Modeling the Output Performance of Al 0 . 3 Ga 0 . 7 As / InP / Ge Triple-Junction Solar Cells for a Venus Orbiter Space Station

The performance of Al0.3Ga0.7As/InP/Ge triple-junction solar cells (TJSC) at the geosynchronous orbit of Venus had been simulated in this paper by assuming that the solar cells were put on a hypothetical Venus orbiter space station. The incoming solar radiation on TJSC was calculated by a blackbody radiation formula, while PC1D program simulated the electrical output performance. The results show that the incoming solar intensity at the geosynchronous orbit of Venus is 3000 W/m2, while the maximum solar cell efficiency achieved is 38.94%. Considering a similar area of the solar panel as the International Space Station (about 2500 m2), the amount of electricity produced by Venus orbiter space station at the geosynchronous orbit of Venus is 2.92 MW, which is plenty of energy to power the space station for long-term exploration and intensive research on Venus.


Introduction
Space exploration and the human effort to find a new place to live in the outer space has never been weakened since the dawn of NASA in 1958.The observation and exploration of Mars, Europa, Enceladus or even Gliese 581 g are some of the highlights in our effort to find a new habitable place in the future.Comparing to Mars, which is located about 0.52 AU (Astronomical Unit) from Earth, Venus offers a less distance to Earth with only 0.28 AU.The almost similar size of Venus makes this planet sometimes called Earth's twin and sheds some hopes for future human colonization.However, the hostile conditions of Venus's atmosphere, which is dominated by carbon dioxide and sulfuric acid droplets, makes its surface temperature reach above 450 • C and discounts any possibility of making this planet a habitable place in the future.There is still some research considering Venus as a promising place to live done, among others, by Landis et al. [1][2][3][4][5][6][7].Even US National Academies of Science Space Studies placed Venus exploration as one of the highest priorities for medium-class future missions [8].Landis et al. proposed some ideas to intensively studying Venus by using a solar airplane, sending a robotic exploration of the surface and atmosphere of Venus [3,5,6,[9][10][11][12][13].Based on the fact that the upper atmosphere of Venus at an altitude of 50 km has similar pressure, gravity, density, and radiation protection to that of the Earth, NASA had proposed a High-Altitude Venus Operational Concept (HAVOC) project to conduct a 30-day crewed mission into Venus atmosphere.Although this project is no longer active, more ideas and refinement to this conceptual mission are still ongoing [14,15].Japan has also shown interest in studying Venus by sending a Venus Climate Orbiter (VCO) in the year of 2010 [16] to intensively study the climate of Venus.In 2015, Japan Aerospace Exploration Agency (JAXA) discovered a new phenomenon called the Venusian equatorial jet, a strong wind in the low and middle cloud layer (45 to 60 kilometers of altitude) of Venus atmosphere [17].
To conduct a continuous and intensive study on Venus exploration, we propose the development of an ISS-like station (ISS stands for the international space station) dedicated to studying Venus.Having this IVOSS (international Venus orbiter space station), more intensive research and missions can be deployed to this planet, including the one proposed by Landis et al. [3,9].To power this hypothesized space station, a high-efficiency solar cell based on the combination of III-V groups solar cells like GaInP, GaInAs, AlGaAs, InP, and GaAs might be used in the form of multijunction solar cells (MJSC).The unique electronic structure of III-V based materials had long been known to have a wide range of applications, such as in quantum wells LED [18][19][20][21][22][23], laser [24], sensors [25], and also solar cells [26][27][28][29][30][31].Those III-V groups solar cells are known for their ability to withstand harsh conditions in the outer space, such as energetic particles and high temperature [32][33][34][35].
The MJSC is an arrangement of several p-n junctions of semiconducting materials which are stacked following the order of their bandgap energies.The highest bandgap material is put on top while the lowest in the bottom.This arrangement will minimize the spectrum loss and increase the efficiency of MJSC as compared to a single junction solar cell.The typical MJSC on Earth's surface can produce above 30% efficiency under one sun solar radiation and almost approaching 50% when exposed to several hundreds of times of solar radiation by using solar concentrators [36][37][38].The closer distance of Venus to the sun will ensure more power produced by the IVOSS's solar panels at this position as compared to the Earth's geosynchronous orbit.The most common solar cells used for the space application is GaAs which can produce efficiency of up to 22.08% [39], while InGaP/GaAs/InGaAs TJSC can deliver 37.9% efficiency [40].For the latest development and high-efficiency record of MJSC especially for the space application, one can refer to Reference [41].
In this paper, we simulate the performance of Al 0.3 Ga 0.7 As/InP/Ge TJSC for the application in the hypothetical IVOSS space station.The selection of Al 0.3 Ga 0.7 As compound as a first subcell was based on its higher energy gap (1.817 eV) which allows more spectral energy to be absorbed by MJSC.Most of the experimental and modeling reports were based on GaInAs and GaInP ternary compounds and they rarely discussed the AlGaAs based solar cell [42][43][44][45].This paper was intended to broaden our perspective in terms of material selection and its consequence to the total efficiency of MJSC, especially for the extra-terrestrial application.The simulation was done using an ideal (toy) model in which each subcell was simulated independently without considering the tunnel junction between each subcell.The solar cell in this simulation is assumed to be an array of the multi-homo-junction solar cell in which the p and n-type of each subcell were made from the same material.A similar schematic model has been used by other researchers, such as Reference [46,47].The temperature of each subcell was held constant in this simulation (at T = 25 • C) by assuming that the solar panels were equipped with a temperature control system, such as in Reference [48,49].The effect of cosmic radiation was also not taken into account in this simulation.The IVOSS was positioned at the geosynchronous orbit of Venus and cleared from the atmospheric blanket of Venus so that the ideal blackbody radiation formula could approximate the incoming radiation.The performance of TJSC at the geosynchronous orbit of Venus will be compared to its performance at the geosynchronous orbit of Earth.
Since this paper emphasizes the simulation approach of MJSC, we do not discuss the specific fabrication technique of MJSC.We assume that Al 0.3 Ga 0.7 As/InP/Ge has a similar fabrication technique as other III-V MJSC, such as GaP/InGaAs/InGaSb [50] where the IMM (inverted metamorphic multi-junction solar cells) concept is applied.The growing of subcells in the IMM concept is started from the top to the bottom-cell using the MOCVD (metal organic chemical vapor deposition) technique [47] and can produce a 34.2% efficiency in space application [51].Various fabrication techniques, such as molecular beam epitaxy (MBE), were able to fabricate InGaAs/GaAs quantum dot solar cell [52] and InGaP/GaAs/GaInAs monolithic tandem solar cell [53].

Materials and Methods
The incoming solar radiation to MJSC was prepared by calculating the spectral irradiance using the blackbody radiation formula.The response of each junction (subcell) and the amount of the transmitted radiation were calculated using the absorption coefficient formula and the Berr-Lambert's-like equation.Finally, the electric power produced by each subcell was simulated using PC1D program.The PC1D program solves the highly nonlinear transport equation of electron (and hole) in a semiconductor device by discretizing the equation using the finite element method (FEM).The Poisson equation consisting of the spatial-dependence of local quasi-Fermi potential, conductivity and current density at each node were linearized iteratively and solved by matrix inversion method until it reached the convergence.[54].
The distance R svg is the distance from the center of the sun to the geosynchronous orbit of Venus, and defined as: where R sv is the distance between the center of the sun to the center of Venus (R sv = 1.0748 × 10 11 m), and R vg is the distance between the center of Venus to its geosynchronous orbit (R vg = 1.5372 × 10 9 m).
The schematic of distances is shown in Figure 1.
Photonics 2019, 6, x FOR PEER REVIEW 3 of 12 The incoming solar radiation to MJSC was prepared by calculating the spectral irradiance using the blackbody radiation formula.The response of each junction (subcell) and the amount of the transmitted radiation were calculated using the absorption coefficient formula and the Berr-Lambert's-like equation.Finally, the electric power produced by each subcell was simulated using PC1D program.The PC1D program solves the highly nonlinear transport equation of electron (and hole) in a semiconductor device by discretizing the equation using the finite element method (FEM).The Poisson equation consisting of the spatial-dependence of local quasi-Fermi potential, conductivity and current density at each node were linearized iteratively and solved by matrix inversion method until it reached the convergence.[54].
The distance Rsvg is the distance from the center of the sun to the geosynchronous orbit of Venus, and defined as: where Rsv is the distance between the center of the sun to the center of Venus (Rsv = 1.0748 × 10 11 m), and Rvg is the distance between the center of Venus to its geosynchronous orbit (Rvg = 1.5372 × 10 9 m).
The schematic of distances is shown in Figure 1.The surface temperature of the sun was set to T = 6000 K.The incoming spectral irradiance (the radiation intensity divided by the wavelength) of blackbody radiation received by the IVOSS in Venus geosynchronous orbit is expressed as: where rs is the diameter of the sun, λ is the radiation wavelength, h is Planck's constant (h = 6.626 × 10 −34 J.s), and kB is the Boltzmann's constant (kB = 1.38 × 10 −23 J/K).By integrating the whole spectrum, the total power density (the entire area under the I(λ) vs. λ curve) at a particular distance from the sun can be found.The same formula was also used to calculate the incoming spectral irradiance received in Earth's geosynchronous orbit by modifying all the distance parameters in Equation ( 2).For a terrestrial application on Earth, plenty of accurate spectral irradiance data, such as AM1.5G and AM1.5D, can be utilized.However, the actual/experimental data on solar radiation intensity at the geosynchronous orbit of Venus to the best of authors' knowledge are not readily available.The High Altitude Venus Operational Concept (HAVOC) project by NASA [15] calculated that the solar intensity at the altitude of 50 km from the Venus surface is around 1.42 kW/m 2 .This value is smaller as compared to the blackbody calculation at the geosynchronous orbit of Venus located at a distance of about 115 times of the Venus radius.The amount of electric power gained by the space station at the geosynchronous orbit of Venus can be calculated via a simple blackbody radiation formula.The surface temperature of the sun was set to T = 6000 K.The incoming spectral irradiance (the radiation intensity divided by the wavelength) of blackbody radiation received by the IVOSS in Venus geosynchronous orbit is expressed as: where r s is the diameter of the sun, λ is the radiation wavelength, h is Planck's constant (h = 6.626 × 10 −34 J.s), and k B is the Boltzmann's constant (k B = 1.38 × 10 −23 J/K).By integrating the whole spectrum, the total power density (the entire area under the I(λ) vs. λ curve) at a particular distance from the sun can be found.The same formula was also used to calculate the incoming spectral irradiance received in Earth's geosynchronous orbit by modifying all the distance parameters in Equation ( 2).For a terrestrial application on Earth, plenty of accurate spectral irradiance data, such as AM1.5G and AM1.5D, can be utilized.However, the actual/experimental data on solar radiation intensity at the geosynchronous orbit of Venus to the best of authors' knowledge are not readily available.The High Altitude Venus Operational Concept (HAVOC) project by NASA [15] calculated that the solar intensity at the altitude of 50 km from the Venus surface is around 1.42 kW/m 2 .This value is smaller as compared to the blackbody calculation at the geosynchronous orbit of Venus located at a distance of about 115 times of the Venus radius.The amount of electric power gained by the space station at the geosynchronous orbit of Venus can be calculated via a simple blackbody radiation formula.
The coefficient of absorption of each subcell was calculated using Equation (3) following Reference [55]: where α(λ) is the coefficient absorption as a function of the wavelength, E g is the bandgap energy of the corresponding junction and E is the incoming photon energy at a particular wavelength.Once we have the spectral irradiance, we can input this to PC1D with several additional steps.There are several options in preparing the solar radiation input in PC1D program, through the internal source (monochromatic or blackbody radiation) or the external source.In this paper, we will use the external radiation source obtained from the calculation of blackbody radiation at the geosynchronous orbit of Venus and Earth in Equation ( 2).Those external spectrums must be saved in *.spc format and have two columns of data, the wavelength and power density F(λ) (in W/m 2 ).The amount of data read by PC1D program only limited to 200 rows, therefore for more than 200 pieces of data we have to average the input data by following the scheme as seen in Figure 2. As an example, to average three subsequent data, the interval of i th wavelength is defined as, while the i th power density is, and q is the number data segment considered in the particular range (in the case above q = 2), The intensity of the i th data is, and the corresponding wavelength λ i is For this TJSC simulation, the wavelength spans from 112 nm to 2500 nm with 1.00 nm data increment.There is a maximum limit of 200 pieces of data to be included in PC1D program, so in our simulation, we have to average every 13 pieces of data to become a single piece of data of λ vs. I(λ).The coefficient of absorption of each subcell was calculated using Equation (3) following Reference [55] : where α(λ) is the coefficient absorption as a function of the wavelength, Eg is the bandgap energy of the corresponding junction and E is the incoming photon energy at a particular wavelength.Once we have the spectral irradiance, we can input this to PC1D with several additional steps.There are several options in preparing the solar radiation input in PC1D program, through the internal source (monochromatic or blackbody radiation) or the external source.In this paper, we will use the external radiation source obtained from the calculation of blackbody radiation at the geosynchronous orbit of Venus and Earth in Equation ( 2).Those external spectrums must be saved in *.spc format and have two columns of data, the wavelength and power density F(λ) (in W/m 2 ).The amount of data read by PC1D program only limited to 200 rows, therefore for more than 200 pieces of data we have to average the input data by following the scheme as seen in Figure 2. As an example, to average three subsequent data, the interval of i th wavelength is defined as, while the i th power density is, and q is the number data segment considered in the particular range (in the case above q = 2), The intensity of the i th data is, and the corresponding wavelength λi is For this TJSC simulation, the wavelength spans from 112 nm to 2500 nm with 1.00 nm data increment.There is a maximum limit of 200 pieces of data to be included in PC1D program, so in our simulation, we have to average every 13 pieces of data to become a single piece of data of λ vs. I(λ).The incoming intensity to the n th subcell, I n depends on the amount of the previous solar radiation I n−1 , the thickness of the previous subcell d n−1 , and the absorption coefficient of the previous subcell α n−1 (λ), following Equation (4): With α 0 = 0 and d 0 = 0 representing the open space (vacuum), medium and I 0 is obtained from Equation (2).The thickness of the n th cell, d n was calculated using the PC1D program.Since this program can only simulate one layer at a time, several simulations depending on the number of junctions involved must be performed.For each set of simulation, the electrical performance of the TJSC in the form of the short circuit current (I SC ), the open circuit voltage (V OC ) and the output power of each subcell (P n ) was recorded.The total efficiency (η) of a mechanically-stacked TJSC was calculated by summing up all electric power produced by each subcell: To analyze the individual performance of each subcell, we also define some terms, i.e., relative efficiency (η n ) and relative loss (L n ) of each subcell: where P n is the electric power produced by the n th subcell, and P n_abs is the absorbed power of the n th subcell, and P n 0 is the incoming power at n th subcell (P n 0 = I n •A) with A is the area of the solar cell.The fill factor (FF) of each subcell was calculated via the formula below, where V noc and I nsc is the open circuit voltage and the short circuit current of the n th subcell, respectively.The intensity (or power) distribution in each subcell follows this relation below, In which the subscript labels denote incoming, absorbed, transmitted, output, and dissipated intensity, respectively.

The Solar Radiation Spectrums
The spectrum of incoming radiation (blackbody approximation) on the geosynchronous orbit of Venus and Earth were shown in Figure 3.The total power density (intensity) as calculated by Equation ( 6) on the geosynchronous orbit of Venus is 3000 W/m 2 and for Earth's geosynchronous orbit is 1557 W/m 2 .If it is assumed that IVOSS has the same solar panel area as ISS has, which is around 2500 m 2 , the total potential of solar energy available at the geosynchronous orbit of Venus is about 7.50 MW, which is plenty of energy to power the space station.The transmitted radiation to the next subcell depends on the absorption coefficient and the optimum thickness of the solar cell's materials.The first subcell, Al0.3Ga0.7As,absorbs the solar radiation from 112 nm up to its cut-off wavelength of 645 nm.The second subcell, InP, absorbs the radiation in the medium wavelength region up to 868 nm, and the last subcell, Ge, works in the long wavelength region up to 1765 nm.

Simulation of the Performance of the Solar Cells at the Geosynchronous Orbit of Venus
The power producing simulations were performed by using the PC1D program using a series connection model of subcells.By maintaining the same amount of current in each subcell, the optimum value of subcell's thickness and the amount of doping were optimized by the quick batch mode in PC1D program.The input parameters for PC1D program are shown in Table 1.The thickness of the subcell grows as we move from the first to the third subcell.The first subcell is the thinnest (2.889 µm for Al0.3Ga0.7As)as compared to other subcells due to plenty of solar radiation received by this subcell.The next subcells, on the other hand, must be thicker (4.222 µm for InP and 15.56 µm for Ge) to absorb as much transmitted radiation as possible.The thickness of the subcells in this simulation is comparable to the result of other III-V MJSC (GaP/InGaAs/InGaSb) by Reference [50] where the cumulative (emitter and base) thickness of the first, second and third subcell are 10.35 µm, 4.55 µm, and 14.20 µm, respectively.The n-doping dominates the carrier concentration of each subcell in the TJSC since the electron plays the role of a charge carrier.The n and p-doping density in this simulation are also within the same range (10 17 to 10 19 ) as Reference [50].The simulation results on the spectral and electrical performance of TJSC are shown in Table 2.For simplicity, the unit of intensity in this table was mW/cm 2 (not W/m 2 ), since the area of the subcell in the PC1D simulation was set to 1.0 cm 2 .For the first subcell, the incoming radiation is 300 mW/cm 2 , Figure 3.The incoming spectral irradiance at the geosynchronous orbit of Venus and Earth calculated using a blackbody radiation formula.The total power density (intensity) at the geosynchronous orbit of Venus is 3000 W/m 2 , while for Earth it is 1557 W/m 2 .
The transmitted radiation to the next subcell depends on the absorption coefficient and the optimum thickness of the solar cell's materials.The first subcell, Al 0.3 Ga 0.7 As, absorbs the solar radiation from 112 nm up to its cut-off wavelength of 645 nm.The second subcell, InP, absorbs the radiation in the medium wavelength region up to 868 nm, and the last subcell, Ge, works in the long wavelength region up to 1765 nm.

Simulation of the Performance of the Solar Cells at the Geosynchronous Orbit of Venus
The power producing simulations were performed by using the PC1D program using a series connection model of subcells.By maintaining the same amount of current in each subcell, the optimum value of subcell's thickness and the amount of doping were optimized by the quick batch mode in PC1D program.The input parameters for PC1D program are shown in Table 1.The thickness of the subcell grows as we move from the first to the third subcell.The first subcell is the thinnest (2.889 µm for Al 0.3 Ga 0.7 As) as compared to other subcells due to plenty of solar radiation received by this subcell.The next subcells, on the other hand, must be thicker (4.222 µm for InP and 15.56 µm for Ge) to absorb as much transmitted radiation as possible.The thickness of the subcells in this simulation is comparable to the result of other III-V MJSC (GaP/InGaAs/InGaSb) by Reference [50] where the cumulative (emitter and base) thickness of the first, second and third subcell are 10.35 µm, 4.55 µm, and 14.20 µm, respectively.The n-doping dominates the carrier concentration of each subcell in the TJSC since the electron plays the role of a charge carrier.The n and p-doping density in this simulation are also within the same range (10 17 to 10 19 ) as Reference [50].The simulation results on the spectral and electrical performance of TJSC are shown in Table 2.For simplicity, the unit of intensity in this table was mW/cm 2 (not W/m 2 ), since the area of the subcell in the PC1D simulation was set to 1.0 cm 2 .For the first subcell, the incoming radiation is 300 mW/cm 2 , with 136.18 mW/cm 2 is absorbed and 163.82 mW/cm 2 (54.61%) is transmitted to the next subcell.About 65 mW of electricity is produced in each cm 2 area of the first subcell (21.67% relative efficiency as compared to the incoming radiation on the first subcell).The dissipated energy in the first subcell is 71.18 mW (23.73% relative energy loss).Therefore, the amount of electric power produced in the first subcell is slightly smaller than the energy loss.In the second subcell, the incoming radiation power received is 163.82 mW/cm 2 , of which 60.08 mW/cm 2 is absorbed and 103.74 mW/cm 2 (63.32%) is transmitted to the third subcell.The electric power produced by the second subcell is 43.4 mW (about 26.49% relative efficiency), while the energy loss is only 15.48 mW (9.45% relative loss).The amount of electric power produced by the second subcell is bigger (by a factor of 2.8) than the energy loss.In the third subcell, the incoming solar radiation intensity is 103.74 mW/cm 2 .Most of the incoming solar intensity in the third subcell will be passed to the air (84.2 mW or about 81.16%) and only 18.84% absorbed.The absorbed power in 1.0 cm 2 is 19.54 mW, and only 8.42 mW of electric power produced (8.12% of relative efficiency), while 11.12 mW will be dissipated (10.72% relative energy loss).The total efficiency of the Al 0.3 Ga 0.7 As/InP/Ge TJSC in geosynchronous orbit of Venus is 38.94%.This amount of efficiency is within the range of some recent results on III-V group multijunction solar cells [30,37,[56][57][58][59].The maximum power gained in 1.0 m 2 solar panel at Venus's geosynchronous orbit is 1168.2W. By assuming the total area of solar panel of IVOSS is similar to ISS, which is around 2500 m 2 , the amount of power produced by Al 0.3 Ga 0.7 As/InP/Ge TJSC at the geosynchronous orbit of Venus is 2.92 MW.Based on PC1D optimization, the amount of current flows in a series connected subcells is 47.7 mA, while the open circuit voltage V OC in the first subcell is bigger than in the second subcell and the third subcell.Almost similar current is found in a CuInGaSe (CIGS) based solar cell [60] applied in space application.The V OC of the second subcell and the third subcell is only 68.87% and 17.09% of the first subcell, respectively.This gradation of V OC is expected, as those voltages are related to the amount of electrical power produced by each subcell.The I-V diagram of Al 0.3 Ga 0.7 As/InP/Ge TJSC at the geosynchronous orbit of Venus is shown in Figure 4.
Photonics 2019, 6, x FOR PEER REVIEW 7 of 12 with 136.18 mW/cm 2 is absorbed and 163.82 mW/cm 2 (54.61%) is transmitted to the next subcell.About 65 mW of electricity is produced in each cm 2 area of the first subcell (21.67% relative efficiency as compared to the incoming radiation on the first subcell).The dissipated energy in the first subcell is 71.18 mW (23.73% relative energy loss).Therefore, the amount of electric power produced in the first subcell is slightly smaller than the energy loss.In the second subcell, the incoming radiation power received is 163.82 mW/cm 2 , of which 60.08 mW/cm 2 is absorbed and 103.74 mW/cm 2 (63.32%) is transmitted to the third subcell.The electric power produced by the second subcell is 43.4 mW (about 26.49% relative efficiency), while the energy loss is only 15.48 mW (9.45% relative loss).The amount of electric power produced by the second subcell is bigger (by a factor of 2.8) than the energy loss.In the third subcell, the incoming solar radiation intensity is 103.74 mW/cm 2 .Most of the incoming solar intensity in the third subcell will be passed to the air (84.2 mW or about 81.16%) and only 18.84% absorbed.The absorbed power in 1.0 cm 2 is 19.54 mW, and only 8.42 mW of electric power produced (8.12% of relative efficiency), while 11.12 mW will be dissipated (10.72% relative energy loss).The total efficiency of the Al0.3Ga0.7As/InP/GeTJSC in geosynchronous orbit of Venus is 38.94%.This amount of efficiency is within the range of some recent results on III-V group multijunction solar cells [30,37,[56][57][58][59].The maximum power gained in 1.0 m 2 solar panel at Venus's geosynchronous orbit is 1168.2W. By assuming the total area of solar panel of IVOSS is similar to ISS, which is around 2500 m 2 , the amount of power produced by Al0.3Ga0.7As/InP/GeTJSC at the geosynchronous orbit of Venus is 2.92 MW.
Based on PC1D optimization, the amount of current flows in a series connected subcells is 47.7 mA, while the open circuit voltage VOC in the first subcell is bigger than in the second subcell and the third subcell.Almost similar current is found in a CuInGaSe (CIGS) based solar cell [60] applied in space application.The VOC of the second subcell and the third subcell is only 68.87% and 17.09% of the first subcell, respectively.This gradation of VOC is expected, as those voltages are related to the amount of electrical power produced by each subcell.The I-V diagram of Al0.3Ga0.7As/InP/GeTJSC at the geosynchronous orbit of Venus is shown in Figure 4.The same procedure of current producing simulation using PC1D program was done for solar cells application at the geosynchronous orbit of Earth.The same input parameter set up as in Table 1 (bandgap, thickness, and p and n doping density) is also used in this simulation, and the only difference is the input spectral irradiance.The simulation results on the spectral and electrical performance of TJSC at the geosynchronous orbit of Earth are shown in Table 3.Since the distance of this orbit to the sun is further as compared to the geosynchronous orbit of Earth, the amount of solar radiation and the electric power produced in this condition is smaller.The first subcell receives 155.7 mW of solar radiation power for every 1.0 cm 2 of the panel area and produces a 33.3 mW of electric power (about 21.39% of relative efficiency).The dissipated power in the first subcell is 37.4 mW (24.02% relative loss of power), while the transmitted power to the second subcell is 85 mW (54.6% of the incoming intensity to the first subcell).Similar to the case of Venus's geosynchronous orbit, the amount of electric power produced by the first subcell in Earth's geosynchronous orbit is slightly smaller than the relative energy loss.In the second subcell, the electric power generated is 22.10 mW (26% of relative efficiency), while the dissipated power is 9.05 mW (about 10.6% relative loss).The amount of electric power produced by the second subcell is bigger (by a factor of 2.4) than the energy loss.The amount of transmitted power to the third subcell is 53.85 mW, about 63.35% of the incoming intensity at the second subcell.The electric power produced by the third subcell is 4.0 mW (about 7.4% relative efficiency), while the dissipated power is 6.13 mW (about 11.4% relative loss).The amount of the transmitted power from the third subcell to free space is 43.72 mW, approximately 81.19% of the incoming intensity at the third subcell.The total efficiency of the Al 0.3 Ga 0.7 As/InP/Ge TJSC at the geosynchronous orbit of Earth in this simulation is 38.15%.The similar amount of power efficiency of Al 0.3 Ga 0.7 As/InP/Ge TJSC in both orbital conditions might come from the fact that in both cases the only variable is the amount of incoming solar radiation.For 1.0 m 2 solar panel at the geosynchronous orbit of Earth, the maximum power gained is about 594 W. The amount of current flows in a series connected subcells in Earth's geosynchronous orbit is 24.8 mA.A comparable result of I SC is also found in GainAsP/InGaAs MJSC as a consequence of current-limiting behavior of subcell as shown by its non-zero slope of I-V curve near the short-circuit current [61].The open circuit voltage V OC in the first subcell is bigger than in the second subcell and the third subcell.The V OC of the second subcell and the third subcell are only 68.59% and 16.14% of V OC of the first subcell respectively.The gradation of V OC in the Earth's geosynchronous orbit is similar to Venus's geosynchronous orbit condition since those voltages are related to the amount of electric power produced by each subcell.The I-V diagram of Al 0.3 Ga 0.7 As/InP/Ge TJSC is shown in Figure 5.

Conclusions
We have ideally simulated the performance of Al0.3Ga0.7As/InP/Getriple-junction solar cells for an application in a hypothetical International Venus Orbiter Space Station (IVOSS).Although the simulation parameters here are ideal compared to experimentally achievable results, we find that Al0.3Ga0.7As/InP/GeTJSC could reach 38.94% power efficiency and can produce 2.92 MW of electricity to power this space station (assuming a 2500 m 2 of solar panel area).As a comparison, we also showed that the same TJSC (with the same parameter simulation) applied to a space station at the geosynchronous orbit of Earth only produces 1.48 MW of electric power.The vast amount of electricity produced by Al0.3Ga0.7As/InP/GeTJSC in Venus geosynchronous orbit condition opens up an opportunity to conduct long-term and intensive research on Venus in the future.

Conclusions
We have ideally simulated the performance of Al 0.3 Ga 0.7 As/InP/Ge triple-junction solar cells for an application in a hypothetical International Venus Orbiter Space Station (IVOSS).Although the simulation parameters here are ideal compared to experimentally achievable results, we find that Al 0.3 Ga 0.7 As/InP/Ge TJSC could reach 38.94% power efficiency and can produce 2.92 MW of electricity to power this space station (assuming a 2500 m 2 of solar panel area).As a comparison, we also showed that the same TJSC (with the same parameter simulation) applied to a space station at the geosynchronous orbit of Earth only produces 1.48 MW of electric power.The vast amount of electricity produced by Al 0.3 Ga 0.7 As/InP/Ge TJSC in Venus geosynchronous orbit condition opens up an opportunity to conduct long-term and intensive research on Venus in the future.

Figure 1 .
Figure 1.The schematic of distances of the geosynchronous orbit of Venus.

Figure 1 .
Figure 1.The schematic of distances of the geosynchronous orbit of Venus.

Figure 2 .
Figure 2. The schematic picture of power density (intensity) averaging technique.(All units in arbitrary).

Figure 2 .
Figure 2. The schematic picture of power density (intensity) averaging technique.(All units in arbitrary).

Figure 3 .
Figure 3.The incoming spectral irradiance at the geosynchronous orbit of Venus and Earth calculated using a blackbody radiation formula.The total power density (intensity) at the geosynchronous orbit of Venus is 3000 W/m 2 , while for Earth it is 1557 W/m 2 .

Figure 4 .
Figure 4.The electrical performance (I-V diagram) of Al0.3Ga0.7As/InP/GeTJSC at the geosynchronous orbit of Venus.All subcells were connected in a series connection and possess the same current.

Figure 4 . 46 8 of 12 3. 3 .
Figure 4.The electrical performance (I-V diagram) of Al 0.3 Ga 0.7 As/InP/Ge TJSC at the geosynchronous orbit of Venus.All subcells were connected in a series connection and possess the same current.

Figure 5 .
Figure 5.The electrical performance of Al0.3Ga0.7As/InP/GeTJSC at geosynchronous of Earth.All subcells were connected in a series and possess the same current.

Figure 5 .
Figure 5.The electrical performance of Al 0.3 Ga 0.7 As/InP/Ge TJSC at geosynchronous of Earth.All subcells were connected in a series and possess the same current.

Table 1 .
Input parameter for PC1D program.

Table 1 .
Input parameter for PC1D program.

Table 2 .
Simulation results of TJSC at the geosynchronous orbit of Venus.

Table 2 .
Simulation results of TJSC at the geosynchronous orbit of Venus.

Table 3 .
Simulation results of TJSC at the geosynchronous orbit of Earth.