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Transcript of Cell Process 1. Cell and transport phenomena (2) Liang Yu Department of Biological Systems...
Cell Process1. Cell and transport phenomena (2)
Liang Yu
Department of Biological Systems Engineering
Washington State University
02. 12. 2013
Main topics
Cell and transport phenomena
High performance computation
Metabolic reactions and C-13 validation
Enzyme and molecular simulation
Physiological Fluid Mechanics
FluidA material that deforms continuously when subjected to a force applied tangentially to a surface
Biological fluidQuite complex, exhibiting solid and liquid-like behavior and deforming in a time-dependent fashion
Fluid mechanicsThe study of the motion of fluids in response to the application of stresses
Physiological Fluid MechanicsConcerned with fluid flow within organisms and the relation between fluid flow and physiological processes
Conservation relations and momentum balances
Fluid kinematics: describe fluid motion in time and space
Eulerian description: observing motion from a fixed reference frame
Lagrangian description: observing motion from a moving reference frame
Deference between Eulerian and Lagrangian description
River bank
If record the motion from the riverbank, Eulerian description (fixed reference frame )
If you are on the boat as it drifts with the current, Lagrangian description (moving)
Eulerian approach
Describes the flow field (velocity, acceleration, pressure, temperature, etc.) as functions of position and time
Do not follow particles, i.e. different particles will flow through the same point at different times
Relatively low computation, most fluid mechanics textbooks and papers use this system
The time-change of the velocity in such a measurement
Called the partial derivative of the temperature with respect to time, or local accelerate
, ,x y z
v
t
Velocity field: , , ,v v x y z t
(x,y,z)
Fluid element and properties
• The behavior of the fluid is described in terms of macroscopic properties:– Velocity u.– Pressure p.– Density .r– Temperature T.– Energy E.
• Properties are averages of a sufficiently large number of molecules.
• A fluid element can be thought of as the smallest volume for which the continuum assumption is valid.
xy
z
dy
dx
Faces are labeled North, East, West,
South, Top and Bottom
dz
Lagrangian approach
Follow individual particles, positions of specified particles are the objectives
Track (or follow) it as it moves, and monitor change in its properties
The properties may be velocity, temperature, density, mass, or concentration, etc in the flow field
The recorded properties are associated with the same fluid particle, but at different locations and at different times
The time-change of the velocity in such a measurement
Dv
Dt
Called material derivative or substantial derivative. It reflects time change in the velocity (or any other properties) of the tagged fluid particles as observed by an observer moving with the fluid. Lagrangian approach is also called “particle based approach”.
Lagrangian approach
Relatively high computation, difficult to use for practical flow analysis
Fluids are composed of billions of molecules
Interaction between molecules hard to describe/model
, , ,AA A A
dyv x y z t
dt
, , ,AA A A
dzw x y z t
dt
, , ,AA A A
dxu x y z t
dt
The above equations determine the path of the particle A if the position is specified at some initial instant in its path history
Acceleration
, , ,v v x y z t
Fluid velocity is a function of the three spatial coordinates x, y, z, and if the flow is unsteady, time t
The total differential is defined as v v v v
dv dx dy dz dtx y z t
dv v dx v dy v dz v
dt x dt y dt z dt t
Acceleration is a vector defined as the rate of change of velocity
x y z
v v v va v v v
x y z t
Local acceleration Convective acceleration
Dv vv v
Dt t
Rate of change for a fluid particle• Terminology: fluid element is a volume stationary in
space, and fluid particle is a volume of fluid moving with the flow.
• A moving fluid particle experiences two rates of changes:– Change due to changes in the fluid as a function of time.– Change due to the fact that it moves to a different location in the
fluid with different conditions.
• The sum of these two rates of changes for a property per unit mass is called the total or substantive derivative D /Dt:
• With dx/dt=u, dy/dt=v, dz/dt=w, this results in:dt
dz
zdt
dy
ydt
dx
xtDt
D
grad
tDt
D.u
Rate of change for a stationary fluid element
• In most cases we are interested in the changes of a flow property for a fluid element, or fluid volume, that is stationary in space.
• However, some equations are easier derived for fluid particles. For a moving fluid particle, the total derivative per unit volume of this property f is given by:
• For a fluid element, for an arbitrary conserved property f :
grad
tDt
D.u
0)( u div
t 0)()(
udiv
t
Continuity equation Arbitrary property
(for moving fluid particle) (for given location in space)
Dt
Ddiv
tgrad
tdiv
t
)(.)()(
uuu
zero because of continuity
Dt
Ddiv
t
)(
)(u
Rate of increase of of fluid element
Net rate of flow of out of fluid element
Rate of increase of for a fluid particle=
Fluid particle and fluid element• We can derive the relationship between the equations for a
fluid particle (Lagrangian) and a fluid element (Eulerian) as follows:
Control volumes
A convenient region of space
For examining the flow of
mass, momentum, and energy
Control volume is arbitrary
Control volume can be fixed in
size or may change size with
time
Simple geometry is square (2D)
or cube (3D)
Continuity equation• Rate of increase of mass in fluid element equals the
net rate of flow of mass into element.• Rate of increase is:• The inflows (positive) and outflows (negative) are
shown here:
zyxt
zyxt
)(
xy
z
( ) 1.2
ww z x y
z
( ) 1
.2
vv y x z
y
zyxx
uu
2
1.)(
zxyy
vv
2
1.)(
yxzz
ww
2
1.)(
( ) 1.2
uu x y z
x
Continuity equation
• Summing all terms in the previous slide and dividing by the volume xyz results in:
• In vector notation:
• For incompressible fluids r / t = 0, and the equation becomes:
div u = 0.• Alternative ways to write this: and
0)()()(
zw
yv
xu
t
0)( u div
t
Change in density Net flow of mass across boundariesConvective term
0
zw
yv
xu 0
i
ixu
Navier–Stokes equation (Momentum equation )
Describe the motion of fluid substances
Applying Newton's second law to fluid motion
Assumption the fluid stress is the sum of a diffusing viscous term (proportional to the gradient of velocity) and a pressure term - hence describing viscous flow
Constant density, ρ
Constant viscosity, μ
Continuity (incompressible flow)
A solution of the Navier–Stokes equations is called a velocity field or flow field, which is a description of the velocity of the fluid at a given point in space and time
Momentum equation in three dimensions• Derive conservation equations for momentum for fluid
particles. Then use the above relationships to transform those to an Eulerian frame (for fluid elements).
• Start with deriving the momentum equations from Newton’s second law: rate of change of momentum equals sum of forces.
• Rate of increase of x-, y-, and z-momentum:
• Forces on fluid particles are:– Surface forces such as pressure and viscous forces.– Body forces, which act on a volume, such as gravity, centrifugal,
Coriolis, and electromagnetic forces.
Dt
Dw
Dt
Dv
Dt
Du
Dt
DvmaF
Viscous stresses• Stresses are forces per area.
Unit is N/m2 or Pa.• Viscous stresses denoted by t.• Suffix notation tij is used to
indicate direction.• Nine stress components.
– txx, tyy, tzz are normal stresses. E.g. tzz is the stress in the z-direction on a z-plane.
– Other stresses are shear stresses. E.g. tzy is the stress in the y-direction on a z-plane.
• Forces aligned with the direction of a coordinate axis are positive. Opposite direction is negative.
Forces in the x-direction
x
z
y
zyxx
pp )
2
1.(
zyx
x
pp )
2
1.(
yxzzzx
zx tt )2
1.(
yxzzzx
zx tt )2
1.(
zxyyyx
yx t
t )21.(
zxyyyx
yx t
t )21.(
zyxxxx
xx tt )2
1.(
zyx
xxx
xx tt )2
1.(
Net force in the x-direction is the sum of all the force components in that direction.
Momentum equation
• Set the rate of change of x-momentum for a fluid particle Du/Dt equal to:– the sum of the forces due to surface stresses shown in the previous slide, plus– the body forces. These are usually lumped together into a source term SM:
– p is a compressive stress and txx is a tensile stress.
• Similarly for y- and z-momentum:
Mxzxyxxx Szyx
p
Dt
Du
ttt )(
Myzyyyxy Szy
p
xDtDv
ttt
)(
Mzzzyzxz S
zp
yxDtDw
)( ttt
Application of Momentum balances
Pressure-driven flow through a narrow rectangular
channel
Pressure-driven flow through a Cylindrical tube
Flow is induced by a pressure gradient, which could be produced by a pump or gravity.
These examples also examine the effect of geometry upon the flow and the shear stress.
Flow through these kinds of channels are important in many biomedical devices such as hemodialyzers and ultrafiltration.
Pressure-driven flow through a narrow rectangular channel
Assumption:1. The flow is pressure driven; that is, pressure varies only in the direction of flow2. The fluid density is constant, which indicates that the fluid is incompressible3. The flow is steady; that is, pressure, shear stress and velocity do not change with
time4. The fluid is Newtonian5. Edge effect are neglected. To meet this assumption, we require a long, wide
channel; that is, h/w<<1 and h/L <<1, where w is the width and L is the length of the channel
6. The flow is laminar
Pressure-driven flow through a narrow rectangular channel
Parallel-plate channels are used widely to study the effect of flow on cell adhesion and cell function. Since there is no net momentum flow and the flow is steady, the sum of all forces must equal zero.The only forces arising are those due to pressure and shear stress.
0yx yxx x x x x xp p y z x zt t
A momentum balance in the x direction yields
Pressure-driven flow through a narrow rectangular channel
Dividing by ∆x∆y∆z and taking the limit as each goes to zero results in the ordinary differential equation
yxddp
dx dy
t
The pressure changes only in the x direction (i.e., dp/dx=f(x)) and the shear stress changes in the y direction (i.e., dτ/dy=g(y))
( ) ( )f x g y
Integrate f(x) to yield
1 2p C x C
Pressure-driven flow through a narrow rectangular channel
The pressure can be specified at two locations, away from both the entrance and exit. Thus, at x=x0, p=p0, and at x=xL, p=pL. Defining ∆p=p0-pL and L=xL-x0 to remove C1 and C2
0 0
pp p x x
L
yxd p
dy L
t
Integrate τ to yield
3yx
py C
Lt
Newton’s law of viscosity
xyx
du
dyt
Pressure-driven flow through a narrow rectangular channel
Substitute into Newton’s law of viscosity
3xdu p
y Cdy L
After integrating this equation
2 342x
p C yu y C
L
Apply the boundary condition that ux=0 at y=±h/2
3 0C 24 8
pC h
L
2 2
2
41
8x
ph yu
L h
Pressure-driven flow through a narrow rectangular channel
The velocity is a maximum at y=02
8max
phu
L
2
max 2
41x
yu u
h
The volumetric flow rate is the integral of the velocity over the cross-sectional area
2/2 /2max
max 2/2 0 /2
4 21
3
h w h
xh h
y u whQ u dzdy u w dy
h
Pressure-driven flow through a narrow rectangular channel
Analytic solution
yx
py
Lt
2 2
2
41
8x
ph yu
L h
Numerical solution
yxd p
dy L
t
xyx
du
dyt
Pressure-driven flow through a narrow rectangular channel
function NewtonianFluidFlowRectangular% Pressure-driven flow through a cylindrical tube% Solve momentum equation to obtain shear stress and velocity distribution% Laminar Flow in a Horizontal rectangular channel (Newtonian Fluid)% clear allclc global deltaP L mu HdeltaP = 1;L = 1.5;mu = 1.0e-3;H = 0.1;a = 0;b = H; % Sovle the problem of ODE-BVP% initialize of solution with a guess of y1(r)=0,y2(r)=0,y3(r)=0 solinit = bvpinit(linspace(a,b,100),[0 0 0]);sol = bvp4c(@ODEs,@BCfun,solinit);
Use Matlab to provide analytic solution and numerical solution
∆ p= 1(Pa) H=0.1(m) L=xL-x0=1.5(m) µ= 1.0 x 10-3 (Pa s, N s/m2)
Pressure-driven flow through a narrow rectangular channel
% Analysis resultsh = sol.x/2;TauAnal = deltaP*h/L;uAnal = (deltaP*H^2/(8*mu*L))*(1-(2*h/H).^2);umAnal = deltaP*H^2/(8*mu*L); % Plot% Shear stresstau = sol.y(1,:);%tau = [0 tau];plot(h,tau,'b-',h,TauAnal,'h-.')xlabel('Plane hight h£¬m')ylabel('Shear stress£¬kg/(m s^2)')legend('Numerical results','Analysis results')figure% Velocity distributionplot(h,sol.y(2,:),'b-',h,uAnal,'h-.')xlabel('Plane hight h£¬m')ylabel('Velocity£¬m/s')legend('Numerical results','Analysis results') % Average velocityfprintf('\tAverage velocity: um = %.4f',sol.y(3,end))
Pressure-driven flow through a narrow rectangular channel
function dydh = ODEs(h,y)global deltaP L mu HTau = y(1);u = y(2);um = y(3);dTaudh = deltaP/L/2; dudh = -Tau/mu/2;dumdh = u*2*h/H^2; dydh = [dTaudh; dudh; dumdh]; % ------------------------------------------------------------------function bc = BCfun(ya,yb)bc = [ya(1); yb(2); ya(3)];
Pressure-driven flow through a narrow rectangular channel
Pressure-driven flow through a narrow rectangular channel
We also can use Matlab PDEtool to provide numerical solution
Pressure-driven flow through a narrow rectangular channel
Pressure-driven flow through a narrow rectangular channel
Pressure-driven flow through a narrow rectangular channel
Pressure-driven flow through a narrow rectangular channel
Pressure-driven flow through a narrow rectangular channel
Pressure-driven flow through a narrow rectangular channel
Pressure-driven flow through a narrow rectangular channel
Pressure-driven flow through a narrow rectangular channel
Pressure-driven flow through a narrow rectangular channel
Pressure-driven flow through a narrow rectangular channel
Pressure-driven flow through a narrow rectangular channel
Pressure-driven flow through a narrow rectangular channel
Pressure-driven flow through a narrow rectangular channel
Pressure-driven flow through a narrow rectangular channel
Pressure-driven flow through a narrow rectangular channel
Pressure-driven flow through a narrow rectangular channel