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History Matching and Permeability Increases of Mature Coalbed Methane Wells in San Juan Basin

机译:圣胡安盆地成熟煤层井的历史匹配和渗透性增加

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We discuss detailed well history matches, from the San Juan basin, of coalbed methane (CBM) gas rates, water rates, and pressures. In the sweetspot (fairway) the matching includes permeability that increases strongly with depletion, and is assumed to be exponential, as indicated by independent well tests spaced over time. The permeability increases are well matched by the Palmer-Mansoori (P-M) model. We present statistics of permeability matching to field results by the P-M model in the fairway. First, initial cleat porosities are 0.05-0.17% and consistent with porosities derived from observed water rates. Large permeability increases are not consistent with large cleat porosities. Second, the permeability increase ratio, defined by the maximum permeability reached over the permeability at initial reservoir pressure, varies from 16-170. Third, the matrix shrinkage parameters agree with a recent lab measurement. Fourth, cleat-volume compressibility mostly increases with depletion, when matrix shrinkage becomes dominant and cleats open wider. Last, in many wells north-east of the fairway the perm increase with depletion was found to be similar to that seen in fairway wells. This again suggests cleat porosities less than roughly 0.3%. At low reservoir pressures (<300 psi), we find that the exponential permeability increase flattens. This we have interpreted as coal failure due to stress changes instigated by matrix shrinkage. In fact the P-M model for stress changes can predict the onset of shear failure with depletion, which generally agrees with the timing of the flattening. This adds validity to the general applicability of the P-M model in CBM plays. The modeling is important in being able to better forecast gas rates and estimated ultimate recovery (EUR) for CBM wells, which can remain profitable for decades.
机译:我们讨论了煤层甲烷(CBM)煤气率,水费和压力的San Juan盆地的详细悠久历史匹配。在甜点(球道)中,匹配包括耗尽强烈增加的渗透率,并且被认为是指数的,如随时间间隔的独立井测试所示。 PALMER-MANSOORI(P-M)模型磁导率升高均匀。我们将P-M型号在球道中呈现渗透率匹配与现场结果的统计。首先,初始夹层孔隙率为0.05-0.17%,符合来自观察到的水速率的孔隙率。渗透性较大的渗透性不符合大的夹层孔隙率。二,通过在初始储层压力下达到的最大渗透率达到的最大渗透率限定的渗透性增加率从16-170之间变化。第三,矩阵收缩参数与最近的实验室测量一致。第四,当矩阵收缩变得优势和夹板开放宽时,纤维体积压缩性大部分随着耗尽而增加。最后,在众多井中的前沿,发现烫发与耗尽相似,与球道井中看到的相似。这再次表明夹层孔隙率小于大约0.3%。在低水库压力(<300 psi),我们发现指数渗透率增加平坦。这是由于基质收缩造成的压力变化导致的煤气失效。实际上,用于应力变化的P-M模型可以预测耗尽的剪切失效的开始,这通常同意扁平化的时序。这增加了对CBM播放中P-M型号的一般适用性的有效性。该建模对于能够更好的预测煤气速率和估计为CBM井的终极回收率(EUR),这对于几十年来,这可能保持有利可图。

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