Submitted:
25 July 2024
Posted:
26 July 2024
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Abstract
Keywords:
1. Introduction
2. The Tool
2.1. Block #1
- The latitude ϕ and the local longitude λ, denoted as λlocal, of the geographical site where the PV module is installed (ϕ is equal to 0° at the equator, and ranges from 0° to 90° to the north, from 0° to -90° to the south; λlocal is equal to 0° at the Prime, or Greenwich, meridian, and ranges from 0° to 180° to east, from 0° to -180° to west).
- The longitude λstandard of the standard meridian on which the clock time (CKT, also referred to as watch time or standard local time) is based.
- The day of the year n.
- The CKT values during the day, i.e., the daytime discretization.
- The solar declination δ, i.e., the angle between the Sun rays (the beam radiation) and the equatorial plane, which is positively defined in the northern hemisphere. Angle δ can be reasonably assumed constant during a day (it varies by at most 0.5°), and dependent on the day of the year n through the empirical Cooper’s relation
- The so-called True Local Time (TLT), which can be obtained from the CKT by applying two corrections. The first correction is dictated by the difference between the local longitude λlocal and the longitude of the standard meridian λstandard; more specifically, the displacement of 1° between these longitudes corresponds to 4 minutes. The second correction is made to account for the non-constancy of the rotation rate of the Earth around the Sun during the year. This effect can be described by introducing a characteristic time referred to as Equation of Time (Eqt) expressed in minutes, which depends on n through the following relation [20,21,22]:
- The hour angle ω, i.e., the angular displacement of the Sun with respect to the local meridian compared to the case in which TLT=12 due to the rotation from west to east of the Earth around its axis (also denoted as angle subtended by the Sun [23]). Angle ω is negative in the morning, positive in the afternoon, and given by [20,22,24,25,26,27]
2.2. Block #2
- The latitude ϕ of the site.
- The CKT values.
- The azimuth angle of the module front γ, which defines the module orientation, as it is the angular displacement from south of the projection of the normal to the module front onto the horizontal plane. An azimuth γ=0° means that the front is south-oriented; γ is positive clockwise (to west), reaching 180° next to north, and is negative counter-clockwise (to east), reaching -180° next to north [21]. Hence, γ=90° corresponds to a module with west-oriented front, while γ=-90° identifies an east-oriented front.
- The tilt angle of the module front β, which is the inclination with respect to the horizontal plane.
- The solar declination δ and the hour angle ω computed by block #1.
- The azimuth angle of the module rear γrear=γ-180°.
- The tilt angle of the module rear as the complement of β, that is, βrear=180°-β.
2.3. Block #3
- The solar altitude α evaluated by block #1.
- The azimuth angles γ, γrear, the tilt angles β, βrear, and the incidence angles θ, θrear.
- The total irradiance Gtoth, the diffuse irradiance Gdh hitting the horizontal plane (the beam, or direct, irradiance Gbh is determined as Gtoth-Gdh), and the ambient temperature Tamb vs. CKT at the selected geographical site. For the analysis performed in Section 3, these data were taken from the PhotoVoltaic Geographical Information System (PVGIS) website [28]. Here it is stated that they were evaluated for the mean day of the chosen month from satellite data through a sophisticate algorithm accounting for sky obstruction (shading) by local terrain features (hills or mountains) calculated from a digital elevation model.
- The albedo value, namely, the ratio of reflected upward radiation from the ground to the incident downward radiation upon it (typical albedo values are 0.04 for fresh asphalt, 0.1-0.15 for soil ground, 0.25-0.3 for green grass, 0.4 for desert sand, 0.55 for fresh concrete, and 0.8 for freshly fallen snow).
- Some key parameters available in the datasheet, i.e., the temperature TNOCT, the short circuit current Iscnom, and the percentage temperature coefficient TCIsc of the short-circuit current Isc, the definitions of which will be provided in the following.
- The block calculates
- The diffuse irradiance on the front coming from the sky, for which there are two options.
- The diffuse irradiance on the front due to the reflection from the ground, typically considered as a Lambertian (isotropic) process, calculated as
- The total irradiances on the front (G) and rear (Grear). The total irradiance on the front is calculated as
2.4. Block #4
- The module is composed by N series-connected cells, each modeled with a subcircuit implementing the SDM described above, which is fed with G, Grear, ΔT.
- The module can be partitioned into a chosen number of subpanels, each equipped with a bypass diode.
- The PSPICE temperature of all components embedded in the circuit is forced to the reference value T0=27°C; the temperature rise ΔT, represented as a voltage, is provided to analog behavioral modeling, or ABM, components (nonlinear current/voltage sources) to modify the temperature-sensitive parameters.
2.5. Simplified variant of the tool for monofacial modules
3. Results and Discussion
3.1. Optimization of Orientation and Tilt for a Bifacial Module
- By specifically referring to the monofacial module, the energy produced by orienting the frontside to west is slightly better than the one obtained by orienting it to east; this result is reasonable since Naples faces the sea to the west while mountains lie to the east.
- As a main finding, it is observed that in these cases the bifacial module allows achieving a significant improvement. While the monofacial panel receives beam irradiance for only half of the day, bifacial panels benefit from effective beam irradiance (hitting the module sides with low incidence angles) both in the morning (rear for a west-oriented panel, as sketched in Figure 5b, and front for an east-oriented one) and afternoon (the other way around).
- West- and east-oriented vertical bifacial panels produce the same amount of energy.
- West- and east-oriented vertical bifacial modules (which produce the same energy) offer equal or even improved performance with respect to the reference monofacial counterpart during the time span from April to September, in which they benefit from a low incidence angle of the Sun rays hitting the front and rear of the panel in the mid-morning and the mid-afternoon [1,10]. In terms of yearly energies (all reported in Table 2), the gain compared to the reference monofacial case amounts to 2.5% and 15% for albedo values equal to 0.2 and 0.5, respectively.
- West- and east-oriented vertical bifacial modules also provide a considerable production improvement with respect to the south-oriented vertical bifacial counterpart, which is estimated to be 13-15%, regardless of the albedo. This is again due to the much better performance of west- and east-oriented panels from April to September, while during wintertime the south-oriented module performs better. An in-depth insight into this behavior can be achieved by showing the normalized maximum power over CKT on July 15 (Figure 11a) and December 15 (Figure 11b) for such cases. In July (and more in general during the whole period from late spring to early autumn), it is confirmed that the orientations of the module front to west and east allow for a very effective exploitation of the beam light impinging on one of the two sides in the mid-morning and on the other in the mid-afternoon, whereas in December (and more in general during wintertime) the orientation to south is better over the mid-day. Along the whole year, the first effect markedly prevails over the second.
3.2. Nonuniform Irradiance Distribution over the Panel Rear
- G=370.49 W/m2, T=38.55°C, Iph=1.064 A, Grear=153.33 W/m2, Iph,rear=0.408 A at 11:00 AM;
- G=88.23 W/m2, T=31.5°C, Iph=0.259 A, Grear=436.45 W/m2, Iph,rear=1.114 A at 3:00 PM.
3.3. Cracked Cell(s)
4. Conclusions
Author Contributions
Funding
Institutional Review Board Statement
Informed Consent Statement
Data Availability Statement
Conflicts of Interest
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| Naples Italy |
Stuttgart Germany [20] |
Madison WI, USA [21] |
Cape Town South Africa |
|---|---|---|---|
|
inputs ϕ=40°50’ λlocal=14°15’ λstandard=15° July 15 (n=196), CKT=16 (4:00 PM) daylight-saving time |
inputs ϕ=48°46’ λlocal=9°10’ λstandard=15° July 1 (n=182), CKT=12 (12:00 AM) daylight-saving time |
inputs ϕ=43°04’ λlocal=-89°-23’ λstandard=-90° February 3 (n=34), CKT=10.5 (10:30 AM) standard time |
inputs ϕ=-33°-55’ λlocal=18°25’ λstandard=30° December 10 (n=344), CKT=9.25 (9:15 AM) standard time |
|
outputs δ=21.52° Eqt=-5.79 minutes TLT=14.85 (2:51 PM) ω=42.80° α=49.13° |
outputs δ=23.12° Eqt=-3.46 minutes TLT=10.55 (10:33 AM) ω=-21.70° α=59.15° |
outputs δ=-16.97° Eqt=-13.49 minutes TLT=10.32 (10:19 AM) ω=-25.26° α=25.64° |
outputs δ=-23.05° Eqt=7.14 minutes TLT=8.60 (8:36 AM) ω=-51.05°α=44.31° |
| Orientation (γ) and tilt (β) | Normalized yearly-produced energy [Wh/Wp] | |
|---|---|---|
| Monofacial | Bifacial | |
| γ=0° (south), β=30° | 1630 (reference) | 1709 (albedo=0.2) 1736 (albedo=0.5) 1763 (albedo=0.8) |
| γ=0° (south), β=90° | 1000 | 1440 (albedo=0.2) 1650 (albedo=0.5) 1860 (albedo=0.8) |
| γ=90° (west), β=90° | 855 | 1670 (albedo=0.2) 1880 (albedo=0.5) 2095 (albedo=0.8) |
| γ=-90° (east), β=90° | 685 | 1670 (albedo=0.2) 1880 (albedo=0.5) 2095 (albedo=0.8) |
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