首页> 外文会议>Indonesian Petroleum Association Annual Convention >ESTIMATION OF FORMATION AND CONDENSED WATER CHEMISTRY FROM WIRELINE FORMATION TESTER AND DST WATER SAMPLES: A CASE STUDY FROM ABADI GAS FIELD
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ESTIMATION OF FORMATION AND CONDENSED WATER CHEMISTRY FROM WIRELINE FORMATION TESTER AND DST WATER SAMPLES: A CASE STUDY FROM ABADI GAS FIELD

机译:从丝网形成测试仪和DST水样中估算形成和冷凝水化学的估算 - Abadi气田的案例研究

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For a gas field development, water chemistry is an important data for wireline logging data interpretation as well as facility designs, i.e. corrosion / scale / hydrate management, facility metallurgy, and sludge / waste water management. Especially for a remote and offshore gas field, it is critical because modifications of the existing facilities are very difficult and sometimes impossible. On the other hand, sampling and analysis of formation and condensed water chemistry is always embarrassed by contamination of drilling fluid filtrate, completion brine and, cement. There are many published studies and various commercialized sampling methods for iriinimizing the filtrate in the water sample. Specific sample preservation and measurement / analysis are also available for many important substances. In Abadi Gas Field, water samples were collected and analyzed in six exploration and appraisal wells by bottom hole sampling using wireline formation tester (WFT) as well as Drill Stem Test (DST) surface sampling. The samples taken by wireline formation tester were contaminated by potassium chloride (KCl) water base mud (WBM), and the samples taken by DSTs were supposed to be mixtures of formation water, condensed water, and KCl WBM. Sodium thiocyanate was used as a tracer in the drilling mud, however it didn't work perfectly as a reliable indicator because the concentrations were inconsistent among those measured at the rig site and those at the on-shore laboratory. This paper shows the original methods of estimating the formation water and condensed water chemistry which exploit the major ions' concentration as a package of contamination indicator as well as the tracer concentration. Lessons learned and future recommendation for water sampling and analysis are also introduced.
机译:对于气田开发,水化学是有线测井数据解释以及设施设计的重要数据,即腐蚀/级/水合物管理,设施冶金和污泥/废水管理。特别是对于遥远和近海气体领域,这是关键的,因为现有设施的修改非常困难,有时是不可能的。另一方面,通过钻井液滤液,完成盐水和水泥污染,形成和凝聚水化学的采样和分析总是令人尴尬的。有许多已发表的研究和各种商业化的采样方法,用于利用水样中的滤液。许多重要物质也可提供具体的样品保存和测量/分析。在Abadi Gas Testa(WFT)以及钻杆试验(DST)表面采样中,收集并分析水样并通过底部孔采样进行了近六个勘探和评估井。通过氯化钾(KCl)水基泥(WBM)污染丝网形成测试仪的样品,并且DSTS的样品应该是地层水,冷凝水和KCl WBM的混合物。硫氰酸钠用作钻井泥浆中的示踪剂,但它并没有作为可靠的指示剂完全起作用,因为浓度在钻机现场测量的那些和在岸上实验室中的浓度不一致。本文介绍了估计地层水和冷凝水化学的原始方法,该化合物利用主要离子'浓度作为污染指示剂的包装以及示踪剂浓度。还介绍了经验教训和对水抽样和分析的建议。

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