Apart from kerogen, other components of organic shales also contribute to wettability characteristics . Clay minerals, commonly found in shale formations, possess hydrophilic surfaces that can strongly interact with water molecules, promoting water-wetness. In contrast, organic matter, such as bitumen and migrated oil, tends to be oil-wet, leading to heterogeneous wettability within shale formations. Recent research in the field of organic shale wettability has focused on understanding the factors affecting wettability alteration and its impact on hydrocarbon recovery . Experimental studies have explored the effects of temperature, pressure, chemical composition, and mineralogy on the wettability of organic shales. These studies aim to develop predictive models and techniques to optimize extraction processes.