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Lumped parameter
negligible internal resistance (Bi < 0.1)
temperature only varies with time (temp variation in all 3 spatial directions can be ignored)
When can we ignore internal resistance
small L (thin slab)
high k
large A
Biot number
conductive resistance (R_int) / convective resistance (R_ext)
thermal diffusivity
alpha = k / rho*cp
What happens to the series solution when t is large?
The exponential terms drop off more quickly, so you don’t need as many terms for a good approximation
What are long times?
Fo > 0.2
Conditions to use Heisler
uniform initial temp (T_i)
constant boundary fluid temp (T_inf)
perfect geometry
far from edges
no heat gen
constant thermal properties
long times
Semi-infinite region
extends to infinity in two directions
has a single identifiable surface in another direction (depth)
idealization of heat transfer for short times and/or tick material
In reality do semi-infinite regions exist
No, it’s simply an idealization
When can we use the series approach?
Fo > 0.2 (long times)
When should we use semi-infinite approach?
Thickness >= 4sqrt(alpha*t)
What are the two forms of convective heat transfer
free/natural - driven by material density
forced - due to external force
What is the velocity boundary layer
a small layer of fluid where most of the change in the fluid’s velocity happens (0—> u_inf)
When does the thermal boundary layer exist?
If there is a temperature difference between the surface and bulk fluid
Reynolds number (Re)
ratio of inertia to viscous force
Prandtl number (Pr)
ratio of momentum diffusivity and thermal diffusivity
Does flux change along the flow?
Yes, ask you move down the plate the boundary layer changes thickness and the temperature gradient changes.
When is flux along the plat the highest?
Start of the plate b/c it has the biggest gradient here
Laminar flow
Re < 2e5
orderly
Turbulent flow
Re > 3 e 5
chaotic
Nusselt number (Nu)
ratio of the fluid’s conductive resistance to the fluid’s convective resistance
depends on type of convection
forces (Re, Pr)
natural (Ra, Pr)
What happens when the fluid velocity is increased?
more heat transfer
thinner boundary layer (smaller diff over which temp change observed)
What is the characteristic length for convection?
entire length of plate or diameter of long cylinder/sphere
Grashof number (Gr)
ratio of the bouyancy to viscous force on fluid
Rayleigh number (Ra)
buoyancy-driven flow in natural convection
latent heat of fusion
enthalpy difference due to change of phase from solid —> liquid (occurs at melting temp Tm)
latent heat of vaporization
enthalpy difference due to change of phase from liquid —> vapor (occurs at boiling temp)
Freezing stages of pure water
supercooling
nucleation
crystal growth
maturation
What happens to water at it freezes?
volume and density change, high degree of expansion, k increases (takes longer to thaw)
Freezing stages in tissues
intracellular and extracellular fluid reach melting temp
ice nucleation begins in extracellular space first
plasma membrane prevents ice crystals into cytoplasm
osmotic pressure develops
water flows out of cell and freezes there (causes cellular dehydration)
mass concentration vs molar concentration
mass concentration = mass / unit vol
molar concentration = moles / unit vol
related by molecular weight
What is solubility
The extent to which a solute is dissolved in a solvent
Henry’s law
describes the pressure dependence of the solubility of a gas in solution
Hygroscopic vs. non-hygroscopic
hygroscopic - vapor pressure surrounding solid is a function of solid temperature AND moisture content
non-hygroscopic - vapor pressure surrounding a solid is only a function of termperature
Arrhenius law
rxn rate general increate with temperature
What is k”
partition coefficient; explains solid liquid equilibrium
What variable determines if the convection is forced or natural?
free fluid velocity (u_inf). If this value is zero, then natural.