First off, let me clarify, I am not challenging anybody's knowledge or expertise. Simply trying to be a bit geeky and dive into the details so that over time I absorb more and more of this information.
See my post #34 for more information.
You seem to be assuming that all tissues are off-gassing as you ascend.
I guess I am. I am surprised that we have tissues that are so sensitive to pressure that even a few inches of water pressure will keep them on-gassing. It seems like those tissues would by default be the fast tissues. What compartment, in my scenario, or any scenario at a microscopic level cannot off gas during the apropriate partial pressure of an ascent? For my question, a _very_ slow, possibly impractical ascent? Even if the off gassing is incredibly slow, there has to be some depth along the ascent path where each tissue's partial pressure is met, no? At some point on the ascent, if slow enough, won't every tissue reach a partial pressure equilibrium for the current depth and begin to off gas if that depth is reduced? This is why I asked if we were talking about a "practical for scuba" sweet spot of ascent rate vs a law of physics sweet spot. I guess I figured that a really slow ascent rate would be the perfect form of decompression. Slow tissues are allowed to off gas slowly and near zero chance of a bubble forming. I am not suggesting that all tissues would reach equilibrium at the same time, only that if an ascent was slow enough, all tissues would reach ambient saturation seconds and inches below the surface.
Those slower tissues will one-by-one reach equilibrium and then begin to off-gas as you ascend,
Agreed. Wholeheartedly. This is also the assumption you said I made above.
but you will not be off-gassing in ALL tissues until you are on the surface.
But you and I just agreed that they would? At least at any practical level. If an ascent were slow enough, wouldn't any practically measurable tissue that had nitrogen in it at a depth of a foot or two be at ambient pressures?
I understand the different compartment idea, admittedly at a very amateurish level. At the extreme, even the fast tissues would have an elevated nitrogen equilibrium at a foot of depth. Maybe immeasurable, but there. This is why I asked about a _very_ slow ascent. I am still working my head around a "too slow ascent rate." I remember the SB thread that contained a really nice on-gassing computer simulation. (Which I didn't find with a cursory look. I think that you were a contributor.) It explained this really well but I don't think it addressed anything like a too slow ascent rate. I understand that equilibrium will be reached at different depths for different tissues. Again, in my proposed scenario, we are talking about a possibly impractically slow ascent. I was just surprised that a diver could ascend too slowly. Just digging for an understanding.
Let me ask it in a different way. This doesn't tie directly to my original question but it is possibly a more practical question. Is scenario two actually at a higher risk of DCS than scenario one?
Scenario 1) I am doing a 60 minute dive to 45' depth, I stay there the maximum amount of time to allow for a safe "industry standard" ascent to the surface, 53 minutes. Then ascend normally at 30ft per minute. (2 minute descent. 3 min safety stop, 90 second combined ascent, so a 53+ minute bottom time)
Scenario 2) I am doing a 60 minute dive to 45' depth. It take two minutes to descend to 45'. At that time, I take 58 minutes to at ascend 45 feet smoothly to the surface. Roughly an ascent rate of .8 feet per minute.