Introduction
Water is an essential nutrient [
1] and plays a vital role in metabolism by maintaining cellular shape, supporting cellular functions, and serving as a transport medium for nutrients and wastes [
2]. Water is especially important to women who are pregnant or nursing. During gestation, plasma volume expands [
3], and amniotic fluid protects the developing child [
4]. An average woman gains about 11 kg of body mass during pregnancy, and a large portion of this gain (approximately 7–8 L) is due to water retention [
5]. During the postpartum period, nursing mothers experience an increased water loss via breast milk, representing approximately 700 ml per day at 8 weeks postpartum [
6,
7]. These increased physiological needs for water pose a challenge to the neuroendocrine mechanisms that regulate fluid–electrolyte balance and suggest evolving water requirements from conception to lactation.
Despite the importance of water to both the mother and developing child, research on the regulation of total body water balance, daily water needs, and biomarkers of hydration in pregnant and lactating women is scarce. Even less is known about how maternal hydration may impact either mother or fetus during pregnancy or into early life. Consequently, the dietary reference intakes of water during pregnancy in both Europe and the USA (2.3 and 3.0 L day
−1, respectively) are based only upon the increased amount of water needed to offset the increased caloric intake during pregnancy (i.e., 300 ml day
−1 for 300 kcal day
−1) [
8,
9]. During lactation, adequate intake of total water increases to 2.7 [
8] and 3.8 [
9] L day
−1 in Europe and the USA, respectively, to offset water lost in breast milk.
While dietary reference intakes provide guidelines for adequate intake for the population [
8,
9], individual water needs vary greatly depending upon personal water intake via the diet, and personal water losses through physical activity, environmental, and other factors. Among the various sources of daily water loss, urine output has been identified as one way to assess hydration in the individual. Urine volume and concentration represent the end result of intake and loss, after accounting for differences in sweat loss and dietary solute load. Manz et al. [
10] suggested that 24-h urine concentration reflects the kidney’s self-regulation of fluid volume deficit or excess, and provides an indication of the sum of all water gains and losses in healthy individuals. Other recent publications [
11,
12] support this concept with data showing that, in healthy men and non-pregnant women, urinary hydration biomarkers including urine osmolality (
U
OSM) and specific gravity (
U
SG) represent inter- and intra-individual differences of daily fluid intake in high- versus low-volume consumers. While useful in a clinical or laboratory setting,
U
OSM is not readily available to the general population. However, urine color (
U
COL), a tool that requires little cost, laboratory instrumentation, and expertise, may be valuable as a surrogate hydration marker for daily monitoring of urine concentration. While
U
COL has been demonstrated to track changes in daily hydration habits in the general adult population [
13‐
15], no study has assessed its utility or validity in pregnant or lactating women. During pregnancy, serum osmolality is reduced approximately 8–10 mOsm kg
−1, changing the point of isotonicity between urine and blood at the kidney, potentially impacting free water clearance and
U
OSM and thus potentially interrupting the previously reported relationship between
U
OSM and
U
COL in non-pregnant women. Additionally, some research reports increased void frequency [
16] and increased 24-h urine volume with lower 24-h
U
OSM in pregnant women [
17], but decreased void frequency [
16] and decreased 24-h urine volume with higher 24-h
U
OSM in lactating women [
18]. Given that increased 24-h urine volume is associated with lighter urine color and lower osmolality in non-pregnant, non-lactating women [
14], this suggests the relationship between
U
COL and
U
OSM may be skewed in, or between, pregnant and lactating women compared to control women and warrants further investigation.
Thus, the purpose of this investigation was to determine whether
U
COL was a valid measure of urine concentration in pregnant and lactating women, as well as pair-matched non-pregnant and non-lactating controls. The validity of urine color was evaluated in two ways: first, by determining the relationships between 24-h
U
COL and biomarkers of urine concentration, specifically 24-h
U
OSM and 24-h
U
SG, utilizing a Spearman’s rank-order correlation, and second, by determining the diagnostic accuracy of
U
COL (24-h and single samples, separately), to accurately identify
U
OSM ≥ 500 mOsm kg
−1, utilizing receiver operating characteristic curve analysis, sensitivity, and specificity. Maintaining
U
OSM under this cutoff has been associated with ensuring adequate daily fluid intake and urine output for the reduction in risk for urolithiasis or decline in kidney function, as well as avoidance of high plasma vasopressin concentrations often linked to disease states [
19].
Discussion
There is no clear consensus on what represents an optimal 24-h urine concentration, either for the general population or specifically for pregnant and lactating women. Approximately 800 mOsm kg
−1 has been proposed and used as an upper limit for euhydration [
25,
26]. However, 500 mOsm kg
−1 has been suggested as a threshold for “appropriate” [
27] or “optimal” [
19] hydration, supported by observed associations between low 24-h fluid intake, low 24-h urine volume, and/or high 24-h urine concentration and the development of kidney stones [
28], urinary tract infection [
29], hyperglycemia [
30], chronic kidney disease [
31], and rate of decline in estimated glomerular filtration rate [
32,
33]. Given the heightened importance of water balance in pregnancy, it appears prudent to leave a reasonable margin between a target 24-h urine osmolality and the upper limit for euhydration, and thus, 500 mOsm kg
−1 was deemed appropriate. This value is also supported as a desirable 24-h urine osmolality in the EFSA opinion on dietary reference values for water [
8].
We adopted a
U
OSM under 500 mOsm kg
−1 as a goal for pregnant and lactating women to optimize body water balance [
8] and avoid potential negative health consequences [
19]. However, the technical requirements of measuring
U
OSM (i.e., instrumentation, expertise) preclude its use during daily activities and emphasize the need for simple, noninvasive hydration assessment techniques such as
U
COL [
34‐
36]. Figures
2 and
3 demonstrate that 24-h
U
COL was significantly correlated with
U
SG and
U
OSM in pregnant and lactating women. While a range of
U
SG and
U
OSM is associated with each
U
COL for pregnant and lactating women, the degree of variation is similar to relationships demonstrated in other subject populations, including non-pregnant women [
14], men [
37], the elderly [
38,
39], and children [
40] where correlation coefficients have ranged from 0.48 to 0.93. This variation may be explained by the fact that urine color and urine osmolality are generated by two different mechanisms. Urine color is produced by the concentration of urochome in the urine, which is generated by metabolic processes and independent of diet [
41,
42]; urine osmolality is determined by the concentration of solute (e.g., Na
+, K
+, Cl
−, urea) in the urine [
43]. Despite variation between measures of urine concentration and urine pigmentation, the two remain significantly correlated and adequate means of assessing hydration status in multiple populations.
Further, ROC curve analyses (Table
2) indicated that
U
COL provided adequate diagnostic accuracy to allow women to successfully monitor
U
COL in order to maintain a urine concentration below 500 mOsm kg
−1. Because a
U
COL ≥ 4 was associated with high sensitivity (i.e., a high true positive rate), a negative test (i.e., a
U
COL of 1, 2, or 3) largely ruled-out the possibility of
U
OSM being greater than 500 mOsm kg
−1. Thus, when a
U
COL ≥ 4 is observed,
U
OSM is likely ≥500 mOsm kg
−1 and warrants increased fluid consumption (assuming no change in solute load) to reduce urine concentration below 500 mOsm kg
−1. A visual seemingly equal split of single-sample
U
OSM above and below 500 mOsm kg
−1 at a
U
COL of 4 in pregnant women is present (Figs.
4,
5); this is statistically evident in the trade off between sensitivity and specificity at that criterion value (Table
2). In order to capture as many true positives as possible, the criterion value will favor a higher sensitivity than specificity; thus, a
U
COL of 4 emerges as the criterion value to identify
U
OSM ≥ 500 mOsm kg
−1 with the greatest sensitivity. A lesser AUC in ROC curve analyses for 24-h urine samples in pregnant women statistically represents this variability (Fig.
4; Table
2). While the AUC for 24-h
U
COL in pregnant women was significantly different from the other groups, the AUC was still statistically significant, and the criterion value was the same as the criterion value identified in the other groups. This implies that the clinical use of 24-h
U
COL in pregnant women to determine whether 24-h
U
OSM is ≥500 mOsm kg
−1 is still valid, but less diagnostically accurate compared to other groups. Future research should evaluate potential sources of this variation.
Monitoring and optimizing water intake during pregnancy and lactation is important, given the inherent physiological challenges to water balance. Increased daily water intake supports expanded total body water, tissue development during gestation, and water loss due to emesis, if experienced. Increased water intake also offsets the water secreted in breast milk. In addition to optimizing body water balance, 24-h water intake impacts fetal and maternal health. For example, acute oral fluid intake of 1–2 L increases amniotic fluid volume in women with both normal and low amniotic fluid volumes [
44], but little is known about the effects of habitual maternal fluid intake on development of the child in utero or during the neonatal period. In studies involving hypotonic plasma volume expansion, plasma osmolality decreased for both mother and fetus [
45], demonstrating the exchange of fluids between compartments. The change in plasma osmolality and concomitant change in plasma vasopressin has been noted in both acute water loading and 12-h fluid deprivation in pregnant women. Together with the newfound association between high vasopressin and development of preeclampsia [
46], these data suggest that adequate water intake during pregnancy might be important for the health of the mother and the fetus. Given the importance of the gestational period and early life on future health outcomes, further research into maternal hydration and health is of fundamental importance. The present investigation may serve as a foundation for future research to identify practical means of monitoring hydration status and enacting behavioral change to promote adequate fluid intake during pregnancy and lactation.
In summary, the present investigation demonstrates that pregnant or lactating women, in addition to non-pregnant and non-lactating women, can use
U
COL as a practical indicator of
U
OSM, and thus, as a reference for whether fluid intake has been adequate. Women who present with
U
COL < 4 likely have a
U
OSM < 500 mOsm kg
−1, suggesting that their fluid intake is adequate to compensate for daily losses and maintain a healthy urine output. Women who present with
U
COL ≥ 4 likely have a
U
OSM ≥ 500 mOsm kg
−1 and should increase fluid consumption to reduce urine concentration, thereby reducing the risk of potential health complications [
19,
28‐
33].