Assessing polyacrylamide solution chemical stability during a polymer flood in the Kalamkas field, Western Kazakhstan

M. Sagyndikov, I. Salimgarayev, E. Ogay, R. Seright, S. Kudaibergenov
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引用次数: 3

Abstract

During a polymer flood, the field operator must be convinced that significant chemical investment is not compromised at the early stages of polymer injection. Further, dissolved oxygen in the viscous polymer solution must be controlled at a safe level, where viscosity loss will be insignificant. Under anaerobic conditions,the hydrolyzed polyacrylamide (HPAM) solution is stable even if iron ions are present in the process water. Thus, in the field operation, introduced oxygen and existing iron ions will cause an enormous viscosity decline. The geochemical calculation reveals that dissolved oxygen can rapidly deplete after entering Kalamkas formation. This paper confirms this prediction through a combination of laboratory measurements and field observations. This study is based on rheology measurements of polymer solutions and produced fluid from the offset production well associated with the Kalamkas oilfield in Western Kazakhstan. Comprehensive analysis confirms no viscosity loss at the surface facilities during polymer preparation and injection at a Pol- ymer Slicing Unit and significant viscosity loss at an Eductor-type unit caused by oxygen introduced during polymer solution preparation. However, even introduced high dissolved oxygen levels that degrade polymer at the surface can be rapidly depleted during contact with the formation, thereby promoting polymer chemical stability in the reservoir.
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评估哈萨克斯坦西部Kalamkas油田聚合物驱过程中聚丙烯酰胺溶液的化学稳定性
在聚合物驱过程中,现场作业人员必须确信,在聚合物注入的早期阶段,大量的化学投资不会受到影响。此外,粘性聚合物溶液中的溶解氧必须控制在安全水平,这样粘度损失就微不足道了。在厌氧条件下,水解聚丙烯酰胺(HPAM)溶液是稳定的,即使铁离子存在于工艺水中。因此,在现场作业中,引入的氧和现有的铁离子会引起粘度的巨大下降。地球化学计算表明,溶解氧进入Kalamkas地层后会迅速耗竭。本文通过实验室测量和野外观测相结合的方法证实了这一预测。该研究基于哈萨克斯坦西部Kalamkas油田邻井的聚合物溶液和采出液的流变学测量。综合分析证实,在聚合物制备和聚合物切片单元注入过程中,表面设施没有粘度损失,而在聚合物溶液制备过程中引入氧气导致的educector型单元粘度损失明显。然而,即使引入了高溶解氧水平,使聚合物在表面降解,也会在与地层接触时迅速耗尽,从而提高了聚合物在储层中的化学稳定性。
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