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Microbially mediated porosity enhancement in carbonate reservoirs: Experiments with samples from the Salem, Sligo, and Smackover formations.

机译:碳酸盐岩储层中微生物介导的孔隙度增加:使用塞勒姆,斯莱戈和斯马科夫地层样品的实验。

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摘要

This study used petrographic thin sections, scanning electron microscopy, and confocal laser microscopy to document microbially mediated dissolution of carbonate reservoir rocks. The samples studied came from three carbonate units that are hydrocarbon reservoirs; the Salem, Sligo, and Smackover formations. These samples were inoculated with bacteria, and then treated with nutrient solutions followed by ethanol to promote generation of acetic acid by bacteria. Dissolution occurred in calcite-dominated rocks and in dolomitized rocks. Noticeable changes first occurred after nine weeks of ethanol treatment and significant change only occurred after twelve weeks of ethanol treatment. The size of the vuggy pores created increased from 1 mum or less to over 5 mum, and rarely over 10 mum, in length.
机译:这项研究使用岩相薄片,扫描电子显微镜和共聚焦激光显微镜来记录微生物介导的碳酸盐储层岩石的溶解。研究的样品来自碳酸盐岩储层的三个碳酸盐单元。 Salem,Sligo和Smackover编队。这些样品用细菌接种,然后用营养液处理,然后用乙醇处理,以促进细菌生成乙酸。溶解发生在方解石为主的岩石和白云石化的岩石中。乙醇处理九周后首先发生了明显的变化,乙醇处理十二周后才发生显着变化。产生的孔洞的尺寸从1毫米或更小增加到5毫米以上,很少超过10毫米。

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