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MHD

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Magneto-Hydrodynamics
(MHD)
Pouya Pourkarim
Niloofar Pourjafari
Outline
οƒ˜ MHD equations
οƒ˜ Behavior of a fluid in the presence of electromagnetic fields
οƒ˜ Flux freezing: An MHD case study
MHD equations
οƒ˜
πœ•πœŒ
+ 𝛻. πœŒπ‘£ = 0
πœ•π‘‘
(continuity equation)
οƒ˜
𝑑𝑣
1
𝜌
= −𝛻𝑝 +
𝐽 × π΅ + 𝐹𝑣 + πœŒπ‘”
𝑑𝑑
𝑐
(force equation)
οƒ˜
1 πœ•π΅
𝛻×𝐸 =−
𝑐 πœ•π‘‘
(Faraday’s law)
οƒ˜
4πœ‹
𝛻×𝐡 =
J
𝑐
(Ampere’s law (neglecting displacement current))
οƒ˜
1
𝐽 = 𝜎(𝐸 + 𝑣 × π΅)
𝑐
(Ohm’s law)
οƒ˜
𝑝=
πΎπœŒπ›Ύ
(equation of state)
Ideal Ohm’s law
𝐽 = 𝜎𝐸
E’ and J’ are measured in the rest frame of the medium
𝐽=𝐽
1
𝐸 = 𝐸 + (𝑣 × π΅)
𝑐
1
𝐽 = 𝜎(𝐸 + 𝑣 × π΅)
𝑐
1
𝐸+ 𝑣×𝐡 =0
𝑐
For a medium moving with velocity v relative to the laboratory
Behavior of a fluid in the presence of electromagnetic fields
οƒ˜ Electromagnetic effect
οƒ˜ Mechanical effect
Electromagnetic effect
Time dependence of a magnetic field:
πœ•π΅
πœ•π‘‘
=π›»× π‘£×𝐡 +
𝑐2
𝛻2𝐡
4πœ‹πœŽ
Derivation:
1
𝐽 1
𝐽 = 𝜎 𝐸+ 𝑣×𝐡 →𝐸 = − 𝑣×𝐡
𝑐
𝜎 𝑐
πœ•π΅
πœ•π‘‘
= −c𝛻 × πΈ = 𝛻 × π‘£ × π΅ −
𝛻×𝐡 =
4πœ‹
𝐽
𝐢
→𝛻×𝐽 =
𝑐
𝛻
4πœ‹
𝑐
𝜎
(𝛻 × π½)
× π›»×𝐡 =
𝑐
4πœ‹
𝛻 𝛻. 𝐡 − 𝐡(𝛻. 𝛻)
πœ•π΅
𝑐2 2
=π›»× π‘£×𝐡 +
𝛻 𝐡
πœ•π‘‘
4πœ‹πœŽ
πœ•π΅
𝑐2 2
=
𝛻 𝐡
πœ•π‘‘ 4πœ‹πœŽ
(Fluid at rest)
4πœ‹πœŽπΏ2
𝜏=
𝑐2
This means that an initial configuration of magnetic field will decay away in a diffusion time.
πœ•π΅
= 𝛻 × (𝑣 × π΅)
πœ•π‘‘
𝐸×𝐡
𝑀=𝑐
𝐡2
(Infinite conductivity)
Time dependence of a magnetic field: (Infinite conductivity)
πœ•π΅
=π›»× π‘£×𝐡
πœ•π‘‘
𝑑
πœ•
= + 𝑣. 𝛻
𝑑𝑑 πœ•π‘‘
convective derivative: total time rate of change of a quantity moving
instantaneously with the velocity v.
𝑑𝐡 πœ•π΅
=
+ 𝑣. 𝛻 . 𝐡
𝑑𝑑
πœ•π‘‘
𝛻 × π‘£ × π΅ = 𝑣 𝛻. 𝐡 − 𝐡 𝑣. 𝛻 → 𝑣. 𝛻 𝐡 = −𝛻 × (𝑣 × π΅)
→
𝑑𝐡 πœ•π΅
=
− 𝛻 × (𝑣 × π΅)
𝑑𝑑
πœ•π‘‘
𝑑∅𝐡
𝑑
=
𝑑𝑑
𝑑𝑑
𝐡. π‘›π‘‘π‘Ž =
𝑠
𝑠
𝛻 × π‘£ × π΅ . π‘›π‘‘π‘Ž =
𝑠
𝑠
πœ•π΅
. π‘›π‘‘π‘Ž −
πœ•π‘‘
𝑣 × π΅ . 𝑑𝑙
𝛻 × (𝑣 × π΅). π‘›π‘‘π‘Ž
𝑠
Stokes theorem
𝑐
πœ•π΅
. π‘›π‘‘π‘Ž =
πœ•π‘‘
𝛻 × π‘£ × π΅ . π‘›π‘‘π‘Ž =
𝑠
𝑑∅𝐡
=0
𝑑𝑑
𝑣 × π΅ . 𝑑𝑙
𝑐
Magnetic flux through any loop moving with the local fluid velocity is constant in time. In
other words, the lines of force are frozen into the fluid and are carried along with it.
The component of v perpendicular to B can be identified as the velocity w of the lines of
magnetic force.
1
𝐸 + (𝑣 × π΅) = 0
𝑐
(Ohm’s ideal law)
→ 𝑀 × π΅ = −𝑐𝐸
𝐸×𝐡
→𝑀=𝑐
𝐡2
𝐢 =𝐴×𝑋 →𝑋 =
𝐢×𝐴
𝐴. 𝐴
Magnetic Reynolds number:
A useful parameter to distinguish between situations in which diffusion of the field lines relative to the
fluid occurs and those in which the lines of force are frozen in is the magnetic Reynolds number.
π‘…π‘š =
𝛻 × (𝑣 × π΅)
𝑐2 2
𝛻 𝐡
4πœ‹πœŽ
π‘…π‘š ≫ 1
Transport of the lines of force with the fluid dominates over diffusion
π‘…π‘š β‰ͺ 1
Diffusion dominates over transport of the lines of force with the fluid
Mechanical effect
𝑑𝑣
1
𝜌
= −𝛻𝑝 + 𝐽 × π΅ + 𝐹𝑣 + πœŒπ‘”
𝑑𝑑
𝑐
(force equation)
𝑑𝑣
1
𝜌
= 𝐹+ 𝐽×𝐡
𝑑𝑑
𝑐
𝐽 = 𝜎(𝐸 +
1
𝑣
𝑐
× π΅)
𝜎𝐡2
𝐽 × π΅ = σ𝐸 × π΅ −
𝑣⊥
𝑐
𝑑𝑣
𝜎𝐡2
𝜌
= 𝐹 − 2 (𝑣⊥ − 𝑀)
𝑑𝑑
𝑐
The velocity of flow of the fluid perpendicular to B, decays from some initially arbitrary value in a time
of the order of:
πœŒπ‘ 2
𝜏=
𝜎𝐡2
to a value:
πœŒπ‘ 2
𝑣⊥ = 𝑀 +
𝐹
𝜎𝐡2 ⊥
4πœ‹
𝐽
𝑐
1
1
(𝐽 × π΅) =
𝛻×𝐡 ×𝐡
𝑐
4πœ‹
𝛻×𝐡 =
1
𝐡2
1
𝐽 × π΅ = −𝛻
+
𝐡. 𝛻 𝐡
𝑐
8πœ‹
4πœ‹
𝐡2
π‘π‘š =
8πœ‹
1
𝛻 𝐡2 = 𝐡. 𝛻 𝐡 + 𝐡 × π›» × π΅
2
𝑑𝑣
1
𝜌
= −𝛻𝑝 − π›»π‘π‘š + πœŒπ‘” +
𝐡. 𝛻 𝐡
𝑑𝑑
4πœ‹
𝜌
𝑑𝑣
𝑑𝑑
= −𝛻 𝑝 + π‘π‘š + πœŒπœ“ +
1
4πœ‹
𝐡. 𝛻 𝐡
𝑔 = −π›»πœ“
𝑝 + π‘π‘š + πœŒπœ“ = π‘π‘œπ‘›π‘ π‘‘π‘Žπ‘›π‘‘
Apart from gravitational effects, any change in mechanical pressure must be balanced by an opposite
change in magnetic pressure. If the fluid is to be confined within a certain region so that p falls rapidly to
zero outside that region, the magnetic pressure must rise equally rapidly in order to confine the fluid.
MHD Flow between Boundaries with Crossed Electric and Magnetic Fields
Illustrating the behavioral differences between freezing force
lines and diffusion through them, and the E × B drift.
οƒΌ Ignore gravity
οƒΌ No pressure gradient in x direction
οƒΌ Incompressible fluid
οƒΌ Viscous fluid
οƒΌ Conducting fluid
οƒΌ Nonconducting boundary surfaces at z = 0 and z = a
οƒΌ Planes moving with different speeds 𝑉1 and 𝑉2 in x direction
οƒΌ Uniform magnetic field 𝐡0 in z direction
οƒΌ System is infinite in x – y plane
Figure 1. Flow of viscous conducting fluid
in a magnetic field between two plane
surfaces moving with different velocities.
Any electric fields?
Faraday′s Law
πœ•π΅
=0
𝛻 × πΈ = 0 → 𝐸 = −π›»πœ™
πœ•π‘‘
(𝐡 × π‘£) × π΅
𝐸×𝐡
𝑀=
=𝑐
𝐡2
𝐡2
→ A constant electric field is present
→ Electric field is in the y direction
Any other magnetic fields?
Moving fluid tend to carry field lines
→ An x component 𝐡π‘₯ (𝑧) of magnetic induction in addition to the z component 𝐡0
οƒΌ Incompressible fluid → Continuity equation becomes 𝛻 ⋅ v = 0
The steady state form of force equation becomes:
𝛻𝑝 =
1
𝐽 × π΅ + πœ‚π›» 2 𝑣
𝑐
The only non vanishing component of J is 𝐽𝑦 (𝑧):
1
𝐽𝑦 (𝑧) = 𝜎 𝐸0 − 𝐡0 𝑣(𝑧)
𝑐
(v(z) is the x component of velocity)
2
The force equation separate in 3 dimensions: πœ•π‘ = 𝜎𝐡0 𝐸 − 𝐡0 𝑣 + πœ‚ πœ• 𝑣
0
2
πœ•π‘₯
𝑐
𝑐
πœ•π‘
=0
πœ•π‘¦
πœ•π‘
𝜎𝐡π‘₯
𝐡0
=−
𝐸0 − 𝑣
πœ•π‘§
𝑐
𝑐
πœ•π‘§
οƒΌ No pressure gradient in x direction:
The first equation can be written as
πœ•2𝑣
𝑀
−
πœ•π‘§ 2
π‘Ž
2
𝑀
𝑣=−
π‘Ž
2
𝑐𝐸0
𝐡0
𝜎𝐡02 π‘Ž2
Where M is the Hartmann number and is defined as: 𝑀 =
πœ‚π‘ 2
1 2
Hartmann number can be thought as the ratio of magnetic viscosity to normal viscosity.
The solution to the equation using the boundary conditions
𝑣 0 = 𝑉1 and 𝑣 π‘Ž = 𝑉2 is:
𝑣 𝑧 =
𝑉1
π‘ π‘–π‘›β„Ž
sinh 𝑀
𝑀
π‘Ž−𝑧
π‘Ž
+
𝑉2
𝑀𝑧
π‘ π‘–π‘›β„Ž
sinh 𝑀
π‘Ž
+
𝑐𝐸0
𝐡0
1−
π‘ π‘–π‘›β„Ž 𝑀
π‘Ž−𝑧
π‘Ž
𝑀𝑧
+π‘ π‘–π‘›β„Ž π‘Ž
sinh 𝑀
οƒ˜ First limiting case: 𝐡0 → 0 (𝑀 → 0)
𝑧
𝑣 𝑧 = 𝑉1 + (𝑉2 − 𝑉1 ) (Laminar Flow)
π‘Ž
οƒ˜ Second limiting case: 𝑀 ≫ 1: (Magnetic viscosity
dominates and flow mostly follows E × B drift)
For π‘Ž ≫ 𝑧 we obtain
𝑐𝐸0
𝑐𝐸0 −𝑀𝑧
𝑣 𝑧 ≃
+ (𝑉1 −
)𝑒
𝐡0
𝐡0
Figure 2. Velocity profile of the two limits
π‘Ž
While 𝜈 𝑧 = 𝑉1 exactly at the surface, there is a rapid
transition in a distance of order (a/M) to the E × B drift
value.
Near z = a, we simply switch 𝑉1 with 𝑉2 and z with a-z
Figure 3. Transport of lines of magnetic induction
The magnetic field 𝐡π‘₯ (𝑧) can be determined by the equation
πœ•π΅π‘₯ 4πœ‹
4πœ‹πœŽ
1
=
𝐽 =
(𝐸0 − 𝐡0 𝑣)
πœ•π‘§
𝑐 𝑦
𝑐
𝑐
Assuming that 𝐡π‘₯ vanishes at z = a and z = 0 and substituting
𝜈 with its calculated formula we have
𝐡π‘₯ z = 𝐡0
4πœ‹πœŽπ‘Ž2
𝑐2
𝑉2 −𝑉1
2π‘Ž
𝑀
𝑀 𝑀𝑧
π‘π‘œπ‘ β„Ž 2 −π‘π‘œπ‘ β„Ž 2 − π‘Ž
𝑀
𝑀 π‘ π‘–π‘›β„Ž 2
π‘…π‘š
Figure 4. Axial component of magnetic induction
Which in the two limiting cases of 𝑀 ≫ 1 and 𝑀 β‰ͺ 1 reduces to
𝐡π‘₯ z ≃ 𝑅𝑀 𝐡0
𝑧
𝑧
1− ,
π‘Ž
π‘Ž
1
1 − (𝑒 −𝑀𝑧
𝑀
π‘“π‘œπ‘Ÿ 𝑀 β‰ͺ 1
π‘Ž
+ 𝑒 −𝑀
π‘Ž−𝑧 π‘Ž
),
π‘“π‘œπ‘Ÿ 𝑀 ≫ 1
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