黄骅坳陷石炭-二叠系凝析油气地球化学特征及来源分析     

徐进军  李宁  金强  刘吉华  楼达  滕建成 《吉林大学学报(地球科学版)》2020,50(2):644-652

深层油气勘探是未来油气资源的重要接替领域。渤海湾盆地下伏石炭-二叠系煤系烃源岩自油气勘探取得新突破以来,一直是深层油气领域研究的热点。黄骅坳陷新部署的QG8井奥陶系碳酸盐岩储层和YG1井二叠系砂岩储层获高产凝析油气流,其来源判别问题是深层油气勘探的关键。针对QG8、YG1井凝析油气开展的生物标志化合物、有机碳稳定同位素和原油物性研究表明：两口井的凝析油均为低黏度、低密度的典型轻质原油,具有姥鲛烷优势（Pr/Ph>2.8）,QG8井凝析油饱和烃δ¹³C为-29.1‰、芳烃δ¹³C为-26.8‰;天然气δ¹³C₁偏重,介于-39.7‰~-36.4‰之间,干燥系数大于0.8,重烃可达16.2%,为偏干湿气。QG8与YG1井凝析油特征与黄骅坳陷石炭-二叠系煤系烃源岩（饱和烃δ¹³C为-29.26‰~-26.87‰,芳烃δ¹³C为-26.62‰~-24.15‰）及KG4井原油物性（0.757 1~0.840 2 g/cm³）相近,天然气特征则相似于济阳坳陷GBG1井的煤成气（δ¹³C₁为-43‰~-35‰）,表明高产的凝析油气来自石炭-二叠系煤系烃源岩。证实渤海湾盆地深层石炭-二叠系煤系具有生烃潜力和油气勘探前景。  相似文献   

石油碳、氢同位素组成的研究   总被引：12，自引：1，他引：11  

沈平  徐永昌 《沉积学报》1998,16(4):124-127

通过对我国18个含油气区、385个石油样品进行碳、氢同位素和部分馏份碳同位素分析,将所获数据对两种不同性质的石油如正常原油和轻质（凝析）油分别研究其碳、氢同位素地球化学特征,提出轻质（凝析）油的碳同位素值（δ13C为-32.5‰～ -24.3‰）比正常原油δ13C为-34.4‰～ -24.6 ‰．6‰）相对偏高;石油馏份中芳烃碳同位素组成的变化受母质继承效应更为明显。因此,用芳烃碳同位值可以判识不同母质来源的石油。与海相有关的轻质（凝析）油的氢同位素值大于-15.0‰,而非海相轻质（凝析）油的δD值( δD为-21.0‰～-1.05‰）基本覆盖了海相轻质油的分布范围,从淡水－微咸水－半咸水和海水环境其氢同位素有明显变重趋势,表明氢同位素主要与沉积环境密切相关。  相似文献   

东海平湖油气田中高渗凝析气藏开发效果分析   总被引：1，自引：0，他引：1  

蒲庆南  夏欣  赵天沛 《海洋地质译丛》2008,(1):36-40

东海平湖油气田放鹤亭始新统平湖组气藏,属中高渗砂岩中低凝析油含量凝析气藏,1999年3月投入生产,采用衰竭式开采,至今已有8个年头,目前仍处于开发稳产阶段,日生产天然气量在140×10^4m^3左右。通过对平湖油气田凝析气藏开发生产状况跟踪研究发现,其采气速度高、主力气藏气井无水采气期普遍较长、气油比随着压力下降而上升、凝析油含量随着压力下降而下降、天然气采收率将优于开发方案设计值,同时也发现,防止气井出水、出砂是中高渗凝析气藏开发中应予以高度重视的问题。平湖油气田凝析气藏开发,在技术上和经济上都取得了较好的效果,可以借鉴于类似凝析气田的开发实践中。  相似文献   

红台凝析气田合理产能研究     

仓辉 《海洋地质译丛》2008,(2):95-100

气井合理产能是凝析气藏开发的一项重要指标，关系到气藏的开发水平和经济效益。在深入分析红台凝析气田开采特征的基础上，运用最小携液产气量、一点法、类比法、数值模拟法等多种方法开展气藏合理产能研究。首次给出适合红台凝析气田的一点法计算公式，论证红台凝析气田合理产能为1.0×10^8m^3。  相似文献   

叶城凹陷柯东1井凝析油及柯克亚原油的油源分析     

王强  ;彭平安  ;曾建  ;邹艳荣  ;于赤灵  ;张宝收  ;肖中尧 《地球化学》2014,(5):469-476

塔里木盆地叶城凹陷拥有多套烃源岩层,主要为石炭系卡拉乌依组、二叠系棋盘组与普司格组2-3段、侏罗系煤系地层与叶尔羌群等,这些烃源岩都可能是柯东1井凝析油和柯克亚第三系原油的母源。在这一地区,油源一直是一个很具争议性的问题。选取了叶城凹陷克里阳构造带柯东1井2个凝析油、柯克亚构造带7个第三系原油,以及叶城凹陷各烃源岩层具有代表性的17个烃源岩样品,对其生物标志物及正构烷烃单体烃稳定碳同位素比值等参数进行了详细的测试分析。油油对比揭示,柯东1井原油与柯克亚第三系原油在正构烷烃组分、成熟度与稳定碳同位素组成等特征上具有明显的相似性,显示同源的特征。油源对比显示,普司格组2-3段下部是这些原油的源岩。这一烃源岩层具有与柯克亚地区原油一致的成熟度和相似的特征性生物标志物,即高含量的重排藿烷、Ts和 C27-C29重排甾烷等,而其他烃源岩层则不具备这类特征。较高成熟阶段形成的原油,解释了普司格组2-3段烃源岩可溶有机质与柯东1井等原油在单体烃稳定碳同位素比值上具有2‰~3‰的差别。  相似文献   

Alkyl Naphthalenes and Phenanthrenes: Molecular Markers for Tracing Filling Pathways of Light Oil and Condensate Reservoirs   总被引：1，自引：0，他引：1  

LI Meijun  WANG Tieguan  LIU Ju  ZHANG Meizhu  LU Hong  MA Qinglin  GAO Lihui 《《地质学报》英文版》2010,84(5):1294-1305

<正>Condensates and light oils are generally characterized by high maturity,low concentration of sterane and terpane biomarkers and low content of non-hydrocarbon fraction.As a result,some commonly-used sterane,terpane and carbazole migration parameters in conventional oil reservoirs may have a certain limitation in condensate and light oil reservoirs for their poor signal-noise ratios in the gas chromatography-mass spectrometry(GC-MS).Naphthalene,phenanthrene and their methylated substituents,however,are present in significant concentrations in condensates and light oils.Taking the Fushan depression(in the Beibuwan Basin,Northern South China Sea) as an example, this paper attempts for the first time to use polycyclic aromatic hydrocarbon(PAH)-related parameters to trace migration directions and filling pathways for condensate and light oil reservoirs.The result shows that TMNr(i.e.1,3,7-TMN/(1,3,7-TMN + 1,2,5-TMN),TMN:trimethylnaphthalene)),MPI-1 (i.e.1.5×(2-MP + 3-MP)/(P + 1-MP + 9-MP),P:phenanthrene MP:methylphenanthrene),MN/DMN (Σmethylnaphthalene/Σdimethylnaphthalene,%) and MN/TMN(Σmethylnaphthalene/Σtrimethylnaphthalene, %) can be used to trace the filling pathways of condensate and light oil reservoirs.These parameters,together with geological consideration and other bulk oil properties(e.g.the gas to oil ratio and density),suggest that the condensates and light oils in the Huachang oil and gas field are mainly sourced from the Bailian sag that is located to the northeast of the Huachang uplift in the Fushan depression.  相似文献   

全球大型凝析气田的分布特征及其形成主控因素   总被引：4，自引：0，他引：4       下载免费PDF全文

杨德彬  朱光有  刘家军  苏劲  张斌  费安国 《地学前缘》2010,17(1):339

随着勘探的不断深入,越来越多的凝析气藏被发现,并受到重视。目前全球共发现106个大型凝析气田,分布于全球70多个沉积盆地。凝析气田主要分布于西西伯利亚盆地、滨里海盆地、波斯湾盆地、扎格罗斯盆地、美国墨西哥湾及塔里木盆地等。通过对全球各大凝析气田进行系统的研究,发现凝析气藏主要分布在石炭系—新近系储层中,以构造圈闭为主,储集体物性较差,属于低孔低渗型,凝析气和凝析油的密度均相对较低。凝析气田的形成和展布主要受控于有效烃源岩分布、有利的储盖组合、圈闭类型、晚期成藏、特殊的温压系统和烃类体系组分等条件。根据其成因机理,将凝析气藏分为原生凝析气藏和次生凝析气藏。  相似文献   

Effects of entrapped residual air bubbles on tracer transport in heterogeneous soil: Magnetic resonance imaging study   总被引：1，自引：0，他引：1  

Vladimira Jelinkova  Michal SnehotaAndreas Pohlmeier  Dagmar van DusschotenMilena Cislerova 《Organic Geochemistry》2011,42(8):991-998

Magnetic resonance imaging (MRI) was used to study the process of infiltration and solute transport in an undisturbed soil sample of coarse sandy loam. The sample was subjected to the recurrent ponded infiltration (RPI) experiment, which was carried out in order to assess the changes in the entrapped air volume and its impact on steady state flow rates and solute breakthrough. The main stages of the first and second experimental RPI runs were monitored using an MRI sequence that follows both water density and magnetic relaxation. In a steady state stage of each experimental run a nickel nitrate pulse was injected in order to visualize the solute breakthrough. Effluent from the sample was collected for chemical analysis and a breakthrough curve of the nickel was constructed. To obtain information about the soil structure and to reveal potential preferential pathways, the soil sample was scanned using computed tomography. The local nickel ion transport breakthrough was evaluated from MR images in a series of local observation points distributed along the selected preferential pathways.The preferential flow instability phenomenon with the emphasis on air bubble formation was shown by detecting a 60% decrease of the steady state infiltration rate. The detailed analyses of MRI measurements at observation points revealed air bubble formation, producing a flow rate decrease accompanied by redirection of nickel ion transport trajectories. By analyzing M0 maps it was found that the volumetric water content decrease was 2.2%.  相似文献   

沙坡头地区地形对凝结水形成特征的影响   总被引：3，自引：1，他引：2  

潘颜霞  王新平  张亚峰  虎瑞 《中国沙漠》2014,34(1):118-124

以沙坡头地区经草方格沙障固定的典型流动沙丘作为研究对象,采用PVC管手动称重法和布板法（CPM—Cloth-Plate Method）对该区不同地形位置凝结水的形成特征进行了研究。结果表明：地形作用下凝结水的形成量和形成间期均表现为中等空间异质性;不同坡向凝结水形成量符合经典的水汽对流模型,丘间低地凝结水形成量最高,迎风坡凝结水形成量高于背风坡,具体表现为：丘间低地>西面向坡>北面向坡>丘顶>南面向坡>东面向坡;同一坡向不同坡位处凝结水形成量表现为：坡脚>坡中>坡顶;坡度与凝结水形成量呈负的线性相关关系,随着坡度的增加,凝结水形成量逐渐减少,垂直坡面上凝结水形成量仅为水平面的一半。这说明地形是影响干旱区凝结水形成特征的重要因子。  相似文献   

Experiments of methane gas solubility in formation water under high temperature and high pressure and their geological significance     

J. Ma  Z. Huang 《Australian Journal of Earth Sciences》2017,64(3):335-342

The solubility of methane in formation water and water content in the coexisting gas phase were measured under the conditions of high temperature and high pressure, using an ultra-high-pressure fluid PVT system, where the experimental temperature reached up to 453 K and pressure reached up to 130 MPa. Experimental results show the following (1) The two phases of gas and liquid still exhibit an obvious interphase interface even under high temperatures and pressures. (2) When temperatures exceed 353 K, the solubility of methane in formation water increases as the temperature and pressure rise. The growth rate of solubility is faster under a relatively low temperature and pressure, and slower at a relatively high temperature and pressure, but the solubility will not increase without limit. In this experiment, the solubility of methane in formation water reached its peak when the temperature was at 453 K and the pressure at 130 MPa. (3) Water content in the coexisting gas phase increases as temperature rises, with a smaller increase at relatively low temperatures and a much greater increase at relatively high temperatures but decreases with the increasing pressure, more rapidly under low pressure and more slowly under high pressure. The solubility of methane in formation water and the water content in the coexisting gas phase are controlled by both temperature and pressure, but using classic calculation models, these two parameters under high temperatures and pressures are inconsistent with our experimental data. Therefore, the study is significant and highlights other possible effects on solubility and condensate water content. Additionally, an example from the Yinggehai Basin in the South China Sea, where the temperature and the pressure are high, demonstrates the influence of solubility and phase behaviour on natural gas migration, its formation and the distribution of gas reservoirs.  相似文献