scholarly journals Contribution of Dietary Composition on Water Turnover Rates in Active and Sedentary Men

Nutrients ◽  
2021 ◽  
Vol 13 (6) ◽  
pp. 2124
Author(s):  
Alice E. Disher ◽  
Kelly L. Stewart ◽  
Aaron J. E. Bach ◽  
Ian B. Stewart

Body water turnover is a marker of hydration status for measuring total fluid gains and losses over a 24-h period. It can be particularly useful in predicting (and hence, managing) fluid loss in individuals to prevent potential physical, physiological and cognitive declines associated with hypohydration. There is currently limited research investigating the interrelationship of fluid balance, dietary intake and activity level when considering body water turnover. Therefore, this study investigates whether dietary composition and energy expenditure influences body water turnover. In our methodology, thirty-eight males (19 sedentary and 19 physically active) had their total body water and water turnover measured via the isotopic tracer deuterium oxide. Simultaneous tracking of dietary intake (food and fluid) is carried out via dietary recall, and energy expenditure is estimated via accelerometery. Our results show that active participants display a higher energy expenditure, water intake, carbohydrate intake and fibre intake; however, there is no difference in sodium or alcohol intake between the two groups. Relative water turnover in the active group is significantly greater than the sedentary group (Mean Difference (MD) [95% CI] = 17.55 g·kg−1·day−1 [10.90, 24.19]; p = < 0.001; g[95% CI] = 1.70 [0.98, 2.48]). A penalised linear regression provides evidence that the fibre intake (p = 0.033), water intake (p = 0.008), and activity level (p = 0.063) predict participants’ relative body water turnover (R2= 0.585). In conclusion, water turnover is faster in individuals undertaking regular exercise than in their sedentary counterparts, and is, in part, explained by the intake of water from fluid and high-moisture content foods. The nutrient analysis of the participant diets indicates that increased dietary fibre intake is also positively associated with water turnover rates. The water loss between groups also contributes to the differences observed in water turnover; this is partly related to differences in sweat output during increased energy expenditure from physical activity.

2005 ◽  
Vol 93 (2) ◽  
pp. 199-203 ◽  
Author(s):  
Klaas R. Westerterp ◽  
Guy Plasqui ◽  
Annelies H. C. Goris

Although water is an important nutrient, there are no recommended intake values. Here, water intake, energy intake, physical activity and water loss was measured over 1 week in summer and in winter. Subjects were healthy volunteers, forty-two women and ten men, mean age of 29 (sd 7) years and mean BMI 21·8 (sd 2·2) kg/m2. Water intake was measured with a 7 d food and water record. Physical activity level (PAL) was observed as the ratio of total energy expenditure, as measured with doubly labelled water, to resting energy expenditure as measured in a respiration chamber. Water loss was measured with the deuterium elimination method. Water loss was highly reproducible and ranged from 0·20 to 0·35 l/MJ, independent of season and activity level, with higher values in women. Water loss was related to water and energy intake in summer (r 0·96, P<0·0001 and r 0·68, P<0·001, respectively) as well as in winter (r 0·98, P<0·0001 and r 0·63, P<0·01, respectively). Water loss was, for men, higher in subjects with a higher physical activity in summer (r 0·94, P<0·0001) and in winter (r 0·70, P<0·05). Normalizing water loss for differences in energy expenditure by expressing water loss in litres per MJ resulted in the same value for men in summer and winter. For women, physical activity-adjusted values of water loss were higher, especially in summer. In men, water turnover was determined by energy intake and physical activity, while seasonal effects appeared through energy expenditure. Women showed a higher water turnover that was unrelated to physical activity.


The Condor ◽  
1982 ◽  
Vol 84 (3) ◽  
pp. 332 ◽  
Author(s):  
Philip U. Alkon ◽  
Berry Pinshow ◽  
A. Allan Degen

Nutrients ◽  
2019 ◽  
Vol 11 (3) ◽  
pp. 565 ◽  
Author(s):  
Ana Isabel Laja García ◽  
Maria de Lourdes Samaniego-Vaesken ◽  
Teresa Partearroyo ◽  
Gregorio Varela-Moreiras

The achievement of adequate hydration status is essential for mental and physical performance and for health in general, especially in children and adolescents. Nevertheless, little is known about hydration status of this population, mainly due to the limited availability of research tools; thus, the objective of the current study was to adapt and validate our hydration status questionnaire in a Spanish adolescent-young population. The questionnaire was validated against important hydration markers: urine colour, urine specific gravity, haemoglobin, haematocrit and total body water and involved 128 subjects aged between 12–17 years. Water intake was also estimated through a three-day dietary record and physical activity was assessed through accelerometers. Participants completed the questionnaire twice. Water balance and water intake were correlated with urine specific gravity and with total body water content. Water intake obtained by the questionnaire was correlated with results from the three-day dietary record. The intraclass correlation coefficient indicated moderate concordance between both recordings and the Cronbach’s alpha revealed high consistency. The Bland and Altman method indicated that the limits of agreement were acceptable to reveal the reliability of the estimated measures. In conclusion, this is the first time that a questionnaire is valid and reliable to estimate hydration status of adolescent-young populations.


2004 ◽  
Vol 286 (2) ◽  
pp. F394-F401 ◽  
Author(s):  
Aarthi Raman ◽  
Dale A. Schoeller ◽  
Amy F. Subar ◽  
Richard P. Troiano ◽  
Arthur Schatzkin ◽  
...  

Despite recent interest in water intake, few data are available on water metabolism in adults. To determine the average and range of usual water intake, urine output, and total body water, we administered 2H oxide to 458 noninstitutionalized 40- to 79-yr-old adults living in temperate climates. Urine was collected in a subset of individuals ( n = 280) to measure 24-h urine production using p-aminobenzoic acid to ensure complete collection. Preformed water intake was calculated from isotopic turnover and corrected for metabolic water and insensible water absorption from humidity. Preformed water intake, which is water from beverages and food moisture, averaged 3.0 l/day in men (range: 1.4-7.7 l/day) and 2.5 l/day in women (range: 1.2-4.6 l/day). Preformed water intake was lower in 70- to 79 (2.8 l/day)- than in 40- to 49-yr-old men and was lower in 70- to 79 (2.3 l/day)- than in 40- to 49- and 50- to 59-yr-old women. Urine production averaged 2.2 l/day in men (range: 0.6-4.9 l/day) and 2.2 l/day in women (0.9-6.0 l/day). There were no age-related differences in results in women, but 60- to 69-yr-old men had significantly higher urine output than 40- to 49- and 50- to 59-yr-old men. Only the 70- to 79-yr-old group included sufficient blacks for a racial analysis. Blacks in this age group showed significantly lower preformed water intake than did whites. Whites had significantly higher water turnover rates than blacks as well. Multivariate regression indicated that age, weight, height, and body mass index explained <12% of the gender-specific variance in water input or urine output, yet repeat measures indicated that within-individual coefficient of variation was 8% for preformed water intake ( n = 22) and 9% for 24-h urine production ( n = 222). These results demonstrate that water turnover is highly variable among individuals and that little of the variance is explained by anthropometric parameters.


1968 ◽  
Vol 19 (1) ◽  
pp. 129
Author(s):  
PH Springell

Twenty-four steers, comprising British (Hereford and Hereford x Shorthorn), Zebu (Africander), and Zebu cross (British x Brahman or Africander) breeds, were either maintained on pasture, or yarded and fed on diets of a low and a high nutritional value. Tritiated water was injected into the animals on five occasions at intervals of 3 months. The body water content and the water turnover rate were calculated, and some of the sources of variation defined. Observed differences in the water content are attributable to nutritional factors rather than to breed differences. The mean body water content ranged from 615 to 809 ml/kg fasting body weight, where the higher values were associated with a poor diet. The mean half-life of tritiated water was lower in summer (as low as 58 hr) than in winter (up to 128 hr) in grazing and well-fed yarded steers. On a poor diet, however, the half-life in yarded cattle remained high and almost constant throughout the year, dropping to below 100 hr on only a single occasion. Occasionally the half-life was breed dependent, but generally no significant differences between breeds could be found. While mean turnover rates of up to 7.1 ml kg-1 hr-1 were found in better-fed cattle in summer, the value in poorly fed animals was almost constant throughout the year at about 3.3 ml kg-1 hr-1. There was, however, a winter minimum in the well-fed yarded and grazing groups. The turnover rate was also influenced by breed only to a limited extent. The results are interpreted in the light of their possible significance in the adaptation to a tropical environment, and in relation to their value in predicting the body composition.


1971 ◽  
Vol 22 (2) ◽  
pp. 291 ◽  
Author(s):  
NG Yates ◽  
WV Macfarlane ◽  
R Ellis

The growth of Hereford, Friesian x Hereford, and Friesian x Shorthorn calves was studied under grazing conditions in the south-east of South Australia during the autumn period of minimal dry pasture. Measurements of body water content, water turnover, and body weight changes of calves were undertaken during an 8-week period after calving in February 1968. From these measurements, estimates were made of liveweight gain and the yield of body solids per unit of water turnover (milk intake). The subsequent development of the calves was also measured. The average birth weights of the three groups were not significantly different. The 8-week total of water intake (milk) was 405 � 14.3 1. in Shorthorn cross calves, 279 � 18.0 1. for Hereford cross, and 263 � 14.3 1. among the Herefords. Over the first 8 weeks body weight gain (g/24 hr) was highest in the Shorthorn cross calves and their body solids gain was 63 % greater than that of the Hereford cross calves but only 29 % greater than that of the Hereford calves. Water turnover (1.124 hr) of the Shorthorn cross calves was 45 % greater than that of the Hereford cross calves and 54% greater than that of the Hereford calves over the 8-week period. There was no significant difference between the three groups in body weight or solids gain per unit of milk intake (g/l), though the average conversion of milk to solids by Herefords was greater than that of the other breeds. The Shorthorn cows weighed less than the other groups after calving and their average relative and absolute loss of weight during lactation was greatest. The offspring of the Shorthorn cows had the highest water intake expressed as a function of the body weight0.75 of the cows. The water turnover of Shorthorn calves as a function of calf weight0.82 was also greater than that of the other calves. The correlations between body weight gain (g/24 hr) and water turnover (l./24 hr) and between body solids gain (g/24 hr) and water turnover (l./24 hr) were 0.815 (P < 0.001) and 0.632 (P < 0.01) respectively. The correlation between cow body weight loss and calf body weight gain was 0.481 (P < 0.05). A group of nine Friesian x Hereford calves studied for 11 weeks after calving in April 1969 on newly grown winter rainfall pasture 50 km north of Adelaide had both average water turnover (l./24 hr) and body weight gains (g/24 hr) substantially higher than those of any group in the previous year. The efficiency of conversion estimated as body solids gain and body weight gain per unit of water intake was, however, similar to those of the Hereford calves in 1968. The differences between the years are presumed to follow from differences in the amount of pasture available in the dry season, relative to pasture after the rains had come. Average body water content (TOH space) was 801 ml/kg body weight at the beginning of the measurements and gradually fell to 713 ml/kg at 11 weeks.


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