Atmospheric Mining in the Outer Solar System: Resource Capturing, Exploration, and Exploitation
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Atmospheric Mining in the Outer Solar System: Mining Design Issues and Considerations,” AIAA 2009- 4961, August 2009
Atmospheric Mining in the Outer Solar System: Resource Capturing, Storage, and Utilization Bryan Palaszewski* NASA John H. Glenn Research Center Lewis Field MS 5-10 Cleveland, OH 44135 (216) 977-7493 Voice (216) 433-5802 FAX [email protected] Fuels and Space Propellants Web Site: http://www.grc.nasa.gov/WWW/Fuels-And-Space-Propellants/foctopsb.htm Abstract Atmospheric mining in the outer solar system has been investigated as a means of fuel production for high energy propulsion and power. Fusion fuels such as Helium 3 (3He) and hydrogen can be wrested from the atmospheres of Uranus and Neptune and either returned to Earth or used in-situ for energy production. Helium 3 and hydrogen (deuterium, etc.) were the primary gases of interest with hydrogen being the primary propellant for nuclear thermal solid core and gas core rocket-based atmospheric flight. A series of analyses were undertaken to investigate resource capturing aspects of atmospheric mining in the outer solar system. This included the gas capturing rate for hydrogen helium 4 and helium 3, storage options, and different methods of direct use of the captured gases. Additional supporting analyses were conducted to illuminate vehicle sizing and orbital transportation issues. Nomenclature 3He Helium 3 4He Helium (or Helium 4) AMOSS Atmospheric mining in the outer solar system CC Closed cycle delta-V Change in velocity (km/s) GCR Gas core rocket GTOW Gross Takeoff Weight H2 Hydrogen He Helium 4 IEC Inertial-Electrostatic Confinement (related to nuclear fusion) ISRU In Situ Resource Utilization Isp Specific Impulse (s) K Kelvin kWe Kilowatts of electric power LEO Low Earth Orbit MT Metric tons MWe Megawatt electric (power level) NEP Nuclear Electric Propulsion NTP Nuclear Thermal Propulsion NTR Nuclear Thermal Rocket OC Open cycle O2 Oxygen PPB Parts per billion STO Surface to Orbit ________________________________________________________________________ * Leader of Advanced Fuels, AIAA Associate Fellow I. -
The Mystery and Majesty
The mystery and majesty Nearly 40 years after THE SPACE AGE BLASTED off when the Soviet Union launched the Voyager 2 visited Uranus world’s first artificial satellite in 1957. Since then, humanity has explored our cosmic and Neptune, scientists are backyard with vigor — and yet two planets have fallen to the planetary probe wayside. eager for new expeditions. In the 63 years since Sputnik, humanity has only visited Neptune and Uranus once BY JOEL DAVIS — when Voyager 2 flew past Uranus in January 1986 and Neptune in August 1989 40 ASTRONOMY • DECEMBER 2020 of the ICE GIANTS — and even that wasn’t entirely pre- interstellar mission, more than a dozen pro- In 1781, Uranus became the first planet planned. The unmitigated success of posals have been offered for return missions ever discovered using a telescope. Nearly 200 years later, Voyager 2 Voyager 1 and 2 on their original mission to one or both ice giants. So far, none have became the first spacecraft to visit to explore Jupiter and Saturn earned the made it past the proposal stage due to lack Uranus and Neptune, in 1986 and 1989 respectively. NASA/JPL twin spacecrafts further missions in our of substantial scientific interest. Effectively, solar system and beyond, with Neptune and the planetary research community has been Uranus acting as the last stops on a Grand giving the ice giants the cold shoulder. Tour of the outer solar system. But recently, exoplanet data began In the 31 years since Voyager 2 left the revealing the abundance of icy exoplanets Neptune system in 1989 and began its in our galaxy “and new questions about WWW.ASTRONOMY.COM 41 With a rotation axis tilted more than 90 degrees compared to its orbital plane, Neptune likewise has a highly tilted rotation axis and tilted magnetic axis. -
Neptune 1 Neptunian Day = 16.1 Earth Hours
1 Neptunian day = 16.1 Earth hours When the Voyager 2 spacecraft flew past Neptune 1 Neptunian year = 165 Earth years Neptune in 1989, two dark spots were visible in Neptune's atmosphere. The Neptune is the outermost smaller one (left, below center) was a ice giant planet in our solar system. storm, but the Great Dark Spot (far left) Small amounts of methane in its was just a gap in Neptune's methane atmosphere lend it a deep blue colour. cloud deck. The Great Dark Spot had Neptune was discovered because its vanished by the time the Hubble Space gravity slightly alters the orbit of Uranus. Telescope viewed Neptune in 1994, but Observing Uranus’ orbit after its a new dark spot had appeared in the discovery enabled astronomers to opposite hemisphere. predict the existence and location of a previously unknown planet. That planet, Neptune, was discovered on September 23, 1846. Neptune and Triton (seen as crescents above) are shown below with their correct sizes and separation relative to the Sun in this scale model. Neptune's largest moon, Triton, is shown above. Triton orbits Neptune opposite to the direction Neptune spins. The tidal bulges Triton raises on Neptune pull backwards on Triton, pulling Triton a tiny distance closer to Neptune with every orbit. Eventually Triton will either crash into Neptune or be torn apart and form bright rings around Neptune like those around Saturn. Above, cirrus-type clouds on Neptune cast All images (Neptune does have a few rings already. They are much narrower and darker from NASA’s shadows on deeper cloud layers. -
Flight in the Jovian Stratosphere. Engine Concept and Flight Altitude
Flight in the Jovian Stratosphere – Engine Concept and Flight Altitude Determination Nedislav S. Veselinov,1 Martin N. Karanikolov, 1 Vladislav V. Shihskin1, Dimitar M. Mladenov2 Sofia University “St. Kliment Ohridski”, Sofia, Bulgaria An effective method for detailed observation of the Solar System planets is the use of vehicles that can perform flight in their atmospheres, with the most promising of them being Flyers (aircraft for other planets atmospheres). Besides the advantage of probing the atmosphere directly, they have the ability to fly on selected direction and altitude, making them suitable for collecting information over large areas. Equipping the Flyer with nuclear propulsion will allow it to conduct flight for months without the need of combustible fuel or oxidizer to be carried on board. Among the planets of the Solar System and their satellites, Jupiter is a viable target for exploration, since it features thick atmosphere suitable for aerodynamic flight, there is no solid surface that can be contaminated after end of the mission, and the atmospheric data for designing a Flyer is readily available. This paper proposes a mathematical model for evaluating the thrust, the lift and the maximum allowable mass for horizontal steady flight as functions of the altitude and different heat chamber temperatures. I. Introduction F ROM the beginning of the space era, over thirty probes have been sent into the atmosphere or landed on the surface of the other planets in the Solar System. However, most of them lacked the capability for sustained flight. The only vehicles that successfully reached and conducted continuous flight in the atmosphere of a planet other than the Earth were the Vega-1 and Vega-2 balloons in 1985. -
Our Solar System Lithograph
National Aeronautics and and Space Space Administration Administration OURSOLARSYSTEM 2013 www.nasa.gov Inside Educational Product Our Solar System Earth Meteors and Meteorites Saturn Pluto and Charon Educators Grades K–12+ LS-2013-07-003-HQ Our Star — The Sun Earth’s Moon Moons of the Solar System Moons of Saturn Comets JPL 400-1489 07/13 Mercury Mars Jupiter Uranus Kuiper Belt and Oort Cloud Venus Asteroids Galilean Moons of Jupiter Neptune What Is a Planet? NASA EDUCATIONAL RESOURCES Educator Resource Center Network (ERCN) The EarthSpace portal (www.lpi.usra.edu/earthspace) is a national clearinghouse for higher information space and Earth The NASA portal (www.nasa.gov) is the gateway for information NASA’s Educator Resource Center (ERC) network helps edu- sciences, with resources for undergraduate education in plan- about content, programs, and services offered for the general cators learn about NASA educational resources and provides etary science and solar and space physics. public and the education community. NASA’s goal is to improve NASA materials. interactions for students, educators, and families with NASA Regional Educator Resource Centers offer access to NASA edu- NASA multimedia (www.nasa.gov) features International Space and its education resources. cational materials for educators. NASA has formed partnerships Station coverage, live special events, interactive educational live shows, electronic field trips, aviation and space news, and NASA’s education home page (www.nasa.gov; click on “For with universities, museums, and other educational institutions to historical NASA footage. Links to a variety of NASA resources Educators”) serves as the portal for information about edu- serve as Regional ERCs in many states. -
YEAR in REVIEW 2011 a PUBLICATION of the AMERICAN INSTITUTE of AERONAUTICS and ASTRONAUTICS Change Your Perception of MESHING
cover-fin12-2011_AA Template 11/18/11 11:37 AM Page 1 11 AMERICA AEROSPACE December 2011 DECEMBER 2011 YEAR IN REVIEW 2011 A PUBLICATION OF THE AMERICAN INSTITUTE OF AERONAUTICS AND ASTRONAUTICS change your perception of MESHING VISIT US AT THE AIAA AEROSPACE SCIENCES MEETING 9-12 JANUARY 2012 > THIS IS NOT THE FUNNEST PART OF THE PROJECT. You’re not generating a computational grid for pleasure. It’s simply a necessary step in the process of completing your analysis, so you can improve the performance of your design. With its intuitive interface, high-level automation, and sophisticated grid generation algorithms, Pointwise helps ease you through the process. Try it for free, and see how Pointwise can reduce your meshing pain. POINTWISE. Reliable People, Reliable Tools, Reliable CFD Meshing. Toll Free (800) 4PTWISE www.pointwise.com toc.DEC2011a_AA Template 11/17/11 10:46 AM Page 1 December 2011 EDITORIAL 3 OUT OF THE PAST 76 2011 SUBJECT AND AUTHOR INDEX 78 CAREER OPPORTUNITIES 84 THE YEAR IN REVIEW Adaptive structures 4 Intelligent systems 39 Aeroacoustics 12 Legal aspects 32 Aerodynamic decelerators 25 Life sciences 56 Aerodynamic measurement Lighter-than-air systems 30 technology 13 Liquid propulsion 51 Aerospace power systems 44 Materials 6 Aerospace traffic management 68 Meshing, visualization and Air-breathing propulsion systems computational environments 21 integration 45 Nondeterministic approaches 7 Aircraft design 26 Nuclear and future flight Air transportation 24 propulsion 52 Applied aerodynamics 14 Plasmadynamics and lasers -
Tessmann Planetarium Guide to the Solar System
TESSMANN PLANETARIUM GUIDE TO THE SOLAR SYSTEM Solar System The Sun and Inner Planets The Sun makes up about 99.8% of the mass in the solar system. This means that almost the entire mass of the solar system is in the Sun. SUN FACTS Diameter: 864,000 miles across (109 times the Earth’s diameter) Surface Temperature: 9980° Fahrenheit (F) Core Temperature: 27,000,000° F Duration of Rotation (Solar day): 27 to 31 days Composition: Made up mostly of hydrogen (70%) and helium (28%) and other (2%) Important spacecrafts: Solar Dynamics Observatory (SDO), Solar and Heliospheric Observatory, Solar Terrestrial Relations Observatory (STEREO), and many others. Also known as: Sol The Sun 2 The Sun is the center of our solar system; all the planets in our The Sun is a Yellow Dwarf Star system orbit around the Sun near the Earth’s orbital plane. 1,200,000 Earths can fit into the Sun. The Sun outshines about 80% of the stars in the Milky Way. However, there are many stars that are much bigger and brighter than our Sun. Our Sun is a mere runt compared to the biggest of these. The Sun is a G type star and takes about 225 million years to make one orbit around the Milky Way. It is known as a yellow dwarf, although its color is actually more white than yellow. It generates energy through nuclear fusion in its core. The Sun is located in the Orion arm of the Milky Way. Sunspots are areas of strong magnetic activity and lower tem- perature on the surface of the Sun. -
Solar System Exploration Augmented by In-Situ Resource Utilization: Human Mercury and Saturn Exploration
NASA/TM—2020-220308 AIAA–2015–1654 Solar System Exploration Augmented by In-Situ Resource Utilization: Human Mercury and Saturn Exploration Bryan A. Palaszewski Glenn Research Center, Cleveland, Ohio May 2020 NASA STI Program . in Profi le Since its founding, NASA has been dedicated • CONTRACTOR REPORT. Scientifi c and to the advancement of aeronautics and space science. technical fi ndings by NASA-sponsored The NASA Scientifi c and Technical Information (STI) contractors and grantees. Program plays a key part in helping NASA maintain this important role. • CONFERENCE PUBLICATION. Collected papers from scientifi c and technical conferences, symposia, seminars, or other The NASA STI Program operates under the auspices meetings sponsored or co-sponsored by NASA. of the Agency Chief Information Offi cer. It collects, organizes, provides for archiving, and disseminates • SPECIAL PUBLICATION. Scientifi c, NASA’s STI. The NASA STI Program provides access technical, or historical information from to the NASA Technical Report Server—Registered NASA programs, projects, and missions, often (NTRS Reg) and NASA Technical Report Server— concerned with subjects having substantial Public (NTRS) thus providing one of the largest public interest. collections of aeronautical and space science STI in the world. Results are published in both non-NASA • TECHNICAL TRANSLATION. English- channels and by NASA in the NASA STI Report language translations of foreign scientifi c and Series, which includes the following report types: technical material pertinent to NASA’s mission. • TECHNICAL PUBLICATION. Reports of For more information about the NASA STI completed research or a major signifi cant phase program, see the following: of research that present the results of NASA programs and include extensive data or theoretical • Access the NASA STI program home page at analysis. -
Space Theme Circle Time Ideas
Space Crescent Black Space: Sub-themes Week 1: Black/Crescent EVERYWHERE! Introduction to the Milky Way/Parts of the Solar System(8 Planets, 1 dwarf planet and sun) Week 2: Continue with Planets Sun and Moon Week 3: Comets/asteroids/meteors/stars Week 4: Space travel/Exploration/Astronaut Week 5: Review Cooking Week 1: Cucumber Sandwiches Week 2: Alien Playdough Week 3: Sunshine Shake Week 4: Moon Sand Week 5: Rocket Shaped Snack Cucumber Sandwich Ingredients 1 carton (8 ounces) spreadable cream cheese 2 teaspoons ranch salad dressing mix (dry one) 12 slices mini bread 2 to 3 medium cucumbers, sliced, thinly Let the children take turns mixing the cream cheese and ranch salad dressing mix. The children can also assemble their own sandwiches. They can spread the mixture themselves on their bread with a spoon and can put the cucumbers on themselves. Sunshine Shakes Ingredients and items needed: blender; 6 ounce can of unsweetened frozen orange juice concentrate, 3/4 cup of milk, 3/4 cup of water, 1 teaspoon of vanilla and 6 ice cubes. Children should help you put the items in the blender. You blend it up and yum! Moon Sand Materials Needed: 6 cups play sand (you can purchased colored play sand as well!); 3 cups cornstarch; 1 1/2 cups of cold water. -Have the children help scoop the corn starch and water into the table and mix until smooth. -Add sand gradually. This is very pliable sand and fun! -Be sure to store in an airtight container when not in use. If it dries, ad a few tablespoons of water and mix it in. -
Atmospheric Mining in the Outer Solar System (AMOSS): JPC 2011 Paper
National Aeronautics and Space Administration Atmospheric Mining in the Outer Solar System: Aerial Vehicle Mission and Design Issues 51th AIAA/ ASME/ SAE/ ASEE Joint Propulsion Conference and Exhibit Propulsion and Energy Forum Orlando, FL Bryan Palaszewski NASA Glenn Research Center Cleveland OH July 2015 www.nasa.gov 1 National Aeronautics and Space Administration Introduction • Why atmospheric mining? • Resource capturing: helium 3, hydrogen, helium. • Aerospacecraft as uninhabited aerial vehicles (UAVs), cruisers for weather reconnaissance, monitoring, etc. • Engine issues. – Gas core engines, closed cycle. – Lifetime(s). • Orbital transfer vehicle (OTV), lander, factory sizing and optimization(s). • Observations. • Concluding remarks. www.nasa.gov 2 National Aeronautics and Space Administration In Situ Resource Utilization (ISRU) • In Situ Resource Utilization uses the materials from other places in the solar system to sustain human exploration • Using those resources reduces the reliance on Earth launched mass, and hopefully reduces mission costs • There are powerful capabilities to free humans from Earth www.nasa.gov 3 National Aeronautics and Space Administration Why Atmospheric Mining? • Benefits: – Large amount of matter to mine (hydrogen and helium 3) – Potentially easier than mining regolith (dust) and rock – Larger reservoir of materials not readily available in regolith (and in a gaseous state) • Potential drawbacks – Dipping deep into the gravity well of planets is expensive for propulsion systems – Lifetime of systems – -
Aerospace Micro-Lesson
AIAA AEROSPACE M ICRO-LESSON Easily digestible Aerospace Principles revealed for K-12 Students and Educators. These lessons will be sent on a bi-weekly basis and allow grade-level focused learning. - AIAA STEM K-12 Committee. THE VOYAGER MISSIONS Forty years ago this month, on August 20, 1977, Voyager 2 was launched from Cape Canaveral in Florida. Its companion spacecraft, Voyager 1, launched two weeks later, on September 5. Voyager 1 flew past Jupiter on March 5, 1979 and Saturn on November 12, 1980. The slower-moving Voyager 2 reached Jupiter on July 9, 1979 and Saturn on August 25, 1981. Taking advantage of a very unusual alignment of the outer planets, Voyager 2 went on to Uranus, reaching it on January 24, 1986, and Neptune, which it flew past on August 25, 1989. (The dates given are those of the spacecraft’s closest approaches to the planets.) The two spacecraft are now leaving the Solar System and starting to fly into interstellar space. Next Generation Science Standards (NGSS): Discipline: Earth and Space Sciences. Crosscutting Concept: Scale, proportion, and quantity. Science & Engineering Practice: Obtaining, evaluating, and communicating information. GRADES K-2 NGSS: Earth’s Place in the Universe: Use observations of the sun, moon, and stars to describe patterns that can be predicted. In 1977, the United States launched two spacecraft to the outer planets of the Solar System. Their primary mission was to explore the planets Jupiter and Saturn. They discovered many new facts about the planets such as how complicated the rings of Saturn are and that Jupiter’s moon Io has active volcanoes (which makes it very different from our own moon). -
Atmospheric Mining in the Outer Solar System (AMOSS): JPC 2011 Paper
National Aeronautics and Space Administration Atmospheric Mining in the Outer Solar System: Outer Planet Orbital Transfer and Lander Analyses 52th AIAA/ ASME/ SAE/ ASEE Joint Propulsion Conference and Exhibit Propulsion and Energy Forum Salt Lake City, UT Bryan Palaszewski NASA Glenn Research Center Cleveland OH July 2016 www.nasa.gov 1 National Aeronautics and Space Administration Introduction • Why atmospheric mining? • Resource capturing: helium 3, hydrogen, helium. • Orbital transfer vehicle (OTV), lander, factory sizing. • System optimization(s) and issues. • Observations. • Concluding remarks. www.nasa.gov 2 National Aeronautics and Space Administration In Situ Resource Utilization (ISRU) • In Situ Resource Utilization uses the materials from other places in the solar system to sustain human exploration • Using those resources reduces the reliance on Earth launched mass, and hopefully reduces mission costs • There are powerful capabilities to free humans from Earth www.nasa.gov 3 National Aeronautics and Space Administration Why Atmospheric Mining? • Benefits: – Large amount of matter to mine (hydrogen and helium 3) – Potentially easier than mining regolith (dust) and rock – Larger reservoir of materials not readily available in regolith (and in a gaseous state) • Potential drawbacks – Dipping deep into the gravity well of planets is expensive for propulsion systems – Lifetime of systems – Repetitive maneuvers – Cryogenic atmospheric environments – Long delivery pipelines www.nasa.gov 4 National Aeronautics and Space Administration