IBEX spacecraft detects fast neutral hydrogen coming from the moon

June 18, 2009,
NASA's Interstellar Boundary Explorer has made the first detection of neutral atoms coming from the Moon (background image). The color-coded data toward the bottom shows the neutral particles and geometry measured at the Moon on Dec. 3, 2008. IBEX spins at four rotations per minute with its field of view sweeping over the moon each spin over about 10 hours. The neutral atoms are summed in 6 degree bins with the lunar direction indicated by the white arrow. IBEX detects particles produced by reflection and neutralization of the incident solar wind protons at toward the spacecraft. The Earth, moon and spacecraft shown toward the top are not to scale. Credit: Southwest Research Institute

NASA's Interstellar Boundary Explorer (IBEX) spacecraft has made the first observations of very fast hydrogen atoms coming from the moon, following decades of speculation and searching for their existence.

During spacecraft commissioning, the IBEX team turned on the IBEX-Hi instrument, built primarily by Southwest Research Institute (SwRI) and the Los Alamos National Laboratory, which measures atoms with speeds from about half a million to 2.5 million miles per hour. Its companion sensor, IBEX-Lo, built by Lockheed Martin, the University of New Hampshire, NASA Goddard Space Flight Center, and the University of Bern in Switzerland, measures atoms with speeds from about one hundred thousand to 1.5 million mph.

"Just after we got IBEX-Hi turned on, the moon happened to pass right through its field of view, and there they were," says Dr. David J. McComas, IBEX principal investigator and assistant vice president of the SwRI Space Science and Engineering Division. "The instrument lit up with a clear signal of the neutral atoms being detected as they backscattered from the moon."

The , the supersonic stream of charged particles that flows out from the sun, moves out into space in every direction at speeds of about a million mph. The Earth's strong magnetic field shields our planet from the solar wind. The moon, with its relatively weak magnetic field, has no such protection, causing the solar wind to slam onto the moon's sunward side.

From its vantage point in space, IBEX sees about half of the moon -- one quarter of it is dark and faces the nightside (away from the sun), while the other quarter faces the dayside (toward the sun). Solar wind particles impact only the dayside, where most of them are embedded in the , while some scatter off in different directions. The scattered ones mostly become neutral atoms in this reflection process by picking up electrons from the lunar surface.

The IBEX team estimates that only about 10 percent of the solar wind ions reflect off the sunward side of the moon as neutral atoms, while the remaining 90 percent are embedded in the lunar surface. Characteristics of the lunar surface, such as dust, craters and rocks, play a role in determining the percentage of particles that become embedded and the percentage of neutral particles, as well as their direction of travel, that scatter.

McComas says the results also shed light on the "recycling" process undertaken by particles throughout the solar system and beyond. The solar wind and other charged particles impact dust and larger objects as they travel through space, where they backscatter and are reprocessed as neutral atoms. These atoms can travel long distances before they are stripped of their electrons and become ions and the complicated process begins again.

The combined scattering and neutralization processes now observed at the moon have implications for interactions with objects across the solar system, such as asteroids, Kuiper Belt objects and other moons. The plasma-surface interactions occurring within protostellar nebula, the region of space that forms around planets and stars -- as well as exoplanets, planets around other stars -- also can be inferred.

IBEX's primary mission is to observe and map the complex interactions occurring at the edge of the solar system, where the million miles per hour solar wind runs into the interstellar material from the rest of the galaxy. The spacecraft carries the most sensitive neutral atom detectors ever flown in space, enabling researchers to not only measure particle energy, but also to make precise images of where they are coming from.

Around the end of the summer, the team will release the spacecraft's first all-sky map showing the energetic processes occurring at the edge of the . The team will not comment until the image is complete, but McComas hints, "It doesn't look like any of the models."

Source: Southwest Research Institute (news : web)

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thermodynamics
not rated yet Jun 18, 2009
Good question nkalanaga. There should be a lot of hydrogen, but even more interesting is that this shows indirect proof that there should also be plenty of helium 3. helium 3 is a relatively rare isotope that is formed in the sun. It is also an isotope that is expected to be a great fuel for the next generation (if there is a first generation) of fusion reactors. Take a look at the helium-3 page in Wikipedia for the interesting physics involved. The idea is that by confirming the hydrogen they are indirectly confirming the He-3 flux. That will give hydrogen and He-3 for the second generation fusion reactors as well as hydrogen for fuel. The idea of hydrogen for a combustion fuel is not that important because they also have both hydrogen and oxygen in the form of ice (which they are pretty certain exists at the poles).
Soylent
1 / 5 (1) Jun 19, 2009
Would there be enough to make it practical to recover the hydrogen as a byproduct of metal or oxygen production? If so, the moon could supply both fuel and oxygen for spacecraft.


When you make oxygen gas from water you automatically get as much hydrogen gas as you need, additional hydrogen is redundant.

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