425
e rfc (x) are the bi-logarithmic and additional variable functions. Consequently, the
DOS of various earth surface planes, here named as ϱ PC (ω), is confirmed by estimating the photonic energy frequencies and energy functions of Maxwell’s theory
in the nanostructure [25, 43, 44]. In a 1D earth surface plane, the DOS is thus provided by  PC
e
e
ω
ω ω
ω ω
( )∝ −
−
(
)
1
Θ
, where Θ(ω − ω e ) where ω e denotes the
frequency of PBE at the used DOS.
Then the bandgap has been used to precisely determine the qualitative states of the
non-Weisskopf-Wigner modes and the cool-state photons calculated by the isotropic
classification of the earth surface plane (Fig.  21.5). In the earth surface plane, the
bandgap is closer to the DOS and it is determined by  PC
e
e
ω
ω ω
ω ω
( )∝ −
−
(
)
1
Θ
.
This DOS is thereafter determined considering the electromagnetic field vectors on the
earth surface [45–47]. In 2D and 1D earth surface plane, the cool-state photons’
DOS shows a real logarithmic divergence close to the PBE, which is ϱ PC (ω) ∝  − [l
n|(ω − ω 0 )/ω 0 | − 1]Θ(ω − ω e ), where ω e defines the primary point of the peak of
DOS distribution of ground-state photon emissions [24, 30].
Fig. 21.4 Illustration of heating energy-level photon activation; (a) total energy intensity of the
a.u. as a function of photon absorbance with respect to wavelengths of 287 nm, (b) 535 nm, and
(c) 880 nm
Results and Discussion