Pressure
differentials govern fluid movement across physiologic semi-permeable
membranes, and two of these forces are hydrostatic/hydraulic pressure and
osmotic pressure. The third factor is the permeability of the capillary
membranes. There will be an escape of water and solute into the interstitial
space resulting in interstitial edema whenever the hydrostatic pressure is much
higher than the osmotic pressure inside the intravascular space. Edema also
occurs when there is capillary leakage due to impaired membrane integrity such
as in burns or anaphylaxis.
Hydrostatic
pressure stems from the action of gravity of a column of fluid while hydraulic
pressure refers to the action delivered by a pump. Together, these two forces
contribute to blood pressure and fluid movement into and out of the vascular
space.[1] Regulation becomes particularly important at the level of the
capillary, the point in the circulatory system where permeability exists to
both solute and water.
Osmotic
pressure relies on selective permeability in membranes. Take two of the major
ions of the extracellular fluid: Na+ and Cl-, which can move rapidly between
plasma and interstitial fluid spaces, thereby making them ineffective osmotic
agents. Proteins, by contrast, are mostly restricted to the plasma compartment,
making them effective osmotic agents in the ability to draw water from the
interstitial space (where protein concentration is low) to the plasma
compartment (where protein concentration is high). The effective osmotic
pressure in this example exerted by the plasma proteins on the fluid movement
between the two compartments represents colloid osmotic pressure or the plasma
oncotic pressure.[2]
While the
filtration-reabsorption balance model is the classically taught version, recent
studies have shown that it has limitations in accurately depicting
microcirculation in most tissues. Michael and Phillips challenged the
traditional model when they used capillaries of frog mesentery to demonstrate
that fluid absorption occurred transiently when hydrostatic pressure in the
capillary (Pc) fell below plasma oncotic pressure (πc). In the steady state,
though, the fluid dynamics changed. When hydrostatic pressure in the capillary
(Pc) was lower than plasma oncotic pressure (πc) in this setting, no absorption
occurred. This evidence that capillaries in low-pressure organ systems can
absorb fluid only transiently and not continuously made it apparent that an
additional factor that influences dynamics, namely the interplay between
oncotic pressure of the interstitium and capillary filtration rate.[3]
Exceptions exist, in which net absorption does take place in the steady state,
as has been shown in lymph nodes, peritubular capillaries of the cortex, and
the ascending vasa recta of the medulla.
A
discussion of fluid movement across membranes would be incomplete without a
discussion of Starling forces. Blood pressure within a capillary (approximately
36 mmHg), referred to as the capillary hydrostatic pressure(P), constitutes an
outward filtration force from the plasma space to the interstitium.[1] The
opposing force, meaning the hydrostatic pressure exerted by the interstitium
(P) towards the capillary is normally close to zero, making it non-contributory
to net fluid movement across capillary membranes. The major reabsorptive force
in this system comes from the colloid osmotic pressure within the capillary
(π), normally around 24 mmHg, whereas the colloid osmotic pressure of the
interstitium (πi) drawing fluid out of the vasculature is normally close to
zero. A balance normally exists between the blood pressure in the capillary and
the plasma colloid oncotic pressure, resulting in a constant vascular volume
within the system over time. In reality, filtration exceeds reabsorption by
roughly 10%, with the excess non-reabsorbed filtrate being returned to the
vascular system via lymphatics.[3] The last contributors to this system are
coefficients for filtration (K), which
converts the hydraulic pressure differentials to flow, and a reflection coefficient (σ) that relates
to the membrane's impermeability. The Starling equation can then be written as
below:
Net flow of
fluid across a capillary wall = (K) * [filtration forces - reabsorptive forces]
or
Net flow =
(K) * [(P + π) - (P + π)]
P = blood
pressure, π = colloid osmotic pressure; and the subscripts: c = capillary, i =
interstitial fluid
These
forces change along the length of the capillary, with the greatest changes
occurring with blood pressure. At the arteriolar end of the capillary, the
blood pressure is roughly 36 mmHg and falls to about 15 mm Hg at the venous end
of the capillary. The colloid osmotic pressure at the arteriolar end remains
relatively constant at about 25 mmHg
Importantly,
the Starling forces only describe the movement of water across membranes in the
vascular system and the mechanism behind constancy in vascular volume.
Colloid
osmotic pressure can be calculated using the Van’t Hoff factor equation. The
usefulness of this calculation, though, becomes complicated in abnormal
physiologic conditions due to several factors including the lack of
proportional changes in protein and salts, heterogeneity in the proteins
involved, and interaction between the protein. This difficulty warrants
measuring the colloid osmotic pressure directly in certain situations.
One method
of direct measurement of interstitial colloid osmotic pressure is the wick
method,[4] which involves the sampling of interstitial COP with
multifilamentous nylon wicks, which are first washed and soaked in priming
solution before being sewn into the subcutaneous tissue of an animal being
studies. After a certain period, the wicks are pulled out, and the wick fluid
isolated by centrifugation.
Another
method of measurement called the crossover method involves priming the wicks in
several different solutions of various concentrations. COP in the fluid within
the wick increases during implantation only in wicks primed with fluid with
lower protein concentration than the ISF. By plotting the COP of the priming
fluid against the COP of wick fluid after implantation, a linear plot can be
constructed with the crossing point of the two representing the true COP of the
interstitium.[4]
Normal
variation in colloid osmotic pressure has been a topic of research. For
example, mean colloid osmotic pressure is 21.1 mmHg in those younger than 50
years old, and significantly lower at 19.7 mm Hg in those between ages 70 and
89.[5] Males also had significantly higher COP than females across age groups.
Critical
care is a setting in which the clinical manifestations of abnormal fluid
balance are seen and have a crucial influence on patient outcomes. Pulmonary
edema, for example, can result when the gradient between COP and pulmonary
artery wedge pressure (PAWP) is reduced – PAWP in this example represents the
outward hydrostatic pressure in the pulmonary vascular space. Rackow showed
that the greater the decrease in COP-PAWP gradient, the greater the increase in
the severity of pulmonary edema.[6] They extrapolated from this that COP-PAWP
gradient predicted mortality in shock patients but did not influence outcomes
in patients with pulmonary edema without shock.
In left
ventricular failure, due to the significantly elevated left ventricular
end-diastolic volume and pressure, the PAWP is proportionately increased
resulting in the reduced COP-PAWP gradient. Fluid enters the pulmonary
interstitial space, i.e., pulmonary edema. During such circumstances, the edema
fluid will be more in the dependent areas because the patient experiences
increased shortness of breath when lying down (orthopnea). Clinically it will
be different from other edema states secondary to reduced plasma protein
concentration which results in edema in all interstitial spaces and, therefore,
generalized clinical edema (anasarca).
We can
measure colloid osmotic pressure to better understand the mechanism of
pulmonary edema in left ventricular failure. The primary insult, an increase in
left ventricular filling pressure, causes a sequence of counterreactions aimed
at restoring fluid balance. A filtrate depleted of protein passes by
ultrafiltration through the lung capillaries, thereby creating a higher COP in
plasma that may partly counterbalance the elevated hydrostatic pressure
accumulated. The lymphatic system of the lungs provides a safety mechanism to
remove fluid from the air spaces until this mechanism is saturated.[5]
Investigators
have tried to manipulate the COP-PAWP gradient by increasing the plasma COP via
albumin infusion as a way of restoring intravascular blood volume and reversing
the fluid loss to the interstitium. After all, albumin accounts for roughly 80%
of the total oncotic pressure exerted by blood plasma on interstitial fluid.
Infusion of albumin alone may produce improvement in 40% of critically ill
patients, according to one study, while adding a potent diuretic like
ethacrynic acid improved that percentage to 70%.[5] From this, it is worth
noting that albumin infusion alone as a means of correcting fluid balance is an
oversimplification of the backbone physiological concepts outlined by Starling.
The quality of membranes involved, transcapillary escape of albumin after
infusion, changes in plasma volume, and other factors come into play.
Hypoalbuminemia
may occur clinically as a result of impaired albumin absorption (Kwashiorkor)
or albumin loss from the gut (protein-losing enteropathy), impaired protein
synthesis by the liver (chronic liver disease), or protein loss through the
kidneys (nephrotic syndrome). Under such circumstances, the colloid osmotic
pressure will be significantly reduced resulting in water and solutes escaping
into the interstitial space from the capillaries. These are all causes of
generalized anasarca resulting from reduced colloid osmotic pressure.
Pregnancy
is another physiologic circumstance in which fluid shifts take place between
intravascular and interstitial spaces, with COP playing a role. An increase in
plasma volume takes place in normal pregnancy, which accounts for a fall in COP
assuming there is no corresponding increase in colloids. Red cell volume
increases during pregnancy as well, although less than plasma volume, which
causes a decrease in hematocrit during the first and second trimester of normal
pregnancy. Wu and colleagues directly measured serum total solids (STS) as a
marker of COP, since the principal component of STS is albumin, the main
colloid determinant of COP. They found that STS (and therefore COP) fell
gradually during pregnancy to a low point between 30 to 34 weeks gestation and
proceeded to rise toward term, following a quadratic equation parabolic trend.
Correlating this with mean blood pressure indicates the direction of fluid
shifts throughout pregnancy.[7]
Damage to
the microvasculature is one of many physiologic changes that occur in
long-standing diabetes. The disturbance in capillary permeability to proteins,
in particular, leads to changes in the transcapillary colloid osmotic gradient.
Patients with long-standing Type 1 diabetes without nephropathy had reduced
interstitial colloid osmotic pressure with increased transcapillary osmotic
gradient compared to normal subjects. [8] Increased microvascular permeability
to proteins should in itself increase the amount of protein in the
interstitium, thereby increasing interstitial oncotic pressure. The reason for
the opposite finding in this study was thought to be due to increased net
capillary filtration, either because of increased capillary filtration coefficient
or increased hydrostatic capillary pressure and the resultant lymphatic
wash-out of proteins from the interstitium. An increased colloid osmotic
gradient between vascular space and interstitium facilitates the preservation
of plasma volume and limits the development of edema.[8]
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5. Morissette
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7. Wu PY,
Udani V, Chan L, Miller FC, Henneman CE. Colloid osmotic pressure: variations
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8. Fauchald
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https://www.ncbi.nlm.nih.gov/books/NBK541067/
Published on 26 April 2024