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A SIMULTANEOUS DETERMINATION OF PERMEABILITY AND KLINKENBERG COEFFICIENT FROM AN UNSTEADY-STATE PULSE-DECAY EXPERIMENT

机译:同时测定不稳态脉冲衰减实验的渗透性和克隆贝格系数

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The unsteady state gas flow experiment is an appealing technique to determine the intrinsic permeability k1 and Klinkenberg gas slippage factor b of tight rock samples. "Pulse-Decay" and "Draw-Down" techniques consist in recording the pressure difference ΔP(t) at the core plug edges when a pulse of higher pressure initially applied at the inlet of the sample, relaxes through the core. The interpretation of the pressure-decay signal represents a challenge for a reliable estimation of k1 and b. On the basis of a previous analysis where the optimal experimental conditions were defined, the objective of this paper is to present an inverse technique that makes use of a complete model of interpretation. To begin with, we recall the classical method of interpretation based on a simplified model proposed in the literature. To circumvent some of the difficulties inherent to this method, we show how an inverse technique, based on the minimization algorithm of Levenberg - Marquardt (1963), can be used along with a complete flow model to perform the estimation of kl and b. Uncertainties on experimental parameters such as the volume of the upstream reservoir, dimensional characteristics of the sample and porosity of the material are introduced, the impact of which on the precision of the estimated values of k1 and b is evaluated. For the sake of clarity and to carefully analyze each parameter independently, the method is illustrated on synthetic signals.
机译:不稳定的状态气体流实验是一种吸引力的技术,用于确定紧密岩石样品的内在渗透性K1和Klinkenberg气体滑动因子B. “脉冲衰减”和“绘制”技术包括在最初在样品入口处施加的较高压力的脉冲时记录芯塞边缘处的压力差ΔP(t),以通过芯放松。压力衰减信号的解释代表了K1和B可靠估计的挑战。在定义最佳实验条件的先前分析的基础上,本文的目的是呈现一种逆技术,这是利用完整的解释模型。首先,我们回顾基于文献中提出的简化模型的古典解释方法。为了规避该方法固有的一些困难,我们展示了基于Levenberg - Marquardt(1963)的最小化算法的逆技术如何与完整的流模型一起使用以执行KL和B的估计。引入了诸如上游贮存器的体积,样品的尺寸特性和材料的孔隙率的实验参数的不确定性,评估其估计值的估计值的精度的影响。为清楚起见并独立分析每个参数,在合成信号上示出了该方法。

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