At last year's BTS, Dr. Sotis explained that at higher ambient pressures, sufficient O2 dissolves in the blood plasma to support the body's needs without any hemoglobin transport at all (with the numbers to show it). IIRC, this is linearly proportional to depth. However, as one ascends, the amount of dissolved O2 decreases, and one depends to a progressively greater extent on hemoglobin transport. Thus, CO problems often present on ascent even though we normally change to progressively higher PPO2 as we go. The higher PPO2 cannot compensate for the lower ambient pressure, the O2 reaching the tissues drops, and you pass out.
It takes an inspired oxygen partial pressure of nearly 3 ATA in order for the arterial oxygen content to increase to the point that deoxygenation of hemoglobin isn't necessary. That is not duplicated under normal diving conditions. Also (r/t John's comment), CO does in fact cause tissue damage by binding to citochrome C oxidase in the mitochondria (the metabolic organs of the cells) and disrupting cellular metabolism. It also binds to myoglobin in the muscle cells. This is why the carboxyhemoglobin level in a poisoning victim is a poor predictor of outcome. In practice, some CO toxicity effects could be overcome by hyperoxia while diving, but as more CO is bound to the molecules described above, this effect would be rapidly negated.
Best regards,
DDM
Last edited: