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Osmotic Activity of Body Fluids
The concentration of solutes in the fluid compartments depends on the osmotic activity generated by the
ion species contained in each compartment. When two solutions are separated by a semipermeable
membrane, water moves across the membrane to equalize the concentration of osmotically active
particles to which the membrane is impermeable. The maintenance of osmotic equilibrium across a
semipermeable membrane is based primarily on the number of solute particles rather than on the molar
concentration of the solution on each side of the membrane due to the flow of water.
The unit of measurement of osmotically active particles is the osmole (Osm) or milliosmole (mOsm)
rather than the conventional units of solute concentration such as milliequivalents per liter (mEq/L). In
solution, osmolarity (mOsm/L) and osmolality (mOsm/kg water) define the osmotic activity of
particles. When 1 mol of NaCl dissociates in water to Na+ and Cl−, it produces 2 Osm. The same
relationship holds true of dissociating salts of multivalent ions such as calcium and magnesium. One mol
of a nondissociating molecule, such as glucose, produces 1 Osm (1,000 mOsm). The measured
osmolality of a solution may not equal the calculated osmolality if the ions do not totally dissociate.
Body fluids are aqueous solutions composed of water and various solutes within the different body
fluid compartments. Because cells are bounded by a semipermeable membrane, adding free water to the
fluid surrounding a cell causes water to move across the cell membrane to equalize the osmolality
differential between the intracellular and extracellular compartments. On a larger scale, adding free
water to the ECF of the body causes an immediate expansion of the extracellular space, followed by a
redistribution of water into the intracellular compartment (Fig. 11-1A). Conversely, loss of free water
from the extracellular space ultimately leads to a shift of water from the intracellular to the
extracellular space (Fig. 11-1B). An osmotic gradient of just 1 mOsm generates a pressure gradient of
19.3 mm Hg.
Colloid Oncotic Pressure (Colloid Osmotic Pressure)
Plasma proteins are confined primarily to the intravascular space and contribute to the osmotic pressure
developed between the plasma and the interstitial fluid. Normal plasma protein levels of 7 g/dL
contribute approximately 0.8 mOsm/L.
Figure 11-1. A: The equilibration of water from the extracellular to the intracellular space after the addition of free water to the
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extracellular fluid compartment. Osmolality transiently decreases in the extracellular compartment, causing water to move across
the cell membranes into the intracellular space. B: Similar shifts after free water loss from the extracellular compartment. Water
moves from the intracellular space to the extracellular space in response to the osmolal gradient that is established.
Osmoregulation
4 Osmolality of body fluids stays fairly constant at approximately 285 to 295 mOsm/L as the result of
tightly regulated water balance. Osmoreceptor cells in the paraventricular and supraoptic nuclei of the
hypothalamus exert central control over the thirst mechanism and antidiuretic hormone (ADH) secretion
from the posterior pituitary.5 In the presence of excess free water, ECF osmolality falls toward 280
mOsm/kg H2O, thirst is inhibited, and ADH levels decline. In the absence of ADH, the permeability of
renal collecting tubules to water is decreased, causing free water reabsorption to decrease and excretion
to increase. Urine osmolality (Uosm) can decline to 50 mOsm/kg H2O (Fig. 11-2). As excess free water is
eliminated, Posm begins to rise. Conversely, free water depletion causes an increase in Posm. As Posm
approaches 295 mOsm/kg H2O, thirst is stimulated as is ADH secretion. As ADH levels rise to
approximately 5 pg/mL, the renal collecting tubules become maximally permeable to water. Water is
reabsorbed from the collecting ducts in response to the concentration gradient developed in the renal
medullary interstitium. Thus, the final concentration of urine depends on both the permeability of the
collecting ducts (controlled by ADH secretion) and the concentration of the medullary interstitium.5
Maximal Uosm may approach 1,200 mOsm/kg H2O. The net effect of these mechanisms is to promptly
return high or low Posm to normal. The high sensitivity of the osmoreceptors and the responsiveness of
the ADH feedback system ensure that even small changes in Posm result in marked alterations in urine
concentration. This relation can be expressed as follows:
Urine osmolality = 95 × Plasma osmolality
Thus, a 1-mOsm change in Posm results in a 95-fold change in Uosm.
Angiotensin II and neural input from medullary baroreceptors can also influence ADH secretion and
thirst, thus tying water balance to hemodynamic alterations. Relatively small changes in pressure have
little effect on ADH secretion, but large decreases in pressure can cause tremendous increases in ADH
release. Therefore, ADH release as a response to changes in serum osmolality is regulated by a very
sensitive system (only small changes in serum osmolality outside its normal range lead to dramatic
changes in ADH release), while the nonosmotic release of ADH occurs in the setting of profound
hypotension for the purposes of preserving volume homeostasis with the subsequent effect of water
retention regardless of serum osmolality (Fig. 11-3).
Tonicity of Body Fluids
Tonicity refers to the effect of the particles on cell volume. (NB: Osmolality defines the concentration of
osmotically active particles in solution.) Permeable solutes can freely cross cell membranes, whereas
impermeable solutes cannot. Although permeable solutes contribute to the osmolality of a solution, they
have no effect on tonicity because they contribute neither to oncotic gradients across cell membranes
nor to alterations in cell volume. Sodium is an example of an impermeable solute that affects both
osmolality and tonicity. Urea and ethanol are permeable solutes that contribute to osmolality but have
little effect on tonicity because they distribute equally across membranes.
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Figure 11-2. The relation of plasma antidiuretic hormone (arginine vasopressin [AVP]) secretion to plasma (A) and urine (B)
osmolality in healthy adults in varying states of water balance. (Reproduced with permission from Robertson GL, Berl T. Water
metabolism. In: Brenner BM, Rector FC Jr, eds. The Kidney. Philadelphia, PA: WB Saunders; 1986:392.)
Figure 11-3. Effect of acute changes in blood volume or pressure on the osmoregulation of antidiuretic hormone (ADH;
vasopressin). The heavy oblique line in the center represents the relation between plasma ADH and osmolality under
normovolemic, normotensive conditions. The lines to the left and right show the shift in the relation when blood volume or blood
pressure is acutely decreased or increased by the percentage indicated in the circles. (Reproduced with permission from Robertson
GL. Physiology of ADH secretion. Kidney Int 1987;32(Suppl 21):520.)
Both impermeable and permeable solutes can contribute to hyperosmolar and hypoosmolar states.
However, hypoosmolar states are always accompanied by hypotonicity, whereas hyperosmolar states
are not always associated with hypertonicity. There may be marked hyperosmolality without
hypertonicity with elevation of blood urea nitrogen (BUN) levels because urea is a freely permeable
molecule. In contrast, elevated levels of plasma glucose in diabetic patients are associated with
hyperosmolarity and associated hypertonicity. Insulin increases the transport of glucose across cell
membranes, rendering these osmoles ineffective and reducing hypertonicity. Plasma hyperglycemia is
associated with the movement of intracellular water to the extracellular space. This causes expansion of
ECF and plasma volume and a consequent decrease in the concentration of plasma sodium. For every
100 mg/dL elevation in blood glucose, measured serum sodium is calculated to fall 1.5 mEq/L, without
an actual alteration of body sodium content. The osmotic diuresis caused by the elevated glucose level
tends to normalize the serum sodium if adequate hydration is maintained. Some patients with
uncontrolled diabetes also have marked hyperlipidemia. Because of this, the concentration of measured
sodium falls. This condition is termed pseudohyponatremia, an artifactual hyponatremia most commonly
caused by severe hypertriglyceridemia, or by severe hyperproteinemia.
Plasma osmolality (Posm) is an excellent measure of total body osmolality. Osmolality differentials
between fluid compartments are only transient because fluid shifts maintain isosmotic conditions.
Sodium is the predominant extracellular cation; thus, estimates of Posm can be made by simply doubling
the serum sodium concentration (serum [Na+]):
Posm (mOsm/L) = 2 × serum [Na+]
Because glucose and BUN may make significant contributions to Posm in certain disease states, this
formula is modified for glucose and for BUN:
Posm (mOsm/L) = 2 × Serum [Na+] - Glucose/18 − BUN/2.8
Discrepancies of greater than 15 mOsm/L between calculated Posm and Posm measured in the clinical
laboratory may be the result of the presence of other osmotically active particles, such as mannitol,
ethanol, or ethylene glycol, or of a reduced fraction of plasma water secondary to high levels of
myeloma proteins or hypertriglyceridemia.
FLUID BALANCE
Sodium Concentration and Water Balance
Abnormalities in serum sodium are usually indicative of abnormal TBW content. This is due to sodium
being the primary extracellular cation. As potassium is the predominant intracellular cation, the serum
[Na+] approximates the sum of the exchangeable total body sodium (Na+
e) and total body
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exchangeable potassium (K+
e) divided by TBW:
Serum [Na+] = (Na+
e − K+
e)/TBW
Because the sum of total body solute content (Na+
e − K+
e) remains relatively stable over time, changes
in TBW content is, therefore, inversely proportional to changes in the serum [Na+] (Fig. 11-4).
Volume Control
5 Changes in volume (i.e., hypovolemic/nonosmotic stimuli) are detected by both osmoreceptors and
baroreceptors.3 The osmoreceptors are responsible for the day-to-day fine-tuning of volume by
responding to changes in tonicity, whereas the baroreceptors contribute relatively little to the control of
fluid balance under normal conditions. As mentioned previously, large changes in circulating volume
(10% to 20% blood volume loss) can modify the osmoregulation of ADH secretion. Cardiac atrial
baroreceptors control volume by means of sympathetic and parasympathetic neural mechanisms,
whereas ANP released by atrial myocytes in response to atrial wall distention may influence sodiumlinked volume control by inhibition of renal sodium reabsorption.6–8
Figure 11-4. Relation between serum [Na+] and the ratio of (Na+e + K+e) to total body water (TBW). (Reproduced with
permission from Edelman IS, Liebman J, O’Meara MP, et al. Interrelationships between serum sodium concentration, serum
osmolarity and total exchangeable sodium, total exchangeable potassium and total body water. J Clin Invest 1958;37:1236.)
Osmoreceptors
Specialized cells in the hypothalamus that respond to changes in extracellular tonicity are known as
osmoreceptors. It is believed that the activity of ion channels in the cell membrane, aquaporins, and
changes in cell volume contribute to the function of these receptors. As the majority of the ECF tonicity
is contributed by sodium, under normal physiologic conditions, these receptors function as “osmosodium” receptors. Osmoreceptors can respond to changes in tonicity as small as a few percent. In
effect, these receptors monitor water balance by monitoring the tonic effect of changes in water
volume. Therefore, ECF [Na+] is an effective monitor of TBW.
Baroreceptor Modulation of Volume Control
Effective circulating volume describes that portion of the extracellular volume that perfuses the organs of
the body and affects the baroreceptors. The effective circulating volume normally corresponds to the
intravascular volume.
Changes in the effective circulating volume are sensed by volume receptors in the intrathoracic
capacitance vessels and atria, pressure receptors of the aortic arch and carotid arteries, intrarenal
baroreceptors, and hepatic and cerebrospinal volume receptors.8,9 These stretch receptors respond to
changes in pressure and circulating volume and, through a complex system of neural and hormonal
actions, alter sodium and water balance in the kidneys. Hormonal effects are mediated by the renin–
angiotensin system, aldosterone, ANP, dopamine, and renal prostaglandins.
Baroreceptor Function
The low-pressure baroreceptors of the intrathoracic vena cava and atria are located in vessels that are
distensible and not affected by sympathetic stimulation; thus, they are ideally situated to detect changes
in venous volume.8 These receptors send continuous signals through vagal afferent nerves to the
cardiovascular control centers of the medulla and hypothalamus, which, in turn, send signals through
parasympathetic and sympathetic fibers to the heart and kidneys. Changes in stretch of these vessels
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