biophysics seminar 2. november...
TRANSCRIPT
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Biophysics seminar 2. November 2011.
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♦ Diffusion
♦ Osmosis
♦ Properties of water
♦ Exercises
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Biological importance:
♦ Transport of substances in biological systems
♦ Transport processes through cell membrane metabolism
gas exchange between blood and the lungs
♦ Stimuli
♦ Absorbtion of medicines
♦ Chemical reactions
♦ Thermodiffusion
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Brownian motion
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Onsager’s equation
(linear, irreversible processes )
J=XL
The flow density of the extensive quantity (J) is linearly
proportional to the gradient of the intensive quantity (X)
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Diffusion is a time-dependent process,
constituted by random motion of given
entities and causing the statistical
distribution of these entities to spread in
space.
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Matter flow rate
[mol/s]
Matter flow density
[mol/m2s]
A
n
A
IJ v
v
Jv which given the number of moles of substance „A”
travelling through a unit surface during a time interval
of unity.
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After few days The beginning state
Fick’s experiment:
Adolf Eugen Fick (1829-1901)
German anatomist and physiologist
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A
n
A
IJ v
v
Onsager’ s equation
J≈X
Gradient of concentration
intensive quantity
Matter flow density
extensive quantity
x
c
A
n
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x
cDJ
Fick’s 1th law:
matter flow density is linearly proportional to the drop in concentration
negative sign: diffusion current is in the direction where the concentration drops
D – diffusion coefficient
The amount of substance that diffuses through a surface unit during a
time unit if the concentration drop was unity.
depends on both the diffusing particle and the medium in which the
particle diffuses
Unit: m2/s
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For spherical particles (r) in a viscous medium (η) at T temperature:
Stokes-Einstein equation:
r
kTD
6
temperature (T)
the higher the temperature, the stronger the thermal motion
geometry of the particle
globular proteins diffuse more easily than fibres
molar mass of the particle (M) heavier particles diffuse more slowly
viscosity of the medium (η)
diffusion is faster in gases than in liquids
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What is the problem?
We quantitated diffusion in 1D (along the x axis) assuming spatial
variations in the concentration (c(x)), but…
…we did not consider that c is not constant in time: c (x, t)!
We have to connect the variation of
concentration in time to those in space:
FICK’S 2ND LAW
space + time-dependence of diffusion
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OUT IN particles diffusing IN
matter flow density
particles diffusing OUT
matter flow density
We quantitate diffusion in 1D (along the x axis)
Let’s assume a tiny volume (∆V), where the concentration (c) is constant
in space, so we only have to consider the time dependence: c(t)
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Calculated from concentration = Calculated from matter flow density
= (Jx-Jx+ Δx) A Δt (ct+Δt-ct)AΔx
Δc Δx = - ΔJ Δt
t
c
x
J
Fick’s II. law
x
cDJ
From Fick’s I.
Law
Δn = Δnin - Δnout
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The heatflow causes the flow of particles.
The beginning concentration is homogen
The temperature is inhomogen →flow of particles
The heat flows from warm place to the cold place.
The lighter particles diffuse faster in the direction of
the warmer regions
In the warmer regions the lighter, in the colder
regions the heavier particles dominate
The Soret effect
The Dufour effect
The mater flow causes the heatflow.
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Osmosis
Special case of diffusion.There is a filter (semipermeable membrane).
Semipermeable Membrane
The semipermeable membrane functions similar to a fine sieve, only molecules that are small enough can pass.
Bacteria
Medium sized Molecules, e.g. b2-Microglobulin
Water Flow is Easily Possible
Erythrocyte, Red Blood Cell
Albumin, as Example of a Big Protein Molecule
Electrolytes
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Allows smaller slovent molecules to
pass through, but not the larger
solute molecules →”filter”
pl: animal skin pellicles, walls of living
cells, ceramic plate with holes,
cellophane
Osmosis
Unidirectional matter flow,
which takes place by means
of diffusion.
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Water in
Water out
Water in
Water out
Water out
Water in
CLASSIFYING SOLUTIONS ON THE BASIS OF OSMOTIC PRESSURE
♦ Same osmotic pressure: ISOTONIC
Extra- and intracellular solutions with the same osmotic
pressure
The osmotic pressure of the solutions in the cells of
human body = osmotic pressure of a 0,87 % (n/n)
(0.15 M) NaCl solution→physiologic saline solution
♦ Lower osmotic pressure: HYPOTONIC
Extracellullar solution has lower osmotic pressure than
the intracellular solution→water influx
♦Higher osmotic pressure: HYPERTONIC
Extracellular solution has higher osmotic pressure than
the intracellular solution→water efflux
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water
Sugar solution Semipermeable
membrane
t
Solvent IN
Solvent flows in The pressure grow in
membrane
Solvent flow out
♦ The pressure can increase until dynamic equilibrium
♦ The amount of solvent flowing out is same as the amount of solvent
flowing in. Reason: Pressure difference
♦ Osmotic equilibrium
♦ The pressure difference is the osmotic pressure
t0
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Pressure that has to be exerted on the solution connected to pure
solvent by a semipermeable membrane to reach dynamic equilibrium,
to counteract osmosis.
ghposmotic ρ- density
h- height of the liquid column
g- 9,81 m/s2
Van’t Hoff’s-law
cRTposmotic c- concentration of solution
R-universal gas constant
T-temperature
The osmotic pressure exerted by any substance in dilute solution is the same
as that it would exert if present as gas in the same volume.
pozmózis V=nRT
ozmózis
np RT
V
For diluted solutions and perfect semipermeable membranes using the
equation of state of the ideal gas:
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The roles of diffusion and osmosis 1. Dialysis
The process in which different molecules or macromolecules are sorted
by semipermeable membrane.
Remove soluble chemical toxic from body instead of kidneys.
Dialysis
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FRAP denotes an optical technique capable of quantifying the
two dimensional lateral diffusion of a molecularly thin film
containing fluorescently labeled probes, or to examine single
cells. This technique is very useful in biological studies of cell
membrane diffusion and protein binding.
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Specific heat of water Surface tension of water
Specific melting heat of water Evaporation heat of water
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Density of water
Density anomaly density of
water is the greatest at 4 °C.
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The phase diagram of water
1atm
100 C
0 C
Pre
ssure
Temperature
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The unusually high specific heat, surface tension, specific melting heat, evaporation
heat, melting and boiling point, are all explained by the large number of hydrogen
bonds that stabilize the structure of water. The density of ice is lower than that of liquid
water because of the hexagonal crystal structure and the “holes” within.
Explaining the properties of water
Biological relevance of water Density anomaly: seas and lakes freeze at the surface, enableing fish
and other animals to survive.
Large specific heat: helps maintaining a constant temperature, living
organisms will not grow cold easily.
Large evaporation heat: organisms can release heat easily.
Large dipole moment: makes it an excellent solvent for nutrients and
other biologically important molecules, form hydrate shell around
macromolecules (DNA, proteins).
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The water that contains 33 gram / liter of sodium
chloride (NaCl), typical of seawater, has an ionic
concentration of c = 1.128 mol / liter. The ambient
temperature T = 300 K. Calculate the osmotic
pressure. (R=0.082 liter*bar)
p=2*27.8 bar
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Calculate the concentration if solution in water
(300K) has osmotic pressure of 3.00 atm.
c=P/RT
c=0,122 M
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Thank you for your
attention!