kwinter
Contributor
According to your profile, Chesty, you have been diving for several years and have over 100 dives and deep certification. So you are not asking this question as a beginner wondering why pressure is less near the surface. And you are quoting GUE doctrine, so you are bright enough to question AJ's Kool-Ade ;-) Now let's see if we can address what I THINK you are really asking.
You should have no problem understanding that the pressure differential as you ascend gets bigger and bigger each meter. It's a 50% change from 30m (4ATA) to 10m (2ATA). It's another 50% change from there to the surface. So a 20 meter change at depth has the same physiologic impact as a 10 meter change near the surface.
You also must know that nitrogen (N2) and other "inert" gasses dissolve into your blood and tissues under pressure. These dissolved gasses have 2 ways of coming out of solution in your body as you ascend and reduce the pressure. When you ascend slowly so that the pressure gradient is small between the gas you are breathing and the level of that gas in your tissues, the dissolved gas gets exchanged at your lungs and gets exhaled. This is called "offgassing." If you ascend too quickly so that the pressure differential is too great for a slow transfer of the gas in its dissolved state, then the excess gas comes out of solution in the tissues and blood and forms bubbles. This is called "really bad ****."
The object of decompression or any ascent in diving is to maximize offgassing and avoid really bad ****. You should be able to see that this means slowing your ascent rate as you come up so that the pressure differential percent doesn't get too high. In simple terms, this would be a linear graph roughly analogous to gradient factors. In philosophical terms, it is exactly what TSandM mentioned about Zeno's Paradox. And I personally want to thank Lynne for raising the level of discussion.
As for the GUE recommendation, I think it should be clear that the ascent rate should really change constantly as you ascend. But since that is virtually impossible to model, then a step-change approach is taken with as fast as 9m/min for certain depths and then 6m/min, 3m/min and finally 1m/min. The object is to slow your ascent to maintain a constant percentage pN2 difference to enhance offgassing and avoid bubbles.
Did that help?
iPhone. iTypo. iApologize.
You should have no problem understanding that the pressure differential as you ascend gets bigger and bigger each meter. It's a 50% change from 30m (4ATA) to 10m (2ATA). It's another 50% change from there to the surface. So a 20 meter change at depth has the same physiologic impact as a 10 meter change near the surface.
You also must know that nitrogen (N2) and other "inert" gasses dissolve into your blood and tissues under pressure. These dissolved gasses have 2 ways of coming out of solution in your body as you ascend and reduce the pressure. When you ascend slowly so that the pressure gradient is small between the gas you are breathing and the level of that gas in your tissues, the dissolved gas gets exchanged at your lungs and gets exhaled. This is called "offgassing." If you ascend too quickly so that the pressure differential is too great for a slow transfer of the gas in its dissolved state, then the excess gas comes out of solution in the tissues and blood and forms bubbles. This is called "really bad ****."
The object of decompression or any ascent in diving is to maximize offgassing and avoid really bad ****. You should be able to see that this means slowing your ascent rate as you come up so that the pressure differential percent doesn't get too high. In simple terms, this would be a linear graph roughly analogous to gradient factors. In philosophical terms, it is exactly what TSandM mentioned about Zeno's Paradox. And I personally want to thank Lynne for raising the level of discussion.
As for the GUE recommendation, I think it should be clear that the ascent rate should really change constantly as you ascend. But since that is virtually impossible to model, then a step-change approach is taken with as fast as 9m/min for certain depths and then 6m/min, 3m/min and finally 1m/min. The object is to slow your ascent to maintain a constant percentage pN2 difference to enhance offgassing and avoid bubbles.
Did that help?
iPhone. iTypo. iApologize.