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8.2 Approved modes for ultrasound therapy   197




                   Table 8.4  Types of acoustic streaming and specifications [9].
                   Streaming       Assumptions           Characteristics
                   Slow            U <<  u Re  << 1       U ∝  u                                                                         U ∝u
                                    0    19                0  1                                                                          U <<u19Re<<1
                                                                                                                                            1
                                                                                                                                           0
                                                                                                                                           0
                                                          F (acoustic force) ∝ α u 2 1                                                   F   (acoustic force)∝αu12
                                                          u ( ⋅∇  u ) (Convective acceleration) 0                                        (u⋅∝)u   (Convective acceleration)∝0
                                                                                 ≈
                   Fast            U ≥  u R ≥ 1          For coarse-grained streaming,                                                   U ≥u19Re≥1
                                                                2+
                                                                 n
                                                                                                                                           0
                                    0   19  e             U ∝ α u 1  , n is value for                                                    U ∝αu12+n
                                                           0
                                                                                                                                           0
                                                         nonlinearity of the wave,
                                                              u Convective acceleration)
                                                          u ( ⋅∇ ) (                                                                     u⋅∝uConvective acceleration
                                                         Is significant.
                   Coarse-grained   Traveling acoustic wave   Streaming away from sound source
                   (multidimensional)   from single source along   into viscous fluid. The Reynolds
                   Eckart          an axis               number determines whether
                                   L  (characteristic length   the streaming is fast or slow.                                            *****
                                   scale) >>  λ                   L                                                                      >>λ
                                                          Re  =  ρ U                                                                     Re*****=ρfU *****µ
                                                            L  f  0  µ                                                                            0
                   One-dimensional   u ( ⋅∇  u ) =  0    Streaming away from sound
                   Eckart                                source into unbounded fluid. The                                                u⋅∝u=0
                                   Momentum equation is   Reynolds number determines
                                   linear.               whether the streaming is fast or slow.
                                   Traveling acoustic wave        L
                                   from single planner source   Re L  =  ρ f U 0
                                   with  L >>  λ                  µ                                                                      Re*****=ρfU *****µ
                                                                                                                                         *****>>λ
                                                                                                                                                  0
                   Medium-grained   Acoustic wave bounded   The Reynolds number determines
                   (Rayleigh)      along sound propagation   whether the streaming is fast or slow.
                                   path: standing acoustic        L
                                   wave. Incompressible   Re L  =  ρ f U 0
                                   everywhere and inviscid in     µ                                                                      Re*****=ρfU *****µ
                                                                                                                                                  0
                                   bulk of fluid         Vortex flow; the scale of the vortices
                                                         is approximately the same as the λ.
                                                         Analysis valid only outside viscous
                                                         boundary layer.
                   Fine-grained    Acoustic wave         The Reynolds number determines
                   (Schlichting)   bounded along sound   whether the streaming is fast or slow.
                                   propagation path:              L
                                   standing acoustic wave.   Re L  =  ρ f U 0  µ                                                         Re*****=ρfU *****µ
                                   Classical assumptions:                                                                                         0
                                   incompressible everywhere   Bounded along sound propagation
                                   and inviscid in bulk of fluid.  path: standing wave. Vortex flow; the
                                                         scale of the vortices is approximately
                                                         the same as the λ.
                   U 0 , streaming velocity; u 1 , acoustic particle velocity.
                  of the sound flow for 80°C water to be increased by 50% between two rigid parallel
                  plates. For particles of the same density as the fluid, the effects of viscosity on the
                  ultrasound force are negligible, but as the density of particles increases, the viscosity
                  effects increase by up to 30%.
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