Long queue for Mars One pioneering + Adapting to different gravities

When the cost of putting people on Mars drops to an affordable range, there will be no shortage of people wanting to go there to build a new world: Life on Mars to become a reality in 2023, Dutch firm claims: Thousands apply to become one of four astronauts selected to set up a human colony in a plan that comes with snags – guardian.co.uk.

Regarding the effects of living for a long period in gravity that’s 38% of that on earth, we don’t know the effects. The only data on fractional gravity is from the Apollo astronauts that spent a few days on the Moon and this was too short a time to have any effect.

To answer such questions, the Space Studies Institute has proposed the G-Lab, a rotating tethered habitat system for doing long term animal studies at different gravity strengths.

For a Mars settlement plan, it is not unreasonable to make the working assumption that it would be too dangerous to attempt to re-adapt to earth. However, my guess is that it will in fact be quite possible for a long term Mars resident to adapt to Earth’s gravity. The fundamental physical capacity to withstand that level of gravity will remain and can be retrained.

Ultimately, it would make sense to have a transport system traveling from Mars to Earth to provide rotation to generate spin gravity. This would allow for the gravity to be gradually increased from 0.38g to 1.0g over the course of the months long trip and allow passengers to gradually adapt to Earth conditions.

The Space Show: Chuck Killian and the Mars Desert Research Station

Chuck Killian of the Mars Society came to the Space Show on Friday and talked about the Mars Desert Research Station in Utah where they have been simulating Mars missions for ten years: Charles (Chuck) Killian, Friday, 4-26-13 | Thespaceshow’s Blog.

Space on the John Batchelor Show: Bob Zimmerman and Hotel Mars – April 23-25

Bob Zimmerman reports on the latest space news during regular weekly slots (usually Tuesday and Thursdays) on the John Batchelor radio program. See the iTunes free Podcast for links to the latest shows.

Tuesday 04/23/13 Batchelor Hour 3 

  • Antares success
  • SpaceX grasshopper success
  • Virgin Galactic space tourism success.

Thursday 04/25/13 Batchelor Hour 4

  • Russian Progress cargo spacecraft’s antenna problem
  • Apophis and the keyhole
  • Cassini sees meteoroids hitting Saturn’s rings
  • Climate change prediction misses

===

Wednesday 04/24/13 Batchelor Hour 1
The weekly Hotel Mars segment this week with David Livingston included guest William Borucki of NASA who talked about the recent discovery by the Kepler space observatory of exoplanets in the habitable zone of their stars.

Update April.29.13: I missed this in my earlier scan of the JBS programs last week. I see that my friend Jeff Foust of The Space Review   (+ spacetoday.net, Space Politics, and NewSpace Journal) spoke on the John Batchelor Show last Tuesday 04/23/13 about the Chelyabinsk fireball event.

Budget moon flights and a SSTO Ariane

Robert Clark on his blog Polymath ponders ideas for Budget Moon flights and Budget Moon flights with a lightweight crew capsule.

He also looks at converting an Ariane 6 design into a single-stage-to-orbit vehicle: The Coming SSTO’s: multi-Vulcain Ariane.

Cassini spots meteoroids hitting Saturn’s rings

The latest discovery by Cassini:

NASA Probe Observes Meteors Colliding With Saturn’s Rings

PASADENA, Calif. — NASA’s Cassini spacecraft has provided the first direct evidence of small meteoroids breaking into streams of rubble and crashing into Saturn’s rings.

These observations make Saturn’s rings the only location besides Earth, the moon and Jupiter where scientists and amateur astronomers have been able to observe impacts as they occur. Studying the impact rate of meteoroids from outside the Saturnian system helps scientists understand how different planet systems in our solar system formed.

The solar system is full of small, speeding objects. These objects frequently pummel planetary bodies. The meteoroids at Saturn are estimated to range from about one-half inch to several yards (1 centimeter to several meters) in size. It took scientists years to distinguish tracks left by nine meteoroids in 2005, 2009 and 2012.

Details of the observations appear in a paper in the Thursday, April 25 edition of Science.

Results from Cassini have already shown Saturn’s rings act as very effective detectors of many kinds of surrounding phenomena, including the interior structure of the planet and the orbits of its moons. For example, a subtle but extensive corrugation that ripples 12,000 miles (19,000 kilometers) across the innermost rings tells of a very large meteoroid impact in 1983.

“These new results imply the current-day impact rates for small particles at Saturn are about the same as those at Earth — two very different neighborhoods in our solar system — and this is exciting to see,” said Linda Spilker, Cassini project scientist at NASA’s Jet Propulsion Laboratory in Pasadena, Calif. “It took Saturn’s rings acting like a giant meteoroid detector — 100 times the surface area of the Earth — and Cassini’s long-term tour of the Saturn system to address this question.”

The Saturnian equinox in summer 2009 was an especially good time to see the debris left by meteoroid impacts. The very shallow sun angle on the rings caused the clouds of debris to look bright against the darkened rings in pictures from Cassini’s imaging science subsystem.

“We knew these little impacts were constantly occurring, but we didn’t know how big or how frequent they might be, and we didn’t necessarily expect them to take the form of spectacular shearing clouds,” said Matt Tiscareno, lead author of the paper and a Cassini participating scientist at Cornell University in Ithaca, N.Y. “The sunlight shining edge-on to the rings at the Saturnian equinox acted like an anti-cloaking device, so these usually invisible features became plain to see.”

Tiscareno and his colleagues now think meteoroids of this size probably break up on a first encounter with the rings, creating smaller, slower pieces that then enter into orbit around Saturn. The impact into the rings of these secondary meteoroid bits kicks up the clouds. The tiny particles forming these clouds have a range of orbital speeds around Saturn. The clouds they form soon are pulled into diagonal, extended bright streaks.

“Saturn’s rings are unusually bright and clean, leading some to suggest that the rings are actually much younger than Saturn,” said Jeff Cuzzi, a co-author of the paper and a Cassini interdisciplinary scientist specializing in planetary rings and dust at NASA’s Ames Research Center in Moffett Field, Calif. “To assess this dramatic claim, we must know more about the rate at which outside material is bombarding the rings. This latest analysis helps fill in that story with detection of impactors of a size that we weren’t previously able to detect directly.”

The Cassini-Huygens mission is a cooperative project of NASA, the European Space Agency and the Italian Space Agency. NASA’s Jet Propulsion Laboratory, Pasadena, Calif., a division of the California Institute of Technology, Pasadena, manages the Cassini-Huygens mission for NASA’s Science Mission Directorate in Washington. JPL designed, developed and assembled the Cassini orbiter and its two onboard cameras. The imaging team consists of scientists from the United States, England, France and Germany. The imaging operations center is based at the Space Science Institute in Boulder, Colo.

For images of the impacts and information about Cassini, visit: http://www.nasa.gov/cassini and http://saturn.jpl.nasa.gov .

Meteors Meet Saturn's Rings - NASA

Meteors Meet Saturn’s Rings

Five images of Saturn’s rings, taken by NASA’s Cassini spacecraft between 2009 and 2012, show clouds of material ejected from impacts of small objects into the rings. Clockwise from top left are two views of one cloud in the A ring, taken 24.5 hours apart, a cloud in the C ring, one in the B ring, and another in the C ring. Arrows in the annotated version point to the cloud structures, which spread out at visibly different angles than the surrounding ring features.

The clouds of ejected material were visible because of the angle sunlight was hitting the Saturn system and the position of the spacecraft. The first four images were taken near the time of Saturn equinox, when sunlight strikes the rings at very shallow angles, nearly directly edge-on. During Saturn equinox, which occurs only every 14.5 Earth years, the ejecta clouds were caught in sunlight because they were elevated out of the ring plane. The last image was taken in 2012 at a very high-phase angle, which is the sun-Saturn-spacecraft angle. This geometry enabled Cassini to see the clouds of dust-sized particles in the same way that dust on a surface is easier to see when the viewer is looking toward a light source.

The angle that the clouds are canted gives the time elapsed since the cloud was formed (see PIA14941). The A ring cloud formed 24 hours before its first apparition in the top left box; it formed 48.5 hours before the top middle image. The other three clouds were approximately 13 hours, four hours, and one hour old (respectively) at the times they were seen. See PIA11674 for more information on ring impacts.

The Cassini-Huygens mission is a cooperative project of NASA, the European Space Agency and the Italian Space Agency. The Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the mission for NASA’s Science Mission Directorate, Washington, D.C. The Cassini orbiter and its two onboard cameras were designed, developed and assembled at JPL. The imaging operations center is based at the Space Science Institute in Boulder, Colo.

For more information about the Cassini-Huygens mission visit http://www.nasa.gov/cassini and http://saturn.jpl.nasa.gov.

Everyone can participate in space