In this section, we conduct numerical simulations to analyze the transmission characteristics and spatial coherence of the PCLED array in the ocean. In practical applications, the analyses of the optical field and photons in array beam transmission complement each other based on the specific application requirements. As the intensity decreases to the nanowatt level (
) or below, only a small number of photons pass through, requiring consideration of the discreteness and quantum nature of photons. Consequently, the description of the optical field may no longer be applicable. For our simulations, we choose a maximum distance of
and the peak magnitude of the average light intensity distribution is on the order of
. The sub-beam is selected from the widely used green light in the underwater blue-green light band. Moreover, we set the parameter values based on typical values, as shown in
Table 1.
Table 1.
Parameter Settings.
Parameters | Values | Parameters | Values | Parameters | Values |
---|
| 525 [24] | | 0.01 | | 6.4 [25] |
N | 8 | | 51.2 | | 3 |
| 0.053 | | 0.003 | | 0.056 |
| | | | | −2.5 |
3.1. Average Light Intensity
The experimental LED measurements of the spatial coherence lengths were performed using classical techniques as described in [
11,
15,
26]. Additionally, controlling LED-based sources, as outlined in [
27,
28], could be utilized to obtain the spatial coherence length. Based on the collective data, we carefully selected two specific spatial coherence lengths,
and
, representing typical sub-beams for further analysis. By incorporating Equation (
9) and conducting numerical analysis using
Figure 2,
Figure 3 and
Figure 4, we examine the influence of transmission distance
L, attenuation parameters, turbulence parameters, and light source parameters on the average light intensity of the radial PCLED beam array during its propagation in oceanic turbulence.
Figure 2 presents the impact of different
L on the average light intensity of the radial PCLED beam array during its propagation in the ocean. The values of other parameters remain consistent with those specified in
Table 1. The figure reveals that for shorter transmission distances, the light intensity distribution of the beam array displays multiple peaks. As the transmission distance increases, the effects of attenuation and turbulence on the beam array become more pronounced, resulting in the spreading and overlapping of sub-beams. Consequently, the on-axis light intensity gradually increases, leading to a more concentrated energy distribution. For
and
, at a transmission distance of
m, the beam array attains a maximum light intensity of approximately 40
. As the spatial coherence length decreases, the light intensity distribution degrades into a Gaussian-like distribution earlier as the distance increases, accompanied by a notable reduction in peak intensity. The beam spreading of the converging beam becomes more prominent. For a transmission distance of 10m, the peak intensities decrease to 26.17
and 5.11
for
and
, respectively. This demonstrates that the intensity distribution of the beam array is significantly influenced by water attenuation and turbulence parameters. Further analysis is provided in
Figure 3 and
Figure 4.
To provide a clearer understanding of the influence of different water attenuation coefficients on the beam array, a transmission distance of
m is selected.
Figure 3 illustrates the average light intensity of the radial PCLED beam array propagated through oceanic turbulence for water attenuation coefficients of 0
, 0.056
, 0.150
, and 0.305
in different water types [
21]. The other parameters remain the same as
Table 1. From the figure, it is evident that under the conditions of
and
, the impact of various attenuation coefficients on the beam array after normalization is proportionally the same. As the water attenuation coefficient increases, the average light intensity along the optical transmission path of the PCLED beam array notably decreases. For
, the maximum light intensity values of the PCLED beam array corresponding to different attenuation coefficients are 46.02
, 26.28
, 10.22
, and 2.17
, respectively. In the case of
, the maximum light intensity values are 8.94
, 5.10
, 1.99
, and 0.42
, respectively. This finding confirms that the water attenuation coefficient affects the average intensity distribution of the beam array, independent of the spatial coherence of the sub-beams within the light source.
To provide a more comprehensive understanding of the influence of turbulence parameters on the average light intensity of the radial PCLED beam array,
Figure 4 depicts the average light intensity at a transmission distance of
m for various values of kinetic energy dissipation rate
, temperature dissipation rate
, temperature-to-salinity ratio
, as well as the sub-beam spatial coherence length
. The values of the other parameters are given in
Table 1. From the analysis of
Figure 4a,b, it is evident that as the value of
decreases, indicating larger turbulence scales and increased turbulence intensity [
29], the impact on the average light intensity of the PCLED beam array becomes less significant. In the case of
=
,
, and
shown in
Table 2, the light intensity distribution gradually transitions from a multi-peak distribution to a Gaussian-like distribution. This observation reveals that as the
changes on the order of micrometers, the peak intensity of the beam array diminishes by approximately a factor of 12. Based on
Figure 4(a2,b2), with an increase in
, there is a substantial augmentation in turbulence intensity, resulting in notable alterations in both the distribution and peak intensity of light. This escalation signifies a more active oceanic turbulence [
30]. Notably, the impact on the array’s light intensity distribution is more pronounced when the
is larger. Based on
Figure 4(c3,b3), as
increases, there is a gradual decrease in the peak intensity of the array beams, accompanied by a transition in the light intensity distribution from a multi-peak pattern to a Gaussian-like distribution. This degradation is particularly prominent when
is smaller.
To further analyze the impact of
on the array beams,
Figure 5 illustrates the variations in the average light intensity of the radial PCLED array beams at a distance of
m for different
. When
, the light source can be approximated as a laser array, and while
, the light source can be regarded as a fully incoherent light array. The curves overlap as for
values of 50
and 0. As observed from the graph, when
is smaller, the average light intensity of the array beams is influenced by attenuation and turbulence along the oceanic transmission path. Not only does it achieve combining of sub-beams earlier, but it also results in a larger combining spot size. For the aforementioned parameter values of
, the peak light intensity of the radial PCLED array beams is 0.77
, 0.91
, and 0.92
, respectively. This finding aligns with conclusions drawn from underwater experimental studies, where LEDs with smaller
values exhibit closer underwater light transmission distances and larger beam spreading compared to lasers with larger
values [
29].
The radial fill factor parameter, denoted as
, is introduced to quantify the compactness of the beam array arrangement. A smaller value indicates a tighter arrangement of the beams, with
.
Figure 6 illustrates the light intensity distribution of the PCLED beam array at the observation plane of
m for various
. When
, the peak light intensities of the radial PCLED beam array are 26.28
, 27.09
, and 48.95
for
values of 3, 2, and 1, respectively. When
, the peak light intensities of the array are 5.11
, 10.01
, and 16.38
, respectively. As
increases, the peak light intensity decreases, accompanied by the dispersion of beam energy and a spreading effect on the array beam. This reduction in intensity is a consequence of decreased coherence between the sub-beams, arising not only from the spatial coherence length of the individual sub-beams but also from the decreased compactness of the beam array arrangement as a whole.
3.2. Array Beam Width
Numerical simulations of the average light intensity reveal that the water attenuation coefficient does not cause beam spreading. Combining with Equation (
12),
Figure 7 and
Figure 8 numerically analyze the effects of the turbulence parameters of
,
,
, and
on the beam width of the radial PCLED beam array in oceanic turbulence. The remaining parameters are set as described in
Table 1.
Figure 7 depicts the changes in the beam width of the radial PCLED beam array as
L increases under different turbulence parameters. From the graph, it is evident that for
and
, the array beam undergoes varying degrees of spreading under different turbulence conditions. Specifically,
Figure 7a shows a gradual change in the array beam width starting from
m, while
Figure 7b indicates that the array beam width experiences changes from
m. As the turbulence parameter
decreases,
increases, and
increases, array beam spreading becomes more pronounced, shown in
Table 3. Specially, when
is
or
, the array width is affected by turbulence to almost the same extent. However, at
and
values of 500
and 50
, the array widths are 0.197 m and 0.536 m, respectively. In brief, the spreading effect of the radial PCLED array beam width is mainly influenced by the turbulence parameters
and
, while the influence of
is relatively smaller. Additionally, a smaller value of
leads to a reduced spreading effect.
To further investigate the impact of
on the array width,
Figure 8 depicts the variations in the beam width of the radial PCLED array for
values of 5000
, 500
, and 50
. From the graph, it can be observed that as the value of
decreases, the beam width increases. Specifically, for the mentioned parameter values of
, the array beam width starts changing from
m,
m, and
m, respectively. At the observation plane located at
m, the corresponding beam widths are measured as
m,
m, and
m. When considering practical engineering applications, it becomes crucial to select an appropriate value of
based on specific requirements. This finding emphasizes the significance of accounting for beam spreading in LED array systems and highlights their advantages in short-range directional transmission and positioning applications.
Figure 9 illustrates the variations in the beam width of the radial PCLED beam array in oceanic turbulence with increasing
L for different values of
, with other parameters as listed in
Table 1. From the graph, it can be observed that as
decreases, the spreading of the array beam becomes more pronounced. Particularly at the observation plane of
m, when
, the beam width of the radial PCLED beam array is 2.8 times larger for
compared to
. When
, the beam width variations of the array overlap for different radial fill factors after
m.
3.3. Spatial Coherence
Investigating the spatial coherence of the received array beam section not only enhances system performance and reliability but also improves interference resistance, enables precise beam management and control, and provides guidance for antenna design and optimization. By utilizing Equation (
13), it is possible to analyze the changes in the spatial coherence of the PCLED beam array in the oceanic transmission path. This analysis takes into account
L,
, turbulence parameters, and
.
To comprehensively analyze the variation patterns of
,
Figure 10 illustrates the changes in
as
L increases for different values of
. To illustrate the comparison of results, the values of
are introduced as 5000
, 500
, and 50
, respectively. By setting
, the corresponding values of
can be obtained, enabling the determination of the variation patterns of
on the observation plane with increasing distance. From the graph, it is evident that as
varies,
exhibits a multi-peak phenomenon. For
L values of 50 m, 100 m, and 150 m, when
, the corresponding values of
are
mm,
mm, and
mm, respectively. When
, the values of
are
mm,
mm, and
mm, and when
, the values of
are
mm,
mm, and
mm. This indicates that under the given conditions of oceanic turbulence parameters, when the transmission distance is relatively short, the free-space diffraction effect of the beam is stronger than the turbulence effect, resulting in an increased distribution width of
. As
L increases, the cumulative effect of turbulence becomes more pronounced. However, due to the relatively small value of
, the turbulence effect does not dominate the variation in the distribution of
. As a result, the coherence of the beam is minimally affected, and the distribution width of
continues to increase. This finding suggests that the spatial coherence of PCLED arrays is less affected by turbulence in the oceanic transmission path compared to laser arrays discussed in literatures.
To investigate the impact of turbulence parameters on the spatial coherence of the array beams for different
values,
Figure 11 depicts the variations of
at the observation plane with
m, considering
values of 5000
, 500
, and 50
, and the specific values of
are shown in
Table 4. From
Figure 11a–c, it can be observed that as
and
increase and
decreases, the beam width
of the array gradually narrows, indicating a degradation of spatial coherence. The distribution of the beam’s spatial coherence evolves from a multi-peak distribution to a Gaussian distribution.
Figure 12 illustrates the impact of different
on the spatial coherence distribution of radial PCLED array beams at the observation plane of
m. The remaining parameters are consistent with those specified in
Table 1. The graph demonstrates that increasing the value of
leads to a decrease in
, with the values approaching each other. Specifically, when
is set to 5000
, 500
, and 50
, the corresponding values of
are
mm,
mm, and
mm, respectively. Combining this information with the preceding average intensity distribution, it becomes evident that the micrometer level of
for PCLED array itself exhibit a dampening effect on the oceanic turbulence phenomenon at observation planes characterized by relatively low light intensities.
To further analyze the influence of the radial filling factor of the light source on the spatial coherence of the array,
Figure 13 illustrates the variation curve of the beam array’s spatial coherence at the observation plane with
m. The graph reveals that an increasing value of
leads to a more dispersed arrangement of the beams, resulting in a significant reduction in the width of the
value distribution. Moreover, the distribution of the array’s spatial coherence exhibits oscillations with multiple peaks as the distance from the axis increases. However, at the observation plane with
m, where the light intensity is relatively weak, the variation in the spatial coherence of the beam array is not obvious. When considering
values of 1, 2, and 3, with
, the corresponding
values are
mm,
mm, and
mm, respectively. When
, the
values are
mm,
mm, and
mm, respectively. When
, the
values are
mm,
mm, and
mm, respectively. These findings indicate that the radial PCLED beam array itself possesses the ability to suppress turbulence effects during oceanic transmission. Furthermore, by optimizing diversity reception, the application of LED array light sources can be extended beyond close-range high-speed transmission purposes, such as underwater communication and imaging.