Hypotonic, Hypertonic and Isotonic How facilitated diffusion (osmosis) works in different solutions.
Isotonic and hypertonic sodium loading in supine humans
Transcript of Isotonic and hypertonic sodium loading in supine humans
Isotonic and hypertonic sodium loading in supine humans
L . J . A N D E R S E N , 1 T. U. S. J E N S E N , 2 M. H. B E S T L E 1,3 and P . B I E 1
1 Department of Medical Physiology, Panum Institute, University of Copenhagen, Copenhagen, Denmark
2 Danish Aerospace Medical Centre of Research, Rigshospitalet, Copenhagen, Denmark
3 Department of Clinical Physiology, Herlev Hospital, Herlev, Denmark
ABSTRACT
The hypothesis that hypertonic saline infusion induces a greater natriuresis than infusion of the same
amount of sodium as isotonic saline was tested in 8 supine subjects on fixed sodium intake of
150 mmol NaCl day±1. Sodium loads equivalent to the amount of sodium contained in 10% of
measured extracellular volume were administered intravenously over 90 min either as isotonic saline
or as hypertonic saline (850 mmol L±1). A third series without saline infusion served as time control.
Experiments lasted 8 h. Water balance and sodium loads were maintained by replacing the excreted
amounts every hour. Plasma sodium concentrations only increased following hypertonic saline
infusion (by 2.7 � 0.3 mmol L±1). Oncotic pressure decreased signi®cantly more with isotonic saline
(4.1 � 0.3 mmHg) than with hypertonic saline (3.2 � 0.2 mmHg), indicating that isotonic saline
induced a stronger volumetric stimulus. Renal sodium excretion increased more than a factor of four
with isotonic and hypertonic saline but also increased during time control (factor of three). Cumulated
sodium excretions following isotonic (131 � 13 mmol) and hypertonic saline (123 � 10 mmol) were
statistically identical exceeding that of time control (81 � 9 mmol). Plasma angiotensin II decreased
in all series but plasma ANP concentrations and urinary excretion rates of endothelin-1 remained
unchanged. In conclusion, hypertonic saline did not produce excess natriuresis. However, as the two
loading procedures induced similar natriureses during different volumetric stimuli, part of the
natriuresis elicited by hypertonic saline could be mediated by stimulation of osmoreceptors involved
in renal sodium excretion. The supine position does not provide stable time control conditions with
regard to renal excretory function.
Keywords angiotensin II, human subjects, osmoreceptors, sodium homeostasis.
Received 5 October 1998, accepted 12 January 1999
It is generally accepted that renal sodium excretion is
controlled primarily by mechanisms sensitive to chan-
ges in body ¯uid volume. However, in several animal
experiments, infusion of hypertonic saline induces a
natriuretic response that exceeds the response to iso-
tonic saline although the latter is associated with a
greater volumetric stimulus (Emmeluth et al. 1990,
Huang et al. 1995). This excess natriuresis may be in-
duced by stimulation of speci®c osmoreceptors in-
volved in the control of renal sodium excretion
(Thornborough et al. 1973, Zucker & Kaley 1976,
Emmeluth et al. 1992, McKinley et al. 1992). Recently,
we found that an increase in plasma sodium concen-
tration may also contribute to the natriuresis of intra-
venous salt loading in normal seated subjects (Andersen
et al. 1998). However, compared with other species, the
response to hypertonic saline infusion seemed to be
relatively small in humans and osmostimulated nat-
riuresis could only be demonstrated in subjects on high
sodium intake (Andersen et al. 1998). It could be hy-
pothesized that the natriuretic response to hypertonic
saline is dependent on the relative hypervolemia that is
associated with ingestion of a high sodium diet. Ac-
cordingly, sodium depletion inhibits osmostimulated
natriuresis in dogs (Gilmore & Nemeh 19841 ). The
purpose of the present investigation was to further
elucidate osmoregulatory control of sodium excretion
following isotonic and hypertonic salt loading. Subjects
were placed in the supine position. Compared with the
seated position this increases the load to central volume
receptors allowing us to investigate whether this mod-
erate hypervolemia could augment the response to
hypertonic vs. isotonic saline loading. In addition, the
duration of the experiment was extended by 3 h
Correspondence: Lars Juel Andersen, MD, Panum Institute, building 6.5.8, 3 Blegdamsvej, DK-2200 Copenhagen, Denmark.
Acta Physiol Scand 1999, 166, 23±30
Ó 1999 Scandinavian Physiological Society 23
compared with our previous protocol (Andersen et al.
1998).
METHODS
Experiments were performed in eight healthy male
volunteers. Subjects were 24±30 years old, weighing
74.4±85.1 kg. All gave informed consent and the study
was approved by the Ethics Committee of Copenhagen
(j.nr. KF 01±011/96).
Approximately 2 weeks prior to the experiments,
each subject's extracellular volume (ECV) was deter-
mined as the distribution volume of [51Cr] EDTA
according to the method described by Brùchner-Mor-
tensen (1982). Brie¯y, 3.5 MBq of [51Cr] EDTA was
injected intravenously and four venous samples were
drawn 180, 200, 220 and 240 min after injection. ECV
measurements and all experiments were performed af-
ter subjects had been on a controlled diet containing
150 mmol NaCl day±1 for 4 days. Sodium turnover
was veri®ed by measuring 24 h urinary sodium excre-
tion the day before the experiment.
The night before the experiment the subject slept at
the laboratory. At 07.00 hours he was awakened and
consumed a light standardized low-salt breakfast (3
slices of toast, 15 g marmalade, and 500 mL of tap
water). The subject was instrumented with two cathe-
ters (Ven¯on, 18 gauge) in super®cial cubital veins for
blood sampling and infusion of saline. After the in-
sertion of the catheters, the subject emptied his bladder
and was weighed. The subject remained supine
throughout the study and was allowed to stand up only
for micturition. The degree of hydration was main-
tained throughout the experiment by drinking of water
in amounts equal to those voided plus 1 mL min±1 as
replacement for the insensible2 water loss. Thirst
sensation was not monitored. Room temperature was
kept around 24 °C.
Each experiment lasted 8 h. After 1 h of baseline,
saline was infused over the following 90 min. After
infusion, sampling continued for another 5� h. Two
series of infusion plus time control were performed on
separate days. In one infusion series (ISOT), a salt load
was infused as 0.9% saline in amounts equal to 10% of
measured ECV, i.e. a load of 1.44 � 0.01 L of isotonic
saline. In the other infusion series (HYPR), an identical
amount of sodium was infused as a 5% solution
(0.26 � 0.01 L of 5% saline). Infusions were adminis-
tered by an automatic infusion pump (LifeCareÒPump, Model 4, Abbott, Ill, USA3 ). The time control
series (CONTR) was identical to infusion series, but
without saline infusion. At least 2 weeks of recovery
were allowed between each experiment.
Urine was collected by voluntary micturition during
the last minute of every hour. After each urine collec-
tion, urinary concentration of sodium was measured and
the excreted amount of sodium was replaced by i.v.
injection of isotonic saline at the beginning of the sub-
sequent period in order to maintain the sodium load.
The injected volume was subtracted from the volume of
water administered orally to maintain hydration status.
Blood (12 mL) was sampled in heparinized tubes at
the beginning and the end of the baseline period, and in
the middle of every remaining 1-h period for mea-
surements of sodium, osmolality, haematocrit, protein
and oncotic pressure. Baseline values are presented as
the mean of the ®rst two blood samples. Additional
blood samples for hormone analyses (20 mL) were
collected in prechilled polyethylene tubes containing
aprotinine (300 KIU mL±1) and EDTA (3 lmol mL±1)
during baseline and in the middle of period 2, 4, 6 and 8.
The withdrawn blood was replaced by twice the
amount of saline. Blood samples were centrifuged at
+4 °C and plasma was stored at )18 °C until analysed
for concentrations of angiotensin II (ANG II) and atrial
natriuretic peptide (ANP).
Haematocrit was determined by centrifugation4 .
Oncotic pressure was determined by a colloid osmo-
meter (4400 Colloid Osmometer, Wescor, Utah, USA5 ).
A SMAC3 instrument (Bayer) was used to measure
haemoglobin and plasma protein concentrations. Urine
and plasma sodium concentrations were measured by
an ion-selective electrode system (KNA-2, Radiometer)
and osmolality by freezing-point depression (model
3DII, Advanced Instruments, MA, USA6 ).
Arterial systolic and diastolic pressures were re-
corded semiautomatically four times every hour
(Propaq 102, Protocol Systems Inc., Or, USA7 ) and
the mean of these values were used to calculate
mean arterial pressure (MAP) from the formula:
MAP � diastolic pressure + 1/3 ´ pulse pressure.
Hormone concentrations in plasma and urine sam-
ples were quanti®ed by radioimmunoassays after ex-
traction. Thawed samples were acidi®ed with 4% acetic
acid and peptides were extracted by use of C18 Sep-Pak
cartridges (Waters, MA, USA8 ), as previously described
(Emmeluth et al. 1994). After elution, the samples were
dried and stored at )18 °C in tubes topped with N2
until analysis for hormone immunoreactivity. ANP was
determined according to the assay procedure described
earlier (SchuÈtten et al. 1987) by use of an antibody
(RAS8798) purchased from Peninsula Laboratories9 ,
CA, USA. Extraction recovery was 85%. Detection
limit was 1.5 pg mL±1 sample. Intra-assay coef®cient of
variation was 6%. Immunoreactivity of ANG II was
determined by use of an antibody (Ab-5±030682)
produced by P. Christensen10 . The assay procedure has
been described by Kappelgaard et al. 197611 ). Extraction
recovery was 85%. Detection limit was 1.4 pg mL±1
sample. Intra-assay coef®cient of variation was 5%. The
Osmostimulated sodium excretion á L J Andersen et al. Acta Physiol Scand 1999, 166, 23±30
24 Ó 1999 Scandinavian Physiological Society
procedure for measuring endothelin-1 concentrations
in extracted urine samples has previously been de-
scribed (Emmeluth et al. 1992). The detection limit was
0.16 pg mL±1 urine and extraction recovery was 91%.
Intra-assay and inter-assay coef®cients of variation were
5.2% and 6.5%, respectively. Hormone results have not
been corrected for incomplete recovery. Measurements
of plasma concentrations of arginine vasopressin failed
for technical reasons.
Statistics
Results are presented as mean � SE. Data were sub-
jected to one-way analysis of variance (ANOVA) for re-
peated measures (Winer 1971). In case of signi®cantly
large F-values, all possible differences were evaluated
by Newman±Keuls' test. Selected differences between
series were evaluated using paired Student's t-test. Level
of signi®cance was in all cases 0.05.
RESULTS
Subjects ECV ranged between 13.9 and 14.8 L with a
mean of 14.4 � 0.1 L (18.1 � 0.2% of body wt.).
Twenty-four hour sodium excretion was 147 �
12 mmol during the last day of controlled sodium intake.
Plasma sodium concentration and osmolality in-
creased during HYPR and peaked immediately after
end of infusion (from 139.2 � 0.3 to 141.9 � 0.3
mmol L±1 and from 289.9 � 1.3 to 293.3 � 1.1 mos-
mol L±1, respectively). Plasma sodium concentration
remained signi®cantly elevated throughout the obser-
vation period although values decreased after end of
infusion (Fig. 1). Plasma osmolality decreased during
the recovery period to values not signi®cantly different
from the preinfusion value (Table 1). However, plasma
osmolality also decreased during CONTR and ISOT
and the average plasma sodium concentration and
Figure 1 Plasma concentration of sodium. Values are mean � SE.
e: control; n: isotonic saline infusion; d: hypertonic saline infusion.
Values marked with * are signi®cantly different from the pre-infusion
value by ANOVA (P < 0.05) and Newman±Keuls' test.
Table 1 Plasma osmolality, plasma protein, oncotic pressure and haemotocrit
Sampling time, minutes after the start of urine sampling
Period, no 1 2 3 4 5 6 7 8
Time, min 30 90 150 210 270 330 390 450
Plasma osmolality,mosmol kg±1 H2O
CONTR 289.3 � 0.7 287.2 � 1.0* 286.0 � 1.0 285.8 � 0.6* 285.3 � 0.6* 284.8 � 1.1* 284.3 � 0.7* 283.3 � 0.7*
ISOT 287.5 � 0.6 287.4 � 0.8 285.1 � 0.9* 285.5 � 0.6* 285.6 � 0.9* 285.8 � 0.9* 285.5 � 1.1* 284.5 � 0.7*
HYPR 289.9 � 1.3 292.3 � 1.4 293.3 � 1.1* 291.8 � 0.8 290.4 � 1.3 290.4 � 1.1 290.3 � 1.0 290.6 � 1.2
Plasma protein concentration, g L±1
CONTR 66.3 � 1.0 65.3 � 1.0 65.7 � 0.9 65.8 � 0.8 64.8 � 0.8 64.8 � 0.8 64.2 � 0.7* 64.7 � 0.8
ISOT 66.3 � 1.1 62.5 � 1.1* 59.0 � 0.9* 61.1 � 1.1* 62.1 � 0.8* 60.3 � 1.1* 60.4 � 1.2* 61.0 � 0.9*
HYPR 66.4 � 0.9 63.5 � 0.9* 60.4 � 0.9* 61.8 � 0.9* 62.5 � 0.7* 60.8 � 0.9* 61.1 � 0.6* 61.0 � 0.6*
Oncotic pressure, mmHg
CONTR 24.7 � 0.3 24.3 � 0.3 24.3 � 0.2 24.5 � 0.3 23.8 � 0.3* 23.9 � 0.4* 23.5 � 0.2* 23.8 � 0.3*
ISOT 24.7 � 0.4 22.4 � 0.5* 20.5 � 0.4* 21.4 � 0.3* 21.9 � 0.4* 21.2 � 0.4* 21.0 � 0.3* 21.0v0.4*
HYPR 24.5 � 0.3 23.0 � 0.2* 21.4 � 0.2* 22.1 � 0.2* 22.3 � 0.3* 21.6 � 0.3* 21.6 � 0.2* 21.6 � 0.3*
Haematocrit, %
CONTR 43.2 � 0.8 42.4 � 0.9* 42.6 � 0.9* 42.8 � 1.0 42.3 � 0.8* 42.3 � 0.9* 41.8 � 0.8* 41.8 � 0.9*
ISOT 44.0 � 0.9 42.0 � 1.1* 40.7 � 1.0* 40.6 � 1.0* 41.3 � 1.0* 40.8 � 1.1* 40.8 � 1.1* 40.9 � 1.1*
HYPR 44.3 � 0.8 42.8 � 1.0* 41.3 � 0.9* 41.4 � 0.9* 41.8 � 0.9* 41.4 � 1.0* 41.2 � 1.0* 41.3 � 1.0*
Values are mean � SE. isotonic (ISOT) or hypertonic (HYPR) saline was infused intravenously between 60 and 150 min. Results marked with *
are signi®cantly different from period 1 (P < 0.05) by analysis of variance and Newman±Keuls' test.
Ó 1999 Scandinavian Physiological Society 25
Acta Physiol Scand 1999, 166, 23±30 L J Andersen et al. � Osmostimulated sodium excretion
osmolality from 120 to 480 min was signi®cantly higher
during HYPR than during the two other series.
Plasma oncotic pressure, plasma protein and ha-
ematocrit decreased immediately after start of saline in-
fusions (Table 1 and Fig. 2). These decreases were more
pronounced during ISOT than during HYPR. The mean
decrease in oncotic pressure during ISOT from period 3±
8 was to 85.9 � 0.8% of basal which was a signi®cantly
greater reduction than during HYPR (89.0 � 0.6%).
During CONTR, haematocrit also decreased signi®-
cantly but to a smaller extent than during ISOT and
HYPR. Oncotic pressure and plasma protein also de-
creased in the latter observation periods (Table 1).
Sodium excretion increased in all experimental series,
including CONTR during which sodium excretion in-
creased gradually throughout the experiment from a
baseline of 82 � 15 to 256 � 12 lmol min±1 (Fig. 3).
During the ®rst 4 h, hypertonic and isotonic saline in-
fusion induced very similar natriuretic responses
(84 � 10 to 306 � 28 lmol min±1 and 99 � 19 to
300 � 31 lmol min±1, respectively). By the end of the
observation, the natriuresis following isotonic saline
exceeded that following hypertonic saline (414 � 29 vs.
349 � 33 lmol min±1). However, the cumulative sodi-
um excretion during ISOT (131 � 13 mmol) was not
statistically different from that observed during HYPR
(123 � 10 mmol). The responses to both infusion series
exceeded that of the CONTR series (81 � 9 mmol).
Urine ¯ow increased gradually during CONTR from
2.7 � 0.4 to 6.2 � 0.6 mL min±1 observed in the last
experimental period. Urine ¯ow also increased during
ISOT from 2.4 � 0.5 to 10.6 � 0.4 mL min±1 but de-
creased from 2.4 � 0.5 to 1.8 � 0.3 mL min±1 during
HYPR (Fig. 4). Free water clearance followed the same
pattern as urine ¯ow with increases from )0.2 � 0.4 to
2.8 � 0.6 mL min±1 and from )0.5 � 0.3 to 6.0 � 0.4
mL min±1 during CONTR and ISOT, respectively, and
a decrease from 0.2 � 0.4 to )2.3 � 0.1 mL min±1
during HYPR.
A marginal increase in mean arterial pressure and
diastolic blood pressure was observed in the very last
period of observation during ISOT (Table 2). Diastolic
arterial blood pressure also increased slightly but sig-
ni®cantly during CONTR whereas no changes were
observed during HYPR. Systolic arterial blood pressure
remained unchanged in all series. Heart rate tended to
decrease but this was only signi®cant during CONTR
Figure 2 Relative change in plasma oncotic pressure. Values are
mean � SE. e: control; j: isotonic saline infusion; d: hypertonic
saline infusion. Values marked with * are signi®cantly different from
the preinfusion value by ANOVA (P < 0.05) and Newman±Keuls' test.
Figure 3 Renal sodium excretion. Values are mean � SE. e: control;
j: isotonic saline infusion; d: hypertonic saline infusion. Values
marked with * are signi®cantly different from the preinfusion value by
ANOVA (P < 0.05) and Newman±Keuls' test. Values marked with #
are signi®cantly different from corresponding value in the hypertonic
saline series by Student's t-test (P < 0.05).
Figure 4 Urine ¯ow. Values are mean � SE. e: control; j: isotonic
saline infusion; d: hypertonic saline infusion. Values marked with *
are signi®cantly different from the preinfusion value by ANOVA
(P < 0.05) and Newman±Keuls' test.
26 Ó 1999 Scandinavian Physiological Society
Osmostimulated sodium excretion á L J Andersen et al. Acta Physiol Scand 1999, 166, 23±30
and HYPR. Creatinine clearance did not change mea-
surably in any of the series (Table 2).
Basal plasma concentrations of ANG II varied be-
tween series (Table 3). Samples were not measured in
the same assay, which may explain at least some of this
variation. However, the relative changes seem com-
patible (Fig. 5). From period 4 to 8, mean plasma ANG
II had decreased to 24 � 6, 27 � 5 and 61 � 6% of
preinfusion levels during ISOT, HYPR and CONTR,
respectively.
Basal plasma concentration of ANP varied between
30 � 3 and 36 � 3 pg mL±1 and remained unchanged
in all series (Table 3). Urinary excretion rates of en-
dothelin-1 varied between 18 � 3 and 23 � 3 pg min±1
and also remained statistically unchanged in all series
(Table 3).
Table 2 Haemodynamic variables and creatinine clearance
Sampling time, minutes after the start of urine sampling
Period, no 1 2 3 4 5 6 7 8
Time, min 30 90 150 210 270 330 390 450
Mean arterial blood pressure, mmHg
CONTR 80 � 2 81 � 2 82 � 2 82 � 2 81 � 2 80 � 2 82 � 2 83 � 2
ISOT 81 � 2 81 � 2 83 � 2 84 � 3 84 � 2 83 � 2 84 � 2 86 � 3*
HYPR 84 � 3 86 � 2 85 � 2 82 � 2 82 � 2 83 � 2 84 � 3 85 � 2
Systolic blood pressure, mmHg
CONTR 116 � 4 117 � 4 117 � 4 118 � 3 114 � 4 115 �4 117 � 4 118 � 4
ISOT 117 � 3 115 � 5 115 � 4 117 � 3 117 � 3 115 � 3 117 � 3 117 � 3
HYPR 120 � 4 120 � 4 120 � 3 116 � 3 117 � 3 118 � 3 120 � 3 120 � 2
Diastolic blood pressure, mmHg
CONTR 61 � 2 62 � 2 65 � 2 65 � 2* 65 � 1* 63 � 1 64 � 2 65 � 2*
ISOT 63 � 2 64 � 2 67 � 2 67 � 2 68 � 2 67 � 2 68 � 2 70 � 3
HYPR 65 � 3 68 � 2 68 � 2 64 � 2 65 � 2 65 � 2 66 � 3 67 � 2
Heart rate, beats min±1
CONTR 58 � 3 58 � 4 56 � 3 56 � 3 54 � 2* 53 � 3* 54 � 3* 52 � 2*
ISOT 57 � 3 56 � 3 55 � 3 57 � 4 53 � 2 53 � 2 52 � 3 52 � 2
HYPR 56 � 3 58 � 3 56 � 3 55 � 3 54 � 3 53 � 3 51 � 3* 51 � 3*
Creatinine clearance, mL min±1
CONTR 152 � 9 145 � 7 145 � 15 137 � 2 132 � 2 142 � 6 128 � 9 138 � 9
ISOT 158 � 8 144 � 7 154 � 13 152 � 9 150 � 9 152 � 10 147 � 8 140 � 11
HYPR 154 � 9 132 � 2 154 � 3 144 � 7 152 � 7 132 � 4 137 � 3 147 � 5
Values are mean � SE. isotonic (ISOT) or hypertonic (HYPR) saline was infused intravenously between 60 and 150 min. Results marked with *
are signi®cantly different from period 1 (P < 0.05) by analysis of variance and Newman±Keuls' test.
Table 3 Plasma hormone concentrations and urinary excretion rate of endothelin-1
Sampling time, min after the start of urine sampling
Period, no 1 2 4 6 8
Time, min 30 90 210 330 450
Plasma ANG II, pg ml)1
CONTR 14.2 � 3.0 11.2 � 2.6 9.3 � 2.7* 9.5 � 2.3* 9.9 � 2.7*
ISOT 6.4 � 1.3 3.8 � 1.1* 1.7 � 0.4* 1.2 � 0.3* 1.4 � 0.3*
HYPR 8.3 � 1.8 5.9 � 0.9* 3.0 � 1.0* 2.1 � 0.7* 2.5 � 0.8*
Plasma ANP, pg ml)1
CONTR 36 � 3 35 � 3 35 � 3 31 � 3 30 � 3
ISOT 30 � 6 28 � 2 35 � 3 32 � 3 31 � 3
HYPR 34 � 3 34 � 3 36 � 3 32 � 3 33 � 2
Urinary excretion rate of endothelin-1, pg min)1
CONTR 18 � 3 19 � 2 16 � 2 19 � 2 23 � 4
ISOT 18 � 3 14 � 2 13 � 2 15 � 3 51 � 25
HYPR 23 � 3 27 � 2 24 � 5 30 � 3 26 � 3
Values are means � SE. Isotonic (ISOT) or hypertonic (HYPR) saline was infused intravenously between 60 and 90 min. Results marked with *
are signi®cantly different from period 1 (P < 0.05) by analysis of variance and Newman Keuls test.
Ó 1999 Scandinavian Physiological Society 27
Acta Physiol Scand 1999, 166, 23±30 L J Andersen et al. � Osmostimulated sodium excretion
DISCUSSION
We compared the natriuretic responses to hypertonic
vs. isotonic saline infusion in normal supine subjects to
elucidate the effect of osmostimulation on the renal
handling of an acute sodium load. Experiments were
performed under well-de®ned and strictly controlled
conditions with regard to sodium status, individual
adjustment of dosage, and replacement of water and
salt losses throughout the study.
Stimulation of osmoreceptors
As expected, plasma sodium concentration and plasma
osmolality increased immediately after the start of in-
fusion of hypertonic saline and peaked by the end of
infusion (Fig. 1). The next 2 h plasma sodium con-
centration and osmolality decreased somewhat al-
though the excreted amounts of sodium were replaced
intravenously period by period throughout the experi-
ments. Probably, the load was not evenly distributed
throughout the ECV immediately after administration
but 2 h seems to be an unexpected long time for
reaching equilibrium. According to previous ®ndings in
normal subjects by Watenpaugh et al. (1992), a rapidly
administered intravenous salt load is evenly distributed
throughout ECV in less than 60 min. Slower trans-
portation of sodium to other compartments, e.g. the
intestines could be responsible for the fall in plasma
sodium after stop of infusion but this cannot be de-
termined from the present data. At any rate, plasma
sodium concentration remained higher than that ob-
served during CONTR and ISOT and only during
HYPR could osmoreceptors be stimulated as a conse-
quence of the loading procedure.
Stimulation of volume receptors
The decreases in oncotic pressure indicate that isotonic
saline induced a greater increase in plasma volume than
hypertonic saline. Accordingly, the stimulus to central
volume receptors should be greater during ISOT than
during HYPR. This notion is supported by our recent
®ndings in normal subjects, where similar isotonic saline
infusions indeed induced increases in central venous
pressure (CVP) and plasma volume that were signi®-
cantly higher than those induced by 5% saline (Ander-
sen et al. 1998). Changing body position to supine may
alter the CVP responses to salt loading. However, the
larger increase in CVP following isotonic saline was
independent of the initial sodium status of the subject
and therefore maintained at different levels of central
blood volume. Schrier et al. (1969) also found a greater
expansion of plasma volume and ECV when a given salt
load was infused as isotonic saline compared with 5%
saline. Thus, there are several lines of evidence in favour
of the notion that the salt loading induced a stronger
volumetric stimulus during ISOT than during HYPR.
Natriuretic responses to salt loading
Provided that volumetric stimuli dominate over os-
motic stimuli in the control of renal sodium excretion,
ISOT should be associated with a more pronounced
natriuresis than HYPR. However, the ®rst 4 h after
start of infusion, the natriuretic responses during
HYPR and ISOT were very similar. Therefore, we
suggest that part of the natriuresis during HYPR was
mediated by the increase in plasma sodium concentra-
tion and this increase was suf®cient to compensate for
the difference in the volumetric loads in the two series.
During the last 2 h of observation the natriuresis of
ISOT did exceed that of HYPR. But at this time plasma
sodium concentration had decreased somewhat to-
wards control values, which may explain the relative
decrease in sodium excretion by the end of HYPR. In
dogs, the excess natriuresis following hypertonic vs.
isotonic saline loading has been shown to decline after
end of infusion even in cases when plasma sodium
concentration remained elevated (Emmeluth et al.
1990). Unfortunately, most other animal studies on
osmostimulation and sodium handling have been ter-
minated shortly after end of infusion, making it im-
possible to evaluate the time frame of the natriuretic
responses to hypertonic vs. isotonic salt loading
(Emmeluth et al. 1992, 1994, 1996, Huang et al. 1995).
Very recently we demonstrated that isotonic and
hypertonic saline loading induced identical natriuretic
responses in seated subjects on high sodium intake. In
contrast the response to isotonic saline exceeded the
response to hypertonic saline in the same subjects when
they were on low sodium diet (Andersen et al. 1998).
Figure 5 Relative change in plasma angiotensin II concentration.
Values are mean � SE. e: control; j: isotonic saline infusion; d:
hypertonic saline infusion. Values marked with * are signi®cantly
different from the preinfusion value by ANOVA (P < 0.05) and
Newman±Keuls' test.
28 Ó 1999 Scandinavian Physiological Society
Osmostimulated sodium excretion á L J Andersen et al. Acta Physiol Scand 1999, 166, 23±30
Thus, the responses to salt loading in these supine
subjects are qualitatively similar to those observed in
seated subjects on high sodium intake. The modest
central hypervolemia associated with the supine posi-
tion may have potentiated the response to hypertonic
saline infusion compared with the response in seated
subjects on low sodium intake. It is remarkable how a
change in posture from seated to supine has a profound
effect on renal excretory function during time control
conditions. Renal sodium excretion increased substan-
tially during CONT and the supine position does
therefore not provide a steady-state situation. In con-
trast, the seated position appears to provide very stable
conditions over several hours without regard to hae-
modynamic, humoral and renal excretory functions
(Andersen et al. 1998). These ®ndings emphasize the
importance of the inclusion of a time control series.
Alternatively, the supine position should be avoided in
acute studies of water and electrolyte homeostasis.
In several animal models, the natriuresis following
hypertonic infusion has been found to exceed that
following isotonic or hypotonic infusion by a factor of
2±5 (Childers & Schneider 1981, Emmeluth et al. 1990,
Huang et al. 1995) even when protocols are very similar
to the present one (e.g. Emmeluth et al. 1990). How-
ever, infusion of hypertonic saline has also failed to
induce excess natriuresis in one study on dogs (Schrier
et al. 1969). Papper et al. found that hypertonic and
isotonic saline infusion induced similar natriuretic re-
sponses in supine subjects even when the hypertonic
infusion increased plasma sodium concentration more
than 8 mmol L±1 (Papper et al. 195612 ). The absence of
excess natriuretic responses following hypertonic
loading in humans indicates that the operational range
of osmostimulated natriuresis in humans is smaller than
that observed in other species.
Natriuretic mechanisms
Osmostimulated natriuresis is probably mediated by a
humoral signal as renal denervation does not abolish
the response to central osmostimulation (Emmeluth
et al. 1996). However, the efferent signal to the kidney
is not yet identi®ed.
Plasma ANG II decreased by 82% and 74% during
ISOT and HYPR, respectively. In seated subjects re-
ceiving similar salt loads, plasma ANG II only de-
creased by » 40±50% (Andersen et al. 1998). The
somewhat greater suppression of ANG II observed in
the present study may be explained by the different
body positions of the subjects during the two sets of
investigations. Plasma ANG II decreased by some 33%
during CONTR whereas plasma levels remained un-
changed during time control in the seated subjects.
Corrected for these differences, the effect of a given
salt load on the suppression of ANG II seems sur-
prisingly constant. If ANG II is maintained at high
levels by exogenous administration during saline infu-
sion in humans (Singer et al. 1994) and dogs (Andersen
et al. 1998, abstract) the natriuresis is markedly inhib-
ited. Together, these ®ndings strongly indicate that a
decrease in plasma ANG II is a necessary condition for
the natriuresis of salt loading and ANG II may be the
main controller of sodium excretion in response to salt
loading as well as to changes in posture.
In contrast, plasma ANP remained unchanged in all
series. Apparently, the relative slow infusion rate did
not provide a volumetric stimulus that was powerful
enough to stimulate ANP secretion, not even during
ISOT. Similarly, plasma ANP was unaffected by
hypertonic as well as isotonic salt loading in seated
subjects (Andersen et al. 1998).
Endothelin-1 has been found to be natriuretic in
small doses in dogs (Sandgaard & Bie 1996) and the
urinary excretion rate of endothelin-1 is increased
with increasing sodium excretion following stimula-
tion of central osmoreceptors suggesting that en-
dothelin-1 may be involved in the natriuresis of
osmostimulation (Emmeluth et al. 1996). However,
urinary excretion of endothelin-1 did not change
measurably in the present study and it is unlikely that
the observed changes in sodium excretion were in-
duced by endothelin-1.
The changes in urine ¯ow and free water clearance
indicate that plasma vasopressin decreased during
CONTR and ISOT but increased during HYPR. This
notion is also supported by previous ®ndings in seated
subjects (Andersen et al. 1998). Although vasopressin is
involved primarily in water balance it may have some
antinatriuretic effect in humans (Andersen et al. 1990).
It is therefore possible that some of the natriuresis
during ISOT and CONTR could be contributed to a
fall in plasma AVP. Similarly, increased plasma vaso-
pressin may have prevented an excess natriuresis during
HYPR.
Haemodilution has been shown to be a potent
natriuretic stimulus, and this may contribute to the
natriuresis observed in all series (Johansen et al. 1997).
To what extent haemodilution has a direct renal effect
or acts through changes in for example ANG II is
unknown. At any rate, the haemodilution seemed more
pronounced during ISOT, which should augment an
excess natriuresis in response to isotonic saline. The
increases in blood pressure during CONT and by the
end of ISOT were less than 5 mmHg and we ®nd it
highly unlikely that natriuresis occurred as a conse-
quence of this minute increase in blood pressure. There
were no signi®cant changes in creatinine clearance, but
this parameter is not a very precise estimate of glo-
merular ®ltration rate in humans.
Ó 1999 Scandinavian Physiological Society 29
Acta Physiol Scand 1999, 166, 23±30 L J Andersen et al. � Osmostimulated sodium excretion
SUMMARY
The supine position did not provide a stable base line
situation with regard to renal salt and water excretion.
The natriureses seen in response to hypertonic and
isotonic saline infusion were very similar over the ®rst
5 h despite indications that isotonic saline provides a
stronger volumetric stimulus than hypertonic saline.
Consequently, it is suggested that part of the natriuresis
following hypertonic saline was mediated by the in-
crease in plasma concentration of sodium. The re-
sponses were very similar to those previously found in
seated subjects on high sodium intake. Unlike many
animal experiments, the natriuresis following hypertonic
infusion did not exceed that following isotonic saline
and the operational range of osmostimulated natriuresis
in humans appears smaller than seen in other species.
The natriuresis occurring in all series may be mediated
by decreases in plasma ANG II concentration but not
by plasma ANP or urinary levels of endothelin-1.
The authors thank Bodil Svenson, Birthe Lynderup Christensen,
Sigurd Kramer Hansen, Inge Pedersen, Barbara Sùrensen, and Trine
Eidsvold for expert technical assistance. We also wish to thank
Dr Steen Levin Nielsen for expert assistance in calculations of
subjects extracellular volume. The experiments were supported by
The Danish Medical Research Council, Danish Foundation for the
Advancement of Medical Science, Kong Christian den Tiendes
Foundation, Engineer August Frederik Wedell Erichsens Foundation,
Direktùr Jacob Madsens & Hustru Olga Madsens Foundation, and
The Danish Heart Foundation.
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30 Ó 1999 Scandinavian Physiological Society
Osmostimulated sodium excretion á L J Andersen et al. Acta Physiol Scand 1999, 166, 23±30