ASEN 5016 Lecture 21: Gravity-Dependent Physical Processes


OBJECTIVES

1.      Identify primary gravity-dependent and -independent forces acting at the level of cells and/or molecules

2.      Analyze and utilize applications of dimensionless numbers to assess relative forces


Is it really “Zero-g” up there?                                                                                                 

"It is a mathematical fact that the casting of this pebble from my hand alters the centre of gravity of the universe."

Thomas Carlyle


Gravity can produce two effects on an object:

- deformation (weight, structural)

            and/or

- displacement (motion, transport)


Structural

 

-         stress and strain relationships dependent on physical properties

 


Transport

 

-         motion dependent on density differences

 


Stokes Sedimentation – "creeping flow" (no inertia)

 For Re < 1 à "creeping flow" à no slip stream

 Reynolds Number

Re = inertial / viscous = r L V / μ

r = density

L = length

V = velocity

μ = viscosity

Swimming bacterium (Re = 10-7) equivalent to a human swimming through asphalt! (Purcell)

Steady state (terminal) velocity à dV/dt = 0

Review of Newton’s Second Law of Motion

·        m (d2z / dt2) = 0 (no accelerated motion)

·        F (grav) = [4/3 p a3 r] g

·        F (bouy) = [4/3 p a3 r0] g

·        F (drag) = f (dz/dt)

à m (d2z / dt2) = F (grav) – F (bouy) – F (drag) 

S F = 0 = (4/3 p a3 r g) – (4/3 p a3 r 0 g) – (6p μ a V)

or

Vsed = 2/9 (ρcellρfluid) (g/μ) a2

Vsed = sedimentation velocity (cm/sec)

ρcell = density of cell

ρfluid  = density of fluid

g = gravity acceleration = 980 cm/sec2

μ = viscosity

a = effective Stokes’ radius = (3V/4π)1/3

Navier-Stokes “Creeping Flow” for a sedimenting bacterial cell:  Vsed ~ 0.06 microns/sec

 

 


Diffusion

Brownian Motion (or Einstein’s “random walk”)

Volume of a sphere: v = 4/3 p r3

Effective Stokes radius for cylinder: a = (3v / 4p )1/3

RMS distance diffused:                  

<x>2 = 2Dt

 

            <x> = Root Mean Square diffusion distance

            t = time

 

D = KbT / (6π μ a)

D = Diffusion coefficient

Kb = 1.38x10-23 J/Molecule° K

particles > ~2-5 mm in aqueous solution à "non Brownian"


Maxwell-Boltzman Equilibrium Distribution

Defines particle concentration gradient

Nh / No = e - [ (VΔρ g h)/(Kb T) ]

 

Nh / No = ratio of cell concentration at height h to 0

V = cell volume

            Δρ = density difference (cell-fluid)

            g = gravity (9.8 m/sec2)

h = height

            Kb = Boltzman constant  = 1.38 x 10-23 J / (particle ° K)

            T = temperature °K (°K = °C + 273)

 

·        Nh / No = 1 – colloidal

·        Nh / No < 1 – distributed

·        Nh / No = 0 - fully sedimented

More info and particle distribution animation…

 


Gradient-driven diffusion becomes more complex.

Binary diffusion (one solute concentration gradient in a solvent) is governed by Fick’s law:

-j1 = D dc1/dx

where -j1 is the flux of species 1 along the x axis as a function of concentration (c) and its diffusion coefficient (D). 

Bi-directional diffusion (a concentration of one particle species migrating into an opposite gradient of another) is further characterized by the Stefan-Maxwell relationship for dilute gases, and does not require designating solute or solvent:

                       n-1

Ñyi = S [yi yj / Dij ] (Vj-Vi)

                       j=1

where V is volume average velocity, D is the relevant diffusion coefficient, and y is a mole fraction.  (A parallel form of this relationship can be used for liquids, but the diffusion coefficient values are no longer the same as for the binary case.)


 Dimensionless Parameters

 

Damköhler (Da)

max reaction rate to max transport rate

Sherwood (Sh)

total mass transport to diffusion only

Peclet (Pe)

convection to diffusion

Schmidt (Sc)

momentum to diffusion

Reynolds (Re)

momentum to drag

Grashof (Gr)

buoyancy to viscous resistance

 

Peclet Number à convective motion / diffusive motion

Pe = (Vsed L) / D

            Vsed = sedimentation velocity (cm/sec)

            D = Diffusion Coefficient (cm2 / sec)

            L = Characteristic Length (cm)

·        if Pe > 10 à convection dominant, neglect diffusion

·        if Pe < 0.1 à diffusion dominant, neglect sedimentation

 for a typical cell, 0.1 < Pe < 10

·        prokaryotes, Pe < 1

·        eukaryotes, Pe > 1


Other Factors

Intercellular and extracellular factors

Inside the cell…

·        Nucleus  / cytoplasm density difference

·        Microfilaments – actin, myosin, etc.

·        Microtubules – tubulin, dynein, kinesin, etc.

·        Intermediate filaments – cytokeratins, skin, etc.

·        Shear force

 Outside the cell…

Transport phenomena

·        Nutrient diffusion and uptake rate

·        Waste excretion and dispersion

Boundary layer issues

Electrostatic surface forces

Bulk fluid mixing

Cell motility

Other forces?


Summary

1.      Characterize the physical aspects of the biological system

2.      Identify all forces acting on the system (g-dependent and –independent)

3.      Draw a Free Body Diagram (intra- and extracellular components)

4.      Correlate observed biological responses to specific physical factors

5.      Isolate cause-and-effect gravity-dependent and independent relationships

6.      Establish a cascade chain of events (beginning with the ‘gravity trigger’ and ending with the observed biological response)


 

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