Upload
agenor-valadares-santos
View
227
Download
0
Embed Size (px)
Citation preview
8/6/2019 Training 1new
1/25
Centrifugation Theory and
Practice
Routine centrifuge rotors
Calculation ofg-force
Differential centrifugation
Density gradient theory
8/6/2019 Training 1new
2/25
Centrifuge rotors
Fixed-angle
axis of rotation
At rest
Swinging-bucket
g
Spinning g
8/6/2019 Training 1new
3/25
Geometry of rotors
b c
rmax
rav
rmin
rmax
rav
rmin
Sedimentation path length
axis of rotation
a
rmax rav rmin
8/6/2019 Training 1new
4/25
k-factor of rotors
The k-factor is a measure of the time taken for a
particle to sediment through a sucrose gradient
The most efficient rotors which operate at a high
RCF and have a low sedimentation path lengththerefore have the lowest k-factors
The centrifugation times (t) and k-factors for two
different rotors (1 and 2) are related by:
2
211
k
tkt !
8/6/2019 Training 1new
5/25
Calculation ofRCFand Q
2
1000
18.11
QrxRCF
r
RCFQ 299!
RCF= Relative Centrifugal Force (g-force)
Q = rpm; r= radius in cm
8/6/2019 Training 1new
6/25
RCF in swinging-bucket and
fixed-angle rotors at 40,000 rpm
Beckman SW41 swinging-bucket (13 ml)
gmin = 119,850g; gav = 196,770g;
gmax = 273,690g
Beckman 70.1Ti fixed-angle rotor (13 ml)
gmin = 72,450g; gav = 109,120g;
gmax = 146,680g
8/6/2019 Training 1new
7/25
g
d
v
lp
Q
VV
18
)(2
!
Velocity of sedimentation of a particle
v = velocityofsedimentation d= diameterofparticle
Vp = densityofparticle Vl= densityofliquid
Q = viscosityofliquidg = centrifugalforce
8/6/2019 Training 1new
8/25
Differential centrifugation Density of liquid is uniform
Density of liquid
8/6/2019 Training 1new
9/25
Size of major cell organelles Nucleus 4-12 Qm
Plasma membrane sheets 3-20 Qm
Golgi tubules 1-2 Qm
Mitochondria 0.4-2.5 Qm
Lysosomes/peroxisomes 0.4-0.8 Qm Microsomal vesicles 0.05-0.3Qm
8/6/2019 Training 1new
10/25
Differential centrifugation of a
tissue homogenate (I)
1000g/10 min
Decant
supernatant
3000g/10 minetc.
8/6/2019 Training 1new
11/25
Differential centrifugation of a
tissue homogenate (II)1. Homogenate 1000g for 10 min
2. Supernatant from 1 3000g for 10 min
3. Supernatant from 2 15,000g for 15 min
4. Supernatant from 3 100,000g for 45 min
Pellet 1 nuclear
Pellet 2 heavy mitochondrial
Pellet 3 light mitochondrial
Pellet 4 microsomal
8/6/2019 Training 1new
12/25
Differential centrifugation (III)
Expected content ofpellets
1000g pellet: nuclei, plasma membrane
sheets 3000g pellet: large mitochondria, Golgi
tubules
15,000g pellet: small mitochondria,lysosomes, peroxisomes
100,000g pellet: microsomes
8/6/2019 Training 1new
13/25
Differential centrifugation (IV
) Poor resolution and recovery because of:
Particle size heterogeneity
Particles starting out at rmin have furthest to
travel but initially experience lowest RCF
Smaller particles close to rmax
have only a
short distance to travel and experience the
highest RCF
8/6/2019 Training 1new
14/25
Differential centrifugation (V)
Fixed-angle rotor:
Shorter sedimentation path
length
gmax > gmin
Swinging-bucket rotor:
Long sedimentation path length
gmax >>> gmin
8/6/2019 Training 1new
15/25
Differential centrifugation (VI)
Rate of sedimentation can be modulated byparticle density
Nuclei have an unusually rapid
sedimentation rate because of their sizeAND high density
Golgi tubules do not sediment at 3000g, in
spite of their size: they have an unusuallylow sedimentation rate because of their verylow density: (Vp - Vl) becomes rate limiting.
8/6/2019 Training 1new
16/25
Density Barrier Discontinuous Continuous
Density gradient centrifugation
8/6/2019 Training 1new
17/25
How does a gradient separate
different particles?
Least dense
Most dense
8/6/2019 Training 1new
18/25
g
d
vlp
Q
VV
18
)(2 !
WhenVp > Vl :vis +veWhenVp = Vl :vis 0
Predictions from equation (I)
8/6/2019 Training 1new
19/25
gd
v lpQ
VV
18
)(2 !
WhenVp < Vl :vis -ve
Predictions from equation (II)
8/6/2019 Training 1new
20/25
Summary ofprevious slides
A particle will sediment through a
solution ifparticle density > solution
density
Ifparticle density < solution density,
particle will float through solution
When particle density = solution density
the particle stop sedimenting or floating
8/6/2019 Training 1new
21/25
Buoyant densitybanding
Equilibriumdensity banding
Isopycnic
banding
1
5
2
3
4
8/6/2019 Training 1new
22/25
1
2
3
3 Formats for separation ofparticles according
to their density
Whendensityofparticle < densityofliquidVis -ve
8/6/2019 Training 1new
23/25
Discontinuous
Resolution of density gradients
ContinuousDensity Barrier
I II
8/6/2019 Training 1new
24/25
Problems with top loading
8/6/2019 Training 1new
25/25
Vp >> Vl :vis +veforallparticles
throughoutthe
gradient
Separation ofparticles according to size