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GRAIL

The Gravity Recovery and Interior Laboratory (GRAIL) was an American lunar science mission in NASA's Discovery Program which used high-quality gravitational field mapping of the Moon to determine its interior structure. The two small spacecraft GRAIL A (Ebb) and GRAIL B (Flow)[5][6] were launched on 10 September 2011 aboard a single launch vehicle: the most-powerful configuration of a Delta II, the 7920H-10.[1][7][8] GRAIL A separated from the rocket about nine minutes after launch, GRAIL B followed about eight minutes later. They arrived at their orbits around the Moon 25 hours apart.[9][10] The first probe entered orbit on 31 December 2011 and the second followed on 1 January 2012.[11] The two spacecraft impacted the Lunar surface on December 17, 2012.[12]

Gravity Recovery and Interior Laboratory
Artist's interpretation of the GRAIL tandem spacecraft above the lunar surface.
OperatorNASA / JPL[1][2]
COSPAR ID2011-046 (A, B)
SATCAT no.37801, 37802
Websitemoon.mit.edu
Mission duration1 year, 3 months, 7 days, 9 hours
Spacecraft properties
ManufacturerMassachusetts Institute of Technology, LMSS
Launch mass202.4 kg (each)[3]
Dry mass132.6 kg (292 lb)
Power(Solar array / Li-ion battery)
Start of mission
Launch dateSeptember 10, 2011, 13:08:52.775 (2011-09-10UTC13:08:52Z) UTC
RocketDelta II 7920H-10 D-356
Launch siteCape Canaveral SLC-17B
Entered serviceDecember 31, 2011 (Ebb)
January 1, 2012 (Flow)
Orbital parameters
Reference systemSelenocentric
RegimePolar orbit[4]
Semi-major axis1,788.0 kilometres (1,111.0 mi)
Periselene altitude25 kilometres (16 mi)
Aposelene altitude86 kilometres (53 mi)
Period113 minutes
Lunar impactor
Impact dateGRAIL A: December 17, 2012, 22:28:51 UTC
Impact site75°36′30″N 33°24′15″E / 75.6083°N 33.4043°E / 75.6083; 33.4043
Lunar impactor
Impact dateGRAIL B: December 17, 2012, 22:29:21 UTC
Impact site75°39′01″N 33°09′51″E / 75.6504°N 33.1643°E / 75.6504; 33.1643
← Kepler
InSight →
 
MoonKAM shot

Overview edit

 
Fourth grade students at Emily Dickinson Elementary School in Bozeman, Montana who suggested names Ebb and Flow.[6]

Maria Zuber of the Massachusetts Institute of Technology was GRAIL's principal investigator. NASA's Jet Propulsion Laboratory managed the project. NASA budgeted US$496 million for the program to include spacecraft and instrument development, launch, mission operations, and science support.[13] Upon launch the spacecraft were named GRAIL A and GRAIL B and a contest was opened to school children to select names. Nearly 900 classrooms from 45 states, Puerto Rico and the District of Columbia, participated in the contest. The winning names, Ebb and Flow, were suggested by 4th grade students at Emily Dickinson Elementary School in Bozeman, Montana.[6]

Each spacecraft transmitted and received telemetry from the other spacecraft and Earth-based facilities. By measuring the change in distance between the two spacecraft, the gravity field and geological structure of the Moon was obtained. The two spacecraft were able to detect very small changes in the distance between one another. Changes in distance as small as one micrometre were detectable and measurable.[14][15] The gravitational field of the Moon was mapped in unprecedented detail.[4][16][17][18][19]

Objectives edit

  • Map the structure of the lunar crust and lithosphere
  • Understand the asymmetric thermal evolution of the Moon
  • Determine the subsurface structure of impact basins and the origin of lunar mascons
  • Ascertain the temporal evolution of crustal brecciation and magmatism
  • Constrain the deep interior structure of the Moon
  • Place limits on the size of the Moon's inner core

The data collection phase of the mission lasted from 7 March 2012 to 29 May 2012, for a total of 88 days. A second phase, at a lower altitude, of data collection began 31 August 2012,[20] and was followed by 12 months of data analysis.[4] On 5 December 2012 NASA released a gravity map of the Moon made from GRAIL data.[21] The knowledge acquired will aid understanding of the evolutionary history of the terrestrial planets and computations of lunar orbits.[22]

Spacecraft edit

Instruments edit

 
Gravity map of the Moon by GRAIL
  • Ka band Lunar Gravity Ranging System (LGRS), derived from the Gravity Recovery and Climate Experiment (GRACE) instrument.[23] 90% of the GRACE software was reused for GRAIL.[24]
  • Radio science beacon (RSB)
  • Moon Knowledge Acquired by Middle school students (MoonKAM).[25] Each MoonKAM system (one per spacecraft) consists of a digital video controller and four camera heads.[26] Click here [1] for a MoonKAM photo from lunar orbit.

Propulsion edit

Thrusters aboard each spacecraft were capable of producing 22 newtons (4.9 lbf).[23] Each spacecraft was fueled with 103.5 kilograms (228 lb) of hydrazine to be used by the thrusters and main engine to enable the spacecraft to enter lunar orbit and transition to the science phase of its mission. The propulsion subsystem consisted of a main fuel tank and a Re-repressurization system which were activated shortly after lunar orbit insertion.[27]

Mission profile edit

Launch attempts edit

All times are in EDT (UTC-4).

Attempt Planned Result Turnaround Reason Decision point Weather go (%) Notes
1 8 Sep 2011, 8:37:06 am scrubbed[28] high level winds 8 Sep 2011, 8:30 am 40% A weather balloon was released minutes before the decision point to take the latest readings of upper level winds and Air Force weather reconnaissance aircraft were aloft beginning at 7 am.
2 8 Sep 2011, 9:16:12 am scrubbed[28] 0 days, 0 hours, 39 minutes high level winds 8 Sep 2011, 9:07 am 40% [29] Range was reconfigured for omni antennae instead of tracked ones to support 99 degree azimuth.
3 9 Sep 2011, 8:33:25 am abandoned[28] 0 days, 23 hours, 17 minutes rocket propulsion 40% An issue with the rocket's propulsion system was detected while the Delta 2 rocket was drained of fuel.
4 10 Sep 2011, 8:29:45 am scrubbed[28] 0 days, 23 hours, 56 minutes high level winds 10 Sep 2011, 8:21 am 60%
5 10 Sep 2011, 9:08:52 am Success[28] 0 days, 0 hours, 39 minutes

Transit phase edit

 
Animation of GRAIL-A's trajectory from 10 September 2011 to 17 December 2012
   GRAIL-A ·   Moon ·   Earth
 
GRAIL-transit-Earth-Moon
 
Animation of GRAIL-A's trajectory around Moon from 31 December 2011 to 30 April 2012
   GRAIL-A ·   Moon

Unlike the Apollo program missions, which took three days to reach the Moon, GRAIL made use of a three- to four-month low-energy trans-lunar cruise well outside the Moon's orbit and passing near the Sun-Earth Lagrange point L1 before looping back to rendezvous with the Moon. This extended and circuitous trajectory enabled the mission to reduce fuel requirements, protect instruments and reduce the velocity of the two spacecraft at lunar arrival to help achieve the extremely low 50 km (31 mi) orbits with separation between the spacecraft (arriving 25 hours apart) of 175 to 225 km (109 to 140 mi).[22][30] The very tight tolerances in the flight plan left little room for error correction leading to a launch window lasting one second and providing only two launch opportunities per day.[29]

Science phase edit

The primary science phase of GRAIL lasted for 88 days, from 7 March 2012 to 29 May 2012. It was followed by a second science phase that ran from 8 Aug 2012 into early Dec 2012.

The gravity mapping technique was similar to that used by Gravity Recovery and Climate Experiment (GRACE), and the spacecraft design was based on XSS-11.[31]

The orbital insertion dates were December 31, 2011 (2011-12-31) (for GRAIL-A) and January 1, 2012 (2012-01-01) (for GRAIL-B).[28] The initial lunar orbits were highly elliptical near-polar, and were later lowered to near-circular at about 25-86 km altitude with a period of about 114 minutes.[32]

The spacecraft were operated over the 88-day acquisition phase, divided into three 27.3 day long nadir-pointed mapping cycles. Twice each day there was an 8-hour pass in view of the Deep Space Network for transmission of science and "E/PO MoonKam" data.[33]

The first student-requested MoonKam images were taken by Ebb from 2012 March 15-17 and downlinked to Earth March 20. More than 2,700 schools spanning 52 countries were using the MoonKAM cameras. [34]

Flow's MoonKam camera captured LRO as it flew by at a distance of about 12 miles (20 km) on May 3. It's the first footage of a moon-orbiting robotic spacecraft taken by another one.[35]

Terminal phase edit

 
Ebb and Flow's final moments.
 
GRAIL's final resting spot.
This animation shows the last three orbits of the spacecraft, with views of the impact site. The impact occurs on the night side of a waxing crescent Moon, so the view shifts from a natural color Moon to a false-color elevation map.
LRO flies over the north pole of the Moon, where it has a very good view of the GRAIL impact. The second part of this video is the view from LRO through LAMP's slit, showing the impact and the resulting plume.

Final experiment and mission end edit

At the end of the science phase and a mission extension, the spacecraft were powered down and decommissioned over a five-day period. The spacecraft impacted the lunar surface on December 17, 2012.[33][36][37][38][39][40] Both spacecraft impacted an unnamed lunar mountain between Philolaus and Mouchez at 75°37′N 26°38′W / 75.62°N 26.63°W / 75.62; -26.63. Ebb, the lead spacecraft in formation, impacted first. Flow impacted moments later. Each spacecraft was traveling at 3,760 miles per hour (1.68 km/s). A final experiment was conducted during the final days of the mission. Main engines aboard the spacecraft were fired, depleting remaining fuel. Data from that effort will be used by mission planners to validate fuel consumption computer models to improve predictions of fuel needs for future missions.[41] NASA has announced that the crash site will be named after GRAIL collaborator and first American woman in space, Sally Ride.[42]

Moon – Oceanus Procellarum ("Ocean of Storms")
 
Ancient rift valleys – rectangular structure (visible – topography – GRAIL gravity gradients) (October 1, 2014).
 
Ancient rift valleys – context.
 
Ancient rift valleys – closeup (artist's concept).

Results edit

Gravity passes through matter. In addition to surface mass, a high-resolution gravity field gives a blurred, but useful, look below the surface. Analyses of the GRAIL data have produced a series of scientific results for the Moon.

  • The resolution of the gravity field has improved by a large amount over pre-GRAIL results. Early analyses gave the Gravitation of the Moon with fields of degree and order 420 and 660.[43][16][17] Subsequent analyses have resulted in higher degree and order fields.[18][19] Maps of the gravity field were made.
  • The crustal density and porosity were determined.[44] The crust was fragmented by large ancient impacts.
  • Long narrow linear features were found that are interpreted to be ancient tabular intrusions or dikes formed by magma.[45]
  • Combining gravity and Lunar Laser Ranging data gives the 3 principal moments of inertia.[46] The moments indicate that a dense core is small.
  • Combining gravity and lunar Topography, 74 circular impact basins were identified.[47] Strong increases in gravity that are associated with circular impact basins are mascons discovered by Muller and Sjogren.[48] The strongest gravity anomalies are from basins filled with dense mare material, but the strong gravity also requires that the boundary between the crust and denser mantle be warped upward. Where the crust is thicker, there may be no mare fill but the crust-mantle boundary is still warped upward.
  • The radius, density, and rigidity of interior layers is inferred.[49]
  • The Orientale basin is the youngest and best-preserved impact basin on the Moon.[50] The gravity field of this 3-ring basin was mapped at high resolution.

See also edit

References edit

  1. ^ a b . United Launch Alliance. 2011. Archived from the original on 1 September 2011. Retrieved 2 September 2011.
  2. ^ . Sally Ride Science. 2010. Archived from the original on 2010-04-28. Retrieved 2010-04-15.
  3. ^ "GRAIL" (PDF). NASA. Retrieved November 30, 2022.
  4. ^ a b c "About GRAIL". Massachusetts Institute of Technology. Retrieved 2011-03-12.
  5. ^ Schontzler, Gail (18 January 2012). "Bozeman class wins contest to name satellites orbiting moon". Bozeman Daily Chronicle. Retrieved 2018-12-18.
  6. ^ a b c Agle, DC. "Montana Students Submit Winning Names for NASA Lunar Spacecraft". NASA JPL.
  7. ^ (PDF) (Report). United Launch Alliance. 2010. Archived from the original (PDF) on 30 September 2011. Retrieved 2 August 2011.
  8. ^ Grey Hautaluoma (10 December 2007). "New NASA Mission to Reveal Moon's Internal Structure and Evolution". NASA. Retrieved 31 August 2011.
  9. ^ Moon-bound twin GRAIL spacecraft launch success
  10. ^ Spaceflight101 2015-02-11 at the Wayback Machine
  11. ^ "First of NASA's GRAIL Spacecraft Enters Moon Orbit". NASA. Retrieved 1 January 2012.
  12. ^ GRAIL Twins crash into the Moon to complete highly successful Mission 2015-02-11 at the Wayback Machine
  13. ^ "Press Kit. Gravity Recovery and Interior Laboratory (GRAIL) Launch" (PDF). NASA. August 2011. p. 7. Retrieved 4 December 2022.
  14. ^ GRAVITY RECOVERY AND INTERIOR LABORATORY (GRAIL) MISSION: STATUS AT THE INITIATION OF THE SCIENCE MAPPING PHASE, 43rd Lunar and Planetary Science Conference (2012)
  15. ^ Washington Post December 17, 2012
  16. ^ a b Konopliv, Alex S.; Park, Ryan S.; Yuan, Dah-Ning; Asmar, Sami W.; Watkins, Michael M.; Williams, James G.; Fahnestock, Eugene; Kruizinga, Gerhard; Paik, Meegyeong; Strekalov, Dmitry; Harvey, Nate (2013). "The JPL lunar gravity field to spherical harmonic degree 660 from the GRAIL Primary Mission: GRAIL LUNAR GRAVITY". Journal of Geophysical Research: Planets. 118 (7): 1415–1434. Bibcode:2013JGRE..118.1415K. doi:10.1002/jgre.20097. hdl:1721.1/85858. S2CID 16559256.
  17. ^ a b Lemoine, Frank G.; Goossens, Sander; Sabaka, Terence J.; Nicholas, Joseph B.; Mazarico, Erwan; Rowlands, David D.; Loomis, Bryant D.; Chinn, Douglas S.; Caprette, Douglas S.; Neumann, Gregory A.; Smith, David E. (2013). "High‒degree gravity models from GRAIL primary mission data". Journal of Geophysical Research: Planets. 118 (8): 1676–1698. Bibcode:2013JGRE..118.1676L. doi:10.1002/jgre.20118. hdl:2060/20140010292. ISSN 2169-9097.
  18. ^ a b Konopliv, Alex S.; Park, Ryan S.; Yuan, Dah-Ning; Asmar, Sami W.; Watkins, Michael M.; Williams, James G.; Fahnestock, Eugene; Kruizinga, Gerhard; Paik, Meegyeong; et al. (2014). "High-resolution lunar gravity fields from the GRAIL Primary and Extended Missions". Geophysical Research Letters. 41 (5): 1452–1458. Bibcode:2014GeoRL..41.1452K. doi:10.1002/2013GL059066.
  19. ^ a b Lemoine, Frank G.; Goossens, Sander; Sabaka, Terence J.; Nicholas, Joseph B.; Mazarico, Erwan; Rowlands, David D.; Loomis, Bryant D.; Chinn, Douglas S.; Neumann, Gregory A.; Smith, David E.; Zuber, Maria T. (28 May 2014). "GRGM900C: A degree 900 lunar gravity model from GRAIL primary and extended mission data". Geophysical Research Letters. 41 (10): 3382–3389. Bibcode:2014GeoRL..41.3382L. doi:10.1002/2014GL060027. PMC 4459205. PMID 26074638.
  20. ^ Gravity Recovery and Interior Laboratory: News & Features: NASA's GRAIL Moon Twins Begin Extended Mission Science 2013-04-09 at the Wayback Machine. Solarsystem.nasa.gov. Retrieved on 2013-07-21.
  21. ^ Gravity Recovery and Interior Laboratory: News & Features: NASA's GRAIL Creates Most Accurate Moon Gravity Map 2013-05-11 at the Wayback Machine. Solarsystem.nasa.gov. Retrieved on 2013-07-21.
  22. ^ a b "GRAIL: Mission Overview". MIT. Retrieved 10 September 2011.
  23. ^ a b "Spacecraft and Payload". Massachusetts Institute of Technology.
  24. ^ . MIT. Archived from the original on 2012-03-05. Retrieved 2012-12-14.
  25. ^ . Sally Ride Science. 2010. Archived from the original on 2010-04-27. Retrieved 2010-04-15.
  26. ^ "GRAIL Launch Press Kit" (PDF). NASA. Retrieved 31 August 2011.
  27. ^ "Satellite Missions Catalogue - GRAIL". eoPortal.org. Retrieved December 3, 2022.
  28. ^ a b c d e f Harwood, William. "NASA launches GRAIL lunar probes". CBS News. Retrieved 11 September 2011.
  29. ^ a b Justin Ray (17 August 2011). "GRAIL Launch Window Chart". SpaceFlight Now. Retrieved 9 September 2011.
  30. ^ . NASA. Archived from the original on 3 October 2011. Retrieved 10 September 2011.
  31. ^ Taylor Dinerman (31 December 2007). "Is XSS-11 the answer to America's quest for Operationally Responsive Space?". The Space Review. Retrieved 31 August 2011.
  32. ^ Grail mission news. March 2012
  33. ^ a b "GRAIL: Mission Design". MIT.
  34. ^ "NASA GRAIL Returns First Student-Selected Moon Images". Jet Propulsion Laboratory.
  35. ^ "Spacecraft Pass Each Other at the Moon".
  36. ^ "NASA GRAIL Twins Complete Their Moon Impact". NASA. 17 December 2012. Retrieved 2012-12-17.
  37. ^ Wall, Mike (13 December 2012). "Twin GRAIL probes readied for crash into Moon". NBC News. Retrieved 18 February 2013.
  38. ^ Wall, Mike (11 December 2012). "Twin NASA Probes to Crash into Moon Next Week". Space.com. Retrieved 18 February 2013.
  39. ^ "Twin NASA spacecraft prepare to crash into moon". Phys.org. 13 December 2012. Retrieved 13 December 2012.
  40. ^ Knapp, Alex (14 December 2012). "NASA Prepares To Crash Its Probes Into The Moon". Forbes. Retrieved 2012-12-13.
  41. ^ "NASA Probes Prepare for Mission-Ending Moon Impact". NASA, Jet Propulsion Laboratory. Retrieved 18 February 2013.
  42. ^ Mike Wall (17 December 2012). "Moon Probes' Crash Site Named After Sally Ride". Space.com. Retrieved 18 February 2013.
  43. ^ Zuber, M. T.; Smith, D. E.; Watkins, M. M.; Asmar, S. W.; Konopliv, A. S.; Lemoine, F. G.; Melosh, H. J.; Neumann, G. A.; Phillips, R. J.; et al. (2013). "Gravity Field of the Moon from the Gravity Recovery and Interior Laboratory (GRAIL) Mission". Science. 339 (6120): 668–671. Bibcode:2013Sci...339..668Z. doi:10.1126/science.1231507. ISSN 0036-8075. PMID 23223395. S2CID 206545934.
  44. ^ Wieczorek, M. A.; Neumann, G. A.; Nimmo, F.; Kiefer, W. S.; Taylor, G. J.; Melosh, H. J.; Phillips, R. J.; Solomon, S. C.; Andrews-Hanna, J. C.; et al. (2013). "The Crust of the Moon as Seen by GRAIL". Science. 339 (6120): 671–675. Bibcode:2013Sci...339..671W. doi:10.1126/science.1231530. ISSN 0036-8075. PMC 6693503. PMID 23223394.
  45. ^ Andrews-Hanna, J. C.; Asmar, S. W.; Head, J. W.; Kiefer, W. S.; Konopliv, A. S.; Lemoine, F. G.; Matsuyama, I.; Mazarico, E.; McGovern, P. J.; et al. (2013). "Ancient Igneous Intrusions and Early Expansion of the Moon Revealed by GRAIL Gravity Gradiometry". Science. 339 (6120): 675–678. Bibcode:2013Sci...339..675A. doi:10.1126/science.1231753. ISSN 0036-8075. PMID 23223393. S2CID 18004181.
  46. ^ Williams, James G.; Konopliv, Alexander S.; Boggs, Dale H.; Park, Ryan S.; Yuan, Dah-Ning; Lemoine, Frank G.; Goossens, Sander; Mazarico, Erwan; Nimmo, Francis; et al. (2014). "Lunar interior properties from the GRAIL mission". Journal of Geophysical Research: Planets. 119 (7): 1546–1578. Bibcode:2014JGRE..119.1546W. doi:10.1002/2013JE004559. S2CID 7045590.
  47. ^ Neumann, Gregory A.; Zuber, Maria T.; Wieczorek, Mark A.; Head, James W.; Baker, David M. H.; Solomon, Sean C.; Smith, David E.; Lemoine, Frank G.; Mazarico, Erwan; et al. (2015). "Lunar impact basins revealed by Gravity Recovery and Interior Laboratory measurements". Science Advances. 1 (9): e1500852. Bibcode:2015SciA....1E0852N. doi:10.1126/sciadv.1500852. ISSN 2375-2548. PMC 4646831. PMID 26601317.
  48. ^ Muller, P. M.; Sjogren, W. L. (1968). "Mascons: Lunar Mass Concentrations". Science. 161 (3842): 680–684. Bibcode:1968Sci...161..680M. doi:10.1126/science.161.3842.680. ISSN 0036-8075. PMID 17801458. S2CID 40110502.
  49. ^ Matsuyama, Isamu; Nimmo, Francis; Keane, James T.; Chan, Ngai H.; Taylor, G. Jeffrey; Wieczorek, Mark A.; Kiefer, Walter S.; Williams, James G. (2016). "GRAIL, LLR, and LOLA constraints on the interior structure of the Moon". Geophysical Research Letters. 43 (16): 8365–8375. Bibcode:2016GeoRL..43.8365M. doi:10.1002/2016GL069952. hdl:10150/621595. S2CID 36834256.
  50. ^ Zuber, M. T.; Smith, D. E.; Neumann, G. A.; Goossens, S.; Andrews-Hanna, J. C.; Head, J. W.; Kiefer, W. S.; Asmar, S. W.; Konopliv, A. S.; et al. (2016). "Gravity field of the Orientale basin from the Gravity Recovery and Interior Laboratory Mission". Science. 354 (6311): 438–441. Bibcode:2016Sci...354..438Z. doi:10.1126/science.aag0519. ISSN 0036-8075. PMC 7462089. PMID 27789835.

External links edit

  • NASA
  • NASA GRAIL (Gravity Recovery and Interior Laboratory) – mission home page
  • MIT GRAIL Home Page
  • NASA Science Missions: GRAIL (Gravity Recovery and Interior Laboratory)
  • NASA 360 New Worlds New Discoveries 2/2 Retrieved 6/3/2011.
  • Behind The Scenes of My NASA GRAIL Experience – Day One (AM)

grail, other, uses, grail, disambiguation, gravity, recovery, interior, laboratory, american, lunar, science, mission, nasa, discovery, program, which, used, high, quality, gravitational, field, mapping, moon, determine, interior, structure, small, spacecraft,. For other uses see Grail disambiguation The Gravity Recovery and Interior Laboratory GRAIL was an American lunar science mission in NASA s Discovery Program which used high quality gravitational field mapping of the Moon to determine its interior structure The two small spacecraft GRAIL A Ebb and GRAIL B Flow 5 6 were launched on 10 September 2011 aboard a single launch vehicle the most powerful configuration of a Delta II the 7920H 10 1 7 8 GRAIL A separated from the rocket about nine minutes after launch GRAIL B followed about eight minutes later They arrived at their orbits around the Moon 25 hours apart 9 10 The first probe entered orbit on 31 December 2011 and the second followed on 1 January 2012 11 The two spacecraft impacted the Lunar surface on December 17 2012 12 Gravity Recovery and Interior LaboratoryArtist s interpretation of the GRAIL tandem spacecraft above the lunar surface OperatorNASA JPL 1 2 COSPAR ID2011 046 A B SATCAT no 37801 37802Websitemoon wbr mit wbr eduMission duration1 year 3 months 7 days 9 hoursSpacecraft propertiesManufacturerMassachusetts Institute of Technology LMSSLaunch mass202 4 kg each 3 Dry mass132 6 kg 292 lb Power Solar array Li ion battery Start of missionLaunch dateSeptember 10 2011 13 08 52 775 2011 09 10UTC13 08 52Z UTCRocketDelta II 7920H 10 D 356Launch siteCape Canaveral SLC 17BEntered serviceDecember 31 2011 Ebb January 1 2012 Flow Orbital parametersReference systemSelenocentricRegimePolar orbit 4 Semi major axis1 788 0 kilometres 1 111 0 mi Periselene altitude25 kilometres 16 mi Aposelene altitude86 kilometres 53 mi Period113 minutesLunar impactorImpact dateGRAIL A December 17 2012 22 28 51 UTCImpact site75 36 30 N 33 24 15 E 75 6083 N 33 4043 E 75 6083 33 4043Lunar impactorImpact dateGRAIL B December 17 2012 22 29 21 UTCImpact site75 39 01 N 33 09 51 E 75 6504 N 33 1643 E 75 6504 33 1643Discovery program KeplerInSight MoonKAM shot Contents 1 Overview 2 Objectives 3 Spacecraft 3 1 Instruments 3 2 Propulsion 4 Mission profile 4 1 Launch attempts 4 2 Transit phase 4 3 Science phase 4 4 Terminal phase 4 5 Final experiment and mission end 5 Results 6 See also 7 References 8 External linksOverview edit nbsp Fourth grade students at Emily Dickinson Elementary School in Bozeman Montana who suggested names Ebb and Flow 6 Maria Zuber of the Massachusetts Institute of Technology was GRAIL s principal investigator NASA s Jet Propulsion Laboratory managed the project NASA budgeted US 496 million for the program to include spacecraft and instrument development launch mission operations and science support 13 Upon launch the spacecraft were named GRAIL A and GRAIL B and a contest was opened to school children to select names Nearly 900 classrooms from 45 states Puerto Rico and the District of Columbia participated in the contest The winning names Ebb and Flow were suggested by 4th grade students at Emily Dickinson Elementary School in Bozeman Montana 6 Each spacecraft transmitted and received telemetry from the other spacecraft and Earth based facilities By measuring the change in distance between the two spacecraft the gravity field and geological structure of the Moon was obtained The two spacecraft were able to detect very small changes in the distance between one another Changes in distance as small as one micrometre were detectable and measurable 14 15 The gravitational field of the Moon was mapped in unprecedented detail 4 16 17 18 19 Objectives editMap the structure of the lunar crust and lithosphere Understand the asymmetric thermal evolution of the Moon Determine the subsurface structure of impact basins and the origin of lunar mascons Ascertain the temporal evolution of crustal brecciation and magmatism Constrain the deep interior structure of the Moon Place limits on the size of the Moon s inner core The data collection phase of the mission lasted from 7 March 2012 to 29 May 2012 for a total of 88 days A second phase at a lower altitude of data collection began 31 August 2012 20 and was followed by 12 months of data analysis 4 On 5 December 2012 NASA released a gravity map of the Moon made from GRAIL data 21 The knowledge acquired will aid understanding of the evolutionary history of the terrestrial planets and computations of lunar orbits 22 Spacecraft editInstruments edit nbsp Gravity map of the Moon by GRAIL Ka band Lunar Gravity Ranging System LGRS derived from the Gravity Recovery and Climate Experiment GRACE instrument 23 90 of the GRACE software was reused for GRAIL 24 Radio science beacon RSB Moon Knowledge Acquired by Middle school students MoonKAM 25 Each MoonKAM system one per spacecraft consists of a digital video controller and four camera heads 26 Click here 1 for a MoonKAM photo from lunar orbit Propulsion edit Thrusters aboard each spacecraft were capable of producing 22 newtons 4 9 lbf 23 Each spacecraft was fueled with 103 5 kilograms 228 lb of hydrazine to be used by the thrusters and main engine to enable the spacecraft to enter lunar orbit and transition to the science phase of its mission The propulsion subsystem consisted of a main fuel tank and a Re repressurization system which were activated shortly after lunar orbit insertion 27 Mission profile editLaunch attempts edit All times are in EDT UTC 4 Attempt Planned Result Turnaround Reason Decision point Weather go Notes 1 8 Sep 2011 8 37 06 am scrubbed 28 high level winds 8 Sep 2011 8 30 am 40 A weather balloon was released minutes before the decision point to take the latest readings of upper level winds and Air Force weather reconnaissance aircraft were aloft beginning at 7 am 2 8 Sep 2011 9 16 12 am scrubbed 28 0 days 0 hours 39 minutes high level winds 8 Sep 2011 9 07 am 40 29 Range was reconfigured for omni antennae instead of tracked ones to support 99 degree azimuth 3 9 Sep 2011 8 33 25 am abandoned 28 0 days 23 hours 17 minutes rocket propulsion 40 An issue with the rocket s propulsion system was detected while the Delta 2 rocket was drained of fuel 4 10 Sep 2011 8 29 45 am scrubbed 28 0 days 23 hours 56 minutes high level winds 10 Sep 2011 8 21 am 60 5 10 Sep 2011 9 08 52 am Success 28 0 days 0 hours 39 minutes nbsp Spacecraft technicians close the payload fairing around GRAIL before launch nbsp GRAIL awaits launch at Cape Canaveral Air Force Station nbsp Fire and smoke light up a blue sky as a United Launch Alliance Delta II Heavy rocket propels GRAIL into space Transit phase edit nbsp Animation of GRAIL A s trajectory from 10 September 2011 to 17 December 2012 GRAIL A Moon Earth nbsp GRAIL transit Earth Moon nbsp Animation of GRAIL A s trajectory around Moon from 31 December 2011 to 30 April 2012 GRAIL A Moon Unlike the Apollo program missions which took three days to reach the Moon GRAIL made use of a three to four month low energy trans lunar cruise well outside the Moon s orbit and passing near the Sun Earth Lagrange point L1 before looping back to rendezvous with the Moon This extended and circuitous trajectory enabled the mission to reduce fuel requirements protect instruments and reduce the velocity of the two spacecraft at lunar arrival to help achieve the extremely low 50 km 31 mi orbits with separation between the spacecraft arriving 25 hours apart of 175 to 225 km 109 to 140 mi 22 30 The very tight tolerances in the flight plan left little room for error correction leading to a launch window lasting one second and providing only two launch opportunities per day 29 Science phase edit The primary science phase of GRAIL lasted for 88 days from 7 March 2012 to 29 May 2012 It was followed by a second science phase that ran from 8 Aug 2012 into early Dec 2012 The gravity mapping technique was similar to that used by Gravity Recovery and Climate Experiment GRACE and the spacecraft design was based on XSS 11 31 The orbital insertion dates were December 31 2011 2011 12 31 for GRAIL A and January 1 2012 2012 01 01 for GRAIL B 28 The initial lunar orbits were highly elliptical near polar and were later lowered to near circular at about 25 86 km altitude with a period of about 114 minutes 32 The spacecraft were operated over the 88 day acquisition phase divided into three 27 3 day long nadir pointed mapping cycles Twice each day there was an 8 hour pass in view of the Deep Space Network for transmission of science and E PO MoonKam data 33 The first student requested MoonKam images were taken by Ebb from 2012 March 15 17 and downlinked to Earth March 20 More than 2 700 schools spanning 52 countries were using the MoonKAM cameras 34 Flow s MoonKam camera captured LRO as it flew by at a distance of about 12 miles 20 km on May 3 It s the first footage of a moon orbiting robotic spacecraft taken by another one 35 Terminal phase edit nbsp Ebb and Flow s final moments nbsp GRAIL s final resting spot source source source source source source source source This animation shows the last three orbits of the spacecraft with views of the impact site The impact occurs on the night side of a waxing crescent Moon so the view shifts from a natural color Moon to a false color elevation map source source source source source source source source LRO flies over the north pole of the Moon where it has a very good view of the GRAIL impact The second part of this video is the view from LRO through LAMP s slit showing the impact and the resulting plume Final experiment and mission end edit At the end of the science phase and a mission extension the spacecraft were powered down and decommissioned over a five day period The spacecraft impacted the lunar surface on December 17 2012 33 36 37 38 39 40 Both spacecraft impacted an unnamed lunar mountain between Philolaus and Mouchez at 75 37 N 26 38 W 75 62 N 26 63 W 75 62 26 63 Ebb the lead spacecraft in formation impacted first Flow impacted moments later Each spacecraft was traveling at 3 760 miles per hour 1 68 km s A final experiment was conducted during the final days of the mission Main engines aboard the spacecraft were fired depleting remaining fuel Data from that effort will be used by mission planners to validate fuel consumption computer models to improve predictions of fuel needs for future missions 41 NASA has announced that the crash site will be named after GRAIL collaborator and first American woman in space Sally Ride 42 Moon Oceanus Procellarum Ocean of Storms nbsp Ancient rift valleys rectangular structure visible topography GRAIL gravity gradients October 1 2014 nbsp Ancient rift valleys context nbsp Ancient rift valleys closeup artist s concept Results editGravity passes through matter In addition to surface mass a high resolution gravity field gives a blurred but useful look below the surface Analyses of the GRAIL data have produced a series of scientific results for the Moon The resolution of the gravity field has improved by a large amount over pre GRAIL results Early analyses gave the Gravitation of the Moon with fields of degree and order 420 and 660 43 16 17 Subsequent analyses have resulted in higher degree and order fields 18 19 Maps of the gravity field were made The crustal density and porosity were determined 44 The crust was fragmented by large ancient impacts Long narrow linear features were found that are interpreted to be ancient tabular intrusions or dikes formed by magma 45 Combining gravity and Lunar Laser Ranging data gives the 3 principal moments of inertia 46 The moments indicate that a dense core is small Combining gravity and lunar Topography 74 circular impact basins were identified 47 Strong increases in gravity that are associated with circular impact basins are mascons discovered by Muller and Sjogren 48 The strongest gravity anomalies are from basins filled with dense mare material but the strong gravity also requires that the boundary between the crust and denser mantle be warped upward Where the crust is thicker there may be no mare fill but the crust mantle boundary is still warped upward The radius density and rigidity of interior layers is inferred 49 The Orientale basin is the youngest and best preserved impact basin on the Moon 50 The gravity field of this 3 ring basin was mapped at high resolution See also edit nbsp Spaceflight portal List of artificial objects on the Moon Satellite gravimetry SelenoidReferences edit a b Delta II Set to Launch NASA s GRAIL Mission United Launch Alliance 2011 Archived from the original on 1 September 2011 Retrieved 2 September 2011 The GRAIL Mission A Fact Sheet Sally Ride Science 2010 Archived from the original on 2010 04 28 Retrieved 2010 04 15 GRAIL PDF NASA Retrieved November 30 2022 a b c About GRAIL Massachusetts Institute of Technology Retrieved 2011 03 12 Schontzler Gail 18 January 2012 Bozeman class wins contest to name satellites orbiting moon Bozeman Daily Chronicle Retrieved 2018 12 18 a b c Agle DC Montana Students Submit Winning Names for NASA Lunar Spacecraft NASA JPL Delta II The Industry Workhorse PDF Report United Launch Alliance 2010 Archived from the original PDF on 30 September 2011 Retrieved 2 August 2011 Grey Hautaluoma 10 December 2007 New NASA Mission to Reveal Moon s Internal Structure and Evolution NASA Retrieved 31 August 2011 Moon bound twin GRAIL spacecraft launch success Spaceflight101 Archived 2015 02 11 at the Wayback Machine First of NASA s GRAIL Spacecraft Enters Moon Orbit NASA Retrieved 1 January 2012 GRAIL Twins crash into the Moon to complete highly successful Mission Archived 2015 02 11 at the Wayback Machine Press Kit Gravity Recovery and Interior Laboratory GRAIL Launch PDF NASA August 2011 p 7 Retrieved 4 December 2022 GRAVITY RECOVERY AND INTERIOR LABORATORY GRAIL MISSION STATUS AT THE INITIATION OF THE SCIENCE MAPPING PHASE 43rd Lunar and Planetary Science Conference 2012 Washington Post December 17 2012 a b Konopliv Alex S Park Ryan S Yuan Dah Ning Asmar Sami W Watkins Michael M Williams James G Fahnestock Eugene Kruizinga Gerhard Paik Meegyeong Strekalov Dmitry Harvey Nate 2013 The JPL lunar gravity field to spherical harmonic degree 660 from the GRAIL Primary Mission GRAIL LUNAR GRAVITY Journal of Geophysical Research Planets 118 7 1415 1434 Bibcode 2013JGRE 118 1415K doi 10 1002 jgre 20097 hdl 1721 1 85858 S2CID 16559256 a b Lemoine Frank G Goossens Sander Sabaka Terence J Nicholas Joseph B Mazarico Erwan Rowlands David D Loomis Bryant D Chinn Douglas S Caprette Douglas S Neumann Gregory A Smith David E 2013 High degree gravity models from GRAIL primary mission data Journal of Geophysical Research Planets 118 8 1676 1698 Bibcode 2013JGRE 118 1676L doi 10 1002 jgre 20118 hdl 2060 20140010292 ISSN 2169 9097 a b Konopliv Alex S Park Ryan S Yuan Dah Ning Asmar Sami W Watkins Michael M Williams James G Fahnestock Eugene Kruizinga Gerhard Paik Meegyeong et al 2014 High resolution lunar gravity fields from the GRAIL Primary and Extended Missions Geophysical Research Letters 41 5 1452 1458 Bibcode 2014GeoRL 41 1452K doi 10 1002 2013GL059066 a b Lemoine Frank G Goossens Sander Sabaka Terence J Nicholas Joseph B Mazarico Erwan Rowlands David D Loomis Bryant D Chinn Douglas S Neumann Gregory A Smith David E Zuber Maria T 28 May 2014 GRGM900C A degree 900 lunar gravity model from GRAIL primary and extended mission data Geophysical Research Letters 41 10 3382 3389 Bibcode 2014GeoRL 41 3382L doi 10 1002 2014GL060027 PMC 4459205 PMID 26074638 Gravity Recovery and Interior Laboratory News amp Features NASA s GRAIL Moon Twins Begin Extended Mission Science Archived 2013 04 09 at the Wayback Machine Solarsystem nasa gov Retrieved on 2013 07 21 Gravity Recovery and Interior Laboratory News amp Features NASA s GRAIL Creates Most Accurate Moon Gravity Map Archived 2013 05 11 at the Wayback Machine Solarsystem nasa gov Retrieved on 2013 07 21 a b GRAIL Mission Overview MIT Retrieved 10 September 2011 a b Spacecraft and Payload Massachusetts Institute of Technology GRAIL Mission Operations amp Data Processing MIT Archived from the original on 2012 03 05 Retrieved 2012 12 14 About GRAIL MoonKAM Sally Ride Science 2010 Archived from the original on 2010 04 27 Retrieved 2010 04 15 GRAIL Launch Press Kit PDF NASA Retrieved 31 August 2011 Satellite Missions Catalogue GRAIL eoPortal org Retrieved December 3 2022 a b c d e f Harwood William NASA launches GRAIL lunar probes CBS News Retrieved 11 September 2011 a b Justin Ray 17 August 2011 GRAIL Launch Window Chart SpaceFlight Now Retrieved 9 September 2011 Mission Design NASA Archived from the original on 3 October 2011 Retrieved 10 September 2011 Taylor Dinerman 31 December 2007 Is XSS 11 the answer to America s quest for Operationally Responsive Space The Space Review Retrieved 31 August 2011 Grail mission news March 2012 a b GRAIL Mission Design MIT NASA GRAIL Returns First Student Selected Moon Images Jet Propulsion Laboratory Spacecraft Pass Each Other at the Moon NASA GRAIL Twins Complete Their Moon Impact NASA 17 December 2012 Retrieved 2012 12 17 Wall Mike 13 December 2012 Twin GRAIL probes readied for crash into Moon NBC News Retrieved 18 February 2013 Wall Mike 11 December 2012 Twin NASA Probes to Crash into Moon Next Week Space com Retrieved 18 February 2013 Twin NASA spacecraft prepare to crash into moon Phys org 13 December 2012 Retrieved 13 December 2012 Knapp Alex 14 December 2012 NASA Prepares To Crash Its Probes Into The Moon Forbes Retrieved 2012 12 13 NASA Probes Prepare for Mission Ending Moon Impact NASA Jet Propulsion Laboratory Retrieved 18 February 2013 Mike Wall 17 December 2012 Moon Probes Crash Site Named After Sally Ride Space com Retrieved 18 February 2013 Zuber M T Smith D E Watkins M M Asmar S W Konopliv A S Lemoine F G Melosh H J Neumann G A Phillips R J et al 2013 Gravity Field of the Moon from the Gravity Recovery and Interior Laboratory GRAIL Mission Science 339 6120 668 671 Bibcode 2013Sci 339 668Z doi 10 1126 science 1231507 ISSN 0036 8075 PMID 23223395 S2CID 206545934 Wieczorek M A Neumann G A Nimmo F Kiefer W S Taylor G J Melosh H J Phillips R J Solomon S C Andrews Hanna J C et al 2013 The Crust of the Moon as Seen by GRAIL Science 339 6120 671 675 Bibcode 2013Sci 339 671W doi 10 1126 science 1231530 ISSN 0036 8075 PMC 6693503 PMID 23223394 Andrews Hanna J C Asmar S W Head J W Kiefer W S Konopliv A S Lemoine F G Matsuyama I Mazarico E McGovern P J et al 2013 Ancient Igneous Intrusions and Early Expansion of the Moon Revealed by GRAIL Gravity Gradiometry Science 339 6120 675 678 Bibcode 2013Sci 339 675A doi 10 1126 science 1231753 ISSN 0036 8075 PMID 23223393 S2CID 18004181 Williams James G Konopliv Alexander S Boggs Dale H Park Ryan S Yuan Dah Ning Lemoine Frank G Goossens Sander Mazarico Erwan Nimmo Francis et al 2014 Lunar interior properties from the GRAIL mission Journal of Geophysical Research Planets 119 7 1546 1578 Bibcode 2014JGRE 119 1546W doi 10 1002 2013JE004559 S2CID 7045590 Neumann Gregory A Zuber Maria T Wieczorek Mark A Head James W Baker David M H Solomon Sean C Smith David E Lemoine Frank G Mazarico Erwan et al 2015 Lunar impact basins revealed by Gravity Recovery and Interior Laboratory measurements Science Advances 1 9 e1500852 Bibcode 2015SciA 1E0852N doi 10 1126 sciadv 1500852 ISSN 2375 2548 PMC 4646831 PMID 26601317 Muller P M Sjogren W L 1968 Mascons Lunar Mass Concentrations Science 161 3842 680 684 Bibcode 1968Sci 161 680M doi 10 1126 science 161 3842 680 ISSN 0036 8075 PMID 17801458 S2CID 40110502 Matsuyama Isamu Nimmo Francis Keane James T Chan Ngai H Taylor G Jeffrey Wieczorek Mark A Kiefer Walter S Williams James G 2016 GRAIL LLR and LOLA constraints on the interior structure of the Moon Geophysical Research Letters 43 16 8365 8375 Bibcode 2016GeoRL 43 8365M doi 10 1002 2016GL069952 hdl 10150 621595 S2CID 36834256 Zuber M T Smith D E Neumann G A Goossens S Andrews Hanna J C Head J W Kiefer W S Asmar S W Konopliv A S et al 2016 Gravity field of the Orientale basin from the Gravity Recovery and Interior Laboratory Mission Science 354 6311 438 441 Bibcode 2016Sci 354 438Z doi 10 1126 science aag0519 ISSN 0036 8075 PMC 7462089 PMID 27789835 External links edit nbsp Wikimedia Commons has media related to GRAIL GRAIL Mission NASA NASA GRAIL Gravity Recovery and Interior Laboratory mission home page MIT GRAIL Home Page NASA Science Missions GRAIL Gravity Recovery and Interior Laboratory NASA 360 New Worlds New Discoveries 2 2 Retrieved 6 3 2011 Behind The Scenes of My NASA GRAIL Experience Day One AM Retrieved from https en wikipedia org w index php title GRAIL amp oldid 1199703347, wikipedia, wiki, book, books, library,

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