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what does the karman reduce to flat plate |
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Stationary and Moving bodies under influences of F |
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Branch of mechanics that deals with bodies at REST |
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Branch of mechanics that deal with bodies in motion |
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behavior of fluids in motion or at rest and their interaction with solids or other boundaries |
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Same as FM, but sets fluids at rest to V=0 |
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Study of motion of fluids that can be approx as INCOMPRESSOBLE |
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Nusselt number = convection heat transfer/conduction heat transfer =hL/k |
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a fluid always deforms under shear stress |
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Stress and strain is proportional in solids, but in fluid, stress is proportional to strain rate |
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Pressure P in relation to stress |
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P is normal stress in fluid at rest |
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GAS vs LIQUID wict filling space |
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gas fills entire available space, liquid forms free surface |
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Fluid sticks to solid surface - forms boundary layer due to viscocity |
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Viscous vs Inviscid regions of flow |
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visc - flows in which friction effects are significant invisc - viscos forces are nigligibly small compared to inertial or pressure forces |
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Flow speed in form of Ma and incompressible approx |
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Ma = V/c - approx inc if Ma < 0,3 this is because that usually approx less that 5% density change |
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Steady - no change at a point w/time |
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No change with location over specified region |
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quantity of matter or region in space chosen to study |
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The mass or region outside the system |
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real or imaginary surface that separates the system from the surrounding (either fixed or movable |
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fixed amount of mass, no mass accross boundary |
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Properly selected region in space |
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speed of sound for ideal gas |
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viscoucity def/forklaring |
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resistance to deformation |
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Deformation is proportional to shear stress |
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Viscocity in liquids vs gases IRT temp |
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visc down when temp up for liquids, up when temp up for gasses. |
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"a curve that is everywhere tangent to the instantanious local velocity vector" For steady, incomp 2d: u=(dY/dy) v=-(dY/dx) |
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follow path of one particle over a time period |
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Insert several particles and take instantanious pic |
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Steady flow IRT stream, path and streakline |
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all the same when flow is steady |
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Rate of heat transfer for flat plate |
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curves of constant scalar properties |
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Inviscid region of flow (when to approx) |
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for steady incomp flow - (du/dx)+(dv/dy)+(dw/dz)=0 |
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When can you use stream and potential function? |
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For incompressible, steady, irrotational 2-d |
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What is friction force equal to on flat plate? |
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Same as Tw*A (because Tw=(Ft/A)) |
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h is equal to heat transfer coefficient |
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Tau - what is this equal to (in terms of differential)? |
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translation, rotation, linear strain shear strain |
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Why do we use nondim navier stokes? |
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to see relative effects of terms, and where one or more overpowers the other terms |
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what is the Modified reynolds analogy |
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It allows you to calculate heat transfer coeff from knowledge of friction. |
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what is residual in CFD context |
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it is a measure of how much our variables differ from the exact solutions. -put all terms on one side, the difference from zero is residual. |
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starting point to get to a solutions. wrong in the beginning, but get more and more correct as we iterate. |
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numerical method of marching towards solution |
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solution converges to true value (not necessarilly) |
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volume flow rate through pipe |
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V'=integral(0-2pi)integral(0-R)(u(r)*r)dr(d(theta) = 2pi*integral(0-R)(u(r)*r)dr
flrste integralet blir 2pi, husk å gange med r på nste integral. |
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Hva må du huske når du tar med tyngdekraft i navier stokes? |
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Tyngdekraften fungerer som en dP/dy- altså navier stokes forkortes til dP/dy = rho*gy |
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Reynolds analogy limitations |
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limted to flows of fluid with prantl near unity such as gases and negiligable pressure gradient in flow direction |
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Hva gjør du for å finne pressure field for u og v? |
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1 - sjekk for continuity 2 -kort ned navier stokes - finn deretter dP/dx fra x momentun og deretter dP/dy fra y momentum. 3 sjekk for smooth function!! dP/(dxdy) skal være lik dP(dydx) - dersom dette ikke stemmer er det ikke smooth function, og vi kan ikke fortsette |
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boundary conditions for oil film wall |
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dv/dx = 0 ved x lik h! gå tilbake til dv/dx og sett inn x lik h - løs for C1 |
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hvordan kan du bevise at en fartsprofil bare er funsksjon av en variabel tidlig? |
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Sett inn i continuity equation - så står du igjen med kun f.eks. du/dx=0 - som sier at u bare er funksjon av x |
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Can wald interval be trusted? when? |
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Helst høy n - en dersom distibusjonen er normal eller approx normal kan vi stole på den d også |
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