The Body Fluid
Compartments: Extracellular and
Intracellular Fluids; Interstitial Fluid and Edema
The maintenance
of a relatively constant volume and a
stable composition of the body fluids is essential for homeostasis.
Fluid Intake
and Output Are Balanced During Steady-State Conditions
The relative
constancy of the body fluids is remarkable because there is continuous exchange
of fluid and solutes with the external environment as well as within the
different compartments of the body.
Daily Intake of
Water
Water is added
to the body by two major sources:
(1) it is ingested in the form of liquids or
water in the food, which together normally add about 2100 ml/day to the body
fluids.
(2) it is synthesized in the body as a result
of oxidation of carbohydrates, adding about 200 ml/day. This provides a total
water intake of about 2300 ml/day.
Daily Loss of Body Water
Insensible Water Loss. Some of the water losses cannot be precisely regulated. For example, there is a continuous loss of water
by evaporation from the respiratory tract and diffusion through the skin, which
together account for about 700 ml/day of water loss under normal conditions.
This is termed insensible water loss because we are not
consciously aware of it.
The insensible
water loss through the skin occurs independently of sweating, the average
water loss by diffusion through the skin is about 300 to 400 ml/day.
Fluid Loss in Sweat.
The amount of water lost by sweating is highly variable, depending on
physical activity and environmental temperature. The volume of sweat normally
is about 100 ml/day, but in very hot weather or during heavy exercise, water loss in sweat
occasionally increases to 1 to 2 L/hour. This would rapidly deplete the body
fluids if intake were not also increased by activating the thirst mechanism.
Water Loss in Feces.
Only a small amount of water (100 ml/day) normally is lost in the feces.
This can increase to several liters a
day in people with severe diarrhea.
Water Loss by the Kidneys.
The remaining water loss from the body occurs in the urine excreted by
the kidneys. There are multiple mechanisms that control the rate of urine excretion.
In fact, the most important means by which the body maintains a balance between
water intake and output, as well as a balance between intake
and output of most electrolytes in the body, is by controlling the rates
at which the kidneys excrete these substances. For example, urine volume can be
as low
as 0.5 L/day in a dehydrated person or as high as 20 L/day in a person who has been drinking tremendous amounts of water. This variability of intake
is also true for most of the electrolytes of the body, such as sodium,
chloride, and potassium. In some people, sodium intake may be as low as 20
mEq/day, whereas in others, sodium intake may be as high as 300 to 500
mEq/day.The kidneys are faced with the task of adjusting the excretion rate of water
and electrolytes to match precisely the intake of these substances, as well as
compensating for excessive losses of fluids and electrolytes that occur in
certain disease states.
Body Fluid Compartments
The total
body fluid is distributed mainly between two compartments:
the extracellular
fluid and the intracellular fluid.
Fig: Summary
of body fluid regulation, including the major body fluid compartments and the
membranes that separate these compartments. The values shown are for an average
70-kilogram person
The
extracellular fluid is divided into the interstitial fluid and the blood
plasma.In the average 70-kilogram adult human, the total body water is
about 60 per cent of the body weight, or about 42 liters.This percentage can
change, depending on age, gender, and degree of obesity.
Intracellular Fluid Compartment
About 28 of the 42 liters of fluid in the body are inside the 75
trillion cells and are collectively called the intracellular fluid. Thus,
the intracellular fluid constitutes about 40 per cent of the total body weight
in an “average” person.
the intracellular fluid of all the different cells together is
considered to be one large fluid compartment.
Extracellular Fluid
Compartment
All the fluids outside the cells are collectively called the extracellular
fluid. Together these fluids account for about 20 per cent of the body
weight, or about 14 liters in a normal 70-kilogram adult. The two largest
compartments
of the extracellular fluid are:
The interstitial fluid: which
makes up more than three fourths of the extracellular fluid.
The plasma: which makes up almost
one fourth of the extracellular fluid, or about 3 liters. The plasma is
the non cellular part of the blood; it exchanges substances continuously
with the interstitial fluid through the pores of the capillary
membranes. These pores are highly permeable to almost all solutes
in the extracellular fluid except the proteins. Therefore, the
extracellular fluids are constantly mixing,
so that the plasma and interstitial fluids have about the same
composition except for proteins, which have a higher concentration in
the plasma.
Blood Volume
Blood contains both extracellular fluid (the fluid in plasma) and
intracellular fluid (the fluid in the red blood cells). However, blood is
considered to be a separate fluid compartment because it is contained in a chamber of its own, the circulatory system.
The blood volume is especially important in the control of cardiovascular dynamics.
The average blood volume of adults is about 7 per
cent of body weight, or about 5 liters. About 60 per cent of the blood
is plasma and 40 per cent is red blood cells, but these percentages can vary
considerably in different people, depending on gender, weight, and other
factors.
Constituents of Extracellular and Intracellular Fluids:
Ionic Composition of Plasma and Interstitial Fluid Is
Similar
Because the plasma and interstitial fluid are separated only by highly
permeable capillary membranes, their ionic composition is similar. The most
important difference between these two compartments is the higher concentration
of protein in the plasma; because the capillaries have a low permeability to
the plasma proteins, only small amounts of proteins are leaked into the
interstitial spaces in most tissues. Because of the Donnan effect, the
concentration of positively charged ions (cations) is slightly greater (about 2
per cent) in the plasma than in the interstitial fluid. The plasma proteins
have a net negative charge and,
therefore, tend to bind cations, such as sodium and potassium ions, thus
holding extra amounts of these cations in the plasma along with the plasma proteins. Conversely, negatively
charged ions (anions) tend to have a slightly higher concentration in the
interstitial fluid compared with the plasma, because the negative charges of
the plasma proteins repel the negatively charged anions. For practical purposes,
however, the concentration of ions in interstitial fluid and in the plasma is considered to
be
about equal; the extracellular
fluid, including the plasma and the interstitial fluid, contains large amounts
of sodium and chloride ions, reasonably large amounts of bicarbonate ions, but
only small quantities of potassium, calcium, magnesium, phosphate, and organic
acid ions. The composition of extracellular fluid is carefully regulated by
various mechanisms, but especially by the kidneys. This allows the cells to remain
continually bathed in a fluid that contains the proper concentration of
electrolytes and nutrients for optimal cell function.
Fig: Chemical
compositions of extracellular and intracellular fluids
Important Constituents of the Intracellular Fluid
The intracellular fluid is separated from the extracellular fluid by a
cell membrane that is highly permeable to water but not to most of the
electrolytes in the body. In contrast to the extracellular fluid, the
intracellular
fluid contains only small quantities of sodium and chloride ions and
almost no calcium ions. Instead, it contains large amounts of potassium and
phosphate
ions plus moderate quantities of magnesium and sulfate ions, all of
which have low concentrations in the extracellular fluid. Also, cells contain
large amounts of protein, almost four
times as much as in the plasma.
Regulation of Fluid Exchange and Osmotic Equilibrium Between
Intracellular and Extracellular Fluid:
The relative amounts of
extracellular fluid distributed between the plasma and interstitial
spaces are determined mainly by the balance of hydrostatic and colloid
osmotic forces across the capillary membranes. The distribution
of fluid between intracellular and extracellular compartments, in
contrast, is determined mainly by the osmotic effect of the smaller
solutes— especially sodium, chloride, and other electrolytes—acting
across the cell membrane.
The reason for this is that the cell membranes are highly
permeable to water but relatively impermeable to even small ions such as
sodium and chloride. Therefore, water moves across the cell membrane
rapidly, so that the intracellular fluid remains isotonic with the
extracellular fluid.
Basic
Principles of Osmosis and Osmotic Pressure
Osmosis is the net diffusion of water across a
selectively permeable membrane from a region of high water concentration to one
that has a lower water concentration. When a solute is added to pure water,
this reduces the concentration of water in the mixture. Thus, the higher the solute concentration in a
solution, the lower the water concentration. Further, water diffuses
from a region of low solute concentration (high water concentration)
to one with a high solute concentration (low water concentration). Because
cell membranes are relatively impermeable to most solutes but highly permeable
to water (i.e., selectively permeable), whenever there is a higher
concentration of solute on one side of the cell membrane, water diffuses
across the membrane toward the region of higher solute concentration. Thus, if
a solute such as sodium chloride is added to the extracellular fluid, water
rapidly diffuses from the cells through the cell membranes into the
extracellular fluid until the water concentration on both sides of the membrane
becomes equal. Conversely, if a solute such as sodium chloride is removed from
the extracellular fluid, water diffuses from the extracellular fluid through
the cell membranes and into the cells. The rate of diffusion of water is called
the rate of osmosis.
The osmotic pressure of a solution is directly proportional to the
concentration of osmotically active particles in that solution. This is true
regardless of whether the solute
is a large molecule or a small molecule. For
example, one molecule of albumin with a molecular weight of
70,000 has the same osmotic effect as one molecule of glucose with a
molecular weight of 180. One molecule of sodium chloride, however, has
two osmotically active particles, Na+ and Cl–, and therefore has twice the
osmotic effect of either an albumin molecule or a glucose molecule.
Osmolarity of the Body Fluids.
the approximate osmolarity of the
various osmotically active substances in
plasma, interstitial fluid, and intracellular fluid. Note that about 80 per
cent of the total osmolarity of the interstitial fluid and plasma is due to
sodium and chloride ions, whereas for intracellular fluid, almost half the
osmolarity is due to potassium ions, and the remainder is divided among many
other intracellular substances, the total osmolarity of each of the three compartments
is about 300 mOsm/L, with the plasma being about 1 mOsm/L greater than that of
the interstitial and intracellular fluids.The slight difference
between plasma and interstitial fluid is caused by the osmotic effects
of the plasma proteins, which maintain about 20 mm Hg greater pressure in the
capillaries than in the surrounding
interstitial spaces.
Isotonic,
Hypotonic, and Hypertonic Fluids.
If a cell is placed in a solution of impermeant solutes having an osmolarity
of 282 mOsm/L, the cells will not shrink or swell because the water
concentration
in the intracellular and extracellular fluids is equal and the solutes
cannot enter or leave the cell. Such a solution is said to be isotonic because
it neither shrinks
nor swells the cells. Examples of isotonic solutions include a 0.9 per
cent solution of sodium chloride or a 5 per cent glucose solution. These
solutions are important in clinical medicine because they can be infused into
the blood without the danger of upsetting osmotic equilibrium between the
intracellular and extracellular fluids.
If a cell is
placed into a hypotonic
solution that has a lower concentration of impermeant solutes (less than 282
mOsm/L), water will diffuse into the cell, causing it to swell; water will
continue to diffuse into the cell, diluting the intracellular fluid while also
concentrating the extracellular fluid until both solutions have about the same
osmolarity. Solutions of sodium chloride with a concentration of less than 0.9
per cent are hypotonic and cause cells to swell.
If a cell is placed in a hypertonic
solution having a higher concentration of impermeant solutes, water will flow
out of the cell into the extracellular fluid, concentrating the intracellular fluid
and diluting the extracellular fluid. In this case, the cell will shrink until
the two concentrations become equal. Sodium chloride solutions of greater than
0.9 per cent are hypertonic.
Edema: Excess
Fluid in the Tissues
Edema refers to
the presence of excess fluid in the body tissues. In most instances, edema
occurs mainly in the extracellular fluid compartment, but it can involve
intracellular fluid as well.
Intracellular
Edema
Two conditions
are especially prone to cause intracellular swelling:
(1) depression of the metabolic systems of the
tissues.
(2) lack of adequate nutrition to the cells.
For example, when blood flow to a tissue is
decreased, the delivery of oxygen and nutrients is reduced. If the blood flow
becomes too low to maintain normal tissue metabolism, the cell membrane ionic
pumps become depressed. When this occurs, sodium ions that normally leak into
the interior of the cell can no longer be pumped out of the cells, and the excess
sodium ions inside the cells cause osmosis of water into the cells. Sometimes this can
increase intracellular volume of a tissue area—even of an entire ischemic
leg, for example—to two to three times normal. When this occurs, it is usually a
prelude to death of the tissue.
Intracellular
edema can also occur in inflamed tissues. Inflammation usually has a direct
effect on the cell membranes to increase their permeability, allowing sodium and other ions to diffuse into the
interior of the cell, with subsequent
osmosis of water into the cells.
Extracellular Edema
Extracellular
fluid edema occurs when there is excess fluid accumulation in the extracellular
spaces. There are two general causes of extracellular edema:
(1)
Abnormal leakage of fluid from the plasma to the
interstitial spaces across the capillaries.
(2) Failure of the lymphatic to return fluid from the interstitium back
into the blood. The most common clinical cause of interstitial fluid
accumulation is excessive capillary fluid
filtration.
Fluids in the “Potential Spaces” of the Body:
It include the pleural cavity, Pericardial cavity, peritoneal cavity, and synovial cavities, including both the joint
cavities and the bursae. Virtually all these potential spaces have surfaces
that almost touch each other, with only a thin layer of fluid in between, and
the surfaces slide over each other. To facilitate the sliding, a viscous proteinaceous fluid lubricates the surfaces.
Edema Fluid in the Potential Spaces Is Called “Effusion.”
When edema
occurs in the subcutaneous tissues adjacent to the potential space, this fluid
is called effusion. Thus, lymph blockage or any of the multiple abnormalities
that can cause excessive capillary filtration can cause effusion in the same
way that interstitial edema is caused. The abdominal cavity is especially prone
to collect effusion fluid and the effusion
is called ascites. In serious cases, 20 liters or more of ascitic fluid
can accumulate. The other potential spaces, such as the pleural cavity,
pericardial cavity, and joint spaces, can become seriously swollen when there
is generalized edema.
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