Exploring pre-salt oil deposits poses a significant challenge for the oil and gas industry. Carbonate rock reservoirs, being more susceptible to diagenetic actions, exhibit considerable complexity due to the heterogeneity of the porous system, making exploration activities in this scenario challenging. Microscale analysis of fluid behavior in porous media from X-ray microtomography images and petrophysical system analyses has become increasingly essential for enhancing techniques applied in this sector. To investigate the impact of mineralogy on oil recovery using desulfated seawater (DSW), two samples of coquinas from the Morro do Chaves Formation, Sergipe-Alagoas Basin, considered analogs to the coquinas of the Itapema Formation in the Santos Basin, Brazilian pre-salt, were utilized. Due to the depositional context of this formation, the coquinas from the Morro do Chaves Formation contain terrigenous minerals, primarily quartz, in their composition. This study aims to understand how different percentages of these terrigenous minerals associated with carbonate minerals can influence reservoir oil recovery. For this purpose, 3D image analyses obtained by micro-CT at different saturation phases: dry, water-saturated formation, oil-aged, and at various contact times with DSW were employed. To confirm observations acquired through images, the contact angle of the system was measured, where samples aged in oil came into contact with recovery water. Image analyses were conducted using profiles of both porosity and fluid saturation present in the pores. As a result, indications were observed that terrigenous minerals influence rock wettability. The sample containing higher percentages of these minerals demonstrated an affinity with oil, while the other, lacking these minerals, exhibited water-wettability. Different interpretations, however, could be identified: desulfated seawater did not benefit oil recovery, as the sample with a high content of terrigenous material showed the highest efficiency in removing residual oil; another interesting aspect found in this sample was the tendency for gas entrapment, as the percentage of pores filled with air remained practically constant during the process.
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