11.4 Kinking and magnetic helicity 353
The three direction gradients∇θ,∇Φ,and∇φform an orthonormal coordinate system
and an element of volume in this system is given by
d^3 r=dlΦdlθdlφ=
dΦdθdφ
∇θ·∇Φ×∇φ
(11.57)
sincedθ=dlθ|∇θ|,dφ=dlφ|∇φ|,anddΦ=dlΦ|∇Φ|. Thus,
Ktwist =
1
4 π^2
∫Φ
0
dΦ
∫ 2 π
θ=0
dθ
∫(2π)−
φ=0
dφ
(
−ψ+Φψ′
)
= −
∫Φ
0
ψdΦ+
∫Φ
0
ψ′ΦdΦ
= 2
∫Φ
0
Φ
dψ
dΦ
dΦ. (11.58)
where the integration limit(2π)−corresponds to being infinitesimally less than 2 π.The last
line has been obtained using the relationship
∫
d(ψΦ)=[ψΦ]surfaceaxis =
∫
Φdψ+
∫
ψdΦ
and noting that the integrated term vanishes sinceψ=0in theflux tube surface andΦ=0
on theflux tube axis.
11.4.3Evaluation ofKwrithe
Connectivity of theflux tube is now the important issue. In order to evaluate theKwrithe
integral the volume element is expressed as
d^3 r=dl·ds (11.59)
wheredlis an increment of length along the axis anddsis an element of surface in the plane
perpendicular to the axis so thatBaxis·ds=dΦ.Because the line integral will involve a
complete circuit of theflux tube axis, in contrast to the earlier evaluation ofKtwist, we now
avoid using the gradient of a scalar to denote distance along the axis. Using Eq.(11.59) the
writhe helicity may therefore be expressed as
Kwrithe =
∫
Caxis
Aaxis·dlaxis
∫
dΦ
= Φ
∫
Caxis
Aaxis·dlaxis. (11.60)
This integral differs topologically from the integrals of the previous section, because here
the contour is acomplete circuit, i.e.,φvaries from 0 to 2 π,and not from 0 to 2 π−.
A contour pathCof an integral
∫
CA·dlmay be continuously deformed into a new
contour pathC′without changing the value of the integral provided no magneticflux is
linked by the surfaceSbounded byCandC′;this behavior is a three dimensional analog
to the concept of analyticity for a contour integral in the complex plane. The validity of
this assertion is established by the relation
0=
∫
S
B·ds=
∮
A·dl=
∫
C
A·dl−
∫
C′
A·dl. (11.61)