Distribution and turnover of water in Merino sheep selected for high wool production

1966 ◽  
Vol 17 (4) ◽  
pp. 491 ◽  
Author(s):  
WV Macfarlane ◽  
CHS Dolling ◽  
B Howard

Estimates of the distribution of body water and the rate of water turnover were made on medium Peppin Merino ewes grazing on Mitchell grass association pasture in south-western Queensland during January and November. It so happened that the January measurements were made while the sheep were on lush green pasture following good rains, and that the November measurements were made on dry pasture after a number of months of low rainfall. The estimates made on each sheep included those of plasma volume, extracellular volume, total body water, plasma protein, and water turnover per 24 hr. The ewes, which were approximately 4¼ and 4¾ years of age at the times of measurement, were drawn either from a flock which had been under selection for high clean wool production per head or from a control flock in which all animals used for breeding had been chosen at random from those available. Twelve ewes from each flock were observed in January, and a different set of 10 ewes from each flock was observed in November. Body fluid compartments, as millilitres per kilogram body weight, were greater during the wet: than during the dry period. Plasma volumes were significantly greater in January than in November by 10.3% for the selected ewes and 18.2% for control ewes. The estimates of extracellular volume showed a similar significant difference between the months (15.4% for selected ewes and 17.4% for controls). The January measurements of total body water exceeded the November observations by 9.6% in the selected ewes and 11.2% in the control ewes, both increases being significant. In none of these three characteristics, however, were the selected ewes significantly different from the control ewes during either January or November. The 24 hr turnover of water in millilitres per kilogram body weight was significantly greater in January than in November by 30% for selected sheep and 51.1% for controls. The high water content of pasture during January greatly reduced the free water intake from troughs (ratio of respective water intakes of control and selected sheep was 100/123.7 in November and 1.3/1.5 in January); and the low dry matter content of the food became the major determinant of water turnover. When grazing relatively dry grasses in November, the selected sheep turned over significantly more water than did the controls (ratio control to selected was 100/113.7), but in January the turnovers were not significantly different (control/selected = 137.5/128.7).

1996 ◽  
Vol 80 (4) ◽  
pp. 1118-1125 ◽  
Author(s):  
C. Fusch ◽  
W. Gfrorer ◽  
C. Koch ◽  
A. Thomas ◽  
A. Grunert ◽  
...  

Thirteen healthy subjects (11 men and 2 women; 30.2 +/- 5.4 yr; 73.5 +/- 10.3 kg; 178.9 +/- 10.4 cm; body mass index, 22.9 +/- 1.6 kg/m2) participated at the 62-day expedition to the Broad Peak (8,047 m), Pakistan. Weight, body water, and water turnover (deuterium dilution and elimination) were measured eight times to assess long-term changes. Body weight fell during the ascent to the base camp [from 73.2 +/- 9.8 (baseline) to 71.7 +/- 9.7 kg; P < 0.05] and decreased until the end of the base camp stay (66.7 +/- 7.2 kg; P < 0.0001). Body compartments changed at different rates. Total body water decreased during the ascent (from 43.1 +/- 7.3 to 41.0 +/- 7.7 liters; P < 0.05) and remained unchanged until the base camp was reached (41.2 +/- 6.9 liters; P < 0.01) but decreased further during the base camp stay (40.6 +/- 5.2 liters). Water content of the body (total body water-to-body weight ratio) fell during the ascent (from 58.6 +/- 3.4 to 55.8 +/- 4.4%; P < 0.01), approached the baseline value during the base camp (57.4 +/- 4.0 and 58.3 +/- 5.1%), and increased again until the end of the base camp (60.6 +/- 3.4 and 60.9 +/- 4.3%). The compartment of the solids increased during the ascent (from 30.2 +/- 3.4 to 32.2 +/- 4.9 kg; P < 0.01) and approached the baseline value on arrival at the base camp (30.5 +/- 4.7 kg). Until the end of the base camp, the compartment of the solids fell (26.9 +/- 2.6 and 26.1 +/- 4.0 kg), indicating that weight loss was due to a loss of body solids, presumably mostly fat mass. Water turnover during the pretest period (sea level) was 45 +/- 7 ml.kg-1.day-1; it increased during the ascent (56 +/- 11 and 60 +/- 10 ml.kg-1.day-1) but remained constant during the base camp stay (63 +/- 12, 58 +/- 9, and 56 +/- 10 ml.kg-1.day-1). It increased during the ascent to Broad Peak (73 +/- 20 ml.kg-1.day-1; P < 0.05) and even more during the descent to civilization (83 +/- 17 ml.kg-1.day-1; P < 0.05).


Rangifer ◽  
1985 ◽  
Vol 5 (1) ◽  
pp. 2 ◽  
Author(s):  
Terje S. Larsen ◽  
Arnoldus Schytte Blix

<p>Total body water and water turnover were measured at different times throughout the year in 3 captive Norwegian reindeer, using a tritiated water dilution method (Holleman et al. 1982). Total body water (percent of body weight) increased during late autumn and winter, from 59.1 &plusmn; 1.5 % in October to 72.5 &plusmn; 2.0 % in April. Using the equatation by Pace and Rathbun (1945) for predicting total body fat (% fat = 100 - % water/0.732), this increase in total body water indicates a concomitant reduction in body fat, from a maximum value of 18.9 &plusmn; 2.6 % (of body weight) in October to a minimum of 0.9 &plusmn; 2.7 % in April. During summer, on the other hand, fat content increased at the expense of a reduced percentage of body water. Water turnover was low in winter (December - April), ranging between 30.8 &plusmn; 5.2and43.6 &plusmn; 13.5ml.d-'. kg-1, but increased nearly fourfold during summer (June-August) with a maximum of 117.7 &plusmn; 5.9 ml.d-1. kg-1 in August. Positive correlations between water turnover and food intake and between water turnover and ambient temperature were found, the latter probably resulting from an incidental correlation between food intake and ambient temperature.</p><p>Sesongmessige forandringer i totalt kroppsvann, kropps-sammensetning og vannomsetning hos reinsdyr.</p><p>Abstract in Norwegian / Sammendrag: Totalt kroppsvann og vannomsetning av vann ble m&aring;lt til forskjellige &aring;rstider i 3 norske reinsdyr ved hjelp av utvasking av tritiert vann (Holleman et al. 1982). Totalt kroppsvann (prosent av kroppsvekt) &oslash;kte utover h&oslash;sten og vinteren, fra 59.1 &plusmn; 1.5 % i oktober til 72.5 &plusmn; 2.0 % i april. Ved hjelp av en ligning som er gitt av Pace og Rathbun (1945) for beregning av totalt kroppsfett (% fett = 100 - % vann/0.732), fant en at denne &oslash;kningen i vanninnhold tilsvarte en samtidig reduksjon i fettinnhold, fra en maksimums-verdi p&aring; 18.9 &plusmn; 2.6 % av kroppsvekt i oktober til et minimum p&aring; 0.9 &plusmn; 2.7 % i april. Utover sommeren &oslash;kte derimot innholdet av fett p&aring; bekostning av vanninnholdet. Omsetningen av vann var lav vinterstid (desember - april), varierende mellom 30.8 &plusmn; 5.2 og 43.6 &plusmn; 13.5 ml.d-1.kg-1, men &oslash;kte nesten fire ganger i l&oslash;pet av sommeren (juni - august) til et maksimum p&aring; 117.7 &plusmn; 5.9 ml.d-1.kg-1 i august. Det ble funnet positive korrelasjoner mellom vannomsetning og forinntak og mellom vannomsetning og omgivelsestemperatur. Sistnevnte korrelasjon kan muligens skyldes en tilfeldig sammenheng mellom forinntak og omgivelsestemperatur.</p><p>Vuodenaikaiset muutokset poron ruumiin kokonaisvesim&aring;&aring;r&aring;ss&aring;, ruumiin koostumuksessa ja vesiaineenvaihdunnassa.</p><p>Abstract in Finnish / Yhteenveto: Ruumiin kokonaisvesima&aring;r&aring;&aring; ja vesiaineenvaihduntaa mitattiin eri vuodenaikoina 3 norjalaisella porolla k&aring;ytt&aring;m&aring;ll&aring; apuna tritioitua vetta (Holleman et al. 1982). Ruumiin kokonaisvesim&aring;ar&aring; (prosenttia ruumiinpainosta) lis&aring;antyi syksyll&aring; ja talvella lokakuun 59.1&plusmn;1.5%:sta 72.5&plusmn;2.0%:i huhtikuussa. K&aring;ytt&aring;m&aring;ll&aring; Pacen ja Rathbunin (1945) ruumiin kokonaisrasvapitoisuude laskukaavaa (rasva % = 100 - vesi %/0.732) huomattiin tam&aring;n vesim&aring;&aring;r&aring;n lisa&aring;ntymis johtuvan samanaikaisesta rasvapitoisuuden v&aring;henemisesta. Rasvapitoisuus laski lokakuun maksimiarvosta 18.9&plusmn;2.6% ruumiinpainosta huhtikuun minimiarvoon, joka oli 0.9&plusmn;2.7% ruumiinpainosta. Kes&aring;ll&aring; rasvapitoisuus lis&aring;antyi puolestaan vesipitoisuuden kustannuksella. Talvella j&aring;k&aring;l&aring;ravinnolla (joulu-huhtikuussa) veden kaytto vaihteli v&aring;lilla 30.8&plusmn;5.2 ja 43.6&plusmn;13.5 ml vrk-1kg-1 mutta se kohosi melkein nelinkertaisesti kesalla (kes&aring;-elokuussa) maksimiarvoonsa 117.7+5.9 ml vrk-1 kg-1 elokuussa. Veden k&aring;yton ja ravinnon oton seka veden k&aring;yton jaymp&aring;riston lampotilan v&aring;lilla oli positiivinen korrelaatio. Viimeksi mainittu korrelaatio voi johtua v&aring;liaikaisesta riippuvuudesta ravinnonoton ja ymp&aring;riston l&aring;mpotilan v&aring;lill&aring;.</p>


1967 ◽  
Vol 18 (6) ◽  
pp. 947 ◽  
Author(s):  
WV Macfarlane ◽  
B Howard ◽  
BD Siebert

During late summer, Border Leicester wethers running with Merinos on a pure Atriplex nummularia stand turned over 10.6 to 17.5 litres (mean 13.7 litres) of water daily, and diluted the sodium and potassium ingested to less than 1000 m-osmoles/litre in the urine. Leicesters used 46% more water than Merinos as litres/24 hr, and 71% more as ml/kg0.82/24 hr. The two breeds produced similar urine concentrations. The sheep showed a wide variation in response, and their individual water turnovers while feeding on Atriplex vesicaria and A. nummularia ranged from 120 to 833 ml/kg0.82/24 hr. This suggests differences in functional types of adjustment to saltbush associations. On a Danthonia community Leicesters again turned over more water than Merinos but only about half as much water was required as on saltbush. Merinos grazing on A. vesicaria (with some grasses available) over 2 years maintained good condition with half the water intake of Merinos on A. nummularia, although the two species of saltbush had similar sodium and potassium contents. Total body water tended to increase with water turnover rate on saltbush. Plasma sodium concentration was inversely related to water turnover, extracellular volume, and total body water on saltbush pastures. The content of extracellular sodium was, however, greatest in the sheep with the least sodium in the food taken.


Author(s):  
Aaron R. Caldwell ◽  
Megan E. Rosa-Caldwell ◽  
Carson Keeter ◽  
Evan C. Johnson ◽  
François Péronnet ◽  
...  

<b><i>Background:</i></b> Debate continues over whether or not individuals with low total water intake (TWI) are in a chronic fluid deficit (i.e., low total body water) [<xref ref-type="bibr" rid="ref1">1</xref>]. When women with habitually low TWI (1.6 ± 0.5 L/day) increased their fluid intake (3.5 ± 0.1 L/day) for 4 days 24-h urine osmolality decreased, but there was no change in body weight, a proxy for total body water (TBW) [<xref ref-type="bibr" rid="ref2">2</xref>]. In a small (<i>n</i> = 5) study of adult men, there were no observable changes in TBW, as measured by bioelectrical impedance, after increasing TWI for 4 weeks [<xref ref-type="bibr" rid="ref3">3</xref>]. However, body weight increased and salivary osmolality decreased indicating that the study may have been underpowered to detect changes in TBW. Further, no studies to date have measured changes in blood volume (BV) when TWI is increased. <b><i>Objectives:</i></b> Therefore, the purpose of this study was to identify individuals with habitually low fluid intake and determine if increasing TWI, for 14 days, resulted in changes in TBW or BV. <b><i>Methods:</i></b> In order to identify individuals with low TWI, 889 healthy adults were screened. Participants with a self-reported TWI less than 1.8 L/day (men) or 1.2 L/day (women), and a 24-h urine osmolality greater than 800 mOsm were included in the intervention phase of the study. For the intervention phase, 15 participants were assigned to the experimental group and 8 participants were assigned to the control group. The intervention period lasted for 14 days and consisted of 2 visits to our laboratory: one before the intervention (baseline) and 14 days into the intervention (14-day follow-up). At these visits, BV was measured using a CO-rebreathe procedure and deuterium oxide (D<sub>2</sub>O) was administered to measure TBW. Urine samples were collected immediately prior, and 3–8 h after the D<sub>2</sub>O dose to allow for equilibration. Prior to each visit, participants collected 24-h urine to measure 24-h hydration status. After the baseline visit, the experimental group increased their TWI to 3.7 L for males and 2.7 L for females in order to meet the current Institute of Medicine recommendations for TWI. <b><i>Results:</i></b> Twenty-four-hour urine osmolality decreased (−438.7 ± 362.1 mOsm; <i>p</i> &#x3c; 0.001) and urine volume increased (1,526 ± 869 mL; <i>p</i> &#x3c; 0.001) in the experimental group from baseline, while there were no differences in osmolality (−74.7 ± 572 mOsm; <i>p</i> = 0.45), or urine volume (−32 ± 1,376 mL; <i>p</i> = 0.89) in the control group. However, there were no changes in BV (Fig. <xref ref-type="fig" rid="f01">1</xref>a) or changes in TBW (Fig. <xref ref-type="fig" rid="f01">1</xref>b) in either group. <b><i>Conclusions:</i></b> Increasing fluid intake in individuals with habitually low TWI increases 24-h urine volume and decreases urine osmolality but does not result in changes in TBW or BV. These findings are in agreement with previous work indicating that TWI interventions lasting 3 days [<xref ref-type="bibr" rid="ref2">2</xref>] to 4 weeks [<xref ref-type="bibr" rid="ref3">3</xref>] do not result in changes in TBW. Current evidence would suggest that the benefits of increasing TWI are not related changes in TBW.


PEDIATRICS ◽  
1962 ◽  
Vol 29 (6) ◽  
pp. 883-889
Author(s):  
Wesley M. Clapp ◽  
L. Joseph Butterfield ◽  
Donough O'Brien

Normal values for both total body water and extracellular water have been determined in 86 premature infants aged 1 to 90 days and weighing 940 to 2,435 gm, with use of the techniques of deuterium oxide and bromide dilution. Nine full-term infants aged 1 to 6 days and weighing 2,590 to 4,985 gm were similarly studied. Nine infants with the respiratory distress syndrome and eight infants of toxemic mothers studied in the first 24 hours of life showed no significant difference in their body water compartments in comparison to a control group of normal infants matched for age and weight. Seven infants of diabetic mothers studied in the first 24 hours of life showed a significant decrease in total body water, expressed as percentage of body weight, with a normal intracellular to extracellular water ratio. These data indirectly support other evidence that there is an increase in body fat in these infants at birth. See Table in the PDF file


1999 ◽  
Vol 45 (7) ◽  
pp. 1077-1081 ◽  
Author(s):  
Graham Jennings ◽  
Leslie Bluck ◽  
Antony Wright ◽  
Marinos Elia

Abstract Background: The conventional method of measuring total body water by the deuterium isotope dilution method uses gas isotope ratio mass spectrometry (IRMS), which is both expensive and time-consuming. We investigated an alternative method, using Fourier transform infrared spectrophotometry (FTIR), which uses less expensive instrumentation and requires little sample preparation. Method: Total body water measurements in human subjects were made by obtaining plasma, saliva, and urine samples before and after oral dosing with 1.5 mol of deuterium oxide. The enrichments of the body fluids were determined from the FTIR spectra in the range 1800–2800 cm−1, using a novel algorithm for estimation of instrumental response, and by IRMS for comparison. Results: The CV (n = 5) for repeat determinations of deuterium oxide in biological fluids and calibrator solutions (400–1000 μmol/mol) was found to be in the range 0.1–0.9%. The use of the novel algorithm instead of the integration routines supplied with the instrument gave at least a threefold increase in precision, and there was no significant difference between the results obtained with FTIR and those obtained with IRMS. Conclusion: This improved infrared method for measuring deuterium enrichment in plasma and saliva requires no sample preparation, is rapid, and has potential value to the clinician.


1969 ◽  
Vol 72 (1) ◽  
pp. 31-40 ◽  
Author(s):  
W. R. McManus ◽  
R. K. Prichard ◽  
Carolyn Baker ◽  
M. V. Petruchenia

SUMMARYThe use of tritiated water to estimate total body-water content of animals experiencing recovery from under-nutrition was studied.The time for equilibration of tritiated water (TOH), given intraperitoneally, with total body water (TBW) was determined in rabbits and in rats. As judged by the specific activity of blood water, equilibration had occurred by 76–125 min in the rabbit and did not appear to be affected by the plane of nutrition. However, between slaughter groups the specific activity of water obtained from the liver 180 min after injection of TOH was significantly different from the specific activity of water simultaneously obtained from the blood plasma. It is concluded that the liver is not a suitable tissue to use for testing achievement of equilibration.As judged by the specific activity of blood water compared to that of water from the whole body macerate, equilibration in mature rats either in stable body condition or undergoing rapid compensatory growth occurred in less than 60 min.A trial comparing TOH-space (corrected by 3% body weight) and actual TBW (by desiccation) was conducted on thirty rabbits which experienced under-nutrition followed by compensatory growth.Prior to under-nutrition the agreement between actual and estimated TBW was satisfactory and within 2·3%. During compensatory growth the agreement was poor— the TOH values over-estimating actual TBW by about 12%.A trial with mature rats confirmed the findings with rabbits. For rats in stable body weight the mean estimated TOH-space for fourteen animals was within 1·2% of the actual TBW. For fourteen rats undergoing compensatory growth the mean estimated TOH-space (corrected by 3% body weight) overestimated actual TBW by 6·2%.


2000 ◽  
Vol 278 (4) ◽  
pp. F585-F595 ◽  
Author(s):  
Martina Heer ◽  
Friedhelm Baisch ◽  
Joachim Kropp ◽  
Rupert Gerzer ◽  
Christian Drummer

A commonly accepted hypothesis is that a chronically high-sodium diet expands extracellular volume and finally reaches a steady state where sodium intake and output are balanced whereas extracellular volume is expanded. However, in a recent study where the main purpose was to investigate the role of natriuretic peptides under day-to-day sodium intake conditions (Heer M, Drummer C, Baisch F, and Gerzer R. Pflügers Arch 425: 390–394, 1993), our laboratory observed increases in plasma volume without any rise in extracellular volume. To scrutinize these results that were observed as a side effect, we performed a controlled, randomized study including 32 healthy male test subjects in a metabolic ward. The NaCl intake ranged from a low level of 50 meq NaCl/day to 200, 400, and 550 meq/day, respectively. Plasma volume dose dependently increased ( P < 0.01), being elevated by 315 ± 37 ml in the 550-meq-NaCl-intake group. However, in contrast to the increased plasma volume, comparable to study I, total body water did not increase. In parallel, body mass also did not increase. Mean corpuscular volume of erythrocytes, as an index for intracellular volume, was also unchanged. We conclude from the results of these two independently conducted studies that under the chosen study conditions, in contrast to present opinions, high sodium intake does not induce total body water storage but induces a relative fluid shift from the interstitial into the intravascular space.


1988 ◽  
Vol 47 (3) ◽  
pp. 435-445 ◽  
Author(s):  
F. R. Dunshea ◽  
A. W. Bell ◽  
K. D. Chandler ◽  
T. E. Trigg

ABSTRACTA two-pool model of tritiated water kinetics was investigated as a means of partitioning total body water into empty body water and gut water in 17 lactating goats. Empty body water, gut water and total body water were of a similar magnitude to, and highly correlated with, a rapidly equilibrating tritiated water pool, a more slowly equilibrating pool and the sum of these two pools, respectively.Empty body fat was poorly correlated with both live weight and empty body weight (R2 = 0·42 and 0·51, respectively). However, there was a strong inverse relationship between the water and fat contents of the empty body. Consequently, empty body fat was accurately predicted by a multiple regression equation which included both empty body weight and empty body water as independent variables (R2 = 0·97). Substitution of these variables with estimates derived from tritiated water kinetics still resulted in a high correlation (R2 = 0·88). Tritiated water kinetics offered little improvement over live weight alone in the prediction of empty body protein, empty body ash or fat-free empty body.


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