3.2 Force balance in tokamak plasmas

Parallel force balance

Consider the force balance in the direction of B. Dotting the equilibrium equation (56) by B, we obtain

0 = B ⋅∇P,
(57)

which implies that P is constant along a magnetic field line. Since Ψ is also constant along a magnetic field line, P can be expressed in terms of only Ψ on a single magnetic line. Note that this does not necessarily mean P is a single-valued function of Ψ, (i.e. P = P(Ψ)). This is because P still has the freedom of taking different value on different magnetic field lines with the same value of Ψ while still satisfying B ⋅∇P = 0. This situation can appear when there are saddle points (X points) in Ψ contours (refer to Sec. A.10) and P takes different functions of Ψ in islands of Ψ sepearated by a X point. For pressure within a single island of Ψ, P = P(Ψ) can be safely assumed.

On the other hand, if P = P(Ψ), then we obtain

B ⋅∇P = dP-
dΨB ⋅∇Ψ = 0,

i.e., Eq. (57) is satisfied, indicating P = P(Ψ) is a sufficient condition for the force balance in the parallel (to the magnetic field) direction.

Toroidal force balance

Next, consider the ϕ component of Eq. (56), which is written

                1∂P
JZBR  − JRBZ = R--∂ϕ.
(58)

Since P = P(Ψ), which implies ∂P∕∂ϕ = 0, equation (58) reduces to

JZBR − JRBZ  = 0
(59)

Using the expressions of the poloidal current density (50) and (51) in the force balance equation (59) yields

∂g      ∂g
---BR + ---BZ = 0,
∂R      ∂Z
(60)

which can be further written

B ⋅∇g = 0.
(61)

According to the same reasoning for the pressure, we conclude that g = g(Ψ) is a sufficient condition for the toroidal force balance. (The function g defined here is usually called the “poloidal current function” in tokamak literature. The reason for this name is discussed in Sec. A.3.)

Force balance along the major radius: Grad-Shafranov equation

Next, consider the force balance in ˆR direction. The Rˆ component of the force balance equation (56) is written

JϕBZ − JZB ϕ = ∂P
              ∂R
(62)

Using the expressions of the current density and magnetic field [Eqs. (6), (51), and (54)], equation (62) is written

− 1△ ∗Ψ-1∂Ψ- − 1-∂g-g-= μ0∂P-.
  R    R ∂R    R ∂R R     ∂R
(63)

Assuming the sufficient condition discussed above, i.e., P and g are a function of only Ψ, i.e., P = P(Ψ) and g = g(Ψ), Eq. (63) is written

− 1△ ∗Ψ 1∂-Ψ − 1-dg-∂Ψ-g-= μ0dP-∂Ψ-,
  R     R∂R    R dΨ ∂R R     dΨ ∂R
(64)

which can be simplified to

△∗Ψ = − μ R2dP-− -dgg,
         0  dΨ   dΨ
(65)

i.e.,

 ∂2Ψ      ∂ ( 1 ∂Ψ )         dP   dg
∂Z2- +R ∂R-  R-∂R-  = − μ0R2 dΨ-− dΨg.
(66)

Equation (66) is known as Grad-Shafranov (GS) equation.

[Note that the Z component of the force balance equation is written

JRBϕ JϕBR = ∂P-
∂Z
⇒−-∂g-
∂Z1-
R-g
R -1
RΨ1-
R∂Ψ-
∂Z = μ0dP-
dΨ∂Ψ-
∂Z
⇒−-dg
dΨ∂Ψ-
∂Z1-
Rg-
R 1-
RΨ-1
R∂Ψ-
∂Z = μ0dP
dΨ∂Ψ-
∂Z
⇒−-dg
dΨ1-
R-g
R -1
RΨ1-
R = μ0dP
dΨ
⇒△Ψ = μ0R2dP
dΨ dg
dΨg

which turns out to be identical with the Grad-Shafranov equation. This is not a coincidence. The reason is that the force balance equation has been satisfied in three different directions (namely, ˆ
ϕ, ˆ
R, and B direction) and thus it must be satisfied in all the directions.]

Using the GS equation, Jϕ can also be expressed as

      1  (    dP    dg )
Jϕ = ---- μ0R2--- + --g  .
     μ0R       dΨ   dΨ
(67)