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Scalar dissipation energy spectrum

As discussed in Section 2.1, in high-Reynolds-number turbulent flows the scalar dissipation rate is equal to the rate of energy transfer through the inertial range of the turbulence energy spectrum. The usual modeling approach is thus to use a transport equation for the transfer rate instead of the detailed balance equation for the dissipation rate derived from (1.27). Nevertheless, in order to understand better the small-scale physical phenomena that determine e, we will derive its transport equation starting from (2.99). [Pg.70]

Likewise, the scalar dissipation rate is related to the scalar energy spectrum by... [Pg.91]

As in Section 2.1 for the turbulent energy spectrum, a model scalar energy spectrum can be developed to describe lop(n). However, one must account for the effect of the Schmidt number. For Sc < 1, the scalar-dissipation wavenumbers, defined by19... [Pg.92]

Note that as Re/, goes to infinity with Sc constant, both the turbulent energy spectrum and the scalar energy spectrum will be dominated by the energy-containing and inertial/inertial-convective sub-ranges. Thus, in this limit, the characteristic time scale for scalar variance dissipation defined by (3.55) becomes... [Pg.92]

The scalar-dissipation wavenumber /cd is defined in terms of /cdi by /cd = Sc1/2kdi-Like the fraction of the turbulent kinetic energy in the dissipation range kn ((2.139), p. 54), for a fully developed scalar spectrum the fraction of scalar variance in the scalar dissipation range scales with Reynolds number as... [Pg.107]

When the scalar spectrum is not fully developed, the vortex-stretching term Vf will depend on the scalar spectral energy transfer rate evaluated at the scalar-dissipation wavenumber 7 (kd, O-32 Like the vortex-stretching term Vf appearing in the transport... [Pg.107]

Figure 4.9. Sketch of CSTR representation of the SR model for 1 < Sc. Each wavenumber band is assumed to be well mixed in the sense that it can be represented by a single variable

Figure 4.9. Sketch of CSTR representation of the SR model for 1 < Sc. Each wavenumber band is assumed to be well mixed in the sense that it can be represented by a single variable <p 2)n- Scalar energy cascades from large scales to the dissipative range where it is destroyed. Backscatter also occurs in the opposite direction, and ensures that any arbitrary initial spectrum will eventually attain a self-similar equilibrium form. In the presence of a mean scalar gradient, scalar energy is added to the system by the scalar-flux energy spectrum. The fraction of this energy that falls in a particular wavenumber band is determined by forcing the self-similar spectrum for Sc = 1 to be the same for all values of the mean-gradient source term.

See other pages where Scalar dissipation energy spectrum is mentioned: [Pg.81]    [Pg.91]    [Pg.123]    [Pg.146]    [Pg.148]    [Pg.62]    [Pg.72]    [Pg.104]    [Pg.127]    [Pg.129]    [Pg.104]    [Pg.85]   
See also in sourсe #XX -- [ Pg.72 , Pg.75 , Pg.369 ]

See also in sourсe #XX -- [ Pg.72 , Pg.75 , Pg.369 ]




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