Yutu still operational after two years

Despite an inability to move, China’s rover Yutu has now set the longevity operational record for rover on the Moon.

Yutu was deployed and landed on the moon via China’s Chang’e-3 lunar probe in 2013, staying longer than the Soviet Union’s 1970 moon rover Lunokhod 1, which spent 11 months on the moon. Its operations have streamed live through Sina Weibo, a Chinese microblogging site, and its Weibo account has nearly 600,000 followers.

Yutu experienced a mechanical control abnormality in 2014, but it was revived within a month and, though it is unable to move, it continues to collect data, send and receive signals, and record images and video.

200 new lunar impact craters discovered

In a paper [pdf] presented this week at a lunar science conference, scientists announced the identification of more than 200 new impact craters on the Moon from Lunar Reconnaissance Orbiter (LRO).

As of 1 May 2015, we have scanned and classified changes in 14,182 NAC temporal pairs using our automated change detection tool leading to the discovery over 200 impact craters ranging in size from 1.5 to 43 m. In addition, we also identified thousands of other surface changes, including about 44,000 low reflectance splotches, 3,500 high reflectance splotches, 850 mixed reflectance splotches, [and] 1 Chinese lander/rover.

They think the splotches are created from impacts too small to see with LRO.

Hat tip James Fincannon.

Study questions scientific dating method

The uncertainty of science: A new study has raised questions about the methods scientists have used to date the late heavy bombardment in the early solar system.

A study of zircons from a gigantic meteorite impact in South Africa, now online in the journal Geology, casts doubt on the methods used to date lunar impacts. The critical problem, says lead author Aaron Cavosie, a visiting professor of geoscience and member of the NASA Astrobiology Institute at the University of Wisconsin-Madison, is the fact that lunar zircons are “ex situ,” meaning removed from the rock in which they formed, which deprives geoscientists of corroborating evidence of impact. “While zircon is one of the best isotopic clocks for dating many geological processes,” Cavosie says, “our results show that it is very challenging to use ex situ zircon to date a large impact of known age.”

The problem is that the removal of the zircon from lunar rocks changes the data enough to make the dating unreliable. The method might work on Earth, but the dating done on Apollo samples can be questioned. This means that much of the supposed history of the solar system, centered on what planetary scientists call the late heavy bombardment, a period 4 billion years ago when the planets were being hit by innumerable impacts as they cleared the solar system of its dusty debris disk, might not have happened as dated from lunar samples. If so, our understanding of when that bombardment ended and life began to form on Earth might be considerably incorrect.

The solution? Get to the planets in person, where you can obtain many samples in situ and thus gather a much deeper understanding of the geology.

Russian lunar mission delayed again

The Russian Luna-Glob has been delayed again, partly due to embargoes imposed by the Ukraine war, and partly due to a lack of money.

The article notes that Russia’s participation in the European ExoMars project has left little resources for this lunar mission, causing delays. It also notes the possibility that the second mission in ExoMars, scheduled for 2018, might be delayed as well. (The first ExoMars mission is scheduled to launch next year.)

All-in-all, this story indicates to me that the Russians continue to have serious underlying financial and management problems throughout their society. Having lost faith in capitalism, after 20 years of not really doing it right, they have returned to a soviet-style big government top-down approach. I doubt it will solve their problems.

Another Google Lunar X-Prize contestant announces launch contract

The competition heats up: Another Google Lunar X-Prize team, SpaceIL, has announced the signing of a launch contract, this time as a secondary payload on a Falcon 9 launch in the latter half of 2017.

Their press release says they are the first to produce an actual contract to the contest, which only means the Moon Express contract hasn’t yet been delivered.

This two launch contracts suggest that the competition for the X-Prize will get interesting in 2017. As a secondary payload, SpaceIL will not be able to schedule its launch. And while Moon Express, as a primary payload on smallsat rocket, can schedule its launch, it is depending on a new untried rocket, Electron, being developed by a new untried rocket company, Rocket Labs.

And since SpaceIL is an Israeli company, be prepared for some Muslim and leftwing heads to explode should it win the X-Prize. How dare they oppress those Palestinians by getting their rover to the Moon first!

Moon Express buys launch contract

The competition heats up: The leading private effort to win the Google Lunar X-Prize, Moon Express, has signed a contract with the smallsat launch company Rocket Labs for three launches.

Mountain View, California-based Moon Express plans to use the launches to send to the moon new, smaller versions of its MX-1 lunar lander. Two of the launches will take place in 2017, with a third to be scheduled. All three will use Rocket Lab’s Electron small launch vehicle, whose first flight is scheduled for no earlier than late 2015 from New Zealand. – See more at: http://spacenews.com/moon-express-buys-rocket-lab-launches-for-lunar-missions/#sthash.J1hEuCp3.dpuf

Rather than piggyback on the major launch of big payload, which would deny them any control over launch dates, they have signed with a new and as yet unproved small rocket company. The result? Not only do we have the chance of getting our first privately built lander on the Moon, the contract jumpstarts a new rocket company designed to put small payloads into space.

Apollo lunar samples crumbling to dust

The uncertainty of science: A comparison between the average particle size of 20 Apollo moon soil samples has discovered that their size has decreased by more than half in the past 40 years.

The differences between the two datasets are stark. For example, the median particle diameter has decreased from 78 microns (0.0031 inches) to 33 microns (0.0013 inches). And in the original sieve data, 44 percent of soil particles were between 90 and 1,000 microns (0.0035 to 0.039 inches) wide; today, just 17 percent of the particles are that large.

The most likely explanation for the degradation is damage caused by water vapor, the scientists say. “Leaching by water vapor causes the specific surface area of a lunar soil sample to multiply, and a system of pores develops,” they wrote in the study, which was published online last week in the journal Nature Geoscience. “These structural changes may be attributed to the opening of existing, but previously unavailable, pore structure or the creation of new surfaces through fracturing of cement or dissolution of amorphous particles.”

I was surprised that in the article above the scientists made no mention of gravity as a factor. These particles were originally formed under lunar gravity, 1/6 that of Earth. I would have thought that their structural strength was partly determined by this, and once brought to Earth’s heavier gravity would have thus slowly deteriorated over time.

Either way, the study illustrates why saving these samples for future researchers was a foolish mistake. Time changes all things, and that change has made these samples no longer a good representation of the Moon. The NASA scientists and managers who decided to store these samples instead of distributing them all for immediate study forgot this basic fact.

The scientists who did this study appear to have not learned this lesson as well. They suggest future samples be stored off-Earth, in a place like ISS. I say, we should instead go to the Moon so often we don’t need to store any samples. When we want a sample, we go and get one.

Shake-ups in the Google Lunar X-Prize competition

One team has withdrawn and two big-name executives have left another team in a shake-up at the Google Lunar X-Prize competition.

This key quote however tells us the real state of the competition, which sadly does not look good:

The competition has repeatedly moved back the deadline to win the prize, which is now set for Dec. 31, 2017. At least one of the 16 remaining teams much announced a launch contract by the end of this year for the competition to continue. The rest of the teams would then have until the end of 2016 to announce launch contracts to stay in the race.

The team that withdrew says it plan to continue its effort but outside the competition. Either way, it looks like someone has to commit to a launch sometime in the next few months or the competition either has to push back its deadlines again or declare no winners. This will be a sad conclusion, as it is entirely possible for private financing to get this done. A failure however would make that appear impossible.

Cubesats to the Moon!

NASA has chosen three cubesat missions to fly lunar planetary orbiters to the Moon, to be launched on the first SLS flight in 2018.

LunaH-Map, along with a number of other deep-space CubeSats, is a candidate to fly to lunar orbit on Exploration Mission-1, the first flight of NASA’s Space Launch System (SLS), which will be the most powerful rocket ever built and will enable astronauts in the Orion spacecraft to travel deeper into the solar system. NASA will provide several CubeSat missions spots on the maiden SLS mission. LunaH-Map is a 6U (“6 unit”) CubeSat. One “unit” is a cube measuring 4.7 inches on a side; LunaH-Map strings six of these CubeSat building blocks together and weighs as much as a small child (about 30 pounds). …

“NASA has funded three different CubeSats to learn more: Lunar IceCube, Lunar FLASHLIGHT and LunaH-Map. They all look for water in different ways and provide different types of information,” [said principal investigator Craig Hardgrove].

The article is focused on LunaH-Map, not on the other two cubesats, but the fact that NASA plans to use “the most powerful rocket ever built” to launch the first three planetary cubesats, so small they could almost be launched by a model rocket, illustrates some of the problems of the SLS program. Even though that first SLS flight is likely to happen, I suspect that, should it falter for any reason (something that would not surprise me), these cubesats could easily be launched on another rocket, and will be.

Putting SLS aside, however, the building of these first planetary cubesats is a very significant development. It once again signals the way unmanned satellite engineering is evolving, finding ways to build spacecraft smaller and less costly.

Russia to do all-female simulated Moon mission

The competition heats up: The Institute of Biomedical Problems in Moscow has announced plans to do an all-female eight day simulated mission to the Moon.

Currently scheduled for October-November 2015, the experiment will differ from the Mars-500 venture not just in duration but most notably in crew composition. For Moon-2015, all the participants will be women, drawn from the staff at IBMP itself.

In their July announcement, IBMP named the ten volunteers from whom the actual crew will be chosen. All have strong scientific, medical or research backgrounds and many have worked in the space or aviation medicine sphere, working closely with cosmonauts before or after visits to the International Space Station (ISS).

The Institute’s focus is medical, so the goal is not to develop engineering to get to the Moon but to study the human body and how it reacts to living in a spacecraft environment. In this case, they can’t simulate weightlessness so the only thing they can study is how the crew interacts with each other in a confined space for a period of time.

Audi joins race to the Moon

The competition heats up: The carmaker Audi has joined one of the teams competing for the Google Lunar X-Prize.

Audi’s part in the project will be to supply technical know how though its Audi Concept Design Studio, including the application of its quattro all-wheel drive technology and its experience in lightweight construction, electric mobility, and piloted driving. The company says it will also help in testing, trials, and quality assurance.

The rover, now named the “Audi lunar quattro,” is scheduled to launch sometime in 2017 and is aimed at a landing zone north of the lunar equator somewhere near 1972 Apollo 17 mission landing site, through the law prevents the rover from actually visiting it because it’s a protected area. “The concept of a privately financed mission to the moon is fascinating,” says Luca de Meo, Audi Board Member for Sales and Marketing. “And innovative ideas need supporters that promote them. We want to send a signal with our involvement with the Part‑Time Scientists and also motivate other partners to contribute their know‑how.”

I should note that the article is wrong when it states “the law prevents the rover from actually visiting” the Apollo 17 site. This law was passed by the U.S. Congress, and this Google team and Audi are not based in the U.S. They are not under its jurisdiction.

Furniture for space!

Students at Rice University have built a chair and table expressly designed for use in a low gravity environment like the Moon or Mars.

The students interviewed astronauts to get an idea of what was needed, and did the design under NASA supervision. Their design is clever in that it can be packed easily, but I still wonder about the weight of transport. I don’t see the first explorers to Mars being able to afford bringing their furniture with them. I expect they will instead figure out ways to improvise chairs and tables from the materials on hand.

Japan to the moon!

The competition heats up: Japan’s space agency has announced plans to send an unmanned lander to the Moon, as early as 2018, as part of a longer range plan to explore Mars.

They also intend to use their new Epsilon rocket to launch it.

Gee, I wonder if the successful efforts of India and China to send probes to both the Moon and Mars had some influence on this decision.

New studies struggle to explain the origin of the Moon

The uncertainty of science: Three new studies on the mystery of the origin of the Moon all appear to better confirm the theory that it was created when the Earth collided with a Mars-sized planet.

It is important to be aware of the uncertainties here. All these studies were done to try to address problems with the impact theory, and though they kind of answer the questions, they leave behind some important doubts.

Did the Moon’s axis shift 3.5 billion years ago?

The uncertainty of science: Because the concentrations of ice on the moon are thought to be located on opposite sides of the planet, both locations 5.5 degrees away from the poles, a team of scientists has proposed that these locations were once the Moon’s poles and that the axis got shifted 3.5 billion years ago when a gigantic volcanic hotspot on the surface erupted.

He and his colleagues assumed that when the ice was deposited, it was centered on the poles. But what kind of event could have moved the poles by 5.5°? Known asteroid impacts were too small or in the wrong location to do the job. Instead, the team hypothesizes that a 3.5-billion-year-old hot spot could have nudged the poles to their present-day position. Pouring out enormous amounts of lava, that hot spot created Oceanus Procellarum, the vast dark spot on the near side of the moon. The Procellarum region is known to have high concentrations of radioactive elements that would have been hot in ancient times. The research team theorizes that this heat would have created a less dense lens in the moon’s mantle that would have caused the axis to wobble into today’s position.

This theory requires that the Moon’s ice is at least this old, which is quite a stretch. Also, if the Procellarum eruption caused a pole shift, I wonder why the other large lunar eruptions, which created the Moon’s other mare, did not shift the poles further and in other directions.

Giant lava tubes possible on the Moon

New analysis of the lunar geology combined with gravity data from GRAIL now suggests that the Moon could harbor lava tubes several miles wide.

David Blair, a graduate student in Purdue’s Department of Earth, Atmospheric and Planetary Sciences, led the study that examined whether empty lava tubes more than 1 kilometer wide could remain structurally stable on the moon. “We found that if lunar lava tubes existed with a strong arched shape like those on Earth, they would be stable at sizes up to 5,000 meters, or several miles wide, on the moon,” Blair said. “This wouldn’t be possible on Earth, but gravity is much lower on the moon and lunar rock doesn’t have to withstand the same weathering and erosion. In theory, huge lava tubes – big enough to easily house a city – could be structurally sound on the moon.”

You can read their paper here. If this is so, then the possibility of huge colonies on the Moon increases significantly, as it will be much easier to build these colonies inside these giant lava tubes.

An iron rain fell on Earth early in its formation

New research attempting to explain why the Earth but not the Moon has so much iron splattered through its mantle has found that iron can be more easily vaporized during impacts than previously thought, and thus rained down on the planet during the early asteroid bombardment.

Principal investigator Kraus said, “Because planetary scientists always thought it was difficult to vaporize iron, they never thought of vaporization as an important process during the formation of the Earth and its core. But with our experiments, we showed that it’s very easy to impact-vaporize iron.” He continued, “This changes the way we think of planet formation, in that instead of core formation occurring by iron sinking down to the growing Earth’s core in large blobs (technically called diapirs), that iron was vaporized, spread out in a plume over the surface of the Earth and rained out as small droplets. The small iron droplets mixed easily with the mantle, which changes our interpretation of the geochemical data we use to date the timing of Earth’s core formation.”

The Moon’s gravity in turn wasn’t sufficient to pull its own iron vapor down. Thus, it does not have much iron in its mantle.

Yutu reveals a complex lunar geology

The uncertainty of science: The Chinese lunar rover Yutu has uncovered a much more complicated geology history than previously predicted at its landing site on the moon.

Those data paint a detailed portrait of the Chang’e 3 landing site, which sits just 165 feet (50 m) away from a 1,475-foot-wide (450 m) crater known as C1. C1 was gouged out by a cosmic impact that occurred sometime between 80 million and 27 million years ago, the study authors said.

Yutu studied the ground it rolled over, characterized the craters it cruised past and investigated an oddly coarse-textured rock dubbed Loong, which measures about 13 feet long by 5 feet high (4 by 1.5 m). Overall, the rover’s observations suggest that the composition of its landing site is quite different from that of the places visited by NASA’s Apollo missions and the Soviet Union’s Luna program.

The rover found 9 distinct layers, suggesting numerous and different past events that layered the surface.

Yutu lives!

Despite an engineering failure that has prevented it from roving after only a few days on the Moon, the Chinese lunar rover Yutu continues to reawaken after each long lunar night, surviving now far longer than its planned three month lifespan.

Since the rover arrived in late 2013, it has now functioned in the hostile lunar environment for more than a year. This, along with other successful long missions, suggests that Chinese space engineering has matured to a point that it has the ability to achieve some significant long term goals.

Earth’s other moon

Link here.

What you might not know is that the moon is not the Earth’s only natural satellite. As recently as 1997, we discovered that another body, 3753 Cruithne, is what’s called a quasi-orbital satellite of Earth. This simply means that Cruithne doesn’t loop around the Earth in a nice ellipse in the same way as the moon, or indeed the artificial satellites we loft into orbit. Instead, Cruithne scuttles around the inner solar system in what’s called a “horseshoe” orbit.

X-Prize contestants team-up to create head-to-head lunar race

The competition heats up: Two Google Lunar X-Prize contestants have teamed up to use the same rocket to get to the Moon together, where they will literally race head to head to see who travels the 500 meter distance first to win the prize.

At a press conference in Tokyo on Monday, the leaders of two Lunar X PRIZE teams—Astrobotic and HAKUTO—announced a plan in which the two teams’ robotic rovers will travel to the moon together and touch down on the lunar surface at the same time. They will then race each other to cover the 500 meters required to win the first place prize of $20 million.

John Thornton, head of Pittsburgh-based Astrobotic (a Carnegie Mellon University spin-off), said in a call with reporters that the partnership with HAKUTO (a spin-off from Tokyo University) represented the first step in realizing his team’s goal of turning robotic moon missions into a viable business. That mission won’t stop with this single partnership. He said the team was in talks with more than half of the other 16 GLXP competitors to carry their rovers to the moon, too, in exchange for sharing the cost of getting there and splitting prize money.

If this happens as they propose, we could be watching as many as ten rovers line up for the race.

South Korea unveils its own lunar rover

The competition heats up: South Korea has revealed its preliminary design for a lunar rover, set to launch in 2020 on a Korean-built rocket.

The article does not indicate whether this project has actually been approved or is merely being touted by Korea Institute of Science and Technology, which made the announcement. The cost to build it is estimated to be more than $7 billion, which seems quite exorbitant and over-priced.

Update: I had misread the conversion in the article from U.S. to Korean currency and thought the proposed cost for this mission was way more than it really is, which is about $7 million, a much more reasonable number. Thanks to Edward for the correction.

Private company offers to fly packages to Moon

Fly me to the moon! A company building a small lunar rover as part of the Google Lunar X-prize competition is now offering, for a small fee, to include private packages with its lander.

Astrobotic Technology on Thursday (Dec. 11) announced the launch of its new “MoonMail” program, which offers to send heirloom rings, family photos, locks of hair and other small personal items on the company’s first private moon mission set to launch in the next few years. With prices based on the item’s size, MoonMail rates start at $460 for a half-inch wide by 0.125-inch tall (1.27 by 0.3 centimeter) capsule and increase to $25,800 for a one by two-inch (2.54 by 5.08 cm) payload. “You can think of the pricing for it to be very similar to ‘it fits, it ships’ at the post office,” John Thornton, Astrobotic CEO, told collectSPACE.com in a call with reporters. “It is essentially a flat-rate box.”

They hope to launch on a Falcon 9. More interestingly, they want to land and explore one of the Moon’s skylight caves.

The first Griffin is slated to launch on a SpaceX Falcon 9 rocket and land at Lacus Mortis, or the “Lake of Death,” a plain of basaltic lava flows in the northeastern part of the moon as viewed from Earth. “There is a unique feature there called a ‘skylight,'” stated Thornton, adding that only about 300 of these sinkhole-like entrances into subsurface caves have been discovered on the moon. “What’s very unique about the skylight at Lacus Mortis is that its walls have collapsed creating a ramp into the cave. … Caves on the surface of the moon could be our natural shelter,” Thornton explained. “So our first mission goes to one of these caves where we hopefully think someday we could settle on the moon. We think it’s a fantastic location to place MoonMail, which ultimately will be a time capsule of our generation for future moon explorers.”

Chinese spacecraft reaches L2

The service module for China’s test lunar probe, that circled the Moon before returning to Earth, has reached L2 as planned.

As of Friday, the service module had been flying for 28 days, and was 421,000 kilometers away from Earth and 63,000 km from the moon. All experiments are going well. The service module was separated from the return capsule of China’s test lunar orbiter, which returned to Earth on Nov. 1 after circling the moon in its eight-day mission launched on Oct. 24.

…After two orbital transfers, the service module re-entered the elliptical orbit with an apogee of 540,000 km and a perigee of 600 km. During the flight, the service module again performed orbital transfer actions twice, and flew along the pre-set Earth-moon transfer orbit. On Nov. 23, it reached the perilune and with the lunar gravity it was able to undertake the orbit maneuver to fly to the L2 point.

This is brilliant management. They not only test return-to-Earth capability, they practice flying a robot ship in deep space, doing complex orbital maneuvers. In addition, depending on the equipment on the service module, they get a cheap unmanned probe for observing the near lunar environment.

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