2 Water travels freely across the cell membranes of most parts of the body. The
cell membrane, however, is only selectively permeable to solutes. The impermeable
solutes are osmotically active and can exert an osmotic pressure that dictates the
distribution of water between fluid compartments. Water moves across the cell
membrane from a region of low osmolality to one of high osmolality. Net water
movement ceases when osmotic equilibrium occurs. Each fluid compartment contains
a major osmotically active solute: potassium in the intracellular space and sodium in
the ECF. The volumes of the two compartments reflect the asymmetrically larger
number of solute particles or osmoles inside the cells.
The capillary wall separates the interstitial fluid from plasma. Because sodium
moves freely across the capillary wall, its concentration is identical across both
sides of the wall. Therefore, no osmotic gradient is generated, and water distribution
between these two spaces is not affected. Plasma proteins, which are confined in the
vascular space, are the primary osmoles that affect water distribution between the
In contrast, urea, which traverses both the capillary
walls and most cell membranes, is osmotically inactive.
Osmolality is defined as the number of particles per kilogram of water (mOsm/kg). It
is determined by the number of particles in solution and not by particle size or
valence. Nondissociable solutes, such as glucose and albumin, generate 1
mOsm/mmol of particles; and dissociable salts, such as sodium chloride, liberate
two ions in solution to produce 2 mOsm/mmol of salt. The osmolality of body fluid is
maintained between 280 and 295 mOsm/kg. Because all body fluid compartments are
iso-osmotic, plasma osmolality reflects the osmolality of total body water. Plasma
osmolality can be measured by the freezing point depression method, or estimated by
the following equation, which takes into account the osmotic effect of sodium,
This equation predicts the measured plasma osmolality within 5 to 10 mOsm/kg.
Although urea contributes to the measured osmolality, it is an ineffective osmole
because it readily traverses cell membranes and, therefore, does not cause significant
fluid shift within the body. Hence, the effective plasma osmolality (synonymous with
tonicity, the portion of total osmolality that has the potential to induce transmembrane
water movement) can be estimated by the following equation:
An osmolal gap exists when the measured and calculated values differ by greater
; it signifies the presence of unidentified particles. When the
individual solute has been identified, its contribution to the measured osmolality can
be estimated by dividing its concentration (mg/dL) by one-tenth of its molecular
weight. Calculating the osmolal gap is used to detect the presence of substances, such
as ethanol, methanol, and ethylene glycol, that have high osmolality. Occasionally,
the osmolal gap can also result from an artificial decrease in the serum sodium
secondary to severe hyperlipidemia or hyperproteinemia.
Routine laboratory analysis reveals the following:
Blood urea nitrogen (BUN), 10 mg/dL
The blood methanol concentration was 108 mg/dL, and the measured plasma osmolality was 333 mOsm/kg.
What is J.F.’s calculated osmolality? Are other unidentified osmoles present?
Using Equation 27-1, J.F.’s total calculated osmolality is
In J.F., the entire osmolal gap can be accounted for by the presence of the methanol
(because 108 mg/dL of methanol will provide 108/3.2 = 33.7 mOsm/kg). It is
unlikely, therefore, that other unmeasured osmoles are present (e.g., ethylene glycol,
isopropanol, and ethanol). The laboratory determination of osmolality measures the
total number of osmotically active particles but not their permeability across the cell
membrane. Methanol increases plasma osmolality but not tonicity because the cell
membrane is permeable to methanol. Therefore, no net water shift occurs between the
intracellular and extracellular compartments. Conversely, mannitol, which is
confined to the extracellular space, contributes to both plasma osmolality and
The kidney plays an important role in maintaining a constant extracellular
environment by regulating the excretion of water and various electrolytes. The
volume and composition of fluid filtered across the glomerulus are modified as the
fluid passes through the tubules of the nephron.
The renal tubule is composed of a series of segments with heterogeneous structures
and functions: the proximal tubule, the medullary and cortical thick ascending limb of
Henle’s loop, the distal convoluted tubule, and the cortical and medullary collecting
(Fig. 27-1). The mechanism for sodium reabsorption is different for each
nephron segment, but it is generally mediated by carrier proteins or channels located
on the luminal membrane of the tubule cell.
adenosine triphosphatase) actively pumps sodium out of the renal tubule cell in
exchange for potassium in a 3:2 ratio. Hence, the intracellular sodium concentration
is kept at a low level. The potassium that is pumped into the cell leaks back out
through potassium channels in the membrane, rendering the cell interior
electronegative. The low intracellular sodium concentration and a negative
intracellular potential produce a favorable gradient for passive sodium entry into the
/K+ ATPase also indirectly provides the energy for active sodium transport
and the reabsorption and secretion of other solutes across the luminal membrane of
the renal tubule. The distal segments are mainly involved in the reabsorption of
sodium and chloride ions and the secretion of hydrogen and potassium ions.
Disorders of Fluid and Electrolyte Metabolism. 5th ed. New York, NY: McGraw-Hill; 1994:545.)
Iso-osmotic reabsorption of the glomerular filtrate occurs in the proximal tubule
such that two-thirds of the filtered sodium and water and 90% of the filtered
bicarbonate are reabsorbed. The Na
/H+ antiporter (exchanger) in the luminal
membrane is instrumental in the reabsorption of sodium chloride, sodium
bicarbonate, and water. The reabsorption of most nonelectrolyte solutes, such as
glucose, amino acids, and phosphates, are coupled to sodium transport.
Both the thick ascending limb of Henle’s loop and the distal convoluted tubule
serve as the diluting segments of the nephron because they are impermeable to water.
Sodium chloride is extracted from the filtrate without water. Sodium transport in both
of these segments is flow-dependent and varies with the amount of sodium ions
delivered from the proximal segments of the nephron. Decreased sodium ions in the
tubular fluid will limit sodium transport in the thick ascending limb of Henle’s loop
and the distal convoluted tubule.
Reabsorption of sodium in the thick ascending limb of Henle’s loop accounts for
approximately 25% of the total sodium reabsorption. Sodium, chloride, and
potassium are reabsorbed by the medullary and cortical portions of the ascending
limb, but the leakage of reabsorbed potassium ions back into the tubular lumen, via
potassium channels, makes the tubular lumen electropositive. This electrical gradient
promotes the passive reabsorption of cations, such as sodium, calcium, and
magnesium, in the distal convoluted tubules. Because the thick ascending limb of
Henle’s loop is impermeable to water, it contributes to the interstitial osmolality in
the medulla. This high osmolality is key to the reabsorption of water by the medullary
portion of the collecting duct under the influence of antidiuretic hormone (ADH,
vasopressin). Therefore, the thick ascending limb of Henle’s loop is important for
both urinary concentration and dilution.
Because, as noted previously, the distal convoluted tubule is also impermeable to
water, the osmolality of the filtrate continues to decline as sodium is being
reabsorbed. In the distal convoluted tubule and collecting duct, sodium is reabsorbed
in exchange for hydrogen ions and potassium. When sodium ions are reabsorbed, the
tubule lumen becomes electronegative, which promotes potassium secretion in the
lumen via potassium channels. Aldosterone enhances sodium reabsorption in the
collecting duct by increasing the number of opened sodium channels.
The collecting duct is usually impermeable to water. Under the influence of ADH,
however, water permeability is increased through an increase in the number of water
channels along the luminal membrane. The amount of water reabsorbed depends on
the tonicity of the medullary interstitium, which is determined by the sodium
reabsorbed in the thick ascending limb of Henle’s loop and urea.
A reduction of intracellular volume often increases effective plasma osmolality;
conversely, decreased effective plasma osmolality is associated with cellular
hydration. Water homeostasis is important in the regulation of plasma osmolality, and
plasma tonicity is maintained within normal limits through a delicate balance
between the rates of water intake and excretion.
The amount of daily water intake includes the volume of water ingested (sensible
intake), the water content of ingested food, and the metabolic production of water
2 To maintain homeostasis, these should be equal to the amount of
water excreted by the kidney and the gastrointestinal (GI) tract (sensible loss) plus
water lost from the skin and respiratory tract (insensible loss).
Changes in plasma tonicity are detected by osmoreceptors in the hypothalamus,
which also houses the thirst center and is the site for ADH synthesis.
plasma tonicity falls below 280 mOsm/kg as a result of water ingestion, ADH
2 water is no longer reabsorbed in the collecting duct, and a large
volume of dilute urine is excreted. Conversely, when the osmoreceptors in the
hypothalamus sense an increased plasma osmolality, ADH is released to increase
water reabsorption. A small volume of concentrated urine is then excreted. The
threshold for ADH release is 280 mOsm/kg, and maximal ADH secretion occurs
when the plasma osmolality is 295 mOsm/kg.
9 Thus, urine osmolality varies from 50
mOsm/kg in the absence of ADH to 1,200 mOsm/kg during maximal ADH release.
The volume of urine produced depends on the solute load to be excreted, as well as
Therefore, for a typical daily solute load of 600 mOsm:
Although the kidney has a remarkable ability to excrete free water, it is not as
efficient in conserving water. ADH minimizes further water loss, but it cannot correct
water deficits. Therefore, optimal osmoregulation requires increased water intake
stimulated by thirst. Both ADH and thirst can be stimulated by nonosmotic stimuli.
For example, volume depletion is such a strong nonosmotic stimulus for ADH release
that it can override the response to changes in plasma osmolality. Nausea, pain, and
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