SPEAKER_04 1:25:06–1:27:12
Okay, so let me talk about what scuba diving is for a second. And again, you'll be able to picture this, okay. So when you go scuba diving, you have to put weight on you to push you down underwater, but once you get underwater a certain depth, there's enough force above you that will push you down. Like you will accelerate into the ocean floor if you allow it to happen. So you have to wear what's called a buoyancy compensator. It's actually like a life vest that you fill up with air to create a balance between the forces that are pushing you down. Then you get enough expansion to hold you up. So you want to try to get what's called neutral buoyancy. So literally you put enough air in the buoyancy compensator to balance the force, and you literally sit at the same place in the water. So you don't sink and you don't go up. But if you sit still and you take a breath in, you go up, and when you exhale, you go down. So you have this little excursion as you breathe in and out. One, if you have some frame of reference, you can actually see yourself going up and down, and you can feel yourself going up and down. So it's a great little representation of this concept. So you take the same thing—it's like, okay, this is a fluid-based kind of representation, but guess what? On Earth, this exact same thing is happening to you as you breathe. We don't feel it as much because we're so grounded by this perception of gravity. So the ground is pushing up against you constantly, and so you feel this sense of acceleration, of perceived gravity. So you don't feel the up and down, but the reality is that as you breathe in, your density is reduced, you go up, and as you breathe out, your density increases and you go down. That's why I always describe ERS as up and IRS as down, is because that's what's happening. But it's based on the behavior of how these helices change the physical shape of the cylinder, and you, sir, are the cylinder.
respirationbuoyancybody mechanicshelical orientationfluid dynamics