1. Introduction
In modern studies, the propagation of SLG in FSO is the understanding of the nature of ray propagation such as intensity, scintillation index, source size, and many factors that can be calculated and analyzed, the sharp dispersion of a Lorentz-Gaussian delivery is a higher order than that of a Gaussian ray propagation. As a result, Lorentz-Gaussian beams have been used as long as with more appropriate reproductions G(Gaussian) and to explain the propagation of SLG in (FSO) free-space optics [
1], also to illustrate the digital phase shifter and its application in communication circuits for design and comparison with Gaussian propagation in FSO [
2]. In addition, the oblique propagation of the Gaussian laser in a turbulent atmosphere was investigated and the Huygens-Fresnel integration process was studied [
3]. In other words, the static model of ITU-R turbulence construction was applied and the mean SLVGB intensity was calculated in the oblique beam propagation at different perpendicular distances [
4], which corresponds to the mean aperture receiver. We once checked the parameters such as the source size factor that affect the energy propagation profile. In addition, the analysis showed that the mean aperture is inflated with increasing distance of the scattering length [
5]. In addition, the study of paraxial propagation in the tropospheric layer according to the width of the beam and the size of the source of the initial profile spread over space, also the structure of constant parameters that explain the wave prefiltration by using SLG beam Kolmogorov [
6,
7,
8] free space, the paraxial propagation of Lorentz was studied such as Lorentz Gauss beams [
9]. The factorial formulations of the Lorentz function and the long-range Lorentz beam were unanimously confirmed [
10,
11]. Moreover, the long-range propagation of the Gaussian beam, although the fractional Fourier transform was trained to the accuracy of Lorentz [
12]. To numerically explore the focal oscillation, the Lorentz-Gaussian beam occupied by the pinhole lens structure was derived [
13]. In addition, the second-order beam propagation for Lorentz or Lorentz-Gauss beam effects was investigated as described in [
14,
15]. the SLG beam was invented by using Lorentz beams as a basis in reference [
16]. Due to these requirements in the area of remote detection and optical transport in free space, extensive studies on the propagation of different laser types in a turbulent atmosphere were also modified. [
17,
18,
19,
20,
21,
22,
23]. Finally, in this paper, we use new modelling and apply the mathematical technique to improve the non-turbulent SLG on beam propagation and its application in optical communication systems.
2. Propagation of an SLG Jet in a Non-Turbulent Troposphere
The super-Lorentz G-beam in the transmitter plane at L = 0 revenue for the formulation, transmitter field of SLG illustrated in the Cartesian coordinate system, the L-axis is latched and the axis propagates as follows:
denotes the transmission field of the SLG beam
,
is the oblique synchronised structure position on the source side, and, beam widths (
) that correspond to the parameters of SLG and
are the wavelength of the SLG beam in the following, let us understand what we have understood by the beam according to Equation (2). If you set the beam order
a, and
b to 1, and 0, is likely that you will hit the vital beam and the original order of Supper LG beams. This has already been explained in this reference [
3,
6,
24].
Wherever the beam widths of the Gaussian part
are denoted by their position and the focal length constant parameter
over the x and y directions [
6,
25], the next point in Equation (3) can be found. The limits of the
constants with the quantity of α=1, are posted in a straight line from the organised standards in ref [
26] and are Hermite polynomial
. Notwithstanding the first impression that the overhead process might cause a theatrical increase in the sum of calculations as
Where Hermite polynomial
, the field basis in equation (1) acts and presents the Huygens-Fresnel integral method in a nonturbulent atmosphere, moreover,
L means the propagation distance between the transducer plane, the receiver field
) evolves in a cartesian coordinate system which is studied in equation (4), [
27]
For the update of the SLG beam via the formula of the extended Huygens-Fresnel integral for the start of the synchronization observed in Eq. (5). Our information is a little from Eq. (1) and Eq. (3, 4) given the new expression to follow in Eq. (5) follow and
.
To evaluate the expansion as shown in the equation (6) as shown
The lower solution of this extension can be seen in equation (7)
By substitution, the above equations containing a number (3, 6, 7) are replaced in equation (8), resulting in a new equation that reads as follows
Eq. (8) describes the receiver field and the determination of the subexpression by substituting Eq. (9) into Eq. (8). It has been observed that it can then be simplified into Eq. (8) as below
We have used approximate statements that solve equation (9a) as shown, but the Γ(.)refers to a gamma function, p is the ray order of the SLG ray, and now is the solution of equation (9) that appears in ref [
24], first equation (9a), and erroneously the imitation exclusively of the synopsis, thus in refs [
24,
26] as obtained equations (9b, 9c, 9d) as below
We use equation (9c) and place the formulation (22.1.1) above it for the same thing to which it refers.
We are about to engrave the equations via Eq.(9a,9b,9c). Moreover, the order of the original life is connected to the order of the equations, as you can see
To illustrate and replace equation (9f) with equation (9g), the results of these equations are then flattering, as shown below and converted as
We obtain equation (9h) by subtracting the variable constant from equation (9g) as traces
We set p = 1, 2, as shown in Eq.(9i), and in what way we evaluate the derivative of Eq.(9i) to originally use an undeveloped Eq.(9h), as scream
By setting a ray order n = 1 and calculating a subsequent copy of Eq.(9i), which first gives the result for calculating the first derivative of Eq.(9j) and becomes the result for recalculating the next derivative of Eq.(9k), as shown below
You can get the result in equation(9m) and then develop equation(9k) through the influence and as follows
In addition, the result of innovative production is clarified in equation(9n) and then equation(9m) is substituted into equation(9i) so that equation(9i) reads as follows
The expression of Eq.(9n) was improved holistically and from the basic Eq.(9n) later Eq.(9p) results as follows
Solve the integral of equation (9q) and the integral of equation (9p) using the formula (3.381.11) of this reference [
24] and substitute equation (9q) as follows
Equation (9p) is the solution key of the integral associated with equation (9i) and can be obtained in equation (10) as follows
To obtain the new equation (11), you must change equation (8) in [
27] as follows.
To be back sequences of Eq. (11), we are applying the factor fixed is an out of the integral and then gets extra Eq. (12) as below
By using the formulation (3.462.2.8) to resolve Eq. (12) we effort to put Eq. (13) into Equation (12) of ref [
24] as verified in Eq. (14) as beneath
If you use equation (14) and equation (14) to solve equation (12), you get the new equation (15), which you can see below
To obtain the solution of the second integral of Eq. (15), which was previously solved in the same way, obtain Eq. (16) as follows
On the other hand, replace equation(16) with equation(15) to solve the second integral with the same formula as in equation(16), and you will get the final result of the receiver field of SLG as given in equation(17), as shown below
The systematic equations derived above for the average intensity and the receptive field appear very complex. But n is the ray order of SLG, which is set to 0.1. As you increase n and gamma, the values drop dramatically when you set n = 5. For the results, the mean density and operational beam size calculations are done quickly by using the formulations that are now derived as described in reference [
28]. As surveys
Although the direction of the receiving plane influences the intensity embodies the intensity of SLG of SLG and is definite as a receiver field.
3. Numeric Computations and Outcomes Analysis
To summarize, the above formula can be used to calculate and derive the propagation of the SLG jet and the average intensity of a non-turbulent atmosphere. In addition, the standardized intensity of the SLG in Figures (4,8,11,13) is dented in different orders of magnitude, so a non-turbulent atmospheric environment of this jet dictates the positions of the jet order (00,01,10,11), scientifically at static propagation distances. Since the x and y directions in Eq. (18) are divisible, the unit of mean intensity in the x path is considered in the figures above. However, the factors used for the calculations are chosen as traces: and λ = 0.8μm. In addition, the standardized intensity power of a Gaussian beam with similar source size is shown in each figure for easy comparison. Since the sharp propagation of the super-LG jet in the basal plane is more advanced than the propagation of the Gaussian jet, the propagation of the SLG jet in a non-turbulent troposphere is less demanding than the propagation of the Gaussian jet. In addition, the difference between the propagation of the SLG beam and the Gaussian beam is increased by specifying the propagation distance z. Therefore, the measured 2D receiver field change between the hypothetical and the mathematical propagation in the x-direction of the SLG beam is shown in Figures (1, 5, 9, 15). In each figure of this receiver plane, the propagation distance is given as z = 2000 m to illustrate the same parameter constant. However, the 2D source field measured with the same parameters is shown in Figures (3,7,10,14). Gaussian part and the smaller Lorentz function The SLG beam is dominated. Therefore, the intensity distribution of the SLG beam in a non-turbulent atmosphere is closest to the Gaussian distribution observed in Figures (1,3,4,5,8,9,11,13,14,15). Accordingly, the effects of the super-Lorentz and Gaussian components are the same and the intensity of the SLG jet has been scattered. To illustrate the propagation of the SLG beam in a turbulent troposphere, the effective receiving field of the SLG beam against the transverse axis in a non-turbulent troposphere is described in each figure. Also, the same control variation of the result for the receiving field in the x and y directions only assumes that the result shown is the same as that observed in each figure. Moreover, the velocity of the SLG beam is the same as that of the smaller beam. As we have already mentioned, these figures (2, 6, 7, 10, 12) refer to the source sizes and propagation distances in different beam orders. To summarize, a hypothetical SLG beam in a non-turbulent troposphere radiates faster at a higher structure constant and is practical in an optical communication system used in lasers. In particular, the comparison with the numerical intensity values is shown in the figures of the receiver field. Finally, we point out symbolically in the figures that the beam has an order in all figures.
Figure 1.
The x-side of an SLG beam at propagation distances in a non-turbulent troposphere is observed in the standardized receiver field of the computational and theoretical deliveries in, z = 2km.
Figure 1.
The x-side of an SLG beam at propagation distances in a non-turbulent troposphere is observed in the standardized receiver field of the computational and theoretical deliveries in, z = 2km.
Figure 2.
SLG beam at propagation distances in a non-turbulent atmosphere, z = 2 km. Stabilized receiver field of the hypothetical propagation on the x-side.
Figure 2.
SLG beam at propagation distances in a non-turbulent atmosphere, z = 2 km. Stabilized receiver field of the hypothetical propagation on the x-side.
Figure 3.
Proliferation reserves in a non-turbulent troposphere, z = 2000 m. Standardized source field supply in the x-guideless of an SLG jet.
Figure 3.
Proliferation reserves in a non-turbulent troposphere, z = 2000 m. Standardized source field supply in the x-guideless of an SLG jet.
Figure 4.
Propagation distances in a non-turbulent troposphere, z = 2000m for Standardized Intensity supplies in the x-side of an SLG beam.
Figure 4.
Propagation distances in a non-turbulent troposphere, z = 2000m for Standardized Intensity supplies in the x-side of an SLG beam.
Figure 5.
The x-side of an SLG beam at spread distances z =2000 m in a nonturbulent troposphere for Regularized receiver field numerical and theoretical distributions.
Figure 5.
The x-side of an SLG beam at spread distances z =2000 m in a nonturbulent troposphere for Regularized receiver field numerical and theoretical distributions.
Figure 6.
Propagation distances z = 2000 m in a non-turbulent troposphere for the standardized receiver field of a hypothetical coverage on the x-side of an SLG beam.
Figure 6.
Propagation distances z = 2000 m in a non-turbulent troposphere for the standardized receiver field of a hypothetical coverage on the x-side of an SLG beam.
Figure 7.
Propagation distance z = 2000 m in the turbulent troposphere for a standardized source field and deliveries on the x-side of an SLG jet.
Figure 7.
Propagation distance z = 2000 m in the turbulent troposphere for a standardized source field and deliveries on the x-side of an SLG jet.
Figure 8.
Dispersion distances z = 2000 m in a non-turbulent troposphere for Standardized Concentration supplies in the x-side of an SLG beam.
Figure 8.
Dispersion distances z = 2000 m in a non-turbulent troposphere for Standardized Concentration supplies in the x-side of an SLG beam.
Figure 9.
SLG jet at proliferation distances z =2000 m in the turbulent troposphere for the mathematical field of the regulated receiver and hypothetical deliveries on the x-side.
Figure 9.
SLG jet at proliferation distances z =2000 m in the turbulent troposphere for the mathematical field of the regulated receiver and hypothetical deliveries on the x-side.
Figure 10.
Propagation of the source size in the turbulent troposphere z = 2000 m for a regulated source field and deliveries on the x-side of an SLG jet.
Figure 10.
Propagation of the source size in the turbulent troposphere z = 2000 m for a regulated source field and deliveries on the x-side of an SLG jet.
Figure 11.
Size of the proliferation source in a raging troposphere z = 2000 m Normalized intensity deliveries in the x-side of an SLG beam.
Figure 11.
Size of the proliferation source in a raging troposphere z = 2000 m Normalized intensity deliveries in the x-side of an SLG beam.
Figure 12.
SLG beam with scattered source size, z =2000 m in the moving troposphere for standardized receiver field, mathematical and hypothetical deliveries in x-direction.
Figure 12.
SLG beam with scattered source size, z =2000 m in the moving troposphere for standardized receiver field, mathematical and hypothetical deliveries in x-direction.
Figure 13.
SLG beam at proliferation source size, z = 2000 m in the turbulent atmosphere for Standardized Strength deliveries in the x-side.
Figure 13.
SLG beam at proliferation source size, z = 2000 m in the turbulent atmosphere for Standardized Strength deliveries in the x-side.
Figure 14.
SLG jet at proliferation source sizes at a distance z = 2000 m in the raging troposphere for the standardized source field and the supply in the x-side.
Figure 14.
SLG jet at proliferation source sizes at a distance z = 2000 m in the raging troposphere for the standardized source field and the supply in the x-side.
Figure 15.
SLG beam at propagation distances z =2000 m in the turbulent troposphere for stabilized receiver field mathematical and hypothetical deliveries on the x-side.
Figure 15.
SLG beam at propagation distances z =2000 m in the turbulent troposphere for stabilized receiver field mathematical and hypothetical deliveries on the x-side.