đ Acoustic Buoyancy is Real
Why you float in water, but not in airâand how sound may be to blame. Youâre at the beach. You wade out, lie backâand float. Effortlessly. But step back onto land, and suddenly you feel your full weight again. Why? Both air and water are fluidsâthey fill containers, flow around objects, and transmit pressure. So what makes one hold you up and the other let you sink? Most people say density. But thatâs not the full story. Hereâs something strange: if you dive about 20 meters deep, that floating stops. Your body starts to sink. Not because the water changedâbut because the pressure did. Buoyancy isnât constant. It depends on how pressure is distributed vertically through the fluid. What if thatâs the real reason we feel weight in air, too? What if gravity isnât pulling us down? What if pressure from infrasound waves are pushing down on usâinfrasound waves that travel up from the Earth, through the atmosphere, up into space? This is the idea behind acoustic buoyancyâa core tenet of Acoustic Gravitic Theory, the wave-based model of gravity and planetary motion developed by Louis Lockett, Sr. It proposes that low-frequency waves, triggered by the Sun and transmitted through Earthâs crust and atmosphere, create vertical pressure gradients that "weigh down" objects through impedance mismatch, not mass-based attraction. In water, your bodyâs density and acoustic impedance typically allow you to resist this pressureâbut once you descend below roughly 20 meters, that buoyant support fades, and you begin to sink. In air, this resistance doesnât occur at allâso you feel the full force of weight. Could this mean gravity is not a force, but a resonance mismatch? Could controlling frequency and impedance cancel out weight entirely? Letâs dig into the physics of fallingâand why you stop floating at 20 meters.