Solar Power Breakthrough :A New Process Stores Energy for Later Use

Within 10 years, homeowners could power their homes in daylight with solar photovoltaic cells, while using excess solar energy to produce hydrogen and oxygen from water to power a household fuel cell. If the new process developed at the Massachusetts Institute of Technology finds acceptance in the marketplace, electricity-by-wire from a central source could be a thing of the past.

“This is the nirvana of what we’ve been talking about for years,” said MIT’s Daniel Nocera, senior author of a paper describing the simple, inexpensive, and efficient process for storing solar energy in the July 31 issue of the journal “Science.”

“Solar power has always been a limited, far-off solution. Now we can seriously think about solar power as unlimited and soon,” Nocera said.

Until now, solar power has been a daytime-only energy source, because storing extra solar energy for later use is expensive and inefficient. But Nocera and his team of researchers have hit upon an elegant solution.
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Signs of Hidden Ocean Underneath Titan’s Crust

A strange shift in the position of mountains and lakes on the surface of Saturns moon Titan can best be explained, researchers say, by positing a layer of liquid water (blue) some 100 kilometers below the surface.NASA-JPL

TITAN'S HIDDEN OCEAN: A strange shift in the position of mountains and lakes on the surface of Saturn's moon Titan can best be explained, researchers say, by positing a layer of liquid water (blue) some 100 kilometers below the surface.NASA-JPL

Astronomers’ mental image of Titan, the solar system’s second-largest moon, used to be that of a vast swimming pool. But maybe they should have imagined a water bed instead.

Last year, researchers reported that radar mapping of Titan by the Cassini spacecraft had found a peculiar shift in landmarks on the moon’s surface of up to 19 miles (30 kilometers) between October 2004 and May 2007.

Now investigators say the best explanation is a moon-wide underground ocean that disconnects Titan’s icy crust from its rocky interior.

“We think the structure is about 100 kilometers of ice sitting atop a global layer of water … maybe hundreds of kilometers thick,” says Cassini scientist Ralph Lorenz of Johns Hopkins University Applied Physics Laboratory in Laurel, Md.

If confirmed, Titan would be the fourth moon in the solar system thought to contain such an internal water ocean, joining Jupiter’s satellites Ganymede, Callisto and Europa. Researchers believe that heat from radioactivity in a moon’s core or gravitational squeezing may melt a layer of frozen water.
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Scientists Confirm Liquid on Saturn’s Moon Titan

In this natural color view, taken by the Cassini spacecraft in 2007, Titans surface is shrouded by a thick, orange haze

SMOGGY MOON: In this natural color view, taken by the Cassini spacecraft in 2007, Titan's surface is shrouded by a thick, orange haze

NASAs Cassini orbiter captured this view of Titans Ontario Lacus from about 680 miles (1,100 kilometers) away in December 2007. A bright shoreline surrounds the hydrocarbon lake.

NASA's Cassini orbiter captured this view of Titan's Ontario Lacus from about 680 miles (1,100 kilometers) away in December 2007. A bright shoreline surrounds the hydrocarbon lake.

Researchers report in Nature  that they identified a dark liquid lake, surrounded by a lighter shoreline and a “beach,” on the surface of Saturn’s moon Titan. The foot-shaped lake is the first verified extraterrestrial body of liquid, and is likely filled with hydrocarbons, simple compounds also common on Earth.

“This is the first definitive evidence for both liquid and liquid hydrocarbons on Titan,” says lead study author Robert Brown, a professor of planetary science at the University of Arizona’s Lunar and Planetary Laboratory (LPL) in Tucson.
Instruments on NASA’s orbiting Cassini spacecraft, which has studied Saturn and its satellites including Titan, its biggest moon, since June 2004, revealed the presence of the organic (carbon-containing compound) liquid ethane in a Lake Ontario–size body in Titan’s southern hemisphere. Similar-looking patches abound in the northern hemisphere, indicating that Titan’s surface is likely dotted with such hydrocarbon seas.

The researchers confirmed the presence of liquid ethane with Cassini’s Visible and Infrared Mapping Spectrometer (VIMS), which picked up the hydrocarbon’s telltale light spectrum signature. The ethane forms when sunlight breaks down methane in Titan’s upper atmosphere. It is theorized that this ethane then forms clouds and rains onto the ground, cutting streams via erosion and pooling them into lakes.

Titan has long fascinated astronomers with its hazy, orange-colored atmosphere that extends over 600 miles (965 kilometers) from the moon’s surface. Titan is the only moon with such a thick gas cover. The atmosphere contains mostly nitrogen and traces of methane and other hydrocarbons including propane, the fuel of choice for barbecues here on Earth. With a diameter of 3,200 miles (5,150 kilometers), Titan is bigger than Mercury and only about 25 percent smaller than Mars, making it the second-biggest moon in the solar system behind Jupiter’s Ganymede.

Liquid ethane or methane has been suspected to exist on the Titanian surface. This finding supports the idea that Titan has a “hydrological cycle” as does Earth, but instead of water (forming clouds, raining out and evaporating into clouds again), there are two substances—methane and ethane—at play, says study co-author Christophe Sotin, a planetary scientist at NASA’s Jet Propulsion Laboratory in Pasadena, Calif.

In addition to ending the debate over liquid on Titan, the discovery may help determine the course of future missions. NASA and the European Space Agency have been discussing a return to Titan; this finding bolsters the case for sending a “splashdown lander,” or a floating probe, into a lake on Titan to sample its contents, says Ralph Lorenz, a planetary scientist at the Johns Hopkins University Applied Physics Laboratory in Laurel, Md.

The liquid pool, named Ontario Lacus after the North American Great Lake of similar size, absorbs nearly all light, which means it would look dark to the human eye, says LPL’s Brown. The data also reveals that the lake’s surface is smooth, without any ripples or waves, which Brown says is surprising. He and his team had expected to see some wave action caused by presumed winds there.
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NASA Spacecraft Confirms Water on Mars

Laboratory tests aboard NASA’s Phoenix Mars Lander have identified water in a soil sample. The lander’s robotic arm delivered the sample Wednesday to an instrument that identifies vapors produced by the heating of samples.

“We have water,” said William Boynton of the University of Arizona, lead scientist for the Thermal and Evolved-Gas Analyzer, or TEGA. “We’ve seen evidence for this water ice before in observations by the Mars Odyssey orbiter and in disappearing chunks observed by Phoenix last month, but this is the first time Martian water has been touched and tasted.”

With enticing results so far and the spacecraft in good shape, NASA also announced operational funding for the mission will extend through Sept. 30. The original prime mission of three months ends in late August. The mission extension adds five weeks to the 90 days of the prime mission.

“Phoenix is healthy and the projections for solar power look good, so we want to take full advantage of having this resource in one of the most interesting locations on Mars,” said Michael Meyer, chief scientist for the Mars Exploration Program at NASA Headquarters in Washington.

The soil sample came from a trench approximately 2 inches deep. When the robotic arm first reached that depth, it hit a hard layer of frozen soil. Two attempts to deliver samples of icy soil on days when fresh material was exposed were foiled when the samples became stuck inside the scoop. Most of the material in Wednesday’s sample had been exposed to the air for two days, letting some of the water in the sample vaporize away and making the soil easier to handle.

“Mars is giving us some surprises,” said Phoenix principal investigator Peter Smith of the University of Arizona. “We’re excited because surprises are where discoveries come from. One surprise is how the soil is behaving. The ice-rich layers stick to the scoop when poised in the sun above the deck, different from what we expected from all the Mars simulation testing we’ve done. That has presented challenges for delivering samples, but we’re finding ways to work with it and we’re gathering lots of information to help us understand this soil.”

Since landing on May 25, Phoenix has been studying soil with a chemistry lab, TEGA, a microscope, a conductivity probe and cameras. Besides confirming the 2002 finding from orbit of water ice near the surface and deciphering the newly observed stickiness, the science team is trying to determine whether the water ice ever thaws enough to be available for biology and if carbon-containing chemicals and other raw materials for life are present.

The mission is examining the sky as well as the ground. A Canadian instrument is using a laser beam to study dust and clouds overhead.

“It’s a 30-watt light bulb giving us a laser show on Mars,” said Victoria Hipkin of the Canadian Space Agency.

“The details and patterns we see in the ground show an ice-dominated terrain as far as the eye can see,” said Mark Lemmon of Texas A&M University, lead scientist for Phoenix’s Surface Stereo Imager camera. “They help us plan measurements we’re making within reach of the robotic arm and interpret those measurements on a wider scale.”

THE MISSION
The University of Arizona is honored to be the first public university to lead a mission to Mars. The Phoenix Mars Mission, scheduled to land May 25, 2008, is the first in NASA’s “Scout Program.” Scouts are designed to be highly innovative and relatively low-cost complements to major missions being planned as part of the agency’s Mars Exploration Program.

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