distribution of ⅰ type of kerogen ranges narrowly , being 50 837 ~ 53 828 cal / mol for mudstone and carbonate rock ;
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在镜质体反射率Ro演化史和干酪根成烃演化史的基础上分析了烃源岩成烃过程,在部分凹陷新生代以来烃源岩有二次生烃过程。
Analysing generation hydrocarbon process of hydrocarbon source rocks on reflectance of vitrinite evolutional history and caseate generation hydrocarbon history , hydrocarbon source rocks in most of depressions have experienced two oil and gas generation periods .
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在国内Ⅰ、Ⅱ、Ⅲ型干酪根的三组模拟实验资料基础上,经过生烃产物油气配方的摩尔组成计算,应用PR状态方程计算了生烃产物的PVT相图;
Based on three domestic groups of simulation experiment data of kerogen type ⅰ,ⅱ, and ⅲ, and through the calculation of mole composition of hydrocarbon-generation products , pvt phase maps are computed by applying pr state equation ;
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作者选择某些特定化合物代替其同类化合物,以判别干酪根热解-气相色谱(Py-Gc)参数。
In order to determine PY - GC parameters of kerogen , certain compounds are selected to replace the other similar compounds .
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100MPa压力下温度和水对干酪根结构状态影响的实验研究
Experimental study of the influence of temperature and water on the structure state of kerogen at 100 MPa pressure
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根据元素分析、岩石热解(Rock-Eval)的指标,两个层段的干酪根在大类上都属于腐殖型。
According to data of element analysis and Roek-Eval analysis , both kerogens in the two sections belong to humic type .
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火山热液中的高温酸性组分(H2S,SO2,HF和HCl等)以及过渡金属元素可促进干酪根中碳-氧键、碳-硫等键的断裂,对油气生成具有催化作用。
Acidic components with high temperature ( H 2 S , SO 2 , HF , HCl and so on ) and transitional metal elements in the volcanic hydrothermal fluid may promote the bond fission of C-O and C-S in kerogen , and has catalytic action on hydrocarbon generation .
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应用固体13C核磁波谱分析技术,采用自然演化与热压模拟相结合探讨了干酪根热演化过程中碳骨架与官能团的变化规律,提出脂碳是生烃主要贡献者。
Solid 13C nuclear magnetic resonance spectrometer and natural evolution combining with thermocompression simulator are used for analysis of variation of carbon matrix and functional group in the course of kerogen thermal evolution , showing that lipid carbons mainly contribute to the hydrocarbon generation .
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以热解特征判别干酪根类型
A new method for identifying kerogen types based on Pyrolysis Characteristics
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粘土矿物对干酪根热解产物的影响及其作用机理
Effect of clay minerals on kerogen pyrolysis and the reaction mechanism
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爱沙尼亚干酪根催化降解生烃过程及动力学研究
Study on Characteristics and Kinetics of Catalytic Degradation from Estonia Kerogen