Geochemical Techniques to Detect Sources of Fluids in Highly Pressured Casing-Casing Annuli CCA

Dr. Peter Birkle, Hamdi A. AlRamadan
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Abstract

The buildup of high casing-casing annulus (CCA) pressure compromises the well integrity and can lead to serious incidents if left untreated. Potential sources of water causing the elevated CCA pressure are either trapped water in the cement column or water from a constant feeding source. This study utilizes inorganic geochemical techniques to determine the provenance of CCA produced water as trigger for high pressure in newly drilled wells. Affinities in the hydrochemical (major, minor and trace elements) and stable isotopic (δ2H, δ18O) composition are monitored to identify single fluid types, multi-component mixing and secondary fluid alteration processes. As a proof-of-concept, geochemical fingerprints of CCA produced water from three wells were correlated with potential source candidates, i.e., utilized drilling fluids (mud filtrate, supply water) from the target well site, Early - Late Cretaceous aquifers and Late Jurassic - Late Triassic formation waters from adjacent wells and fields. Geochemical affinities of CCA water with groundwater from an Early Cretaceous aquifer postulate the presence one single horizon for active water inflow. Non-reactive elements (Na, Cl) and environmental isotopes (δ2H, δ18O) were found to be most suited tools for fluid identification. 2H/1H and 18O/16O ratios of supply water and mud filtrate are close to global meteoric water composition, whereas formation waters are enriched in 18O. Elevated SO4 and K concentrations and extreme alkaline conditions for CCA water indicates the occurrence of minor secondary alteration processes, such the contact of inflowing groundwater with cement or fluid mixing with minor portions of KCl additives. The presented technology in this study enables the detection of high CCA pressure and fluid leakages sources, thereby allowing workover engineers to plan for potential remedial actions prior to moving the rig to the affected well; hence significantly reducing operational costs. Appropriate remedial solutions can be prompted for safe well abandonment as well as to resume operation at the earliest time.
高压套管-套管环空流体来源的地球化学检测技术
高套管-套管环空(CCA)压力的积累会损害井的完整性,如果不及时处理,可能会导致严重事故。导致CCA压力升高的潜在水源要么是水泥柱中截留的水,要么是来自恒定进料源的水。本研究利用无机地球化学技术确定了CCA采出水的来源,作为新钻井高压的触发因素。通过监测水化学(主要、次要和微量元素)和稳定同位素(δ2H、δ18O)组成的亲和关系,识别单一流体类型、多组分混合和二次流体蚀变过程。作为概念验证,三口井的CCA采出水地球化学指纹与潜在的候选来源(即目标井场的利用钻井液(泥浆滤液、供水)、早-晚白垩世含水层和邻近井和油田的晚侏罗世-晚三叠纪地层水)相关。CCA水与早白垩世含水层地下水的地球化学亲和性假设了活水流入存在单一层位。非活性元素(Na, Cl)和环境同位素(δ2H, δ18O)被认为是最适合的流体识别工具。补给水和泥浆滤液的2H/1H和18O/16O比值接近全球大气水组成,而地层水富集于18O。CCA水体SO4和K浓度的升高和极端碱性条件表明发生了次要蚀变过程,如流入地下水与水泥接触或与少量KCl添加剂混合的流体。本研究中介绍的技术能够检测高CCA压力和流体泄漏源,从而使修井工程师能够在将钻机移至受影响的井之前制定潜在的补救措施;因此大大降低了运营成本。适当的补救措施可以促进安全弃井,并尽早恢复作业。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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