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    Centrifugation Theory and

    Practice

    Routine centrifuge rotors

    Calculation ofg-force

    Differential centrifugation

    Density gradient theory

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    Centrifuge rotors

    Fixed-angle

    axis of rotation

    At rest

    Swinging-bucket

    g

    Spinning g

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    Geometry of rotors

    b c

    rmax

    rav

    rmin

    rmax

    rav

    rmin

    Sedimentation path length

    axis of rotation

    a

    rmax rav rmin

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    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 !

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    Calculation ofRCFand Q

    2

    1000

    18.11

    QrxRCF

    r

    RCFQ 299!

    RCF= Relative Centrifugal Force (g-force)

    Q = rpm; r= radius in cm

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    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

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    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

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    Differential centrifugation Density of liquid is uniform

    Density of liquid

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    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

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    Differential centrifugation of a

    tissue homogenate (I)

    1000g/10 min

    Decant

    supernatant

    3000g/10 minetc.

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    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

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    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

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    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

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    Differential centrifugation (V)

    Fixed-angle rotor:

    Shorter sedimentation path

    length

    gmax > gmin

    Swinging-bucket rotor:

    Long sedimentation path length

    gmax >>> gmin

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    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.

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    Density Barrier Discontinuous Continuous

    Density gradient centrifugation

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    How does a gradient separate

    different particles?

    Least dense

    Most dense

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    g

    d

    vlp

    Q

    VV

    18

    )(2 !

    WhenVp > Vl :vis +veWhenVp = Vl :vis 0

    Predictions from equation (I)

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    gd

    v lpQ

    VV

    18

    )(2 !

    WhenVp < Vl :vis -ve

    Predictions from equation (II)

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    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

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    Buoyant densitybanding

    Equilibriumdensity banding

    Isopycnic

    banding

    1

    5

    2

    3

    4

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    1

    2

    3

    3 Formats for separation ofparticles according

    to their density

    Whendensityofparticle < densityofliquidVis -ve

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    Discontinuous

    Resolution of density gradients

    ContinuousDensity Barrier

    I II

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    Problems with top loading

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    Vp >> Vl :vis +veforallparticles

    throughoutthe

    gradient

    Separation ofparticles according to size