Tag Archives: water on mars?

Curiosity Rover Drills Into Mars Rock, Finds Water

Space.com
Miriam Kramer
The hole drilled into this rock target, called "Cumberland," was made by NASA's Mars rover Curiosity on May 19, 2013.
© NASA/JPL-Caltech/MSSS The hole drilled into this rock target, called “Cumberland,” was made by NASA’s Mars rover Curiosity on May 19, 2013.NASA’s Curiosity rover is continuing to help scientists piece together the mystery of how Mars lost its surface water over the course of billions of years.The rover drilled into a piece of Martian rock called Cumberland and found some ancient water hidden within it. Researchers were then able to test a key ratio in the water with Curiosity’s onboard instruments to gather more data about when Mars started to lose its water, NASA officials said. In the same sample, Curiosity also detected the first organic molecules it has found. Mission scientists announced the discovery in a news conference today (Dec. 15) at the American Geophysical Union’s convention in San Francisco, where they also unveiled Curiosity’s first detection of methane on Mars.

“It’s really interesting that our measurements from Curiosity of gases extracted from ancient rocks can tell us about loss of water from Mars,” Paul Mahaffy, Curiosity’s SAM (Sample Analysis at Mars) instrument principal investigator at NASA’s Goddard Space Flight Center in Greenbelt, Maryland, said in a statement. [Photos: The Search for Water on Mars]

Curiosity measured the ratio of deuterium (heavy hydrogen) to “normal” hydrogen. This D-to-H ratio can help scientists see how long it takes for water molecules to escape, because the lighter hydrogen molecules fly toward the upper atmosphere more freely than deuterium does.

The D-to-H ratio in Cumberland is about half the ratio found in the Martian atmosphere’s water vapor today, NASA officials said. This suggests that the planet lost much of its surface water after the Cumberland rock formed, space agency officials added in the same statement.

But the water sample is also about three times “heavier” than Earth’s oceans. This means that if Mars’ surface water started off with a D-to-H ratio like Earth’s, then most of the Martian water likely disappeared before Cumberland formed about 3.9 billion to 4.6 billion years ago.

The Cumberland measurement fills in a gap for scientists studying different epochs of Martian geological evolution. This sampling marks the first time scientists have been able to measure what the water on Mars may have been like during the Hesperian period, when this rock was formed, said Mahaffy, who is the lead author of a Mars water study published in the journal Science this week.

Previously, scientists have used Martian meteorites on Earth to sample Martian water; however, none of those space rocks date back to the Hesperian period.

“You have the whole period from 2.5 billion to 4 billion years old, and there’s no data that we have from Mars meteorites just because we haven’t found any yet, I guess,” Mahaffy told Space.com. “So, it’s very gratifying to be able to fill in that picture a little bit.”

Follow Miriam Kramer @mirikramer. Follow us @Spacedotcom, Facebook and Google+. Original article on Space.com.

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Water Found on Mars!

H2 oh my: NASA’s Curiosity rover finds water in Mars dirt

By Mike Wall

Published September 26, 2013

  • curiosity-mosaic-sol-85

    SA’s Mars rover Curiosity is a mosaic of photos taken by the rover’s Mars Hand Lends Imager taken on Sol 85, the rover’s 85th Martian day, as Curiosity was sampling rocks at a stop dubbed Rocknest in Gale Crater. Image released Sept. 26, 2013.(NASA/JPL-CALTECH/MALIN SPACE SCIENCE SYSTEMS)

  • curiosity-rocknest-closeup

    At left, a closeup view of the Mars rock target Rocknest taken by the Curiosity rover showing its sandy surface and shadows that were disrupted by the rover’s front left wheel. At right, a view of Mars samples from Curiosity’s third dirt scoop (SCIENCE/AAAS)

  • curiosity-chemin-science-result

    This image depicts the science result from the Mars rover Curiosity’s CheMin instrument, showing an X-ray diffraction of the rover’s fifth scoop of Martian dirt. The black semi-circle at the bottom is the shadow of the beam stop. Image released(SCIENCE/AAAS)

Future Mars explorers may be able to get all the water they need out of the red dirt beneath their boots, a new study suggests.

NASA’s Mars rover Curiosity has found that surface soil on the Red Planet contains about 2 percent water by weight. That means astronaut pioneers could extract roughly 2 pints of water out of every cubic foot of Martian dirt they dig up, said study lead author Laurie Leshin, of Rensselaer Polytechnic Institute in Troy, N.Y.

“For me, that was a big ‘wow’ moment,” Leshin told SPACE.com. “I was really happy when we saw that there’s easily accessible water here in the dirt beneath your feet. And it’s probably true anywhere you go on Mars.” [The Search for Water on Mars (Photos)]

The new study is one of five papers published in the journal ScienceThursday that report what researchers have learned about Martian surface materials from the work Curiosity did during its first 100 days on the Red Planet.

Soaking up atmospheric water
C
uriosity touched down inside Mars’ huge Gale Crater in August 2012, kicking off a planned two-year surface mission to determine if the Red Planet could ever have supported microbial life. It achieved that goal in March, when it found that a spot near its landing site called Yellowknife Bay was indeed habitable billions of years ago.

‘The dirt is acting like a bit of a sponge and absorbing water from the atmosphere.’

– Laurie Leshin, of Rensselaer Polytechnic Institute 

But Curiosity did quite a bit of science work before getting to Yellowknife Bay. Leshin and her colleagues looked at the results of Curiosity’s first extensive Mars soil analyses, which the 1-ton rover performed on dirt that it scooped up at a sandy site called Rocknest in November 2012.

Using its Sample Analysis at Mars instrument, or SAM, Curiosity heated this dirt to a temperature of 1,535 degrees Fahrenheit, and then identified the gases that boiled off. SAM saw significant amounts of carbon dioxide, oxygen and sulfur compounds — and lots of water on Mars.

SAM also determined that the soil water is rich in deuterium, a “heavy” isotope of hydrogen that contains one neutron and one proton (as opposed to “normal” hydrogen atoms, which have no neutrons). The water in Mars’ thin air sports a similar deuterium ratio, Leshin said.

“That tells us that the dirt is acting like a bit of a sponge and absorbing water from the atmosphere,” she said.

Some bad news for manned exploration
SAM detected some organic compounds in the Rocknest sample as well — carbon-containing chemicals that are the building blocks of life here on Earth. But as mission scientists reported late last year, these are simple, chlorinated organics that likely have nothing to do with Martian life. [The Hunt for Martian Life: A Photo Timeline]

Instead, Leshin said, they were probably produced when organics that hitched a ride from Earth reacted with chlorine atoms released by a toxic chemical in the sample called perchlorate.

Perchlorate is known to exist in Martian dirt; NASA’s Phoenix lander spotted it near the planet’s north pole in 2008. Curiosity has now found evidence of it near the equator, suggesting that the chemical is common across the planet. (Indeed, observations by a variety of robotic Mars explorers indicate that Red Planet dirt is likely similar from place to place, distributed in a global layer across the surface, Leshin said.)

The presence of perchlorate is a challenge that architects of futuremanned Mars missions will have to overcome, Leshin said.

“Perchlorate is not good for people. We have to figure out, if humans are going to come into contact with the soil, how to deal with that,” she said.

“That’s the reason we send robotic explorers before we send humans — to try to really understand both the opportunities and the good stuff, and the challenges we need to work through,” Leshin added.

A wealth of discoveries
The four other papers published in Science today report exciting results as well.

For example, Curiosity’s laser-firing ChemCam instrument found a strong hydrogen signal in fine-grained Martian soils along the rover’s route, reinforcing the SAM data and further suggesting that water is common in dirt across the planet (since such fine soils are globally distributed).

Another study reveals more intriguing details about a rock Curiosity studied in October 2012. This stone — which scientists dubbed “Jake Matijevic” in honor of a mission team member who died two weeks after the rover touched down — is a type of volcanic rock never before seen on Mars.

However, rocks similar to Jake Matijevic are commonly observed here on Earth, especially on oceanic islands and in rifts where the planet’s crust is thinning out.

“Of all the Martian rocks, this one is the most Earth-like. It’s kind of amazing,” said Curiosity lead scientist John Grotzinger, a geologist at the California Institute of Technology in Pasadena. “What it indicates is that the planet is more evolved than we thought it was, more differentiated.”

The five new studies showcase the diversity and scientific value ofGale Crater, Grotzinger said. They also highlight how well Curiosity’s 10 science instruments have worked together, returning huge amounts of data that will keep the mission team busy for years to come.

“The amount of information that comes out of this rover just blows me away, all the time,” Grotzinger told SPACE.com. “We’re getting better at using Curiosity, and she just keeps telling us more and more. One year into the mission, we still feel like we’re drinking from a fire hose.”

The road to Mount Sharp
The pace of discovery could pick up even more. This past July, Curiosity left the Yellowknife Bay area and headed for Mount Sharp, which rises 3.4 miles into the Martian sky from Gale Crater’s center.

Mount Sharp has been Curiosity’s main destination since before the rover’s November 2011 launch. Mission scientists want the rover to climb up through the mountain’s foothills, reading the terrain’s many layers along the way.

“As we go through the rock layers, we’re basically looking at the history of ancient environments and how they may be changing,” Grotzinger said. “So what we’ll really be able to do for the first time is get a relative chronology of some substantial part of Martian history, which should be pretty cool.”

Curiosity has covered about 20 percent of the planned 5.3-mile trek to Mount Sharp. The rover, which is doing science work as it goes, may reach the base of the mountain around the middle of next year, Grotzinger said.

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NASA confirms history of water on Mars

NASA confirms Curiosity rover found evidence of ancient stream on Mars

Published May 31, 2013

FoxNews.com

  • gravel river mars.jpg

    The Link outcrop of rocks on Mars (left) with similar rocks seen on Earth (right). The image of Link, obtained by NASA’s Curiosity rover, shows rounded gravel fragments, or clasts, up to a couple inches within the rock outcrop. (NASA/JPL-Caltech/MSSS and PSI)

  • marsstream12.jpg

    This image taken by the NASA rover Curiosity shows sediment at the bottom of an ancient streambed on Mars. (AP/NASA)

A new analysis of pebble-containing slabs investigated by NASA’s Curiosity rover confirms a stream once ran through Gale Crater on Mars.
During a pit stop last year, Curiosity came upon hundreds of smooth, round pebbles that look strikingly similar to deposits in river banks on Earth.

‘Most people are familiar with rounded river pebbles. Seeing something so familiar on another world is exciting.’

– Rebecca Williams of the Planetary Science Institute 

Scientists believe the rover rolled onto an ancient streambed, but needed to study the stones in more detail. So Curiosity snapped high-resolution pictures and fired its laser at several pebbles to analyze the chemical makeup.

Researchers say the roundness of the stones was shaped by a fast-flowing stream that probably was ankle to waist-deep. Curiosity landed in the crater near the equator last summer.

Rebecca Williams of the Planetary Science Institute, the lead author of the new report, said that researchers were able to determine the depth and speed of the water that once flowed at the site.

“These conglomerates look amazingly like streambed deposits on Earth,” Williams said. “Most people are familiar with rounded river pebbles. Maybe you’ve picked up a smoothed, round rock to skip across the water. Seeing something so familiar on another world is exciting and also gratifying.”

Sanjeev Gupta, a co-author of the report, said that analysis of the amount of rounding on the pebbles indicates that the stream was flowing at a sustained, vigorous speed.

“The rounding indicates sustained flow. It occurs as pebbles hit each other multiple times. This wasn’t a one-off flow. It was sustained, certainly more than weeks or months, though we can’t say exactly how long,” Gupta said.

The stream carried the gravel at least a few miles, the researchers estimated.

The analysis appears in Friday’s issue of the journal Science.

The Associated Press contributed to this report.

Read more: http://www.foxnews.com/science/2013/05/31/rounded-pebbles-on-mars-reveal-past-flowing-water/?intcmp=features#ixzz2V24BCUAn

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Oldest Water On Earth Found

I remember an episode of Dr. Who where they found really old water at the core of a planet.  As I recall, that did not go that well…

Oldest Water on Earth Found Deep Underground

The finding suggests ancient life might be found within Earth and on Mars 

BY LIVE SCIENCE


A scientists takes a sample of water from a mine deep underground in Ontario, Canada. The water turned out to be 2.6 billion years old, the oldest known water on Earth. (B. Sherwood Lollar et al.)

A pocket of water some 2.6 billion years old – the most ancient pocket of water known by far, older even than the dawn of multicellular life – has now been discovered in a mine 2 miles below the Earth’s surface.

The finding, announced in the May 16 issue of the journal Nature, raises the tantalizing possibility that ancient life might be found deep underground not only within Earth, but insimilar oases that may exist on Mars, the scientists who studied the water said.

Geoscientist Barbara Sherwood Lollar at the University of Toronto and her colleagues have investigated deep mines across the world since the 1980s. Water can flow into fractures in rocks and become isolated deep in the crust for many years, serving as a time capsule of what their environments were like at the time they were sealed off.

In gold mines in South Africa 1.7 miles (2.8 kilometers) deep, the scientists previouslydiscovered microbes could survive in pockets of water isolated for tens of millions of years. These reservoirs were many times saltier than seawater, “and had chemistry in many ways similar to hydrothermal vents on the bottom of the ocean, full of dissolved hydrogen and other chemicals capable of supporting life,” Sherwood Lollar said. [Strangest Places Where Life Is Found on Earth]

To see what other ancient pockets of water might exist, Sherwood Lollar and her colleagues investigated copper and zinc mines near the city of Timmins in Ontario, Canada. “As the prices of copper, zinc and gold have gone up, mines now go deeper, which has helped our search for long-isolated reservoirs of water hidden underground,” Sherwood Lollar said.

‘Mind-blowing’ find

“Sometimes we went down in cages – they’re not called elevators underground – that dropped us to the levels we wanted to go,” Sherwood Lollar told OurAmazingPlanet. “Other times, we went down ramp mines, which have curling spiral roadways, so we could actually drive all the way down.”

The scientists analyzed water they found 2 miles deep. They focused on noble gases such as helium, neon, argon and xenon. Past studies analyzing bubbles of air trapped within ancient rocks found that these rare gases could occur in distinct ratios linked with certain eras of Earth’s history. As such, by analyzing the ratios of noble gases seen in this water, the researchers could deduce the age of the water.

The scientists discovered the fluids were trapped in the rocks between 1.5 billion and 2.64 billion years ago.

“It was absolutely mind-blowing,” Sherwood Lollar said. “These weren’t tens of millions of years old like we might have expected, or even hundreds of millions of years old. They were billions of years old.”

The site was formed by geological activity similar to that seen in hydrothermal vents. “We walked along what used to be ocean floor 2.7 billion years ago,” Sherwood Lollar said. “You could still see some of the same pillow lava structures now seen on the bottom of the ocean.”

Signs of life?

This ancient water poured out of the boreholes the team drilled in the mine at the rate of nearly a half-gallon per minute. It remains uncertain precisely how large this reservoir of water is.

“This is an extremely important question and one that we want to pursue in our future work,” Sherwood Lollar said. “We also want to see if there are habitable reservoirs of similar age around the world.”

Sherwood Lollar emphasized they have not yet found any signs of life in the water from Timmins. “We’re working on that right now,” she said. “It’d be fascinating to us if we did, since it’d push back the frontiers of how long life could survive in isolation.”

And the implications of such a finding would extend beyond the extremes of life on Earth.

“Finding life in this energy-rich water is especially exciting if one thinks of Mars, where there might be water of similar age and mineralogy under the surface,” Sherwood Lollar said.

If any life once arose on Mars billions of years ago as it did on Earth, “then it is likely in the subsurface,” Sherwood Lollar said. “If we find the water in Timmins can support life, maybe the same might hold true for Mars as well.”

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