Physical activity and heat stress shape water needs in pregnant endurance athletes
Srishti Sadhir, Amanda McGrosky, Zane S Swanson, Anna Tavormina, Keri Tomechko, Herman Pontzer

TL;DR
Pregnant endurance athletes have higher water needs due to physical activity and heat stress, which could impact policy for vulnerable populations.
Contribution
This study quantifies how physical activity and heat stress interact to influence water turnover in pregnant athletes.
Findings
Athletes had consistently high water turnover from preconception through pregnancy.
Physical activity was positively linked to water turnover in early pregnancy but not in the third trimester.
Higher heat index conditions slightly strengthened the relationship between physical activity and water turnover.
Abstract
Pregnancy, heat stress, and physical activity (PA) are all known to independently increase human water requirements. We hypothesize that climate conditions and behavioral strategies interact to shape water needs in highly active pregnancies. We recruited 20 female endurance runners who were pregnant (8–16 weeks gestational age; n = 13) or planning to be pregnant (n = 7) for an observational, prospective cohort study. At three timepoints in the study (preconception, 8–16 weeks, and 32–35 weeks), we measured water turnover (WT) using the deuterium dilution and elimination technique, PA using ActiGraph wGT3X-BT accelerometers, and heat index (HI) using historical temperature and humidity data. We also compared athletes to nonathletes from a previously published study. Athletes maintained high WT from preconception through the end of pregnancy. PA was positively associated with WT among…
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Figure 1
Figure 2| Variables at enrollment | Athletes ( | Nonathletes ( |
|---|---|---|
| Age (years) | 32.1 ± 1.9 | 30.3 ± 4.3 |
| Preconception body mass (kg) | 59.0 ± 8.2 | 59.3 ± 6.0 |
| Preconception BMI (kg/m2) | 21.6 ± 2.4 | – |
| Total gestational weight gain (kg) | 12.7 ± 3.9 | 14.5 ± 4.5 |
| Variable | Group | Preconception | Early pregnancy (8–16 weeks) | Third trimester (32–25 weeks) | ANOVA | ||||
|---|---|---|---|---|---|---|---|---|---|
|
| Sum Sq | Mean Sq |
|
| |||||
| TBW (kg) | Athletes ( | 35.27 ± 3.89 | 33.52 ± 3.68 | 38.08 ± 3.97 | 2 | 199.6 | 99.78 | 6.75 | .003 |
| Nonathletes (n = 34) | 31.68 ± 3.90 | 33.97 ± 3.81 | 38.70 ± 4.05 | ||||||
| Mean daily WT (l/day) | Athletes ( | 5.26 ± 1.41 | 4.51 ± 1.21 | 4.40 ± 0.98 | 2 | 3.96 | 1.98 | 1.51 | .23 |
| Nonathletes (n = 34) | 3.59 ± 0.43 | 3.78 ± 0.42 | 4.39 ± 0.45 | – | – | – | – | – | |
| One-week running distance (km) | Athletes ( | 48.3 ± 17.6 | 44.4 ± 19.5 | 16.7 ± 22.8 | 2 | 8036 | 4018 | 9.01 | .0006 |
| One-week MVPA in 10-min bouts (min) | Athletes ( | 461.6 ± 164 | 410.2 ± 163.8 | 402.4 ± 380.0 | 2 | 108 844 | 54 422 | 1.61 | .21 |
| One-week mean daily step count | Athletes ( | 14 075 ± 3795 | 11 562 ± 3155 | 9226 ± 3962 | 2 | 134 480 574 | 67 240 287 | 5.10 | .01 |
| Mean daytime HI (°F) | Athletes ( | 58.6 ± 26.5 | 64.6 ± 18.6 | 64.8 ± 16.8 | 2 | 15 442 | 109.7 | 0.30 | .74 |
| WT ~ HI + MVPA + HI*MVPA + BMI + gestational age | WT ~ HI + step count + HI*step count + BMI + gestational age | ||||
|---|---|---|---|---|---|
| Covariate | β Coefficient (SE) |
| Covariate | β Coefficient (SE) |
|
| (intercept) | 3.28 (1.84) | .08 | (intercept) | 3.36 (1.97) | .08 |
| HI | −0.021 (0.015) | .16 | HI | −0.025 (0.018) | .18 |
| MVPA | −0.0026 (0.0024) | .30 | Step count | −0.000046 (0.00010) | .65 |
| BMI | 0.089 (0.075) | .23 | BMI | 0.061 (0.071) | .86 |
| Gestational age | −0.0090 (0.011) | .41 | Gestational age | −0.0023 (0.016) | .99 |
| HI*MVPA | 0.000067 | .05 | HI*step count | 0.0000026 (0.0000015) | .10 |
| Total Sum of Squares | 13.39 | Total Sum of Squares | 14.90 | ||
| Residual Sum of Squares | 13.60 | Residual Sum of Squares | 13.96 | ||
| R-Squared | 0.09 | R-Squared | 0.12 | ||
- —National Science Foundation10.13039/100000001
- —Leakey Foundation10.13039/100005966
- —Triangle Center for Evolutionary Medicine10.13039/100014264
- —Wenner-Gren Foundation10.13039/100001388
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Taxonomy
TopicsMuscle metabolism and nutrition · Thermoregulation and physiological responses · Adipose Tissue and Metabolism
INTRODUCTION
Water needs and water turnover (WT; L/day) increase during pregnancy in step with increased daily energy expenditure and total body water (TBW; kg) to accommodate the growing fetus [1, 2]. In nonpregnant cohorts, high physical activity (PA) and high ambient temperature also increase water needs through water loss via sweating for evaporative cooling [1, 3–5]. In this paper, we consider how pregnancy, PA, and weather conditions interact to shape water needs. We examine changes to WT in pregnant athletes who train during pregnancy under varied environmental conditions. Water needs are often estimated in pregnant populations [6] but this study employs the gold-standard deuterium dilution method to measure TBW and WT.
Water intake requirements
The National Academy of Medicine recommends daily water intake as: 3.7 l/day for males; 2.7 l/day for nonpregnant, nonlactating females; 3.0 l/day for pregnant females; and 3.8 l/day for lactating females [7]. In 458 American adults, measured WT was 3.0 l/day for males and 2.5 l/day for females [8], similar to self-reported NHANES water intake data [5]. In a global sample of 5604 adults, WT was higher: 4.3 l/day for males and 3.4 l/day for females [1]. Globally, water intake varies widely, from 1 to 10 l/day, which, in addition to age, sex, and body mass, reflects differences in environment and behavior [1, 3–5].
In pregnancy, TBW expands by 7–8 l, making up nearly 61% of total gestational weight gain (GWG), due to the modified effects of the renin-angiotensin-aldosterone and atrial natriuretic peptide pathways [2, 9]. Notably, TBW accretion, through blood plasma volume expansion, is positively correlated with neonatal birth weight and outcomes [2, 9]. Greater fluid intake is also positively associated with amniotic fluid index, which affects fetal outcomes [10]. From a clinical perspective, ensuring that water intake requirements are met during pregnancy reduces the risk of adverse outcomes in expecting mothers [2, 9, 11–16].
Maintaining water balance in pregnancy
With various physiological and environmental challenges faced by mother and fetus, pregnancy acts as a strong selective force in determining initial survival and long-term health over the life course [17]. Due to increased water needs paired with high rates of water excretion [2], pregnant females are at greater risk of dehydration, which can negatively impact maternal and fetal health [2, 11, 14, 16, 18]. Previous research has shown total fluid intake (i.e. WT rate) increases to mitigate dehydration in pregnancy, as measured by urinary biomarkers of hydration [19]. Water needs also increase with PA [1, 3, 4, 20], and endurance athletes routinely experience acute dehydration during competitions [20, 21]. It is unknown how water intake requirements change during highly active pregnancies, especially in chronically hot environmental conditions [11]. These variables likely interacted in the human evolutionary past as pregnant females undertook active, subsistence-based lifestyles in variable environments.
In pregnant Gambian farmers, frequent heat exposure during agricultural tasks was associated with increased maternal heat exhaustion symptoms and increased maternal and fetal heat strain [15]. Participants reported behavioral changes to mitigate heat stress when possible [22]. Indeed, Yamada et al. found a smaller effect of outdoor temperature on WT in industrialized populations that are buffered by indoor climate control.
Climate change poses a particular threat to pregnancies in populations without adequate indoor climate control. Globally, 1.8–4.1 billion people lack indoor cooling solutions, many of whom undertake physically demanding occupations, even in pregnancy [23]. Current pregnancy guidelines support ≥ 150 min per week of moderate-intensity PA in mild-moderate temperatures and avoidance of high heat/humidity exposure during exercise [24–26]. However, these guidelines lack consistency, are not fully evidence-based, and are not specific about exposure time, gestational age, temperature ranges, heat acclimatization, and PA types. It is imperative to understand how both PA and environmental conditions affect water needs in pregnancy to mitigate health risks [11, 13].
Hypothesis and predictions
We hypothesize that weather conditions and behavioral strategies interact to shape water needs in pregnant athletes:
Prediction 1: Mean daily WT is greater in athletes compared to relatively sedentary nonathletes. Prediction 2: Moderate-to-vigorous PA (MVPA) and mean daily step count are independently and positively associated with WT in the preconception period and across pregnancy. The slope of this association is expected to be greater with a higher heat index (HI). Prediction 3: Irrespective of PA, there is a positive association between daytime HI and WT in the preconception period and across pregnancy.
To test these predictions, we investigated behavioral and physiological changes over pregnancy in endurance athletes living in diverse climatic regions. We also compare water needs between athlete and nonathlete pregnancies [27].
METHODOLOGY
Participant recruitment and study design
Female participants who were either pregnant (<16 weeks gestational age) or planning a pregnancy were recruited for an observational, prospective cohort study. We recruited participants aged 18–35 years with preconception BMI 18.5–26.0 kg/m^2^ who resided in the USA or Canada and who did not use medications that alter metabolism. Participants were required to self-report at least 300 min/week MVPA prior to conception, inclusive of >32 km/week of running and training at Tier 2: at least 3 times/week with the purpose of competing at the local level or above [28]. This research was approved by the Institutional Review Board of Duke University (Pro00108341). All participants provided informed consent upon recruitment. All study activities were conducted remotely for nationwide recruitment and study compliance with COVID-19 restrictions.
Deuterium dilution and elimination method
We measured TBW (kg) and WT (L/day) 2–3 times (preconception, if applicable; 8–16 weeks; 32–35 weeks) using the deuterium dilution and elimination technique [29]. This method enriches the participant’s body water pool in deuterium (D), a stable, naturally occurring isotope of hydrogen. The rate of deuterium depletion was measured over a 7-day period from isotopic enrichments in the 3 postdose urine samples using the slope-intercept method. Details on this method are found in Supplementary Materials.
PA variables
Participants continuously wore a hip-worn ActiGraph wGT3X-BT accelerometer (Actigraph, LLC) during each deuterium dilution week, including during sleep. This triaxial device measures displacement and acceleration at a 30 Hz sampling rate to quantify movement [30, 31]. Participants self-reported when they placed and removed the device. Files were downloaded from the ActiLife 6 software (Version 6.13.5, ActiGraph, LLC). Data processing took place in R [32] using GGIR (version 3.0.9) and PhysicalActivity (version 0.2.4) packages [33, 34]. Wear-time validation and data processing details can be found in Supplementary Materials. The PA outcomes were daily step counts over 7 days from the PhysicalActivity package and mean MVPA in 10-minute bouts over 7 days from the GGIR package.
Comparative nonathlete data
We extracted TBW and WT data from a comparative study of energy requirements during pregnancy in nonathlete participants of normal BMI (19.8–26.0 kg/m^2^; n = 34) from Butte et al. [27]. For recruitment, participants self-reported “moderate activity,” defined as 20–30 min of moderate exercise at least three times per week [27]. Gestational age of 0 weeks was assigned as “preconception,” 22 weeks as “early pregnancy,” and 36 weeks as “third trimester” to allow for comparison with the athlete participants. Slopes of deuterium depletion (kD) and the dilution spaces of hydrogen (NH; kg) and oxygen (NO; kg) were extracted from Table 4 in Butte et al. [27] and used to calculate TBW and WT (Supplementary Materials).
HI variable
Historical weather data was downloaded from The National Weather Service (www.wunderground.com/) based on participant zip codes. We collected daily weather metrics for the 7 days spanning the deuterium dilution week. For temperatures greater than or equal to 80°F, HI was calculated with the Rothfusz equation [35]. For temperatures below 80°F, HI was calculated with the simplified Rothfusz equation (Supplementary Materials). To ensure we captured daytime HI, we averaged HI values per day between 6:00 and 18:00 and then averaged all daily values across the 7-day deuterium dilution period.
Statistical analysis
All data manipulation and analyses were conducted in R [32] (Supplementary Materials). We used one-way ANOVA tests and Bonferroni post hoc tests to assess potential changes in mean PA and WT between time periods.
We used random-effects linear panel regression to test for the independent effects of HI and PA on WT, as well as an interaction effect of HI*PA on WT. Gestational age and BMI were included as covariates. Models were indexed by subject and time period:
We used multiple linear regression to test for the independent effects of HI and PA on WT within each time period:
We compared TBW and WT results between the athletes and nonathletes using a one-way repeated measures ANOVA test (Type III), as well as an ANCOVA test (Type III) to include body mass and gestational age as covariates. To assess differences in WT between athletes and nonathletes at each time period, we employed a Bonferroni post hoc test.
RESULTS
Demographic summary and descriptive statistics
A total of 20 athlete participants were included in this study. Demographic and anthropometric variables are listed in Table 1 and Supplementary Table S1. At enrollment, participants had a mean age of 32.1 ± 1.9 years. Seven participants began data collection in the preconception period, while 13 participants began data collection in early pregnancy at a mean gestational age of 15.2 ± 5.4 weeks. Participants remained in the study for 10.8 ± 3.4 months. Total GWG was 12.7 ± 3.9 kg. Mean daily WT did not differ between time periods (F = 1.51, P = .23) (Fig. 1; Table 2). Mean TBW increased over gestation (F = 6.75, p = 0.003) (Table 2).
Combined violin-boxplots demonstrate no significant difference in WT across preconception, early pregnancy, and third trimester time periods in athletes (n = 20). Mean WT from nonathletes (n = 34) across the three-time points are represented by diamonds. Results from one-way ANOVA investigating WT differences between study (athletes vs. nonathletes) indicate no significant difference: df = 1, Sum Sq = 4.12, Mean Sq = 4.12, F = 3.38, P = .07.
Data on PA are summarized in Table 2. There were 315 days of accelerometry with a 92.7% adherence, yielding 292 wear days with an average of 6.5 days per participant per measurement period. For participants recruited in the preconception period (n = 7), step count was 14 075 ± 3795 steps/day, and MVPA was 461.6 ± 164.5 min/week. Preconception running distance was 48.3 ± 17.6 km/week. Weekly running distance decreased from early pregnancy (44.4 ± 19.5 km/week) to the third trimester (16.7 ± 22.8 km/week) (F = 9.01, P = .0006), with 11 participants stopping their running activities altogether by the third trimester. Participants maintained MVPA (461.6 ± 164.5 min/week in preconception, 410.2 ± 163.8 min/week in early pregnancy, and 402.4 ± 380.0 min/week in the third trimester) (F = 1.61, P = .21), though the range and variability in MVPA were greater during the third trimester (SD: 163.8 vs. 380.0 min/week). Participants reported more low-impact endurance activities as alternatives to running in late pregnancy to mitigate pain, soreness, and changes to gait and pacing. Alternative activities included swimming, cycling, and brisk walking. Daily step count was reduced from preconception (14 075 ± 3795 steps/day) to the third trimester (9226 ± 3962 steps/day) (F = 5.10, P = .01).
Linear panel regression analysis of the effects of PA, HI, and PA*HI on WT
There was no relationship between MVPA and WT (β = −0.0026, P = .30), nor between HI and WT (β = −0.021, P = .16) (Table 3). There was a positive, nonsignificant trend in the interaction effect of MVPAHI on WT (β = 0.000067, P = .05). For the step count outcome, there was no relationship between daily step count and WT (β = −0.000046, P = .65), nor between HI and WT (β = −0.025, P = .18) (Table 3). There was no relationship in the interaction effect of step countHI on WT (β = 0.0000026, P = .10). By visualizing the postestimation plots of the panel regression models (Supplementary Fig. S1), we found possible evidence of a more positive relationship (slope) between MVPA and WT, as well as step count and WT, as HI increased.
Multiple linear regression analysis of the independent effects of MVPA and HI on WT during each time period
In the preconception period, there was no relationship between MVPA and WT (β = 0.052, P = .54), nor between HI and WT (β = 0.017, P = .81) (Fig. 2a and c; Supplementary Table S8). In early pregnancy, there was a significant, positive relationship between MVPA and WT (β = 0.0043, P = .02), where there was a 0.13 l increase in daily WT with every 30-min weekly increase in MVPA (Fig. 2a; Supplementary Table S9). There was no relationship between HI and WT (β = 0.016, P = .27) (Fig. 2c; Supplementary Table S9). In the third trimester, there was no relationship between MVPA and WT (β = 0.001, P = .38), nor between HI and WT (β = −0.018, P = .14) (Fig. 2a and c; Supplementary Table S10).
Relationship between environmental factors and WT in athletes. (a) MVPA in 10-minute bouts positively predicts WT in early pregnancy only. (b) Step count positive predicts WT in preconception and early pregnancy only. (c) There is no relationship between mean daytime HI and WT at any time period during preconception and pregnancy.
Multiple linear regression analysis of the independent effects of step count and HI on WT during each time period
In the preconception period, there was a significant, positive relationship between step count and WT (β = 0.00034, P = .02), where there was a 0.34 l increase in daily WT with each 1000-step daily increase (Fig. 2b; Supplementary Table S8). There was no relationship between HI and WT (β = 0.019, P = .20) (Fig. 2c; Supplementary Table S8). In early pregnancy, there was a significant, positive relationship between step count and WT (β = 0.00025, P = .004), where there was a 0.25 L increase in daily WT with every 1,000-step daily increase (Fig. 2b; Supplementary Table S9). There was a positive, nonsignificant trend between HI and WT (β = 0.023, P = .07) (Fig. 2c; Supplementary Table S9). In the third trimester, there was no relationship between step count and WT (β=0.00005, p = 0.43), nor between HI and WT (β = −0.019, P = .13) (Fig. 2b and c; Supplementary Table S10).
Comparative analysis between athletes and nonathletes
Mean TBW for nonathletes was 31.68 ± 3.90 kg in preconception, 33.97 ± 3.81 kg in early pregnancy, and 38.70 ± 4.05 kg in the third trimester (Table 2). Mean WT for nonathletes was 3.59 ± 0.43 l/day in preconception, 3.78 ± 0.42 l/day in early pregnancy, and 4.39 ± 0.45 l/day in the third trimester (Table 2).
Athletes did not have greater TBW than nonathletes (F = 2.87, P = .09). However, when accounting for body mass and gestational age, group was a significant predictor of TBW (F = 6.81, P = .01) (Supplementary Table S11). Body mass (F = 239.11, P < .0001) and gestational age (F = 141.61, P < .0001) were significant predictors of TBW, with greater effects than group designation (Supplementary Table S11). TBW was only greater in athletes compared to nonathletes in preconception (P < .0001) (Supplementary Table S12). There was no difference in TBW between groups in early pregnancy (P = .48) and in the third trimester (P = .36) (Supplementary Table S12).
Athletes had greater daily WT overall compared to nonathletes (F = 27.29, P < .0001) (Supplementary Table S13). When accounting for body mass and gestational age, group was still a significant predictor of WT (F = 17.54, P < .0001) (Supplementary Table S13). Body mass (F = 3.66, P = .06) and gestational age (F = 3.35, P = .07) were marginal predictors of WT (Supplementary Table S13). The difference in WT between athletes and nonathletes was driven by preconception (P < .0001) and early pregnancy (P < .0001) time periods (Supplementary Table S14). There was no difference in WT between groups in the third trimester (P = .99) (Supplementary Table S14).
DISCUSSION
Our results somewhat support the hypothesis that weather conditions and behavioral strategies interact to shape water needs in pregnant athletes. While athletes did not reduce MVPA from preconception to the third trimester, daily step count was significantly reduced. Step count includes habitual activities throughout the 24-h cycle, whereas MVPA may represent more intentional PA bouts in this population [36–38]. Athletes accommodated MVPA by reducing nonintentional PA throughout the day, or by moving to lower-impact, lower-intensity activities. In doing so, WT did not increase throughout pregnancy. Since HI did not predict WT, athletes may have moved indoors, shifted activity patterns to different times of the day, or moved to more amenable locations for PA to reduce sweating and water intake needs. Despite the role of behavioral modification, we were able to detect a slight positive interaction effect of PA and HI on water requirements across gestation.
Expansion of TBW occurred similarly in both athlete and non-athlete pregnancies, given similar body sizes between groups, so WT rate is the primary physiological strategy to deal with water stress. Athletes in preconception had a higher WT (5.26 l/day) than nonathlete participants (3.59 l/day), a global sample of nonpregnant females (3.4 l/day), and an American sample of nonpregnant females (2.5 l/day), reflecting the additional water needs with high PA [1, 8]. Both the athlete (4.40 l/day) and nonathlete (4.39 l/day) cohorts had higher WT in the third trimester compared to the global and American samples [1, 8], reflecting the additional water needs associated with pregnancy.
We are unsure of PA differences between the athletes and nonathletes, since accelerometry was not routinely employed in studies until the 2010s [39]. However, studies of pregnancy in other nonathlete cohorts report low MVPA, particularly in the third trimester [40–46]. A PA recruitment criterion was included for the non-athlete comparative sample, which was lower than athlete recruitment (Methodology). Given the prevalence of overreporting bias in survey-based PA measurements [47], preconception PA in the nonathlete sample was likely lower than the athlete sample in this study.
Pregnant people across the world face multiple stressors to water balance, including lack of indoor climate control; exposure to hot, water-scarce, and nonpotable water environments; and high workloads [15, 23]. While pregnant people are told to avoid high heat and humidity during PA, not enough data exists to establish thresholds [24–26]. Our results suggest that the current water intake guidelines that exist are too low for highly active pregnant populations experiencing high heat stress. With the threat of climate change expected to exacerbate extreme heat conditions, evidence-based policies are required to protect particularly vulnerable populations.
When comparing humans with other apes, Pontzer and colleagues [48] found that humans have evolved better water conservation strategies, despite having a higher sweating capacity through high eccrine gland density [49, 50]. These strategies may include the development of external noses for water recovery [48] and lower hair density to reduce sweating [49, 50]. It is also unknown how water requirements differ in pregnancy between ape species, since interspecies TBW expansion, urine concentrating abilities, and other pregnancy traits may be variable. In addition, social buffering of water stress may be more prevalent in humans, as interdependence within social groups (e.g. cooperative breeding) may better allow pregnant individuals to seek amenable environmental conditions and reduce PA [51]. Conversely, females of other ape species often undertake pregnancy without assistance from group members [51].
Limitations
We were unable to account for specific microclimates experienced by athletes. Indoor heat stress is an important driver of global heat-related morbidity and mortality [52]. Athletes were likely buffered by indoor climate control, which has been found in other higher-income populations [1]. As a result of higher-income status, this population may experience better economic/social buffering to accommodate PA during pregnancy, even in climates with high heat stress, without suffering negative health outcomes. Thus, athletes in this study are not representative of global climate experience across all pregnant populations.
This study relied on PA measured by accelerometry, which tracks acceleration-based activities. For this reason, we restricted recruitment of athletes who predominantly undertake other modes of exercise, like weight training. It is likely that we did not capture stationary activities through accelerometry, which still contribute to overall water needs.
CONCLUSION
We report on water requirements for pregnant endurance athletes, which were higher than nonathletes but attenuated in the third trimester. PA was positively associated with WT among athletes for preconception and early pregnancy but not for the third trimester. HI weakly predicted a more positive slope in hotter, more humid weather conditions. Yet, pregnant athletes overall had good control of their environment to mitigate the risk of extreme dehydration, with no adverse outcomes reported [2, 14, 16]. Adverse pregnancy outcomes are expected to increase with climate change. To better understand dynamic water needs, a greater diversity of human populations and nonhuman primate species is required for study.
Supplementary Material
eoaf003_suppl_Supplementary_Figure_S1
eoaf003_suppl_Supplementary_Material
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