Nitrogen absorption, and tissue "compartments"

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debajo agua

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Hi,

When dealing with dive tables or algorithms, I'm curious about what a "tissue compartment" for Nitrogen absorption means; In particular, why are there "six compartments" of nitrogen absorption that US navy tables take into account? What are the six tissue compartments and do they each have a different name?

TIA,
 
The idea of tissue compartments goes back more than 100 years. Different theorists have different numbers of compartments. Here is a quick and overly simplified summary.

When nitrogen is absorbed into the body, the rate at which it is absorbed and later released varies from one tissue to another. The more liquid it is, the faster; the more blood passes through the tissue (perfusion), the faster. Some tissues are called fast tissues and some tissues are called slow tissues because of this varying rate. Nitrogen is absorbed and released through a process called diffusion. The nitrogen molecules move about randomly. When you have been on the surface hanging around for long enough, the amount of nitrogen in the air you breathe and the tissues in your body is the same. That is because the random motion of the molecules has evened out--as many molecules are going into the body as you breathe as are going out. Your body is said to be at equilibrium.

When you descend to 99 feet, every lungful of air you breathe has 4 times as many molecules in it as on the surface, so there are now 4 times as many molecules going into your body as out. That difference is called a gradient. The higher the gradient, the faster your tissues absorb nitrogen. As you swim around at 99 feet, the tissues become more and more saturated with nitrogen. This lowers the gradient, so the rate at which you absorb nitrogen slows down. This slowing down is approximated by a concept called halftimes. A very fast tissue will be half way to being saturated in 5 minutes, but it will be slowing down. It will get half way from that point in another 5 minutes. Then it will be halfway from that point in the next 5 minutes. Eventually it will be saturated and have the same level of nitrogen as the air you are breathing. That will take about 6 times the amount of time it took it to get to the half way point.

When you ascend, the opposite happens. When you have more nitrogen in your tissues than the air, it will start to leave the tissues.

There are many tissues in the body, so in order to plan decompression, they could not describe then all, and a number theoretical tissues were created instead. These are sometimes called compartments. They do not correspond to specific tissues but to a range of tissues that are similar. The tissues mentioned above that get half way to saturation in 5 minutes are said to have a 5 minute half time. That is sometimes called the 5 minute compartment.

The purpose is to help calculate how much nitrogen has entered the body and what needs to be done to get it out safely.
 
I forgot to mention the names of the compartments.

The original model by Haldane about 100 years ago had 5 halftimes: 5, 10, 20, 40 and 75 minutes. In the 1950s, the Navy added a 120 minute compartment to make 6. Since then, they added 160, 200, and 240 minute compartments to make 9.
 
This is absolutely the best, clearest, concise description of the absorption-diffusion process I have ever read. Thanks a bunch for this. Ed



The idea of tissue compartments goes back more than 100 years. Different theorists have different numbers of compartments. Here is a quick and overly simplified summary.

When nitrogen is absorbed into the body, the rate at which it is absorbed and later released varies from one tissue to another. The more liquid it is, the faster; the more blood passes through the tissue (perfusion), the faster. Some tissues are called fast tissues and some tissues are called slow tissues because of this varying rate. Nitrogen is absorbed and released through a process called diffusion. The nitrogen molecules move about randomly. When you have been on the surface hanging around for long enough, the amount of nitrogen in the air you breathe and the tissues in your body is the same. That is because the random motion of the molecules has evened out--as many molecules are going into the body as you breathe as are going out. Your body is said to be at equilibrium.

When you descend to 99 feet, every lungful of air you breathe has 4 times as many molecules in it as on the surface, so there are now 4 times as many molecules going into your body as out. That difference is called a gradient. The higher the gradient, the faster your tissues absorb nitrogen. As you swim around at 99 feet, the tissues become more and more saturated with nitrogen. This lowers the gradient, so the rate at which you absorb nitrogen slows down. This slowing down is approximated by a concept called halftimes. A very fast tissue will be half way to being saturated in 5 minutes, but it will be slowing down. It will get half way from that point in another 5 minutes. Then it will be halfway from that point in the next 5 minutes. Eventually it will be saturated and have the same level of nitrogen as the air you are breathing. That will take about 6 times the amount of time it took it to get to the half way point.

When you ascend, the opposite happens. When you have more nitrogen in your tissues than the air, it will start to leave the tissues.

There are many tissues in the body, so in order to plan decompression, they could not describe then all, and a number theoretical tissues were created instead. These are sometimes called compartments. They do not correspond to specific tissues but to a range of tissues that are similar. The tissues mentioned above that get half way to saturation in 5 minutes are said to have a 5 minute half time. That is sometimes called the 5 minute compartment.

The purpose is to help calculate how much nitrogen has entered the body and what needs to be done to get it out safely.
 
Hi,
you can use divePAL (the basic version is free) to see the compartments "in action" (as defined by Buhlmann ZH-L16C model); just draw a dive profile (or get a profile from the thousands already online), analyze it and see the 16 compartments go up and down during your dive :wink:

divepal_scubalab_1.jpg
Alberto (aka eDiver)
 
Thanks for the reply. Of course, when one question is answered, new questions arise: Someone suggested to me, that a fast descent would increase bottom time, the idea being that fewer respiration on descent = less time for Nitrogen to be absorbed into the body while descending. Taking into consideration 1/2 time for Nitrogen absorption, would there be any validity to this argument? Besides my question, are there any known benefits from a quick descent vs slow descent?
 
The number of respirations (and their volume) are not variables in nitrogen loading. If is a function of the percentage of nitrogen in the breathing gas, and depth and time. The small changes in the gas composition as the body processes it are of no significant consequence. Nothing wrong with a fast descent as long as you are in control and able to manage the pressure change (and be a good buddy).
 
boulderjohn,

Geeze, that was nicely done!
 
Someone suggested to me, that a fast descent would increase bottom time

I would think this would be true to some extent, but remember that the deeper you go, the quicker you build up nitrogen. So quickly descending at the surface wouldn't help you much. Quickly descending at 100' to 130' should make a much bigger difference. As awap mentioned though, it's not because you're breathing less. Way too much nitrogen in each breath to matter. Now theoretically if you could dive down on one big gulp of surface air at 1atm... then yeh, that would help you lol.

Just my guess. Not a fact. I'll bet you I'm probably wrong! Now we just have to wait...
 
https://www.shearwater.com/products/teric/

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