9.1 Definition

The magnetic surface average of a physical quantity G(ψ,𝜃,ϕ) is defined by

             ∫ ∫ ∫
           (     ΔΨ Gd3V )
⟨G ⟩ ≡ ΔliΨm→0  ∫-∫ ∫--d3V-- ,
                 Δ Ψ
(221)

where the volume integration is over a small volume between two adjacent flux surfaces with Ψ differing by Ψ. [This formula (with finite ΔΨ) is used in TEK code to calculate the radial heat flux.]

The above 3D volume integration can also be written as a 2D surface integration. The differential volume element is given by d3V = |𝒥|dψd𝜃dϕ, where 𝒥 is the Jacobian of (ψ,𝜃,ϕ) coordinates. Using this, equation (221) is written as

          ( ∫ ∫ ∫             )
⟨G⟩ = lim    -∫ ∫-Δ∫Ψ-G|𝒥-|dψd𝜃dϕ
     Δ∫Ψ ∫→0       ΔΨ |𝒥 |dψd 𝜃dϕ
      ---G|𝒥|d𝜃dϕ-
   =  ∫ ∫ |𝒥 |d𝜃dϕ ,                                 (222)
which is a 2D averaging over a magnetic surface and thus is called magnetic surface average. Note that the surface averaging of any n0 harmonic is zero (n is the toroidal mode number). Therefore the magnetic surface average contains only the contribution from the n = 0 component, i.e., axisymmetric component. (On the other hand, m0 poloidal harmonics of G can contribute to the surface average since the Jacobian has a poloidal angle dependence.) Using this and noting that 𝒥 is axisymmetric, then expression (222) is written as
      ∫
⟨G⟩ = -G0(∫ψ,𝜃)|𝒥|d𝜃,
           |𝒥 |d𝜃
(223)

where G0(𝜃) is defined by the following Fourier expansion:

     +∑∞
G =      Gn(ψ,𝜃)exp(− inϕ).
    n=−∞
(224)

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“Zonal” and “mean” components

Gis sometimes called the “zonal” component of G if the radial wavelength of Gis much smaller than the equilibrium scale length. If the radial wavelength of Gis comparable to the equilibrium scale length, Gis usually called “mean” component in tokamak literature. For example, mean flows are of system space scale and thus are easy to be observed in experiments. On the other hand, the “zonal” flow, which usually refers to the turbulence generated secondary flow, is of much smaller radial scale (the radial wavelength of zonal flow is of several Larmor radius) and thus is difficult to observe in experiments.

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Sometimes, we do not want the Jacobian to explicitly appear in the formula. This can be achieved by writing the differential volume element as

d3V = Rd ϕ-dΨ-dl .
          |∇ Ψ|  p
(225)

Using Bp = |∇Ψ|∕R, the volume element is further written as

        dΨ
d3V = dϕ---dlp
        Bp
(226)

Using this, the averaging defined in Eq. (221) is written as

           ∫ ∫ ∫      dΨ
⟨G ⟩ = lim  -∫-∫Δ ∫-Ψ Gd-ϕBpdlp
      ΔΨ→0      ΔΨ dϕdBΨpdlp
      ∫ ∫ G-1dϕdl
    = -∫-∫-Bp----p.                              (227)
          B1p dϕdlp
If G is axisymmetric, then the above equation is written as
      ∮ G-1 dlp
⟨G ⟩ =-∮-B1p---.
         Bpdlp
(228)

(Equation (228) is used in the GTAW code to calculate the magnetic surface averaging.) Using Eq. (168) and Bp = |∇Ψ|∕R, equation (228) can also be written as

     ∫ 2π G|𝒥|d𝜃
⟨G ⟩ =-0∫2π------.
       0 |𝒥 |d𝜃
(229)

Using the expression of the volume element = |𝒥|d𝜃dϕdψ, the volume within a magnetic surface is written

       ∫      ∫               ∫ ψ ∫ 2π
V (ψ) =  dτ =   |𝒥|d𝜃dϕdψ = 2π ψ   0  |𝒥 |d𝜃dψ.
                                0
(230)

Using this, the differential of V with respect to ψ is written as

 ′   dV     ∫ 2π
V ≡  dψ-= 2π    |𝒥|d𝜃.
             0
(231)

Using this, Eq. (229) is written as

G= 2π-
V ′ 02πG|𝒥|d𝜃