蜡灭低温捕集成藏新机理

Yunyan Gan, Li Chen, Jinqing Zhang, O. Mullins, Zhenghe Yan, Ji Tian, Xiaofei Gao, Weihua Chen, Haizhang Yang, J. Hao
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引用次数: 0

摘要

在南中国海,大约一半的生产油田含有一种奇怪而神秘的石油。首先,这些含蜡原油几乎不含溶解气体,气泡点只有几个大气压。地层从未被抬升到非常浅的深度,以便脱气到那么低的溶解气。其次,这些原油也缺乏其他较轻的烷烃成分,最高可达C12,无论如何,这些烷烃都不能通过德加工艺去除。这些原油也不能被比C12重的正构烷烃完全生物降解,所以在这个过程中没有去除较轻的正构烷烃。从成熟度的角度来看,这些原油也没有可靠的解释。这类储层流体早已为人所知,但对其形成机理却一直不甚了解。针对这些储层流体性质,相应盆地的含油气系统建模并不准确;因此,在盆地建模和对石油的了解方面都存在很大的不确定性。本文首次介绍了一种新发现的储层形成机制,以解释这些看似不一致的流体性质。这种新机制的核心是“蜡除冷捕获”。当运移中的原油在运移路径上遇到其蜡样温度(WAT)时,蜡会从原油中结晶出来,形成大面积的局部蜡沉积,并伴有相关的被困液体。它确实被温度困住了。可移动的脱蜡流体相可以继续向上运移,要么被困在单独的常规储层中,要么通过渗漏渗漏。在持续下沉后,持有固体蜡的地层可以加热到WAT以上,从而使这些以前冻结的油重新活化。然后,这种蜡质油可以继续运移,可能沿着沉降改变的运移路径。然后,这些蜡质油可以填满与迁移路径相关的圈闭,并一直被圈闭到今天。脱蜡低温捕集过程起到了组分分馏器的作用,将初始含蜡油在空间上分离为轻质液体和气态组分,其中一部分为含蜡和闭塞的较重液体,另一部分为含蜡和闭塞的较重液体。原油在运移过程中经历气相演化的相变是常规的,但在这种情况下,两相同时运移。在脱蜡捕集过程中,由于固体蜡和脱蜡流体相的迁移率不同,存在一种空间分离的固液相转变。本文综述了南海蜡质“零gor”原油的分布及烃源岩特征。它描述了一种系统的方法来识别脱蜡过程并排除其他可能性。该分析综合了许多流体性质,包括PVT、GC、GOR、WAT和热成熟度,以及盆地模拟的油气运移和地层埋藏历史。对这一过程的认识为认识不同流体的成因及其在盆地内的分布打开了一扇新的窗口,为油气系统建模提供了时间约束和生烃运移指导。当烃源岩中的含蜡油沿着温度低于WAT温度的路径运移时,就会发生蜡灭低温圈闭。这一过程在南中国海非常普遍,对于全球高含蜡量油田来说,这一过程也应该是普遍的。但直到现在,这个新机制才被发现。实践证明,该模型具有创新性,为盆地建模引入了一种新的运移模式,最终为油田勘探提供了重要指导。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A Novel Reservoir Forming Mechanism with Wax-Out Cryo Trapping
In South China Sea, about one half of the producing oilfields contain a type of strange and enigmatic oil. First, these waxy crude oils contain almost no solution gas, with bubble points of few atmospheres only. The formation has never been uplifted to very shallow depths to be degassed to that low-level of solution gas. Second, these crude oils also lack of other lighter alkane components up to C12, which, in any event, cannot be removed by a degas process. These crude oils are also not biodegraded with the full complement of n-alkanes heavier than C12, so the lighter n-alkanes have not been removed by this process. There is no credible explanation of these crude oils from maturity considerations either. This kind of reservoir fluid has long been known, however, has not been understood in terms its mechanism of formation. Petroleum system modeling in corresponding basins has not been accurate with regard to these reservoir fluid properties; thereby yielding significant uncertainty in both basin modeling and understanding the oil. This paper introduces a newly identified reservoir forming mechanism, for the first time, to account for these seemingly discordant fluid properties. Central to this new mechanism is "Wax-Out Cryo Trapping". When a crude oil in migration encounters its Wax Appearance Temperature (WAT) along the migration path, the wax can crystallize out of the oil yielding a large, localized wax deposit with associated trapped liquids. It is indeed trapped by the temperature. The mobile, dewaxed fluid phase can continue in migration up either becoming trapped in a separate conventional reservoir or lost via a seep. After continued subsidence, the formation holding the solid wax can heat above WAT thereby remobilizing this formerly frozen oil. This waxy oil can then proceed in migration, possibly along a migration path altered by subsidence. This waxy oil can then fill traps associated with the migration path and remain trapped until present day. The Wax-Out Cryo Trapping process is acting as a compositional fractionator spatially separating the initial waxy oil into its light liquid and gas fractions in one fraction and its waxy and occluded heavier liquids in the other fraction. It is routine to have crude oils undergo the phase transition of gas evolution in migration, but in that case, both phases migrate together. In the Wax-Out Cryo Trapping, there is a solid liquid phase transition with spatial separation based on very different mobilities of solid wax and the dewaxed fluid phase. The paper summarizes the distribution of the waxy "zero-GOR" crude oil in South China Sea and the source rock characteristics. It describes a systematic approach to identify the wax-out process and to rule out other possibilities. This analysis integrated many fluid properties, including PVT, GC, GOR, WAT, and thermal maturity, with hydrocarbon migration and formation bury history from basin modeling. The understanding of this process opens a new window to understand origin of the different fluids and their distribution within the basin, providing the time constraints and guidance for hydrocarbon generation and migration in petroleum system modeling. Wax-Out Cryo Trapping can happen when waxy oil from source rock migrates along paths with temperatures lower than the WAT temperature. This process is shown to be very common in the South China Sea, and it should also be somewhat common globally for the high wax content oilfields. But it is until now, this new mechanism just got discovered. It is proved to be an innovated model, introduce a new migration pattern for basin modeling and eventually provides the important guidance for oilfield exploration.
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