Skip to main content Accessibility help

Water balance throughout the adult life span in a German population

Published online by Cambridge University Press:  16 September 2011

Friedrich Manz
Research Institute of Child Nutrition, Rheinische Friedrich-Wilhelms University Bonn, Heinstueck 11, D-44225Dortmund, Germany
Simone A. Johner
Research Institute of Child Nutrition, Rheinische Friedrich-Wilhelms University Bonn, Heinstueck 11, D-44225Dortmund, Germany
Andreas Wentz
Hospital Düren, Paediatric Clinic, Roonstrasse 30, D-52351Düren, Germany
Heiner Boeing
German Institute of Human Nutrition (DifE), Potsdam-Rehbrücke, Arthur-Scheunert-Allee 114-116, D-14558Nuthetal, Germany
Thomas Remer
Research Institute of Child Nutrition, Rheinische Friedrich-Wilhelms University Bonn, Heinstueck 11, D-44225Dortmund, Germany
E-mail address:
Rights & Permissions[Opens in a new window]


Mild dehydration, defined as a 1–2 % loss in body mass caused by fluid deficit, is associated with risks of functional impairments and chronic diseases. Whether water requirements change with increasing age remains unclear. Therefore, the aim of the present investigation is to quantify hydration status and its complex determining factors from young to old adulthood to analyse age-related alterations and to provide a reliable database for the derivation of dietary recommendations. Urine samples collected over a 24 h period and dietary records from 1528 German adults (18–88 years; sub-sample of the first National Food Consumption Survey) were used to calculate water intake (beverages, food and metabolic water) and water excretion parameters (non-renal water losses (NRWL), urine volume, obligatory urine volume) and to estimate hydration status (free-water-reserve) and ‘adequate intake (AI)’. Median total water intake (2483 and 2054 ml/d, for men and women, respectively (P < 0·0001)), decreased with increasing age only in males (P = 0·001). Obligatory urine volume increased in both sexes (P < 0·0001) due to decreased renal concentration capacity. The latter was balanced by a decrease of NRWL (P < 0·05), leaving the free-water-reserve and therefore hydration status almost unchanged. Calculated ‘AI’ of total water was the same for young (18–24 years) and elderly ( ≥ 65 years) adults (2910 and 2265 ml/d, for men and women, respectively). The present study is the first population-based examination showing that total water requirements do not change with age although ageing affects several parameters of water metabolism. Reduced sweat loss with increasing age appears to be primarily responsible for this observation.

Full Papers
Copyright © The Authors 2011

Water constitutes approximately one-half of human body weight(Reference Wang, Deurenberg and Wang1) and is essential for human life and health. Total body water is tightly regulated and there is increasing evidence that even mild dehydration (defined as a 1–2 % loss in body mass caused by fluid deficit) may play a role in various morbidities like urolithiasis, constipation and hypertension(Reference Manz and Wentz2). Especially the elderly ( ≥ 65 years) are at an increased risk of dehydration because they experience a decrease in thirst sensation and at the same time have an impaired capacity of their kidneys to concentrate the urine(Reference Rolls and Phillips3Reference Jequier and Constant5).

However, the scientific basis for water intake recommendations for the elderly is scarce and the recommendations from different nutrition societies are not consistent. The German Nutrition Society, for example, recommends a lower total water intake with increasing age(6). In contrast, the US Institute of Medicine provides constant water intake recommendations (adequate intake (AI)) for younger and older adults. These AI values were based on the median total water intake of young adults to ensure an adequate amount of consumption in the elderly(7). The European Food Safety Authority is trying to develop a European standard at present(8). However, until now, detailed and representative data on water intake and hydration status of a population, which is the requirement to derive a reliable basis for intake recommendations, are missing.

Some years ago, we presented a concept of estimating individual 24 h hydration status(Reference Manz, Wentz and Sichert-Hellert9). It complies with the concept of Dietary Reference Intakes from the US Institute of Medicine(7), i.e. that the AI of a nutrient is the observed or experimentally determined estimated intake at which the risk of inadequacy is very low – only 2–3 %(7). The 24 h hydration status of a subject is inadequate if the 24 h urine osmolality is above the mean ( − 2 sd) value of experimentally determined maximum urine osmolality (for the respective life-stage group)(Reference Manz and Wentz10). The difference between the 24 h urine volume and the obligatory urine volume (i.e. the hypothetic volume necessary to excrete the actual 24 h urine solutes) is called the free-water-reserve(Reference Manz, Wentz and Sichert-Hellert9) – measuring the individual 24 h euhydration (calculations in detail are described in the Methods section).

Free-water-reserve is determined by various parameters of water metabolism: beverages and food water intake, metabolic water, non-renal water losses (NRWL), urine volume and obligatory urine volume. It is widely known that nearly all of these parameters undergo changes with increasing age. Elderly people show lower sweat losses(Reference Kenney and Hodgson11, Reference Torii12), and therefore NRWL decreases; at the same time renal concentration capacity becomes impaired(Reference Manz and Wentz10), resulting in an increased obligatory urine volume.

The aim of the present investigation was to quantify hydration status and its complex determining factors from young to old adulthood to analyse possible age-related alterations and provide a reliable basis for the derivation of dietary recommendations. We used data from the public use file and new results from the analysis of stored urine samples from the Verbundstudie Ernährungserhebung und Risikofaktoren-Analytik (VERA) study population of the National Food Consumption Survey of Germany in 1986–8(Reference Speitling, Hüppe and Kohlmeier13).


Between 1986 and 1988, a representative sample of 24 632 persons of the Federal Republic of Germany living in 11 141 households took part in the first National Food Consumption Survey(Reference Kübler, Baltzer and Grimm14, Reference Heseker, Adolf and Eberhardt15), documenting and analysing nutrition behaviour and physical activity by 7 d records and personal interviews. From this population, a representative sub-sample of 2006 persons aged 18–88 years was taken randomly and 24 h urine samples were collected from each subject (Cooperative Study: Nutrition Survey and Risk Factors Analysis, VERA)(Reference Heseker, Adolf and Eberhardt15, Reference Schneider, Eberhardt and Heseker16). The original diet and health survey from which the information used in the present study was obtained had ethical approval from the commissioning Federal Ministry of Research and Technology, the Institutional Review Board of the Faculty of Nutritional Sciences, Justus-Liebig-University Giessen, Germany, and the Scientific Advisory Council of the VERA study. Urine collection, over a 24 h period, was carried out on one of the days of dietary recording; subjects were instructed by the interviewer how to perform 24 h urine collection. Completely collected frozen urine samples were directly transported to the laboratory for analysis. Remaining samples were stored at < − 80°C. Urine osmolality was analysed (Osmometer OM 802-D; Vogel, Giessen, Germany) in the year 2003 from stored urine samples ( < − 80°C). Stability of urine osmolality was previously checked by remeasurements of 24 h urine samples after 15 years of storage. Recovery rates of more than 95 % ensured no disturbing effects of storage duration on urine osmolality. Measurements of 24 h urine osmolality were combined with previous measurements of urine volume and creatinine (Jaffé method) as well as data from the dietary record of the day of urine collection as available in the public use files of the VERA study(Reference Adolf17). In 115 subjects, single urine data were missing. In 269 subjects, the urine collection time was not in the range of 1200–1560 min. In ninety-one subjects, 24 h urine creatinine was below 0·1 mmol/kg per d in males and 0·09 mmol/kg per d in females(Reference Remer, Neubert and Maser-Gluth18). In two subjects, 24 h urine volume was below 300 ml and in one subject, body weight was missing. The final data sets included the data of 1528 subjects (women: 58·2 %; proportion of women in the initial VERA sample: 57·0 %; in the German population (1986–8, ≥ 20 years): 52·7 %).

Hydration status

Total water intake corresponds to the sum of beverages, metabolic water and water in food (including milk and milk products) taken from the dietary record of the day of urine collection. All foods and beverages consumed were recorded, using food scales for weighing or standardised containers and templates to estimate the consumed amounts.

In water balance, total water intake corresponds to total water losses, which is the sum of NRWL and 24 h urine volume. Thus, NRWL correspond to the difference of calculated total water intake and measured 24 h urine volume:


Renal solutes excretion (mOsm/d) corresponds to the product of urine osmolality (mOsm/kg) and 24 h urine volume (litres/d, assuming 1 kg water corresponds to 1 litre). Obligatory urine volume is defined as the water volume necessary to excrete 24 h urine solutes at the age-related lower limit of maximum urine osmolality (mean ( − 2 sd)). Based on literature data of standardised tests of renal concentration capacity in subjects in industrialised countries, the lower limit of maximum urine osmolality has been estimated to be 830 mOsm/kg minus 3·4 mOsm/kg per year starting from an age of 20 years(Reference Manz and Wentz10). The calculation of obligatory urine volume for an age above 20 years is:


Free-water-reserve corresponds to the difference of the 24 h urine volume and the obligatory urine volume


It quantifies individual 24 h hydration status(Reference Manz, Wentz and Sichert-Hellert9). If the value is positive, the subject is euhydrated. If it is negative (due to a 24 h urine osmolality above the mean ( − 2 sd) value of maximum urine osmolality), the subject is hypohydrated or in a hydration status in the range at risk of hypohydration.

In a population, euhydration is ensured if at least 97 % of the subjects show positive values of free-water-reserve(7). Euhydration may be achieved in a population at risk of hypohydration by a general increase in the level of total water intake (the theoretically required increase is represented by the calculated 3rd percentile value of free-water-reserve). Thus, the AI of total water of a population is the sum of median total water intake minus the 3rd percentile value of free-water-reserve(7, Reference Manz, Wentz and Sichert-Hellert9):


Another reasonable, less practicable concept to ensure euhydration is the reduction of obligatory urine volume (by the amount of the 3rd percentile volume of free-water-reserve) by a decrease of urine solutes excretion:


The high NRWL in men can be divided into an energy-related part (in accordance with the common approach of relating water intake recommendations to units of energy intake(8, 19)) and a male-specific part, accounting for the generally higher NRWL in males than in females, even if the differences in energy intake are taken into account. The energy-related part corresponds to the product of the age-group-specific mean female NRWL and the corresponding ratio of mean male and female energy intakes:


Statistical analysis

Anthropometric data, energy intake and results of water balance are given as means and standard deviations, stratified by age groups of 18–24, 25–49, 50–64 and ≥ 65 years. These age ranges were selected according to the actual age categorisation of the German Nutrition Society(6). Sex differences were tested by an unpaired t-test. To investigate the effects of age on the various parameters of water balance, a linear regression model was calculated for each parameter adjusted for energy intake and physical activity. Physical activity was defined as the sum of daily sports activities+cycling+moderate to vigorous physical activities (such as cleaning or gardening) and was expressed in hours. All regression models were run sex-stratified. Concerning free-water-reserve, the effects of the following factors were additionally included and tested for significance: education (four levels: elementary school, secondary school without diploma, diploma, academic studies), region (n 4: north, west, middle, south), size of place of residence (four categories: < 2000, < 20 000, < 500 000, ≥ 500 000 inhabitants) and mean income per person of a household (five categories: < 500, < 1000, < 1500, < 2000, ≥ 2000 D-Mark (approximately corresponding to € today). To directly compare male and female parameters of water metabolism, differences of mean male and mean female parameters were calculated after adjusting the values of women to the energy intake of men (i.e. after multiplication of the female values with the age-group-specific ratio of mean male and female energy intakes). An effect was accepted as significant if the P value (two-tailed) was below 0·05. All calculations were performed by using SAS procedures (version 8.02; SAS Institute, Cary, NC, USA).


Anthropometric data, energy intake and results of the parameters of water balance of males and females from a formerly representative sample (n 1528) of the German population in 1986–8 aged 18–88 years (VERA study) are presented in Tables 1 and 2, respectively. Comparison between sexes showed a significance level of P < 0·0001 for most of the presented parameters, except for urine solutes/energy (P = 0·0002) and urine volume (P = 0·49).

Table 1 Anthropometric data, energy intake and results of water balance of men from a formerly representative sample of the German population (VERA study)

(Mean values and standard deviations and medians)

FWR, free-water-reserve; AI, adequate intake.

* Metabolic water (ml) = 0·41 × protein intake (g)+0·55 × carbohydrate intake (g) +1·07 × fat intake (g)+1·17 × alcohol intake (g).

Table 2 Anthropometric data, energy intake and results of water balance of women from a formerly representative sample of the German population (VERA study)

(Mean values and standard deviations and medians)

FWR, free-water-reserve; AI, adequate intake.

* Metabolic water (ml) = 0·41 × protein intake (g) +0·55 × carbohydrate intake (g)+1·07 × fat intake (g) +1·17 ×  alcohol intake (g).

Median total water intake was 2483 ml/d in men and 2054 ml/d in women (P < 0·0001). Free-water-reserve was negative in 40 % of males and 19 % of females. Euhydration would have been ensured in 97 % of German adults, if the water balance had been improved by 427 ml/d in men and 211 ml/d in women by (a) an AI of total water of 2910 ml/d or 1·04 ml/kcal in men and 2265 ml/d or 1·05 ml/kcal in women, (b) a decrease of urine solutes excretion of 319 mOsm/d in men and 158 mOsm/d in women or (c) a mixture of both measures. Free-water-reserve was different in men and women (P < 0·0001). Education, region, size of place of residence, or income per person of a household (except in males, P = 0·03) had no effect on free-water-reserve.

Several parameters of 24 h water metabolism were affected by age (Table 3 and Fig. 1). Urine osmolality decreased with age in both sexes (men − 3·0 mOsm/kg per year; women − 2·4 mOsm/kg per year, results from the linear regression of age on osmolality, adjusted for energy intake, and physical activity, Table 3). Total water intake remained constant with age in men (P = 0·2); in women it increased (P = 0·001). Comparing men (women) above 65 years with those 18–24 years old, the proportion of beverages at 100 % total water input decreased slightly by 4·1 % (5·0 %; statistically not significant), whereas food water increased by 5·4 % (7·3 %). The proportion of metabolic water decreased slightly with − 1·4 % ( − 2·3 %). The proportion of NRWL at 100 % water output decreased by 22·2 % (10·3 %), whereas the proportion of obligatory urine volume increased by 18·1 % (10·9 %) and the proportion of free-water-reserve remained almost unchanged at +4·0 % ( − 0·4 %). The excretion of urine solutes slightly increased with age in both sexes. Concomitantly, an age-related increase in urine volume and a decrease of urine osmolality occurred.

Table 3 Effect of age (β) on different parameters of water metabolism in the VERA study population

* For two men and five women, no physical activity record was available.

Results of the linear regression model with age (in years) as independent continuous variable, adjusted for energy intake and physical activity.

Metabolic water (ml) = 0·41 × protein intake (g)+0·55 × carbohydrate intake (g)+1·07 × fat intake (g)+1·17 × alcohol (g).

Fig. 1 Comparison of parameters of water excretion between (a) men and (b) women (n 1528), categorised according to age. Water excretion in urine: , free-water-reserve; □, obligatory volume. Non-renal water loss: , male specific; , energy related; , total.

In Table 4, the hydration status of German men and women is compared after adjusting the different parameters for the sex differences in energy intake (by multiplying the female parameters of hydration status with the age-group-specific male-to-female energy ratio). The more unfavourable hydration status of men, indicated by a lower free-water-reserve of 359 ml/d (Table 4), originated from a reduced total water intake of 238 ml/d and a male-specific higher NRWL (mainly sweat loss) of 199 ml/d which was partly compensated by a lower obligatory urine volume of 78 ml/d. The male-specific NRWL were lowest in men ≥ 65 years (Fig. 1).

Table 4 Differences between mean male and mean female parameters of water metabolism after adjusting the values of women to the energy intake of men

* The lower free-water-reserve of men of 359 ml/d (100 %) originated from a reduced total water intake of 238 ml/d (66 %) and a male-specific higher non-renal water loss of 199 ml/d (55 %) partly compensated by a lower obligatory urine volume of 78 ml/d (22 %).


In the present study, the exceptional combination of dietary weighed records and concomitantly utilisable 24 h urine samples (n 1528) was used to estimate individual 24 h hydration status from young to old adulthood in a formerly representative population sample. These data were only available in the earlier, but not the most recent German food consumption survey. For the first time, age-related effects on hydration status and its complex determining factors could be evaluated, allowing us to draw a quite complete picture of the underlying physiological alterations and to derive a reliable basis for water intake recommendations.

Although ageing affected nearly all parameters of water metabolism, the hydration status itself – as sum of these parameters (water intake, metabolic water, NRWL, urine volume and obligatory urine volume) – did not change with age. Older men and women promoted water supply by the increased consumption of food with a high water and low energy content and counteracted it by an increased sodium intake(Reference Kohlmeier, Thefeld and Stelte20). Focusing on the side of water losses, the increased demand for obligatory urine volume by the age-related decrease of renal concentrating capacity is well known(Reference Manz and Wentz10). In males of our study, the age-related decrease in NRWL predominantly compensated the increase of obligatory urine volume; in females, this NRWL-decrease was less pronounced and did therefore only partly compensate increased obligatory urine volume. However, the remaining ‘gap’ of water requirements with increasing age in women was balanced by slightly increasing total water intakes – showing the remarkably precise regulation of an adequate hydration status throughout life.

Both overall and maximum sweating rates decreased with age and this was greater in males than females(Reference Kenney and Hodgson11, Reference Torii12). As a general physiological concept, it can be assumed that the difference of NRWL in men and women is the sum of a basic energy-related part and a male-specific part (see Methods – hydration status). In our study, the male-specific NRWL was remarkably lower in men above 50 years of age (114 ml/d) than in men younger than 50 years (about 270 ml/d, Table 4). In men ≥ 65 years old, energy-adjusted NRWL even fell below the values for women, resulting in negative male-specific NRWL of − 10 ml/d. The well-known sex differences in sweating rates between men and women(Reference Gagnon, Jay and Lemire21) that do not occur until puberty(Reference Rees and Shuster22) lead to the suggestion that androgen activity may be one important factor involved in the change of the male-specific NRWL coinciding with adrenarche and declining in the elderly. Several authors concluded that male hormones (e.g. testosterone) enhance the sweat response and female hormones (e.g. oestradiol) inhibit it(Reference Ichinose-Kuwahara, Inoue and Iseki23, Reference Araki, Toda and Matsushita24). Immunohistochemical studies that detected expression of androgen receptors in eccrine sweat gland cells in adults support this hypothesis(Reference Choudhry, Hodgins and Van der Kwast25, Reference Pelletier and Ren26).

Mean 24 h urine osmolality, an indirect parameter of hydration status, was 682 mOsm/kg in men and 569 mOsm/kg in women. Mean osmolalities in spontaneous urine samples of two representative groups in Germany and the USA showed comparable levels(Reference Singhof and Manz27, Reference Kutz, Cook and Carter-Pokras28). Overall, however, mean urine osmolalities from small groups of healthy subjects from all over the world were surprisingly widely scattered, indicating the large intercultural differences of urine osmolality and hinting at remarkable differences in the hydration status of different societies. Mean urine osmolality ranged from 909 mOsm/kg (China, 50-year-old adults(Reference Zhang, Huang and Li29)), across 536 mOsm/kg (UK, adults with a mean age of 44 years(Reference Fogarty30)) to 392 mOsm/kg (Poland, children aged 5–18 years(Reference Manz and Wentz10)). It is not possible to define a physiological or natural narrow urine osmolality range as it is always influenced by the cultural context and habitual food intake. Only after additionally considering 24 h urine volume, urine solute excretion and maximum urine osmolality, quantification of individual 24 h hydration status is possible.

One unexpected finding was the almost parallel age-related decrease in the mean urine osmolality seen in our study (men − 3·0 mOsm/kg per year; women − 2·4 mOsm/kg per year) and observed in standardised renal concentration tests ( − 3·4 mOsm/kg per year)(Reference Manz and Wentz10) as well as in the USA ( − 3·9 mOsm/kg per year)(Reference Kutz, Cook and Carter-Pokras28). These consistent findings in different cultures hint at a hypothetical physiological homeostatic mechanism that might regulate ad libitum drinking behaviour(Reference Epstein, Ramsay and Booth31) to counterbalance the age-related decrease in renal concentration capacity. In consequence, the free-water-reserve remains constant.

The important feature of the presented concept of free-water-reserve and calculation of AI is that it is not only based on median total water intake and maximum concentration capacity of the kidneys, but considers individual 24 h hydration status and adds a safety margin to ensure adequate water intakes in nearly all (97 %) healthy persons of a population. This safety margin was defined by the 3rd percentile of free-water-reserve. No negative effects have to be expected by the resulting water surplus in individuals with a more favourable hydration status as water balance is regulated with precision in a wide range of water needs and intakes(Reference Sawka, Cheuvront and Carter32). The fact that to date only a few countries included water in their dietary recommendations, and most of them not even considered renal concentration capacity but only based their recommendations on observed intakes(8), shows the need for research in more depth in this topic. The concept of free-water-reserve can serve as a suitable measure to derive specific water intake recommendations also outside Germany (considering the population-specific maximum renal concentration capacity).

According to the concept of free-water-reserve, 40 % of men and 19 % of women with a free-water-reserve below zero were at risk of hypohydration. These sex differences in hydration status are also common in other industrialised countries, where males usually show a higher urine osmolality than females(Reference Kutz, Cook and Carter-Pokras28, Reference Waters, Sussman and Asscher33). Many biological and social differences such as higher physical activity and preference for food with a low water and high energy density (e.g. meat products, fast food) in men compared to women may be responsible for this phenomenon(Reference Ebner and Manz34). In the present study, the in-detail analysis of parameters of water metabolism revealed that the strikingly higher prevalence of negative free-water-reserve in men was due to higher NRWL and lower total water intakes that were only partly compensated by a lower obligatory urine volume (Table 4).

In the investigated population, adequate total water intake would have been ensured if all men (women) drank two (one) additional cups of beverages per d. A corresponding decrease in the obligatory urine volume by a lower urinary excretion of solutes is no realistic option. In men (women), protein intake would have had to be reduced by 56 (28) g/d or NaCl intake by 9·3 (4·6) g/d. If AI of total water is to be attained by an exclusive increase in beverage consumption, median beverage intake in this German men (women) should have been 1826 (1354) ml/d. This value is, at least in men, clearly higher than the current German recommendation(6) of about 1400 ml – depending on age – for beverage intake. Current recommended total water intakes for older adults (51 to < 65 and ≥ 65 years: 2250 ml/d, not sex-stratified) are nearly equivalent to the observed median total water intakes in the present study (2282 and 2126 ml/d for 50 to < 65 and ≥ 65 years, respectively). However, these intake levels were accompanied by a prevalence of 29 and 27 % of the respective age group that was at risk of hypohydration (i.e. had a free-water-reserve < 0 ml/d), indicating the need for a revision of the current German intake recommendations. Compared to the US recommendation of the Institute of Medicine of 3700 (2700) ml for men (women), our calculated AI are substantially lower, probably mainly due to the traditionally higher water intakes in the USA compared to Germany(Reference Manz and Wentz35, Reference Popkin, D'Anci and Rosenberg36). As US AI were only set on the observed median intake at which an adequate hydration was assumed (estimated by plasma osmolality), it cannot be excluded that also for the US population lower AI values would be sufficient.

The main limitation of our study is the fact that the data presented in this study were collected a considerable number of years ago, and therefore we cannot draw reasonable conclusions on the actual hydration status of the German population. However, the estimated values for an adequate total water intake should be independent of the time of data collection, as the corresponding results have been yielded with a physiologically based ‘free-water-reserve and water balance’ assessment tool. Furthermore, we could only estimate whole non-renal water losses and were not able to differentiate between stool water, insensible water loss by respiration and through the skin (i.e. perspiration or transepidermal diffusion) and sweat loss.

In this formerly representative German sample, younger and older adults showed a similar hydration status. Correspondingly, total water requirements did not increase with age, clearly indicating that there is no need for age-specific water intake recommendations for the elderly (in contrast to sex stratification which appears necessary). Nevertheless, the elderly run a higher risk of dehydration, partly because their perception of thirst seems to be impaired(Reference Rikkert, Hoefnagels, Deurenberg, Arnaud, Baumgartner, Morley, Rosenberg and Toshikazu37) and a larger water volume is necessary to excrete a given renal solute load(Reference Manz and Wentz10). It can be assumed that the physiological mechanisms which were responsible for the age-independent and widely constant total water requirements observed in this German sample (i.e. compensation of decreased renal concentration capacity by decreased NRWL, especially in men) may represent a universal finding with transferability also to other populations.


The present examination was supported by the Ministry of Science and Research, North Rhine-Westphalia, Germany. F. M. designed the study and together with S. A. J. wrote the report; A. W. was involved with analysis and interpretation of the study; H. B. provided administrative and statistical support; T. R. was responsible for the urine analysis and contributed to data interpretation. All authors contributed to the final version of the report. None of the authors has any conflict of interest in regard to this study. The authors thank Professor W. Kübler and Dr K.-J. Moch, Giessen, for their basic contributions to the NVS and VERA studies and the permission to use the respective public use files.


1Wang, Z, Deurenberg, P, Wang, W, et al. (1999) Hydration of fat-free body mass: review and critique of a classic body-composition constant. Am J Clin Nutr 69, 833841.CrossRefGoogle ScholarPubMed
2Manz, F & Wentz, A (2005) The importance of good hydration for the prevention of chronic diseases. Nutr Rev 63, S2S5.CrossRefGoogle ScholarPubMed
3Rolls, BJ & Phillips, PA (1990) Aging and disturbances of thirst and fluid balance. Nutr Rev 48, 137144.CrossRefGoogle ScholarPubMed
4Kenney, WL & Chiu, P (2001) Influence of age on thirst and fluid intake. Med Sci Sports Exerc 33, 15241532.CrossRefGoogle ScholarPubMed
5Jequier, E & Constant, F (2010) Water as an essential nutrient: the physiological basis of hydration. Eur J Clin Nutr 64, 115123.CrossRefGoogle ScholarPubMed
6Deutsche Gesellschaft für Ernährung (Hrsg.) (2008) Reference Values for Nutrient Intake (in German). Umschau Verlag: Frankfurt a. M.Google Scholar
7Institute of Medicine (2006) Dietary Reference Intakes: The Essential Guide to Nutrient Requirements. Washington, DC: National Academic Press.Google Scholar
8European Food Safety Authority (2009) Scientific opinion of the Panel on Dietetic Products Nutrition and Allergies. Draft dietary reference values for water. EFSA J 249.Google Scholar
9Manz, F, Wentz, A & Sichert-Hellert, W (2002) The most essential nutrient: defining the adequate intake of water. J Pediatr 141, 587592.CrossRefGoogle Scholar
10Manz, F & Wentz, A (2003) 24-h hydration status: parameters, epidemiology and recommendations. Eur J Clin Nutr 57, Suppl. 2, S10S18.CrossRefGoogle ScholarPubMed
11Kenney, WL & Hodgson, JL (1987) Heat tolerance, thermoregulation and ageing. Sports Med 4, 446456.CrossRefGoogle ScholarPubMed
12Torii, M (1995) Maximal sweating rate in humans. J Hum Ergol (Tokyo) 24, 137152.Google ScholarPubMed
13Speitling, A, Hüppe, R, Kohlmeier, M, et al. (1992) Methodological Handbook Nutrition Survey and Risk Factor Analysis. VERA-Schriftenreihe Band Ia. Niederkleen: Wissenschaftlicher Fachverlag Dr. Fleeck.Google Scholar
14Kübler, W, Baltzer, H, Grimm, R, et al. (1997) National Food Consumption Survey (NVS) and Cooperative Study: Nutrition Survey and Risk Factor Analysis (VERA). Synopsis and Perspectives. VERA-Schriftenreihe Band XIV a. Niederkleen: Wissenschaftlicher Fachverlag Dr. Fleeck.Google Scholar
15Heseker, H, Adolf, T, Eberhardt, W, et al. (1992) Lebensmittel- und Nährstoffaufnahme Erwachsener in der Bundesrepublik Deutschland (Food and Nutrient Intake in Adults in the Federal Republic of Germany). VERA-Schriftenreihe Band III. Niederkleen: Wissenschaftlicher Fachverlag Dr. Fleeck.Google Scholar
16Schneider, R, Eberhardt, W, Heseker, H, et al. (1992) Die VERA Stichprobe im Vergleich mit Volkszählung, Mikrozensus und anderen nationalen Erhebungen (The VERA Sample Compared with Census, Microcensus and Other National Studies). VERA-Schriftenreihe Band II. Niederkleen: Wissenschaftlicher Fachverlag Dr. Fleeck.Google Scholar
17Adolf, T (1994) Public Use File National Food Consumption Survey (NVS) and Cooperative Study: Nutrition Survey and Risk Factor Analysis (VERA). Gießen: Institut für Ernährungswissenschaften.Google Scholar
18Remer, T, Neubert, A & Maser-Gluth, C (2002) Anthropometry-based reference values for 24-h urinary creatinine excretion during growth and their use in endocrine and nutritional research. Am J Clin Nutr 75, 561569.CrossRefGoogle ScholarPubMed
19National Research Council (1989) Recommended Dietary Allowances, 10th ed.Washington, DC: National Academic Press.Google Scholar
20Kohlmeier, M, Thefeld, W, Stelte, W, et al. (1995) Versorgung Erwachsener mit Mineralstoffen und Spurenelementen in der Bundesrepublik Deutschland (Minerals and Trace elements supply in adults in the Federal Republic of Germany). VERA-Schriftenreihe Band V. Niederkleen: Wissenschaftlicher Fachverlag Dr. Fleeck.Google Scholar
21Gagnon, D, Jay, O, Lemire, B, et al. (2008) Sex-related differences in evaporative heat loss: the importance of metabolic heat production. Eur J Appl Physiol 104, 821829.CrossRefGoogle ScholarPubMed
22Rees, J & Shuster, S (1981) Pubertal induction of sweat gland activity. Clin Sci (Lond) 60, 689692.CrossRefGoogle ScholarPubMed
23Ichinose-Kuwahara, T, Inoue, Y, Iseki, Y, et al. (2010) Sex differences in the effects of physical training on sweat gland responses during a graded exercise. Exp Physiol 95, 10261032.CrossRefGoogle ScholarPubMed
24Araki, T, Toda, Y, Matsushita, K, et al. (1979) Age differences in sweating during muscular exercise. J Physiol Fitness Jpn 28, 239248.Google Scholar
25Choudhry, R, Hodgins, MB, Van der Kwast, TH, et al. (1992) Localization of androgen receptors in human skin by immunohistochemistry: implications for the hormonal regulation of hair growth, sebaceous glands and sweat glands. J Endocrinol 133, 467475.CrossRefGoogle ScholarPubMed
26Pelletier, G & Ren, L (2004) Localization of sex steroid receptors in human skin. Histol Histopathol 19, 629636.Google ScholarPubMed
27Singhof, S & Manz, F (2001) Flüssigkeitsversorgung der Senioren im Deutschland (Water supply in seniors in Germany). Aktuel Ernaehr Med 102106.CrossRefGoogle Scholar
28Kutz, FW, Cook, BT, Carter-Pokras, OD, et al. (1992) Selected pesticide residues and metabolites in urine from a survey of the US general population. J Toxicol Environ Health 37, 277291.CrossRefGoogle Scholar
29Zhang, L, Huang, X, Li, X, et al. (1997) Alterations in renal function in patients with obstructive sleep apnea syndrome and effects of continuous positive airway pressure. Chin Med J (Engl) 110, 915918.Google ScholarPubMed
30Fogarty, AJ (1971) The significance of sodium in renal stone formation. Br J Urol 43, 403405.CrossRefGoogle ScholarPubMed
31Epstein, A (1991) Thirst and salt intake: a personal review and some suggestions. In Thirst, pp. 481501 [Ramsay, D and Booth, D, editors]. London: Springer.CrossRefGoogle Scholar
32Sawka, MN, Cheuvront, SN & Carter, R 3rd (2005) Human water needs. Nutr Rev 63, S30S39.CrossRefGoogle ScholarPubMed
33Waters, WE, Sussman, M & Asscher, AW (1967) Community study of urinary pH and osmolality. Br J Prev Soc Med 21, 129132.Google ScholarPubMed
34Ebner, A & Manz, F (2002) Sex difference of urinary osmolality in German children. Am J Nephrol 22, 352355.CrossRefGoogle ScholarPubMed
35Manz, F & Wentz, A (2005) Hydration status in the United States and Germany. Nutr Rev 63, S55S62.CrossRefGoogle ScholarPubMed
36Popkin, BM, D'Anci, KE & Rosenberg, IH (2010) Water, hydration, and health. Nutr Rev 68, 439458.CrossRefGoogle ScholarPubMed
37Rikkert, M, Hoefnagels, W & Deurenberg, P (1998) Age-related changes in body fluid compartments and the assessment of dehydration in old age. In Hydration and Aging, pp. 1332 [Arnaud, M, Baumgartner, R, Morley, J, Rosenberg, I and Toshikazu, S, editors]. New York, NY: Springer Publishing Company.Google Scholar

Full text views

Full text views reflects PDF downloads, PDFs sent to Google Drive, Dropbox and Kindle and HTML full text views.

Total number of HTML views: 87
Total number of PDF views: 451 *
View data table for this chart

* Views captured on Cambridge Core between September 2016 - 18th January 2021. This data will be updated every 24 hours.

Hostname: page-component-77fc7d77f9-g622z Total loading time: 0.35 Render date: 2021-01-18T04:33:17.750Z Query parameters: { "hasAccess": "1", "openAccess": "0", "isLogged": "0", "lang": "en" } Feature Flags last update: Mon Jan 18 2021 04:02:07 GMT+0000 (Coordinated Universal Time) Feature Flags: { "metrics": true, "metricsAbstractViews": false, "peerReview": true, "crossMark": true, "comments": true, "relatedCommentaries": true, "subject": true, "clr": true, "languageSwitch": true, "figures": false, "newCiteModal": false, "shouldUseShareProductTool": true, "shouldUseHypothesis": true, "isUnsiloEnabled": true }

Send article to Kindle

To send this article to your Kindle, first ensure is added to your Approved Personal Document E-mail List under your Personal Document Settings on the Manage Your Content and Devices page of your Amazon account. Then enter the ‘name’ part of your Kindle email address below. Find out more about sending to your Kindle. Find out more about sending to your Kindle.

Note you can select to send to either the or variations. ‘’ emails are free but can only be sent to your device when it is connected to wi-fi. ‘’ emails can be delivered even when you are not connected to wi-fi, but note that service fees apply.

Find out more about the Kindle Personal Document Service.

Water balance throughout the adult life span in a German population
Available formats

Send article to Dropbox

To send this article to your Dropbox account, please select one or more formats and confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your <service> account. Find out more about sending content to Dropbox.

Water balance throughout the adult life span in a German population
Available formats

Send article to Google Drive

To send this article to your Google Drive account, please select one or more formats and confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your <service> account. Find out more about sending content to Google Drive.

Water balance throughout the adult life span in a German population
Available formats

Reply to: Submit a response

Your details

Conflicting interests

Do you have any conflicting interests? *