深层储层中气体冲洗石油的直接证据:综合流体包裹体分析的启示

IF 2.6 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Organic Geochemistry Pub Date : 2024-05-04 DOI:10.1016/j.orggeochem.2024.104778
Xinzhuo Wei , Keyu Liu , Wenfang Yuan , Peng Yang , Lu Zhou , Jianliang Liu , Haijun Yang , Xiujian Ding
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引用次数: 0

摘要

根据实验室实验和建模,有人提出气冲油是形成某些凝析气藏的基本过程,但这种过程在地下储层中很少有记录。这里,我们报告了在中国西部库车前陆盆地的一个深层储层中发现的一种独特的黄环油包裹体(YROIs),它记录了地下的气冲油过程。研究采用了一整套流体包裹体分析方法,包括流体包裹体岩相学、微测温、荧光光谱学、PVT 建模和分子组成分析,对黄带油包裹体的发生、组成、相态和捕集过程中的 PVT 条件进行了研究。加热时,固态环在 46 ℃ 左右开始熔化,并在高于或等于共生水性内含物的相应均化温度下与液相均化。在室温下测量时,YROI 的荧光光谱峰值在 530 nm 和 550 nm 之间,在 650 nm 附近有一个较高的光谱肩;但在均质化温度下测量时,大多数光谱显示出明显的 "蓝移",且没有 650 nm 的光谱肩。一些带有黄色厚环的 YROI 在室温下显示出 570 纳米和 630 纳米的双光谱峰,在均质化温度下重新测量时,其光谱峰没有变化。通过同步荧光光谱和气相色谱-质谱分析得出的分子组成表明,酪酸环的组成富含多芳香族化合物。PVT建模表明,怡红岩是在高压条件下被困住的,压力超过相应静水压力的50%。怡红岩被解释为是在高温和超压条件下(约110 °C和60兆帕)被困住的,这与早期富蜡油的高强度(湿)气体冲洗有关。当储层油中的轻烃成分被气体部分去除时,富含多芳烃化合物的蜡/树脂成分可能会因物理化学分馏而析出。含蜡/树脂胶体数量不等的异质烃类流体在地表下夹带 "黄环油",这些蜡/树脂胶体随后在室温下凝聚成固体环,附着在油包裹体的内壁上。储层中出现黄色环状油包裹体可能表明在高压下蜡油被气体快速冲刷,其最低均化温度可能接近其捕获温度。
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Direct evidence of gas flushing oil in deep reservoirs: Insight from integrated fluid inclusion analyses

Gas flushing of oil has been proposed as an essential process for forming some condensate gas reservoirs based on laboratory experiments and modeling but such a process has rarely been documented in subsurface reservoirs. Here, we report a unique type of yellow-ringed oil inclusions (YROIs) discovered from a deep reservoir in the Kuqa Foreland Basin, Western China that recorded the gas flushing of oil process in the subsurface. The occurrence, composition, phase state and PVT conditions of YROIs during trapping were investigated using a suite of fluid inclusion analytical methods including fluid inclusion petrography, microthermometry, fluorescence spectroscopy, PVT modeling and molecular composition analysis.

YROIs found in the reservoir are three-phase (solid–liquid-vapor) fluid inclusions at room temperature with solid rings of 2–3 μm thickness and estimated volume percentages varying between 5 % and 15 %. When heated the solid ring starts to melt at around 46 °C and homogenized with the liquid phase at or above their corresponding homogenization temperatures of coeval aqueous inclusions. YROIs have fluorescence spectral peaks between 530 nm and 550 nm and an elevated spectral shoulder around 650 nm when measured at room temperature; but most spectra show a distinct “blue shift” and an absence of the 650 nm shoulder when measured at their homogenization temperatures. Some YROIs with thick yellow rings show dual spectral peaks at 570 nm and 630 nm at room temperature and their spectral peaks do not change when remeasured at their homogenization temperatures. Molecular compositions derived from synchronous fluorescence spectra and GC-MS analysis suggest that the compositions of YROIs are rich in polyaromatic compounds. PVT modeling indicates that YROIs were trapped under high pressure conditions with a pressure exceeding 50 % of the corresponding hydrostatic pressure.

YROIs are interpreted to have been trapped under an elevated temperature and overpressure condition (around 110 °C and 60 MPa) relating to an intensive (wet) gas flushing of an early-charged wax-rich oil. When light hydrocarbon components in the reservoir oil were partially removed by gas, the wax/resin components rich in polyaromatic hydrocarbon compounds may precipitate due to physio-chemical fractionation. YROIs were entrapped in subsurface from a heterogeneous hydrocarbon fluid containing variable amounts of wax/resin colloids, which subsequently coalesce to form solid rings adhering to the inner wall of oil inclusions at room temperature. The presence of yellow-ringed oil inclusions in a reservoir may be indicative of a rapid gas flushing of waxy oil under high pressure, and their minimum homogenization temperature may approximate their trapping temperature.

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来源期刊
Organic Geochemistry
Organic Geochemistry 地学-地球化学与地球物理
CiteScore
5.50
自引率
6.70%
发文量
100
审稿时长
61 days
期刊介绍: Organic Geochemistry serves as the only dedicated medium for the publication of peer-reviewed research on all phases of geochemistry in which organic compounds play a major role. The Editors welcome contributions covering a wide spectrum of subjects in the geosciences broadly based on organic chemistry (including molecular and isotopic geochemistry), and involving geology, biogeochemistry, environmental geochemistry, chemical oceanography and hydrology. The scope of the journal includes research involving petroleum (including natural gas), coal, organic matter in the aqueous environment and recent sediments, organic-rich rocks and soils and the role of organics in the geochemical cycling of the elements. Sedimentological, paleontological and organic petrographic studies will also be considered for publication, provided that they are geochemically oriented. Papers cover the full range of research activities in organic geochemistry, and include comprehensive review articles, technical communications, discussion/reply correspondence and short technical notes. Peer-reviews organised through three Chief Editors and a staff of Associate Editors, are conducted by well known, respected scientists from academia, government and industry. The journal also publishes reviews of books, announcements of important conferences and meetings and other matters of direct interest to the organic geochemical community.
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