UNSTEADY VISCOUS FLOW Du 2 g p u Dt Assume linear, horizontal motion u t 1 p x u 2 y 2 Viscous effects confined to within some finite area near the boundary → boundary layer In unsteady viscous flows at low Re the boundary layer thickness δ grows with time; but in periodic flows, it remains constant If the pressure gradient is zero, Navier-Stokes equation (in x) reduces to: u t u 2 y 2 u t u 2 y 2 Heat Equation– parabolic partial differential equation - linear Requires one initial condition and two boundary conditions u x , y ,t 0 0 @ y u 0 @ y 0 u U Impulsively started plate – Stokes first problem y U Total of three conditions u t u 2 y 2 Heat Equation– parabolic partial differential equation Can be solved by “Separation of Variables” Suppose we have a solution: u y , t Y y T t Substituting in the diff eq: May also be written as: Y y T t t 2 y 2 Y y T t Y y T t Y y T t Moving variables to same side: T t T t The two sides have to be equal for any choice of y and t , The minus sign in front of k is for convenience Y y Y y T t T t Y y Y y k T t T t Y y Y y Y kY 0 Y T k T 0 y t t T T u x , y , t 0 0 u y , t Y y T t 2 T T This equation contains a pair of ordinary differential equations: k 2 kY 0 @ y k T 0 @ y 0 0 Y u 0 U Y 0 u U 0 T 0 k T 0 k t Y T T k 2 y 2 kY 0 ln T k t A t Y B cos k y C sin ky T Ae k t Y B cos k y C sin ky n Applying B.C., kn B = 0; C =1; L u y , t Y y T t 2 2 u An e n t L ny sin L u Ue increasing time y 2 4 t Alternative solution to“Separation of Variables” – “Similarity Solution” u t u u x , y ,t 0 0 y @ y 2 2 u 0 @ y 0 New independent variable: y t t y 2 d u Substituting into 2 2t d 4 t d heat equation: d 2 t d 2 y u from: 2 t η is used to transform heat equation: du u U d y d 1 d d 2 d 2t d 1 d 2 t d 2 2 2 y 2 4 t d d u u 2 du d 0 2 d u d 2 2 du d u 0 0 as @ @ 0 2 BC turn into 1 u 0 u U du To transform second f order into first order: d df d 2 f 0 With solution: df f e 2 d f Ae 2 erf 2 Integrating to u A e d B obtain u: 0 2 Or in terms of the error function: erf 2 e 2 d u U 1 erf 0 For η > 2 the error function is nearly 1, so that u → 0 u U 1 erf For η > 2 the error function is nearly 1, so that u → 0 Then, viscous effects are confined to the region η < 2 This is the boundary layer δ y 2 t 2 2 t 4 t δ grows as the squared root of time increasing time u U 1 erf y 2 t UNSTEADY VISCOUS FLOW Oscillating Plate – Stokes’ second problem u t u 2 y 2 @ y u bounded @ y 0 u U cos t y Ucos(ωt) Look for a solution of the form: u Y y cos t Re Y y e i t e i t cos t i sin t Euler’s formula u Re Y y e Fourier’s transform in the time domain: u Substitution into: t Ye i t i Ye i t t u y 2 y Y A exp 1 i Y 0 e Y 2 U Y 0 Y 0 y 2 i t i y Y 2 Y i Y 2 Y 0 i y 1 i 2 y B exp 1 i 2 B 0 2 2 2 B.C. in Y u 2 i t Y 0 U Y U exp 1 i A U y 2 y 2 2 Y U exp 1 i Most of the motion is confined to region within: y 2 2 u Re Ye i t Ue y y cos t @ y y Ue Ue 1 0 . 37 U @ y 4 / y Ue Ue 4 2 Ue 0 . 06 U y Ucos(ωt) u Ue y y cos t UNSTEADY VISCOUS FLOW Oscillating Plate u t u 2 y 2 @ y W u 0 W y @ y 0 u U cos t Ucos(ωt) Look for a solution of the form: u Y y cos t Re Y y e i t e i t cos t i sin t Euler’s formula u Re Y y e Fourier’s transform in the time domain: u Substitution into: t Ye i t i Ye i t t u y 2 y Y A exp 1 i A B U 2 e Y 2 Y 0 U Y W 2 y i t i Y y 2 Y 0 0 Y 2 i Y i y 2 1 i 2 y B exp 1 i 2 0 A exp 1 i 2 2 2 B.C. in Y u 2 i t y 2 W B exp 1 i 2 W 2 A B U 0 Ae W 1 i 0 U B e B Y U Ue Be 2 sinh 1 i W 1 i Be e e e A U 1 2 sinh sinh (1 i )( W y ) sinh (1 i )W W 2 sinh Y Ae y Be y @W sinh (1 i )W (1 i )W Y U sinh (1 i )( W y ) sinh (1 i )W Y U W y W y U 1 W y u U 1 cos t W @ W e e sinh (1 i )W 2 sinh 1 ( 1 i ) W 2e (1 i ) y Y U exp Same solution as for unbounded oscillating plate y u U 1 cos t W