Fluid Intake
The major determinant of fluid intake in a healthy adult is habit. Thirst, another important determinant of fluid intake, can be caused by several physiologic mechanisms.
4 These include dryness of the oral mucous membranes, increase in osmolality of the body fluids (osmoreceptor-mediated thirst), decrease in extracellular fluid volume (ECV) (baroreceptor-mediated thirst), and increased renin secretion (angiotensin-mediated thirst). Osmoreceptor-mediated thirst is the most common cause of thirst in healthy adults. This mechanism becomes less effective with aging. Thus, older adults often have a greater need for water before they become thirsty. Cultural factors have an important influence on fluid intake. For example, intake of certain herbal teas may be considered necessary by some individuals when they become ill. Many people refuse to drink cold water when they have certain illnesses due to their cultural beliefs. In clinical settings, health care professionals often regulate the fluid intake. Routes of fluid intake include oral, rectal, intravenous, and intraosseous, as well as through tubes into body cavities. Oral fluid intake includes liquids and the water contained in food, as well as water made by cellular metabolism of ingested nutrients.
Fluid Distribution
Two types of fluid distribution operate in the body. First, fluid is distributed between the vascular and interstitial spaces, the two subcompartments of the extracellular compartment. Second, fluid
is distributed between the extracellular and intracellular compartments. Different processes regulate these two types of fluid distribution.
Fluid distribution between the vascular and interstitial spaces is regulated by filtration. Filtration is the net result of four opposing forces. Two of these forces tend to move fluid out of the capillaries, whereas the other two tend to move fluid into the capillaries. Which direction the fluid moves in any one location depends on which forces are stronger. The two forces that tend to move fluid out of capillaries are the blood hydrostatic pressure (outward force against the capillary walls) and the interstitial fluid osmotic pressure (inward pulling force caused by particles in interstitial fluid). The two forces that tend to move fluid into capillaries are the blood osmotic pressure (inward pulling force caused by particles in blood) and the interstitial fluid hydrostatic pressure.
Usually, the blood hydrostatic pressure is highest at the arterial end of a capillary, and there is filtration from the capillary into the interstitial fluid. This flow of fluid out of the capillaries is useful in carrying oxygen, glucose, amino acids, and other nutrients to the cells that are surrounded by interstitial fluid. Most proteins are too large to cross into the interstitial fluid and remain in the capillary. At the venous end of a capillary, the blood hydrostatic pressure is usually lower and the blood osmotic pressure higher because fluid has left the capillary but the proteins have remained. These changes cause a net flow of fluid from the interstitial space back into the venous end of a capillary. The flow of fluid back into the capillaries is physiologically useful in carrying carbon dioxide, metabolic acids, and other waste products into the blood for further metabolism or excretion.
Changes in any of the four forces that determine the direction of filtration at the capillaries can cause abnormal distribution between the vascular and interstitial compartments. The most common abnormal distribution is edema, which is expansion of the interstitial space. Edema can be caused by increased blood hydrostatic pressure (e.g., venous congestion), increased microvascular permeability that allows proteins to leak into interstitial fluid, increased interstitial fluid osmotic pressure (e.g., inflammation), decreased blood osmotic pressure (e.g., hypoalbuminemia), or blockage of the lymphatic system, which normally removes excess fluid from the interstitial space and returns it to the vascular compartment.
The second type of fluid distribution occurs between the extracellular and intracellular compartments. This process is regulated by osmosis. Cell membranes are freely permeable to water, but the passage of ions and other particles depends on membrane transport processes. Osmotic pressure is an inward-pulling force caused by particles in a fluid. Both the extracellular and intracellular fluids exert osmotic pressure. Because the osmolality of the two compartments normally is the same, the osmotic pressures are the same. Therefore, the force pulling water into the cells balances the force pulling water into the interstitial space, maintaining the normal fluid distribution. If the osmolality of the extracellular fluid changes, however, then osmosis occurs, altering the fluid distribution until the osmolality in the extracellular and intracellular compartments again is the same. For example, if the extracellular fluid becomes more concentrated (increased osmolality), then the osmotic pressure of the extracellular fluid becomes higher than the osmotic pressure of the intracellular fluid. Water leaves the intracellular compartment until the intracellular fluid becomes as concentrated as the extracellular fluid. This process decreases the amount of water that is distributed into the intracellular compartment. Similarly, if the extracellular fluid becomes more dilute (decreased osmolality), then the osmotic pressure of the extracellular fluid becomes lower than the osmotic pressure of the intracellular fluid. Water moves by osmosis into the intracellular compartment until the intracellular fluid becomes as dilute as the extracellular fluid. This process increases the amount of water that is distributed into the intracellular compartment.
In summary, fluid distribution between the vascular and interstitial compartments depends on filtration, the net result of four forces that act on fluid at the capillary level. Fluid distribution between the extracellular and intracellular compartments depends on osmosis, the movement of water across cell membranes to equilibrate particle concentrations.
Fluid Excretion
Normal routes of fluid excretion are respiratory tract, urine, feces, and skin (insensible perspiration and sweat). In a standard adult, approximately 400 mL of water is excreted daily through the respiratory tract, even if the person is fluid-depleted. This amount increases during fever. The urine volume of a healthy adult varies according to the fluid intake, the needs of the body, and the hormonal status. It averages 1,500 mL. Major hormones that regulate urinary excretion of fluid are summarized in
Table 7-1. Diuretics, ethanol, and caffeine increase urine volume. Fecal excretion of water averages 200 mL per day in healthy adults who have a normal fluid balance and a fully functioning bowel. Diarrhea causes a dramatic increase in fecal excretion of water.
Insensible perspiration is fluid excretion through the skin that is not visible. It averages 500 mL per day in a healthy adult. Insensible perspiration occurs even if the person is fluid-depleted. It increases during fever. Sweat is visible fluid excretion through the skin. The volume of sweat varies greatly depending primarily on thermoregulatory needs.
Fluid Loss by Abnormal Routes
Examples of abnormal routes of fluid loss are emesis, drains, suction, paracentesis, and hemorrhage. Third-spacing (e.g., ascites) can be considered abnormal fluid loss, even though the fluid remains in the body, because the fluid is not freely available to the normal fluid compartments.
Summary of Fluid Balance
In summary, the processes of fluid intake, fluid distribution, fluid excretion, and fluid loss by abnormal routes act together to determine fluid balance or imbalances. A change in one of these processes must be matched by a change in another to maintain fluid balance. For example, if an increased urine output is matched by an increased fluid intake, then fluid balance can be maintained. If changes in one or more of these processes are not matched by changes in the others, however, then a fluid imbalance occurs. Fluid imbalances may be characterized by altered volume of fluid (ECV imbalances), altered concentration of fluid (osmolality imbalances), or a combination of both.