首页> 外文会议>Congreso y Exposición Internacional del Petróleo en México (Memorias Técnicas 2006) >H2S Associated With Heavy Oils in Reservoirs Under Primary Production: Cases of Grimbeek and El Alba Fields in Gulf of San Jorge Basin, Argentina S
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H2S Associated With Heavy Oils in Reservoirs Under Primary Production: Cases of Grimbeek and El Alba Fields in Gulf of San Jorge Basin, Argentina S

机译:初级生产储层中与重油相关的H2S:阿根廷圣豪尔赫盆地海湾Grimbeek和El Alba油田的案例

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Reservoir souring is a well-documented problem that appears normally when seawater is injected into sweet reservoirs during secondary recovery programs (1) In these cases, microbiologic souring by the growth of sulphate-reducing bacteria (SRB) is the most accepted mechanism. In some cases, H2S production is reported from the earliest stages of reservoir development. This phenomenon has been named "geologic souring" (2) because the H2S source is generated in the geological past and it is related to some element within the petroleum basin, but not-related to modern microbiological or geochemical processes. Recently, H2S production has been recorded in El Alba-1 and Grimbeek-1 reservoirs (Manantiales Behr area, San Jorge Basin) where there are no previous reports of sources of H2S. Furthermore, water flooding has not been implemented before the H2S measurement campaing in the field. Thus, the H2S generation mechanism is the main target of this study. Correlations of isotopic chemical analyses and isotopic measurements from gas, waters and oil samples were developed and integrated into the geological and enginnering information. After the interpretation stage, a monitoring plan and some mitigation options were suggested. The H2S measurements, geological data and isotopic signatures do not allow locating the H2S source by thermo-chemical decomposition of sedimentary rocks (e.g. anhydrite), kerogen cracking or petroleum decomposition. Chemical data indicate that the sulphate, soluble in connate water, is the most plausible source of sulphur. Moreover microbiological activity is most likely the mechanism of biochemical reduction, even the reservoir show stressing conditions to bacterial development. According to the results, some biocides combined with H2S-scavenging are recommended to mitigate this production inconvient.
机译:水库变压是一个有据可查的问题,通常是在次级恢复计划期间将海水注入甜水库中时通常出现的问题(1)在这些情况下,由硫酸盐还原细菌(SRB)的生长引起的微生物变酸是最被接受的机制。在某些情况下,据报道从储层开发的最早阶段就开始生产硫化氢。这种现象被称为“地质变质”(2),因为H2S源是在地质历史中产生的,并且与石油盆地中的某些元素有关,但与现代微生物或地球化学过程无关。最近,在El Alba-1和Grimbeek-1水库(圣豪尔赫盆地Manantiales Behr地区)记录了H2S的产生,以前没有关于H2S来源的报道。此外,在野外进行H2S测量之前尚未进行注水。因此,H2S的生成机理是本研究的主要目标。天然气,水和石油样品的同位素化学分析和同位素测量的相关性已开发出来,并整合到了地质和工程信息中。在解释阶段之后,提出了一项监测计划和一些缓解措施。 H2S测量,地质数据和同位素特征不允许通过沉积岩(例如硬石膏)的热化学分解,干酪根裂解或石油分解来定位H2S源。化学数据表明,可溶于天然水中的硫酸盐是最合理的硫源。此外,微生物活性最有可能是生物化学还原的机制,即使储层也显示出对细菌发育的胁迫条件。根据结果​​,建议将某些杀菌剂与H2S清除剂结合使用,以减轻这种不便的产生。

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