作为预测巴拉那盆地Irati和Rio Bonito组碳氢化合物和二氧化碳储存前景的一项措施的储层质量评估

Richardson M. Abraham-A , Colombo C.C.G. Tassinari , Fabio Taioli , Haline V. Rocha , Orlando C. da Silva
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引用次数: 2

摘要

到目前为止,加强碳氢化合物回收过程加上二氧化碳储存是地质结构中最便宜的碳捕获和储存(CCS)选择。然而,在没有生产/枯竭碳氢化合物储层的地区,如圣保罗西南部的Irati和Rio Bonito地层,也在勘探储层以储存二氧化碳。因此,该研究涉及基于岩石物理学的流动单元因子来预测储层的质量,主要关注基于页岩、碳酸盐岩、砂岩和粉砂岩单元的碳氢化合物生存能力和CO2储存可能性。涉及研究目标模型的方法在Irati和Rio Bonito地层中并不常见。根据声密度-孔隙度(ФS-D)方法,页岩的孔隙度范围为0.02至0.15,粉砂岩的孔隙度范围0.028至0.18,碳酸盐岩的孔隙度范围0.03至0.21,砂岩的孔隙度为0.10至0.31。页岩的渗透率(k)为0.00005mD至36.6mD,粉砂岩为0.0008mD至132mD,碳酸盐为0.025mD至786mD,砂岩为8mD至10000mD。结果表明,基于Ф,k、自由流体指数FFI、储层质量指数RQI和流动带指数FZI,砂岩的流体传输指数更为显著。此外,在某些情况下,这些参数对碳酸盐岩来说相当重要,对粉砂岩来说效果较差,对页岩来说相对不重要。然而,页岩的总有机物含量(TOC)值高达10.5%,表明其具有生烃潜力。砂岩中的显著值(例如Ф≥25%和FFI≥20%)表明储层具有油气聚集的潜力。砂岩具有相当大的物理性质,表明储层岩石单元具有合理的流体(如天然气)回收率和CO2注入率。因此,根据研究结果,Irati组页岩是可行的烃源岩,Rio Bonito组砂岩是潜在的油气藏。随后,未来的碳氢化合物生产活动将加强该地区的二氧化碳储存选择。此外,研究结果可作为相关油气勘探研究的输入数据。然而,如果进一步的研究表明碳氢化合物储量在商业上不可行,这些发现也将有助于在需要时划定专门的地质储层用于CO2储存。
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Reservoir quality evaluation as a measure to forecast hydrocarbon and CO2 storage prospects in Irati and Rio Bonito Formations, Paraná Basin

Enhanced hydrocarbon recovery processes coupled with CO2 storage are, by far, the cheapest carbon capture and storage (CCS) options in geological structures. However, reservoirs are also being explored for CO2 storage in regions without producing/depleted hydrocarbon reservoirs, such as the Irati and Rio Bonito Formations in the southwestern part of São Paulo. Therefore, the study involves petrophysics-based flow unit factors to predict the reservoirs’ quality, primarily focusing on hydrocarbon viability with CO2 storage possibilities based on the shale, carbonate, sandstone and siltstone rock units. The methodology involving the models for the research objective is uncommon for the Irati and Rio Bonito Formations. The porosity range is 0.02 to 0.15 in shales, 0.028 to 0.18 in siltstones, 0.03 to 0.21 in carbonates, and 0.10 to 0.31 in sandstones based on the sonic-density porosity (ФS-D) approach. Permeability (k) is 0.00005mD to 36.6mD in shales, 0.0008mD to 132mD in siltstones, 0.025mD to 786mD in carbonates and 8mD to 10000mD in sandstones. The results show more significant fluid transmission indices for the sandstone based on Ф, k, free fluid index-FFI, reservoir quality index-RQI, and flow zone indicator-FZI. Also, the parameters are considerably significant for carbonates in some instances, less effective for siltstone and comparatively insignificant for shale. However, shales` total organic content (TOC) values are up to 10.5%, suggesting their hydrocarbon generation potentials. Significant values (e.g., Ф ≥25% and FFI ≥20%) in sandstones indicate reservoirs with the potential for hydrocarbon accumulation. Considerable physical qualities, as presented for the sandstone, suggest reservoir rock units with reasonable fluid (e.g., gas) recovery and CO2 injection rates. Therefore, based on the research results, the Irati Formation shales are viable hydrocarbon source rocks, and the Rio Bonito Formation sandstones are potential hydrocarbon reservoirs. Subsequently, future hydrocarbon production events will enhance CO2 storage options in the region. Furthermore, the research results may serve as input data in related hydrocarbon exploration studies. However, if further research indicates non-commercially viable hydrocarbon reserves, the findings will also aid in delineating dedicated geological reservoirs for CO2 storage when needed.

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