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New Method to Estimate Damaged Formation Permeability With Well Testing

机译:通过试井估算受损地层渗透率的新方法

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Most composite solutions used in modern well test interpretationuse the "step-permeability" model where the altered formationsare divided into two or more concentric zones, each withconstant permeability. Depending on the causes of alteration orvariation, this model can deviate significantly from the realcondition. A formation can be altered because of stressredistribution, drilling damage, solids co-production, mineralprecipitates, and drilling mud invasion, each factor more likely togenerate spatially-varying permeabilities rather than constant kzones. Experimental data confirm that a continuous permeabilitymodel is more realistic than the step permeability model.A new semi-analytical solution with smooth radius-dependentpermeability has been developed to analyze well test results fromsuch altered formations. The altered formation is approximatedas a concentric two-zone composite model: an exterior intactzone that retains the original unaltered permeability, and aninterior zone where the permeability values have been alteredand change as a function of radius. The permeability in thisnear-well zone can change continuously to the originalpermeability or to a different value at the boundary with theexterior zone, where there is a step-change in permeability. Thechoice of an increase or decrease of permeability with radiuswithin the altered zone depends on the nature of the actualalteration. The permeability can also be simulated as a step-wisefunction if appropriate parameters are used; in such situations,the model collapses to conventional step-wise composite models.Other parameters such as formation porosity and compressibilityof each zone can also be different, but they are assumed constantfor this derivation. The new solution is derived in Laplace space, Most composite solutions used in modern well test interpretationuse the "step-permeability" model where the altered formationsare divided into two or more concentric zones, each withconstant permeability. Depending on the causes of alteration orvariation, this model can deviate significantly from the realcondition. A formation can be altered because of stressredistribution, drilling damage, solids co-production, mineralprecipitates, and drilling mud invasion, each factor more likely togenerate spatially-varying permeabilities rather than constant kzones. Experimental data confirm that a continuous permeabilitymodel is more realistic than the step permeability model.A new semi-analytical solution with smooth radius-dependentpermeability has been developed to analyze well test results fromsuch altered formations. The altered formation is approximatedas a concentric two-zone composite model: an exterior intactzone that retains the original unaltered permeability, and aninterior zone where the permeability values have been alteredand change as a function of radius. The permeability in thisnear-well zone can change continuously to the originalpermeability or to a different value at the boundary with theexterior zone, where there is a step-change in permeability. Thechoice of an increase or decrease of permeability with radiuswithin the altered zone depends on the nature of the actualalteration. The permeability can also be simulated as a step-wisefunction if appropriate parameters are used; in such situations,the model collapses to conventional step-wise composite models.Other parameters such as formation porosity and compressibilityof each zone can also be different, but they are assumed constantfor this derivation. The new solution is derived in Laplace space,Most composite solutions used in modern well test interpretationuse the "step-permeability" model where the altered formationsare divided into two or more concentric zones, each withconstant permeability. Depending on the causes of alteration orvariation, this model can deviate significantly from the realcondition. A formation can be altered because of stressredistribution, drilling damage, solids co-production, mineralprecipitates, and drilling mud invasion, each factor more likely togenerate spatially-varying permeabilities rather than constant kzones. Experimental data confirm that a continuous permeabilitymodel is more realistic than the step permeability model.A new semi-analytical solution with smooth radius-dependentpermeability has been developed to analyze well test results fromsuch altered formations. The altered formation is approximatedas a concentric two-zone composite model: an exterior intactzone that retains the original unaltered permeability, and aninterior zone where the permeability values have been alteredand change as a function of radius. The permeability in thisnear-well zone can change continuously to the originalpermeability or to a different value at the boundary with theexterior zone, where there is a step-change in permeability. Thechoice of an increase or decrease of permeability with radiuswithin the altered zone depends on the nature of the actualalteration. The permeability can also be simulated as a step-wisefunction if appropriate parameters are used; in such situations,the model collapses to conventional step-wise composite models.Other parameters such as formation porosity and compressibilityof each zone can also be different, but they are assumed constantfor this derivation. The new solution is derived in Laplace space,and numerical Laplace inversion is used.
机译:现代试井解释中使用的大多数复合解决方案 使用“阶梯渗透率”模型,其中改变的地层 分为两个或多个同心区域,每个同心区域 恒定磁导率。取决于改变的原因或 变化,此模型可能与真实模型有很大的出入 健康)状况。压力会改变地层 重新分配,钻探破坏,固体联产,矿物 沉淀物和钻探泥浆侵入,每个因素更可能导致 产生空间变化的磁导率,而不是常数k 区域。实验数据证实连续渗透性 该模型比阶跃渗透率模型更现实。 一种新的半解析解,其依赖于平滑的半径 已经开发出渗透率来分析来自 这种改变的形式。改变的形式是近似的 作为同心两区复合模型:完整的外观 保留原始不变磁导率的区域,以及 渗透率值已更改的内部区域 并随半径变化。在此的渗透性 近井区域可以连续变化为原始区域 磁导率或与边界的不同值 外部区域,渗透率会发生阶跃变化。这 选择渗透率随半径的增加或减少 更改后的区域内取决于实际的性质 改造。渗透率也可以逐步模拟 如果使用适当的参数,则起作用;在这种情况下 该模型崩溃为常规的逐步复合模型。 其他参数,例如地层孔隙度和可压缩性 每个区域的长度也可以不同,但​​是假定它们是恒定的 为此推导。新的解决方案是在拉普拉斯空间中派生的,大多数用于现代试井解释的复合解决方案 使用“阶梯渗透率”模型,其中改变的地层 分为两个或多个同心区域,每个同心区域 恒定磁导率。取决于改变的原因或 变化,此模型可能与真实模型有很大的出入 健康)状况。压力会改变地层 重新分配,钻探破坏,固体联产,矿物 沉淀物和钻探泥浆侵入,每个因素更可能导致 产生空间变化的磁导率,而不是常数k 区域。实验数据证实连续渗透性 该模型比阶跃渗透率模型更现实。 依赖于平滑半径的新的半解析解 已经开发出渗透率来分析井测试结果 这种改变的形式。改变的形式是近似的 作为同心两区复合模型:完整的外观 保留原始不变磁导率的区域,以及 渗透率值已更改的内部区域 并随半径变化。在此的渗透性 近井区域可以连续变化为原始区域 磁导率或与边界的不同值 外部区域,渗透率会发生阶跃变化。这 选择渗透率随半径的增加或减少 更改后的区域内取决于实际的性质 改造。渗透率也可以逐步模拟 如果使用适当的参数,则起作用;在这种情况下 该模型崩溃为常规的逐步复合模型。 其他参数,例如地层孔隙度和可压缩性 每个区域的长度也可以不同,但​​是假定它们是恒定的 为此推导。新的解决方案源自拉普拉斯空间,现代测井解释中使用的大多数复合解决方案 使用“阶梯渗透率”模型,其中改变的地层 分为两个或多个同心区域,每个同心区域 恒定磁导率。取决于改变的原因或 变化,此模型可能与真实模型有很大的出入 健康)状况。压力会改变地层 重新分配,钻探破坏,固体联产,矿物 沉淀物和钻探泥浆侵入,每个因素更可能导致 产生空间变化的磁导率,而不是常数k 区域。实验数据证实连续渗透性 该模型比阶跃渗透率模型更现实。 依赖于平滑半径的新的半解析解 已经开发出渗透率来分析来自 这种改变的形式。改变的形式是近似的 作为同心两区复合模型:完整的外观 保留原始不变磁导率的区域,以及 渗透率值已更改的内部区域 并随半径变化。在此的渗透性 近井区域可以连续变化为原始区域 磁导率或与边界的不同值 外部区域,其中渗透率存在阶跃变化。这 选择渗透率随半径的增加或减少 更改后的区域内取决于实际的性质 改造。渗透率也可以逐步模拟 如果使用适当的参数,则起作用;在这种情况下 该模型崩溃为常规的逐步复合模型。 其他参数,例如地层孔隙度和可压缩性 每个区域的长度也可以不同,但​​是假定它们是恒定的 为此推导。在拉普拉斯空间中导出了新的解,并使用了数值拉普拉斯反演。

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