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In-Situ Viscosity from Acoustic Logging

机译:原位粘度来自声学测井

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摘要

This work contributes to a concept proposal for obtaining pore fluid viscosity and formation permeability from thermoacoustic measurements (i.e., conducting acoustic logging of pore fluid mobility at different temperature conditions in the wellbore). The acoustic method for mobility estimation from Stoneley wave attenuation and dispersion is widely used in the industry. Currently, nearly all wireline measurements are performed at static thermodynamic conditions in the wellbore. But what happens if thermodynamic conditions are changed and logs are run at different temperature conditions at a given depth? In this case, the measurements of the pore fluid mobility at different temperatures allow obtaining additional information on the pore fluid viscosity and improve the accuracy of permeability estimation by the acoustic method. This work includes experimental and modeling verification of the suggested thermoacoustic method. The experiments were on laboratory core samples; finite-difference poro-visco-elastic code was used for the modeling. The applicability of the method is shown to be dependent on the temperature difference of the formation, accuracy of the Stoneley wave dispersion and attenuation measurements, and the in-situ wellbore pore fluid viscosity, temperature, and pore pressure.
机译:这项工作有助于获得热声测量的孔隙流体粘度和形成渗透性的概念提案(即,在井筒的不同温度条件下进行孔隙流体迁移率的声学测井)。 STONELEY波衰减和分散的移动性估计的声学方法广泛应用于该行业。目前,几乎所有有线测量都在井筒的静态热力学条件下进行。但是,如果改变热力学条件,并且在给定深度的不同温度条件下运行日志会发生什么?在这种情况下,在不同温度下的孔流体迁移率的测量允许获得关于孔隙流体粘度的附加信息,并通过声学方法提高渗透率估计的准确性。这项工作包括建议热声方法的实验和建模验证。实验在实验室核心样本上;有限差异的Poro-Visco-Elastic代码用于建模。该方法的适用性显示为取决于地层的温度差,Stoneley波形分散和衰减测量的精度,以及原位井眼孔隙流体粘度,温度和孔隙压力。

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