Environmental Engineering Reference
In-Depth Information
where T
R
denotes the temperature at which the refrigeration is performed. The work
performed during the cycle is equal to:
I
l
0
MdH
¼ l
0
Z
MdH
þ l
0
Z
b
d
w
¼
MdH
ð
1
:
42
Þ
a
c
The magnetic Ericsson cycle requires a regenerative process. Without
it,
Eq. (
1.42
) can also be written in other terms:
I
Z
Z
Z
Z
d
c
b
d
w
¼
dq
¼
T
R
ds
þ
T
H
ds
þ
T ds
þ
T ds
ð
1
:
43
Þ
a
a
c
b
¼
T
R
D
s
a
d
þ
T
H
D
s
c
b
þ
ð
h
d
h
c
Þþ
ð
h
b
h
a
Þ
Now the COP can be de
ned as:
q
R
w
T
R
D
s
a
d
COP
¼
jj
¼
ð
1
:
44
Þ
j
T
R
D
s
a
d
þ
T
H
D
s
c
b
þ
ð
h
d
h
c
Þþ
ð
h
b
h
a
Þ
j
If we assume that the regeneration is performed without irreversible heat transfer
losses,
then
the
two
enthalpy
differences would
have
to
be
equal
(h
d
−
h
a
). Furthermore, in the ideal Ericsson regenerative cycle, the
entropy difference during refrigeration and heat
h
c
) = (h
b
−
rejection would be equal
Δ
s
c
−
b.
Then the COP of the ideal regenerative Ericsson cycle has the
same value as that of the Carnot cycle:
s
a
−
d
=
−Δ
T
R
D
q
R
w
s
a
d
T
R
T
H
COP
¼
jj
¼
j
¼
ð
1
:
45
Þ
j
T
R
D
s
a
d
T
H
D
s
a
d
T
R
Magnetic Carnot Thermodynamic Cycle
The magnetic Carnot refrigeration cycle (Fig.
1.7
) is only useful for a comparison
with the other refrigeration cycles. In practice its low cooling capacity limits any
applicability in real devices. This well-known cycle operates between two isen-
tropic processes of magnetization and demagnetization and two isothermal pro-
cesses of magnetization and demagnetization. The last process is related to
refrigeration, where the cooling capacity is de
ned as:
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