Title: Diffusion and Osmosis
1Diffusion and Osmosis
2Diffusion defined
- Migration of atoms, ions, molecules or even small
particles through random motion due to thermal
energy - A particle at any absolute temperature T has an
average kinetic energy of 3kT/2, where k is
Bolzmanns Constant. The value of kT at 300oK is
4.14X10-14 g/cm2/sec2. Particle size is not a
factor in this calculation. - Therefore, the mean velocity of a diffusing
particle depends on its mass, so that particles
of different masses have different diffusion
coefficients.
3Diffusing particles undergo random walks
- Because of collisions with other particles, a
diffusing particle changes direction on a
picosecond time scale. Therefore, individual
particles move about randomly and tend to return
to the same spots. - However, if there is a concentration gradient,
the average number of particles moving down the
gradient at any instant will be greater than the
number moving up the gradient there will be a
net flux (Jnet) of particles from the higher
concentration toward the lower concentration.
Therefore, it helps to think of the concentration
gradient as a force that drives particle
movement, even though from the point of view of
an individual particle, all movements are random.
4What a random movement looks like
N18,050 steps the particle has moved a
distance made good of 196 step lengths
5Ficks Law of Diffusion
- The net flux of a solute S in one dimension x is
described by the Fick Eq.as the product of the
concentration gradient (dCs) and the diffusion
coefficient for that solute (Ds). - Jnet -Ds(dCs/dx)
- The units of J are moles/cm2sec and of the
concentration gradient, moles/cm3/cm. - If diffusion is occurring in a 3-dimensional
setting, a cross-sectional area term must be
inserted into the equation.
6Net movement by diffusion is rapid over short
distances, slow over long distances
- Einstein solved the Fick Eq. to show that, on the
average, in a interval of time t, an average
diffusing particle will travel a distance of
(2Dst)1/2 away from its starting point. (For the
model particle in slide 4, this solution would
have predicted a distance made good of 190
steplengths) - So, the distance gained by diffusional motion
increases as the square root of time, rather than
as a direct proportion to time as in linear
motion. - For a particle with Ds 2X10-5 cm2/sec,
instantaneous velocity will average about
566m/sec, - but speed made good will be much slower this
particle will travel a distance of 1 micron in
about 250 microsec, 10 microns in 25 msec, 100
microns in 2.5 sec, and a meter in about a month.
7Permeation through membranes
- If a barrier to free diffusion is inserted into
the system (such as a cells plasma membrane), a
permeability coefficient replaces the term for
the diffusion coefficient.
8How does diffusion physics relate to physiology?
- Delivery and removal of substances by diffusion
sets an upper limit on cell diameter of about 100
microns. - Since surface area is a term in the 3D Fick
equation, structures that must maximize
diffusional flux tend to show expanded surface
area and attenuated linear dimensions. (Think of
the anatomy of the lung or the surface of the
intestine).
9Osmotic flow
- In osmosis, water diffuses along a gradient of
water concentration that is the result of
dilution of water by the presence of solvents
i.e. the higher the solvent concentration, the
lower the water concentration - The potential energy for water movement
represented by a solute concentration gradient is
given by the van tHoff Equation - Posm MRT
- Where the units of Posm are atmospheres, M is the
osmolality of the solution, R is the gas
constant, and T is the absolute temperature.
Generally, a correction has to be added to the
van tHoff eq. to correct for non-ideal behavior
of the solute.
10Colligative properties of solutions
- Osmotic pressure
- Freezing point
- Vapor pressure or boiling point
- Colligative means tied together.The higher the
solute concentration, the higher the osmotic
pressure, the lower the freezing point and the
higher the boiling point, compared to pure water.
11Two kinds of water potential energy
- Osmotic force a form of chemical potential
energy - Hydrostatic force a form of mechanical potential
energy - These forces are interconvertible, so the net
driving force for water between a cell and the
extracellular solution is - RT (Osmcell - Osmext) (Pcell Pext)
12Osmotic swelling is an unavoidable problem for
all cells
- The swelling arises from the presence of
negatively-charged proteins trapped in the
cytoplasm - First, imagine that a water-permeable membrane
separates two rigid compartments. - One compartment has a 150 mmolal concentration
of NaCl. - The other one has 150 mEq/liter of Na and an
equal quantity of anionic charge as protein
however, the protein concentration is only 1
mmolal. - Is there an osmotic gradient?
- Is there a solute gradient?
13Initial conditions
Intermediate conditions Cl- diffused down its
gradient why did Na move against its gradient?
Notice that there is now a gradient of electrical
charge this is a Donnan potential.
Now imagine water trying to move osmotically is
there a gradient of hydrostatic pressure? The
system has come into Gibbs-Donnan equilibrium
all forces are balanced.
14Animal cells could never attain Gibbs-Donnan
Equilibrium
- Why not? The plasma membrane cannot sustain a
hydrostatic pressure gradient. - Without the evolution of some means of avoiding
Gibbs-Donnan equilibrium, there would be no
protein-containing cells.
15The Na/K Pump counteracts G-D equilibration
The Na/K pump undergoes cycles in which it
spends an ATP to eject 3 Na from the cell and at
the same time to take 2 K into the cell. On the
average, this counteracts leakage of Na and K
across the membrane down their electrochemical
gradients. The bottom-line effect of this is to
make the cell effectively impermeable to NaCl.
Gibbs-Donnan equilibrium is not approached and
the cell does not swell, in spite of the presence
of protein anion (X-).
16What if the Na/K pump stops working?