Environmental Engineering Reference
In-Depth Information
5.3 Ferrohydrodynamics and Heat Transfer
in Magnetic Fluids
Most of the work that concerns the motion of a magnetic
fl
uid under a static,
rotating or varying magnetic
of
ferrohydrodynamics. Today, a number of studies have been performed and we
address some of them in this subsection. We start this subsection by providing the
basic governing equations for the homogeneous
eld was performed by Rosensweig [ 7 ], the
father
fl
ow of Newtonian or non-New-
tonian magnetic
uids. These are based on the available literature (Bird et al. [ 91 ],
Neuringer and Rosensweig [ 92 ], Rosensweig [ 7 , 93
fl
95 ]). Furthermore, since we
deal in such equations with the homogeneous distribution of solid particles in the
base (nano
-
fl
uids) or the carrier
fl
uid (particle suspensions), we also present a few
models that relate to the de
nition of the effective thermal conductivity.
The equation of continuity can be written as
o q
o
t þrq~
ð
v
Þ ¼
0
ð 5 : 33 Þ
where v represents the velocity of the magnetic
fl
uid and
ˁ
represents the density of
the magnetic
uid, which may be calculated with help of the solids volume fraction
ϕ V or the solids mass fraction
fl
ϕ m as
1
q ¼ / V q solid þ
ð
1
/ V
Þ q liquid ¼
ð 5 : 34 Þ
/ m
ð
1
/ m
Þ
q solid þ
q liquid
The equation of motion for a (non)Newtonian magnetic fluid can be written
as [ 91 ]
h
i
D
v
Dt ¼ r
~
þr ¼
q
p
þ q~
g
ð 5 : 35 Þ
where ¼ represents the total stress tensor and may be divided into the viscous part
and the magnetic part:
¼
¼ ¼ viscous þ ¼ magnetic
ð 5 : 36 Þ
In order to include the non-Newtonian constitutive model, the viscous stress
tensor may be applied for an incompressible
fl
uid with the generalized Newtonian
model [ 91 ]:
¼
¼ viscous ¼ g r~
v T
v
þr~
¼ g
ð 5 : 37 Þ
o x i v j and
v T
where
r~
v is the velocity gradient tensor with components
o
r~
is the
o
o x j v i , and where the
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