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S edimentation T heory (a) Gravitational sedimentation (b) Centrifugal sedimentation

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2.2 K inetic p roperty. S edimentation. Motion of heavy particles settle down in response to an external force such as gravity , centrifugal force or electric force Rate of sedimentation depends on the strength of the field, masses and shapes of the particles. S edimentation T heory - PowerPoint PPT Presentation
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Motion of heavy particles settle down in response to an external force such as gravity , centrifugal force or electric force Rate of sedimentation depends on the strength of the field, masses and shapes of the particles dimentation Theory ) Gravitational sedimentation ) Centrifugal sedimentation -Sedimentation velocity -Sedimentation Equilibrium 2.2 Kinetic property Sedimentation
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Page 1: S edimentation  T heory (a)  Gravitational sedimentation (b) Centrifugal sedimentation

Motion of heavy particles settle down in response to an exter nal force such as gravity , centrifugal force or electric force

Rate of sedimentation depends on the strength of the field, masses and shapes of the particles

Sedimentation Theory(a) Gravitational sedimentation(b) Centrifugal sedimentation

-Sedimentation velocity-Sedimentation Equilibrium

2.2 Kinetic property

Sedimentation

Page 2: S edimentation  T heory (a)  Gravitational sedimentation (b) Centrifugal sedimentation

(a) Gravitational Sedimentation

m

F1

F2Fb (buoyancy)

Fg (gravity)

Page 3: S edimentation  T heory (a)  Gravitational sedimentation (b) Centrifugal sedimentation

(a) Gravitational Sedimentation

m

F1 = fVg

F2 = mg(1 - 2/1)

At equilibrium :fVg = mg(1 - 2/1)

m = fVg

g(1 - 2/1)M = fNAVg

g(1 - 2/1)1 = density of particle2 = density of medium

F1

F2

Page 4: S edimentation  T heory (a)  Gravitational sedimentation (b) Centrifugal sedimentation
Page 5: S edimentation  T heory (a)  Gravitational sedimentation (b) Centrifugal sedimentation

(b) Centrifugal Sedimentation

•sedimentation velocity•sedimentation equilibrium

= angular velocity (rpm)

Page 6: S edimentation  T heory (a)  Gravitational sedimentation (b) Centrifugal sedimentation

b.1 Sedimentation velocity

an analytical ultracentrifugation method that measures the rate at which molecules move in response to centrifugal force generated in a centrifuge .This sedimentation rate provides information about both the molecular mass and the shape of molecules .In some cases this technique can also measure diffusion coefficients (D).

Page 7: S edimentation  T heory (a)  Gravitational sedimentation (b) Centrifugal sedimentation

b.1 Sedimentation velocity

F1

F1 = fV = f(dr/dt) F2 = m2r (1 - 2/1)

At equilibrium :f(dr/dt) = m 2r (1 - 2/1)

M = sfNA = sRT

(1 - 2/1) D(1 - 2/1)

S = (dr/dt) = m(1 - 2/1) 2r f

r

F2

s = sedimentation coefficient ( Svedberg,1Sv=10-13 s)

~ 80,000 rpm

Page 8: S edimentation  T heory (a)  Gravitational sedimentation (b) Centrifugal sedimentation

b.2 Sedimentation equlibrium

M = 2RT ln (C2/C1) (1 - 2/1) 2 (r2

2-r12)

~ 10,000 rpm

=

Page 9: S edimentation  T heory (a)  Gravitational sedimentation (b) Centrifugal sedimentation

Assignment-3

GGrouproup P PresentationresentationCComparing to omparing to sedimentationsedimentation

G1 : G1 : precipitation,precipitation, aggregationaggregation G2 : G2 : coagulation,coagulation, flocculationflocculation

(10 students per group)

(5 min)

Page 10: S edimentation  T heory (a)  Gravitational sedimentation (b) Centrifugal sedimentation

3.3. O Opticalptical p property roperty

A colloidal system contains particles that affect a light beam by scattering and absorption .

If the particles are of a size comparable to the wavelength () of light or larger, they scatter or absorb light independently .

The same thing happens if they are separated by distances comparable to or greater than the wavelength () of light .

Page 11: S edimentation  T heory (a)  Gravitational sedimentation (b) Centrifugal sedimentation

3.3. C Commonommon O Opticalptical pphenomena henomena

the interaction of light from the sun or moon with the atmosphere, clouds, water, or dust and other particulates

Page 12: S edimentation  T heory (a)  Gravitational sedimentation (b) Centrifugal sedimentation
Page 13: S edimentation  T heory (a)  Gravitational sedimentation (b) Centrifugal sedimentation

Assignment-4

GGroup roup PPresentationresentationG3 : Rayleigh Scattering G3 : Rayleigh Scattering G4 : RamanG4 : Raman ScatteringScatteringG5 : Mie ScatteringG5 : Mie ScatteringG6 : Bragg ScatteringG6 : Bragg Scattering

(10 students per group)

(5 min)


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