This study systematically investigates the impact of dissolved air content on attached cavitation within a Venturi section using a blow-down cavitation tunnel with precise control of dissolved air content. Four distinct cavitation regimes—supercavitation, cloud cavitation, sheet cavitation, and non-cavitation—were observed, with their formation, detachment, and collapse processes documented through high-speed imaging at multiple scales. The study finds that while transitions between the first three cavitation regimes are largely unaffected by changes in the dissolved air content, cavitation disappearance is highly sensitive to these variations. Notably, altering dissolved air content does not significantly impact the cavity length or oscillation characteristics of cloud and sheet cavitation. However, the presence of dissolved air increases the amount of non-condensable bubbles remaining after cavity collapse, leading to enhanced bubble rebound. To elucidate these phenomena, the diffusion of dissolved air during cavitation was estimated and validated, revealing that large cavities are primarily composed of water vapor with limited influence from diffused air. As the cavity volume decreases, the proportion of diffused air increases, which can delay cavitation desinence. This study provides a systematic experimental approach to comprehensively investigate various cavitation regimes and characteristics. It contributes to an in-depth understanding of the effect of dissolved air on cavitation and applies to deep-sea environments, groundwater, and other environments with fluctuating dissolved air content.
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