23
V
v
I
O I
8
2
2
2
r
const,
(2.20)
or the resultant electricity energy generation is shifted by its VEV, Φ r (x) = v + σ(x),
I
V
V V
r
2
2
2
2
2
2
v
v
v
v
(2.21)
V
v
v
v
O
V V
O
V
O V
O V
8
2
2
2
8
2
2
2
2
3
4
(2.22)
Simultaneously, the functional derivative D μ ϕ will become
D
i qA
i
i qA
i
i
i
P
P
P
P
P
P
I
I
I
I I
I
w
w w
1
2
2
r
r
r
r
r
e
e
e
4
4
4
4
(2.23)
D
i
iqA
qA
P
P
P
P
P
P
P
P
I
I I
I
I
I
V
2
2
2
2
1
2
1
2
2
1
2
w w
w
w
w
r
r
r
r
r
4
4
w
2
2
2
2
v
qA
V
P
P
4
(2.24)
Altogether,
(2.25)
To determine the formation of this net electricity generation referred to as (ɧ sef )
on the earth surface, the function of the electrostatic fields has been quantified by
conducting the quadratic calculation and described by the following equation:
(2.26)
Here this net electricity generation (ɧ free ) function certainly will admit a realistic
vector particle of positive mass
2
 = λv
2
integrating the areal A μ (x) function and the
electricity energy generation fields Θ(x) to determine the net electricity energy from
the global solar energy calculation on the earth surface [2, 48].
Material, Methods, and Simulation