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Department of Sports Medicine, Research Center on Aging and Adaptation, Shinshu University School of Medicine, Matsumoto 390-8621, Japan
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ABSTRACT |
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Plasma volume (PV)
expansion by endurance training and/or heat acclimatization is known to
increase aerobic and thermoregulatory capacities in humans.
Also, higher erythrocyte volume (EV) fractions in blood are known to
improve these capacities. We tested the hypothesis that training in a
hypobaric hypoxic and warm environment would increase peak aerobic
power (
O2 peak) and forearm skin
vascular conductance (FVC) response to increased esophageal temperature
(Tes) more than training in either environment alone, by
increasing both PV and EV. Twenty men were divided into four training
regimens (n = 5 each): low-altitude cool (610-m
altitude, 20°C ambient temperature, 50% relative humidity),
high-altitude cool (2,000 m, 20°C), low-altitude warm (610 m,
30°C), and high-altitude warm (HW; 2,000 m, 30°C). They
exercised on a cycle ergometer at 60%
O2 peak for 1 h/day for 10 days in a
climate chamber. After training, PV increased in all trials, but EV
increased in only high-altitude trials (both P < 0.05).
O2 peak increased in all trials
(P < 0.05) but without any significant differences among trials. FVC response to increased Tes was measured
during exercise at 60% of the pretraining
O2 peak at 610 m and 30°C. After
the training, Tes threshold for increasing FVC decreased in
warm trials (P < 0.05) but not in cool trials and was
significantly lower in HW than in cool trials (P < 0.05). The slope of FVC increase/Tes increase increased in
all trials (P < 0.05) except for high-altitude cool
(P > 0.4) and was significantly higher in HW than in
cool trials (P < 0.05). Thus, against our hypothesis,
the
O2 peak for HW did not increase
more than in other trials. Moreover, slope of FVC
increase/Tes increase in HW increased most, despite the similar increase in blood volume, suggesting that factors other than
blood volume were involved in the highest FVC response in HW.
endurance training; altitude; skin blood flow; aerobic power; blood volume; humans
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INTRODUCTION |
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HYPERVOLEMIA INDUCED BY ENDURANCE exercise training and/or heat acclimatization has been suggested to increase aerobic and thermoregulatory capacities (15). This theory appears to be supported mainly by studies investigating the effects of acute plasma volume (PV) expansion on the functions (23). There are several studies showing that acute PV expansion increased maximal aerobic capacity by increasing cardiac stroke volume (5, 11, 23). In addition, skin blood flow (SkBF) during submaximal exercise in a hot environment was reportedly increased by intravenous infusion of saline (19) or albumin solution (7). Because similar increases in SkBF were observed after water immersion (18), posture change from the upright to supine position (1), and negative-pressure breathing (17), the increased SkBF by PV expansion might be caused by stretch of baroreceptors due to increased venous return to the heart.
In contrast to these findings, there have been few studies showing the merits of PV expansion by endurance training or heat acclimatization in thermoregulation, although there are some in maximal aerobic capacity (3, 14). Convertino et al. (3) studied the relative role of exercise training and heat exposure in PV expansion and suggested that not only exercise training but also heat exposure increased PV in an additive way. Costill et al. (4) measured the body fluid and electrolyte balance during recovery from thermal dehydration and suggested that PV expansion was induced by increased extracellular fluid volume, attained by enhanced renal water and Na retention mechanisms during this period. Although both studies suggested the involvement of heat exposure in PV expansion, neither examined the effects on thermoregulation. Although Roberts et al. (21) reported that the sensitivity in cutaneous vasodilation in response to increased esophageal temperature (Tes) was more enhanced after endurance training in a hot environment than in a cool environment, they did not measure PV. Thus heat acclimatization is known to be a major factor in expanding PV, although it is not clear whether the expansion really contributes to the enhanced sensitivity of cutaneous vasodilation, as deduced by the findings from acute PV expansion (7, 19). The first purpose of this study was to clarify this issue.
The second aim of the present study was to assess the effects of altitude training on temperature regulation. Sawka et al. (24) examined the effects of increased fractions of erythrocyte volume (EV) in blood on thermoregulation during exercise in a hot environment. They reported that the increased fraction of EV improved thermoregulation during exercise by reducing Tes thresholds for sweating and increasing sweating sensitivity in response to increased Tes. As for the mechanism, they postulated that the increased arterial oxygen content, induced by EV expansion, might allow systemic oxygen transport requirements for a given level of submaximal exercise to be achieved with lower muscle blood flow, which might enable redistribution of blood flow to the skin. From these findings, we hypothesized that endurance training at a high altitude would expand EV (22) and increase O2 conductance in muscles (27), thus reducing blood flow to muscle and enabling redistribution of blood flow to the skin. Furthermore, because PV was reported to increase after heat acclimatization (3, 14), endurance training in a hypobaric hypoxic and warm environment would cause total blood volume (BV) expansion by increasing both EV and PV more than in either environment alone, leading to higher maximal aerobic power and SkBF through not only increased cardiac stroke volume (14, 29) but also baroreflex-induced vasodilation in the skin (17) and muscles (12).
To accomplish these aims, the maximal aerobic capacity and sensitivity of cutaneous vasodilation were measured before and after endurance training in four different environments: low-altitude cool (LC; 610 m, 20°C), low-altitude warm (LW; 610 m, 30°C), high-altitude cool (HC; 2,000 m, 20°C), and high-altitude warm (HW; 2,000 m, 30°C). The findings were analyzed in relation to EV and PV.
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METHODS |
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This study was approved by the Review Board on Human
Experiments, Shinshu University School of Medicine. Subjects gave their written, informed consent before participating in the study. The blood
properties and physical characteristics of young male subjects [age
23 ± 4 (SD) yr] before each training program are shown in Table
1. The experiments were conducted between
May and June and between September and February 1999, to ensure that
the subjects were not heat acclimated before training.
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Training Programs
Twenty male subjects were divided into four trials according to the environmental conditions for training: 1) LC [atmospheric pressure (Patm), 710 mmHg (610 m); ambient temperature (Ta), 20°C; relative humidity (RH), 50%; n = 5]; 2) HC [Patm, 595 mmHg (2,000 m); Ta, 20°C; RH, 50%; n = 5]; 3) LW (Patm, 710 mmHg; Ta, 30°C; RH, 50%; n = 5); and 4) HW (Patm, 595 mmHg; Ta, 30°C; RH, 50%; n = 5). The environmental conditions were adjusted within the range of ±1 mmHg for Patm, ±0.1°C for Ta, and ±1% for RH in an artificial climate chamber. The low altitude of 610 m was adopted because our laboratory is located at that altitude. The exercise training was performed without fan cooling.Subjects performed cycle ergometer training at 60% of peak aerobic
power (
O2 peak) for 1 h each day.
Training was composed of two 30-min bouts of exercise separated by
10-min rest for 10 days and lasted for 5 days/wk for 2 wk, in an
artificial climate chamber. Because
O2 peak increased with training, the
exercise intensity was readjusted 5 min after the start of exercise
each day so that subjects exercised at a heart rate (HR) of ~140
beats/min, which was assumed to be equivalent to 60% of
O2 peak each day. The reason for
adopting the HR at 5 min as the target HR to be readjusted was that the
HR depended on the relative exercise intensity before body temperature
started to increase. After 5 min of exercise, HR gradually increased in parallel with the increase in Tes, despite the constant
exercise intensity. Total sweat loss (SL) was estimated from body
weight loss after exercise and is expressed in milliliters per kilogram body weight.
Protocols and Measurements
PV,
O2 peak, and forearm skin
vascular conductance (FVC) response to increased Tes were
measured before and after the training, according to that order, on
separate days. The pretraining measurements were accomplished at least
2 days before the start of training, and the posttraining measurements
at least 5 days after the cessation of training in the order of PV, FVC
response, and
O2 peak. The measurements
of PV and FVC response were completed within at least 2 days after the
training to avoid de-acclimatization to heat.
PV.
On the day of PV measurement, subjects reported to the laboratory at
7:00 AM normally hydrated but without having taken any food for 10 h before the measurement. PV was determined by using the Evans blue dye
dilution method (9) for each subject in the sitting
position after 30 min of rest at 28°C Ta and 50% RH. The
BV was calculated from the PV, and hematocrit (Hct) was corrected for
trapped plasma (0.96) and the F-cell ratio (0.91) (10). EV
was calculated as EV = BV
PV. The aliquots of blood were also used to determine blood chemicals, as described in detail in
Blood Properties.
O2 peak.
O2 peak was determined with graded
exercise by using a cycle ergometer in the upright position (Table 1).
Clad in shorts and shoes, subjects entered an environmental chamber
adjusted to 710-mmHg Patm, 25°C Ta, and 50% RH. After
the electrocardiogram electrodes were applied, subjects pedaled at 60 cycles/min at an initial intensity of 60 W. The intensity was increased
by 60 W every 3 min <180 W, above that intensity by 30 W every 2 min <240 W, and then by 15 W every 2 min until subjects did not keep the
rhythm due to exhaustion. The oxygen consumption rate was calculated
from measurements of ventilation volume and expired fractions of
O2 and CO2 (Aeromonitor AE260, Minato, Tokyo,
Japan) every 15 s. In the high-altitude (H) trials,
O2 peak at 595 mmHg and Ta
at 25°C were also measured to determine the exercise intensity for
training at 2,000 m.
O2 peak in the
semirecumbent position was also measured with graded exercise to
determine exercise intensity for the FVC response test.
FVC response test.
Subjects reported to the laboratory at 8:00 AM normally hydrated but
without breakfast. Clad in shorts and shoes, subjects emptied their
bladders; entered the chamber controlled at 710-mmHg Patm, 30°C
Ta, and 50% RH; then sat in the contour chair of the cycle
ergometer in a semirecumbent position and rested for 60 min while all
measurement devices were applied. After the baseline measurements were
taken at rest for 10 min, subjects exercised in the semirecumbent
position at 60% of pretraining
O2 peak for 30-40 min without fan cooling. Forearm SkBF (FBF), HR,
systolic (SAP) and diastolic (DAP) arterial pressures, Tes,
and skin temperature (Tskin) were measured at rest and
during exercise, as described in detail below.

Analyses for the Tes vs. FVC Relationship
As shown in Fig. 1, the Tes vs. FVC relationship was fitted with three regression equations in mean values by using a standard Y minimized regression analysis. The first one was determined by eye from the first sharp increase in Tes before the increase in FVC: 2-10 min in the LC trial, 2-7 min in the HC trial, 2-7 min in the LW trial, and 2-6 min in the HW trial after the start of exercise. Then the second component was determined from the rapid increase in FVC: 10-15 min in the LC trial, 7-12 min in the HC trial, 7-17 min in the LW trial, and 6-12 min in the HW trial. The third component was determined from the measurements after the second component. The Tes threshold for increasing FVC and the second slope of increase (
) in FVC (
FVC) at a given
Tes (
FVC/
Tes) were determined in each
subject for statistical analyses, and the findings are summarized in
Table 2. The threshold and slope
were determined by three separate investigators who were familiar with
the method, and the three values measured by them were averaged. In
addition, the change in the Tes vs. FVC relationship after
training was analyzed by subtracting the pretraining FVC from the
posttraining FVC at every 0.1°C increment of Tes during
exercise in each subject. The missing FVC values at a given Tes were estimated from neighboring points by interpolation
(Fig. 2).
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Blood Properties
The blood to determine PV was also used to measure the Hb concentration (in g/dl; cyanomethohemoglobin method) and Hct (in percent; microcentrifuge method). After the remaining blood was centrifuged, the aliquots of plasma were used to determine the plasma protein concentration (in g/dl; refractometry) and plasma osmolality (Posmol; in mosmol/kgH2O; freezing point depression method; one-ten osmometer; Fiske).Statistics
One-way ANOVA for repeated measures was used to test the difference in exercise intensity and SL during the 10-day training in each trial. Significant differences at various times were determined with Fisher's least significance difference test (Fig. 3A1, B1, C1, and D1). This ANOVA was also used to test the differences in the variables of body weight,
O2 peak, and blood properties (Table
1); and Tes threshold for increasing FVC,
FVC/
Tes, and SL (Table 2) before and after training
in each trial. One-way ANOVA was used to test the differences among the
trials in the changes of these variables after training (Tables 1 and
2). This ANOVA was also used to test the differences in the integrated values of HR,
HR, exercise intensity, and SL for the 10-day training among the trials (Fig. 3A2, B2, C2,
and D2). Two-way ANOVA for repeated measures was used to
test the differences in HR, MAP, Tes, and

) in the comparison of variables among the trials, we
confirmed that the effect size was >0.40 for the F test in
ANOVA, classified as large effect size by Cohen (2), where
statistical power is 0.25 in Tables 1 and 2 (4 trials, n = 20) and 1.00 in Fig. 2 (4 trials, n = 200). Both values were shown in the comparison of mean values among
the trials to demonstrate the power of statistical analyses.
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RESULTS |
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HR, Exercise Intensity, and SL Changes During Each Day's Exercise Training for 10 Days
Figure 3A1 shows HR at the first 5 min of exercise during each day's training for 10 days. Exercise intensity was readjusted after the first 5 min of exercise before Tes increased so that subjects trained themselves at the same relative intensity, ~60%
O2 peak, each day
during the training period. As shown in Fig. 3A1, the HR
during the first 5 min was maintained at 135-140 beats/min. The HR
integrated for the 10-day training period was ~1,400
(beats · min
1 · 10 days
1)
without any significant differences among the trials, as shown in Fig.
3A2 (P > 0.67), suggesting that the
relative exercise intensity was similar during the 10-day training
among the trials.
Although subjects exercised at a constant exercise intensity, their HR
increased with increased body temperature, which is known as
"cardiovascular drift" (6). Figure 3B1
shows the
HR from 5 to 60 min of exercise, during each day's
exercise training, for 10 days. The
HR in the cool (C) trials was
only ~15 beats/min and was maintained at this level until the end of
training. In contrast, the
HR values for the warm (W) trials were
~25 beats/min on the first day of training, which were significantly
higher than those in the C trials. However, the
HR for the LW trial rapidly decreased on the 7th day of training and remained at the reduced level thereafter, with significant differences from the value
on the 1st day of training. However, the
HR for the HW trial was
maintained at the level of the 1st day throughout the 10-day training.
Significant differences between the LW and HW trials were observed
after 7 days (P < 0.01). As shown in Fig. 3B2, the integrated
HR was highest in the HW trial, with
significant differences between the LC and LW trials (P < 0.05) and between the HC and HW trials (P < 0.01),
suggesting that cardiovascular drift during exercise, an index of heat
loading, was significantly higher in the W trials than in the C trials.
Figure 3C1 shows the exercise intensity during each day of the training period. The intensity in all trials increased gradually with training, and a significant increase occurred on the 2nd day in the LC trial, on the 4th day in the HC and LW trials, and on the 5th day in the HW trial. However, as shown in Fig. 3C2, the exercise intensity, integrated for the 10-day training period, was 1,400-1,600 (W/10 days) without any significant differences among the trials (P > 0.35), suggesting that integrated exercise intensity for 10-day training was similar among the trials.
Figure 3D1 shows total SL after 1-h exercise each day of the training period. The SL in all trials increased gradually along with the training, and significant increases occurred on the 2nd day in the HC trial, on the 4th day in the LW trial, on the 5th day in the HW trial, and on the 6th day in the LC trial. As shown in Fig. 3D2, the SL integrated for the 10-day training period was 203 ± 21 ml/kg in the LW trial, which was significantly higher than the 140 ± 8 ml/kg in the LC trial (P < 0.01). Moreover, the integrated SL in the HW trial was 176 ± 15 ml/kg, which was significantly higher than the 121 ± 11 ml/kg in the HC trial (P < 0.05). However, there were no significant differences in SL between the H and low-altitude (L) trials.
Physical Characteristics, BV, and Blood Properties
As shown in Table 1, there were no significant changes in body weight after training in any trial.
O2 peak in all trials increased
significantly by 7-11% (P < 0.05) but without significant differences among the trials. BV and PV in all trials increased significantly (P < 0.05) after training but
without significant differences among the trials (P > 0.49). EV in the H trials, however, increased significantly but not in
the L trials. Hb concentration in the L trials decreased significantly
but not in the H trials, with significantly less decreases in the H
trials than in the L trials, where the statistical power was 0.58 and the effects size was 0.66. Hct did not change significantly after training in any trial, but the reduction after training for the H
trials was significantly lower than that for the L trials
(P < 0.05), where the statistical power was 0.50 and
the effects size was 0.60. There were no significant differences in
plasma protein concentration and Posmol before and after
training in any trial.
FVC Response Test
Table 3 shows the HR, MAP, Tes, and


Figure 1 illustrates FVC as a function of Tes during the
FVC response test, and the Tes threshold for increasing
FVC,
FVC/
Tes of the second component, and SL in each
subject are summarized in Table 2 for statistical analyses. The
Tes threshold was significantly decreased in the LW
(P < 0.05) and HW (P < 0.01) trials
after training. The magnitude of the Tes threshold in the
HW trial was significantly higher than in the LC trial
(P < 0.05), where the statistical power was 0.52 with
an effect size of 0.62. The second slope of
FVC/
Tes
increased significantly in the LC, LW, and HW trials (P < 0.05), whereas in the HC trial it remained unchanged. The magnitude
of the increase in the slope for the HW trial was significantly higher
than in the LC trial (P < 0.05), where the statistical
power was 0.65 with an effect size of 0.71. The SL decreased
significantly in the HW trial (P < 0.05), whereas that in the HC trial tended to increase after training but without any
significant difference among the trials.
Figure 2 shows the change in FVC response to increased Tes after training. In the LC trial, the FVC response was significantly enhanced above 37.4°C Tes after training (P < 0.05), whereas that in the HC trial tended to be reduced, and significant differences were observed above 37.4°C Tes relative to that in the LC trial (P < 0.01). The FVC response in the LW trial was significantly improved above 37.2°C Tes (P < 0.05) but was not significantly different from that in the LC trial. In contrast, the FVC response in the HW trial was significantly improved compared with that in the LW trial, and significant increases relative to that in the LW trial were observed over the range of Tes, except for 37.7 and 37.9°C (P < 0.01). The statistical power and effective size for the comparison among the trials were 1.00 and 0.49, respectively.
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DISCUSSION |
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The present study was conducted to test the hypothesis that
training in a hypobaric hypoxic and warm environment would increase
O2 peak and sensitivity of cutaneous
vasodilation in hyperthermia more than training in either environment
alone, by increasing both PV and EV. However, the increases in
O2 peak and BV were similar among the
trials, although EV increased significantly higher in the H trials,
whereas it remained unchanged in the L trials. In addition, the FVC
response to increased Tes tended to be enhanced more in the
W trials than in the C trials, despite the similar increase in BV, with
the highest magnitude in the HW trial and the lowest in the HC trial.
These findings suggest that factors other than BV, related to
atmospheric temperature and Patm for endurance training, were involved
in the varied FVC response.
In the present study, the number of subjects per trial would be too small for sufficient statistical analyses in the comparison of variables among the trials. However, this number of subjects was maximal for us to accomplish the study within a limited period of 1 yr to avoid any seasonal effects on the results. As mentioned above, we rejected the null hypothesis at P < 0.05 after confirming that the level of the effect size was >0.40, which was recognized as a large level in the F test of ANOVA (2).
Another concern in the design of the present study was the examination
of the aerobic capacity and FVC response to increased Tes
up to 5 days after the cessation of training, during which period
responses would be returning toward pretraining levels. However, PV
measurement and the FVC response test were performed within 2 days
after the training, followed by the
O2 peak measurement. Moreover, as shown
in Table 3, HR at 5 min after the start of exercise for the FVC
response test was reduced by ~5 beats/min at the same intensity of
60% pretraining
O2 peak, a 5-8%
reduction in relative exercise intensity, almost equal to the relative
increase in
O2 peak. Thus posttraining
O2 peak was likely to remain unchanged
after the posttraining FVC response test.
As shown in Table 1,
O2 peak increased
by 300 ml/min (5%), and BV increased by 200-250 ml (4-5%)
in every trial. Coyle et al. (5) reported that
O2 peak increased by 200 ml/min (4%)
after acute expansion of 200 ml of PV. Hopper et al. (11)
reported that, in untrained adult men, stroke volume during submaximal
exercise increased by 11% in response to acute expansion of 400 ml of
PV. Also, 200 ml of acute EV expansion were reported to increase
maximal aerobic power by 200-500 ml/min (23). Thus,
in the present study, the increase in
O2 peak at a given increase in BV was
almost identical to that obtained from acute expansion of PV or EV
(5, 11, 23), suggesting that the increase in
O2 peak was at least partially caused by the increase in BV in the present study.
As shown in Fig. 1 and Table 2, the Tes threshold for
increasing FVC was lowered significantly in the LW trial but not in the
LC trial. The second slope of
FVC/
Tes was
significantly increased in both trials, but the magnitude of the
increase was fourfold higher in the LW trial than in the LC trial.
Moreover, as shown in Fig. 2, the enhanced FVC response in the LW trial occurred at lower Tes than in the LC trial. These findings
were obtained despite the similar increase in BV, suggesting that
factors other than BV were involved in the higher increase in FVC
response in the LW trial.
Roberts et al. (21) examined the effects of endurance
training or heat acclimatization on FBF response to increased
Tes and reported that the Tes threshold for
cutaneous vasodilation decreased significantly more by exercise
training in a hot environment than in a cool environment, although the
changes in the slope of
FBF/
Tes were small and
inconsistent. As for the mechanism, Nadel et al. (16)
suggested that the lowered Tes threshold for sweating after
heat acclimatization was mainly caused by central mechanisms, such as a
reduction in the central nervous system point of zero sweating drive,
whereas the increased sensitivity of sweating at a given
Tes was mainly caused by peripheral mechanisms, such as
an increased sensitivity to the central sweating drive at the glandular
level. Recently, Shido et al. (26) reported in humans that
heat exposure at a fixed time of day shortened the sweating latency and
decreased the rectal temperature threshold for sweating at the same
time of day when exposed to heat, whereas it remained unchanged at
other times of the day. Because BV and Posmol remained
unchanged throughout their study, they suggested that central
modification of thermoregulation would lower the threshold after heat
exposure. Thus not only peripheral, but also central, mechanisms might
be involved in a more enhanced FVC response for the LW trial.
Experimentally, integrated
HR (Fig. 3B1) and SL (Fig.
3D1) during training were significantly greater in the LW
trial than in the LC trial, suggesting more heat loading during training in the LW trial.
The FVC response in the HC trial remained unchanged, despite the
significant increases in EV and PV (Figs. 1 and 2, Table 2). Sawka et
al. (24) reported that an ~200-ml increase in EV by
acute infusion of erythrocyte attenuated the
Tes during exercise in a hot environment. Recently, they reported that a 200-ml
increase in EV reduced the Tes threshold for sweating and enhanced the sensitivity of sweating at a given
Tes
(25). They postulated that polycythemia would enable a
greater fraction of cardiac output to perfuse the skin and enhance
sweating because oxygen transport requirements for a given level of
submaximal exercise would be achieved with lower muscle blood flow. To
examine that hypothesis, Patterson et al. (20) recently
studied the effects of acute infusion of 400 ml of whole blood, of
which Hct was 60%, on temperature regulation during exercise. However,
they found that the SkBF response was attenuated by increased EV,
whereas sweating was enhanced. They suggested that the lower core
temperature due to enhanced sweating reduced the SkBF response. In the
HC trial, EV was significantly increased by 92 ml, and SL in the FVC
response test increased in four of five subjects but with no
statistical significance in mean values. Thus the present findings appear to agree with those of Patterson et al. (20),
suggesting that the increased EV did not increase the FVC response in
the HC trial.
In contrast, the exposure to a hypobaric hypoxic and hot environment in
the HW trial appeared to increase the FVC response by a greater extent
than in the LW trial (Fig. 2 and Table 2). This finding may be
explained by more heat loading in the HW trial than in the LW trial
after 7 days of training. As shown in Fig. 3B1,
cardiovascular drift estimated from
HR in the LW trial decreased after 7 days of training, which may have been caused by enhanced heat
dissipation due to increased evaporative heat loss and/or heat
conductance (8). However,
HR in the HW trial remained unchanged until the end of training. Because cardiovascular drift is
known to reflect increased Tes (6), the higher
HR in the HW trial after 7 days of training suggested that the
Tes during exercise training remained higher in the HW
trial than in the LW trial until the end of the 10-day training. The
higher Tes loading in the HW trial might have increased the
FVC response more in the LW trial by modifications of central and
peripheral thermoregulatory mechanisms, as described above (16,
26).
The precise reason for the higher
HR (or Tes) in the HW
trial compared with the LW trial after 7 days of training is unclear. However, Kolka et al. (13) studied the body temperature
regulation during exercise on a cycle ergometer at 60% of
altitude-specific
O2 peak in an
artificial chamber, where the altitudes were simulated sea level, 2,596 m, and 4,575 m and where Ta was controlled at 30°C and
30% RH, equivalent to the environment of the W trials in the present
study. They reported that the sensitivities of the increases in FBF and
the sweat rate at a given
Tes were both reduced with
increasing altitude. Thus the higher heat loading and higher
Tes in the HW trial compared with the LW trial may have
been caused by the reduced heat dissipation function at 2,000 m, which
may overcome the effect of the increased FVC response in the HW trial
measured at 610 m (Fig. 1).
Another possible explanation for the most enhanced FVC response in the
HW trial was due to the significant increase in EV of 130 ml for the HW
trial. Sawka et al. (25) reported that the sensitivity of
the sweating response to increased Tes at a given increase
in EV was more enhanced in heat-acclimatized subjects than in those
unacclimatized. If it is true also in the case of the FVC response, the
increased EV would have enhanced the sensitivity synergistically with
heat acclimatization in the HW trial. Thus heat acclimatization in a
hypobaric hypoxic environment increased the sensitivity of
FVC/
Tes more than in a normobaric and normoxic environment, which might be related to the increased EV in addition to
heat exposure.
In summary, the
O2 peak in all trials
increased similarly with a concomitant increase in BV but without any
significant differences among the trials against our hypotheses.
Moreover, the FVC response to hyperthermia varied among the trials,
regardless of BV, increasing more after training in a warm environment
than in a cool environment at a given altitude. However, the magnitude of the increase in FVC response was more enhanced after heat
acclimatization at a high altitude than at sea level. Thus the FVC
response after endurance training was affected by other factors than
BV, such as by Patm as well as temperature for training.
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ACKNOWLEDGEMENTS |
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We thank the volunteer subjects for participating in this study.
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FOOTNOTES |
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This study was supported in part by grants from the Uehara Memorial Foundation; the Descente and Ishimoto Memorial Foundation for the Promotion of Sports Science; and the Ministry of Education, Science, Sports and Culture of Japan. For this study, Y. Takeno was a recipient of the Recognition Award for Meritorious Research at Experimental Biology 2000 from the American Physiological Society, Environmental and Exercise Physiology Section.
Address for reprint requests and other correspondence: H. Nose, Dept. of Sports Medicine, Shinshu Univ. School of Medicine, 3-1-1 Asahi Matsumoto 390-8621, Japan (E-mail: nosehir{at}sch.md.shinshu-u.ac.jp).
The costs of publication of this article were defrayed in part by the payment of page charges. The article must therefore be hereby marked "advertisement" in accordance with 18 U.S.C. Section 1734 solely to indicate this fact.
Received 28 November 2000; accepted in final form 25 May 2001.
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REFERENCES |
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|
|
|---|
1.
Brengelmann, GL,
Johnson JM,
Hermansen L,
and
Rowell LB.
Altered control of skin blood flow during exercise at high internal temperature.
J Appl Physiol
43:
790-794,
1977
2.
Cohen, J.
Statistical Power Analysis for the Behavioral Sciences (2nd ed.). Hillsdale, NJ: Lawrence Erlbaum Assoc, 1988, p. 273-403.
3.
Convertino, VA,
Greenleaf JE,
and
Bernauer EM.
Role of thermal and exercise factors in the mechanism of hypervolemia.
J Appl Physiol
48:
657-664,
1980
4.
Costill, DL,
Branam G,
Fink W,
and
Nelson R.
Exercise induced sodium conservation: changes in plasma renin and aldosterone.
Med Sci Sports Exerc
8:
209-213,
1976.
5.
Coyle, EF,
Hopper MK,
and
Coggan AR.
Maximal oxygen uptake to plasma volume expansion.
Int J Sports Med
11:
116-119,
1990[Web of Science][Medline].
6.
Ekelund, LG.
Circulatory and respiratory adaptation during prolonged exercise.
Acta Physiol Scand
292, Suppl:
1-38,
1967.
7.
Fortney, SM,
Vroman NB,
Beckett WS,
and
LaFrance ND.
Effect of exercise hemoconcentration and hyperosmolality on exercise responses.
J Appl Physiol
65:
519-524,
1988
8.
Gisolfi, C,
and
Robinson S.
Relations between physical training, acclimatization, and heat tolerance.
J Appl Physiol
26:
530-534,
1969
9.
Greenleaf, JE,
Convertino VA,
and
Mangseth GR.
Plasma volume during stress in man: osmolality and red cell volume.
J Appl Physiol
47:
1031-1038,
1979
10.
Gregersen, MI,
and
Rawson RA.
Blood volume.
Physiol Rev
39:
307-342,
1959
11.
Hopper, MK,
Coggan AR,
and
Coyle EF.
Exercise stroke volume relative to plasma volume expansion.
J Appl Physiol
64:
404-408,
1988
12.
Kamijo, Y,
Takeno Y,
Sakai A,
Inaki M,
Okumoto T,
Itoh J,
Yanagidaira Y,
Masuki S,
and
Nose H.
Plasma lactate concentration and muscle blood flow during dynamic exercise with negative-pressure breathing.
J Appl Physiol
89:
2196-2206,
2000
13.
Kolka, MA,
Stephenson LA,
Rock PB,
and
Gonzalez RR.
Local sweating and cutaneous blood flow during exercise in hypobaric environments.
J Appl Physiol
62:
2224-2229,
1987
14.
Mier, CM,
Domenick MA,
Turner NS,
and
Wilmore JH.
Changes in stroke volume and maximal aerobic capacity with increased blood volume in men and women.
J Appl Physiol
80:
1180-1186,
1996
15.
Nadel, ER.
Physiological adaptations to aerobic training.
Am Sci
73:
334-343,
1985.
16.
Nadel, ER,
Pandolf KB,
Roberts MF,
and
Stolwijk JA.
Mechanisms of thermal acclimation to exercise and heat.
J Appl Physiol
37:
515-520,
1974
17.
Nagashima, K,
Nose H,
Takamata A,
and
Morimoto T.
Effect of continuous negative-pressure breathing on skin blood flow during exercise in a hot environment.
J Appl Physiol
84:
1845-1851,
1998
18.
Nielsen, B,
Rowell LB,
and
Bonde-Petersen F.
Cardiovascular responses to heat stress and blood volume displacement during exercise in man.
Eur J Appl Physiol Occup Physiol
52:
370-374,
1984[Medline].
19.
Nose, H,
Mack GW,
Shi X,
Morimoto K,
and
Nadel ER.
Effect of saline infusion during exercise on thermal and circulatory regulations.
J Appl Physiol
69:
609-616,
1990
20.
Patterson, MJ,
Cotter JD,
and
Taylor NA.
Thermal tolerance following artificially induced polycythaemia.
Eur J Appl Physiol Occup Physiol
71:
416-423,
1995[Medline].
21.
Roberts, MF,
Wenger CB,
Stolwijk JA,
and
Nadel ER.
Skin blood flow and sweating changes following exercise training and heat acclimation.
J Appl Physiol
43:
133-137,
1977
22.
Sawka, MN,
Convertino VA,
Eichner ER,
Schnieder SM,
and
Young AJ.
Blood volume: importance and adaptations to exercise training, environmental stresses, and trauma/sickness.
Med Sci Sports Exerc
32:
332-348,
2000[Web of Science][Medline].
23.
Sawka, MN,
and
Coyle EF.
Influence of body water and blood volume on thermoregulation and exercise performance in the heat.
Exerc Sport Sci Rev
27:
167-218,
1999[Medline].
24.
Sawka, MN,
Dennis RC,
Gonzalez RR,
Young AJ,
Muza SR,
Martin JW,
Wenger CB,
Francesconi RP,
Pandolf KB,
and
Valeri CR.
Influence of polycythemia on blood volume and thermoregulation during exercise-heat stress.
J Appl Physiol
62:
912-918,
1987
25.
Sawka, MN,
Gonzalez RR,
Young AJ,
Dennis RC,
Valeri CR,
and
Pandolf KB.
Control of thermoregulatory sweating during exercise in the heat.
Am J Physiol Regulatory Integrative Comp Physiol
257:
R311-R316,
1989
26.
Shido, O,
Sugimoto N,
Tanabe M,
and
Sakurada S.
Core temperature and sweating onset in humans acclimated to heat given at a fixed daily time.
Am J Physiol Regulatory Integrative Comp Physiol
276:
R1095-R1101,
1999
27.
Terrados, N,
Melichna J,
Sylven C,
Jansson E,
and
Kaijser L.
Effects of training at simulated altitude on performance and muscle metabolic capacity in competitive road cyclists.
Eur J Appl Physiol Occup Physiol
57:
203-209,
1988[Web of Science][Medline].
28.
Whitney, RJ.
The measurement of volume changes in human limbs.
J Physiol (Lond)
121:
1-27,
1953.
29.
Wyndham, CH,
Rogers GG,
Senay LC,
and
Mitchell D.
Acclimization in a hot, humid environment: cardiovascular adjustments.
J Appl Physiol
40:
779-785,
1976
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