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New Method to Estimate Damaged Formation Permeability With Well Testing

机译:估计损坏形成渗透率的新方法

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Most composite solutions used in modern well test interpretation use the "step-permeability" model where the altered formations are divided into two or more concentric zones, each with constant permeability. Depending on the causes of alteration or variation, this model can deviate significantly from the real condition. A formation can be altered because of stress redistribution, drilling damage, solids co-production, mineral precipitates, and drilling mud invasion, each factor more likely to generate spatially-varying permeabilities rather than constant k zones. Experimental data confirm that a continuous permeability model is more realistic than the step permeability model. A new semi-analytical solution with smooth radius-dependent permeability has been developed to analyze well test results from such altered formations. The altered formation is approximated as a concentric two-zone composite model: an exterior intact zone that retains the original unaltered permeability, and an interior zone where the permeability values have been altered and change as a function of radius. The permeability in this near-well zone can change continuously to the original permeability or to a different value at the boundary with the exterior zone, where there is a step-change in permeability. The choice of an increase or decrease of permeability with radius within the altered zone depends on the nature of the actual alteration. The permeability can also be simulated as a step-wise function if appropriate parameters are used; in such situations, the model collapses to conventional step-wise composite models. Other parameters such as formation porosity and compressibility of each zone can also be different, but they are assumed constant for this derivation. The new solution is derived in Laplace space, and numerical Laplace inversion is used.
机译:在现代测试解释中使用的大多数复合溶液使用,当改变的地层被分成两个或更多个同心区域,各个孔的“级渗透性”模型一起使用,每个模型具有恒定的渗透性。根据改变或变化的原因,该模型可以从真实情况下偏离。由于应力再分布,钻孔损伤,固体共同生产,矿物沉淀物和钻井泥侵入,钻孔损伤和钻井泥侵入的形成,每个因素更可能产生空间不同的渗透率而不是恒定的k区。实验数据证实,连续渗透性模型比步进渗透性模型更加真实。已经开发出一种具有平滑半径依赖性渗透性的新的半分析解决方案,以分析来自这种改变的地层的良好测试结果。改变的形成近似为同心双区复合模型:保留原始未改变的渗透率的外部完整区域,以及作为半径的函数改变和变化的内部区域。在该近孔区域中的渗透率可以连续变为原始渗透性或与外部区域的边界处的不同值,在那里存在渗透性的阶跃变化。在改变区域内的半径增加或渗透率的选择取决于实际改变的性质。如果使用适当的参数,还可以将渗透率模拟为逐步功能;在这种情况下,该模型折叠到传统的逐步复合模型。其他参数,例如每个区域的形成孔隙率和可压缩性也可以不同,但​​是对于该衍生来假设它们是恒定的。新的解决方案衍生在拉普拉斯空间中,使用数值拉普拉斯反演。

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