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Departments of 1 Clinical Studies and 2 Pathobiology, Ontario Veterinary College, University of Guelph, Guelph, Ontario, Canada N1G 2W1
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ABSTRACT |
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This study examined the effects of
hyperhydration, exercise-induced dehydration, and oral fluid
replacement on physiological strain of horses during exercise-heat
stress. On three occasions, six horses completed a 90-min exercise
protocol (50% maximal O2 uptake,
34.5°C, 48% relative humidity) divided into two 45-min periods
(exercise I and
exercise II) with a 15-min recovery
between exercise bouts. In random order, horses received
no fluid (NF), 10 liters of water (W), or a carbohydrate-electrolyte
solution (CE) 2 h before exercise and between exercise bouts. Compared with NF, preexercise hyperhydration (W and CE) did not alter heart rate, cardiac output (
), stroke volume (SV), core
body temperature, sweating rate (SR), or sweating sensitivity during
exercise I. In contrast, after
exercise II, exercise-induced
dehydration in NF (decrease in body mass: NF, 5.6 ± 0.8%; W, 1.1 ± 0.4%; CE, 1.0 ± 0.2%) resulted in greater heat storage,
with core body temperature ~1.0°C higher compared with W and CE.
In exercise II, the greater thermal
strain in NF was associated with significant
(P < 0.05) decreases in
(10 ± 2%), SV (9 ± 3%), SR, and sweating
sensitivity. We concluded that 1)
preexercise hyperhydration provided no thermoregulatory advantage;
2) maintenance of euhydration by
oral fluid replacement (~85% of sweat fluid loss) during exercise in
the heat was reflected in higher
, SV, and SR with
decreased heat storage; and 3) W or
an isotonic CE solution was equally effective in reducing physiological strain associated with exercise-induced dehydration and heat stress.
dehydration; hyperhydration; oral fluid replacement; sweating; ion losses; temperature regulation; body temperature; equine
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INTRODUCTION |
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IN HUMAN ATHLETES it is well established that
hypohydration, or a reduction in total body water (TBW), impairs
cardiovascular function and increases heat strain during prolonged
dynamic exercise (1, 8, 28, 34, 35). Moreover, the
increments in thermal and cardiovascular strain are directly related to
the magnitude of hypohydration (28, 35). In horses, as in humans,
cutaneous evaporative heat loss (sweating) is the primary mechanism for temperature regulation during exercise (18). Rates of sweat fluid loss
in horses can exceed 10-12 l/h (25), and, even in moderate ambient
conditions, dehydration equivalent to ~6% or more of body mass can
result during 2-3 h of exercise (19). However, the nature of this
exercise-induced dehydration and the impact of the resultant body-water
deficit on thermoregulatory function differ between equine and human
athletes. The ionic composition of equine sweat during exercise is
isotonic to hypertonic (19, 25), with an osmolality ranging from ~290
to 320 mosmol/kgH2O, whereas human
sweat is hypotonic relative to extracellular fluid (ECF).
Therefore, heavy sweat losses will elicit a hypertonic hypohydration in
human subjects, whereas the approximately isotonic nature of equine
sweat results in an isosmotic to hyposmotic hypohydration. Because
plasma hyperosmolality has been demonstrated to impair thermoregulation
(12, 17, 29), an isotonic fluid loss could mitigate the effect of
hypohydration on thermoregulatory mechanisms. Kingston et al. (20)
reported that progressive dehydration (~6% loss of body mass) did
not alter sweating rate (SR) or heat storage in horses during >3 h of
low-intensity exercise [40% maximal
O2 uptake
(
O2 max)] in
moderate ambient conditions. Conversely, Naylor and co-workers (30)
demonstrated that isotonic and hypertonic hypohydration (3.2-3.9%
decrease in body mass) induced before exercise resulted in increased
heat storage during 40 min of exercise at 40%
O2 max in similar
conditions. This impairment to thermoregulation was attributed to
decrements in heat transfer from core to periphery rather than
decreases in SR or sensitivity of the sweating response (30). Taken
together, these findings suggest that, at least during low-intensity
exercise in moderate ambient conditions, hydration state has no effect
on sweating responses and the rate of cutaneous evaporative heat loss
in horses. Importantly, however, no study has evaluated the effects of
hydration state on thermoregulation in horses during exercise-heat
stress, when the greater thermal strain increases reliance on sweating
for heat dissipation.
Given the detrimental effects of hypohydration on thermoregulation,
appropriate strategies for fluid replacement are required to minimize
thermal strain and optimize exercise performance. In human subjects,
fluid-replacement strategies that limit increases in plasma
hyperosmolality will mitigate any impairment to thermoregulation associated with hypohydration (8, 14, 35). Several investigators have
reported that pure water or hypotonic solutions are similarly effective
for attenuation of thermal and circulatory strain during exercise-heat
stress (2-4). In horses, however, secretion of electrolyte-rich
sweat (Na+ concentration
~120-140 mM; Cl
concentration ~135-155 mM) results in marked contraction of the ECF space but minimal change in extracellular osmolality (19, 25). In
this circumstance, ingestion of water could dilute the ECF space and
limit mobilization of water from the intracellular fluid (ICF) space to
the ECF compartment. Conversely, ingestion of sodium-containing fluid
may assist in the maintenance of ECF and blood volumes by creating an
osmotic gradient between the ECF and ICF spaces (31). No study has
evaluated the effects of water vs. an isotonic electrolyte solution on
thermal and circulatory regulation in horses during exercise-heat
stress.
Preexercise hyperhydration (increased TBW) has been advocated for reduction of thermal strain during exercise-heat stress. However, there are conflicting results regarding the thermoregulatory effects of hyperhydration during exercise in human subjects. Some investigators have reported that hyperhydration can reduce thermal strain (16, 23), whereas other studies have indicated no thermoregulatory advantage over the maintenance of euhydration during exercise (3, 22). Given the difficulty in ensuring adequate voluntary fluid intake by horses, preexercise hyperhydration is a practical strategy for optimization of fluid balance during prolonged exercise. Sosa León et al. (37) reported no differences between hyperhydrated and control horses for cardiac output, heart rate, or rise in core body temperature (Tcore) during 90 min of exercise despite maintenance of a higher plasma volume in the fluid-treated group. Importantly, however, these trials were conducted in moderate ambient conditions (19-20°C); in hotter conditions, when rates of sweat fluid loss and rise in Tcore are greater, it is possible that hyperhydration will assist cardiovascular and thermoregulatory responses during exercise.
The primary purpose of this study was to examine the effects of hydration state on physiological strain of horses during exercise-heat stress. Specifically, we determined the effects of hyperhydration, and of hypohydration with or without oral fluid replacement, on thermal and circulatory responses during 90-min of moderate-intensity exercise in hot ambient conditions. We hypothesized that 1) preexercise hyperhydration would enhance thermoregulatory responses (lower Tcore, improve sweating) compared with euhydrated subjects and 2) maintenance of euhydration by oral fluid replacement would reduce physiological strain during exercise-heat stress. We further hypothesized that addition of electrolytes to oral rehydration solutions would improve the effectiveness of oral fluid replacement. Therefore, a further objective of the study was to compare the efficacy of water vs. an isotonic electrolyte solution for attenuation of thermal and circulatory strain during exercise.
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MATERIALS AND METHODS |
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The care and use of animals followed the "Guide to the Care and Use of Experimental Animals" (Canadian Council on Animal Care, Ottawa, ON). All animal experiments were conducted after approval by the Animal Care Committee of the University of Guelph and performed in compliance with their recommendations.
Experimental animals.
Six Thoroughbred horses (4 geldings and 2 mares), ranging in age from 3 to 6 yr, and weighing 420-475 kg [455 ± 10.0 (SE) kg], were used. Each horse's right carotid artery was surgically relocated to a subcutaneous position at least 6 mo before the study.
All horses were housed indoors during the experimental period and fed a
diet of timothy grass-alfalfa hay and mixed grain supplemented with 100 g NaCl and 50 g KCl daily. The diet was designed to meet
the National Research Council guidelines for the nutritional
requirements of horses performing regular exercise and training. All
horses were conditioned and undertaking regular treadmill exercise but
were not heat acclimated. The
O2 max of
each horse was determined twice 7-10 days before the start of the
experiments by use of an incremental step test and an
open-circuit calorimeter (13). The mean
O2 max was 140 ± 8 ml · kg
1 · min
1.
From linear regression analysis, the running speed that elicited 50%
O2 max was calculated
for each horse.
Experimental protocols.
The study was designed as a crossover, with each horse completing
standardized exercise tests after each of the following treatments:
1) no fluid (NF): no oral fluid
during the experimental period; 2)
water (W): 20 liters of water, administered via nasogastric tube in
10-liter doses, with the first dose given 2 h before exercise and the
second dose given after 45 min of exercise; and
3) carbohydrate-electrolyte solution
(CE): 20 liters of CE solution administered using the same protocol as
for the W treatment. The CE was isotonic (305 mosmol /kgH2O) and contained
105 mM Na+, 15 mM
K+, 132 mM
Cl
, and 5% carbohydrate
(as sucrose). This volume of fluid was chosen on the basis of previous
studies in our laboratory in which the rate of sweat fluid loss in
trained Thoroughbred horses was measured under similar exercise and
environmental conditions (25). The temperature of the orally
administered W or CE was 25°C. The order of treatments was
randomized (but balanced), with a minimum of 7 days between experiments
for each horse.
O2 max (range 4.4-4.6 m/s) for two 45-min periods (exercise
I and exercise II) with a 15-min rest
between phases, during which the second dose of oral fluid was
administered. A fan mounted above and 0.5 m in front of the treadmill
was used to maintain an air velocity of 3.5-4 m/s over the
anterior and dorsal aspects of the horse. Air velocity was measured
with an anemometer (Davis Instruments, Hayward, CA) positioned at three
sites: lateral midcervical region, lateral and dorsal thorax, and
dorsal to the gluteal region of the hindquarters.
During each phase of exercise, heart rate (HR), pulmonary artery
temperature (Tpa), rectal
temperature (Tre), SR,
hematocrit, and plasma osmolality and total solids concentration (TS)
were measured at 5-min intervals. Middle gluteal muscle temperature (Tmus) was measured before and
after each phase of exercise. O2 uptake (
O2),
CO2 production
(
CO2), respiratory exchange
ratio (RER), cardiac output (
), and stroke volume
(SV) were measured at 0, 5, 15, 30, and 45 min of exercise in each
phase. Body mass was measured immediately before and after
completion of each exercise phase.
Analytic methods. Tpa was measured by inserting a copper-constantan thermocouple (IT-14, Physitemp Instruments, Clifton, NJ) into the pulmonary artery within an 8-Fr polyethylene catheter. For measurement of Tre, a thermocouple (T-180, Physitemp Instruments) was inserted 25-30 cm proximal to the anal sphincter. Tmus was measured by inserting a needle thermocouple (MT-23, Physitemp Instruments) ~4 cm into the muscle through the lumen of an 18-gauge 37-mm needle. All thermocouples had response times of ~1°C/s and were calibrated in a heated water bath with a precision thermometer (Fisher Scientific, Mississauga, ON). All measurements of Tmus were performed after aseptic preparation and local analgesia of the skin.
Local SR was measured on the left lateral thorax by use of a direct sweat-collection method, as described elsewhere (20, 25). In brief, a sealed polyethylene pouch enclosing a 150-cm2 area of skin was attached to an area of shaved skin with a dermal adhesive. The edges of the pouch were further sealed by dermal tape that covered the pouch-skin margin. A ventral reservoir, formed by a deep fold in the polyethylene, separated accumulating sweat from the skin surface and facilitated the removal of all collected sweat through polyethylene tubing (ID 1.67 mm, Intramedic; Becton Dickinson) incorporated into the lateral margin of the pouch. Sweat samples were collected every 5 min throughout each phase of exercise and during the 15 min rest between exercise I and exercise II. SR, expressed as milliliters per square meter per minute, was calculated on the basis of the volume of sweat collected at the end of each time interval from the measured skin area within the pouch. Therefore, the measured SR represents the average rate of sweat production over a 5-min period. Total sweat fluid loss was calculated from the change in body mass after accounting for fecal and estimated respiratory water losses (19, 20). No horse voided urine during any of the trials. Sweating sensitivity was defined as the slope of the regression line representing the individual 5-min local SR and Tpa values obtained during the linear phase of the exercise transient (up to 20-25 min in each bout of exercise) (29). Sweating sensitivity was expressed as milliliters per minute per square meter per degree Celsius. Percent dehydration was estimated from the difference in body mass after each phase of exercise compared with the body weight recorded 2 h before exercise. Arterial and mixed venous blood samples for measurement of hemoglobin concentration, oxygen content, mixed-venous hematocrit, and plasma TS and osmolality were collected before the first fluid treatment, immediately before exercise I and exercise II, and at 5-min intervals during each phase of exercise. Blood samples were collected anaerobically into 7.5-ml syringes containing 100 IU of heparin lithium (Sarstedt, Nümbrecht, Germany); placed in an ice-water bath; and analyzed for hemoglobin concentration, oxygen saturation, and oxygen content within 30 min of collection (OSM 3 Hemoximeter; Radiometer, Copenhagen, Denmark). Hematocrit was determined by the microhematocrit method. Plasma was then separated from the cells by high-speed centrifugation (14,000 rpm for 5 min) and analyzed for TS by refractometry (model SPR-T2, Atago). The percent change in plasma volume (PV) was calculated by using the change in plasma TS (26). This calculation assumes there is no net movement of protein either to or from the vascular compartment during exercise. Plasma osmolality was determined by freezing-point depression (model 3MO Plus, Advanced Instruments, Needham, MA). All analyses were performed in duplicate.
O2 and
CO2 were measured with an
open-flow respiratory gas-collection system consisting of a lightweight
loose-fitting mask; flexible tubing; a flow-controlling baffle; a
section of rigid tubing containing a venturi and a pressure transducer;
a vacuum motor; and a multiport gas-sampling system.
During exercise, flow rates of ~6,000-7,000 l/min were used.
Within 15 min of the start of exercise, the
O2 (Ametek model S-3A/1, Thermox
Instruments Division, Pittsburgh, PA) and
CO2 (Ametek model CD-3A, Thermox Instruments Division) analyzers were calibrated against a certified gas
mixture (Canox, Mississauga, ON). A differential pressure transducer
(Validyne, Northbridge, CA) was used to monitor flow rate, and the
system was calibrated before and after each experiment by use of the
nitrogen-dilution technique (10). Both gas analyzers and the pressure
transducer were interfaced with a laboratory computer (Apple IIe) and
processed by using a scientific software package (Superscope II, GW
Instruments, Somerville, MA). Standard equations were used to calculate
O2 and
CO2. At each measurement period, gas samples for determination of
O2 and
CO2 were collected at 10-s
intervals for 2 min; the data reported represent mean values for
O2 and
CO2 during each measurement
period. The RER values were calculated by dividing
CO2 by
O2. A cardiotachometer (Equistat model HR-8A, Equine Exercise Physiology and Biomechanics, Unionville, PA) was applied on the horse's chest to record HR.
was calculated, by using the Fick principle, from
measured
O2 and the
arteriovenous O2 content
differences at each time point. SV was derived from the quotient of
and HR.
Statistical analyses. Data were analyzed by using two-way analysis of variance for repeated measures, with main effects of fluid treatment and time. After a significant F-test, Student-Newman-Keuls (to detect differences between fluid treatments) and Dunnett's (to detect differences within a treatment group) tests were used to identify pairwise differences. Regression analyses were utilized to examine effects of hydration state and plasma osmolality on sweating responses. Differences were considered significant when P < 0.05. All data are expressed as means ± SE.
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RESULTS |
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Effects of preexercise fluid administration. Significant (P < 0.01) decreases in hematocrit and plasma TS were evident 2 h after fluid administration (i.e., immediately before exercise) (Fig. 1, A and B), indicating hyperhydration in W and CE conditions before exercise compared with NF. Values for hematocrit and plasma TS in NF were unchanged at the end of the 2-h period before exercise. PV immediately before exercise I, as determined by changes in plasma TS, was increased by 8.7 and 12.1% for the W and CE treatments, respectively. Administration of W resulted in a significant (P < 0.05) decrease in plasma osmolality (Fig. 1C), whereas plasma osmolality was unchanged in NF and CE.
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Metabolic responses.
One horse in the NF treatment was unable to complete the exercise
protocol because of fatigue. At the point of fatigue (30 min in
exercise II),
Tpa in this horse was 42.5°C.
As a result, data from the end of exercise in NF represent means ± SE for five horses. There was no effect of treatment on
O2,
CO2, and RER during exercise
(Table 1). Aerobic heat production was
estimated from the
O2 data.
It was assumed that each liter of
O2 consumed had an energy
equivalent of 21 kJ and that 80% of the calorific value of
O2 was released as heat (18). When
normalized for body surface area [body surface area = 1.09 + 0.008 × body mass (kg)], aerobic heat production ranged
from 1,629 ± 95 to 1,795 ± 77 W/m2, with no significant
between-trial differences.
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Changes in body mass and blood variables in response to exercise. Loss of body weight in the W and CE treatments, as a result of the 20 liters of fluid administered, was significantly (P < 0.01) lower compared with NF (Table 2). In NF, body mass was decreased by 24.1 ± 2.5 kg after exercise (5.6 ± 0.8% of preexercise body mass). When expressed as a percentage of preexercise TBW (0.66 × body mass; Ref. 5), this decrease represented an ~8% reduction in TBW. In contrast, in W and CE treatments, the net decreases in body mass and TBW were ~1.0 and 1.5%, respectively, of pretrial body weight.
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Temperature responses. Figure 3, A and B, shows Tpa and Tre during exercise. The rise in Tpa and Tre during exercise I (~3.2 and 2.5°C, respectively) was not significantly different between the three trials. During the final 20 min of exercise II, Tpa and Tre were significantly (P < 0.01) higher in NF compared with W and CE. At the end of exercise Tpa and Tre were ~1.0 and ~0.8°C, respectively, higher in NF than in W and CE. In all treatments, Tmus increased by ~4°C during exercise I, with no significant difference between trials (Table 2). In contrast, the increase in Tmus during exercise II was significantly (P < 0.01) greater in NF compared with W and CE. At the end of exercise, Tmus was ~1°C higher in NF than in W and CE.
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Sweating responses.
SRs during exercise, as determined by the volume of sweat collected
from the sealed pouch on the thorax, are presented in Fig.
4. In all treatments, SRs increased from
the start of exercise and continued to increase until the end of
exercise I; SRs were similar among the
three trials. Although SRs declined during the 15-min period between
exercise phases, SRs at the start of exercise II were ~16-20
ml · m
2 · min
1.
In all treatments, SRs increased rapidly during the initial 20-25
min of exercise II. SR then remained
relatively constant for the remainder of exercise in W and CE, with
values for SR significantly (P < 0.05) higher compared with the corresponding time points in
exercise I. In contrast, after the
first 15-20 min of exercise II,
there was a decline in SR in NF such that values were significantly
(P < 0.05) lower compared with W and CE during the final 20 min of exercise
II. Consistent with this decrease in local SR, whole
body sweat fluid loss during exercise II was significantly
(P < 0.05) lower in NF (11.4 ± 0.6 liters) than in W (13.5 ± 1.0 liters) and CE (13.8 ± 0.7 liters). In W and CE, the volume of fluid administered before and
during the exercise trial replaced ~85% of sweat losses (Table 2).
Mean values for sweating sensitivity during exercise are presented in
Fig. 5. There were no between-group
differences for sweating sensitivity during exercise
I. However, in exercise
II, sweating sensitivity in NF was significantly
(P < 0.05) lower compared with W and
CE. Figure 6 depicts the relationship
between sweating sensitivity during exercise
II and both total body mass loss
(n = 18 observations) and final plasma
osmolality (n = 18 observations). Sweating sensitivity decreased as
total body mass loss (P < 0.001) and
plasma osmolality (P < 0.005)
increased.
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Cardiovascular responses to exercise.
In W and CE, HR,
, and SV were stable throughout
exercise (Fig. 7,
A-C). In NF, the cardiovascular
responses were similar to the other treatments during
exercise I. However, there were progressive decreases in
and SV during the final 30 min of exercise II such that values
were significantly (P < 0.05) lower than in W and CE at 30 and 45 min of exercise in this bout.
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DISCUSSION |
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The major question addressed in this study was whether preexercise hyperhydration or attenuation of progressive dehydration would improve thermal and circulatory regulation in horses during moderate-intensity exercise in hot conditions. To answer this question, we have measured thermal, sweating, and cardiovascular responses during 90 min of exercise, with subjects receiving NF (control condition), W, or an isotonic CE solution before and at the midpoint of the trial. Under the moderately hot environmental conditions (34.5 ± 0.3°C, 48 ± 5% relative humidity), we hypothesized that evaporative heat loss (sweating) would be the primary mechanism for heat dissipation and, in subjects not provided fluid, the large sweat fluid losses would result in substantial dehydration. Furthermore, we hypothesized that decrements in internal and peripheral heat transfer associated with progressive dehydration would exacerbate heat storage during exercise.
The most significant findings of the present study were
1) preexercise hyperhydration (W and
CE in exercise I) provided no thermoregulatory advantage compared with NF;
2) maintenance of euhydration by
oral administration of fluid (W and CE in exercise II) at a volume equivalent to ~85% of sweat fluid
loss mitigated heat storage, as reflected by lower
Tpa,
Tre, and
Tmus at the end of exercise;
3) maintenance of euhydration
prevented decrements in local SR, sweating sensitivity,
, and SV associated with dehydration in the NF
condition; and 4) W or an isotonic
CE solution was equally effective in reducing physiological strain
associated with exercise-induced dehydration and heat stress.
Few studies have examined the influence of preexercise fluid
administration (hyperhydration) on thermoregulatory and cardiovascular responses in the horse during prolonged exercise. Sosa León and colleagues (37) administered fluid equivalent to 4% of body weight 90 min before an exercise test consisting of 90 min of low-intensity
exercise (30%
O2 max).
In that study, fluid-treated horses maintained higher PV during
exercise compared with untreated controls, but there were no
differences between treatments for cardiovascular and thermal
variables. The work intensity and ambient conditions employed in the
present study represented a much higher thermoregulatory strain, as
reflected by end-exercise core temperatures (Tpa) that were
~1.5-2.5°C higher than those reported in the study by Sosa
León et al. for work of similar duration. Despite the higher
workload and more severe environmental conditions we found no evidence
that preexercise hyperhydration reduced physiological strain.
Similarly, Latzka et al. (22) reported that preexercise hyperhydration
(water or glycerol) in human subjects did not provide any additional
thermoregulatory advantage over maintenance of euhydration during
compensable exercise-heat stress.
In human subjects, numerous investigations have demonstrated that even small amounts of dehydration (1-2% reduction in body weight) during moderate-intensity exercise can augment core temperature (4, 28, 34, 35). Furthermore, the magnitude of hyperthermia is directly related to the amount of dehydration accrued during moderate-intensity exercise (28). It also has been demonstrated that the optimal rate of fluid ingestion to attenuate hyperthermia and decrements in cardiovascular function is the rate that most closely matches the extent of fluid loss (8, 28, 34). While the dose of fluid administered in this study did not represent total fluid losses, when compared with NF, replacement of ~85% of sweat fluid losses was effective at attenuating hyperthermia at the exercise intensity and environmental conditions chosen for this experimental protocol.
Our results indicate that the fluid administered was absorbed before exercise and prevented the secondary hemoconcentration that occurred in NF after the initial decrease in PV after the onset of exercise. Furthermore, W or an isotonic CE solution were similarly effective for attenuation of progressive dehydration during exercise. When no fluid was administered, hemoconcentration during exercise was reflected by progressive increases in hematocrit and plasma TS and osmolality during both bouts of exercise (Fig. 1, A and B). In contrast, there was little change in plasma TS and PV (Fig. 2) in W and CE between 5 and 45 min of exercise in the two exercise bouts, indicating that the administered fluid was retained in the vascular compartment. Although there was only a period of ~10 min between administration of the second dose of fluid and the onset of exercise II, it is likely that at least some of this fluid was absorbed. This likelihood is reflected in the further decrease in plasma osmolality in W at the onset of exercise II and minimal change in plasma total solids in W and CE throughout this bout of exercise. Considerable work has been undertaken in exercising human subjects to determine rates of gastric emptying and intestinal absorption of rehydration fluids of various formulations (7, 14, 21, 36), whereas there is little published information on these two processes in horses during exercise (24).
Although our horses were exercising at a moderate intensity, given the
environmental conditions the subjects were unable to achieve a balance
between heat production and dissipation during the first 45 min of
exercise, as reflected by almost linear increases in
Tpa and
Tre. However, no difference in
heat storage was evident between groups at the end of
exercise I. In contrast, at the end of
exercise II, the increase in
Tpa and
Tre was ~0.8 to 1.0°C greater in NF compared with W and CE. Evidence for greater heat storage
in NF was also provided by the ~1.0°C higher value for Tmus at the end of exercise. A
portion of the greater elevation in
Tcore in NF during
exercise II could be attributed to a
direct cooling effect of the fluid administered between
exercise I and exercise II or a decrease in
dissipation of heat (aerobic heat production was similar between
trials). If we assume that the specific heat capacity of the horse is
the same as for humans (3.48 kJ · kg
1 · °C
1),
the cooling effect of the administered fluid (temperature ~25°C) can be estimated on the basis of the specific heat capacity of water
(4.18 kJ · kg
1 · °C
1)
and body temperature at the time of fluid administration
(Tre at the end of
exercise I; Fig.
3B). From these calculations, we estimate that the cooling effect from the administered fluid would result in, at most, an ~0.3°C decrease in Tcore.
Given the ~1°C higher values for
Tpa and
Tre at the end of exercise in NF
compared with W and CE, the greater heat storage must be partially due to a difference in the rate of heat dissipation between the NF and
fluid treatment trials.
Studies in human subjects and other species have established two
principal mechanisms by which dehydration results in a decrease in heat
dissipatory capacity: a reduction in internal transfer of heat from the
body core to the periphery and decreased evaporative heat loss by
decrements in SR and/or sweating sensitivity (1, 3, 8, 17, 28,
29, 34). In the present study, both factors may have contributed to a
decrease in the rate of heat dissipation in NF during the latter stages
of the exercise protocol. Notably, local SR and whole body sweat fluid
loss were significantly lower in NF compared with W and CE during
exercise II (Fig. 4, Table 2). Whereas
local SR of ~50-55
ml · m
2 · min
1
were sustained by the horses in the fluid treatment trials, SR in NF
declined during the last 30 min of exercise
II. This decline in SR (and rate of cutaneous
evaporative heat loss) was temporally related to the exacerbation of
hyperthermia in the NF trial. These observations suggest that, at high
thermal demands, preservation of euhydration is necessary for
maintenance of high SR.
Sweating sensitivity also was significantly lower in NF than in W and CE during exercise II (Fig. 5). These data imply an alteration in sweating control, presumably as a result of the marked dehydration in the NF trial. In human subjects, both threshold temperature for onset of thermoregulatory sweating and sweating sensitivity are altered in a graded manner with hypohydration (29). Both extracellular hyperosmolality (12, 17, 29) and hypovolemia (11) have been implicated as mechanisms for altered sweat sensitivity in the hypohydrated state. In the present study, plasma osmolality increased only in NF and was inversely related to sweating sensitivity in exercise II (P < 0.005; Fig. 6, right). This observation agrees with previous reports in human subjects that have demonstrated an inverse relationship between the extent of plasma hyperosmolality and SR (12, 29, 35). Given the significantly greater PV loss in NF compared with W and CE (Fig. 2), hypovolemia also may have contributed to an alteration in sweating control. However, studies of exercising humans (11, 29, 34) and horses (19) have not demonstrated a consistent relationship between PV and sweating responses.
The altered sweating responses evident in the present study are in
contrast to previous reports in exercising horses in which neither
preexisting hypohydration (~3.5% decrease in TBW) (30) nor
progressive dehydration during prolonged exercise (~6% of body mass)
(19) altered local SR. However, in the study by Kingston et al. (19),
horses were partially rehydrated during the exercise; partial
replacement of body water losses may have mitigated any effect of the
dehydration on thermoregulatory responses. Other factors in the
aforementioned studies that may have contributed to the difference in
sweating responses compared with the present study include a lower
ambient temperature (22-23°C) and a slightly lower rate of
work (40%
O2 max),
which resulted in a slower rate of rise in
Tcore, and associated lower SR.
The lower ambient temperature in the two previous studies would have
reduced dependency on high SR and skin blood flow for heat dissipation;
higher convective heat loss could alter the relationship between
dehydration and hyperthermia. In cooler environmental conditions, in
which there is less dependence on high SR and more potential for
convective heat loss, dehydration may occur without altering the
magnitude of the hyperthermia accrued during exercise.
The greater heat storage in NF could also be attributed to
dehydration-induced alterations in cardiovascular responses. In W and
CE, maintenance of euhydration by fluid administration mitigated the
~10% decrease in
evident in NF during the last 30 min of exercise. Similar to the findings of a previous report
describing cardiovascular responses of hypohydrated horses during
moderate-intensity exercise (30), in the present study the decline in
in NF was attributed to a decrease in SV with
minimal change in HR (Fig. 7,
A-C). Alterations in skin blood
flow and a dehydration-induced decrease in PV may, in part, explain the
reduction in SV (15, 30, 33). Although we had no measures of skin blood
flow or total peripheral (vascular) resistance, it is possible that the decline in
in NF was accompanied by a decrease in
blood flow to the cutaneous circulation. In this circumstance, the
decreases in
and skin blood flow would exacerbate
hyperthermia via a reduction in transfer of heat from core to
periphery. The decreases in
and SV evident in the NF
trial are consistent with data from hypohydrated human subjects during
exercise-heat stress (16, 28, 33). For example, Montain and Coyle (28)
reported that the decline in SV with graded magnitudes of dehydration
during exercise was proportional to the percent body weight loss and the reduction in forearm skin blood flow. Moreover, ingestion of fluid
sufficient to replace 50-80% of the exercise-induced sweat loss
attenuated hyperthermia by maintaining higher skin blood flow compared
with trials in which either no or only a small amount of fluid was
ingested (27, 28).
An interesting feature of the cardiovascular response to exercise-heat
stress in the horses of the present study was the absence of a
progressive increase in HR ("cardiovascular drift"). In human subjects, a progressive decrease in SV during submaximal exercise is
accompanied by a compensatory increase in HR that serves to maintain or
increase
(33). However, superimposition of
dehydration on hyperthermia during exercise-heat stress causes greater
reductions in SV and cardiovascular function, with an eventual decline
in
despite a progressive increase in HR (16). By
comparison, in the W and CE trials, HR,
, and SV were
stable throughout the 90 min of exercise, whereas in NF the decline in
SV during exercise II was not
associated with an increase in HR (Fig. 7, A-C). Previous studies of
horses during prolonged submaximal exercise have also demonstrated
remarkable cardiovascular stability (9, 32), and it is has been
suggested that postural differences between horses (quadripeds) and
humans allow for better maintenance of "central" blood volume and
cardiac filling pressure (9). Nonetheless, the decrease in SV observed
in NF would be expected to invoke a compensatory increase in HR in an
attempt to maintain
. In the absence of data for
other cardiovascular variables, such as central venous and mean
arterial pressures and skin blood flow, we are unable to offer a
suitable explanation for this finding.
This study also compared the efficacy of water and an isotonic electrolyte solution for maintenance of euhydration and reduction of physiological strain during exercise-heat stress. On the basis of measured fluid intake and losses, we observed no difference in hydration between W and CE. Similarly, both fluid treatments were equally effective in mitigating hemoconcentration during exercise (Fig. 1, A and B). In human subjects, there is a strong association between plasma osmolality and thermoregulatory responses (8, 12, 17, 29). However, this relationship has not been demonstrated in the horse (18, 19). In the present study, although there were significant differences in plasma osmolality between the W and CE trials, both before and during exercise, there were no differences between fluid treatments in terms of thermoregulatory or cardiovascular responses. Some (3, 6), but not all (2), studies of human subjects have reported that PV is better maintained with the ingestion of isotonic electrolyte or carbohydrate-electrolyte solutions compared with water during exercise lasting 2-3 h. In the present study, although the CE fluid maintained PV at a higher level than did W during exercise, this difference was significant only at the end of exercise II.
In summary, we observed that 1)
preexercise hyperhydration provided no thermoregulatory advantage
compared with trials in which no fluid was administered;
2) maintenance of euhydration by
oral administration of fluid at a volume equivalent to ~85% of sweat
fluid loss mitigated heat storage, as reflected by lower Tpa,
Tre, and
Tmus at the end of exercise;
3) maintenance of euhydration prevented decrements in local SR, sweating sensitivity,
, and SV associated with progressive dehydration
during exercise; and 4) oral
administration of W or an isotonic CE solution was equally effective in
reducing physiological strain associated with exercise-induced dehydration and heat stress.
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ACKNOWLEDGEMENTS |
|---|
The authors thank Jessie Hare, Karen Gowdy, James Byrne, Lisa Curle, Terrie Leslie, and Hua Shen for technical assistance.
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FOOTNOTES |
|---|
This work was supported by Davis and Lawrence Co. (Cambridge, ON); the Natural Sciences and Engineering Research Council of Canada; and the Equine Research Program of the Ontario Ministry of Agriculture, Food and Rural Affairs.
Address for reprint requests: R. J. Geor, Dept. of Veterinary Clinical Sciences, College of Veterinary Medicine, The Ohio State Univ., 610 Vernon L. Tharp St., Columbus, OH 43210 (E-mail: geor.1{at}osu.edu).
Received 24 November 1997; accepted in final form 4 February 1998.
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