Stable Isotope Analysis of Elements in Kerogen 干酪根中各种元素的稳定同位素分析
The method for determination the aromatic degree of kerogen by X-ray diffraction was discussed. 探讨了用X光衍射技术,测定干酪根芳香度的方法。
Kerogen type is mainly humic, and terrestrial higher plants are the petrologen. 干酪根类型以腐殖型为主,成烃母质为陆地高等植物;
We suggest that maturity, kerogen type and secondary alteration all have a strong influence on the3D fluorescence of the oils. 成熟度、母源岩有机质类型与生源、次生改造等多种因素对原油的三维荧光特征有控制作用。
The solvent swelling ratio of the kerogen from Palougou Coal was determined by two methods, and then the oil primary migration was modeled. 用不同方法确定了扒搂沟煤型干酪根的溶胀比,计算模拟了石油的初次运移。
In accordance with the theory of the formation of oil-shale, Kerogen lies very probably in the lamellar gaps. 油母很可能处于各物相之间的层状间隙中,与油母页岩的形成理论相一致。
The Silurian type ⅲ kerogen from the northern and southern margins of the Sichuan Basin and its geological significance 四川盆地南北缘志留纪Ⅲ型干酪根及其地质意义
Kerogen from some source rocks in the third and forth members of the Sahejie Formation in the Linnan Sag, the Bohai Bay Basin have been reported to be sulfur-rich. 渤海湾盆地临南洼陷沙河街组三段&四段暗色页岩和暗色泥岩干酪根中富含有机硫,对这类干酪根的油气生成模式一直未进行深入的研究。
Research of Kerogen Preparation Control System Based On CAN-BUS 基于CAN-BUS的干酪根自动制备控制系统
As their insolubility in organic solvents, long chain fatty acid salts mainly stay with Kerogen and few enter asphaltene fraction. 而长链脂肪酸盐由于难溶,在目前的有机地球化学处理过程中,它们主要和干酪根混在一起,少量的进入沥青质组分中。
A history of heat flow variation of a Cenozoic basin was inversed by using modelling computation of Ng values obtained from the kerogen samples of maturity series. 本文根据新生代盆地内系列成熟度样品的自由基浓度值,利用拟合计算的方法,反演了盆地热流的变化历史;
Natural gas is not only originated from kerogen cracking, but also from oil cracking. 天然气既可来源于干酪根的裂解气,也可来源于原油的裂解气。
Type of kerogen and its characteristic 干酪根类型及其特征
The efficiency of the elimination of such minerals is measured by the ash content of the residual kerogen. 这些无机物的消除程度是用剩余油母质的灰分含量来测定的。
Study on Characteristics and Kinetics of Catalytic Degradation from Estonia Kerogen 爱沙尼亚干酪根催化降解生烃过程及动力学研究
The element composition and mature of kerogen is an important distinguish mark between great and small scale carlintype gold deposits. 干酪根的元素组成和成熟度是判别大型卡林型金矿床和小型卡林型金矿床或矿点的重要标志。
This separation step is rather lengthy and cannot always be achieved, due to a high residual content of pyrite in the kerogen. 由于油母质中黄铁矿的剩余含量较高,这个分离过程相当长,而且总是不能达到。
The free radicals in kerogen of sedimentary organic matter can be easily determined by using the electron paramagnetic resonance ( EPR) technique. 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。
Kerogen analyses, however, require preliminary isolation of the kerogen by hydrochloric and hydrofluoric destruction of the inorganic minerals. 但是,油母岩分析需要使用盐酸和氢氟酸破坏无机物以便初步分离出油母岩。
Tectonic activities and volcanism in the basin have an influence on hydrocarbon generation of kerogen and its change. 盆地构造活动和火山作用可以促进干酪根的成烃转化。
The other is normal mature crude oil from the thermal degradation of kerogen. 另一种是正常的干酪根热降解成熟原油。
In the diagenesis, kerogen can not produce oils, so immature oils derive directly from the soluble lipids. 在成岩作用阶段,干酪根不产烃,未成熟石油来自可溶类脂物的直接降解成烃作用;
In this paper the hydrogen isotope compositions of methane, crude as well as light oils and kerogen and their relationship with the depositional environments and the maturity of source rocks were discussed in detail. 本文详细讨论了天然气中甲烷、原油、轻质油及干酪根的稳定氢同位素组成,以及它们与源岩沉积时的水介质环境和源岩成熟度的关系。
And the hydrocarbon-generating products by kerogen type ⅲ are all gas phase. 而Ⅲ型干酪根的生烃产物均表现为气相型。
Influence of tectonic activity and volcanism on hydrocarbon generation of kerogen 构造活动和火山作用对干酪根成烃转化的影响
The kinetics of organic matter generating hydrocarbon which based on the composition and structure of kerogen and chemical kinetics. 有机质成烃动力学是定量评价烃源岩生烃潜力的重要研究方法之一,它是建立在干酪根的组成结构和化学反应动力学基础之上的。
Through the thermal simulation experiment of crude oil and kerogen, the thermal evolution process and the end reaction of hydrocarbon thermal cracking are discussed in this paper. 本文通过原油和干酪根的热模拟实验,探讨了热演化过程及烃类裂解的最终反应。
Generation of hydrocarbon from kerogen is one of important genetic types of abnormal pressure in source rock. 干酪根热解成烃作用是烃源岩中异常高压的重要成因之一。
Whole rock analysis and kerogen analysis are two analytical methods of studying hydrocarbon source rock in organic petrology. 全岩分析与干酪根分析是有机岩石学研究烃源岩的两种分析方法。
This paper mainly describes design and implementation of Kerogen automatic preparation instrument, which is extraction instrument. 本论文讲述了干酪根自动制备仪控制系统的设计和实现。干酪根自动制备仪是一种物质提取设备。