Reservoir Characterization for CO2 Sequestration: Assessing the Potential of the Devonian Carbonate Nisku Formation of Central Alberta

C. Eisinger, J. Jensen
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引用次数: 8

Abstract

The Wabamun Lake area of Central Alberta, Canada includes several large CO2 point source emitters, collectively producing more than 30 Mt annually. Previous studies established that deep saline aquifers beneath the Wabamun Lake area have good potential for the large-scale injection and storage of CO2 . This study reports on the characterization of the Devonian carbonate Nisku Formation for evaluation as a CO2 repository. Major challenges for characterization included sparse well and seismic data, poor quality flow tests, and few modern measurements. Wireline porosity measurements were present in only one-third of the wells, so porosity and flow capacity (permeability-thickness) were estimated using wireline electrical measurements. The Archie cementation factor appears to vary between 2 and 3, creating uncertainty when predicting porosity using the electrical measurements; however, high-porosity zones could be identified. The electrically-based flow capacity predictions showed more favorable values using a correlation with core than the relation based on drill stem and production tests. This behavior is expected, since the flow test flow capacities are less influenced by local occurrences of very permeable vuggy and moldic rocks. Facies distributions were modeled using both pixel and object methods. The object models, using dimensions obtained from satellite imaging of modern day environments, gave results that were more consistent with the geological understanding of the Nisku and showed greater large-scale connectivity than the pixel model. Predicted volumes show considerable storage capacity in the Nisku, but flow simulations suggest injection capacities are below an initial 20 Mt/year target using vertical wells. More elaborate well designs, including fracture stimulation or multi-lateral wells may allow this goal to be reached or surpassed.
二氧化碳封存储层特征:评估阿尔伯塔省中部泥盆系碳酸盐岩Nisku组的潜力
加拿大阿尔伯塔省中部的Wabamun湖地区包括几个大型二氧化碳点源排放者,每年总排放量超过3000万吨。前期研究表明,Wabamun湖区深层含盐含水层具有大规模注入和封存CO2的良好潜力。本文报道了泥盆系尼斯库组碳酸盐岩的特征,以评价其作为CO2储集层的能力。表征的主要挑战包括稀疏的井和地震数据,低质量的流动测试,以及很少的现代测量。只有三分之一的井进行了电缆孔隙度测量,因此使用电缆电测量来估计孔隙度和流量(渗透率-厚度)。Archie胶结系数在2到3之间变化,这给使用电测量预测孔隙度带来了不确定性;然而,可以识别出高孔隙度区域。与基于钻杆和生产测试的关系相比,基于岩心的电流量预测结果更有利。这种行为是预料之中的,因为流动试验的流动能力较少受到局部出现的渗透性很强的孔洞和模态岩石的影响。相分布采用像素和对象两种方法建模。物体模型使用从现代环境的卫星图像中获得的尺寸,得出的结果与Nisku的地质认识更加一致,并且比像素模型显示出更大的大规模连通性。Nisku的预测容量显示出相当大的存储容量,但流动模拟表明,使用直井的注入能力低于最初的2000万吨/年目标。更复杂的井设计,包括压裂增产或多分支井,可能会达到或超过这一目标。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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