korikancha
Guest
Hi! I have been trying to learn about decompression theory, reading all the material I got my hands on (I have two of Dr. Wienke's books but, as another poster said, they are not that easy to read...).
I read the material from http://www.deepocean.net/deepocean/index.php (pretty good, I think) and I think I learned quite a bit. However, I am still confused when it comes to M-values (aka critical gradients)... In Buehlmann's they are linear functions of pressure. Now, here is the confusion: WHAT pressure? Is it the alveolar pressure (ambient pressure corrected for water vapor, etc), or is it the partial pressure of the inert gases in the tissue in question? Similarly, in Workman's model the M-values are functions of depth. WHAT depth? Is it the depth that is EQUIVALENT to the alveolar pressure, or to the partial pressure of the inert gases? (I know it is NOT the real under water depth...)
Thanks in advance for all the help! (Just as background, I am a newbie diver but also trained, many, many years ago, as a physicist...)
I read the material from http://www.deepocean.net/deepocean/index.php (pretty good, I think) and I think I learned quite a bit. However, I am still confused when it comes to M-values (aka critical gradients)... In Buehlmann's they are linear functions of pressure. Now, here is the confusion: WHAT pressure? Is it the alveolar pressure (ambient pressure corrected for water vapor, etc), or is it the partial pressure of the inert gases in the tissue in question? Similarly, in Workman's model the M-values are functions of depth. WHAT depth? Is it the depth that is EQUIVALENT to the alveolar pressure, or to the partial pressure of the inert gases? (I know it is NOT the real under water depth...)
Thanks in advance for all the help! (Just as background, I am a newbie diver but also trained, many, many years ago, as a physicist...)