ch 11 iggy F&E Flashcards
how much of our total weight is water
Water (fluid) makes up about 55% to 60% of total weight for younger adults and 50% to 55% of total weight for older adults.
This water is divided into two main compartments (spaces)
Water delivers dissolved nutrients and electrolytes to all organs, tissues, and cells.
(extracellular fluid [ECF])
the fluid outside the cells The ECF space is about one third (about 15 L) of the total body water.
interstitial fluid
Transcellular fluid
The ECF includes interstitial fluid (fluid between cells, “third space”); blood, lymph, bone, and connective tissue water; and the transcellular fluids. Transcellular fluids include cerebrospinal fluid, synovial fluid, peritoneal fluid, and pleural fluid.
(intracellular fluid [ICF]).
the fluid inside the cells
. ICF is about two thirds (about 25 L) of total body water.
Solutes
Solutes are the particles dissolved or suspended in the water.
Solvent
The solvent is the water portion of fluids.
electrolytes
When solutes express an overall electrical charge, they are known as electrolytes.
What three processes control FLUID AND ELECTROLYTE BALANCE to keep the internal environment stable even when the external environment changes
These processes (filtration, diffusion, and osmosis) determine whether fluids and particles move across cell membranes.
Filtration
Filtration is the movement of fluid (water) through a cell or blood vessel membrane because of water pressure (hydrostatic pressure) differences on both sides of the membrane. This pressure is caused by water volume pressing against confining membranes.
hydrostatic pressure
water pressure. caused by water volume against confining membranes. facilitates filtration (movement of fluid thru cell or blood vessel.
Water molecules in a confined space constantly press outward against the membranes, creating hydrostatic pressure (also known as water pressure). This is a “water-pushing” pressure, because it forces water outward from a confined space through a membrane
what determines the hydrostatic pressure of any body fluid space
The amount (volume) of water in any body fluid space determines the hydrostatic pressure of that space. Blood, which is “thicker” than water (more viscous), is confined within the blood vessels. Blood has hydrostatic pressure because of its weight and volume and also from the pressure in arteries generated by the pumping action of the heart.
comparing two fluid spaces
The hydrostatic pressures of two fluid spaces can be compared whenever a porous (permeable) membrane separates the two spaces. If the hydrostatic pressure is the same in both fluid spaces, there is no pressure difference between the two spaces, and the hydrostatic pressure is at equilibrium. If the hydrostatic pressure is not the same in both spaces, disequilibrium exists. This means that the two spaces have a graded difference (gradient) for hydrostatic pressure: one space has a higher hydrostatic pressure than the other. The human body constantly seeks equilibrium. When a gradient exists, water movement (filtration) occurs until the hydrostatic pressure is the same in both spaces (
which direction does the water move
Water moves through the membrane (filters) from the space with higher hydrostatic pressure to the space with lower pressure. Filtration continues only as long as the hydrostatic pressure gradient exists. equilibrium exists when hydrostatic pressure is equal between spaces. water molecules are shared but there is no net movement
Blood pressure
Blood pressure is an example of a hydrostatic filtering force. It moves whole blood from the heart to capillaries where filtration can occur to exchange water, nutrients, and waste products between the blood and the tissues. The hydrostatic pressure difference between the capillary blood and the interstitial fluid (fluid in the tissue spaces) determines whether water leaves the blood vessels and enters the tissue spaces.
capillaries
Capillary membranes are only one cell layer thick, making a thin “wall” to hold blood in the capillaries. Large spaces (pores) in the capillary membrane help water filter freely when a hydrostatic pressure gradient is present
Edema
Edema (excess tissue fluid) forms with changes in hydrostatic pressure differences between the blood and the interstitial fluid such as in right-sided heart failure.
In this condition the volume of blood in the right side of the heart increases because the right ventricle is too weak to pump blood well into lung blood vessels. As blood backs up into the venous and capillary systems, the capillary hydrostatic pressure rises until it is higher than the pressure in the interstitial space. Excess filtration from the capillaries into the interstitial tissue space then forms visible edema.
Diffusion
Diffusion is the movement of particles (solute) across a permeable membrane from an area of higher particle concentration to an area of lower particle concentration (down a concentration gradient) until equilibrium is reached.
Particles in a fluid have random movement from the vibration of atoms in the nucleus. Random movement allows molecules to bump into each other in a confined fluid space. Each collision increases the speed of particle movement. The more particles (higher concentration) present in the confined fluid space, the greater the number of collisions.
As a result of the collisions, molecules in a solution spread out evenly through the available space. They move from an area of higher molecule concentrations to an area of lower concentrations until an equal concentration (amount) is present in all areas. Spaces with many particles have more collisions and faster particle movement than spaces with fewer particles.
Concentration gradient
A concentration gradient exists when two fluid spaces have different concentrations of the same type of particles. Particle collisions cause them to move down the concentration gradient. Any membrane that separates two spaces is struck repeatedly by particles. When the particle strikes a pore in the membrane that is large enough for it to pass through, diffusion occurs
The chance of any single particle hitting the membrane and going through a pore is much greater on the side of the membrane with a higher solute particle concentration.
impearmeable membrane
Cell membranes, unlike capillary membranes, are selective for which particles can diffuse. They permit diffusion of some particles but not others. Some particles cannot move across a cell membrane, even when a steep “downhill” gradient exists, because the membrane is impermeable (closed) to that particle. For these particles the concentration gradient is maintained across the membrane.
differences in comcentrations on specific ions
usually the fluid outside the cell (the extracellular fluid [ECF]) has ten times more sodium ions than the fluid inside the cell (the intracellular fluid [ICF]). This extreme difference is caused by cell membrane impermeability to sodium and by special “sodium pumps” that move any extra sodium present inside the cell out of the cell “uphill” against its concentration gradient and back into the ECF.
facilitated diffusion
For some particles diffusion cannot occur without help, even down steep concentration gradients, because of selective membrane permeability.
glucose cannot cross some cell membranes without the help of insulin. Insulin binds to insulin receptors on cell membranes, which then makes the membranes much more permeable to glucose. Then glucose can cross the cell membrane down its concentration gradient into the cell.
Diffusion across a cell membrane that requires a membrane-altering system (e.g., insulin) is called facilitated diffusion. This type of movement is still a form of diffusion because it does not require extra energy.
Osmosis
Osmosis is the movement of water only through a selectively permeable (semipermeable) membrane. For osmosis to occur, a membrane must separate two fluid spaces, and one space must have particles that cannot move through the membrane. (The membrane is impermeable to this particle.) A concentration gradient of this particle must also exist. Because the membrane is impermeable to these particles, they cannot cross the membrane, but water molecules can.
For the fluid spaces to have equal concentrations of the particle, the water molecules move down their concentration gradient from the side with the higher concentration of water molecules (and a lower concentration of particles along with a greater hydrostatic pressure) to the side with the lower concentration of water molecules (and a higher concentration of particles along with a lower hydrostatic pressure). This movement continues until both spaces contain the same proportions of particles to water. Dilute fluid is less concentrated and has fewer particles and more water molecules than more concentrated fluid. Thus water moves by osmosis down its hydrostatic pressure gradient from the dilute fluid to the more concentrated fluid until a concentration equilibrium occurs
At this point the concentrations of particles in the fluid spaces on both sides of the membrane are equal, even though the total amounts of particles and volumes of water are different. The concentration equilibrium occurs by the movement of water molecules rather than the movement of solute particles.
particle concentration
Particle concentration in body fluid is the major factor that determines whether and how fast osmosis and diffusion occur
This concentration is expressed in milliequivalents per liter (mEq/L), millimoles per liter (mmol/L), and milliosmoles per liter (mOsm/L)
osmolarity
Osmolarity is the number of milliosmoles in a liter of solution;
Because 1 L of water weighs 1 kg, in human physiology osmolarity and osmolality are considered the same, although osmolarity is the actual concentration measured most often. The normal osmolarity value for plasma and other body fluids ranges from 270 to about 300 mOsm/L. The body functions best when the osmolarity of all body fluid spaces is close to 300 mOsm/L.
osmolality
; osmolality is the number of milliosmoles in a kilogram of solution. Because 1 L of water weighs 1 kg, in human physiology osmolarity and osmolality are considered the same, although osmolarity is the actual concentration measured most often.
isosmotic or isotonic (also called normotonic)
The body functions best when the osmolarity of all body fluid spaces is close to 300 mOsm/L. When all fluids have this particle concentration, the fluids are isosmotic or isotonic (also called normotonic) to each other.