高密度Mn3O4/ BaSO4基修井液在碳酸盐岩储层中的损害机理

Nouf H. Alotaibi, Awoye Lawson-Jack, K. Smith, Salako Olaoluwa, Gonzalo Chinea
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摘要

本文的目的是评估由于分散在修井液中的固体(高密度Mn3O4和BaSO4加重材料)和其他颗粒的影响,对碳酸盐多孔介质造成的地层损害机制。重晶石(BaSO4)和四氧化锰(Mn3O4)均为高密度化合物(4.5 ~ 4.8 g/cm3),粒径分别约为50微米和5微米(μm),可显著影响固体侵入的渗透率。利用地层损害实验室模拟器采集选定的岩心样品,直至油藏条件。首先,在岩心驱替之前,对储层岩心桥塞进行了XRD/XRF和基线CT扫描。在使用修井液之前和之后以及去除由修井液形成的滤饼之后,在控制流量的情况下,在氮气驱期间测量了岩心样品的压差。达西方程用于计算渗透率值,岩心桥塞CT扫描用于解释相关的地层损害机制。该研究表明,多孔介质中存在的固体物性堵塞流体通道,以及由于流体高度过滤而形成的较厚的外部滤饼,是导致岩心塞样上观察到的回渗透率降低的主要机制。与外部滤饼相比,内部滤饼与滤液和固体颗粒渗透到孔隙中对观察到的渗透率降低有更大的影响。滤饼的特性在很大程度上受泥浆颗粒类型、粒度和浓度的控制。与重晶石滤饼(BaSO4)滤饼与相同岩石类型的相互作用相比,四氧化锰(Mn3O4)基的修井液滤饼与碳酸盐岩样品表面的组合具有低渗透率,导致更大的压降和更低的产能。滤饼的渗透性随滤度的降低而降低。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Damage Mechanism of High-Density Mn3O4/ BaSO4 Based Workover Fluids in Carbonate Reservoirs
The objective of this paper is to evaluate the formation damage mechanisms on carbonate porous media due to the effect of solids (high-density Mn3O4 and BaSO4 weighting materials) and other particles dispersed in workover fluids. Barite (BaSO4) and Manganese Tetroxide (Mn3O4) are both highly dense compounds (4.5 – 4.8 g/cm3) with particle size of approximately 50 and 5 microns (μm) respectively, which can significantly impact permeability due to solids invasion. A formation damage lab simulator was utilized to take selected core samples up to reservoir conditions. Initially, XRD/XRF and a baseline CT scan of the reservoir core plugs were conducted prior to core flooding. Differential pressures along core samples were measured at controlled flowrates during nitrogen gas flooding carried out before and after the workover fluid application and also, after removal of the filter cake formed by the workover fluid. Darcy's equation was used to calculate permeability values, and core plug CT scans post-floods were used to assist with the interpretation of the associated formation damage mechanism. This study shows that the presence of solids inside the porous media physically plugging fluid pathways and a thick external filter cake due to high fluid filtration are the main mechanisms that contributed to the reduced return permeability observed on the core plug samples. The internal filter cake associated with the penetration of filtrate and solid particles into the pores had a greater effect on the observed permeability reduction compared to that of the external filter cake. The characteristics of the filter cake is strongly controlled by the mud particle type, size, and concentration. The combination of Manganese Tetroxide (Mn3O4) based workover fluid filter cake and the carbonate rock sample's face had low permeability causing a larger pressure drop and a lower productivity compared to the Barite (BaSO4) based filter cake in interaction with the same rock type. The permeability of the filter cake was lowered with decreased filtration.
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