Week 2: Osmosis/Tonicity Flashcards
Osmosis
Movement of water down its concentration gradient due to its thermal motion
Water Concentration
Water concentration is determined by the number of solute particles in solution (not on their size)
High solute concentration = low water concentration
Low solute concentration = high water concentration
Osmotic Pressure
Osmotic pressure is the pressure applied to a solution to stop osmosis (proportional to the number of solute particles)
It is also measure of the “tendency” of a solution to take in water by osmosis (see this again in Starling Forces)
Basically just the pressure of the water flowing into solution due to osmosis
Osmotically Active Particles
The osmol is the unit used to describe the number of solute particles in solution that cause osmosis (osmotically active particles)
Units of concentration:
Osmolality* = # of Osmol/Kg of water (used more often)
Osmolarity* = # of Osmol/L of solution
*for this course, we will consider these to be the same.
Ex. 1.5M CaCl2 –> 1.5M Ca++ and 3M Cl2
Tonicity
Tonicity is the ability of a solution to cause osmosis across a biological cell membrane
The osmolality of cellular fluid is approximately 290-300 mOsmoles/kg water (use 300)
Remember – homeostasis!! You want to maintain this number (300) at relatively constant values
Consider 3 solutions: hypotonic (lower), isotonic (same) and hypertonic (higher) solution
WATER ALWAYS MOVES TO THE HIGHER SOLUTE CONCENTRATION
Cystic Fibrosis
CF is a genetic disorder that affects (among other organs) the lungs
It’s caused by an abnormal protein called the CF transmembrane conductance regulator (CFTR)
Part of a special chloride transporter that regulates the components of mucus lining the lungs (and sweat/digestive fluids)
Periciliary Liquid
Allows cilia to move (between cilia and mucus)
What would happen to the periciliary liquid if the Cl- transporter did not function?
Cl- builds up inside the cell
Negative charge will build up inside the cell
We will get more sodium moving in
Cellular fluid will become more concentrated so that H2O moves into the cell rather than out
Periciliary liquid is diminishing
Mucous cannot be removed, airways become narrow (infections)
Darrow Yannet Diagram
Helps determine the net movement of water across the cell membrane
A way to look at relative changes in the volume and concentration of the ICF and ECF compartments…
Volume on x
Osmolality on y
ECF < ICF
Water Load
Example: hyponatremia
Volume of ECF increases and osmolality decreases (initial)
Water moves into ICF by osmosis
Its concentration decreases
Volume of both compartments increases and osmolality decreases (compared to normal) (Final)
Water Loss
Example: sweating (hypotonic of body fluids)
ECF volume decreases and osmolality increases (initial)
Water moves out of ICF into ECF by osmosis
Solutes stay behind in ICF so the Osmolality increases
Volume of ECF and ICF decreases (compared to normal) (Final)
Osmolality of both compartments increases (compared to normal) (Final)
Water Loss
Example: sweating (hypotonic of body fluids)
ECF volume decreases and osmolality increases (initial)
Water moves out of ICF into ECF by osmosis
Solutes stay behind in ICF so the Osmolality increases
Volume of ECF and ICF decreases (compared to normal) (Final)
Osmolality of both compartments increases (compared to normal) (Final)
Solute Load
Example: drinking too much salt
Osmolality of ECF increases (and vol increase with sea water) (Initial)
Water moves out of ICF into ECF by osmosis
Osmolality of both compartments increases compared to normal (Final)
Volume of ECF increases and decreases in ICF compared to normal (Final)
Solute Loss
Example: Giving blood, kidney disease (dialysis) - if you donate 500mL and drink 500mL water, you will gain the volume but you will lose the solute
ECF volume
Starling Forces
Starling Forces: Factors that influence the fluid exchange at endothelium – between plasma and interstitial fluid
There are 4 forces acting on this fluid:
2 hydrostatic pressures (fluid pressures)
2 colloid osmotic (oncotic) pressures (osmotic pressure created by proteins in plasma and interstitial fluid)