Hi all,
Long time lurker first time poster.
My name's Chris, I'm a spearo from the UK living in France.
I've been in the sport for a couple of years and had a question about the reliability of urge to breathe at depth. My current max depth is 18 meters and I'm wondering how safe it is to stay on the bottom until I get an urge to breathe at such depths?
I understand that Dalton's law means that the increase in partial pressure at depth makes O2 more easily transfer from lungs into the blood even at low O2 levels - something which reverses as we ascend.
I also understand that CO2 doesn't follow the same pattern of diffusion with depth - it's largely unaffected.
My questions then are (based on a dive profile that has ZERO hyperventilation):
1. Does this mean that we are burning through O2 much quicker at depth than we would at the surface?
2. If so, does this completely throw off the reliability of the CO2 and O2 relationship? Is the urge to breathe therefore no longer a valid signal of O2 levels at depth as it would be at the surface in a no pre-dive hyperventilation profile?
3. If this is the case, what can we use as a signal to ascend before O2 levels drop below a level that will kill us on surfacing?
I've had a look through a number of posts on the forum but I cannot find a straight answer - if anyone can answer these questions directly or point me in the direction of a post that can help then I'd be really grateful!
Thanks
Long time lurker first time poster.
My name's Chris, I'm a spearo from the UK living in France.
I've been in the sport for a couple of years and had a question about the reliability of urge to breathe at depth. My current max depth is 18 meters and I'm wondering how safe it is to stay on the bottom until I get an urge to breathe at such depths?
I understand that Dalton's law means that the increase in partial pressure at depth makes O2 more easily transfer from lungs into the blood even at low O2 levels - something which reverses as we ascend.
I also understand that CO2 doesn't follow the same pattern of diffusion with depth - it's largely unaffected.
My questions then are (based on a dive profile that has ZERO hyperventilation):
1. Does this mean that we are burning through O2 much quicker at depth than we would at the surface?
2. If so, does this completely throw off the reliability of the CO2 and O2 relationship? Is the urge to breathe therefore no longer a valid signal of O2 levels at depth as it would be at the surface in a no pre-dive hyperventilation profile?
3. If this is the case, what can we use as a signal to ascend before O2 levels drop below a level that will kill us on surfacing?
I've had a look through a number of posts on the forum but I cannot find a straight answer - if anyone can answer these questions directly or point me in the direction of a post that can help then I'd be really grateful!
Thanks