Archive for the ‘Space Exploration’ Category

The Moonwalk of 1969

Thursday, July 21st, 2011

I remember watching the first human steps on the Moon on 20 July 1969, along with a couple of hundred people at a hotel in the Catskills. It was the only TV set around.


42 years later, it’s worth revisiting the article in The New York Times from that day. Check out the lead…

Men have landed and walked on the moon.

Two Americans, astronauts of Apollo 11, steered their fragile four-legged lunar module safely and smoothly to the historic landing yesterday at 4:17:40 P.M., Eastern daylight time.

Neil A. Armstrong, the 38-year-old civilian commander, radioed to earth and the mission control room here:

“Houston, Tranquility Base here. The Eagle has landed.”

The first men to reach the moon–Mr. Armstrong and his co-pilot, Col. Edwin E. Aldrin, Jr. of the Air Force–brought their ship to rest on a level, rock-strewn plain near the southwestern shore of the arid Sea of Tranquility.

About six and a half hours later, Mr. Armstrong opened the landing craft’s hatch, stepped slowly down the ladder and declared as he planted the first human footprint on the lunar crust:

“That’s one small step for man, one giant leap for mankind.”

His first step on the moon came at 10:56:20 P.M., as a television camera outside the craft transmitted his every move to an awed and excited audience of hundreds of millions of people on earth.

Tentative Steps Test Soil

Mr. Armstrong’s initial steps were tentative tests of the lunar soil’s firmness and of his ability to move about easily in his bulky white spacesuit and backpacks and under the influence of lunar gravity, which is one-sixth that of the earth.

“The surface is fine and powdery,” the astronaut reported. “I can pick it up loosely with my toe. It does adhere in fine layers like powdered charcoal to the sole and sides of my boots. I only go in a small fraction of an inch, maybe an eighth of an inch. But I can see the footprints of my boots in the treads in the fine sandy particles.

After 19 minutes of Mr. Armstrong’s testing, Colonel Aldrin joined him outside the craft.

The two men got busy setting up another television camera out from the lunar module, planting an American flag into the ground, scooping up soil and rock samples, deploying scientific experiments and hopping and loping about in a demonstration of their lunar agility.

They found walking and working on the moon less taxing than had been forecast. Mr. Armstrong once reported he was “very comfortable.”

And people back on earth found the black-and-white television pictures of the bug- shaped lunar module and the men tramping about it so sharp and clear as to seem unreal, more like a toy and toy-like figures than human beings on the most daring and far- reaching expedition thus far undertaken.

Nixon Telephones Congratulations

During one break in the astronauts’ work, President Nixon congratulated them from the White House in what, he said, “certainly has to be the most historic telephone call ever made.”

“Because of what you have done,” the President told the astronauts, “the heavens have become a part of man’s world. And as you talk to us from the Sea of Tranquility it required us to redouble our efforts to bring peace and tranquility to earth.

“For one priceless moment in the whole history of man all the people on this earth are truly one–one in their pride in what you have done and one in our prayers that you will return safely to earth.”

Mr. Armstrong replied:

“Thank you Mr. President. It’s a great honor and privilege for us to be here representing not only the United States but men of peace of all nations, men with interests and a curiosity and men with a vision for the future.”

Mr. Armstrong and Colonel Aldrin returned to their landing craft and closed the hatch at 1:12 A.M., 2 hours 21 minutes after opening the hatch on the moon. While the third member of the crew, Lieut. Col. Michael Collins of the Air Force, kept his orbital vigil overhead in the command ship, the two moon explorers settled down to sleep.

Outside their vehicle the astronauts had found a bleak world. It was just before dawn, with the sun low over the eastern horizon behind them and the chill of the long lunar nights still clinging to the boulders, small craters and hills before them.

Colonel Aldrin said that he could see “literally thousands of small craters” and a low hill out in the distance. But most of all he was impressed initially by the “variety of shapes, angularities, granularities” of the rocks and soil where the landing craft, code-named Eagle had set down.

The landing was made four miles west of the aiming point, but well within the designated area. An apparent error in some data fed into the craft’s guidance computer from the earth was said to have accounted for the discrepancy.

Suddenly the astronauts were startled to see that the computer was guiding them toward a possibly disastrous touchdown in a boulder-filled crater about the size of a football field.

Mr. Armstrong grabbed manual control of the vehicle and guided it safely over the crater to a smoother spot, the rocket engine stirring a cloud of moon dust during the final seconds of descent.

Soon after the landing, upon checking and finding the spacecraft in good condition, Mr. Armstrong and Colonel Aldrin made their decision to open the hatch and get out earlier than originally scheduled. The flight plan had called for the moon walk to begin at 2:12 A.M.

Flight controllers here said that the early moon walk would not mean that the astronauts would also leave the moon earlier. The lift-off is scheduled to come at about 1:55 P.M. today.

Their departure from the landing craft out onto the surface was delayed for a time when they had trouble depressurizing the cabin so that they could open the hatch. All the oxygen in the cabin had to be vented.

Once the pressure gauge finally dropped to zero, they opened the hatch and Mr. Armstrong stepped out on the small porch at the top of the nine-step ladder.

“O.K., Houston, I’m on the porch,” he reported, as he descended.

On the second step from the top, he pulled a lanyard that released a fold-down equipment compartment on the side of the lunar module. This deployed the television camera that transmitted the dramatic pictures of man’s first steps on the moon.

Ancient Dream Fulfilled

It was man’s first landing on another world, the realization of centuries of dreams, the fulfillment of a decade of striving, a triumph of modern technology and personal courage, the most dramatic demonstration of what man can do if he applies his mind and resources with single-minded determination.

The moon, long the symbol of the impossible and the inaccessible, was now within man’s reach, the first port of call in this new age of spacefaring.

Immediately after the landing, Dr. Thomas O. Paine, administrator of the National Aeronautics and Space Administration, telephoned President Nixon in Washington to report:

“Mr. President, it is my honor on behalf of the entire NASA team to report to you that the Eagle has landed on the Sea of Tranquility and our astronauts are safe and looking forward to starting the exploration of the moon.”

The landing craft from the Apollo 11 spaceship was scheduled to remain on the moon about 22 hours, while Colonel Collins of the Air Force, the third member of the Apollo 11 crew, piloted the command ship, Columbia, in orbit overhead.

“You’re looking good in every respect,” Mission Control told the two men of Eagle after examining data indicating that the module should be able to remain on the moon the full 22 hours.

Mr. Armstrong and Colonel Aldrin planned to sleep after the moon walk and then make their preparations for the lift-off for the return to a rendezvous with Colonel Collins in the command ship.

Apollo 11’s journey into history began last Wednesday from launching pad 39-A at Cape Kennedy, Fla. After an almost flawless three-day flight, the joined command ship and lunar module swept into an orbit of the moon yesterday afternoon.

The three men were awake for their big day at 7 A.M. when their spacecraft emerged from behind the moon on its 10th revolution, moving from east to west across the face of the moon along its equator.

Their orbit was 73.6 miles by 64 miles in altitude, their speed 3,660 miles an hour. At that altitude and speed, it took about two hours to complete a full orbit of the moon.

The sun was rising over their landing site on the Sea of Tranquility.

“We can pick out almost all of the features we’ve identified previously,” Mr. Armstrong reported.

After breakfast, on their 11th revolution Colonel Aldrin and then Mr. Armstrong, both dressed in their white pressurized suits, crawled through the connecting tunnel into the lunar module.

They turned on the electrical power, checked all the switch settings on the cockpit panel and checked communications with the command ship and the ground controllers. Everything was “nominal,” as the spacemen say.

LM Ready for Descent

The lunar module was ready. Its four legs with yard-wide footpads were extended so that the height of the 16-ton vehicle now measured 22 feet and 11 inches and its width 31 feet.

Mr. Armstrong stood at the left side of the cockpit, and Colonel Aldrin at the right. Both were loosely restrained by harnesses. They had closed the hatch to the connecting tunnel.

The walls of their craft were finely milled aluminum foil. If anything happened so that it could not return to the command ship, the lunar module would be too delicate to withstand a plunge through earth’s atmosphere, even if it had the rocket power.

Nearly three-fourths of the vehicle’s weight was in propellants for the descent and ascent rockets–Aerozine 50 and nitrogen oxide, which substituted for the oxygen, making combustion possible.

It was an ungainly craft that creaked and groaned in flight. But years of development and testing had determined that it was the lightest and most practical way to get two men to the moon’s surface.

Before Apollo 11 disappeared behind the moon near the end of its 12th orbit, mission control gave the astronauts their “go” for undocking–the separation of Eagle from Columbia.

Colonel Collins had already released 12 of the latches holding the two ships together at the connecting tunnel. He did this when he closed the hatch at the command ship’s nose. While behind the moon, he was to flip a switch on the control panel to release the three remaining latches by a spring action.

At 1:50 P.M., when communications signals were reacquired, Mission Control asked: “How does it look?”

“Eagle has wings,” Mr. Armstrong replied.

The two ships were then only a few feet apart. But at 2:12 P.M., Colonel Collins fired the command ship’s maneuvering rockets to move about two miles away and in a slightly different orbit from the lunar module.

“It looks like you’ve got a fine-looking flying machine there, Eagle, despite the fact you’re upside down,” Colonel Collins commented, watching the spidery lunar module receding in the distance.

“Somebody’s upside down,” Mr. Armstrong replied.

What is “up” and what is “down” is never quite clear in the absence of landmarks and the sensation of gravity’s pull.

As Mr. Armstrong and Colonel Aldrin rode the lunar module back around to the moon’s far side, the rocket engine in the vehicle’s lower stage was pointed toward the line of flight. The two pilots were leaning toward the cockpit controls, riding backwards and facing downward.

“Everything is ‘go,'” they were assured by Mission Control.

Their on-board guidance and navigation computer was instructed to trigger a 29.8-second firing of the descent rocket, the 9,870-pound-thrust throttable engine that would slow down the lunar module and send it toward the moon on a long, curving trajectory.

The firing was set to take place at 3:08 P.M., when the craft would be behind the moon and once again out of touch with the ground.

Suspense built up in the control room here. Flight controllers stood silently at their consoles. Among those waiting for word of the rocket firing were Dr. Thomas O. Paine, the space agency’s administrator, most of the Apollo project officials and several astronauts.

At 3:46 P.M., contact was established with the command ship.

Colonel Collins reported, “Listen, baby, things are going just swimmingly, just beautiful.”

There was still no word from the lunar module for two minutes. Then came a weak signal, some static and whistling, and finally the calm voice of Mr. Armstrong.

“The burn was on time,” the Apollo 11 commander declared.

When he read out data on the beginning of the descent, Mission Control concluded that it “look great.” The lunar module had already descended from an altitude of 65.5 miles to 21 miles and was coasting steadily downward.

Eugene F. Kranz, the flight director, turned to his associates and said, “We’re off to a good start. Play it cool.”

Colonel Aldrin reported some oscillations in the vehicle’s antenna, but nothing serious. Several times the astronauts were told to turn the vehicle slightly to move the antenna into a better position for communications over the 230,000 miles.

“You’re ‘go’ for PDI,” radioed Mission Control, referring to the powered descent initiation–the beginning of the nearly 13-minute final blast of the rocket to the soft touchdown.

When the two men reached an altitude of 50,000 feet, which was approximately the lowest point reached by Apollo 10 in May, green lights on the computer display keyboard in the cockpit blinked the number 99.

This signaled Mr. Armstrong that he had five seconds to decide whether to go ahead for the landing or continue on its orbital path back to the command ship. He pressed the “proceed” button.

The throttleable engine built up thrust gradually, firing continuously as the lunar module descended along the steadily steepening trajectory to the landing site about 250 miles away:

“Looking good,” Mission Control radioed the men.

Four minutes after the firing the lunar module was down to 40,000 feet. After five and a half minutes, it was 33,500 feet. At six minutes, 27,000 feet.

“Better than the simulator,” said Colonel Aldrin, referring to their practice landings at the spacecraft center.

Seven minutes after the firing, the men were 21,000 feet above the surface and still moving forward toward the landing site. The guidance computer was driving the rocket engine.

The lunar module was slowing down. At an altitude of about 7,200 feet, with the landing site still about five miles ahead, the computer commanded control jets to fire and tilt the bug-shaped craft almost upright so that its triangular windows pointed forward.

Mr. Armstrong and Colonel Aldrin then got their first close-up view of the plain they were aiming for. It was then about three and a half minutes to touchdown.

The brownish-gray panorama rushed below them–myriad craters hills and ridges, deep cracks and ancient rubble on the moon, which Dr. Robert Jastrow, the space agency scientist, called the “Rosetta Stone of life.”

“You’re ‘go’ for landing,” Mission Control informed the two men.

The Eagle closed in, dropping about 20 feet a second, until it was hovering almost directly over the landing area at an altitude of 500 feet.

Its floor was littered with boulders.

It was when the craft reached an altitude of 300 feet that Mr. Armstrong took over semimanual control for the rest of the way. The computer continued to have control of the rocket firing, but the astronaut could adjust the craft’s hovering position.

He was expected to take over such control anyway, but the sight of a crater looming ahead at the touchdown point made it imperative.

As Mr. Armstrong said later, “The auto-targeting was taking us right into a football field- sized crater, with a large number of big boulders and rocks.”

For about 90 seconds, he peered through the window in search of a clear touchdown point. Using the lever at his right hand, he tilted the vehicle forward to redirect the firing of the maneuvering jets and thus shift its hovering position.

Finally, Mr. Armstrong found the spot he liked, and the blue light on the cockpit flashed to indicate that five-foot-long probes, like curb feelers, on three of the four legs had touched the surface.

“Contact light,” Mr. Armstrong radioed.

He pressed a button marked “Stop” and reported, “okay, engine stop.”

There were a few more cryptic messages of functions performed.

Then Maj. Charles M. Duke, the capsule communicator in the control room, radioed to the two astronauts:

“We copy you down, Eagle.”

“Houston, Tranquility Base here. The Eagle has landed.”

“Roger, Tranquility,” Major Duke replied. “We copy you on the ground. You got a bunch of guys about to turn blue. We are breathing again. Thanks a lot.”

Colonel Aldrin assured Mission Control it was a “very smooth touchdown.”

The Eagle came to rest at an angle of only about four and a half degrees. The angle could have been more than 30 degrees without threatening to tip the vehicle over.

The landing site, about 120 miles southwest of the crater Maskelyne, is on the right side of the moon as seen from earth. The position: Lat. 0.799 degrees N., Long. 23.46 degrees E.

Although Mr. Armstrong is known as a man of few words, his heartbeats told of his excitement upon leading man’s first landing on the moon.

At the time of the descent rocket ignition, his heartbeat rate registered 110 a minute–77 is normal for him–and it shot up to 156 at touchdown.

At the time of the landing, Colonel Collins was riding the command ship Columbia about 65 miles overhead.

Mission control informed the colonel, “Eagle is at Tranquility.

“Yea, I heard the whole thing,” Colonel Collins, the man who went so far but not all the way, replied. “Fantastic.”

When the Apollo astronauts landed on the Sea of Tranquility, the temperature at their touchdown site was about zero degrees Fahrenheit in the sunlight, even colder in the shade.

During a lunar night, which lasts 14 earth days, temperatures plunge as low as 280 degrees below zero. Unlike earth, the moon, having no atmosphere to act as a blanket, is unable to retain any of the day’s warmth during the night.

During the equally long lunar day, temperatures rise as high as 280 degrees. By the time of Eagle’s departure from the moon, with the sun higher in the sky, the temperatures there will have risen to about 90 degrees.

This particular landing site was one of five selected by Apollo project officials after analysis of pictures returned by the five Lunar Orbiter unmanned spacecraft.

All five sites are situated across the lunar equator on the side of the moon always facing earth. Being on the equator reduces the maneuvering for the astronauts to get there. Being on the near side of the moon, of course, makes it possible to communicate with the explorers.

It’s Alive!

Monday, June 27th, 2011


Thank you, doctor. Nice piece by Jeremey Hsu at Space.com, calling the new Mars exploration spacecraft “Frankenstein” for all the money-saving shortcuts on the build side…

Take the DNA of the deceased NASA Phoenix Mars Lander, add bits and pieces from several lost Mars missions and you have a “Frankenstein” mission competing for a spot on NASA’s space exploration lineup for the next decade.

The mission, once called the Geophysical Monitoring Station, is nameless for now. It would carry a seismometer that flew aboard a doomed Mars Surveyor 98 spacecraft, and a burrowing “mole” device based on an instrument lost during the British Beagle 2 mission’s hard landing in 2003.

But the probe’s goal is clear: to learn the early evolution of terrestrial planets such as Earth by tapping a Martian geological record more than 4 billion years old.

“Mars is not an easy place to land on, but we’ve done it a number of times,” said Bruce Banerdt, a planetary scientist at the Jet Propulsion Laboratory in Pasadena, Calif. “We’re going to try and do it exactly like how we did it with Phoenix a few years ago.”

The mission planners’ willingness to cannibalize technologies from other missions has allowed them to put together the Mars mission for relatively low cost. About 77 percent of the spacecraft is lifted from the Phoenix Mars Lander, and another 20 percent has just minor modifications. Only 3 percent of the spacecraft would need to be built from scratch or completely replaced.

Not specific enough for you? Here’s the abstract (PDF) by Bruce Banerdt and Zainab Nagin Cox…

The GEophysical Monitoring Station (GEMS) is a Phase A Discovery mission designed to fill a longstanding gap in the scientific exploration of the solar system by performing, for the first time, an in-situ investigation of the interior of Mars. This mission would provide unique and critical information about the fundamental processes governing the initial accretion of the planet, the formation and differentiation of its core and crust, and the subsequent evolution of the interior.

The scientific goals of GEMS are to understand the formation and evolution of terrestrial planets through investigation of the interior structure and processes of Mars and to determine its present level of tectonic activity and impact flux. A straightforward set of scientific objectives address these goals: 1) Determine the size, composition and physical state of the core; 2) Determine the thickness and structure of the crust; 3) Determine the composition and structure of the mantle; 4) Determine the thermal state of the interior; 5) Measure the rate and distribution of internal seismic activity; and 6) Measure the rate of impacts on the surface.

To accomplish these objectives, GEMS would carry a tightly-focused payload consisting of 3 investigations: 1) SEIS, a 6-component, very-broad-band seismometer, with careful thermal compensation/control and a sensitivity comparable to the best terrestrial instruments across a frequency range of 1 mHz to 50 Hz; 2) HP3 (Heat Flow and Physical Properties Package), an instrumented self-penetrating mole system that trails a string of temperature sensors to measure the planetary heat flux; and 3) RISE (Rotation and Interior Structure Experiment), which would use the spacecraft X-band communication system to provide precision tracking for planetary dynamical studies. The two instruments would be moved from the lander deck to the martian surface by an Instrument Deployment Arm, with an appropriate location identified using an Instrument Deployment Camera.

In order to ensure low risk within the tight Discovery cost limits, GEMS reuses the successful Lockheed Martin Phoenix spacecraft design, with a cruise and EDL system that has demonstrated capability for safe landing on Mars with well-understood costs. To take full advantage of this approach, all science requirements (such as instrument mass and power, landing site, and downlinked data volume) strictly conform to existing, demonstrated capabilities of the spacecraft and mission system.

It is widely believed that multiple landers making simultaneous measurements (a network) are required to address the objectives for understanding terrestrial planet interiors. Nonetheless, comprehensive measurements from a single geophysical station are extremely valuable, because observations constraining the structure and processes of the deep interior of Mars are virtually nonexistent. GEMS will utilize sophisticated analysis techniques specific to single-station measurements to determine crustal thickness, mantle structure, core state and size, and heat flow, providing our first real look deep beneath the surface of Mars.

Bioluminescence and Chlorophyll Fluorescence

Wednesday, June 8th, 2011

One of many interesting, fantastic details of the film “Avatar” was the bioluminescent plants — and the inter-networked biosystems on Pandora.

Why am I thinking about this? NASA just released details of maps illustrating land plant fluorescence, based on the work of several scientists who published “First observations of global and seasonal terrestrial chlorophyll fluorescence from space.” The abstract:

Remote sensing of terrestrial vegetation fluorescence from space is of interest because it can potentially provide global coverage of the functional status of vegetation. For example, fluorescence observations may provide a means to detect vegetation stress before chlorophyll reductions take place. Although there have been many measurements of fluorescence from ground- and airborne-based instruments, there has been scant information available from satellites. In this work, we use high-spectral resolution data from the Thermal And Near-infrared Sensor for carbon Observation – Fourier Transform Spectrometer (TANSO-FTS) on the Japanese Greenhouse gases Observing SATellite (GOSAT) that is in a sun-synchronous orbit with an equator crossing time near 13:00 LT. We use filling-in of the potassium (K) I solar Fraunhofer line near 770 nm to derive chlorophyll fluorescence and related parameters such as the fluorescence yield at that wavelength. We map these parameters globally for two months (July and December 2009) and show a full seasonal cycle for several different locations, including two in the Amazonia region. We also compare the derived fluorescence information with that provided by the MODIS Enhanced Vegetation Index (EVI). These comparisons show that for several areas these two indices exhibit different seasonality and/or relative intensity variations, and that changes in fluorescence frequently lead those seen in the EVI for those regions. The derived fluorescence therefore provides information that is related to, but independent of the reflectance.

Real science is never too far from science fiction, is it?

That reminds me: I should water the garden.


For Sale: Moon Rocks

Monday, May 23rd, 2011


There’s got to be a good story behind this one. Some looney wanted to sell moon rocks. Yeah, she’s from California…

A woman who tried to sell what she said was a rare piece of moon rock for $1.7 million was detained when her would-be buyer turned out to be an undercover NASA agent, officials said Friday.

The gray rocks, which are considered national treasures and are illegal to sell, were given to each U.S. state and 136 countries by then-President Richard Nixon after U.S. moon missions and can sell for millions of dollars on the black market.

NASA investigators and Riverside County sheriff’s deputies detained the woman after she met Thursday with an undercover NASA investigator at a restaurant in Lake Elsinore, about 70 miles southeast of Los Angeles, the sheriff’s office said. The investigation was conducted over several months.
Authorities swooped after the two agreed on a price and the woman, whose name has not been released, pulled out the rock.

NASA planned to conduct tests to determine whether the rock came from the moon as the woman claimed.

“We don’t know if it’s lunar material,” said Gail Robinson, deputy inspector general at the space agency.

Joseph Gutheinz, a University of Phoenix instructor and former NASA investigator who has spent years tracking down missing moon rocks, said a lunar curator at a special lab at Johnson Space Center would carry out the testing. Among the substances the rock could contain is armalcolite, a mineral first discovered on the moon and named for Neil Armstrong, Buzz Aldrin and Michael Collins, who was on the Apollo 11 lunar mission crew.

The woman has not been arrested or charged. It was unknown how she obtained the rock or came to the attention of NASA.

Gutheinz said the woman could face theft charges if the rock is genuine, or fraud charges if it is not.

What would you do with a moon rock if you had one? “That’s my moon rock.”

“You’re a looney!”

Ooh, A Pwasma Spectwometer!

Wednesday, May 18th, 2011

In addition to Cornell’s cracker-sized satellite, another part of STS-134‘s payload is WISPERS or Canary — a plasma spectrometer designed and built by the Applied Physics Lab at Johns Hopkins University in Laurel, Maryland.

Canary, a plasma spectrometer, will investigate the interaction of approaching spacecraft with the background plasma environment around the ISS and disturbances in the ionosphere caused by space vehicles. The device will also provide a better understanding of the origin and impact of plasma irregularities in the Earth’s ionosphere, and demonstrate low-cost techniques for monitoring those conditions. Canary is the second Wafer Integrated Plasma Spectrometers (WISPERS) device created by APL; engineers used innovative MicroElectroMechanical (MEMS) technology when designing WISPERS to reduce size and energy consumption while increasing sensitivity. The first WISPERS device was launched last year aboard FalconSat-5. “Canary and WISPERS will provide on-orbit data for understanding how spacecraft operations affect the natural environment,” says Robert Osiander, principal investigator for WISPERS at APL.
Canary gathers particles of plasma (an electrically-charged gas) through a hole smaller than the diameter of a human hair; the particles are then sorted according to energy and type by a titanium electrostatic analyzer less than a tenth of an inch thick. By measuring the type and energy levels of plasma around it, Canary can provide warnings of potentially hazardous operating conditions.

“Canary will add an important new tool to those we use to understand the near-Earth space environment,” says Larry Paxton, a space scientist at APL and member of the Canary team. “Canary will also demonstrate a new, cost-effective approach to supporting our nation’s operations in space.”
Canary was built by APL in coordination with the Space Physics and Atmospheric Research Center (SPARC) at the U.S. Air Force Academy, and was funded in part by the Naval Research Laboratory‘s Operationally Responsive Space (ORS) program. Canary is part of the STP-H3 payload, which is integrated and flown under the direction of the Department of Defense’s Space Test Program. Canary is scheduled to be installed on the ISS on flight day 3.

Cornell’s Cracker in Space

Tuesday, May 17th, 2011


How small can a satellite get? The answer, my rocket scientist friend, in blowing in the solar wind. It’s not big or red, but it is from Cornell University

The thin, 1-inch-square chips, in development for three years in the lab of Mason Peck, associate professor of mechanical and aerospace engineering, will be mounted to the Materials International Space Station Experiment (MISSE-8) pallet, which will be attached to the space station, exposing them to the harsh conditions of space to see how they hold up and transmit data.

Although grapefruit-size satellites have been launched before, they have functioned much like larger satellites. The flight dynamics of a chip satellite are fundamentally different from these larger “CubeSats.”

“Their small size allows them to travel like space dust,” said Peck. “Blown by solar winds, they can ‘sail’ to distant locations without fuel. … We’re actually trying to create a new capability and build it from the ground up. … We want to learn what’s the bare minimum we can design for communication from space,” Peck said.

When the MISSE-8 panel is removed and returned to Earth in a few years, the survival of the prototypes will be assessed.

The trip to space is the result of a phone call about a year ago, when one of Peck’s colleagues called to ask if he had anything small that could be ready within a few weeks time to put on the MISSE-8 pallet, as a small patch of space had opened up.

“He didn’t know that we had been working on the satellite-on-a-chip program for a long time, and over the next week we put together these prototypes,” Peck said.

The three prototypes were built entirely by three Cornell students when they were undergraduates — Ryan Zhou ’10 and doctoral candidates Zac Manchester ’09 and Justin Atchison ’10.

The prototypes are physically identical, but each transmits differently. “They all emit at the same frequency … [but] they are different and distinct from each other in ways that we can recognize on the ground,” said Peck. “That’s very important because it’s a pathfinder for something we hope to do in the future. We want to launch a huge number of these things simultaneously but still sort out which is which.”

The current prototypes are mostly made of commercial parts, but Peck’s group has partnered with Draper Lab in Boston to work on making a more space-ready prototype.

“We’re seeing such an explosion in personal electronics … all these components are super high performance, and they have far outstripped what the aerospace industry has at its disposal,” said Peck, noting that these technologies were used on the small satellites.

Cornell, he added, plays a leading role in the field of chip satellites. “We are definitely the first to launch something, and we are the first to be looking at the flight dynamics as a way to enable new ways to explore space,” he said.

Watch the local news report on this “Sputnik on a chip” from Newschannel 9/WYSR-TV

STS-134 Launch: “Good Stuff”

Monday, May 16th, 2011

Endeavour lifted-off beautifully on its final mission. Commander Mark Kelly exchanged wedding bands with Rep. Gabby Giffords, just so she could wear one from “out of this world” upon his return.

Here’s the MECO (main engine cut-off) and separation…

In the report by Al Jazeera, Gabby was reported to have said “good stuff.”

Colliding White Dwarfs

Thursday, April 7th, 2011


From the Monthly Notices of the Royal Astronomical Society, we read about two white dwarf stars that will combine to form a helium-burning star — in roughly 37,000,000 years. Get a load of this abstract

We identify SDSS J010657.39-100003.3 (hereafter J0106-1000) as the shortest period detached binary white dwarf (WD) system currently known. We targeted J0106-1000 as part of our radial velocity program to search for companions around known extremely low-mass (ELM, ~ 0.2 Msol) WDs using the 6.5m MMT. We detect peak-to-peak radial velocity variations of 740 km/s with an orbital period of 39.1 min. The mass function and optical photometry rule out a main-sequence star companion. Follow-up high-speed photometric observations obtained at the McDonald 2.1m telescope reveal ellipsoidal variations from the distorted primary but no eclipses. This is the first example of a tidally distorted WD. Modeling the lightcurve, we constrain the inclination angle of the system to be 67 +- 13 deg. J0106-1000 contains a pair of WDs (0.17 Msol primary + 0.43 Msol invisible secondary) at a separation of 0.32 Rsol. The two WDs will merge in 37 Myr and most likely form a core He-burning single subdwarf star. J0106-1000 is the shortest timescale merger system currently known. The gravitational wave strain from J0106-1000 is at the detection limit of the Laser Interferometer Space Antenna (LISA). However, accurate ephemeris and orbital period measurements may enable LISA to detect J0106-1000 above the Galactic background noise.

For a translation, let’s turn to the Smithsonian’s Christine Pulliam

Out of the 100 billion stars in the Milky Way, only a handful of merging white dwarf systems are known to exist. Most were found by Kilic and his colleagues. The latest discovery will be the first of the group to merge and be reborn.

The newly identified binary star (designated SDSS J010657.39 – 100003.3) is located about 7,800 light-years away in the constellation Cetus. It consists of two white dwarfs, a visible star and an unseen companion whose presence is betrayed by the visible star’s motion around it. The visible white dwarf weighs about 17 percent as much as the Sun, while the second white dwarf weighs 43 per cent as much. Astronomers believe that both are made of helium.

The two white dwarfs orbit each other at a distance of 140,000 miles – less than the distance from the Earth to the Moon. They whirl around at speeds of 270 miles per second (1 million miles per hour), completing one orbit in only 39 minutes.

The fate of these stars is already sealed. Because they wheel around so close to each other, the white dwarfs stir the space-time continuum, creating expanding ripples known as gravitational waves. Those waves carry away orbital energy, causing the stars to spiral closer and closer together. In about 37 million years, they will collide and merge.

When some white dwarfs collide, they explode as a supernova. However, to explode the two combined have to weigh 40 percent more than our Sun. This white dwarf pair isn’t heavy enough to go supernova. Instead, they will experience a second life. The merged remnant will begin fusing helium and shine like a normal star once more.

This binary white dwarf was discovered as part of a survey program being conducted with the MMT Observatory on Mount Hopkins, Ariz. The survey has uncovered a dozen previously unknown white dwarf pairs. Half of those are merging and might explode as supernovae in the astronomically near future.

Yeah, there’s a video…

Soyuz Wanna Get Out or What?

Wednesday, March 16th, 2011

Looks pretty tight in there, comrade. I figure the thrill of orbiting Earth in the ISS is worth the cramped quarters while getting there — and back. Welcome home, Soyuz TMA-01M.

The details, via SpaceflightNow.com

Outgoing Expedition 26 commander Scott Kelly, Soyuz TMA-01M commander Alexander Kaleri and flight engineer Oleg Skripochka undocked from the International Space Station Wednesday, plunged back into the atmosphere and descended to a snowy touchdown in Kazakhstan to close out 159-day mission. With Kaleri at the controls in the descent module’s center seat, flanked by Kelly on his right and flight engineer Skripochka to his left, the Soyuz TMA-01M undocked from the Poisk compartment atop the station’s Zvezda command module at 12:27 a.m. EDT (GMT-4).
After testing repairs to the Soyuz avionics system, Kaleri monitored a four-minute 17-second rocket firing starting at 3:03:17 a.m., slowing the ship by 258 mph to begin the fall to Earth.
The three modules making up the Soyuz TMA-01M spacecraft separated as planned just before atmospheric entry, and the central crew module carrying Kaleri, Skripochka and Kelly lined up for a fiery descent to a parachute- and rocket-assisted touchdown at 3:54 a.m. near Arkalyk in north central Kazakhstan.
Braving blowing snow, brisk winds and temperatures in the 20s, Russian recovery crews and flight surgeons, along with a NASA support team, were standing by to help the astronauts out of the cramped Soyuz descent module.

“The search and recovery forces still working to extract the crew from the Soyuz capsule, which landed safely and on its side, dragging its parachute for what I would consider to be about 25 years or so before it came to rest on its side,” said NASA spokesman Rob Navias, on the scene with recovery crews in Kazakhstan. “The crew reported to be in good shape.”
A few minutes later, Kaleri, Kelly and Skripochka had been pulled from the capsule and carried to reclining chairs. Grainy video from the landing site showed support crews bundling the crew members in blankets as they began their re-adaptation to gravity.

Because of the brutal winter conditions, the recovery team planned to fly the trio to nearby Kustanai for initial medical checks and a traditional Kazakh welcoming ceremony.

Here’s the video…