Geoffrey A. Landis and Joseph Appelbaum
NASA Glenn Research Center 21000 Brookpark Rd., Cleveland, OH
44135published in Space Power, Volume 10 Number 2, pp
225-237 (1991).
Summary
Mars exploration will require power systems to operate on the Martian
surface. One power system is a photovoltaic array. The properties of Mars
relevant to photovoltaic array performance are surveyed. Several types of solar
cells usable in a photovoltaic array are detailed and analyzed, and possible
applications on Mars discussed. The applicability of photovoltaic technology to
manufacturing methane propellant from Mars carbon dioxide is analyzed.
Introduction
Mars is a challenging environment for the use of solar power. In addition to
the lower sunlight intensity compared to Earth orbital applications, the
twelve-hour night (although not as severe as the moon`s 14 day darkness)
requires that any solar power system include a large storage system. Wind, low
temperature, sand, dust, and corrosive peroxide-rich soil, make the Martian
surface an environment one could hardly call benign.
For any manned mission, a significant priority for a power system will be
reliability and absence of dangerous failure modes. Due to the high price of
transporting materials to Mars, an additional priority for a surface power
system will be low weight. Photovoltaics provides low-cost power with high
reliability and no moving parts. It has powered the space program since
Vanguard, and there is every reason to believe it will play a major role in the
coming exploration of Mars.
Sunlight on Mars
The solar intensity on the surface of Mars is considerably lower than that
available in Earth orbit. This is primarily due to the greater distance of Mars
from the sun. The average solar intensity at the orbit of Mars is 590 W/m2,
compared with 1370 W/m2 in Earth orbit. The eccentricity of Mars` orbit results
in a variation in intensity of about ±19% over the course of a year. Scattering
and absorption of light by dust in the Martian atmosphere also decreases the
sunlight available.
The availability of sunlight on Mars has been reviewed elsewhere [1,2,3] and
will be only briefly discussed here.
Figure 1: the Surface of Mars. A view of the
Martian surface from the Viking lander. Of particular interest is the light
color of the sky, indicating the presence of light scattered from atmospheric
dust.
As can be seen in figure 1, the sky of Mars has considerable dust content,
which scatters the incident sunlight. This dust content varies considerably,
depending on the dust storms. When the dust levels are high (typically near
perihelion; around the northern hemisphere winter [4]) the optical depth of the
atmosphere can be much greater than one [1]. At these times very little direct
sunlight reaches the Martian surface, and nearly all of the light reaching the
surface is diffuse scattering from the atmospheric dust. Despite the low amounts
of direct insolation, however, the total light reaching the surface is
appreciable. Figure 2 (from reference 1) shows the total sunlight availability
(integrated over a day) for a horizontally oriented surface, showing the
variation during the year. [Note that the time of year is expressed in units of
areocentric longitude, the position of Mars in orbit around the sun in degrees].
season (areocentric longitude in degrees). Figure 2:
Sunlight on Mars. The global insolation (total of direct and scattered
light) in kW-hr per square meter per day received on a horizontal surface at the
two Viking lander sites VL-1 and VL-2 over the course of a Martian year.
Like Earth, Mars has seasons due to its axial tilt. For locations off the
equator, the number of hours of sunlight varies during the year. This has a
considerable effect on the design of solar systems, particularly if they are to
be designed for worst-case conditions, winter months far north or south of the
equator. Figure 3 shows the number of hours of sunlight as a function of the
time of year ("areocentric longitude") at various locations north of the
equator. Above the Martian arctic and antarctic circles, Mars (like Earth) has
no sunlight at all during the winter, and continuous sunlight during the
summer.
Equator to 40 N
40 N to 80 N
Figure 3: Daylight Hours. Length of
daylight in the northern hemisphere of Mars as a function of latitude and time
of year (areocentric longitude). Top: equator to 40 degrees N; bottom: 40-80
degrees N. Daylight hours in the southern hemisphere the same, but with the
seasons exactly reversed.
Solar Cells
There are three approaches to photovoltaic power. The conventional approach
is the use of deployable high-efficiency flat plate arrays. Existing solar
arrays used in space use either crystalline silicon (Si) or gallium arsenide
(GaAs) solar cells.
Silicon is the most well developed solar cell technology, and has been used
on all but a tiny fraction of space solar arrays. The conversion efficiency of
standard-technology silicon cells currently flown is about 14.5% under standard
space conditions ("Air Mass Zero," or "AM0") [5]. Note that for calculating
operational power, the cell efficiency numbers must be adjusted for the array
packing factor and for corrections to efficiency due to intensity and
temperature.
Silicon solar cells with up to 20% conversion efficiency have been
demonstrated in the laboratory. These cells are not yet space qualified and not
currently available on the market.
Advantages of silicon cells are that large area cells are available (8 by 8
cm cells are being manufactured for Space Station Freedom), the array
manufacturing technology is well developed, and the technology is well
characterized for vibration, thermal-cycling, and other environmental loads of
the space environment.
GaAs cells have higher efficiency than silicon cells. GaAs cells currently
available on the market have an average conversion efficiency of 18.5%.
Efficiency of 21.5% has been achieved in the laboratory. Gallium arsenide cells
are smaller and more brittle than silicon cells, but the technology is being
rapidly developed.
Gallium arsenide cells are currently heavier than silicon cells. Several
technologies under development will make GaAs cells much lighter in weight [5].
The most well-developed of these technologies is CLEFT [6], where an extremely
thin (5 micron) large-area cell is separated from a single-crystal
substrate.
An important measure of power system performance is the specific power (power
output per unit mass). Note that this is typically specified for Earth orbit
conditions. Operation at the Mars surface will decrease the specific power by
the ratio of Mars sun intensity to Earth orbit intensity.
Note that it is possible to measure specific power at the cell level, at the
blanket level, at the array level, or at the power system level. Specific power
at the cell level does not include array structure and is many times higher than
array level specific power. At the blanket level, specific power includes the
coverglass, interconnections, and the backing material, but not the array
structure. This may be an appropriate figure of merit if a flexible or
semi-flexible array is to be simply unrolled horizontally onto the Mars surface
without support structure.
Specific power at the photovoltaic array level (including array structure)
for the best arrays developed to date are shown in table 1.
For currently designed space power systems, the photovoltaic blanket weight
is only about a quarter of the total power generation system mass (excluding
storage). This is shown in table 2 for the space station Freedom solar array.
The array structure and the power management and distribution (PMAD) system
account for three-quarters of the power system mass. This provides a powerful
incentive to develop new and more efficient PMAD systems and to design new array
structures to take advantage of the ultralight blankets.
The second approach to photovoltaic arrays is to use a thin layer of
photovoltaic material deposited onto a flexible substrate [7]. In the 1980`s
considerable research was devoted to development and commercialization of
thin-film photovoltaics for terrestrial power generation. Thin-film solar cells
consist of thin (~1-5 µm) films of photovoltaic material deposited on a
supporting substrate. This approach has lower conversion efficiencies, but due
to the low amount of the active material used, has the potential for high
specific power.
Efficiencies over ten percent have been achieved with three thin-film
materials: amorphous silicon (a-Si), copper indium diselenide
(CuInSe2), and cadmium telluride (CdTe). However, very little
current research is aimed at depositing thin-film cells on lightweight
substrates, since most of the applications being considered are terrestrial,
where weight is not as critical. To enable their use in space, technology for
deposition on extremely lightweight substrates will need to be developed. Thin
film solar cells have not yet been demonstrated in space.
A conservative projection of an achievable thin-film solar cell blanket
usable for space would be a 5% efficient thin-film cell fabricated on a 25
micron thick Kapton substrate. This yields a photovoltaic blanket specific power
of 1.7 kW/kg. An optimistic projection might be a 15% thin-film cell on a 7
micron thick Kapton substrate, leading to a photovoltaic blanket specific power
of 15 kW/kg. These numbers compare favorably to current state of the art
spacecraft solar blankets.
Thin-film cells have other desirable features for space applications. In
addition to low mass, thin-film photovoltaics are also projected to have
considerably lower costs. Materials cost is reduced due to the small amount of
materials required; the cost of labor and assembly is reduced by the fact that
large-area, integrated assemblies are produced directly on the substrate sheet.
A final photovoltaic alternative is to use a concentrator system to focus
light onto small, extremely high efficiency solar cells. This approach has been
tested in space only on small-scale experiments. While conversion efficiencies
of over 30% have been demonstrated using such concentrator systems and
high-efficiency tandem solar cells, concentrator systems will not be practical
for Mars surface power. The difficulty is that concentrator systems can focus
only the direct ("beam") component of the light, and not the diffuse. Since a
baseline power system must be sized to operate under worst-case conditions,
where most of the incident sunlight is diffuse, concentrator systems can be
ruled out.
Some resource-utilization applications require high-temperature processing.
For these applications it may be desirable to concentrate sun to high
intensities using mirrors or lens concentrators. This will allow a system to use
the sunlight directly as heat, rather than converting the sunlight first into
electricity using solar cells. A concentration system can make use of only the
light coming directly from the sun (the direct, or "beam" component of the
insolation). As discussed in previous work [1-3], the direct component of the
insolation is about 50% of the total sunlight during the (northern hemisphere)
spring and summer, but can drop to 10% or less of the total available light
during periods of highly dust-laden air, particularly during the period around
perihelion (northern hemisphere winter), when global dust storms can occur. An
application requiring a concentrator to produce process heat must thus be
designed for operation during relatively clear periods only. This implies that
the mission be scheduled to avoid perihelion, and that the processing system
must be tolerant of the possibility of intermittent shut-down if dusty
atmospheric conditions arise.
A concentrator system will also have to be tolerant of dust loading of the
mirror or lens surfaces.
Environment
In addition to the solar insolation and the fraction of direct and diffuse
sunlight, other environmental factors of importance to photovoltaic system
operation on the Mars surface are the temperature and the wind.
The Martian surface temperature varies from a minimum of 130¡ K to as high as
300¡ K, with a mean of 215¡ K. Air temperatures were measured by Viking at a
height of 1.6 meters above the surface over a (Martian) year of measurement,
including both local and global dust storms. Peak daytime temperatures varied
from about 170¡ K at the Viking-2 site during a global storm, to almost 250¡ K
near the summer solstice [2].
Photovoltaic cell performance increases with decreasing temperatures, with
peak efficiency occurring at 150-200¡ K; at lower temperatures the efficiency
decreases. The temperature coefficient of efficiency depends on the material,
and in general increases as the material bandgap decreases [8]. Thus, low
bandgap materials such as silicon and CuInSe2, which have high coefficients,
increase in performance rapidly at the low temperatures to be found at Mars.
Wind was measured by the Viking landers. Average wind speed at site VL-2 was
about 2 m/sec [4], with winds of over 17 m/sec observed less than 1% of the
time. The atmospheric density varies considerably with season and temperature;
at typical atmospheric conditions, dynamic pressure at the maximum likely wind
velocity of 30 m/sec will be 10 nt/m2. This is a small pressure loading by
terrestrial standards, however, Martian solar arrays will have to be somewhat
more robust than arrays for the moon or deep space.
A final aspect of the Mars environment not well characterized is the soil.
One interpretation of the Viking lander life science experiments is that the
Martian soil contains large amounts of peroxides and superoxides [4]. This
hypothesis needs to be confirmed by direct chemical analysis of the soil. If it
is confirmed, it will be important that solar arrays be built using materials
not subject to attack by oxidants.
Missions
The first use of power systems will be to run the unmanned rovers and
scouting missions needed to investigate the geology (or `areology`) of Mars and
scout out a location for the manned Mars base. Such a vehicle will not require
much energy storage for the night, since it will not typically be operated in
darkness. At dusk, the rover points its solar arrays at the eastern horizon and
"goes to sleep," waking up again when the sun rises high enough to power the
vehicle.
Under contract to NASA, B.D. Hibbs has done a design study on a small Mars
rover with a high-efficiency photovoltaic array mounted to the body of the
vehicle [9]. While the total power is decreased by using a fixed array rather
than one which tracks the sun, this is more than made up for by the added
robustness of the array. Depending on the technology chosen, the array required
can be as small as seven square meters. Power requirements can be quite
modest--only 275 watts average power (less than a moderate-size toaster), with a
night-time `sleep` requirement of only 100 watts. Peak power capability of up to
2000 watts are required, though, for difficult tasks such as climbing over large
boulders.
Figure 4 shows another approach to a rover design, where larger arrays are
designed to be retractable during high-wind periods or when the rover is
moving.
Figure 4: Mars Rover. A Mars rover with a
deployable solar array (artist`s conception by Les Bossinas of NASA Glenn).
(Click picture to view a 1.1MB JPEG file of this image)
An alternative approach to investigating large areas of the Mars surface, and
particularly for scouting for long distances and over rough--but
interesting--terrain, is to use an airborne rover. A solar-powered airplane
designed for Mars by Tony Colozza at NASA Glenn Research Center [10], shown in
figure 5, is designed to be deployed directly into the air and fly continuously,
night and day. Unlike the rover, the airplane must have continuous power over
the night. Solar panels on the wing, tail, and fuselage charge regenerative fuel
cells to allow the plane to stay in the air under cruise power for night flight.
With a design criterion of 100 kg of payload and assuming a 25% efficient solar
panel, the aircraft had a total mass of 438 kg and a wingspan of 120 meters.
Figure 5: Photovoltaic
powered Mars airplane. An unmanned airplane may be more able to scout
over long distances and rough terrain than a ground rover (artist`s conception
by Les Bossinas of NASA Glenn).
For manned missions, two applications are power for life support and
operations and power for resource processing (i.e., propellant manufacture).
Once on the surface, the first priority will be to provide power. An example
power system is discussed by McKissock, Kohout and Schmitz [11]. Their power
cycle was to provide 40kW continuous power during the day, and a reduced power
level of 20 kW during the night. For the night storage capability, they assumed
that the hydrogen/oxygen regenerative fuel cell (RFC) has been developed to
technology readiness. The RFC assumed pressurized gas storage. Cryogenic storage
of reactants was determined to require too much equipment overhead to justify
the slight advantages in storage volume. Round-trip efficiency for the storage
system was 61.5%.
The power system is shown in figure 6. The flexible array is visible deployed
on the ground behind the lander, while the regenerative fuel cell unit, with
spherical pressure tanks for the hydrogen, oxygen, and water reactants, is
visible in the foreground. A roll-out thermal radiator provides thermal
management for the system.
Figure 6.
Photovoltaic power system for a manned Mars mission. In foreground is
the regenerative fuel cell system to provide night power, while the roll-out
solar array is visible on the ground behind the lander (artist`s conception by
Les Bossinas of NASA Glenn). For more information, see "A Solar Power System for an
Early Mars Expedition", NASA TM 103219.
Sample Case: PV Blanket for the "Mars Direct" Scenario Power
In-situ propellant generation on Mars is an option for drastically reducing
the cost of Mars expeditions, which could be used for both manned missions and
for unmanned precursor missions. One scenario for propellant generation on Mars
(proposed by Robert Zubrin and David Baker [12,13]) is Mars Direct, which proposes to generate 107 tons of methane/oxygen
propellant from 5.7 tons of hydrogen brought from Earth plus CO2 from the
Martian atmosphere.
The following analysis shows how the energy requirements for this processing
could be met with a surface photovoltaic array.
The process sequences is:
4 H2 + CO2 --> 2 H2O +
CH4 (Sabatier reaction) (1)
2 H2O --> 2 H2 + O2
(electrolysis) (2)
The hydrogen is then recycled to produce additional methane. Additional
oxygen is produced by thermal decomposition of carbon dioxide [12] or by
pyrolysis of methane back to hydrogen and carbon followed by reactions (1) and
(2) repeated [13].
The baseline Zubrin/Baker scenario requires a 100 kW reactor running for 24
hr/day for 155 days for the propellant production. The energy required for
manufacturing 107 tons of propellant on Mars is 370 MW-hrs of electrical energy.
For the solar-powered case, it is desired to produce the required amount of
propellant in half a Mars year, chosen to avoid the global dust storm
season.
The baseline case studied used the following parameters:
- site = Viking 1 lander site
- propellant production completed in half a Mars year
- season = northern hemisphere summer and spring
- insolation available = 3 kW-hr/m2 per day
- fixed array (no tracking)
- solar array mass = 0.9 kg/m2 (APSA array technology)
- solar array efficiency = 20% under Mars conditions
- storage system: none (propellant production during day only)
The solar cell efficiency of 20% is about the efficiency of currently
available GaAs cells operating at the temperatures expected at Mars. The solar
array specific mass of 0.9 kg/m2 is roughly the target mass of a high-efficiency
solar array designed for GEO [5]. Mars arrays will have a different mass, since
the structure will be different from GEO, but in the absence of an array
designed for Mars, this will serve as an order of magnitude estimate.
The global insolation on a horizontal (non-tracking) surface averages
slightly over 3 kW-hr/m2 per day. Running the system for half a Mars year
results in a total insolation of 1000 kW-hr/m2. No mass allocation for energy
storage is assumed.
The solar array area required for propellant processing is 1850 m2,
equivalent to an array 43 meters square. The PV blanket mass is 1.67 metric
tons, which excludes the structure to hold the array in place, the mass of a
robot or remotely-operated unit to deploy the array, and the mass of power
conditioning, management and distribution equipment (PMAD). If the PMAD and
ancillary equipment weight equals the PV blanket weight, the total required mass
will be 3.33 metric tons.
This is comparable to the baseline power system considered by Zubrin and
Baker, which used a 100 kW nuclear reactor and had a total mass of 3.96 metric
tons.
Conclusions
Solar cells provide one option for providing power on the surface of Mars,
both for unmanned precursor missions and for a manned base. Several types of
photovoltaic technologies are available. Analyses of the applicability of solar
power to Mars shows that photovoltaic power should be feasible, however, many
questions remain to be answered, and development work on the solar cells, the
array technology, and the technology for providing electrical storage for night
operation, will need to be done.
References
A more extensive compilation of references can be found in the Mars
Solar Energy Bibliography
1. J. Appelbaum and G.A. Landis, "Solar Radiation for Mars Power Systems,"
European Space Power Conference, 2-6 Sept. 1991, Florence, Italy; proceedings
published as volume ESA SP-320.
2. G.A. Landis and J. Appelbaum, "Design Considerations for Mars PV Power
Systems," 21st IEEE Photovoltaic Specialists Conf., May 1990, Vol. 2,
1263-1270.
3. J. Appelbaum and D. Flood, "Solar Radiation on Mars," Solar Energy Vol. 45
No. 6, 353-363 (1990). Also available as NASA Technical Memorandum 102299
(1989).
4. D. Kaplan, Environment of Mars 1988, NASA Technical Memorandum 100470
(1988).
5. P.M. Stella and D.J. Flood, "Photovoltaic Options for Solar Electric
Propulsion," NASA Technical Memorandum 103284 (1990).
6. J.C.C. Fan, C.O. Bozler and R.W. McClelland, "Thin Film Gallium Arsenide
Solar Cells," Proc. 15th IEEE Photovoltaic Specialists Conf., 666-672
(1981).
7. G.A. Landis and A.F. Hepp, "Thin-Film Photovoltaics: Status and
Applications to Space Power," European Space Power Conference, 2-6 Sept. 1991,
Florence, Italy; proceedings published as volume ESA SP-320. An earlier version
of this paper is published in Space Power, Vol. 8, No. 1-2, 31-50 (1989).
8. I. Weinberg, C.K. Swartz, and R.E. Hart, "Radiation and Temperature
Effects in Gallium Arsenide, Indium Phosphide, and Silicon Solar Cells," NASA
Technical Memorandum 89870 (1989).
9. B.D. Hibbs, "Mars Rover Feasability Study, Final Report," AeroVironment,
Inc., Report AV-FR-89/7011 (Oct. 1989).
10. A.J. Colozza, "Preliminary Design of
a Long-Endurance Mars Aircraft", NASA Contractor Report 185243 (AIAA
90-2000), April 1990.
11. B. I. McKissock, L.L. Kohout and P.C. Schmitz, "A Solar Power System
for an Early Mars Expedition", NASA Technical Memorandum 103219, , American
Institute of Chemical Engineers Summer National Meeting, August 19-23, 1990.
12. D. Baker and R.M. Zubrin, "Mars
Direct: Combining Near-Term Technologies to Achieve a Two-launch Manned Mars
Mission," J. Brit. Interplanetary Soc. Vol. 43, 519-523 (1990).
13. R.M. Zubrin, D.A. Baker, and O. Gwynne, "Mars Direct: A Simple, Robust,
and Cost Effective Architecture for the Space Exploration Initiative," AIAA
Paper 91-0326 (1991).
Table 1: Specific Power of Solar Arrays (Earth Orbit Solar
Intensity) Best Flight Tested Array: Solar Array Flight Experiment
(SAFE)
Best Currently Built Array: Advanced Photovoltaic Solar Array (APSA)
Best Array Combining Existing Technology: APSA with 20% CLEFT GaAs cells
Table 2. Space Station Freedom Photovoltaic Power System Mass Breakdown per module
(28 kW power produced; 18.75 kW av.
user power)
Element |
Mass
(kg) |
Fraction
(%) |
PV Blanket |
890 |
24.0 |
mast |
330 |
8.8 |
gimbal |
540 |
14.5 |
electrical equip. |
610 |
16.6 |
thermal control |
730 |
19.6 |
misc. integration |
610 |
16.5 |
total |
3710 |
100 |
not including:
Element |
Mass
(kg) |
|
Batteries: |
1300 |
|
Charge/disc. unit |
290 |
|
Array is a quarter of system mass; array plus structure
is half of system mass.
Page by Geoffrey A. Landis October 1996
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