OXYGEN
EXPOSURE MANAGEMENT
by Richard D. Vann
Oxygen metabolism is the primary energy
source in higher life forms, but when oxygen enters the metabolic process
prematurely, reactive oxygen species can form which interfere with normal
function and cause convulsions or other symptoms of oxygen toxicity. Immersion,
exercise, and inspired carbon dioxide increase susceptibility to oxygen toxicity
by elevating cerebral blood flow and oxygen delivery to the brain. The risk of
toxicity is reduced by limiting oxygen exposure, but exposure limits are based
on limited data. Limits for oxygen in mixed gas appear shorter than for pure
oxygen. Open-water experience indicates that convulsions can occur near the
accepted exposure limits. The risk of oxygen toxicity can be modelled
statistically but with uncertain accuracy. The choice of "safe" exposure limits
depends upon the risk of convulsions one is willing to accept. The maximum
"safe" oxygen partial pressure for air or nitrox diving in the water appears to
be in the range of 1.2-1.4 bar though some individuals set the limits as high as
1.6 bar. For pure oxygen, 1.6 bar has been used safely for in-water
decompressions of up to 30 min.
Knowledge of central nervous system (CNS)
oxygen toxicity is unnecessary in order to breathe oxygen underwater safely at a
partial pressure of one bar or less. Considerably more knowledge is needed at
higher partial pressures or when the oxygen pressure changes with time. The real
questions are; how much oxygen can be used safely given our current knowledge,
and how can oxygen be used more effectively without sacrificing safety?
The
Biochemistry of Oxygen Toxicity (Stryer 1988)
Oxygen metabolism is the primary energy
source in higher life forms. Because heat energy produced by oxygen reactions
such as fire would damage tissue, metabolic pathways have evolved that safely
capture small packets of reusable chemical energy. This energy is stored in
molecules called adenosine triphosphate (ATP).
Figure 1 illustrates some features of ATP
production during the breakdown of sugar at normal oxygen partial pressures. The
biochemical processes known as glycolysis use no oxygen and produce relatively
little ATP. The major product of glycolysis, pyruvic acid, enters the Krebs
cycle which releases carbon dioxide and supplies electrons needed to form ATP.
Most ATP is produced in a series of electron transport reactions called the
respiratory chain.
Oxygen usually does not enter the
respiratory chain until the very end where it reacts with hydrogen to form
water. Should oxygen enter the respiratory chain prematurely, molecules like the
superoxide anion (O2-) and hydrogen peroxide (H2O2) can form. These reactive
species of oxygen are potentially toxic but are deactivated by protective
enzymes such as superoxide dismutase and catalase.
When the oxygen partial pressure is raised
(Fig. 2), the production of reactive oxygen species increases and may overwhelm
the protective mechanisms. This can initiate biochemical and physiological
changes that interfere with normal function and cause signs and symptoms we know
as oxygen toxicity.
Signs and
Symptoms of CNS Oxygen Toxicity (Donald 1992; Clark 1993)
Convulsions are the most spectacular and
objective signs and symptoms of CNS oxygen toxicity, but there is no evidence
they lead to permanent damage if the oxygen exposure is discontinued promptly.
This assumes, of course, that drowning or physical injury are avoided.
Experimental oxygen exposures are often terminated by less specific symptoms
including abnormal breathing, nausea, twitching, dizziness, incoordination, and
visual or auditory disturbances. These symptoms do not necessarily precede
convulsions.
Factors which elevate cerebral blood flow,
thereby augmenting oxygen delivery to the brain, appear to increase
susceptibility to oxygen toxicity. These factors include immersion, exercise,
and carbon dioxide. Carbon dioxide may be present in the inspired gas or may be
retained due to inadequate ventilation. Inadequate ventilation can be caused by
high gas density, external breathing resistance, or poor ventilatory response to
carbon dioxide by "CO2 retainers" (Lanphier 1982; Warkander et al. 1990).
Oxygen
Exposure Limits
Oxygen exposure limits like those of Fig.
3 were established to decrease the risk of convulsions for divers breathing pure
oxygen or oxygen in mixed gas. Figure 3 shows three sets of pure oxygen limits
and two sets of mixed gas limits. The U.S. Navy limits from the 1973 Diving
Manual (USN 1973) were published in the 1979 NOAA Diving Manual (NOAA 1979). The
Navy has since modified its pure oxygen limits (Butler and Thalmann 1986) while
NOAA has modified both the pure oxygen and mixed gas limits for its 1991 Diving
Manual (NOAA 1991). Compared with the 1973 Navy/1979 NOAA limits for pure
oxygen, Fig. 3 shows that the 1986 Navy limits are less conservative while the
1991 NOAA limits are more conservative. For mixed gas, the 1991 NOAA limits are
less conservative than the 1973 Navy/1979 NOAA limits.
The changes to the exposure limits of Fig.
3 reflect uncertainty concerning which limits are best and suggest an
examination of the type of data upon which oxygen limits are based. These data
are shown in Fig. 4 and represent most of the CNS toxicity episodes that have
occurred in U.S. experiments during wet, working dives at a single depth for
pure oxygen or for oxygen in mixed gas (Lanphier and Dwyer 1954; Lanphier 1955;
Piantadosi et al. 1979; Vann 1982; Schwartz 1984; Butler and Thalmann 1984,
1986; Butler 1986; Lanphier 1992). The squares represent convulsions, and the
triangles represent symptoms. The 1991 NOAA limits are shown for comparison.
While the discussion below is confined to U.S. data, Donald (1992) has recently
published a large body of British data which will be very important.
The mixed gas incidents occurred at lower
oxygen partial pressures than the pure oxygen incidents. Lanphier, who conducted
oxygen research for the Navy in the 1950's, postulated that high breathing
resistance during deeper mixed gas dives caused carbon dioxide retention which
potentiated oxygen toxicity by increasing cerebral blood flow (Lanphier and
Dwyer 1954). This led him to propose more restrictive limits for mixed gas than
for pure oxygen. In subsequent studies, the lowest partial pressure and shortest
exposure time at which a mixed gas convulsion occurred was 1.6 bar for 40 min
(Vann 1982; Vann and Thalmann 1993). The corresponding exposure for pure oxygen
was 1.76 bar for 72 min (Butler and Thalmann 1984).
The mixed-gas convulsion occurred after 40
min at 100 fsw during a wet, working nitrox chamber dive with a 1.6 bar oxygen
set-point in a rebreather (Vann 1982). Heavy exercise and high breathing
resistance appeared to be contributing factors. Upon decreasing the breathing
resistance and reducing the oxygen pressure to 1.4 bar, 110 dives were conducted
with no further oxygen incidents during 60 min exposures at 100 and 150 fsw with
both nitrox and heliox.
Is an oxygen partial pressure of 1.4 bar
sufficiently conservative given the potential for depth control error, the
unpredictability of carbon dioxide retention, and the minimal mixed-gas exposure
data? The Navy is leaning towards a set-point of 1.2-1.3 bar for rebreathers
where the oxygen partial pressure fluctuates during control around a
pre-determined set-point (Thalmann, personal communication).
The data of Fig. 4 suggest a need for
separate mixed gas and pure oxygen limits but are insufficient to conclusively
prove this need. As a convulsion underwater is potentially fatal, however, a
cautious diver might wish to use separate oxygen and mixed gas limits until
further data firmly establish they are unnecessary.
Open-Water
Experience
What can we learn about oxygen toxicity
from open-water diving with mixed gas and pure oxygen? The incidents described
below took place within the past year.
A mixed gas fatality occurred in a
southeastern U.S. cave where two divers breathed air for 15 min and EAN 40 (40%
O2, balance N2) for 45 min at depths of 80-105 fsw (Menduno 1992). The oxygen
partial pressure was mostly 1.4 bar but occasionally reached 1.5-1.7 bar. After
45 min of hard swimming on enriched air nitrox, one diver convulsed and lost his
regulator. His buddy could not reinsert the regulator, and the diver drowned
after a failed attempt to swim him out of the cave. The oxygen exposure was, for
the most part, less than the 1991 NOAA limit of 1.6 bar for mixed gas diving.
Another enriched air diver who drowned
after an apparent convulsion had told friends that the NOAA limits did not apply
to him (Menduno 1992). His oxygen partial pressure was estimated at 1.7-2.0 bar
for a bottom time of 45-50 min.
An incident involving pure oxygen occurred
in a southeastern U.S. lake (Menduno 1992). After an 8 min exposure at 300 fsw
on a trimix 14/33 (14% O2, 33% He, and 53% N2) a diver decompressed on EAN 32 to
20 fsw where he switched to pure oxygen. Prior to breathing oxygen at 20 fsw
(1.6 bar PO2), his PO2 was 1.4 bar except for 7 min at 1.5-1.7 bar. After 20 min
on oxygen, he unclipped from his decompression line to visit a nearby diver but
drifted down to 35 fsw (2.05 bar PO2) and dozed off. (An Emergency Medical
Technician, he had slept only 2 hrs the previous night.) He was awakened by
abnormal breathing and the onset of convulsions but inflated his buoyancy
compensator before losing consciousness. He recovered from near drowning after
rescue on the surface.
It is commonly assumed that convulsions do
not occur at oxygen pressures of less than about 1.6 bar, but this assumption
depends on a normal seizure threshold. Figure 5 shows the depth-time profile of
an 80 fsw dive that terminated with a convulsion at 34 min (Vann et al. 1992).
The diver breathed EAN 33 with an oxygen partial pressure of 1.26 bar. After
rescue, he was found to have an unreported history of convulsions and to be on
anti-convulsant medication. While such a situation is rare, it emphasizes the
uncertainty of our knowledge, the need to expect emergencies such as oxygen
convulsions or decompression illness, and the necessity for emergency management
plans.
Statistical
Modelling
Do these open-water incidents over
emphasize rare events? What is the risk of a rare event? We can estimate this
risk by statistical modeling of oxygen exposure data (Vann 1988).
Suppose the risk of oxygen toxicity
increased with the concentration of the reactive oxygen species produced during
hyperoxic metabolism (Fig. 2) and represented below by "X". Suppose also that
the rate of change of the local concentration of X were equal to its production
minus its removal. If X were produced in proportion to the local oxygen tension
(c •PO2) and removed at a fixed rate (k), its rate of change would be
dX/dt = c•PO2 - k
where c and k are constants. When
integrated, this first order differential equation gives
X = (c•PO2 - k)•t (1)
The risk of toxicity is
specified by a separate function of X.
Equation 1 defines a family of rectangular
hyperbolas proposed empirically for the pressure-time relationship of pulmonary
and CNS oxygen toxicity (Clark 1974). Statistical modelling derives this
relationship theoretically and finds the constants c and k directly from
experimental data (Vann 1988). This allows the risk of toxicity to be estimated
for any oxygen exposure.
Figure 6 shows three rectangular
hyperbolas for 2%, 5%, and 8% risks of either symptoms or convulsions. These
were estimated from data on 773 pure oxygen exposures. The convulsions,
represented by black dots in Fig. 6, occurred at estimated risks of 2-8%. In a
context of risk, an oxygen exposure limit is the depth and time at the level of
risk which is judged to be acceptable. In Fig. 6, for example, the limit for a
pure oxygen exposure at 25 fsw (1.76 bar) would be 49 min if a 2% risk of either
symptoms or convulsions were judged acceptable. The level of acceptable risk for
a chamber dive where immediate rescue is possible after a convulsion is greater
than for an open-water dive where drowning is the likely outcome.
Statistical modeling can track the
resolution of risk as well as its development. In Fig. 7, for example, a pure
oxygen diver spends 120 min at 20 fsw, 15 min at 40 fsw, and 105 min at 20 fsw.
His risk increases gradually to 0.2% while at 20 fsw and rapidly to 4.1% at 40
fsw. The maximum risk of 4.3% occurs just before surfacing after which the risk
resolves in 10 min.
Unfortunately, the accuracy of the risk
estimates of Figs. 6 and 7 is uncertain because human oxygen exposure data are
limited and their results variable (Donald 1992; Clark 1993). This uncertainty
encourages conservative exposure limits, at present, instead of permitting the
oxygen exposure to be adjusted continuously such that the estimated risk never
exceeds the risk judged to be acceptable. For mixed gas, even less data are
available than for pure oxygen, and the potential for carbon dioxide retention
introduces further uncertainty which makes modeling of mixed gas risk even more
problematic.
What Are
"Safe" Oxygen Exposure Limits?
The choice of "safe" oxygen exposure
limits depends upon the risk of convulsions that one is willing to accept. This
subjective judgment is rendered all the more difficult because so few data are
available from which to estimate risk and because there is so much variability
in the response to oxygen exposure. Variability can be due to exercise, carbon
dioxide retention, gas analysis error, oxygen set-point control, and
susceptibility to oxygen toxicity from inter- and intra-individual differences.
For air or enriched air diving, a maximum
exposure limit of 1.2 bar would appear to be conservative while allowing a
"cushion" for oxygen partial pressure increases due to unplanned depth
excursions. Perhaps 1.4 bar would be acceptable if depth could be carefully
controlled. On the other hand, there are those who testify to diving safely at
1.6 bar. This may well be true, but skepticism is appropriate until these divers
document their claims in the form of computer-recorded depth-time profiles with
certified breathing mixtures (Fig. 5). Denoble et al. (1993) describe a project
and data acquisition software which might help to provide such documentation.
For pure oxygen, commercial (Imbert and
Bontoux 1987) and scientific experience (Fife et al. 1992) suggests that at
least 30 min of in-water oxygen decompression may be possible at 1.61 bar (20
fsw) with little risk of CNS toxicity. Experimental data (Fig. 4) also suggest a
low risk at 1.76 bar (25 fsw), but a small depth excursion can cause large
increases in oxygen pressure. Pure oxygen diving at depths below 20 fsw is more
hazardous.
Improvements in our ability to manage
oxygen exposure are expected as basic studies illuminate the fundamental
biochemistry and physiology, as additional exposure data become available, and
as statistical modeling methods develop. Basic studies have already led to
pharmacological methods for extending oxygen exposure in mice (Oury et al.
1992), but further work is needed before such methods are applied to humans. The
diving community itself can provide some of the necessary exposure data should
it adopt a rigorous approach to data collection. Statistical modeling and
computer tracking of oxygen exposure may eventually lead to guidelines for
variable oxygen partial pressures to supplement single stage oxygen limits (Fig.
3). A particularly important advance that might eliminate much of the current
unpredictability would be a mouthpiece sensor for measuring end-inspired and
end-expired carbon dioxide. In the meantime, a patient and conservative approach
to oxygen exposure management is appropriate to minimize the frequency of
mishaps such as those of the past year.
After graduating in 1965 with a B.S. in
mechanical engineering from Columbia University, Richard Vann worked as a diving
engineer at Ocean Systems, Inc. on Sealab III life support systems and as a
research subject during experimental dives. Following four years in the Navy,
two as Diving Officer for Underwater Demolition Team TWELVE, he attended Duke
University graduating in 1976 with a Ph.D. in biomedical engineering. Since
then, he has conducted research at the F.G. Hall Hypo/Hyperbaric Center of Duke
Medical Center on bubble formation, inert gas exchange, decompression
procedures, oxygen toxicity, breathing apparatus design, and biomaterials. Dr.
Vann is currently an Assistant Research Professor in Anesthesiology, Director of
Applied Research at the Hall Center, and Research Director of the Divers Alert
Network. He can be contacted at: Box 3823, Duke University Mediacal Center,
Durham, NC 27710, fax: 919-684-6002
More Information:
Butler F K Jr., Thalmann E D 1984. CNS
oxygen toxicity in closed-circuit scuba divers. In: Underwater Physiology VIII.
Eds. A.J. Bachrach and M.M. Matzen. UMS, Inc., Bethesda.
Butler F K Jr., and Thalmann E D 1986. CNS
oxygen toxicity in closed-circuit scuba divers. II. Undersea Biomed. Res. 13(2):
193-223.
Clark J M 1974. The toxicity of oxygen.
Am. Rev. Resp. Dis. 110:40-50.
Clark J M 1993. Oxygen toxicity. In: The
physiology and medicine of diving, 4th edn., pp. 121-169. Ed. P.B. Bennett and
D.H.Elliott. London: W.B. Saunders.
Denoble P, Dear G deL, Vann R D 1993. The
epidemiology of decompression illness: a data collection project. Durham, NC;
Divers Alert Network. Version 1.01.
Donald K 1992. Oxygen and the Diver. The
SPA Ltd. Worcs.
Fife C E, Pollard G W, Mebane G Y , Boso A
E, Vann R D 1992. A database of open water, compressed air, multi-day repetitive
dives to depths between 100 and 190 fsw. In: Proceedings of repetitive diving
workshop. M.A. Lang and R.D. Vann (eds.). American Academy of Underwater
Sciences. AAUSDSP-RDW-02-92. Pp. 45-54.
Imbert J P, Bontoux M. 1987. Production of
procedures: COMEX. In: Decompression in surface-based diving. Eds. I. Nashimoto
and E.H. Lanphier. 36th UHMS Workshop. Pub. No. 73(DEC)6/15/87. Pp. 90-100.
Lanphier E H, Dwyer J V 1954. Diving with
self-contained underwater breathing apparatus. NEDU Report 11-54.
Lanphier E H 1955. Nitrogen-oxygen mixture
physiology. Phases 1 and 2. NEDU Report 7-55.
Lanphier E H (Editor). 1982. The
unconscious diver: respiratory control and other contributing factors. Undersea
Medical Society Publication Number 52WS (RC) 1-25-82.
Lanphier E H 1992. The story of CO2
build-up. aquaCorps J. 3(1): 67-69.
Menduno M 1992. Safety first: an analysis
of recent diving accidents. Technical Diver. 3(2): 2-10.
NOAA 1979. NOAA Diving Manual 1979, 2nd
edn. U.S. Department of Commerce, December 1979.
NOAA 1991. NOAA Diving Manual 1991, 3nd
edn. U.S. Department of Commerce, October 1991.
Oury T D, Ho Y S, Piantadosi C A, Crapo J
D 1992. Extracellular superoxide dismutase, nitric oxide, and central nervous
system O2 toxicity. Proc. Nat. Acad. Sci. 89: 9715-9719.
Piantadosi C A, Clinton R L, Thalmann E D
1979. Prolonged oxygen exposures in immersed exercising divers at 25 fsw (1.76
ATA). Undersea Biomed. Res. 6: 347-356.
Schwartz H J C 1984. Manned testing of two
closed-circuit underwater breathing apparatus: U.S. Navy Emerson rig and Fenzy
PO.68. NEDU Report 13-84.
USN 1973. U.S. Navy Diving Manual, Change
1, Tables 9-20 and 13-1.
Vann R D 1982. MK XV UBA Decompression
trials at Duke: A summary report. Final Report on Office of Naval Research
Contract N00014-77-C-0406.
Vann R D 1988. Oxygen toxicity risk
assessment. Final Report on ONR Contract N00014-87-C-0283.
Vann R D, Gerth W A, Southerland D G,
Stanton G R, Pollock N, Kepper W, Heinmiller P. 1992. No-stop repetitive N2/O2
diving with Surface Interval O2 (SIO2): Phase II. Undersea Biomed. Res.
19(Suppl.): 80.
Vann R D and Thalmann E D 1993.
Decompression physiology and practice. In: The Physiology and medicine of
Diving, 4th edn., pp. 376-432. Ed. P.B. Bennett and D.H. Elliott. London: W.B.
Saunders.
Warkander D E, Norfleet W T, Nagasawa G K,
Lundgren C E G. 1990. CO2 retention with minimal symptoms but severe dysfunction
during wet simulated dives to 6.8 atm abs. Undersea Biomed. Res. 17(6): 515-523.
Figure Captions
1. The production of ATP during the
breakdown of sugar at normal (normoxic) oxygen partial pressures.
2. The production of ATP and reactive
oxygen species during the breakdown of sugar at elevated (hyperoxic) oxygen
partial pressures.
3. Oxygen exposure limits for pure oxygen
and for oxygen in mixed gas as published by NOAA and the U.S. Navy. The 1973
U.S. Navy limits (USN 1973) were adopted for the 1979 NOAA Diving Manual (NOAA
1979). These are indicated as USN/NOAA 1979. The Navy revised its pure oxygen
limits in 1986 (Butler and Thalmann 1986). NOAA revised its pure oxygen and
mixed gas limits in 1991 (NOAA 1991). Exposure times and pressures are connected
by line segments to facilitate comparisons. Field application requires step
changes at the indicated points. The original references should be consulted for
operational use.
4. CNS oxygen toxicity data (convulsions
and symptoms) from U.S. experiments with wet, working divers exposed to constant
oxygen partial pressures (Lanphier and Dwyer 1954; Lanphier 1955; Piantadosi et
al. 1979; Vann 1982; Schwartz 1984; Butler and Thalmann 1984, 1986; Butler 1986;
Lanphier 1992). The 1991 NOAA exposure limits for pure oxygen and mixed gas are
shown for comparison (NOAA 1991).
5. The depth-time profile recorded by a
dive computer for an exposure on 32.8% nitrox at a nominal depth of 80 fsw and
oxygen partial pressure of 1.26 bar. The dive was terminated at 34 min by a
convulsion. After rescue, the diver was found to have an unreported history of
convulsions and to be on anti-convulsant medication.
6. Estimates of CNS oxygen toxicity risk
based upon a statistical model (Vann 1988). The model was fitted to experimental
data from 773 pure oxygen exposures which resulted in 11 convulsions and 33
incidents of symptoms. Exposures for estimated risks of 2, 5, and 8% are shown
with the observed convulsions.
7. The development and resolution of CNS
oxygen toxicity risk according to the model of Fig. 6 during a multi-level dive
on pure oxygen.
|