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Journal ArticleDOI

Parker problem in Hall magnetohydrodynamics

28 May 2009-Physics of Plasmas (American Institute of Physics)-Vol. 16, Iss: 5, pp 052111
TL;DR: In this article, a triple deck structure for the Parker problem in Hall magnetohydrodynamics (MHD) is considered, with the magnetic field falling off in the intermediate Hall-resistive region more steeply than that (like 1/x) in the outer ideal MHD region.
Abstract: The Parker problem in Hall magnetohydrodynamics (MHD) is considered. Poloidal shear superposed on the toroidal ion flow associated with the Hall effect is incorporated. This is found to lead to a triple deck structure for the Parker problem in Hall MHD, with the magnetic field falling off in the intermediate Hall-resistive region more steeply (like 1/x3) than that (like 1/x) in the outer ideal MHD region.

Summary (1 min read)

II. GOVERNING EQUATION FOR HALL MHD

  • 10 Nondimensionalize distance with respect to a typical length scale a, magnetic field with respect to a typical magnetic field strength B0, time with respect to the reference Alfvén time A a /VA0, where VA0 B0 / and min, and introduce the magnetic and velocity stream functions according to a Permanent address: University of Central Florida, Orlando, FL 32816- 1364.
  • The Hall magnetic field b is believed to be produced by the dragging of the in-plane magnetic field in the out-of-plane direction by the magnetized electrons near the magnetic neutral surface.

III. PARKER PROBLEM IN HALL MHD

  • Let us assume that the magnetic field lines are straight and parallel to the current sheet.
  • Here, pure resistive annihilation without reconnection of antiparallel magnetic fields in the x ,y-plane occurs.
  • One way to remedy this situation is to recognize the presence of the poloidal shear in the toroidal ion flow, which is intrinsic to the Hall effect.
  • The presence of poloidal shear in the toroidal ion flow basically signifies the generic variation in the out-of-plane ion flow velocity along the outflow direction.

IV. DISCUSSION

  • In recognition of the fact that a signature of the Hall effect is the generation of out-of-plane “separator” components of the magnetic and ion-flow velocity fields, a more accurate representation of the latter appears to be in order for a more complete formulation of the Parker problem.
  • This is accomplished by incorporating poloidal shear into the toroidal ion flow associated with the Hall effect.
  • This is found to lead to a triple-deck structure for the Parker problem in Hall MHD, in accordance with the idea originally put forward by Terasawa.
  • The magnetic field is found to fall off in the intermediate Hall-resistive region more steeply like 1 /x3 than that like 1 /x in the outer ideal MHD region.

ACKNOWLEDGMENTS

  • I acknowledge with gratitude the stimulating interactions with Dr. Luis Chacon that led to this work.
  • My thanks are also due to Dr. Michael Shay and Dr. Michael Johnson for helpful communications and discussions.

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Faculty Bibliography 2000s Faculty Bibliography
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Parker problem in Hall magnetohydrodynamics Parker problem in Hall magnetohydrodynamics
Bhimsen K. Shivamoggi
University of Central Florida
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Phys. Plasmas 16, 052111 (2009); https://doi.org/10.1063/1.3140055 16, 052111
© 2009 American Institute of Physics.
Parker problem in Hall
magnetohydrodynamics
Cite as: Phys. Plasmas 16, 052111 (2009); https://doi.org/10.1063/1.3140055
Submitted: 02 September 2008 . Accepted: 28 April 2009 . Published Online: 28 May 2009
Bhimsen K. Shivamoggi
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Physics of Plasmas 18, 052304 (2011); https://doi.org/10.1063/1.3581092

Parker problem in Hall magnetohydrodynamics
Bhimsen K. Shivamoggi
a
Los Alamos National Laboratory, Los Alamos, New Mexico 87545, USA
Received 2 September 2008; accepted 28 April 2009; published online 28 May 2009
The Parker problem in Hall magnetohydrodynamics MHD is considered. Poloidal shear
superposed on the toroidal ion flow associated with the Hall effect is incorporated. This is found to
lead to a triple deck structure for the Parker problem in Hall MHD, with the magnetic field falling
off in the intermediate Hall-resistive region more steeply like 1/ x
3
than that like 1/ x in the outer
ideal MHD region. © 2009 American Institute of Physics. DOI: 10.1063/1.3140055
I. INTRODUCTION
Numerical simulations
1
suggested that magnetic recon-
nection in resistive magnetohydrodynamics MHD can be
driven by a magnetic flux pile-up. In this process, magnetic
field builds up upstream of a Sweet
2
–Parker
3
current sheet
this field buildup strengthens as the resistivity is decreased,
which leads to an increase in the outflow downstream of the
current sheet. This provides for a remedy for the Sweet–
Parker “bottleneck”
4
limiting the outflow and enabling re-
connection to proceed at the externally imposed rate. How-
ever, as the resistivity is decreased further, the development
of large magnetic pressure gradients upstream of the current
sheet opposes the ion inflow,
5
which is the only means in
resistive MHD to transport magnetic flux into the reconnec-
tion layer. The magnetic flux transport into the reconnection
layer and hence the reconnection rate is reduced—the so-
called pressure problem.
6
The Hall effect
7
can overcome the
pressure problem
8,9
thanks to the decoupling of electrons
from ions on length scales below the ion skin depth d
i
. So, if
the reconnection-layer width is less than d
i
, the electron in-
flow can keep on going, which transports the magnetic flux
into the reconnection layer and hence reduces the flux pile-
up. Dorelli
10
considered the role of Hall effect in magnetic
flux pile-up driven antiparallel magnetic field merging and
gave analytical solutions of the resistive Hall MHD equa-
tions describing stagnation-point ion flows in a thin current
sheet—Parker problem.
11
However, Dorelli’s solution for the
Hall regime turned out to be basically Parkers solution for
the ideal MHD regime. Indeed, the Hall contribution can be
transformed away from Dorelli’s solution by suitably rede-
fining the velocity gradient associated with the stagnation-
point ion flow. A more complete formulation of the Parker
problem in Hall MHD is therefore in order—this is the ob-
jective of this paper.
II. GOVERNING EQUATION FOR HALL MHD
Consider an incompressible, two-fluid, quasineutral
plasma. The governing equations for this plasma dynamics
are in usual notation
nm
e
v
e
t
+ v
e
· v
e
=−p
e
ne
E +
1
c
v
e
B
+ ne
J, 1
nm
i
v
i
t
+ v
i
· v
i
=−p
i
+ ne
E +
1
c
v
i
B
ne
J, 2
· v
e
=0, 3
· v
i
=0, 4
· B =0, 5
B =
1
c
J, 6
E =−
1
c
B
t
, 7
where
J nev
i
v
e
. 8
Neglecting electron inertia m
e
0, Eqs. 1 and 2 can
be combined to give a modified ion equation of motion,
nm
i
v
i
t
+ v
i
· v
i
=−p
i
+ p
e
+
1
c
J B, 9
and a generalized Ohm’s law,
E +
1
c
v
i
B =
J +
1
nec
J B. 10
Nondimensionalize distance with respect to a typical
length scale a, magnetic field with respect to a typical mag-
netic field strength B
0
, time with respect to the reference
Alfvén time
A
a / V
A
0
, where V
A
0
B
0
/
and
m
i
n, and
introduce the magnetic and velocity stream functions accord-
ing to
a
Permanent address: University of Central Florida, Orlando, FL 32816-
1364.
PHYSICS OF PLASMAS 16, 052111 2009
1070-664X/2009/165/052111/4/$25.00 © 2009 American Institute of Physics16, 052111-1

B =
i
ˆ
z
+ bi
ˆ
z
11
v
i
=
i
ˆ
z
+ wi
ˆ
z
and assume that the physical quantities of interest have no
variation along the z-direction. The Hall magnetic field b is
believed to be produced by the dragging of the in-plane mag-
netic field in the out-of-plane direction by the magnetized
electrons near the magnetic neutral surface.
12,13
Equations
9 and 10 then yield
t
+
,
+
b,
=
ˆ
2
, 12
b
t
+ b,
+
,
2
+
,w =
ˆ
2
b, 13
w
t
+ w,
= b,
, 14
where
A,B兴⬅A B · i
ˆ
z
,
d
i
/a,
ˆ
c
2
A
/a
2
.
III. PARKER PROBLEM IN HALL MHD
Consider a stagnation-point ion flow at a current sheet
separating plasmas of opposite magnetizations
11
in Hall
MHD, governed by Eqs. 1214. Let us assume that the
magnetic field lines are straight and parallel to the current
sheet. Here, pure resistive annihilation without reconnection
of antiparallel magnetic fields in the x , y-plane occurs. Spe-
cifically, consider a unidirectional magnetic field
B = B
y
xi
ˆ
y
, 15
with the boundary condition
B
y
0 =0, 16
which is carried toward a neutral sheet at x=0 by a
stagnation-point ion flow,
v
i
=−axi
ˆ
x
+ ayi
ˆ
y
+ wi
ˆ
z
. 17
Noting that the process in question is steady and that the
magnetic field is prescribed as in Eq. 15, Eqs. 1214
become
E +
x
y
b
y
x
=
ˆ
2
x
2
, 18
b
x
y
b
y
x
+
x
w
y
=
ˆ
2
b, 19
w
x
y
w
y
x
+
x
b
y
=0, 20
where
E
t
.
Dorelli
10
looked for a solution of Eqs. 1820 of the
form
b = yfx, 21a
w =
g
1
x, 21b
where
is a constant. However, this solution restricts the
role played by the Hall effect in the process in question.
Indeed, the Hall contribution can be transformed away from
Dorelli’s solution by suitably redefining the velocity gradient
a associated with the stagnation-point ion flow see below.
One way to remedy this situation is to recognize the presence
of the poloidal shear in the toroidal ion flow, which is intrin-
sic to the Hall effect. This aspect is also recognized in the
Hall resistive tearing mode formulation.
14
The presence of
poloidal shear in the toroidal ion flow basically signifies the
generic variation in the out-of-plane ion flow velocity along
the outflow direction. On the other hand, the physical mecha-
nism proposed for the generation of the Hall magnetic field b
Refs. 12 and 13 involves a poloidal shear in the toroidal
electron flow, some of which appears to be coupled also to
the toroidal ion flow. Therefore, we incorporate a poloidal
shear into the toroidal ion flow according to
w =
g
1
x +
2
y
2
g
2
x, 22
where
is a constant characterizing this poloidal shear. The
particular form of poloidal shear superposed on the toroidal
ion flow used in Eq. 22 is motivated by the symmetry prop-
erties of Eqs. 1214 in the ideal limit, which indicate
and w to be even functions of both x and y, and
and b to be
odd function of both x and y;
15
these properties are sustained
by the solutions in the following. Using Eqs. 21a and 22,
Eq. 20 gives
g
1
+
2
y
2
g
2
ax
yg
2
兲共 ay +
x
f
=0, 23
where primes denote differentiation with respect to x.We
obtain from Eq. 23
ax兲共
g
1
=−
x
f
, 24
g
2
x = x
2
. 25
Using Eqs. 21a, 22, 24, and 25, Eq. 19 then
gives
yf
ax f ay +
x
yx
2
=
ˆ
yf
, 26
or
f
+
a
ˆ
xf
f =
ˆ
x
2
x
. 27
Recognizing that the Hall effect becomes important
away from the current sheet at x =0 in what was called the
“intermediate” layer by Terasawa
16
in his investigation of the
Hall resistive tearing mode, a reasonable approximate solu-
tion of Eq. 27 is
052111-2 Bhimsen K. Shivamoggi Phys. Plasmas 16, 052111 2009

fx兲⬇Ax
a
x
2
x
, 28
where A is a constant.
Using Eqs. 21a and 28, Eq. 18 gives
E +
x
ax
Ax
a
x
2
x
x
=
ˆ
2
x
2
,
or
E =
ˆ
B
y
+ a +
AxB
y
+
a
x
2
B
y
2
, 29
which is a generalization of Parker s equation to Hall MHD.
Observe that, for Dorelli’s solution which corresponds to
=0, the Hall contribution represented by the term corre-
sponding to
can be simply transformed away by redefin-
ing the velocity gradient a associated with the stagnation-
point ion flow.
It is important to note that Eq. 29 shows that the triple-
deck structure borrowing the terminology from boundary
layer theory in fluid dynamics
17
in Hall resistive MHD
originally pointed out by Terasawa
16
is operational for the
Parker problem in Hall MHD, as to be expected. Thus, we
have
i a resistive region near the current sheet at x =0,
ii an ideal MHD region away from the current sheet at
x= 0, and
iii a Hall resistive region in between i and ii—called
the intermediate region by Terasawa.
16
In the resistive region, Eq. 29 may be approximated by
E
ˆ
B
y
, 30
which gives Parkers solution,
B
y
E
ˆ
x. 31
In the ideal MHD region, Eq. 29 may be approximated
by
E ⬇共a +
AxB
y
+
a
x
2
B
y
2
, 32
which gives modified Dorelli’s solution,
B
y
2aa +
A
−1+
1+
4Ea +
Aa
2
2
2
1
x
.
33
In the Hall resistive region, Eq. 29 may be approximated
by
E
ˆ
B
y
+
a
x
2
B
y
2
, 34
which gives
B
y
3
ˆ
a
1
x
3
. 35
The triple-deck structure given by Eqs. 31, 33, and
35 is shown in Fig. 1. Noting from Eqs. 21a and 28 that
b = y
Ax +
a
x
2
B
y
, 36
one observes that both in the
Hall resistive region, B
y
1 / x
3
, and
ideal MHD region, B
y
1 / x,
b has a quadrupolar structure. So, Hall effects materialize
only via their signature—the quadrupolar out-of-plane mag-
netic field pattern.
18
IV. DISCUSSION
In recognition of the fact that a signature of the Hall
effect is the generation of out-of-plane “separator” compo-
nents of the magnetic and ion-flow velocity fields, a more
accurate representation of the latter appears to be in order for
a more complete formulation of the Parker problem. In this
paper, this is accomplished by incorporating poloidal shear
into the toroidal ion flow associated with the Hall effect. This
is found to lead to a triple-deck structure for the Parker prob-
lem in Hall MHD, in accordance with the idea originally put
forward by Terasawa.
16
The magnetic field is found to fall off
in the intermediate Hall-resistive region more steeply like
1/ x
3
than that like 1/ x in the outer ideal MHD region.
ACKNOWLEDGMENTS
I acknowledge with gratitude the stimulating interactions
with Dr. Luis Chacon that led to this work. I am thankful to
the referee for his helpful remarks. My thanks are also due to
Dr. Michael Shay and Dr. Michael Johnson for helpful com-
munications and discussions.
1
2
3
0
x
B
y
FIG. 1. Magnetic field profile for the Parker problem in Hall MHD. 1
B
y
x, 2 B
y
1 / x
3
, and 3 B
y
1 / x
052111-3 Parker problem in Hall magnetohydrodynamics Phys. Plasmas 16, 052111 2009

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Abstract: [1] We compute numerical solutions of the resistive Hall MHD equations corresponding to pairwise magnetic island coalescence. The simulation results can be organized according to the relative sizes of three length scales: the electron dissipation length, le; the ion inertial length, di; and the island wavelength, λ. We identify three qualitatively distinct regimes of magnetic island coalescence: (1) the resistive MHD limit, di ≲ le ≪ λ; (2) the “whistler-mediated” limit, le ≪ di ≪ λ; and (3) the “whistler-driven” limit, le ≪ λ ≲ di. In the resistive MHD limit, magnetic flux piles up outside thin current sheets between the islands. The upstream Alfven speed increases with increasing Lundquist number, and the reconnection rate is insensitive to the Lundquist number. In the whistler-driven limit, the electron and ion bulk flows decouple on the island wavelength scale. Magnetic flux pileup does not occur, and the coalescence proceeds on a whistler timescale that is much shorter than the Alfven time. In the whistler-mediated limit, electron and ion bulk flows decouple in spatially localized “ion inertial sheets” around the island separatrices. Flux pileup is reduced, and the upstream Alfven speed approaches a nearly constant value as the Lundquist number is increased. The maximum reconnection rate in the whistler-mediated limit is comparable to that observed in the resitive MHD limit over the Lundquist number range 500 < Sλ < 10000.

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References
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Journal ArticleDOI
TL;DR: In this paper, it was shown that two oppositely directed sunspot fields with scales of 104 km could be merged by Sweet's mechanism, if shoved firmly together, in about two weeks; their normal interdiffusion time would be of the order of 600 years.
Abstract: Sweet's mechanism for the merging of two oppositely directed magnetic fields in a highly conducting fluid is investigated in a semi-quantitative manner. It is shown that two oppositely directed sunspot fields with scales of 104 km could be merged by Sweet's mechanism, if shoved firmly together, in about two weeks; their normal interdiffusion time would be of the order of 600 years. It is suggested that Sweet's mechanism may be of considerable astrophysical importance: It gives a means of altering quickly the configuration of magnetic fields in ionized gases, allowing a stable field to go over into an unstable configuration, subsequently converting much of the magnetic energy into kinetic energy of the fluid.

1,562 citations

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TL;DR: In this paper, a general picture of magnetic reconnection in the framework of 2D incompressible resistive magnetohydrodynamic theory is presented, and a theory of the solution in the external and in the diffusion region is developed and analytical expressions in agreement with the simulation results are obtained by means of a variational principle.
Abstract: A general picture of magnetic reconnection in the framework of 2‐D incompressible resistive magnetohydrodynamic theory is presented. Numerical studies of (quasi‐) steady‐state driven reconnection reveal current sheet formation for Mach numbers M=u/vA exceeding the Sweet–Parker reconnection rate MSP=(η/LvA)1/2. Since the thickness δ of the current sheet is found to be invariant to a change of the resistivity η, its length Δ increases rapidly with decreasing η or increasing M, which can be written in the form Δ∼(M/MSP)4, so that Δ reaches the global system size L within a short range of the parameter M/MSP. The results are rather insensitive to the particular choice of boundary conditions. Because of the presence of a current sheet, the overall reconnection process is quite slow. This picture essentially agrees with Syrovatsky’s [Sov. Phys. JETP 33, 933 (1971)] theory and disproves Petschek’s [AAS/NASA Symposium on the Physics of Solar Flares, (NASA, Washington, DC, 1964) p. 425] mechanism of fast magnetic reconnection. A theory of the solution in the external and in the diffusion region is developed and analytical expressions in agreement with the simulation results are obtained by means of a variational principle. For sufficiently long current sheets the tearing mode becomes unstable in spite of the stabilizing effect of the inhomogeneous flow. The tearing mode contributes to the overall reconnection process, but a general assessment of this effect in the asymptotic regime of almost vanishing η is difficult.

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Book
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TL;DR: In this article, a linear 2-D eigenmode analysis was performed to study the Hall current effect on collisional tearing mode instability and the appearance of the dawn-dusk component of the magnetic field in the magnetotail reconnection region.
Abstract: From a linear 2-D eigenmode analysis, it is found that the Hall current effect on collisional tearing mode instability becomes important for the thin magnetic reversal layer whose width is comparable to the ion inertia length; Hall currents produce a three-dimensional field structure and increase the reconnection (growth) rate. Since the magnetaic reversal layer widths both in the magnetopause and in the magnetotail are reported to become as thin as the ion inertial length (several hundred km) when the reconnection process is supposed to occur, the Hall current effect may explain the appearance of the dawn-dusk component of the magnetic field in the magnetotail reconnection region.

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