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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