Liquid Flow Patterns and Particle Settling Velocity in a Taylor-Couette Cell Using Particle Image Velocimetry and Particle Tracking Velocimetry

SPE Journal Pub Date : 2024-02-01 DOI:10.2118/219459-pa
Andres F. Velez, D. Kalaga, Masahiro Kawaji
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Abstract

Controlling the downhole pressure is an important parameter for successful and safe drilling operations. Several types of weighting agents (i.e., high-density particles), traditionally barite particles, are added to maintain the desired density of the drilling fluid (DF). The DF density is an important design parameter for preventing multiple drilling complications. These issues are caused by the settling of the dense particles, an undesired phenomenon also referred to as sagging. Therefore, there is a need to understand the settling characteristics of heavy particles in such scenarios. To this end, simultaneous measurements of liquid phase flow patterns and particle settling velocities have been conducted in a Taylor-Couette (TC) cell with a rotating inner cylinder and stationary outer cylinder separated by an annular gap of 9.0 mm. Liquid flow patterns and particle settling velocities have been measured using particle image velocimetry (PIV) and particle tracking velocimetry (PTV) techniques, respectively. Experiments have been performed by varying the rotational speed of the inner cylinder up to 200 rev/min, which is used in normal drilling operations. Spherical particles with diameters of 3.0 mm or 4.0 mm and densities between 1.2 g/cm3 and 3.95 g/cm3 were used. The liquid phases studied included deionized (DI) water and mineral oil, which are the basic components of a non-Newtonian DF with a shear-thinning viscosity. The DF is a mud-like emulsion of opaque appearance, which impedes the ability to observe the liquid flow field and particle settling in the TC cell. To address this issue, a solution of carboxymethyl cellulose (CMC) with a 6% weight concentration in DI water was used. This non-Newtonian solution displays shear-thinning rheological behavior and was used as a transparent alternative to the opaque DF. For water, PIV results have shown wavy vortex flow (WVF) to turbulent Taylor vortex flow (TTVF), which agrees with the flow patterns reported in the literature. For mineral oil, circular Couette flow (CCF) was observed at up to 100 rev/min and vortex formation at 200 rev/min. For CMC, no vortex formation was observed up to 200 rev/min, only CCF. The settling velocities for all particles in water matched with the particle settling velocities predicted using the Basset-Boussinesq-Oseen (BBO) equation of motion. For mineral oil and CMC, the results did not match well with the predicted settling velocities, especially for heavy particles due possibly to the radial particle migration and interactions with the outer cylinder wall.
使用粒子图像测速仪和粒子跟踪测速仪测量泰勒-库埃特样品池中的液体流动模式和粒子沉降速度
控制井下压力是成功和安全钻井作业的一个重要参数。为了保持钻井液(DF)的理想密度,需要添加多种类型的加重剂(即高密度颗粒),传统上使用重晶石颗粒。钻井液密度是防止出现多种钻井问题的重要设计参数。这些问题都是由高密度颗粒的沉降引起的,这种不希望出现的现象也被称为下沉。因此,有必要了解重颗粒在这种情况下的沉降特性。为此,我们在一个泰勒-库埃特(TC)样品池中同时测量了液相流动模式和颗粒沉降速度,该样品池由一个旋转的内圆筒和静止的外圆筒组成,两者之间有一个 9.0 毫米的环形间隙。液体流动模式和颗粒沉降速度分别采用颗粒图像测速仪(PIV)和颗粒跟踪测速仪(PTV)技术进行测量。实验中改变了内筒的转速,最高达 200 转/分,这在正常钻孔操作中是常用的。使用的球形颗粒直径为 3.0 毫米或 4.0 毫米,密度介于 1.2 克/立方厘米和 3.95 克/立方厘米之间。研究的液相包括去离子水和矿物油,它们是具有剪切稀化粘度的非牛顿 DF 的基本成分。DF 是一种外观不透明的泥状乳液,妨碍了观察 TC 小室中的液体流场和颗粒沉降。为了解决这个问题,我们使用了重量浓度为 6% 的羧甲基纤维素 (CMC) 在去离子水中的溶液。这种非牛顿溶液具有剪切稀化流变特性,被用作不透明 DF 的透明替代品。对于水,PIV 结果显示出波状涡流(WVF)到湍流泰勒涡流(TTVF),这与文献中报道的流动模式一致。对于矿物油,在最高 100 转/分钟时观察到环形库埃特流 (CCF),在 200 转/分钟时观察到涡流形成。对于 CMC,在 200 转/分钟以下没有观察到涡流形成,只有 CCF。所有颗粒在水中的沉降速度与使用 Basset-Boussinesq-Oseen (BBO) 运动方程预测的颗粒沉降速度一致。对于矿物油和 CMC,结果与预测的沉降速度不太吻合,尤其是重颗粒,这可能是由于颗粒的径向迁移以及与外筒壁的相互作用。
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