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Influence of body temperature on development of fatigue during prolonged exercise in the heat

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We investigated whether fatigue during prolonged exercise in uncompensable hot environments occurred at the same critical level of hyperthermia when the initial value and the rate of increase in body temperature are altered. To examine the effect of initial body temperature [esophageal temperature (Tes) = 35.9 +/- 0.2, 37.4 +/- 0. 1, or 38.2 +/- 0.1 (SE) degrees C induced by 30 min of water immersion], seven cyclists (maximal O2 uptake = 5.1 +/- 0.1 l/min) performed three randomly assigned bouts of cycle ergometer exercise (60% maximal O2 uptake) in the heat (40 degrees C) until volitional exhaustion. To determine the influence of rate of heat storage (0.10 vs. 0.05 degrees C/min induced by a water-perfused jacket), four cyclists performed two additional exercise bouts, starting with Tes of 37.0 degrees C. Despite different initial temperatures, all subjects fatigued at an identical level of hyperthermia (Tes = 40. 1-40.2 degrees C, muscle temperature = 40.7-40.9 degrees C, skin temperature = 37.0-37.2 degrees C) and cardiovascular strain (heart rate = 196-198 beats/min, cardiac output = 19.9-20.8 l/min). Time to exhaustion was inversely related to the initial body temperature: 63 +/- 3, 46 +/- 3, and 28 +/- 2 min with initial Tes of approximately 36, 37, and 38 degrees C, respectively (all P < 0.05). Similarly, with different rates of heat storage, all subjects reached exhaustion at similar Tes and muscle temperature (40.1-40.3 and 40. 7-40.9 degrees C, respectively), but with significantly different skin temperature (38.4 +/- 0.4 vs. 35.6 +/- 0.2 degrees C during high vs. low rate of heat storage, respectively, P < 0.05). Time to exhaustion was significantly shorter at the high than at the lower rate of heat storage (31 +/- 4 vs. 56 +/- 11 min, respectively, P < 0.05). Increases in heart rate and reductions in stroke volume paralleled the rise in core temperature (36-40 degrees C), with skin blood flow plateauing at Tes of approximately 38 degrees C. These results demonstrate that high internal body temperature per se causes fatigue in trained subjects during prolonged exercise in uncompensable hot environments. Furthermore, time to exhaustion in hot environments is inversely related to the initial temperature and directly related to the rate of heat storage.
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Influence of body temperature on the development
of fatigue during prolonged exercise in the heat
JOSE
´GONZA
´LEZ-ALONSO, CHRISTINA TELLER, SIGNE L. ANDERSEN,
FRANK B. JENSEN, TINO HYLDIG, AND BODIL NIELSEN
Human Physiology Department, August Krogh Institute,
University of Copenhagen, DK-2100 Copenhagen, Denmark
Gonza´lez-Alonso, Jose´, Christina Teller, Signe L.
Andersen, Frank B. Jensen, Tino Hyldig, and Bodil
Nielsen. Influence of body temperature on the development
of fatigue during prolonged exercise in the heat. J. Appl.
Physiol. 86(3): 1032–1039, 1999.—We investigated whether
fatigue during prolonged exercise in uncompensable hot
environmentsoccurred atthe samecritical levelof hyperther-
mia when the initial value and the rate of increase in body
temperature are altered. To examine the effect of initial body
temperature [esophageal temperature (Tes)35.9 0.2,
37.4 0.1, or 38.2 0.1 (SE) °C induced by 30 min of water
immersion], seven cyclists (maximal O2uptake 5.1 0.1
l/min) performed three randomly assigned bouts of cycle
ergometer exercise (60% maximal O2uptake) in the heat
(40°C) until volitional exhaustion. To determine the influence
of rate of heat storage (0.10 vs. 0.05°C/min induced by a
water-perfusedjacket), fourcyclists performedtwo additional
exercise bouts, starting with Tes of 37.0°C. Despite different
initialtemperatures, allsubjects fatiguedat anidentical level
of hyperthermia (Tes 40.1–40.2°C, muscle temperature
40.7–40.9°C,skin temperature 37.0–37.2°C)andcardiovas-
cular strain (heart rate 196–198 beats/min, cardiac output
19.9–20.8 l/min). Time to exhaustion was inversely related to
the initial body temperature: 63 3, 46 3, and 28 2min
with initial Tes of 36, 37, and 38°C, respectively (all P
0.05). Similarly, with different rates of heat storage, all
subjects reached exhaustion at similar Tes and muscle tem-
perature (40.1–40.3 and 40.7–40.9°C, respectively), but with
significantly different skin temperature (38.4 0.4 vs. 35.6
0.2°C during high vs. low rate of heat storage, respectively,
P0.05). Time to exhaustion was significantly shorter at the
high than at the lower rate of heat storage (31 4 vs. 56 11
min, respectively, P0.05). Increases in heart rate and
reductions in stroke volume paralleled the rise in core
temperature(36–40°C), withskin bloodflowplateauing atTes
of 38°C. These results demonstrate that high internal body
temperature per se causes fatigue in trained subjects during
prolonged exercise in uncompensable hot environments. Fur-
thermore, time to exhaustion in hot environments is in-
versely related to the initial temperature and directly related
to the rate of heat storage.
hyperthermia; skin blood flow; heart rate; stroke volume
IT IS WELL DOCUMENTED that endurance can be impaired
in hot compared with temperate climates (10, 12, 28)
and that time to exhaustion is influenced by alterations
of the initial body temperature (1, 22, 32, 39). The
attainment of a critically high level of body tempera-
ture has been proposed as the main factor limiting
endurance performance in hot environments (7, 28).
The observation that trained subjects working at 60%
of peak O2uptake (V
˙O2peak) in the heat [40°C, 10%
relative humidity (RH)] for 9–12 consecutive days
improved exercise performance from 48 to 80 min but
fatigued at a core temperature of 39.7°C appears to
support this notion (28). This large improvement in
exercise time to fatigue, however, was drastically re-
duced to 7 min when subjects exercised in a humid hot
environment, yet fatigue still coincided with a core
temperature of 40°C (30). In the same light, Mac-
Dougal et al. (24) previously showed that subjects
always became exhausted at a rectal temperature of
39.4°C, even though the rate of rise had been varied
markedly with a water-perfused suit. More recently,
Fuller et al. (11) found that rats exercising in a hot
environment fatigued at the same abdominal and brain
temperature (40°C) after preexercise body tempera-
ture was altered.
In opposition to the hypothesis of a critically high
body temperature, there are reports indicating that
some untrained subjects fatigue during light exercise
in uncompensable environments with body tempera-
tures of 38°C (23, 26, 38). In untrained subjects, core
temperature at exhaustion from heat strain has been
clearly shown to occur over a range of 38–40°C (23, 26,
38) and to be independent of exercise intensity (26). It
has also been shown that, regardless of hydration or
acclimation status, subjects with high aerobic fitness
perform longer in uncompensable hot environments
and tolerate higher levels of hyperthermia than do
subjects with lower aerobic fitness levels (7). Therefore,
it appears that high body temperature might be the
mainfactorleading tofatigue in theheat in trainedand
in some, but not all, untrained subjects.
Although previous human studies have emphasized
the importance of core temperature, little is known
about exercising muscle temperature at exhaustion.
High muscle temperature might induce structural and
functional alterations in proteins involved in 1) electro-
lyte distributions across the sarcolemma, 2) calcium
release and reuptake by the sarcoplasmic reticulum, 3)
actin-myosin interactions, and 4) mitochondrial respi-
ration, which might potentially contribute to fatigue
(19). However, no previous study has systematically
manipulated the initial value and the rate of rise of
body temperature to determine whether fatigue in hot
environments is related to critically high core and/or
muscle temperatures.
It is also well established that heat stress reduces
stroke volume (SV) and increases heart rate during
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8750-7587/99 $5.00 Copyright r1999 the American Physiological Society1032 http://www.jap.org
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moderately intense exercise to the extent to which
cardiac output might be compromised (35). In a classic
study, Rowell et al. (35) showed a significantly lower
cardiac output (1.0 l/min), central blood volume, and
SV during exercise in a 43°C than in a 26°C environ-
ment at 63–73% V
˙O2peak. This reduced cardiac output
was due to the larger reductions in SV compared with
the parallel increases in heart rate. In a follow-up
study, Rowell et al. (36) found that alterations in
central blood volume, central venous pressure, SV, and
heart rate with heat stress could be restored by perfus-
ing a suit in contact with skin with cold water. In these
previous studies, however, skin blood flow was not
measured. Thus the contribution of higher skin perfu-
sion to SV reductions in conditions of widely different
body temperature remains unknown.
Therefore, the main aim of this study was to investi-
gate whether fatigue in trained athletes occurred at the
same critical level of core and muscle temperature,
despite differences in starting internal temperature
and its rate of rise. Asecondary aim was to determine
the effect of increased body temperature on heart rate,
SV, and skin blood flow under conditions of rather
different initial body temperatures. We hypothesized
that a similar critical level of internal body tempera-
ture would cause fatigue in trained athletes in uncom-
pensable hot environments. Furthermore, we hypoth-
esized that reductions in SV with heat stress are also
influenced by factors other than elevations in skin
blood flow. This hypothesis is based on previous obser-
vations showing that SV declines significantly with
core hyperthermia alone and combined hyperthermia
and hypovolemia when skin blood flow plateaus or
declines during prolonged exercise in the heat (13, 15,
16, 25).
METHODS
General Design
To accomplish these purposes, two different studies were
performed. To identify the effect of different initial body
temperature, one study was performed in the heat after core
temperature had been manipulated to three different levels
(36,37, and38°C) byhaving subjects restin awater tankfor
30 min. Another study examined the influence of the rate of
increase in body temperature (0.05 vs. 0.10°C/min) on heat
exhaustion during prolonged exercise by having subjects
wear a water-perfused jacket.
Subjects
Age, body weight, height, maximal heart rate, and maxi-
mal O2uptake (V
˙O2max) of the seven healthy endurance-
trained men participating in these studies were 28 3yr,
77.9 6.4 kg, 187 6 cm, 200 9 beats/min, and 5.13 0.30
l/min, respectively. The subjects were fully informed of any
risks and discomforts associated with the experiments before
givingtheir informedconsent toparticipate. Thestudies were
approved by the Ethics Committee of Copenhagen and Fred-
eriksberg communities. Before performing the experimental
trials,subjects werefamiliarized withthe experimentalsetup
by cycling in a thermoneutral environment (20°C) for 90
min. Most of the subjects had participated in experiments
involving endurance performance in hot environments before
undergoing these experiments.
Experimental Design
In the study of the initial body temperature, subjects
performed three bouts of cycle ergometer exercise (model 829
E, Monark; 228 6W,881 rpm, 60% V
˙O2max)inan
uncompensable hot environment (40°C, 19% RH; Ereq/Emax
1.2, where Ereq is evaporation required for heat balance and
Emax ismaximal evaporationcapacity) untilvolitionalexhaus-
tion. The following criteria were used to define volitional
fatigue in the present studies: 1) near or maximal values of
perceived exertion, 2) near or maximal heart rate, and 3)
inability to maintain a cadence of 50 rpm. Trials were
randomly assigned and counterbalanced across subjects. Be-
fore exercise, resting body temperatures were manipulated
byimmersing subjectsin waterat 17,36, and40°Cfor 30min.
The conditions were as follows: 1) precooling (C) to an
esophageal temperature (Tes) of 35.9 0.2°C, a muscle
temperature (Tm) of 34.3 0.3°C, and an average skin
temperature (Tsk) of 29.5 0.3°C, 2) control (Con) with Tes of
37.4 0.1°C, Tmof 37.3 0.1°C, and Tsk of 34.2 0.1°C, and
3) preheating (H) to Tes of 38.2 0.1°C, Tmof 38.4 0.1°C,
and Tsk of 35.9 0.1°C (Figs. 1 and 2).
On the day before the experimental testing, the subjects
adopted the same diet, exercise bout (i.e., 1hoflow-
intensity cycling), and fluid intake to standardize the hydra-
tion status. The subjects reported to the laboratory 1h
before the experiment, after ingestion of a light breakfast and
200–300 ml of fluid. On arrival, nude body weight was
recorded. Thereafter, the esophageal probe was inserted
through the nasal passage, and the instruments used to
measureforearm bloodflow,skinblood flow,andskin tempera-
ture were attached to the skin. Thereafter, baseline values of
skin blood flow were obtained while subjects sat for 5–10 min
in a standardized position in the heat. The subjects then
restedfor 30min whileimmersed ina watertank. Thereafter,
subjects toweled dry and walked to the climatic chamber. The
transition period from the time the subjects emerged from the
water tank to the start of exercise was 8–12 min, with the
shortest time occurring during the preheating trial. Tmwas
measured immediately before and after exercise.
During exercise, heart rate, Tes, Tsk, and skin blood flow
were recorded continuously. O2uptake (V
˙O2), cardiac output
(CO2rebreathing), and forearm blood flow were measured
during a 10-min period starting at 3 min of exercise and
before exhaustion (when Tes was 39.5°C). Forearm blood
flow was also measured during the 20- to 25-min period of C
and Con. Blood samples by finger prick were also obtained
before and immediately after exercise for later analysis of
blood glucose and lactate. Nude body weight was recorded
immediately after sweat was wiped off.A rating of perceived
exertion (RPE) was obtained at 10 min and at exhaustion (2).
Subjects received similar encouragement during each of the
trials.
The same control of previous exercise, nutrition, and
hydration status was applied in the study of the rate of heat
storage. On the subjects’ arrival at the laboratory, their nude
body weight was recorded. Skin and esophageal thermo-
couples were then attached to the skin or inserted through
the nasal passage, respectively. Thereafter, subjects rested
for 30 min in the supine position to ensure a similar initial
body temperature before exercise.
In this follow-up study, subjects performed two randomly
assignedbouts ofcycle ergometerexercise(258 20W,872
rpm, 66 3% V
˙O2max) in the heat (41°C, 17% RH) until
volitional fatigue. During exercise the rate of heat storage
1033HYPERTHERMIA AND FATIGUE
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was manipulated by changing the water temperature perfus-
ing the jacket in contact with the skin of the trunk and
forearms (42 vs. 19°C, i.e., high vs. low rate of heat storage).
However, in this study the initial Tes and Tmwere similar in
both trials: 36.9–37.1 0.1 and 36.3–36.5 0.2°C, respec-
tively. During exercise, heart rate was recorded continuously.
An RPE was obtained at 10 min and at exhaustion.
V
˙O2and Cardiac Output
PulmonaryV
˙O2wasmeasured on-linewith ametabolic cart
(model CPX/D, Medgraphics, St. Paul, MN). Cardiac output
was measured in triplicate using the CPX/D computerized
version of the CO2-rebreathing technique of Collier (8) and
corrected for differences between end-tidal and arterial PCO2
(21). Under similar exercise conditions, we previously ob-
served a tight temporal correlation between end-tidal and
arterial PCO2as well as between the estimated mixed venous
PCO2and femoral venous PCO2(r0.85–0.91, P0.0001)
(13). Heart rate was recorded with a PE 3000 Sport Tester
(Polar Electro).
Forearm Blood Flow and Skin Blood Flow
Forearm blood flow was measured using venous occlusion
plethysmography with a mercury-in-Silastic strain gauge
(40), while the wrist of the left forearm rested in a sling. The
hand was elevated 15 cm above the heart level, and the
forearm was tilted 40° from the horizontal axis. Forearm
blood flow values represent the average of 8–10 single
measurements. Skin blood flow was measured using a laser-
Doppler flowmeter (model PF2B, Perimed, Stockolm, Swe-
Fig. 1. Esophageal temperature (A), mean skin temperature (B),
heart rate (C), and skin blood flow (D) during exercise in heat (40°C,
17% relative humidity) during precooling, control, and preheating
trials. Skin blood flow is referenced to resting baseline values
obtained on arrival at the laboratory (0.2–1.2 V; n4). Values are
means SE for 7 subjects. *Significantly different from control,
P0.05.
Fig. 2. Heart rate (A), cardiac output (B), stroke volume (C), skin
blood flow (D), and forearm blood flow (E) plotted against core
temperature during precooling, control, and preheating trials. Values
are means SE for 6 subjects.
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den). The laser-Doppler probe was placed on the left forearm
on the dorsal side, separated 2 cm from the plethysmo-
graphic strain gauge. Skin blood flow and forearm blood flow
were recorded at 100 Hz with use of a MacLab/8s (AD
Instruments) data-acquisition system.
Core, Skin, and Muscle Temperature
Tes was measured with a thermocouple (model MOV-A,
Ellab) inserted through the nasal passage a distance equal to
one-fourth of the subject’s standing height. Tsk was calculated
from the skin temperatures (model A-H3, Ellab) measured at
six sites (i.e., upper arm, forearm, chest, back, thigh, and calf)
byusing theweighting methodof Hardyand DuBois(18). The
esophageal and skin thermocouples were connected to a
recorder (CTF 90008 precision thermometer, Ellab) inter-
faced to an IBM-AT computer. Tmwas measured in the vastus
lateraliswith aneedle probe(model MKA-A,Ellab) inserted3
cm into the muscle.
Percent Dehydration
Percent dehydration was estimated from the differences in
body weight after exercise compared with the preexercise
body weight, with correction for body weight loss due to the
exchange of O2and CO2(33). Nude body weight was deter-
mined on a platform scale (model 1-10, Ohaus) with an
accuracy of 20 g.
Statistical Analysis
A two-way (trial-by-time) repeated-measure ANOVA was
performed to test significance between and within treat-
ments. After a significant Ftest, pairwise differences were
identified using Tukey’s honestly significant difference post
hocprocedure. Whenappropriate, significantdifferenceswere
also identified using Student’s paired t-tests. The significance
level was set at P0.05. Values are means SE unless
otherwise indicated.
RESULTS
Influence of Different Initial Body Temperatures
Body temperatures and performance time. Despite
different initial temperatures, all subjects fatigued at
an identical level of hyperthermia: Tes of 40.1 0.1,
40.2 0.1, and 40.1 0.1°C, Tmof 40.7 0.1, 40.8
0.1, and 40.9 0.1°C, and Tsk of 37.2 0.2, 37.2 0.1,
and 37.0 0.1°C during C, Con, and H, respectively
(Fig. 1, Table 1). In three trials the between-subjects
difference in Tes at exhaustion was 0.1–0.5°C (Table 1).
The rate of heat storage during exercise was the same
in the three conditions. Therefore, time to exhaustion
was inversely related to starting body temperatures:
63 3, 46 3, and 28 2 min in C, Con, and H,
respectively (all P0.05).
Hydration status. Hydration was similar before exer-
cise, as indicated by similar body weights: 76.6 6.6,
77.1 5.8, and 76.4 6.1 (SD) kg before C, Con, and H,
respectively [not significant (NS)]. Furthermore, simi-
lar body weight losses occurred from the start of water
immersion to the end of exercise: 2.0 0.3, 1.9 0.3,
and 2.1 0.2 kg during C, Con, and H, respectively
(PNS).Therefore,the levelof dehydration atexhaus-
tion was also similar in each trial: 2.6 0.4, 2.4 0.3,
and 2.8 0.3% body wt loss during C, Con, and H,
respectively (PNS).
Cardiovascular responses. After 10 min of exercise,
V
˙O2was similar during all conditions (range 3.05
0.05 to 3.11 0.13 l/min), despite the 2.4°C difference
in Tes between C and H. Thereafter, V
˙O2tended to
increase over time. In contrast, cardiac output, SV, and
heart rate were graded in proportion to the magnitude
of hyperthermia. Cardiac output was 22.5 1.1, 21.8
0.8, and 20.3 0.5 l/min, SV was 152 7, 126 6, and
1094ml/beat (allP0.05), andheartrate was140
5, 166 5, and 182 4 beats/min (all P0.05) with Tes
of 36.5, 38.3, and 38.9°C for C, Con, and H, respectively
(Fig. 2). Cardiac output was significantly (P0.05)
lower during H than during C (2.2 0.9 l/min), yet the
differences between these two trials and Con (0.7 0.5
and 1.2 0.8 l/min) did not reach statistical signifi-
cance. Concurrently, arterial mixed-venous O2differ-
ence was 13.9 0.05, 14.0 0.04, and 15.2 0.07
ml/100 ml during C, Con, and H, respectively. However,
these large differences in cardiovascular response at 10
min of exercise were markedly reduced at exhaustion
(Fig. 2). At exhaustion in C, Con, and H, cardiac output
was 20.8 0.7, 20.2 0.6, and 19.9 0.4 l/min; SV was
106 5, 104 4, and 103 4 ml/beat; heart rate was
198 4, 197 4, and 196 4 beats/min; and arterial
mixed-venous O2difference was 15.1 0.3, 15.3 0.6,
and 15.8 0.6 ml/100 ml, respectively (all PNS).
Heart rate at point of fatigue was 98–99% of maximal
heart rate.
Table 1. Individual variability and reproducibility of Tes,T
m, and Tsk at exhaustion
in the study of different initial body temperatures
Subject
Tes TmTsk
Precooling Control Preheating Precooling Control Preheating Precooling Control Preheating
LH 40.3 40.2 39.9 40.4 40.6 40.4 37.3 37.0 36.9
HH 40.0 40.2 40.2 40.2 40.9 41.2 37.3 37.5 37.0
TJ 39.7 40.2 40.3 40.9 41.2 41.2 37.5 37.0 37.1
PM 39.9 40.1 39.9 40.6 40.7 40.5 37.0 37.5 36.9
CJ 40.3 40.3 40.2 41.2 40.7 40.8 37.2 36.6 36.7
JT 40.0 40.4 40.3 40.8 41.0 41.0 36.4 37.4 37.2
HF 40.3 40.2 40.2 40.7 40.8 41.0 37.6 37.3 37.0
MeanSE 40.10.1 40.20.1 40.10.1 40.70.1 40.80.1 40.90.1 37.20.2 37.20.1 37.00.1
Tes, esophageal temperature; Tm, vastus lateralis muscle temperature; Tsk , mean skin temperature.
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Forearm and skin blood flow. During the first 3–8
min of exercise, forearm blood flow was significantly
lower during C than during Con and H: 2.0 0.2 vs.
8.6 1.0 and 11.5 1.4 ml·100 ml1·min1, respec-
tively (P0.05; Fig. 2). At exhaustion, forearm blood
flow was lower during H than during Con and C: 9.6
1.0 vs. 12.1–12.2 1.2 ml·100 ml1·min1, respec-
tively (P0.05).
Baseline resting skin blood flow values (before water
immersion) were 0.2–1.2 V. During exercise, skin blood
flow in Con increased somewhat during the first 10 min
and reached a plateau thereafter (Fig. 1). During H,
skin blood flow was at plateau levels from the initial
minuteofexercise. Incontrast, skin bloodflow duringC
increased gradually after the first 4 min of exercise and
reached a plateau level after 20 min of exercise (Fig. 1).
In all trials, skin blood flow reached a plateau level
after Tes had increased above 38°C (Fig. 2).
Blood lactate and blood glucose. At exhaustion, nei-
ther blood lactate nor blood glucose was different
between trials. Blood lactate ranged from 1.6 0.1 to
2.2 0.2 mM, whereas blood glucose was maintained
at euglycemic levels in all conditions: 6.3 0.1 to 6.7
0.4 mM.
RPE. At 10 min, RPE was significantly lower during
C than during H: 10.6 0.9 vs. 13.7 0.7 units,
respectively (P0.05). RPE increased significantly
over time in all trials. However, RPE at exhaustion was
equally high in all trials: 18.5 0.2 to 18.6 0.3 units
(PNS).
Influence of Different Rates of Heat Storage
Bodytemperatures andperformancetime. Withdiffer-
entrateof heatstorage, allsubjectsreached exhaustion
at similar Tes and Tm(40.3 0.3 vs. 40.1 0.3°C for Tes
and 40.9 0.3 vs. 40.7 0.3°C for Tmduring high vs.
lower rate of heat storage, respectively), but with
significantly (P0.05) different Tsk (38.4 0.4 vs.
35.6 0.2°C for Tsk during high vs. lower rate of heat
storage, respectively; Fig. 3, Table 2). Reflecting the
experimental manipulation, this 3°C difference in Tsk
was attributable only to the effect of the water-perfused
jacket on skin from the trunk and forearms. In both
trials the difference in Tes at exhaustion in each of the
subjects ranged from 0.0 to 0.3°C (Table 2). Time to
exhaustion was significantly shorter during the high
than during the lower rate of heat storage: 31 4 vs.
56 11 min, respectively (P0.05). The large SE
during the lower rate of heat storage trial was due to
differences in relative intensity between subjects. The
two subjects who exercised at 71% V
˙O2max improved
time to exhaustion by 8 and 9 min, whereas the two
subjects who worked at 61% V
˙O2max improved much
more (34 and 48 min). Heart rate response paralleled
the rise in core temperature, being significantly higher
during the high heat storage trial, except at exhaus-
tion, when between-trial differences were not signifi-
cant: 187 7to1897 beats/min or 95–96% of
maximal heart rate (Fig. 3C).
Hydration status. Hydration was similar before exer-
cise, as indicated by similar body weights: 78.3 4.8
and 78.4 4.6 (SD) kg during the high and lower rate
trials, respectively (PNS). Body weight losses during
exercise were higher during the lower rate than during
the high rate of heat storage: 1.7 0.3 vs. 1.1 0.1 kg
(P0.05). Therefore, the levels of dehydration were
higher during the lower rate than during the high rate
of heat storage: 2.1 0.4 vs. 1.5 0.1% body wt loss,
respectively (P0.05).
RPE. At 10 min of exercise, RPE was lower during
thelower rate thanduring thehigh rateof heat storage:
10.8 0.6 vs. 13.0 0.7 units (P0.05). At exhaus-
tion, RPE was equally high in both trials: 19.5 0.5
and 19.8 0.3 units (PNS).
DISCUSSION
Themainaim ofthis study wasto determinewhether
trained subjects fatigued in an uncompensable hot
environment at the same core and muscle tempera-
tures, regardless of the initial value and the rate of rise
of body temperature. We found that exhaustion during
moderate exercise occurred at the same high level of
Fig. 3. Esophageal temperature (A), mean skin temperature (B), and
heart rate (C) during exercise in heat (40°C, 17% relative humidity)
while subjects wore a water-perfused jacket to alter rate of heat
storage. Values are means SE for 4 subjects. *Significantly
different from lower rate of heat storage trial, P0.05.
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internal body temperature and RPE when the initial
value or the rate of increase in body temperature was
altered. We also observed that increases in heart rate
andreductions inSV paralleledtheriseincore tempera-
ture from 36 to 40°C, with skin blood flow plateauing
when core temperature reached 38°C. This suggests
that increases in heart rate might contribute to reduc-
tions in SV with heat stress.
High Temperature and Fatigue
The main finding of these studies was that fatigue
during exercise in the heat was related to high internal
body temperature. This is based on the observation
that, in both studies, trained subjects fatigued at
similar Tes and Tm(40.1–40.3 and 40.7–40.9°C, respec-
tively), even though Tsk was 2–3°C lower during the
lower rate of heat storage trial. The between-trial
variability in core temperature and Tmat exhaustion
was very small in both studies: 0.3 0.1°C (Tables 1
and 2). Time to exhaustion ranged from 28 to 63 min,
being shortest with highest initial body temperature
and higher rate of heat storage. Fatigue in the present
heat stress condition is clearly related to high body
temperature, because these trained cyclists could cycle
to exhaustion at the same intensity in the heat for 2h
when core temperature rose at a slower rate to 39.7
0.2°C (13).
The present findings confirm previous observations
from this laboratory indicating that trained subjects
fatigued with core temperatures of 40°C when work-
ing at 50–60% V
˙O2peak in the heat (40°C, 10% RH) for
9–12 consecutive days (28, 30). Exercise time to fatigue
increasedfrom48 2to803 min fromthe first tothe
lastacclimation day,owing inpartto alower initialcore
temperature with heat acclimation (28). This large
improvement in exercise time to fatigue was drastically
reduced to 5–10 min when the subjects exercised in a
humid environment but still coincided with a core
temperature of 39.9 0.1°C (30). Interestingly, fatigue
in all these previous studies was not associated with
any reductions in cardiac output, exercising leg blood
flow, leg substrate availability and utilization, or accu-
mulation of lactate, K, or other proposed ‘‘fatigue’’
substances (28–30). Furthermore, muscle glycogen lev-
els at the point of fatigue have been shown to be quite
high in these conditions (300 mmol/kg dry wt) (10, 13,
29). Presently, we also observed low concentrations of
blood lactate and euglycemic levels of blood glucose as
wellassimilar heartrateand cardiacoutput at exhaus-
tion. Taken together, it appears that hyperthermia,
rather than altered circulation and metabolism, is the
mainfactorcausing fatigueinthe presentconditions. It
is recognized, however, that these and other factors
such as dehydration, training status, heat acclimation,
and environmental conditions, as well as duration and
intensity of exercise, might interact and alter the
tolerance to hyperthermia (8, 13, 23, 26, 29, 38).
Evidence in humans and animals also supports the
notion that fatigue in hot environments appears to
coincide with a critically high internal body tempera-
ture (6, 11, 12, 14, 17, 24). There are reports indicating
that some untrained subjects fatigued during exercise
inuncompensable hotenvironments withbody tempera-
tures of 38°C (23, 26, 38). In untrained and moder-
ately fit subjects, core temperature at exhaustion from
heat strain during low-intensity exercise has been
shown to occur over a range of 38–40°C (23, 26, 38).
Differences in subjects’training status appear to be the
mainreasonfor thediscrepancyin thetolerance to heat
strain between the present and previous studies (23,
26, 38). In this light, it has been elegantly shown that
subjects with higher aerobic fitness perform longer and
tolerate higher levels of hyperthermia (39.2 vs. 38.8°C)
in uncompensable hot environments than their less fit
counterparts (7). Our present results extend previous
findings by examining high metabolic rates in highly
conditioned athletes. Furthermore, we presently deter-
mined the influence of active muscle temperature on
fatigue in hot environments.
The mechanism by which hyperthermia causes fa-
tigue is not well understood. We have presently ob-
served a similar muscle and core temperature at the
point of fatigue, despite a different upper body skin
temperature in the rate study. Under these conditions,
it is expected that hypothalamic and other internal
organ temperatures would also reach a similarly high
level at the point of fatigue (11). In this context, we
could speculate that fatigue mainly responded to sig-
nals originating in the active muscle, internal organs,
and/or central nervous system, secondary to the rise in
temperature. The detrimental effects of hyperthermia
on muscle function and metabolism are well docu-
mented (4, 9, 10). Furthermore, hyperthermia is known
to stimulate the release of endotoxins and heat shock
proteins from the internal organs, which might contrib-
ute to fatigue (see Ref. 17 for review). Alternatively,
hyperthermia might reduce the central drive for exer-
cise by influencing the motor control center in the brain
Table 2. Individual variability and reproducibility of Tes,T
m, and Tsk at exhaustion in the study
of different rate of increase in body temperature
Subject
Tes TmTsk
High rate Lower rate High rate Lower rate High rate Lower rate
JR 39.6 39.4 40.6 40.1 37.7 35.6
CJ 41.1 40.8 41.6 41.4 39.6 35.8
HF 40.3 40.1 40.7 40.8 38.3 35.9
PM 40.1 40.1 40.5 40.7 38.1 35.2
MeanSE 40.30.3 40.10.3 40.90.3 40.70.3 38.40.4 35.60.2
1037HYPERTHERMIA AND FATIGUE
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(5, 28). Whether these factors interact or act indepen-
dently awaits further investigations. Irrespective of its
origin, however, it is clear that this mechanism acts to
protect humans and animals from reaching tissue
temperatures that jeopardize cell function.
Cardiovascular Responses to Exercise
Anotherinterestingobservation ofthestudy ofdiffer-
ent initial temperatures was that cardiac output was
2.2 0.9 l/min lower during preheating than during
the precooling trial at 10 min of exercise, yet whole
body V
˙O2was unaltered. Previous studies comparing
exercise in hot (36–44°C) vs. neutral environments and
exercise with hot vs. cold water perfusing a suit in
contact with the skin have shown cardiac output to be
increased (27, 29, 35), unchanged (27, 35), or reduced
(35). The present finding that the combined elevations
in Tsk,T
es (2.4–3.1°C), and skin blood flow (8 ml·100
ml1·min1or 4-fold elevation) reduced cardiac output
during moderately intense exercise confirms previous
results of Rowell et al. (35) in untrained subjects. They
observed a significantly lower cardiac output (1.0–1.2
l/min), central blood volume (0.1–0.2 liter), and SV
(20 ml) when subjects exercised in a 43°C than in a
26°C environment at 63–73% V
˙O2peak (34).
In the present study and the study of Rowell et al.
(35), the decrease in cardiac output with hyperthemia
is attributed to the larger decline in SV (Fig. 2). The
mechanism mediating this reduced SV with hyperther-
mia has not been directly elucidated. The prevailing
hypothesis is that reductions in SV with heat stress are
due to increased skin blood flow and volume (20, 34).
Rowell (34) speculated that increased skin blood flow
reduces SV by reducing ventricular filling as a result of
displacement of blood from the central circulation to
peripheral skin veins as core temperature increases.
Evidence showing that the lower SV, central venous
pressure, and central blood volume with whole body
heating are reversed by whole body cooling (36) ap-
pears to support this notion. However, this manipula-
tionaltersnot onlyskin blood flowand Tsk, butalso core
temperature, which have been shown to alter heart
rate and SV independently (16). An increase in Tes of
1°C has been shown to increase heart rate by 9 1
beats/min and reduce SV by 11 3 ml when skin blood
flow was the same (16). It seems, therefore, that the
mechanism mediating SV reductions with heat stress
is complex and might be influenced by several factors.
In the present study with markedly different heat
strain conditions at 10 min of exercise (Fig. 1), it seems
likely that central blood volume and right atrial pres-
sure were also significantly reduced in H compared
with C. An interesting observation was that skin blood
flow reached a plateau at Tes of 38°C in all trials, in
agreement with early and recent reports (3, 13, 15, 25,
30). This indicates that the observed further reductions
in SV with core temperature above 38°C (i.e., 20 ml)
were clearly not associated with increased skin blood
flow (Fig. 2, C–E). This agrees with the observations
that most of the reductions in central blood volume and
right atrial pressure with heat stress occur early in
exercise (31, 35) and that right atrial pressure declines
onlyslightlyafter skinbloodflow hasreacheda plateau
level (31). As shown in Fig. 2A, increases in heart rate
from 130 beats/min to almost maximal levels (196–198
beats/min) were strongly correlated with increases in
core temperature (r20.98, P0.001). Heart rate at a
given temperature was remarkably similar among tri-
als. Because heart rate is influenced by multiple fac-
tors, it is not clear from our experiment to what extent
this increase in heart rate responds to decreased SV
and reduced stretching of the heart (Frank-Starling
mechanism) and/or direct effect of warm blood on the
sinus node and neurohumoral stimuli (37). It seems
reasonable, however, to speculate that the increase in
heart rate at Tes 38°C was largely related to increases
inbodytemperature. Thistheory suggests thatreduced
cardiac filling time (i.e., higher heart rate) might also
contribute to reductions in SV with hyperthermia,
particularly in conditions of reduced central venous
pressure and central blood volume. Another possibility
isthathigh cardiactemperature reducesSVby altering
cardiac contractility.
In conclusion, these results demonstrate that high
body temperature per se causes fatigue in trained
subjects during prolonged exercise in uncompensable
hot environments. Furthermore, time to exhaustion in
hot environments in trained subjects is inversely re-
lated to the initial level of body temperature and
directly related to the rate of heat storage. In addition,
marked elevations in body temperature (2–3°C) and
skin blood flow (4-fold) resulted in significant reduc-
tions in cardiac output due to the larger decline in SV,
yet whole body V
˙O2was unaltered. The observation
that increases in heart rate and reductions in SV
paralleled the rise in core temperature from 36 to 40°C,
while skin blood flow plateaus at Tes of 38°C, supports
thecontentionthat increasesin heartratecontribute to
reductions in SV with heat stress.
The authors thank the subjects for their enthusiasm.
These studies were supported by grants from Team Danmark and
the European Commission. J. Gonza´lez-Alonso was supported by
Marie Curie Research Training Grant FMBICT950007.
Addressfor reprintrequests: J. Gonza´lez-Alonso,The Copenhagen
Muscle Research Center, Rigshospitalet, Section 7652, 20 Tagenvej,
DK-2200 Copenhagen N, Denmark.
Received 17 September 1998; accepted in final form 28 October 1998.
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1039HYPERTHERMIA AND FATIGUE
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... The associated thermoregulatory, (Sawka et al., 1992;Galloway and Maughan, 1997;González-Alonso et al., 1999;Otani et al., 2017), cardiovascular, (González-Alonso et al., 1999;Nassis and Geladas, 2002), metabolic, (Jentjens et al., 2002), and neuromuscular (Nybo and Nielsen, 2001;Morrison et al., 2004;Baillot et al., 2021) changes that occur during exercise in the heat are known to result in declines in aerobic, (Galloway and Maughan, 1997), repeated sprint, (Drust et al., 2005), repeated force production, (Thomas et al., 2006), and cognitive (Racinais et al., 2008) performance. These physiologic (Sawka et al., 1985;Sawka et al., 1992;Mn, 1992;González-Alonso et al., 1995;González-Alonso et al., 1997;Logan-Sprenger et al., 2012;Chou et al., 2018) and performance (Stearns et al., 2009;Casa et al., 2010;Lopez et al., 2011;Distefano et al., 2013;Otani et al., 2016;Adams et al., 2017) outcomes in response to exercise heat stress are further exacerbated by dehydration, which often accompanies exercise. ...
... The associated thermoregulatory, (Sawka et al., 1992;Galloway and Maughan, 1997;González-Alonso et al., 1999;Otani et al., 2017), cardiovascular, (González-Alonso et al., 1999;Nassis and Geladas, 2002), metabolic, (Jentjens et al., 2002), and neuromuscular (Nybo and Nielsen, 2001;Morrison et al., 2004;Baillot et al., 2021) changes that occur during exercise in the heat are known to result in declines in aerobic, (Galloway and Maughan, 1997), repeated sprint, (Drust et al., 2005), repeated force production, (Thomas et al., 2006), and cognitive (Racinais et al., 2008) performance. These physiologic (Sawka et al., 1985;Sawka et al., 1992;Mn, 1992;González-Alonso et al., 1995;González-Alonso et al., 1997;Logan-Sprenger et al., 2012;Chou et al., 2018) and performance (Stearns et al., 2009;Casa et al., 2010;Lopez et al., 2011;Distefano et al., 2013;Otani et al., 2016;Adams et al., 2017) outcomes in response to exercise heat stress are further exacerbated by dehydration, which often accompanies exercise. ...
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This article emphasizes significant recent advances regarding heat stress and its impact on exercise performance, adaptations, fluid electrolyte imbalances, and pathophysiology. During exercise‐heat stress, the physiological burden of supporting high skin blood flow and high sweating rates can impose considerable cardiovascular strain and initiate a cascade of pathophysiological events leading to heat stroke. We examine the association between heat stress, particularly high skin temperature, on diminishing cardiovascular/aerobic reserves as well as increasing relative intensity and perceptual cues that degrade aerobic exercise performance. We discuss novel systemic (heat acclimation) and cellular (acquired thermal tolerance) adaptations that improve performance in hot and temperate environments and protect organs from heat stroke as well as other dissimilar stresses. We delineate how heat stroke evolves from gut underperfusion/ischemia causing endotoxin release or the release of mitochondrial DNA fragments in response to cell necrosis, to mediate a systemic inflammatory syndrome inducing coagulopathies, immune dysfunction, cytokine modulation, and multiorgan damage and failure. We discuss how an inflammatory response that induces simultaneous fever and/or prior exposure to a pathogen (e.g., viral infection) that deactivates molecular protective mechanisms interacts synergistically with the hyperthermia of exercise to perhaps explain heat stroke cases reported in low‐risk populations performing routine activities. Importantly, we question the “traditional” notion that high core temperature is the critical mediator of exercise performance degradation and heat stroke. Published 2011 This article is a U.S. Government work and is in the public domain in the USA. Compr Physiol 1:1883‐1928, 2011.
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Introduction Formula One and other motor car racing drivers race for prolonged periods in hot conditions wearing protective apparel that impairs heat loss. They are thus at risk of a significantly elevated core temperature. The aims of this study were to determine whether the voluntary ingestion of cold fluid aided thermoregulation more effectively than the voluntary ingestion of ambient temperature fluid in a simulated motor racing environment. Methods Eight male participants commenced two 120-min simulated motor racing trials in an environmental chamber (40°C, 50% humidity). During one trial they were provided with 1 L of ambient temperature water (AWT), whilst in the other trial the water temperature was ∼5°C (CWT). A drinking schedule of “1 sip every four minutes” was advocated. Participant core temperature, skin temperature and heart rate were recorded continuously, whilst thermal comfort, response time and cognitive function were assessed at 30-min intervals. Results All participants successfully completed their CWT, but only two completed the full 120-mins of their AWT (AWT trial duration ranged from 80 to 120 min). Despite encouragement to drink more, both the rate of consumption (AWT 333 ± 103 v CWT 436 ± 99 ml/h) and total volume of water consumed (AWT 585 ± 233 v CWT 872 ± 198 ml) were less in the AWT (p < 0.005). At the 75-min point of the trials, participant core temperatures had increased by 1.26 ± 0.29 in AWT and 0.81 ± 0.30 in CWT. Furthermore, at the point of trial cessation, core temperature in the AWT had increased by 1.69 ± 0.36°C, but only 1.17 ± 0.52°C in the CWT (p < 0.05). Participants reported less discomfort and a lower rating of perceived exertion during the CWT. In both trials, response time to the cognitive test decreased as the trials progressed, with no evident difference in response time nor cognitive function between the two trials. Discussion The ingestion of cold water was associated with an ability to continue with volitional performance and associated with an ameliorated increase in core temperature as well as providing psychological benefits of cold “refreshment”.
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Background Taurine (TAU) and creatine (Cr) are common ergogenic aids used by athletes to enhance performance; however, the effect of their combined supplementation, and on recovery in high temperature and humidity environments, has not been studied. Hypothesis Combined TUA and Cr will have greater effect on physiological indicators and repetitive sprint performance recovery after exhaustive exercise under hot and humid conditions than single supplementation or placebo. Study Design Single-blind crossover randomized controlled study. Level of Evidence Level 2. Methods Participants (12 sports students) were assigned randomly to 1 of 4 supplementation intervention groups: placebo (P), taurine (T), creatine (C), or taurine + creatine (T+C). Exercise protocol included exhaustion tests and repeated sprinting exercises were conducted in a laboratory environment at 35 °C/65% relative humidity. Heartrate, blood lactate (BLa), tympanic temperature, thermal sensation, and rating of perceived exertion were monitored throughout. Heartrate variability, time to exhaustion (TTE), reaction time, and countermovement jump (CMJ) height were tracked before and after exhaustion exercise and before sprint exercise. Results TTE was significantly higher in the T+C group than in the P group ( P = 0.04). BLa and tympanic temperature increased rapidly in all 4 conditions, then decreased gradually, and T group peak values were higher than those of P group ( P = 0.04; P < 0.01). CMJ decreased in the C and T+C groups ( P = 0.04; P = 0.04) after exhaustive exercise, unlike other groups ( P > 0.05). Indicators of repeated sprint exercise, peak power, mean power, and power decrement showed a decreasing trend within groups but no difference between groups ( P > 0.05). Conclusion In this small student group, under hot and humid conditions, T+C supplementation significantly enhanced TTE. Clinical Relevance TAU, Cr, and their combined supplementation do not significantly improve repeated sprint performance after exhaustive exercise under hot and humid conditions.
Article
The health issues of hazardous operations in high-temperature environments are increasing concerns to the public, especially since global warming and extreme weather conditions have made the high-temperature work more frequent and harsher. The abnormal elevation of human core temperature (Tcr) due to high temperatures directly leads to a decline in physiological functions and may trigger various heat-related health issues, which is especially threatening for those working in such conditions. However, continuous real-time Tcr monitoring and prediction are challenging, particularly considering the hazardous operations in extremely hot environments. To address this problem, a non-invasive Tcr prediction model combining a Kalman filter and a long-term sequence forecasting deep learning model was developed. This model leverages monitored skin temperature (Tsk) and heart rate (HR) as input features, enabling personalized real-time Tcr predictions for various groups of specialized operations personnel. The model's accuracy was validated using the data from a series of chamber experiments with 13 participants under ambient temperatures ranging from 34 to 40 °C and Tcr range of 37–39 °C. The optimal prediction results, evaluated by the test set using seven-point Tsk combined with HR, obtain a MAE value of 0.07, a RMSE value of 0.09, and a R2 value of 0.93. Additionally, the errors of 95% of all Tcr predictions fell within ±0.17 °C. The proposed model has the advantage of requiring simple input parameters/features and producing high-accuracy predictions, which makes it a practical tool for health monitoring and protection of hazardous operations in high-temperature environments.
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Persistent photoconductivity (PPC) has been observed in boron-doped Si1−xGex/Si quantum wells. The decay kinetics of the PPC effect can be well described by a stretched-exponential function, Ippc(t) = Ippc(0)exp[−(t/τ)β](0<β<1), which is usually observed in many disorder materials. Through the studies of the PPC effect under various conditions, such as different temperature, different photon energy of photoexcitation, and different Ge content, we identify that the alloy potential fluctuations induced by compositional disorder are the origin of the PPC effect in Si1−xGex/Si quantum wells. © 1998 American Institute of Physics.
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The present study examined whether the blood flow to exercising muscles becomes reduced when cardiac output and systemic vascular conductance decline with dehydration during prolonged exercise in the heat. A secondary aim was to determine whether the upward drift in oxygen consumption (V̇ O2 ) during prolonged exercise is confined to the active muscles. Seven euhydrated, endurance‐trained cyclists performed two bicycle exercise trials in the heat (35 °C; 40–50% relative humidity; 61 ± 2% of maximal V̇ O2 ), separated by 1 week. During the first trial (dehydration trial, DE), they bicycled until volitional exhaustion (135 ± 4 min, mean ± s.e.m.), while developing progressive dehydration and hyperthermia (3.9 ± 0.3% body weight loss; 39.7 ± 0.2 °C oesophageal temperature, T oes ). In the second trial (control trial), they bicycled for the same period of time while maintaining euhydration by ingesting fluids and stabilizing T oes at 38.2 ± 0.1 °C after 30 min exercise. In both trials, cardiac output, leg blood flow (LBF), vascular conductance and V̇ O2 were similar after 20 min exercise. During the 20 min‐exhaustion period of DE, cardiac output, LBF and systemic vascular conductance declined significantly (8–14%; P < 0.05 ) yet muscle vascular conductance was unaltered. In contrast, during the same period of control, all these cardiovascular variables tended to increase. After 135 ± 4 min of DE, the 2.0 ± 0.6 l min ⁻¹ lower blood flow to the exercising legs accounted for approximately two‐thirds of the reduction in cardiac output. Blood flow to the skin also declined markedly as forearm blood flow was 39 ± 8% ( P < 0.05 ) lower in DE vs. control after 135 ± 4 min. In both trials, whole body V̇ O2 and leg V̇ O2 increased in parallel and were similar throughout exercise. The reduced leg blood flow in DE was accompanied by an even greater increase in femoral arterial‐venous O 2 (a‐vO 2 ) difference. It is concluded that blood flow to the exercising muscles declines significantly with dehydration, due to a lowering in perfusion pressure and systemic blood flow rather than increased vasoconstriction. Furthermore, the progressive increase in oxygen consumption during exercise is confined to the exercising skeletal muscles.
Article
 Acute and repeated exposure for 8–13 consecutive days to exercise in humid heat was studied. Twelve fit subjects exercised at 150 W [45% of maximum O2 uptake (V.O2,max)] in ambient conditions of 35°C and 87% relative humidity which resulted in exhaustion after 45 min. Average core temperature reached 39.9 ± 0.1°C, mean skin temperature (T– sk) was 37.9 ± 0.1°C and heart rate (HR) 152 ± 6 beats min–1 at this stage. No effect of the increasing core temperature was seen on cardiac output and leg blood flow (LBF) during acute heat stress. LBF was 5.2 ± 0.3 l min–1 at 10 min and 5.3 ± 0.4 l min–1 at exhaustion (n = 6). After acclimation the subjects reached exhaustion after 52 min with a core temperature of 39.9 ± 0.1°C, T– sk 37.7 ± 0.2°C, HR 146 ± 4 beats min–1. Acclimation induced physiological adaptations, as shown by an increased resting plasma volume (3918 ± 168 to 4256 ± 270 ml), the lower exercise heart rate at exhaustion, a 26% increase in sweating rate, lower sweat sodium concentration and a 6% reduction in exercise V.O2. Neither in acute exposure nor after acclimation did the rise of core temperature to near 40°C affect metabolism and substrate utilization. The physiological adaptations were similar to those induced by dry heat acclimation. However, in humid heat the effect of acclimation on performance was small due to physical limitations for evaporative heat loss.
Article
The purpose of the present study was to determine the separate and combined effects of aerobic fitness, short-term heat acclimation, and hypohydration on tolerance during light exercise while wearing nuclear, biological, and chemical protective clothing in the heat (40 degrees C, 30% relative humidity). Men who were moderately fit [(MF); <50 ml . kg-1 . min-1 maximal O2 consumption; n = 7] and highly fit [(HF); >55 ml . kg-1 . min-1 maximal O2 consumption; n = 8] were tested while they were euhydrated or hypohydrated by approximately 2.5% of body mass through exercise and fluid restriction the day preceding the trials. Tests were conducted before and after 2 wk of daily heat acclimation (1-h treadmill exercise at 40 degrees C, 30% relative humidity, while wearing the nuclear, biological, and chemical protective clothing). Heat acclimation increased sweat rate and decreased skin temperature and rectal temperature (Tre) in HF subjects but had no effect on tolerance time (TT). MF subjects increased sweat rate but did not alter heart rate, Tre, or TT. In both MF and HF groups, hypohydration significantly increased Tre and heart rate and decreased the respiratory exchange ratio and the TT regardless of acclimation state. Overall, the rate of rise of skin temperature was less, while DeltaTre, the rate of rise of Tre, and the TT were greater in HF than in MF subjects. It was concluded that exercise-heat tolerance in this uncompensable heat-stress environment is not influenced by short-term heat acclimation but is significantly improved by long-term aerobic fitness.
Article
Three relatively fit subjects performed duplicate 20- to 25-min cycle ergometer exercise bouts at moderate and heavy intensities (40% and 70% Vo2 max) in ambient temperatures of 20, 26, and 36 degrees C. They approached a steady state in internal body temperature (Tes) in all but the heavy exercise in the heat, where Tes rose consistently, averaging 38.84 degrees C at the termination of exercise. Cardiac output (Q), estimated by a rebreathing technique, was proportional to Vo2 and independent of the body temperatures, except during the lower exercise intensity in the heart, where Q averaged 1.31 . min -1 higher throughout. In any environment, forearm blood flow was linearly related to Tes above the Tes threshold for vasodilation, but during heavy exercise in the heat this relationship was severely attenuated above a Tes around 38.0 degrees C, when forearm blood flow exceeded 15 ml.min -1 .100 ml -1. Plasma volume decreases during exercise were primarily a function of the intensity of exercise. During heavy exercise in the heat the relative vasconstriction contributes to the maintenance of an adequate stroke volume preventing a fall in Q. In this case, circulatory regulation has precedence over temperature regulation.
Article
The relation between end-tidal carbon dioxide tension (PETCO2) measured by infrared analysis and arterial carbon dioxide tension (PaCO2) during exercise was systematically examined in five healthy adults at two power outputs (25 and 50% VO2max) and at three frequencies of breathing (15, 30, and 45 breaths/min). PETCO2-PaCO2 varied between -2.5 and +9.1 Torr, was inversely related to the frequency of breathing (r = 0.475), and directly related to tidal volume (VT; r = 0.791) and CO2 output (r = 0.627). An equation was obtained by multiple regression analysis, to predict PaCO2 from PETCO2: PaCO2 = 5.5 +0.90 PETCO2 -0.0021 VT (r = 0.915). The equation was applied to measurements of PETCO2 obtained in two previous studies in 10 subjects in which PaCO2 had been measured, and was found to predict PaCO2 to within 1.04 Torr (+/- SD) for PaCO2 between 25 and 58 Torr (n = 56; r = 0.962). The effect of the response characteristics of the CO2 analyzer on the measurement of PETCO2 was also systematically examined by comparison with a fast-responding respiratory mass spectrometer.
Article
We have investigated further the behavior of skin blood flow (SkBF) as internal temperature (measured as esophageal temperature (Tes)) rises in a heated exercising man. A previous study showed that when skin temperature (Tsk) is driven up in exercising men, the increase in SkBF is less than that found for the same Tes and Tsk in a resting man. In this study, we extended our observations into the range of higher Tes to see if SkBF (measured plethysmographically as changes in forearm blood flow) could be driven to higher levels despite competition with skeletal muscle for cardiac output. After Tsk was elevated to 38 degrees C by means of water-perfused suits, subjects exercised at 525-900 kp.m/min (86-147 W) for 17-30 min while Tsk was held at 38 degrees C. We found that SkBF increase per unit increase in Tes is attenuated at higher Tes. In seven men, the average slope obtained from linear regression of FBF on Tes below 38 degrees C was 7.6 flow units/degrees C. Above 38 degrees C, the average was 2.12 flow units/degrees C. In some subjects, the FBF response appeared virtually saturated at a plateau despite a steady rate of increase in Tes with time. Clearly, SkBF does not increase in direct proportion to Tes without bound. Other stimuli (presumably related to blood pressure regulation) interact either to reduce the rate of SkBF increase or to prevent any further increase after Tes exceeds 38 degrees C.
Article
To determine the cutaneous and resting skeletal muscle vascular responses to prolonged exercise, total forearm blood flow (FBF-plethysmography) (5 men) and forearm muscle blood flow (MBF-[125I]antipyrine clearance) (4 men) were measured throughout 55-60 min of bicycle exercise (600-750 kpm/min). Heart rate (HR) and esophageal temperature (Tes) were also measured throughout exercise. FBF showed only small changes during the first 10 min followed by progressive increments during the 10-40 min interval and smaller rises thereafter. For the full 60 min of exercise, there was an average increase in FBF of 8.26 ml/100 ml-min. MBF showed an initial fall with the onset of exercise (on the average from 3.84 to 2.13 ml/100 ml-min) which was sustained or fell further as exercise continued, indicating that increments in FBF were confined to skin. Much of the increase in FBF occurred despite essentially constant Tes. Results suggest that the progressive decrements in central venous pressure, stroke volume, and arterial pressure previously seen during prolonged exercise are due in part to progressive increments in cutaneous blood flow and volume.