Previously "Lost" Lunokhod 1 Found

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Previously "Lost" Lunokhod 1 Found

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Link:
UC San Diego Physicists Locate Long Lost Soviet Reflector on Moon

April 26, 2010

By Kim McDonald

A team of physicists led by a professor at UC San Diego has pinpointed the location of a long lost light reflector left on the lunar surface by the Soviet Union nearly 40 years ago that many scientists had unsuccessfully searched for and never expected would be found.

The French-built laser reflector was sent aboard the unmanned Luna 17 mission, which landed on the moon November 17, 1970, releasing a robotic rover that roamed the lunar surface and carried the missing laser reflector. The Soviet lander and its rover, called Lunokhod 1, were last heard from on September 14, 1971.

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(Rover Parking Spot): The Lunokhod 1 rover in its final parking spot on the moon.
Credit: NASA/GSFC/Arizona State U.


“No one had seen the reflector since 1971,” said Tom Murphy, an associate professor of physics at UCSD. He heads a team of scientists engaged in a long-term effort to look for deviations of Einstein’s theory of general relativity by measuring the shape of the lunar orbit to within an accuracy of one millimeter, or about the thickness of a paperclip. This is accomplished by timing the reflections of pulses of laser light from reflectors left on the moon by Apollo astronauts and turning the timing measurement into a distance.

“We routinely use the three hardy reflectors placed on the moon by the Apollo 11, 14 and 15 missions,” said Murphy, “and occasionally the Soviet-landed Lunokhod 2 reflector—though it does not work well enough to use when illuminated by sunlight. But we yearned to find Lunokhod 1.”

Three reflectors are required to lock down the orientation of the moon. A fourth adds information about tidal distortion of the moon, and a fifth enhances that information.

Image

(Soviet Rover) The Soviet Lunokhod rovers were about 2.3 meters long and 1.5 meters tall.

“Lunokhod 1, by virtue of its location, would provide the best leverage for understanding the liquid lunar core, and for producing an accurate estimate of the position of the center of the moon—which is of paramount importance in mapping out the orbit and putting Einstein’s gravity to a test,” said Murphy.

Murphy said his team had occasionally looked for the Lunokhod 1 reflector over the last two years, but faced tall odds against finding it until recently. The breakthrough came last month when the high-resolution camera on NASA’s Lunar Reconnaissance Orbiter, or LRO, obtained images of the landing site. The camera team, led by Mark Robinson at Arizona State University, identified the rover as a sunlit speck on the image—miles from where Murphy and his team had been searching. (see: http://www.nasa.gov/mission_pages/LRO/m ... 00318.html ) But until now the existence of the reflector or its precise location was unknown.

“It turns out we were searching around a position miles from the rover,” said Murphy. “We could only search one football-field-sized region at a time. The recent images from LRO, together with laser altimetry of the surface, provided coordinates within 100 meters, and then we were in business and only had to wait for time on the telescope in good observing conditions.”

On April 22, his team sent pulses of laser light from the 3.5 meter telescope at the Apache Point Observatory in New Mexico, zeroing in on the target coordinates provided by the LRO images. Murphy, together with Russet McMillan of the Apache Point Observatory in Sunspot, NM, and UCSD physics graduate student Eric Michelsen found the long lost Lunokhod 1 reflector and pinpointed its distance from earth to within one centimeter. They then made a second observation less than 30 minutes later that allowed the team to triangulate the reflector’s latitude and longitude on the moon, in other words its exact spot on the moon, to within 10 meters—“not bad for a half-hour’s work,” said Murphy. In the coming months, he estimates it will be possible to establish the reflector’s coordinates to better than one-centimeter precision.

The return signal from the reflector was measured by Murphy’s team as a collection of individual particles, or photons, of laser light.

“We quickly verified the signal to be real and found it to be surprisingly bright: at least five times brighter than the other Soviet reflector, on the Lunokhod 2 rover, to which we routinely send laser pulses,” Murphy said. “The best signal we’ve seen from Lunokhod 2 in several years of effort is 750 return photons, but we got about 2,000 photons from Lunokhod 1 on our first try. It’s got a lot to say after almost 40 years of silence.”

Image

(Apollo) Laser beams are sent to reflectors on the moon from a telescope in New Mexico.
Credit: Dan Long, Apache Point Observatory


The discovery of the Soviet reflector came as a surprise, because scientists had actively searched for it for nearly four decades without success. Many scientists had speculated that the Lunokhod 1 rover might have fallen into a crater or parked badly, with its reflector not facing the earth, which would have prevented it from being located by laser pulses.

“Not only now do we know that Lunokhod 1 is there, we also know that it is parked perfectly so that its reflector faces earth,” said Murphy. “In fact, the signal is so surprisingly strong that the rover could not be in anything but a level parking spot with its last commanded roll on the lunar surface deliberately oriented toward the earth.”

Murphy and his colleagues found in a study they published this month that lunar dust may be obscuring the reflectors on the moon. see: Moon Dust His team found that the laser light they bounce off reflectors on the moon is fainter than expected and dims even more whenever the moon is full.

“Near full moon, the strength of the returning light decreases by a factor of ten,” he adds. “We need to understand what is causing this if we are contemplating putting additional scientific equipment on the moon. Finding the Lunokhod 1 reflector will add important clues to this study.”

Murphy’s project, dubbed APOLLO (the Apache Point Observatory Lunar Laser-ranging Operation), is supported by the National Science Foundation and NASA, and includes scientists at the University of Washington, Harvard University, the Massachusetts Institute of Technology, Humboldt State University and the Apache Point Observatory.
I tired to find a Russian news story on this and all I could find was an article on the English Pravda site from February which seemed very concerned and unsure why NASA was "Desperately" looking for the rover and its mirror, even though the answer is self-evident and is in the article itself. :lol:

Anyway, interesting stuff.
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Re: Previously "Lost" Lunokhod 1 Found

Post by PeZook »

Hah!

The LRO mission just keeps paying back. It already returned enough data for another half a century of analysis, easily. I wonder what other interesting things we'll learn about the Moon when more science teams get their cracks at the data?
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Re: Previously "Lost" Lunokhod 1 Found

Post by Coyote »

PeZook wrote:I wonder what other interesting things we'll learn about the Moon when more science teams get their cracks at the data?
Hmmm, how about... a Magnetic Field Region found on Moon (MSNBC) :D

This is interesting:
Magnetic refuge found on Moon
A mini magnetic field has been detected on the surface of the moon

By Larry O'Hanlon

updated 12:39 p.m. MT, Tues., April 27, 2010
A miniature magnetic field has been imaged on the surface of the moon, making it a rare, minimally protective lunar refuge from some aspects of the harsh solar wind.

The magnetic region could be a great place to site a lunar base, since tomorrow's lunar colonists will not only need water (check!), but some protection from the heavy radiation in the solar wind.

"You can think of it as kind of a mini umbrella," said Martin Wieser of the Swedish Institute of Space Physics in Kiruna, Sweden. "It will be effective for certain kinds of (space) weather."

But it is very weak in comparison to Earth's planet-wide magnetic field or even compared to the splotchy magnetospheres of Mars.

The 224-mile- (360-kilometer-) wide magnetosphere was detected by an instrument on the Indian Chandrayaan-1 spacecraft. The mini magnetosphere revealed itself by fewer hydrogen atoms scattering off the surface of the moon. Generally when the solar wind rams into the airless surface of the moon, some hydrogen atoms scatter back into space. Any place with fewer of these atoms rising up from the moon is likely to be shielded magnetically, explained Wieser and his colleagues in their paper published in Geophysical Research Letters.

The researchers also noticed that the dust inside the magnetically shielded zone is brighter than the surrounding areas, which might have something to do with the solar wind weathering that surface differently over the eons.

"I think this is a very exciting observation," said lunar researcher Jasper Halekas of the Space Science Laboratory at the University of California at Berkeley. "There have been a number of indications that theses things were taking place. (But) this is the first directed study that really tells you 'they are there.'"

The lunar magnetospheres are a lot like those on Mars, said Halekas, except that on Mars they are almost certainly the remnants of a global magnetic field that was created by the planet's core. A molten core dynamo on the moon is a bit less likely, however.

"It's still quite possible that there was a dynamo on the moon," said Halekas.

Another possibility is that the mini-magnetosphere was generated by large impacts on the direct opposite side of the moon. Exactly how this works is far from clear, but there does seem to be a correlation between large impact craters and magnetic anomalies at their antipodes, said Wieser.

Ironically, the same magnetic shielding could make these the driest places on the moon. One mechanism believed to generate at least the ingredients for water on the moon are solar protons smacking into the surface, forming hydrogen atoms in the lunar soils. Inside a mini magnetosphere that is less likely to happen, Wieser noted.

Without water, maybe this isn't the best lunar real estate after all.
True, it would be easier to locate a science station near water and just bury it under regolith for shielding, a station here to study the effects would be interesting. It could probably be automated, no need for a manned lab at the site that would require shlepping ice to them.

We're finding out all kinds of cool stuff about the Moon these days.
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