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and correspond to the fast relaxation within the wells. These fast processes are, of
course, not captured by Eq. (237).
Note that the ground-state tunnel splitting is typically very small, so that
it is very difficult to experimentally realize
to see coherent oscillations
of the spin between the two states. To increase , one has to apply a strong
transverse field. In the case W
|
W
|
( W> 0), the levels becomes dehybridized,
ρ eq
ρ eq
++ =
S , and one obtains
S,
S 1
e t
ρ eq
e t
ρ
S ( t )
=
+
(238)
S,
S,
5. Relaxation Rate Between two Tunnel-Split States
The relaxation rate
for the ground-state doublet can be found analytically
[13]. In particular, for the uniaxial model in the presence of a transverse field
along the x axis, with the help of the high-order perturbation theory in H x , one
obtains
−+
m
W 2
m
ψ
|
S z |
ψ
+ =−
2
+
2
m
B H x
W
W 2
m
ψ
|
S x |
ψ
+ =
2
+
2
S y ψ
m
ψ
=−
B H x
m
i
(239)
+
2
Then, from Eq. (155) in components,
ω 0
|
S x |
+
=−
i
ψ
ψ
−+
,x
ψ
S y ψ
B H z +
ψ
|
S z |
ψ
+
B H y
+
ω 0 ψ
S y ψ
=−
i
−+
,y
+
ψ
|
S z |
ψ
+
B H x +
ψ
|
S x |
ψ
+
B H z
=−
i
ω 0
ψ
|
S z |
ψ
+
−+
,z
B H y + ψ
S y ψ
B H x
ψ
|
S x |
ψ
+
(240)
+
with H y =
0 one obtains
=
0
−+
,z
m
B H x
m
=−
i
( W
B H z )
−+
,x
2
m
W 2
m
=
B H x
−+
,y
2
+
2
1
2
( B H x ) 2
W ( W
B H z )
( B H x ) 2
×
(241)
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