Aurion Mission

Monday, August 15, 2011

The Lost city, Atlantis massif and Serpentinization

 
Hand sample of a serpentinite from Lost City Serpentinites form when seawater reacts with peridotite - rocks that form the Earth's mantle and have been brought up to the seafloor by tectonic processes. This picture shows a hand sample of a serpentinite recovered from the Atlantis Massif. Thin fractures in the serpentinite are filled with calcium carbonate. Sample is 16cm wide. Click image for larger view and image credit. (HR)

The The Lost City 2005 Expedition

Gretchen Früh-Green
Senior Research Scientist
Department of Earth Sciences
ETH-Zurich, Switzerland

What Drives Hydrothermal Activity at Lost City?

The chemistry of the vent fluids and fluid circulation at Lost City are not driven by interaction of seawater with hot lava or by cooling of magma at depth. Instead hydrothermal activity at Lost City is driven by chemical reactions between seawater and mantle rocks that make up the underlying basement. This is unlike almost all other known hot spring systems on the seafloor.
The mantle, or peridotite, rocks that comprise the Atlantis massif generally occur at much greater depths in the Earth - typically at depths greater than about 6 kilometers. Because of faulting these mantle rocks are now exposed at or near the seafloor and they are out of equilibrium with their surroundings. These rocks contain large amounts of the mineral olivine (a Mg-Fe silicate) which reacts with seawater at temperatures below 400°C and forms serpentine minerals (hydrous Mg-silicates) and magnetite, an iron oxide that is highly magnetic. This process, referred to as serpentinization, has major geophysical, geochemical and biological consequences for the marine system. It is a fundamental process at slow spreading ridge environments where mantle rocks are commonly exposed near the seafloor.
Photomicrograph of a serpentinite This photomicrograph shows a serpentinite in a polarizing petrographic microscope. During reaction with seawater serpentine (the grey, "snake-like" minerals) forms what is called a mesh texture around olivine grains. The light colored, round minerals are relict grains of olivine. Field of view is 2.5 mm. Click image for larger view and image credit. (HR)

Serpentinization: The Heat Engine at Lost City and Sponge of the Oceanic Crust

An important consequence of serpentinization is the production of heat. The process of serpentinization can provide heat to drive the Lost City hydrothermal system in two ways. First, the mantle rocks underlying Lost City have residual heat from the mantle that can be "mined" through cooling with seawater. A second important source of heat is the alteration reactions themselves, which are termed exothermic because they consume water and produce a significant amount of heat during the transformation of olivine to serpentine and magnetite. The amount of heat produced is directly proportional to the amount of water that is taken up to form the mineral serpentine. In fact, serpentinization consumes an average of about 300 kilograms (approximately 300 liters or 79 US gallons) of water per cubic meter of rock that is altered. At the same time, this process produces about 660,000,000 joules of heat per cubic meter of rock.
The geological significance of heat production is that serpentinization processes are capable of raising the rock temperature by about 260°C (550°F) when not including processes that lead to heat transport and cooling of the rock. It is this heat source that helps drive the Lost City hydrothermal system. This is in strong contrast to other known hydrothermal systems along the mid-ocean ridges which are driven by magmatic heat and are characterized by high temperature, metal-rich fluids that ultimately create spectacular "Black Smoker" sulfide structures.

Face Lifting through Serpentinization

Another important consequence of the formation of serpentine during hydration of mantle rocks is that the density of the rocks change from about 3.3 grams per cubic centimeter (g/cm3) to about 2.7 g/cm3 and the volume of the rocks can increase by 20-40%. Serpentinization also affects other geophysical properties of the oceanic crust by lowering the seismic velocities of the rocks, changing their gravity signatures and mechanical properties, and by increasing their degree of magnetism. The change in density and the expansion of the rocks during serpentinization has the important effect that the mountain becomes lighter and needs more room as it swells up, and thus "lifts" itself to greater elevations. The expansion of the rocks also leads to a greater number of cracks and ultimately causes mass wasting along steep slopes. This in turn creates new fractures that allow seawater to penetrate further into the mountain and react with new portions of rock that contain fresh olivine. Thus, the access of seawater to relatively cool fresh peridotite, controlled by the processes of faulting, volumetric expansion and mass wasting, is crucial to sustain Lost City-type systems.
Radiogenic carbon age dating of the carbonate structures and overlying sediments indicates that the Lost City hydrothermal system has been ongoing for at least 30,000 years. This is at least two orders of magnitude longer that most of the known black smoker systems. Geophysical data also suggests that there is a significant amount of fresh peridotite at depth in the massif that can still be altered, and thus the serpentinization processes in the basement rocks have the potential to drive the Lost City system for hundreds of thousands, if not millions, of years.
This illustration shows the Pacific plate in the east colliding with the Australian plate in the west. Serpentinized peridotites are the most dominant rock type recovered during past expositions on the south wall of the Atlantis Massif and form the basement of the Lost City hydrothermal vent field. This outcrop picture shows partially deformed rocks that occur at the top of the massif. The arm of the 3-person submersible Alvin is shown in the right portion of the image. Click image for larger view and image credit. (HR)

Creating a long-lived, gas-rich hydrothermal environment

Because the Atlantis Massif consist mostly of peridotite and have a distinctly different composition than basalts and slower cooled counterparts (i.e. gabbros), the fluids that circulate beneath Lost City have significantly different compositions than black smoker systems. During alteration of the mantle rocks beneath Lost City, the fluids become extremely basic and reach a pH of 9 to 11. This high pH is very important because when the Lost City fluids are expelled from the chimneys, they mix with seawater and trigger chemical reactions that cause calcium carbonate (CaCO3) and brucite [Mg(OH)2] to precipitate. As long as the Lost City fluids maintain a high pH, abundant limestone will continue to be deposited and the chimneys will continue to grow.
The formation of magnetite during the serpentinization process involves the oxidation of ferrous iron (Fe2+) in olivine to form ferric iron (Fe3+) in magnetite and leads to what is called reducing conditions. As a consequence, reduced gas species, such as hydrogen gas (H2), methane (CH4) and hydrogen sulfide (H2S), can be produced during serpentinization. These dissolved gas species provide important energy sources for microbial activity at Lost City. Thus, the basement rocks and the porous Lost City structures that are bathed volatile-rich, highly alkaline fluids create vital niches for life.
The gases produced at Lost City, the organisms that thrive in them and the long-lived nature of this serpentinite-driven system are very distinct from black-smoker hydrothermal vents and may represent a modern analog for some of the oldest hydrothermal systems on Earth. Thus, understanding this system may provide important new insights for studying early life on Earth as well as for looking for signs of life on other planets.

The Lost City Hydrothermal Field

http://www.lostcity.washington.edu/

Lost City, located 20 km west of the Mid-Atlantic Ridge, is characterized by extreme conditions never before seen in the marine environment: venting of pH 9-11, >90°C, metal-poor fluids from carbonate edifices that tower 60-m above the seafloor. Investigation of this remarkable system has forever changed our views about where and how life can thrive and survive on and in the seafloor and provided new models for the evolution of life on this earth and possibly elsewhere [Kelley et al., 2005]. This system is the longest-lived of any known venting environment in the worlds’ oceans with activity ongoing for at least 120,000 years. Investigations of this site were funded by the National Science Foundation and by the NOAA Ocean Exploration program.
Within the Atlantis Massif, a >14,000 foot tall mountain on which Lost City rests, fluid rock reactions in the ultramafic rocks result in alkaline fluids with high concentrations of abiogenically produced hydrogen, methane, and other low molecular weight hydrocarbons. In concert, these dissolved gases support novel microbial communities. The oxygen-free, interior zones of the chimneys harbor biofilms of a single type of archaea called Lost City Methanoscarcinales that utilizes methane in its metabolism. Bacteria related to CH4- and S-oxidizers, are mostly found in the oxygenated, outer walls of chimneys where fluid chemistry is substantially different than the chimney interiors [Brazelton et al., 2006].
The highly-sculpted, high-surface area of the Lost City structures provides ample space for faunal habitats, and many recovered invertebrates were located within the porous channels and crevices of the carbonate. Surprisingly, while total biomass is low within the field, the field supports a species diversity that appears to be as high as any other known black smoker system on the Mid-Atlantic Ridge spreading center.
The range and complexity of environments hosting peridotites and other ultramafic rocks within the worlds’ oceans is vast and it is unlikely that Lost City is unique. Perhaps the most far-reaching impact of the discovery Lost City-type is the realization that life itself may have originated within these dynamic environments in which geological, chemical, and biological processes are intimately linked.
characterized by extreme conditions never before seen in the marine environment

The serpentinite-hosted Lost City Hydrothermal Field is a remarkable submarine ecosystem in which geological, chemical, and biological processes are intimately interlinked
The Lost City Hydrothermal Field is located 15 km west of the spreading axis of the Mid-Atlantic Ridge at 30°N, near the summit of the Atlantis Massif. The relief of this mountain is similar to that of Mt Rainier, rising nearly 4000 m (>17,000 feet) above the seafloor over a horizontal distance of ~20 km. Unlike Mt Raininer, however, the Atlantis Massif is not formed by volcanic eruptions, but instead by extreme crustal extension during long-lived (1-2 my) faulting and uplift. In concert, these processes have resulted in stripping-off of shallow crustal volcanic material and exposure of magnesium-rich mantle rocks (peridotites).
The summit of the massif is capped by flat-lying sedimentary breccias overlain by fossiliferous pelagic limestone. This cap rock was likely important in formation of the field, acting as an impervious lid trapping both fluids and heat. The cap rock is underlain by a 50-100 m thick highly deformed zone that hosts variable altered ultramafic rocks (foliated serpentinite, talc-amphibole schists) and lesser gabbroic rocks. This shear zone is likely the long-lived detachment fault that exposed the mantle and lower crustal rock sequences that make up the massif. This zone grades downward into massive, jointed peridotite with lesser gabbroic rocks that are not highly deformed.
Lost City Hydrothermal Field lies atop the sedimentary cap rock, on a triangular, down-dropped block that forms a terrace on the edge of the south wall. The largest and most active vents are along an east-west trending lineament more than 300 m long. The lineament is intersected by a ~north-south trending fault, which exposes massive, jointed outcrops of serpentinized rocks that form the major north-south ridge that Lost City rests on. The fracture and fault network in the basement provides permeable pathways that control outflow at the main vent sites. In addition to subvertical faults that channel flow to the largest structures, much of the subsurface flow emanates from surfaces that are parallel to basement to gently west-dipping faults. The steep faults expose relatively old, inactive stockworks of carbonate veins and subhorizontal to subvertical open fractures in the basement rock. These are actively leaking hydrothermal fluid and feeding young, white hydrothermal precipitates.

DIY Monolith Technology

Artifacts_2 The 2001 monolith is a science-fiction icon.  It can represent technology, God, alien influence or intense monkey violence, depending on what exactly you got out of Kubrick's masterpiece.  But will we ever see one?
http://www.dailygalaxy.com/my_weblog/2008/03/monolith-techno.html
Rather than go to all the bother of developing a hyperintelligent computer probe ourselves, the easiest route is the "Christmas" strategy: just wait for someone to give us what we want.  This assumes the existence of aliens, but let's be honest: nobody involved in the search doubts that for a second.  The fact it's always called a "search" is one clue - the unspoken belief that it's definitely out there and we just have to find it.  You can attribute this to hope, loneliness, or faith; but the most convincing reasons are a combination of the sheer size of the universe and the fact that, once you remove the "Invisible Sky Beard" factor from our genesis, it seems unlikely it should only happen here.
But why build monoliths at all?  Because of the universe's speed limit: if you can't get to other stars (because you'd be inconveniently dead of old age before you made it one-hundredth of the way), the only other option is to build a robot to go for you.  Should we observe such a probe it would bring good news and bad .  The good - there's an incredibly advanced alien civilization saying "Hi there, we're here!" The bad is them saying  "Yeah, we can't beat the speed of light either.  You're pretty much stuck there."  Rather a mournful picture of the universe, islands of intelligence stranded by the ridiculous distances between them.  As we reported previously, such systems would likely be Bracewell probes - self-replicating systems able to cover as much universe as possible in search of intelligence.  Clarke's monolith never shows any replicative ability, but the sheer number of them in 3001 would be strong evidence that they can.
The thing is: if human scientists waited for other people to do things for them, we'd still be delaying investigations into fire and non-cave habitats.  Many of the onyx-object's capabilities are within sight of our own technology.  Let's look at a few functions, and how close we've got:
1) Computers
If you're sending a computer probe to represent yourself and your entire culture to anyone you meet, it's got to be pretty good - and since our current AIs can still be confused by handwriting, they probably aren't going to cut it.  But if there's one thing we've gotten really good at it's making our own hardware look embarrassingly simple within a couple of years.  One of the holy grails of computer research is an artificial mind capable of doing anything for us - once developed, the new goal will probably be convincing it to keep doing so.  Able to exist indefinitely in hardware and even turn themselves off over extended periods, AIs would be the ideal interplanetary ambassadors - though whether they're representing us or the "Computer Empire 01" remains to be seen.
2) Communications
This one we've already got.  The movie monolith still uses radio emissions to communicate with homebase - albeit incredibly powerful ones.  These take a millennia per round trip, which is why the probe has to be smart enough to function by itself for the ten centuries or so between instructions.  That might seem like a forbiddingly long time to keep a project going, considering the average human can barely maintain a new year's resolution into February, but any species that's out to engineer other societies is probably better at long term goals than us.  Never mind communicating with distant probes - we've been broadcasting with the same level of technology since "I Love Lucy" (though anybody who receives those particular messages might not be too keen to meet us).
In fact, some believe we can do better.  Studies of quantum entanglement raise the possibility of instantaneous communication over unlimited distances - you still have to spend years transporting half of the entangled atoms to far flung locations, but by affecting one you can communicate with the other.  Anywhere.  To say this technology is in its infancy would be to understate how truly blastocystal it is - and many argue that it's still utterly impossible, with every chance of being right.  But as Mr Clarke himself said, claiming anything to be impossible is a very dangerous proposition - and even the attempt is evidence that we're moving beyond the imagination of one of the greatest visionaries of our time.  Go us!
3) Mental interfaces
The infamous final half hour of 2001, also known as "the psychedelingist cinema ever filmed", represents the monolith reading Dave's mind - and yes, we're already working on that.  We've been able to study individual neuron electrical activity for a while, but that's as far from reading thoughts as biting your fingernails is from open-heart surgery.  More sophisticated interfaces are on the way, however, and they aren't all from the cutting edge of neurological research.  They're coming from where the real money is - gaming. Emotiv Systems have already demonstrated a prototype brain scanning headset, and while the games are at the Space Invader level it may only be a matter of time before our fantasies of being totally immersed in cyber-violence are realised.  Though this may indicate we're some time from being ready to talk to aliens instead of shooting at them. Berkeley scientists have also developed a system that can decode what a human is looking at purely by examining brain activity, an impressive decryption of higher level functions.  Though should that person be watching the 2001 hotel room scene, it's likely that while the computer will know what he sees it won't know what the hell is going on either.
4) Stellar engineering
In 2061 the monoliths get together and turn Jupiter into a mini-star. We'll admit, that's just a tiny bit beyond us at the moment - but considering we still can't tell if we've destroyed our own planet with hairspray or not yet, that's probably for the best.
Even more interesting than the monolith hardware is the function, and what it would tell us about the creators.  It takes a pretty admirable culture to build the most advanced device they're capable of, then pretty much throw it away in the hopes of finding something - we can only hope we reach that stage instead of threatening to shoot our own satellites out of the sky.  We have one ability that might raise us to that level - curiosity.  It might kill cats, but it drives us to invent, to learn, to discover new things about ourselves and the world around us (which only rarely involves killing cats.  Rats are pretty buggered though).  It's the one base urge that can be embraced to conquer lust, hate and greed - and one that might just drive us into the grand futures that Arthur C. Clarke envisioned.
We'd probably only try to communicate with any cultures we find, but that's plenty.  The aliens in 2001 were set on steering the evolution of simpler cultures, but considering half our own planet still kill each other over the exact name of their imaginary friend, telling other worlds how to evolve would be scarier than an eight year old coming out of the Louvre with a packet of permanent markers telling people "I fixed the pictures!"
It'll be some time before we're ready to build our own monolith, a fact made obvious by even its basic design.  The enduring image of the monolith is a pure, unmarked blackness - and can you imagine us even launching something without a logo on it?
Posted by Luke McKinney.

Close-up of Vesta poses puzzle

Astronomers keen to look into strange hole on second-largest asteroid.
Published online 12 August 2011 | Nature | doi:10.1038/news.2011.480
The origin of Vesta's large crater and equatorial ridges is mysterious.NASA/JPL-Caltech/UCLA/MPS/DLR/IDA
Planetary scientists thought they knew what to expect when NASA's Dawn spacecraft returned the first close-up portrait of the giant asteroid Vesta last month. Fuzzy images from the Hubble Space Telescope (HST) taken in 1996 seemed to show that something had taken a big bite out of the asteroid's south polar region1.
The crater was posited as the source of Vesta-like fragments that populate the asteroid belt, and of a surprisingly large fraction of the meteorites found on Earth.
But seconds after viewing the first image, Peter Thomas of Cornell University in Ithaca, New York, shot off an e-mail to other members of the team: "Looks like HST results were fantasy!"
Thomas later realized he had misjudged Dawn's location when he sent that e-mail, but his words give an idea of scientists' surprise. Vesta's huge depression isn't like those of most impact craters: it is ringed by a wall for only about half its circumference, says Dawn team member Paul Schenk of the Lunar and Planetary Institute in Houston, Texas. It also has a large rounded mound in its middle, rather than the usual conical uplift.
Perhaps strangest of all is a series of troughs ringing the asteroid's equator, a feature not seen in any other body in the Solar System and which may be related to the impact and its huge scale.
If it was caused by an impact, the crater is shaping up to be one of the biggest puzzles of the mission, says Chris Russell, principal investigator of the Dawn mission at the University of California, Los Angeles.

Looking for answers

Russell has commissioned a task force of scientists on the Dawn team to solve the puzzle in time for two conferences in October.
New, sharper, images and spectra will help, as will maps of the asteroid's gravity. Dawn is now orbiting Vesta at a distance of about 2,700 kilometres, some six times closer than when the initial observations were made last month.
The task force will use the data gathered from this closer approach to hunt for evidence of whether the hole really was caused by some sort of collision. Tell-tale signs would include rock that has melted and resolidified on the floor of the depression, and a mixture of broken rock and melted material splashed out of the hole by the force of the blow.
Researchers have already come up with several possible explanations for the hole's strange shape. These all assume that the roughly 460-kilometre-wide crater was gouged out by a piece of space debris measuring 40-80 kilometres across.
One idea is that Vesta, which, at 530 kilometres across is the second-largest asteroid in the Solar System, was struck not at its south pole but midway between the pole and the equator. Because it spins rapidly, completing a full rotation in about five hours, Vesta would have reoriented itself so that the gouged-out region became the rock's new south pole.
This would be the most stable configuration for the damaged asteroid, says Schenk. "I don't think we've ever seen before a body with such a large impact and such a high rotation rate," he says.
In January, Martin Jutzi of the University of Bern in Switzerland and Erik Asphaug of the University of California, Santa Cruz, modelled the impact that walloped Vesta and obtained some surprising results2.
They calculate that Vesta completed an entire revolution while the crater was forming. As a result, the debris thrown up by the impact did not settle evenly around the crater, but fell in uneven clumps. This lopsided excavation might explain why a wall runs around only half of the impact site.
The cause of the equatorial troughs remain a mystery, says Asphaug, but they might be the result of material rushing back into the hole created by the impact. "We really don't know the physics when the crater gets to be about the size of the body [it strikes]," he says.
Russell is also hoping that Dawn will explain why Vesta is the brightest member of the asteroid belt, reflecting some 40% of the sunlight that hits it.
Images from the craft have already showed that some regions of the asteroid are brighter than average, and revealed dark streaks on the inside of craters. Compositional information recorded by Dawn's spectrometers may also show whether the bright regions are made from different material or whether they simply have a more crystalline structure, which scatters more light, Russell says. 
  • References

    1. Thomas, P. C. et al. Science 277, 1492-1495 (1997).
    2. Jutzi, M. & Asphaug, E. Geophys. Res. Lett. 38, L01102 (2011).

SETI Claims Three Giant Spaceships Headed Towards Earth?

http://propaganda-dimitrios.blogspot.com/2011/01/seti-claims-three-giant-spaceships.html


Three giant spaceships are heading towards Earth. The largest one of them is 240 kilometers wide. Two others are smaller. At present, the objects are beyond the orbit of Pluto.
It is about time science should say its word regarding the problem, and it did. SETI (Search for Extraterrestrial Intelligence), an independent non-commercial organization, released a sensational statement.
The spaceships were detected by HAARP search system. The system, based in Alaska, was designed to study the phenomenon of northern lights. According to SETI researchers, the objects are nothing but extraterrestrial spaceships. They will be visible in optical telescopes as soon as they reach Mars's orbit. The US government has been reportedly informed about the event. The ships will reach Earth in December 2012.
The date of the supposed space contact with extraterrestrial civilization brings up thoughts about the Mayan calendar, which ends on December 21, 2012. Is it just a coincidence? Most likely, though, SETI researchers mistake the wish for the reality: fifty years of constant monitoring of space have not yielded any results.
Nevertheless, mankind only begins to explore space. We are just newcomers in this huge and unexplored world. Many believe that there are many other civilizations in space beside our own civilization.
The alleged spaceships
Rumor has it that the Americans classified a lot of information about findings on the Moon. In 1988, a prominent Chinese official, a member of the nation's space program, unveiled pictures of human footprints on the lunar surface. The official stated that he had received the information from a reliable source and accused the Americans of concealing that information. The photos were dated from August 3, 1969 - two weeks after Armstrong and Aldrin stepped onto the surface of the Moon on July 20, 1969. Therefore, the materials of the lunar mission were studied and classified by NASA.
On March 15, 2009, The New York Times produced another sensation. The same Chinese official, Mao Kan, stated that he had obtained over than 1,000 secret NASA photographs depicting not only human footprints, but even a human carcass on the surface of the Moon. Some of the bones in the carcass were missing, the official said. The human corpse must have been dropped on the Moon from an alien spaceship, whereas the extraterrestrials kept some tissue samples for research.
The photos were taken by a lunar probe. The absence of air makes it possible to capture minute details from the lunar orbit. The pictures of the carcass were very clear.
Dr. Ken Johnston, former Manager of the Data and Photo Control Department at NASA's Lunar Receiving Laboratory, said that US astronauts had found and photographed ancient ruins of artificial origin on the Moon. Supposedly, US astronauts had seen large unknown mechanisms on the Moon. The data were classified by the US government.
Is all of that just spam or is it fantastic truth? Will we ever know?

Sunday, August 14, 2011

Secret art exhibit on the moon

[via greg.org by way of Boing Boing]

http://www.ethanham.com/blog/2008/03/secret-art-exhibit-on-moon.html
It sounds like a hoax or conspiracy theory, but apparently there is a secret art show on the moon. Artist Forrest "Frosty" Myers managed to have a "Moon Museum" secretly installed on a hatch on a leg of the Apollo 12's Intrepid landing module. Myers had tried to arrange for the art through NASA, but when the project was rejected, he enlisted the help of an unnamed engineer at the Grumman Corporation and did it as guerrilla art (let's see you do that, Banksy!).

Myers arranged for Rauschenberg, Warhol, Oldenburg, Chamberlain, and David Novros to contribute drawings in addition to his own. The six drawings were miniaturized and baked onto an iridium-plated ceramic wafer measuring just 3/4" x 1/2" x 1/40", with the assistance of engineers at Bell Labs.

According to the Times via greg.org, the artworks are Rauschenberg's wavy line; Novros' black square bisected by thin white lines; a computer-generated drawing by Myers; a geometric mouse by Oldenburg; and a template pattern by Chamberlain. Warhol's contribution, which is obscured by the thumb above, is described as "a calligraphic squiggle made up of the initials of his signature."Actually, it's a drawing of a penis.

For those of you with NY Times subscriptions, or a willingness to spend $3.95, the New York Times has a short article from November 22, 1969 about the exhibit.

The statue of the Fallen Astronaut is better known, institutionally approved moon art.

Moscow's Secret Moon Plan - The N-1 Rocket

Date: 04 February 2011 Time: 08:38 AM ET
See how the former Soviet Union planned to match the U.S. Apollo moon landings with the N-1 rocket in this infographic.
Source Space.com: All about our solar system, outer space and exploration

Lifted like a madman

Another great weight training day.  I did everything and a lot of it.  massive amounts of this, incredible amounts of that.  Everything got bigger, stronger and way more better.   Most of the lifting did in fact take place on the moon at this secret Moon base which was built by the combined space agencies of the former Soviet Union and the USA back in the mid 50s.  That’s how I was able to lift such massive amounts of weight today.

:)

Circling the Moon

In a new autobiography, an Apollo 15 pilot tells what it was like to fly solo.

  • By Al Worden With Francis French
  • Air & Space Magazine, July 01, 2011
$Alt
Eric Long/ NASM
Apollo 15’s command and service modules appeared in the window of the lunar module Falcon, which was bringing Dave Scott and Jim Irwin back from the moon, before the vehicles docked in lunar orbit.

Circling the Moon

Explore more photos from the story
The fourth mission to land men on the moon, Apollo 15 was also the first of Apollo’s extended science missions. After a smooth journey, which began on July 26, 1971, commander Dave Scott and lunar module pilot Jim Irwin stayed on the moon for 66 hours, longer than the two previous lunar landings combined. While Scott and Irwin explored the terrain with Apollo’s first lunar rover, command module pilot Al Worden, orbiting alone in the spacecraft Endeavour, photographed the moon and operated scientific instruments studying its surface. NASA’s then-administrator James Fletcher compared Apollo 15’s scientific return with discoveries Charles Darwin made on his five-year around-the-world voyage aboard the HMS Beagle, but the mission was marred by its crew’s bad judgment: The three men had flown postal covers to the moon, signed them, and sold them to a German stamp dealer. After the business arrangement was discovered, NASA management, embarrassed by the scrutiny the agency was receiving, did not fly the men in space again. In his new book, Falling to Earth: An Apollo 15 Astronaut’s Journey to the Moon, Al Worden recalls the pain of the scandal and recounts the unprecedented adventure of his mission. In this excerpt, Worden writes about his rendezvous with Scott and Irwin after three days of orbital solitude and describes making the first extravehicular activity—EVA—beyond Earth orbit.
—The editors
On my last morning alone around the moon, I woke to a breezy blast of mariachi trumpets. With the serene lunar surface gliding by below me, Herb Alpert’s “Tijuana Taxi” was about the strangest music mission control could pipe up over the radio. But still, it got me awake.
On the lunar surface, Dave and Jim suited up for their final moonwalk before they began preparations to lift off and rejoin me. We all had a busy day ahead. Ed Mitchell, the lunar module expert, was back as CapCom for this critical time. He read up a blizzard of numbers to me, telling me where and when I would need to rendezvous with my moving target.
Later in the day, mission control gave Dave clearance to lift off from the moon. On Hadley plain, Falcon’s engine lit, hurling the spacecraft upward. It quickly pitched over, and zipped along the rille on the curving path needed to reach me.
As Dave and Jim rose in the Falcon, I turned on the cassette player. We were an all-Air Force crew, so I figured it would be fun to play the U.S. Air Force anthem to mission control to provide a stirring background. Bad move. My radio signal was heard not only on Earth: For some reason, mission control also patched it through to the Falcon. Dave and Jim, intently focused on their checklists, now had distracting music in their ears. The ground didn’t tell me; perhaps they didn’t realize what they had done themselves until later.
Had something gone wrong with Falcon at that moment, the music could have been a dangerous diversion. Fortunately, everything went according to plan, and Dave and Jim zipped into an orbit below and behind me. I’d trained extensively to catch them if Falcon lurched into some other, wilder orbit. But I never needed to. I soon had a good radar lock on them. Guided by Ed Mitchell back on Earth, Dave and I flew our spacecraft ever closer, mirroring each other’s moves. “You got your lights on, Jim?” I radioed, watching for Falcon’s flashing tracking light.
I looked through the sextant and the telescope to try to find them, but sunlight in the scopes made it hard to see anything. Finally, in the corner of my eye, I spotted a flash of light in the telescope. I manually drove the instruments over to that point, and there it was: a very bright light. “I’ve got your lights now, Dave,” I told them.
As Falcon steadily rose to meet me, Dave and Jim gave Endeavour an extensive look-over, while I photographed them in turn. Falcon had left its descent stage on the surface of the moon and was now much smaller than when I had last seen it. Falcon was so light, a pulse of its thrusters rattled the lunar module around. So it was easier for me to dock using Endeavour. I slowly slid toward them, so gently that we barely touched. Then, with a touch of my thrusters, I pushed forward into a hard dock.
The rendezvous and docking had been fast—and perfect. “Good show, Endeavour,” Dave radioed to me. “Welcome home,” I replied. That might seem like an odd choice of words—after all, we were still a quarter of a million miles from Earth. But Endeavour had become my home, and Dave and Jim were returning from a great adventure.
I’d kept our home clean and tidy for them. But now, as I opened the hatches between the spacecraft, I saw two grimy faces. Their spacesuits were dirty, and I could smell the moondust. It was a new, peculiar odor—dry and gunpowdery. I kept the hatch closed as much as possible while we began to transfer equipment, hoping the floating dust would not spread. I was mostly successful, but the creep of dust was unavoidable. Dave and Jim floated long sample tubes of lunar dirt and boxes of moonrocks through the hatch, which I stowed inside Endeavour under the couches.
While busily running scientific experiments, I also stored Falcon’s flight plans and checklists, food, film magazines full of priceless photos, and—less priceless to me—Dave and Jim’s used urine and fecal bags. Of all the things to return from the lunar surface, did we really need their crap?
Finally, Dave and Jim floated into Endeavour. I was elated to see them. But Dave didn’t look happy. In fact, while Jim looked away sheepishly, Dave began to loudly berate me about the distracting tune piped into the Falcon during liftoff. Didn’t I know I had jeopardized the whole mission, he thundered, by playing that darn music?
This wasn’t the reunion I had expected. I could only apologize and explain that I had only radioed it to Houston, with no clue they would patch it back to the Falcon. My explanation seemed to satisfy Dave for the moment. I guess he eventually forgave me, because months later at an awards ceremony with the Air Force Association, Dave bragged about playing the tune.
There wasn’t time for me or Dave to dwell on the argument. We had too much to do. Behind in the timeline, we hustled to close the hatches. On the first attempt, the spacecraft hatch did not seal correctly, possibly due to some lunar dust. After more time-consuming checks, we finally seemed to have the problem solved, and Dave and Jim could remove their helmets and gloves. They had started their day with a demanding moonwalk, and they hadn’t eaten for eight hours. They were ready to stop for a while and grab some food.

(Page 2 of 3)
Then it was finally time to undock from Falcon. “It’s away clean, Houston,” I reported as the lunar module separated with a bang. The separation had taken longer than planned, so instead of our scheduled rest break, we jumped back into our chores.
Jim and Dave would have worked until they dropped, they were so dedicated to the mission. “We’re still trying to get cleaned up in here and get suits put away and all that sort of stuff,” I told the ground. “It’s awfully cramped quarters, and there’s an awful lot of stuff to move around.” The spacecraft seemed very different now that three of us were crammed in again. “I kind of liked it here by myself,” I added wistfully.
By the time we finished everything on the checklist, we were exhausted. We slept deeply for nine hours. The next morning, we all felt much better. With the three of us scrambling to accomplish tasks, my day seemed much more complicated. I was happy to have Dave and Jim back alive, but I began to miss working alone, when we didn’t all have overlapping tasks.
I had enjoyed my time in orbit. There was so much to see that I never grew bored. The sunlit part of the moon shifted as the days went by, so there were always new places to view. I could have happily spent a few more days there—the same feeling I get at the end of a great vacation. But it was time to go home.
Two days after Dave and Jim had rejoined me in Endeavour, I fired the main engine to propel us away from the moon. I could feel the steady acceleration as it burned for over two minutes. I warily watched the gauges that told me our engine was burning smoothly, speeding us on the curved pathway out of lunar orbit.
I settled in for our three-day coast back to Earth. Mission control signed off, reminding us that “our ever-watchful eye will be on you while you sleep.”
When I woke the next morning, I had to carry out some critical navigation. We had one shot to get back home, and I wanted to be on course from the beginning. While Houston kept an eye on us to make sure we didn’t stray out of a general path of certainty, I hoped to prove it was possible to navigate to and from the moon without their help. I was aiming for a narrow sliver of horizon on a planet tens of thousands of miles away, and there was no margin for error. This far from Earth, the tiniest changes in direction could result in huge errors once we had traveled the remaining distance in our voyage.
I used my sextant and measured the angle between Earth’s horizon and my preselected stars. However, I also had to choose the right place on the horizon. Our planet is about 8,000 miles across, and the horizon is only 50 miles deep. That sounds tiny, and it looked tiny from so far away, but 50 miles was too deep for what I needed to do. I needed more accuracy.
In my training, I had calibrated my eye for a specific part of the atmosphere. Between Earth’s surface and the blackness of space, the atmosphere looked like narrow bands of colors, mostly subtly different reds, magentas, and blues. On Earth I had experimented in simulations to identify a thin color line I could find consistently. I looked for a particular light blue within the atmosphere, and this reduced the 50-mile depth to a much smaller path as we left the moon. It worked even better than it had in the simulators: We stayed firmly on track.
We were still much closer to the moon than to Earth, but because our planet is so much larger, its gravity pulled on us more. We were now truly falling to Earth. It meant nothing to us in the spacecraft—there was no physical sensation of our incredible speed as we shot through the black void.
It was time for the three of us to float back into our spacesuits and help each other zip up before I went out for my EVA to retrieve film from cameras in the Scientific Instrument Module (SIM) bay. “You have a go for depress,” mission control told us. We slowly began to let the oxygen out of the cabin through a special valve in the hatch. Everything in the airless spacecraft looked the same, but I knew now that if I took off my helmet, I would die.
“We’re getting ready to open the hatch,” Dave reported. “Okay. Unlatch.”
“The hatch is open,” I announced. I poked my head outside and carefully mounted a 16-mm movie camera on the hatch to film my spacewalk. Then, grabbing the nearest handrail, I soundlessly floated outside.
I paused a moment and waited for Jim to poke his head and shoulders out of the hatchway behind me. He would stay there to keep an eye on me while I made my way down the side of the spacecraft. Other than our service module glinting in the sunlight, it looked really black out there. I looked down the length of the SIM bay. “You ready, Jim?” I asked. “I’ll work my way down.”

(Page 3 of 3)
After 11 days in space, I was accustomed to weightlessness. With one hand on a handrail, I could turn my body with my wrist. The SIM bay was slightly to the left of the hatch, so I first needed to swing across the face of Endeavour. I let my legs float up, swung around, and worked my way down the side of the spacecraft, hand over hand, never using my feet.
I floated over the mapping camera, then rotated myself on the handrail, placing my feet in special restraints. I hadn’t really had a sense of where I was until this moment. Standing upright on the side of the spacecraft, attached only by my feet and the umbilical that loosely snaked back to the spacecraft hatch, I had a fleeting sense of being deep under the ocean, in the dark, next to an enormous white whale. The sun was at a low angle behind me, so every bump on the outside of the service module cast a deep shadow. I didn’t dare look toward the sun, knowing it would be blindingly bright. In the other direction, and all around me, there was—nothing. It’s a sensation impossible to experience unless you float tens of thousands of miles from the nearest planet. This wasn’t deep dark water, or night sky, or any other wide open space that I could comprehend. The blackness defied understanding, because it stretched away from me for billions of miles.
But there wasn’t time to ponder it too much. I had work to do. I pulled the cover off the panoramic camera, released the film cassette, and tethered myself to it. Jim waited for me at the hatch. “Would you like to get hold of it?” I asked with a laugh as I passed him the film. Jim tethered it inside and released the tether attaching me to it. While Dave stowed the panoramic camera film deeper in the cabin, I floated back down the side of the spacecraft. “Beautiful job, Al baby!” Karl Henize radioed from Earth. “Remember, there is no hurry up there at all.”
“Roger, Karl,” I replied as I grabbed the handrail again. “I’m enjoying it!”
I floated back down the SIM bay, much faster this time. It was time to remove the mapping camera film cassette and bring that back inside. This time the cover didn’t cooperate, and I had to twist and pull hard three or four times before it came away. I pulled the mapping camera film out and floated it back over to Jim, who grabbed the film and unhooked the tether attaching it to me. As we did this, I saw one of the most amazing sights of my life. Jim was perfectly framed by the enormous moon right behind him. It looked as big as the spacecraft, and was dramatically lit by the sun. It could have been the most famous photo in the space program, if I’d been allowed to take a camera out of the spacecraft.
I’d argued for carrying one on my EVA, but the mission planners had worried I’d be busy enough. Now I really wished I’d had one. Well, if I didn’t have a camera, I could at least take a look at where I was. After all, 12 people would walk on the moon during Apollo, but only three would make a deep-space EVA. I would forever be the first, and to this day I hold the record for floating in space farther away from Earth than any other human.
I realized I had a unique viewpoint: I could see the entire moon if I looked in one direction. Turning my head, I could see the entire Earth. The perspective is impossible to have on Earth or on the moon. I had to be far enough away from both.
It was time to float back inside.
Right away, I wished I had spent more time out there just looking around. We had plenty of time. Those film canisters with their priceless images were now safely inside the spacecraft. But I could have soaked in the scene a little more, just for myself.
If I couldn’t take photos outside myself—and Jim had not taken any stills of me either—I knew that at least the 16-mm movie camera should have picked up some spectacular images. But I was wrong. That camera, we learned later, had jammed. It had captured only one frame, showing me floating away.
After retiring from NASA, Al Worden worked in private industry before becoming chair of the Astronaut Scholarship Foundation. Francis French is director of education at the San Diego Air & Space Museum.
Project X-37B OTV aerospace
http://nanobiotechnews.com/project-x-37b-otv-aerospace.html
The U.S. Air Force into orbit a second X-37B secret mini-Shuttle surrounded by an enormous secrecy. The second minitransbordador unmanned X-37B, Blasted off from Cape Canaveral with a day late after being suspended the launch on Friday March 4, 2011, due to cloudy weather and windy it was at launch.
Although Saturday morning the weather with her, had to postpone release again until 17:46, when the East Coast of the United States, that day when detecting a fault in a valve having to be repaired in the last minute.
aero space
The mission is of a classified, although the leaders of the Air Force stated that the purpose was to test new technologies space. However, the secrecy surrounding the mission and the time the ship remains in orbit has alerted several nations if it could be a space weapon. The spacecraft was put into orbit hidden in the upper cone of a rocket type Atlas VOf disposable type.

Features:
The ship is similar to the space shuttles used by NASA but with much smaller dimensions, so much so, that would fit two X-37B aircraft in the hold of a NASA space shuttle. Specifically, the vehicle is about 9 meters long and 4.5 meters wide with a height that is less than 3 meters. Its light weight gives it a body of less than 5 tonnes.
Despite its small size, a powerful engine of 29,341 kN can accelerate the spacecraft to reach more than 28,000 km / h, maintaining its orbit for 7 months, fueled by solar panels with solar cells.
Perhaps most disturbing of all is that no crew thanks to avionics systems similar to those used in the unmanned aircraft RAPTOR. This fact together with the secrecy that has surrounded the project and its launch has been responsible for Russia and China set off alarms.

Development and purpose of the X-37B OTV:
The program of the X-37B Orbital Test Vehicle (Orbital Test Vehicle), has been developed with the participation of government, the arms company DARPA, Air Force and NASA, Boeing remains the prime contractor for the program. Although the original X37 program belonged to the NASA program, which began in 1999 with the aim of creating reusable vehicles, the project was transferred in September 2004 the company DARPA character becoming classified.
The first evidence against the company DARPA during April 2006, when he dropped an X-37 spacecraft called Lifelong Learning, which stands for test vehicle approach and landing, making the first orbital test in December 2010.
The ultimate goal and actual project is still classified, so only expect to fit the statements are true and only case of a program to test new technologies, although it is doubt and fear if the USAF is developing some kind of space weapon or maybe some new type of surveillance system.
The latter is certainly due to the height at which orbits where spy satellites are positioned, and that can take up to four times per hour over the same geographical point. Needless to say the project will continue to matter classified so we can only rely on the truth and we have not reached the age of space wars or the thinking machines.
SAMOS to the Moon - 1.7MB PDF

http://www.nro.gov/foia/declass/frequent.html

Turkish researchers make nanotechnology breakthrough

HDN image
http://www.trdefence.com/2011/06/17/turkish-researchers-make-nanotechnology-breakthrough/
A group of Turkish researchers at an Ankara university have manufactured the longest and thinnest nanowires ever produced, by employing a novel method to shrink matter 10-million fold.
The invention, discovered at Bilkent University’s National Nanotechnology Research Center, or UNAM, is set to appear on the cover of Nature Material magazine’s July edition.
“At this moment, we may not even be able to predict what things will be produced [in the future] using this method,” said Associate Professor Mehmet Bayýndýr who led the research team.
The new method could provide advancements in many fields, including the production of more effective cells for solar panels, DVD’s with massively enhanced capacity, electronics and other novel applications that could be used in medical imaging technologies, according to the Anatolia news agency.
The research team was trying to obtain a patent for their invention, as well as preparing to apply to the Guinness Book of Records for producing the world’s longest and thinnest semiconductor nanowire.
The new technique includes a new thermal size-reduction process to produce indefinitely long nanowire and nanotube arrays with various materials, Bayýndýr said Friday.
“We are enjoying [the fact that] we are getting higher amounts of projects than scientists in developed countries, despite the global economic crisis,” he said.
The project was funded by the Scientific and Research Council of Turkey, or TÜBITAK, the Turkish Academy of Sciences, or TÜBA, and the State Planning Organization, or the DPT.
HDN
Short URL: http://www.trdefence.com/?p=5105

USAF robotic shuttle marks first autonomous spacecraft landing

USAF X-37B Robotic Space Shuttle
http://www.trdefence.com/2010/12/05/usaf-robotic-shuttle-marks-first-autonomous-spacecraft-landing/
A miniature robotic space shuttle wrapped up a 224-day classified military mission and made an unannounced landing in darkness on a California runway on Friday, Air Force officials said.
The Orbital Test Vehicle, or X-37B, touched down at 1:16 a.m. PST at Vandenberg Air Force Base, becoming the first U.S. spaceship to land itself on a runway.
The former Soviet Union’s Buran space shuttle accomplished a similar feat in 1988.
“We are very pleased that the program completed all the on-orbit objectives for the first mission,” program manager Lt. Col. Troy Giese said in a statement.
The project, which was started by NASA in the late 1990s and later adopted by the military, is intended to test technologies for a next-generational space shuttle.
Rather than carry people, however, the military is looking at the spaceplane as a way to test new equipment, sensors and material in space, with the intention of incorporating successful technologies into satellites and other operational systems.
Another key point of the project is to see if the costs and turnaround time between flights can be reduced from months to days.
The Air Force imposed a news blackout on the X-37B’s activities while in orbit, though it was tracked by amateur satellite-watchers throughout its nine-month mission.
The X-37B looks like a space shuttle orbiter, but is smaller, with a similar shape and payload bay for cargo and experiments. But it measures 29 feet, 3 inches in length (8.9 metres) and has a 15-foot (4.5-metres) wing span, compared to the 122-foot (37-metres) orbiters with wing spans of 78 feet (23.8 metres).
Unlike NASA’s space shuttles which can stay in orbit about two weeks, X-37B is designed to spend as long as nine months in space, then land itself on a runway.
The Air Force plans to fly its second X-37B vehicle this spring. The spaceplanes were built by Boeing’s advanced research lab, Phantom Works.
Reuters
Short URL: http://www.trdefence.com/?p=2699

Carbon Nanotubes 1 KM Long

Carbon Nanotubes 1 KM Long
New manufacturing process produces yarns and sheets of carbon nanotubes millions of times the size of previous nanotubes.
The thought of being able to use carbon nanotubes in future projects excites most engineers, but the current size at which they can be produced, renders them pretty much useless. That is until now.
Thanks to Nanocomp Technologies of Concord, New Hampshire, researchers and engineers can now utilize ‘yarns’ and ‘sheets’ of the material.
When carbon nanotubes first entered the spotlight back in 1991, the technology world began brainstorming endless ways the material could be used. The structural, thermal, and electrical properties of these cylindrical-shaped carbon molecules meant that, in theory, they could be used for extremely compact and fast digital computers, rugged electronics, and super strong structures such as a space elevator – a 62,000 mile elevator stretching into space.
carbon-nanotubes
However, researchers have found it difficult to mass produce nanotubes long enough to accomplish any break-through technologies.
Now Nanocomp Technologies, based in Concord, New Hampshire, is bringing the future closer by producing yarns and sheets of nanotubes, in bulk.
On an atomic level, carbon nanotubes look like rolled-up tubes of chicken wire. The tubing is made from a hexagonal lattice of carbon atoms and measures approx one nanometer (one billionth of a meter) in diameter.
Currently, nanotubes are commonly produced in segments about 10,000 nanometers long, to the eye, this looks like a black powder. At this size, the carbon nanotubes full potential is far from utilized, but Nanocomp says it can now produce 18-square-foot sheets and 1 km long yarns of nanotubing.
Nanocomp is using its nanotubing to make lightweight antennas, cables, and electromagnetic interference shields for the military and aerospace markets. Nanocomp is also working with the Office of Naval Research and the U.S. Army’s Natick Soldier Center to develop better body armor.

How It Works

Nanotubes are made by feeding a gas containing a carbon-based feedstock – the raw material – into a long cylindrical furnace. The gas is swept along the furnace until it meets a heated, porous block that is coated with a catalyst.
how-nanocomp-produce-nanotubes
As it squeezes through the pores, the gas is forced into contact with the catalyst, and carbon nanotubes begin to form. A temperature gradient between the porous block and the open end of the furnace supports the tubes as they grow, absorbing material from the reaction gas.
Eventually the nanotubes leave the cylindrical furnace, looking like a wispy, black mass of tube-shaped cotton candy. A rotating anchor or conveyor belt captures the nanotubes as they emerge, turning them into yarns and sheets.