UA PSIO 472 - Quantitative modeling of biological systems

Unformatted text preview:

1Physiology 472/572 - 2010 - Quantitative modeling of biological systems Lecture 14: Stresses in a fluid, Navier-Stokes equations Example of normal stress • a fluid at rest – hydrostatic equilibrium - no shear stress • stress vector T = -pn • all surfaces feel a pressure pushing in on them (imagine swimming deep under water) • p is the hydrostatic pressure • stress tensor is σij = -pδij, i.e., ⎥⎥⎥⎦⎤⎢⎢⎢⎣⎡−−−=ppp000000σ • δij is the Kronecker delta: δij = 1 if i = j, δij = 0 if i ≠ j Incompressible fluid • water and other fluids have little density change under forces encountered in the body • can assume constant density Pressure in an incompressible fluid under gravity • consider a force balance • force on top surface = - p2 A • force on bottom surface = + p1 A • force of gravity = - ρ A(z2 - z1) g • total force is zero so p1 - p2 = ρ g (z2 - z1) • still holds even in a more complicated container2Example -mercury manometer • used in measuring blood pressure • from above, pc - pa = ρ g h • for mercury, ρ = 1.35 x 104 kg/m3, g = 9.81 m/s2 • consider h = 1 mm, then pc - pa = 133.3 Pa = 1333 dyn/cm2 = 1 mmHg • mmHg is often used as a unit of pressure Shear flow of a fluid • two parallel plates, one fixed (u = 0), one moving (u = U) • fluid in space between • fluid resists motion, force τΔS acts on area ΔS of fluid surface • produces shear stress in fluid • by force balance on a control volume, τ must be constant with y Newtonian fluids • for many fluids, shear stress is proportional to velocity gradient • constant of proportionality is viscosity μ No-slip condition • fluid adjacent to a solid surface moves with the surface • true for any continuum Velocity profile in shear flow • suppose u = u(y), τ = μ du/dy for a Newtonian fluid • when y = 0, u = 0 - no slip condition • when y = h, u = U3• τ is constant so u = Uy/h, τ = μU/h • viscous drag is proportional to viscosity • viscous drag is inversely proportional to spacing h Viscosity • units are stress/(velocity/distance) • in SI, Pa⋅s, in cgs, dyn⋅s/cm2 = P (Poise) • 1 P = 0.1 Pa⋅s, 1 cP = 0.001 Pa⋅s ~ viscosity of water • viscosity depends on temperature • for Newtonian fluids (air, water, etc) does not depend on velocity gradient • for many biological fluids, viscosity varies with velocity gradient - "Non-Newtonian" Incompressible fluid • for an incompressible fluid, ∇.u = ∂ui/∂xi = 0 • prove by considering a small control volume δx1 × δx2 × δx3 Stress tensor in a viscous incompressible fluid • recall τ = μ du/dy for a Newtonian fluid in shear flow • stress tensor must be symmetric (conservation of angular momentum) • in tensor form, the stress in simple shear flow is ⎥⎥⎥⎦⎤⎢⎢⎢⎣⎡ττ=0000000σ where τ = μ ∂u1/∂x2 using index notation • in a general flow, represent velocity field as u(x,t) • all the components of ∂ui/∂xj may be non-zero • viscous stress is σij (viscous) = μ (∂ui/∂xj + ∂uj/∂xi)4• total stress is (hydrostatic pressure) + (viscosity) × (velocity gradients) • σij = -pδij + μ (∂ui/∂xj + ∂uj/∂xi), i.e., σ = -pI + μ (∂u/∂x + (∂u/∂x)T) Fluid velocity and acceleration • to find acceleration of fluid, must take derivative of velocity traveling with fluid • if fluid moves from a low-speed to a high speed area, it speeds up, even if the velocity stays constant at each point • e.g. in one dimension, acceleration of fluid = ∂u/∂t + u ∂u/∂x • second term called advective acceleration • in the general case, fluid acceleration = ∂u/∂t + u . ∇u Navier-Stokes equations • general idea is to apply conservation of momentum • fluid may have a body force F (per unit volume) acting on it (e.g., gravity) • resultant force of stress in fluid (per unit volume) = ∇ . σ • conservation of momentum per unit volume gives ρ (∂u/∂t + u . ∇u) = ∇ . σ + F • (∇ . σ)j = (∂/∂xi) (-pδij + μ (∂ui/∂xj + ∂uj/∂xi)) = - ∂p/∂xj + μ ∇2uj using incompressibility condition • or ∇ . σ = -∇p + μ ∇2u • ρ (∂u/∂t + u . ∇u) = -∇p + μ ∇2u + F • Navier-Stokes equations in terms of (u,v,w) and (x,y,z) : 0 = zw + yv + xuF + w + zp- = ]zw w+ yw v+ xw[u + tw F + v + yp- = ]zv w+ yv v+ xv[u + tv F +u + xp- = ]zu w+ yu v+ xu[u + tu


View Full Document
Download Quantitative modeling of biological systems
Our administrator received your request to download this document. We will send you the file to your email shortly.
Loading Unlocking...
Login

Join to view Quantitative modeling of biological systems and access 3M+ class-specific study document.

or
We will never post anything without your permission.
Don't have an account?
Sign Up

Join to view Quantitative modeling of biological systems 2 2 and access 3M+ class-specific study document.

or

By creating an account you agree to our Privacy Policy and Terms Of Use

Already a member?