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Experimental Study of Aerated Mud Flows under Horizontal Borehole Conditions

机译:水平钻孔条件下充气泥浆流的实验研究

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Extensive aerated mud experiments were performed in a unique field-scale elevated pressure and elevated temperature flow loop (6” × 3.5” annular test section, 73 ft length, horizontal configuration without drillpipe rotation). A view port was installed to observe flow patterns in the test section. Two nuclear densitometers were used to measure steady state mean void fraction. During test runs, the liquid and gas phase flow rates were in the range of 50-250 gal/min and 50-150 scf/min, respectively. For all the test runs, measurements of pressure drop and average liquid holdup over the entire annular section were carried out. The two-phase flow patterns were identified by visual observations through the view port. Stratified and slug flow were the two flow patterns observed over the range of the chosen test matrix. The presence of slug flow does not justify many existing simulation practices, which assume a homogeneous gas-liquid flow. A mechanistic model has been developed for aerated mud hydraulics based on conservation equations and existing twophase pipe flow correlations. An extensive sensitivity analysis is presented to quantify the influence of mud properties and flow parameters on the bottom-hole pressure. Comparisons between the predictions of the model and experimental measurements show a satisfactory agreement. The present model is particularly suitable for the design of underbalanced coiled tubing applications.
机译:在独特的现场规模的升高压力和升高温度的流动环路(6英寸×3.5英寸环形测试段,长度73英尺,水平配置,无需钻杆旋转)下进行了广泛的充气泥浆实验。安装了观察孔,以观察测试部分中的流动模式。使用两个核密度计测量稳态平均空隙率。在测试运行期间,液相和气相流速分别在50-250 gal / min和50-150 scf / min的范围内。对于所有测试运行,都对整个环形截面上的压降和平均液体滞留量进行了测量。通过观察孔通过视觉观察来识别两相流动模式。分层和团状流是在所选测试矩阵范围内观察到的两种流型。团状流的存在并不能证明许多现有的模拟实践是合理的,这些实践假定了均匀的气液流动。基于守恒方程和现有的两相管道流量相关性,开发了一种用于充气泥浆水力学的力学模型。进行了广泛的敏感性分析,以量化泥浆性质和流动参数对井底压力的影响。该模型的预测值与实验测量值之间的比较显示出令人满意的一致性。本模型特别适合于欠平衡连续油管应用的设计。

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