During pre-immersion, these variables were higher than normal due to the anxiety attending
imminent immersion in cold water. More typical pre-immersion values for this subject are
known for mean arterial pressure and heart rate during regular daytime activity as a
university professor, and these have been plotted also. Upon cold water immersion, all
three variables were elevated above normal by 10-25 %. Thereafter to 100 min, each
increased fairly uniformly, with mean arterial pressure reaching 140 mmHg, cardiac output
8.71 min-1 and heart rate, 85 beats min-1 At this stage, cardiac output showed the
greatest increase (64 %) from the normal, pre-immersion level, while mean arterial
pressure and heart rate had increased approximately 25 %. Pulse pressure during cooling
was in the range of 80-100 mmHg. The changes in cardiac output during cooling are
appropriate to standard predictions (Altman and Ditter, 1971) in relation to the
non-exercising metabolic response (Hayward et al., 1977) to immersion in 10°C water.
During rewarming, similar cardiovascular responses
(Figure 5) were observed for the no exogenous heat and
inhalation conditions, both showing decreases in cardiac output to near the pre-immersion
level by 30 min. This was associated with declines in heart rate and mean arterial
pressure to normal levels, although for the inhalation condition, mean arterial pressure
remained 10-15 % higher, and heart rate 10-15 % lower than for no exogenous heat.
Considerably-different responses occurred with the bath treatment. During the first 15
min, mean arterial pressure showed a large decrease to approximately 95 mmHg, a
hypotensive level for this individual. From 20 min onward, further decline was arrested by
an abrupt, 55 % increase in heart rate (of about 40 beats min-1) which produced a 30-35 %
increase in cardiac output. During the first 30 min of rewarming, pulse pressures fell
from the elevated range during cooling to approximately 60-70 mmHg for all three
conditions.
Peripheral resistance and stroke volume.
These cardiovascular variables were calculated from those
measured. During cooling, total peripheral resistance was steady in the range of 15-20
mmHg .1-1 min. During rewarming, total peripheral resistance was near 20 mmHg 1-1 min for
the no exogenous heat and inhalation treatments, but fell to 10 mmHg 1-1 min early in the
bath treatment. Stroke volume averaged 0.09 litters and no major changes occurred with
cooling or rewarming.
DISCUSSION
These results show that the four sites of measurement of core
temperature provide similar information on rate of progress into hypothermia, thereby
enabling rectal or tympanic temperature to be used for initial assessment of the level of
hypothermia when a victim is first removed from severe cold stress. However, it is clear
that during the more dynamic events of early resuscitation, when thermal gradients in the
body are being reduced or reversed, there are considerable differentials among the various
sites used to assess core temperature.
During the early period of treatment, rectal and tympanic
temperatures do not adequately reflect temperature changes of the "critical
core" as represented by cardiac temperature. Consequently, these two sites should not
be used as prime criteria for experimental evaluation of the effectiveness of various
treatments for accidental hypothermia.
On the contrary, deep esophageal temperature is a reliable
analogue of cardiac temperature. This was true even when exogenous heat was donated by the
airway, and validates previous interpretations concerning inhalation rewarming which were
based on esophageal temperature (Hayward and Steinman, 1975).
Due to the inappropriateness of routine use of cardiac
catheterization in experimental evaluations of rewarming techniques in conscious humans,
esophageal temperature should be utilized for definitive judgment of the effectiveness of
core rewarming.
The present findings on temperature differentials in the core
during rewarming yield similar conclusions to those derived previously from studies of
anaesthetized patients being rewarmed from hypothermic surgery (Cooper and Kenyon, 1957;
Severinghaus, 1959). However, in the present study. differences among patterns of change
in the various core temperatures are more accentuated. This is probably a result of the
strong vasoconstrictive response in conscious humans during cold stress, which produces a
larger core-to-shell thermal gradient than in anaesthetized patients entering hypothermia
passively.
Reports (Guild, 1978; Marcus, 1978) have concluded (without
measuring cardiac temperature) that inhalation rewarming, due to the small amount of
heat that can be potentially donated, is not more effective than endogenous heat
production alone (spontaneous condition). The present results do not support this
contention.
Cardiac temperature rose with inhalation at twice the rate
observed for no exogenous heat. If "effectiveness" of rewarming is more
appropriately evaluated on the basis of heart or deep esophageal temperatures, rather than
rectal and aural temperature or amount of heat transferred to the body, then inhalation
therapy appears justified.
In cases of severe hypothermia, where ventilation rate is low in
semi-comatose victims, the thermal effect of the inhalation method would be reduced, but
the same condition would also greatly lower the endogenous heat production, making a small
amount of exogenous heat that is donated directly to the thoracic core even more
important. This is validated by the work of Shanks (1975).
The benefit of heat donation
via the airway in severely
hypothermic victims is in addition to the insulative effect of this method of
therapy, namely the avoidance of respiratory heat loss. This factor is particularly
important when first-aid for hypothermia must be provided in the common rescue situation
where the ambient air is very cold.
The combination of airway insulation and heat donation would
increase the probability that cardiac temperature could be stabilized, whereas a
victim with low endogenous heat production and lack of protection from respiratory heat
loss may not be able to avoid further cooling of the heart to much colder peripheral
tissues.
It is important to emphasize that under the conditions of this
experiment, no afterdrop of cardiac temperature occurred with either the spontaneous or
inhalation treatments.
In contrast, bath rewarming did cause a further decline in
cardiac temperature during the initial phase of treatment.
Whereas the afterdrop of rectal temperature which occurred with
all treatments is mainly due to continued heat loss down a thermal gradient in the tissues
towards the colder periphery (Golden and Hervey, 1977), the mechanism of cardiac afterdrop
is more likely due to increased return, centrally, of colder blood from the body shell in
conjunction with decreased peripheral vasoconstriction. The cardiovascular findings of
this study support this proposition because the decreased peripheral resistance (deduced
from the fall in mean arterial pressure and rise in cardiac output) coincided with the
period of afterdrop of cardiac and esophageal temperatures. This
"circulation-induced" afterdrop was associated with raising of the skin
temperature to thermoneutral temperature and above, even though core temperatures were at
their lowest levels.
This confirms experimentally, for the first time in conscious
humans, the long-suspected increase in peripheral circulation which accompanies
"aggressive", external donation of heat to the whole body.
As has already been demonstrated for the thermogenic (shivering)
response during hypothermia of the core (Hayward et al., 1977), maintenance of maximal
peripheral vasoconstriction is dependent on a cold skin.
If this phenomenon also applies to cases of severe hypothermia
(e.g. core temperatures <30°C), then the cardiac afterdrop accompanying bath rewarming
would increase the probability of attaining a sufficiently low temperature to cause
ventricular fibrillation (Keatinge, 1977).
The magnitude of the cardiac afterdrop was relatively small in
the strongly-shivering subject of this study, but could be much larger in a comatose
victim with severe hypothermia.
Cardiac dysfunction would also be enhanced by probable
biochemical disturbances (pH, K+) in the blood returning to the heart from peripheral
tissues which had been relatively ischaemic during a long cooling phase. Such thermal and
chemical challenges to the myocardium would occur just at the time when cardiac excitation
was required to compensate for the relative hypotension derived from peripheral dilation
in response to warm (>30°C) skin temperature. This process or any other factor (such
as limb movement) which would increase the return of peripheral blood to the heart would
be similarly contraindicated during resuscitation from severe hypothermia, even in a
hospital situation where "total physiological control" is often available
(Stine, 1977; Martyn, 1981; Samuelson et al., 1982).
It is important to emphasize that these interpretations from the
present findings are most relevant to first-aid strategies for management of hypothermia
victims at the rescue site or during transport.
This is because the most potentially-dangerous thermal and
cardiovascular events are likely to occur during the first 20-30 min immediately after
removal of the extreme, external cold stress.
By the time a victim who became hypothermic in the water or on a
mountainside is transported to hospital (if that is actually possible), the maximum
potential for cardiac dysfunction due to thermal, chemical and mechanical (Golden, 1973)
stimuli has probably already occurred.
These results confirm the general recommendation (Samuelson et
al., 1982) that unless rescuers are certain that a victim of core cooling has only mild to
moderate hypothermia (e.g. rectal temperature 32 0 C), rapid peripheral heating of the
whole body and exercise should be avoided, with any sources of exogenous heat being
donated to the thoracic and neck regions, the primary aim being to stabilize cardiac
temperatures and secondarily, to facilitate gradual rewarming of the core.
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