Environment-Clean-Generations

Environment-Clean-Generations
THE DEFINITIVE BLOG FOR EVERYTHING YOU NEED TO KNOW ABOUT THE ENVIRONMENT YOU LIVE IN, WITH REFERENCE TO LIFE, EARTH AND COSMIC SPACE SCIENCES, PRESENTED BY ENVIRONMENTAL ENGINEER DORU INDREI, ENVIRONMENTAL QUALITY AND ENERGY SPACIALIST
"Life is not about what we know, but what we don't know, craving the unthinkable makes it so amazing, that is worth dying for." Doru Indrei
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Showing posts with label mars. Show all posts
Showing posts with label mars. Show all posts

Huge Avalanche near Mars's North Pole



A Nasa spacecraft has captured an avalanche of fine ice and dust thundering over a cliff near Mars's north pole. 

It's not the first avalanche captured by the HiRISE camera aboard the Mars Reconnaissance Orbiter - Nasa first detected the phenomenon in 2008, believed to be caused by a thin 'crust' of frozen carbon dioxide (dry ice) which forms during the Martian winter. 

 Ice and dust cascade over a Martian cliff: The camera on the Mars Reconnaissance Orbiter captured the avalanche near Mars's north pole

The HiRISE high resolution camera took the amazing photograph at 85 degrees north on the planet.
The HiRISE camera is one of several hi-tech instruments on board Mars Reconnaissance Orbiter. It's the largest camera ever carried into deep space.
Nasa's ground team says that the events are detectable by a cloud of fine material that erupts when avalanches collapse down slopes on the planet.




Some avalanches on Mars are caused by meteorite impacts, but others are thought to be the result of 'seasons' on the planet, which has winters, just like Earth.
Planetary scientist Ingrid Daubar Spitale of the University of Arizona, who first noticed the avalanches in photos taken by the Mars Reconnaissance Orbiter said, 'It's great to see something so dynamic on Mars. A lot of what we see there hasn't changed for millions of years.'


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Fine ice and dust cascades over a martian polar cliff in March 2010 in another picture captured by the Mars Reconnaissance Orbiter's HiRISE camera.

Ancient Ocean on Mars


The European Space Agency's Mars Express has returned compelling evidence that the red planet once hosted an enormous ocean in its northern plains. The probe's radar detected sediments reminiscent of an ocean floor, within areas that have been suspected to be shorelines.
Jérémie Mouginot from the Institut de Planétologie et d'Astrophysique de Grenoble (IPAG), the University of California in Irvine, and colleagues analysed more than two years of data from Mars Express' Marsis (Mars Advanced Radar for Subsurface and Ionosphere Sounding) radar.

The radar can penetrate deep into the planet's ground, and reveal the first 60 to 80 metres of the planet's subsurface. At these depths, the team found that the northern plains are covered in low-density material.
"We interpret these as sedimentary deposits, maybe ice-rich," says Mouginot. "It is a strong new indication that there was once an ocean here."



The notion of water on Mars and big ideas of oceans in the planet's ancient history are nothing new. But this research provides some of the best evidence yet that there were once large bodies of liquid water on Mars, and it is further proof that water played a role in martian geological history.
"Previous Mars Express results about water on Mars came from the study of images and mineralogical data, as well as atmospheric measurements," said Olivier Witasse, a Mars Express project scientist at the European Space Agency.


This data supports a proposed theory where Mars has had two oceans in its lifetime. One four billion years ago when warmer conditions prevailed, and another three billion years go when subsurface ice melted following a large impact.

This later ocean would have been very temporary. It would only have lasted about a million years or less, Mouginot estimates, and then the water would have either frozen back in place or turned into vapour and lifted gradually into the planet's weak atmosphere.

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"I don't think it could have stayed as an ocean long enough for life to form," Mouginot says.
A recent study from Imperial College London doesn't offer much good news for martian life-hunters, either. Soil analysis at the site of Nasa's Phoenix mission suggest that surface of Mars has dry as a bone for hundreds of millions of years, making it too hostile for any life to survive on the planet's surface

A Portion of Mars could be Friendly to Life


Sunrise at Gale Crater Gale Crater, future home of the Mars Science Laboratory, looms in the distance, distinguished from adjacent craters by its central mountain. Gale Crater straddles the dichotomy boundary of Mars, which separates the broad, flat, and young northern plains from the much older and rougher southern highlands. Water may have flowed across this topographic boundary, from highland to lowland. Last week, the Opportunity rover team found slam-dunk evidence of liquid water on the surface of Mars, an intriguing find for astrobiology. NASA/JPL-Caltech

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Now that we have slam-dunk evidence that Mars was once a wet and likely temperate place, astrobiologists are pondering the implications for ancient Martian life. One new study says the Red Planet has even more habitable space than Earth — albeit underground.

Led by Charley Lineweaver at the Australian National University, researchers compared models of temperature and pressure conditions on Earth with those on Mars, extrapolating how much of Mars might be amenable to hosting Earth-like organisms. Life occupies just one percent of Earth, if you consider the entire planet’s volume from the core to the stratosphere. But apparently three percent of Mars could be habitable, Lineweaver said. Most of this comfortable space is underground, where there would be sufficient pressure and warmth to hold liquid water and perhaps some toasty microbes.



Although the Phoenix lander found ice at the north pole, modern Mars’ surface is too low-pressure to hold on to liquid water, and it’s too cold (average about -81 °F) for water or life as we know it. But nestled underneath the planet’s crust, the habitat could be much more friendly, Lineweaver told AFP.
Lineweaver said his study uses decades of data from a host of Mars missions and compiles information about several sites, rather than just one or two areas. “There are large regions of Mars that are compatible with terrestrial life,” he said.

The Mars Science Laboratory, en route to the planet for an August arrival, is designed to help answer some of these questions. It has several instruments for examining the chemical composition of rocks inside Gale Crater, a region believed to once host flowing water. The Curiosity rover also has some instruments designed to look for the chemical ingredients of life.
The Australian study was published in the journal Astrobiology.

The worms that could lead mankind's way to Mars


  • Worms can survive and reproduce in space
  • Worms found in rubbish tips share 20,000 genes with humans
  • 'Survivors' of mission returned healthy
It may be some time before man sets foot on Mars but the final frontier could soon be crossed by worms.
British scientists have successfully sent them on a mission to the International Space Station to test how they deal with space travel.
Not only did they remain healthy throughout their six-month mission but they produced 24 generations of offspring while in orbit.


Earthling: The tiny Caenorhabditis elegans soilworm is helping scientists to understand how humans could respond the rigours of inter-planetary space-flight
The team from the University of Nottingham carried out the research partly to understand how astronauts would be affected by extended journeys, such as a two-year trip to Mars.
A type of tiny worm found in rubbish tips – Caenorhabditis elegans – was deployed for the 200-mile journey because it shares more than 20,000 genes with humans and its muscles and central nervous system work in a similar way.

When the survivors – worms only live for a few weeks – returned to Earth to be studied, the scientists found they showed normal development movement, feeding patterns, and the capacity to reproduce.
The research could also help scientists understand more about muscle-wasting diseases such as muscular dystrophy.
Space travel in zero-gravity conditions can cause dramatic muscle wastage in astronauts, as it appears to reduce the level of the protein myosin which keeps them strong. 

Space calling: The worms were kept aboard the International Space Station for six months, during which time they showed no adverse effects
Dr Nathaniel Szewczyk, who led the study, said it showed worms could be a successfully used as guinea pigs to test conditions on Mars.
He said: ‘While this sounds like science fiction, a fair number of scientists agree that we could colonize other planets, and will one day need to if mankind wants to avoid extinction.
‘Given the high cost of manned space missions and high failure rate for Mars missions we suggest that these worms as a cheap model to test some of the biological effects of long-distance space travel.
‘It may seem surprising but many of the biological changes that happen during spaceflight affect astronauts nad worms in the same ways.’
His team did a previous test in 2009 where they sent worms to space but only for four days before they were frozen for the return journey.
Dailymail

Curiosity Will Carry Your Name to Mars!


Yes indeed! Those how enrolled to this competition will have the chance that now, on Saturday, november 26 2011, their names will get to Mars with the help of Curiosity rover; the possibility of sending your name to mars started back in 2009.  

Nasa will launch its car-size Curiosity rover this week in it's most expensive and scientifically complicated bid yet to discover if there was ever life on Mars.
Curiosity, which is the prize of Nasa's $2.5 billion Mars Science Laboratory mission, will be launched from Florida's Cape Canaveral Air Force Station on Saturday.
'This is a Mars scientist's dream machine,' Ashwin Vasavada, MSL deputy project scientist at Nasa's Jet Propulsion Laboratory (JPL) in Pasadena, told reporters at a press conference on November 10. 



Curiosity: Nasa will launch its car size rover this Saturday, in this picture the rover examines a rock on Mars with a set of tools at the end of the rover's arm, which extends about 2 meters.

'This rover is not only the most technically capable rover ever sent to another planet, but it's actually the most capable scientific explorer we've ever sent out.'
Curiosity started it's life designed in 2004 and at one ton it weighs five times more than its Mars rover predecessors Spirit and Opportunity.
During the 23 months after landing, Curiosity will analyze dozens of samples drilled from rocks or scooped from the ground as it explores with greater range than any previous Mars rover.
Mission of discovery: Highlighted Russian-built, neutron-shooting instrument on the Curiosity rover of NASA's Mars Science Laboratory mission will check for water-bearing minerals in the ground beneath the rover.
Launch: Nasa graphic detailing the launch (which has now been delayed to Saturday) and the arrival back to earth

Curiosity will also carry the most advanced load of scientific gear ever used on Mars’ surface, a more than 10 times as massive as those of earlier Mars rovers.

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Curiosity is about twice as long and five times as heavy as NASA’s twin Mars Exploration Rovers, Spirit and Opportunity, launched in 2003. 
But it inherited many design elements from them, including six-wheel drive, a rocker-bogie suspension system and cameras mounted on a mast to help the mission’s team on Earth select exploration targets and driving routes. 



Unlike earlier rovers, Curiosity carries equipment to gather samples of rocks and soil, process them and distribute them to onboard test chambers inside analytical instruments.
It has a robotic arm which deploys two instruments, scoops soil, prepares and delivers samples for analytic instruments and brushes surfaces.
Its assignment is to investigate whether conditions have been favorable for microbial life and for preserving clues in the rocks about possible past life.
The goal of the mission is to assess whether the landing area has ever had or still has environmental conditions favorable to microbial life.
Curiosity will land near the foot of a layered mountain inside Gale crater, layers of this mountain contain minerals that form in water.
The portion of the crater floor where Curiosity will land has an alluvial fan likely formed by water-carried sediments.


Size: Showing the scale of the car-size rover against a 7ft man

Selection of Gale followed consideration of more than 30 locations by more than 100 scientists participating in a series of open workshops.
Because the Gale landing site is so close to the crater wall, it would not have been considered safe if the mission were not using this precision.
Advancing the technologies for precision landing of a heavy payload will yield research benefits beyond the returns from Mars Science Laboratory itself.
Those same capabilities would be important for later missions both to pick up rocks on Mars and bring them back to Earth, and conduct extensive surface
exploration for Martian life.

NASA Television’s countdown launch commentary begins at 4:30 a.m. PST (7:30 a.m. EST) on November 26.



Environment Clean Generations
Dailymail

Russia Aims for First Conquest of Mars

Russian Federal Space Agency specialists work with the Phobos-Grunt spacecraft as they prepare to mount it on board a Zenit rocket at the Baikonur cosmodrome in Kazakhstan in October 2011. Russia on Wednesday launches a probe for Mars that aims to collect a chunk of a Martian moon and become Moscow's first successful planetary mission since the collapse of the Soviet Union.
Russia on Wednesday launches a probe for Mars that aims to collect a chunk of a Martian moon and become Moscow's first successful planetary mission since the collapse of the Soviet Union.


The Phobos-Grunt probe is to blast off from the Baikonur cosmodrome in Kazakhstan on a Zenit-2SB rocket at 00:16 am Moscow time (2016 GMT Tuesday), Russia's space agency said in a statement.
Russia hopes the mission will mark a triumphant return to interplanetary exploration, a field from which it has been entirely absent over the last decades even as US probes explored the farthest reaches of the solar system.
If successful, Phobos-Grunt will also help erase the memory of one of Russia's worst ever space failures, when its Mars-96 probe bound for the Red Planet failed to reach orbit and crashed into the ocean in 1996.Environment Clean Generations
Russia is desperate to show it remains a superpower in and is still inspired by the daring spirit of first man in space , in the year it celebrated the 50th anniversary of his historic voyage.
"If Phobos-Grunt fully carries out its mission, then this will be a world class achievement," said Igor Lisov, editor-in-chief of the specialist journal Novosti Kosmonavtiki (Space News).


"The problem with Russian space exploration has been that people have forgotten the taste of victory. The task of this mission is to restore confidence in our abilities and the importance of the task," he told AFP.
The voyage also comes as the world's space powers are showing renewed interest in the possibility of sending a man to in the next decades, possibly in the 2030s.
An undated hand out computer generated image shows a planting unit cowling of the Phobos-Grunt space project. The Phobos-Grunt probe is to blast off from the Baikonur cosmodrome in Kazakhstan on a Zenit-2SB rocket at 00:16 am Moscow time.Environment Clean Generations
Last week six men emerged from 520 days in isolation in Moscow after an unprecedented experiment that attempted to test the psychological and physiological effects of a return trip to Mars. But even in the heyday of Soviet space exploration, Moscow had little luck with Mars. It sent a number of failed missions as NASA enjoyed great success with its Mariner and Viking probes, the latter of which landed on the Red Planet.

The Soviet Union sent its last probes to Mars -- both named Phobos -- in the late 1980s. But the first failed to reach a Martian orbit and the second failed when contact was lost shortly after its arrival.
Most humiliating was the failure of the ambitious Mars-96 probe in November 1996 which broke up over the Pacific Ocean in a disaster that appeared to symbolise the disintegration of the Russian space programme at the time.
The main aim of the Phobos-Grunt mission is to bring back the first ever soil sample from Phobos, the larger of Mars' two moons (the other is called Deimos).

In a landmark space cooperation between Moscow and Beijing, the probe is also expected to deploy a Chinese satellite, Yinghuo-1, which will go into orbit around Mars and observe the planet itself.
If all goes to plan, Phobos-Grunt should reach Mars in 2012 and then deploy its lander for Phobos in 2013 before returning the sample back to Earth in August 2014.

Phobos, which orbits Mars at a radius of just under 10,000 kilometres, is believed to be the closest moon to its planet anywhere in the solar system and scientists hope it will reveal secrets about the origins of the planets.
The probe is carrying numerous international experiments including a capsule of microbes prepared by the US Planetary Society to see if basic life forms can survive on a long mission in deep space.
Phobos-Grunt was to have been launched in 2009 but the date was put back until 2011, the soonest possible launch window when the planet's relative proximity to Earth makes a voyage feasible.

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Mars 500 "We're Ready To Go"


Six-strong crew will emerge from spacecraft at Russian facility on Friday

Project aimed to simulate effects of journey to Red Planet

Carried out experiments and a 'space walk' in Moscow car park

Scientists will need a year to sift through data before deciding next step



Six astronauts will 'return home' this week after spending 520 days in a windowless capsule on a simulated mission to Mars.
They will emerge from their spacecraft - an isolation facility at the Russian Institute for Biomedical Problems (RIBP) in Moscow - on Friday.

But they are already looking forward triumphantly to the ever-realistic possibility of sending man to the Red Planet for real.
The last leg: The Mars500 crew, pictured here in September, will finally emerge from their capsule in Russian on Friday after a 520-day mock mission to Mars. One of the astronauts on board, French engineer Romain Charles, said in a recent diary entry: 'Our international crew went through the Mars500 mission successfully and we're happy and proud to answer positively to the question asked a year-and-a-half ago: 'Is man able to endure, physiologically and psychologically, the confinement of a trip to Mars?' Yes, we're ready to go!'

The $15million Mars500 project is being conducted by the European Space Agency (ESA) and the RIBP with the aim of imitating a complete mission to Mars.
Since the astronauts boarded on June 3 last year, they have undergone experiments, carried out 'Mars Walks' in a car park outside a Moscow block of flats and monitored their own mental health and wellbeing.

Collating data: The crew conducted various experiments on themselves to understand the physical and psychological demands of a long space mission. But perhaps importantly, they weren't able to simulate anti-gravity.

To make the simulation realistic, the crew experienced delayed communication with mission controllers at certain points during the trip.                                                                 
Researchers hope to use data to better understand the physical and psychological challenges that astronauts will face on real deep-space journey.
However, they were not able to re-create the effects of gravity or radiation, leaving some potential gaps in their results.


Astronaut Christer Fuglesang, who heads the science and application division at the Directorate of Human Spaceflight and Operations at ESA, told Space.com: 'The length of Mars500 is unique — there has never been such a long isolation before, so that gives you unique data. 

'From a logistics and communications point of view, it was quite realistic. Of course, there are certain aspects that you cannot simulate. You cannot simulate weightlessness or radiation, for example.'
The project was also useful in determining at what point in long-duration flights humans struggle most - and finding ways to help astronauts cope.


'They have had their ups and downs, but these were to be expected,' Patrik Sundblad, a human life sciences specialist at ESA, said.
'August was the mental low point: it was the most monotonous phase of the mission, their friends and families were on vacation and didn't send so many messages, and there was also little variation in food.

'But we didn't have any kind of hiccup or crisis inside. I did not expect anything major, but it's still been going even better than I could hope for. I'm astonished.'
The crew - made up of Mr Charles, Italian engineer Diego Urbina, Russian physiologist Alexandr Smoleevski, Russian surgeon Sukhrob Kamolov, Russian engineer Alexey Sitev and Chinese astronaut trainer Wang Yue - will remain in medical quarantine for at least three days after they emerge from the hatch.

It is expected to take scientists about a year to analyse the results and decide what step to take next.



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Discovery of how Water was Present on Earth and Mars


The discovery of the mineral jarosite in rocks analyzed by the Mars Rover, Opportunity, on the Martian surface had special meaning for a team of Syracuse University scientists who study the mineral here on Earth. Jarosite can only form in the presence of water. Its presence on Mars means that water had to exist at some point in the past. The trick is in figuring out if jarosite can be used as a proxy for determining when, and under what conditions, water was present on the planet.

The SU scientists have done just that. In a recent study published in an October issue issue of Earth and Planetary Science Letters, Suzanne Baldwin, professor of Earth Sciences in SU's College of Arts and Sciences; and Joseph Kula, research associate and corresponding author for the study, established the "diffusion parameters" for argon in jarosite. In simpler terms, they discovered a way to use the noble gas argon, which accumulates in jarosite over time, to determine the age of the mineral and the surface conditions under which it formed.



The discovery of the mineral jarosite in rocks analyzed by the Mars Rover, Opportunity, on the Martian surface had special meaning for a team of Syracuse University scientists. (Credit: NASA)
                                                                    
The new study is the first in a series of experiments designed to provide a roadmap of sorts for scientists who may someday study Martian samples brought back to Earth. "Our experiments indicate that over billion-year timescales and at surface temperatures of 20 degrees Celsius (68 degrees Fahrenheit) or colder, jarosite will preserve the amount of argon that has accumulated since the crystal formed," Kula says, "which simply means that jarosite is a good marker for measuring the amount of time that has passed since water was present on Mars."

Moreover, since the development of life requires water, knowing when and for how long water was present on the Martian surface has implications for the search for potential habitats harboring life, the scientists say. "Jarosite requires water for its formation, but dry conditions for its preservation," Baldwin says. "We'd like to know when water formed on the surface of Mars and how long it was there. Studying jarosite may help answer some of these questions."


Jarosite is a byproduct of the weathering of rocks exposed at the surface of a planet (such as Earth and Mars). The mineral forms when the right mixture of oxygen, iron, sulfur, potassium and water is present. Once formed, the crystals begin to accumulate argon, which is produced when certain potassium isotopes in the crystals decay. Potassium decay is a radioactive process that occurs at a known rate. By measuring the isotopes of argon trapped within the crystals, scientists can determine the age of the crystals.


However, because argon is a gas, it can potentially escape rapidly from the crystals under hot conditions or slowly over long durations at cold conditions. In order to determine the reliability of the "argon clock" in jarosite, the scientists had to determine the temperature limits to which the crystals could be subjected and still retain the argon. Using a combination of experiments and computer modeling, the team found that argon remains trapped inside the crystals for long periods of time over a range of planetary surface temperatures.

"Our results suggest that 4 billion-year-old jarosite will preserve its argon and, along with it, a record of the climate conditions that existed at the time it formed," Baldwin says. The scientists are in the process of conducting further studies on jarosite that formed less than 50 million years ago in the Big Horn Basin in Wyoming, which they hope will reveal when the minerals formed and how fast environmental conditions changed from water-saturated to dry. The results can be used as a context for interpreting findings on other planets.


Baldwin and Kula are members of the NASA-funded New York Center for Astrobiology at Rensselaer Polytechnic Institute in Troy, N.Y. The center is one of 10 such centers nationally that are part of the NASA Astrobiology Institute, located at NASA's Ames Research Center at Moffett Field, Calif. Their jarosite research is funded by NASA.
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Search For Life in the Right Places


Curious about just how astrobiologists plan to make good on their goal to find life in space in the next 20 years? 


The first will take place later this year, when Russian scientists will tap Earth’s final frontier, the subglacial Antarctic lakes. Any life they find under 2.5 miles of ice in the ancient isolated waters of Lake Vostok won’t technically be extraterrestrial, of course, but it could be new and bizarre – and akin to what’s possibly living in the suspected subsurface oceans on Europa, an ice-covered moon of Jupiter. 


Martians could also be on the horizon. With all the attention the Red Planet gets, it should come as no surprise that NASA’s next big flagship mission is headed there. Later this decade the agency will begin a long-term project to bring Mars rocks back to Earth. Many think the Mars Sample Return mission could be the one that finally finds ET (even if it is a long-dead microbe, not a little green man).


If we don’t find aliens in our own backyard, they could be lurking in other solar systems. As soon as next decade, a Terrestrial Planet Finder mission -- something like the New World’s Observer telescope and starshade in our gallery -- will look for signs of life in the atmospheres of extrasolar planets around other stars.

Here on the ground, the Allen Telescope Array, the first instrument completely devoted to the search for extraterrestrial intelligence (SETI), could analyze enough star systems to come across alien radio transmissions in the next two decades – if the SETI Institute’s new crowd-sourced funding campaign pulls through. Read more about how and when we’ll find life (and what it could look like) in our online-only interview with Seth Shostak, a senior astronomer at the Institute. 


And, just for fun, we’ve also included a round-up of some of our favorite close encounters with “aliens,” including a 1966 UFO chase in Ohio and (possible) microbes on a meteorite announced earlier this year. Happy hunting!

Drilling For Extreme Life

For the past 20 million years, Lake Vostok has been sealed beneath the Antarctic ice sheet. This winter, after nearly 22 years of work, Russian researchers will use mechanical and thermal drills to punch through the final 100 feet before liquid water. Microbes found in Vostok could inform the search for life on the Jovian ice moon Europa, for which a mission could launch in the next decade, and other moons in our solar system thought to contain bodies of liquid water, such as Enceladus and Ganymede.
 
Drilling For Extreme Life: How It Works

THE SITE


Vostok Station once recorded the lowest temperature on Earth: –128ºF. Fortunately for researchers, average temperatures in the austral summer hover around –33º.The Russian team will commence drilling in December. Once scientists reach liquid water, they will allow water to rise up the borehole and freeze over the winter. They will return to Vostok Station in December 2012 to test the core for life.


THE DRILL


A thermal drill tethered to a power cable from the surface will penetrate the final 30 feet of ice. When the drill approaches the water surface, pressure and water sensors will trigger an expandable borehole packer to seal off the channel, preventing drilling fluid from contaminating the lake and allowing scientists to control how quickly the water will rise.

THE LAKE


Lake Vostok, one of the world’s largest lakes by volume, contains more than 1,000 cubic miles of water. At its farthest depths, some 14,000 feet below the surface, pressure reaches up to 438 atmospheres. If drilled improperly, the pressurized water could race up the borehole, causing an explosion powerful enough to destroy Vostok Station.
  
Bringing Mars Home

To determine whether life lives or has lived on Mars, scientists will most likely need to bring a sample of the planet back to Earth. The threestage NASA-ESA Mars Sample Return mission, scheduled to run from 2018 to 2027, will involve rovers, a launcher, and an orbiter equipped with an Earth Entry Vehicle (EEV) that will carry the rocks to Earth for testing. 

PHASE ONE, 2019-2021: COLLECT AND CACHE


Following launch in 2018, a rover will arrive on Mars in January 2019 and will spend nearly two years collecting rocks with a rotary coring drill. After placing as many as 40 cores in a three-inch-wide cylindrical cache, the mobile ’bot will return to its landing site and place the container on the ground.


PHASE TWO, 2025-2026: FETCH AND LAUNCH



A lander carrying the fetch rover and Mars Ascent Vehicle (MAV) will touch down on Mars in September 2025. Over the next three months, the rover will retrieve the cache—up to a nine-mile round-trip journey—and package the rocks in an 11-pound Orbiting Sample (OS) sphere stored inside the MAV. By the following May, the MAV rocket will launch and release the OS into orbit.





PHASE THREE, 2026-2027: RENDEZVOUS AND RETURN


An orbiter will arrive at Mars in the summer of 2023. The craft will use optical and radio-frequency tracking systems to monitor the OS launch and will rendezvous with the samples in around May 2026. The orbiter will capture the OS in a basket and transfer it to the onboard eeV—a three-foot-wide, impact-resistant, heat-shielded craft—before setting out for Earth. On descent to Earth in late 2027, the EEV will decouple from the orbiter and crash-land on the planet. The quarantined samples would then be safely recovered.


 Spotting Distant Life

To view life on other worlds, scientists will need to use a space-based telescope to scan for biosignatures in an exoplanet’s atmosphere while blocking out starlight that could skew results. The New Worlds Observer, a design developed at the University of Colorado, pairs an ultraviolet-optical-infrared telescope with an external starshade.

THE STARSHADE


The 160-foot-wide starshade moves independently to position itself between the telescope and the star. Its 16 “petals” diffract light away from the center of the shadow it casts onto the observatory. 

THE TELESCOPE


The observatory’s 13-foot aperture will collect enough ultraviolet and infrared light reflecting off the planet to distinguish it from interplanetary dust. Future telescope designs will also probably incorporate an internal coronagraph, a device on the instrument that will blot out starlight that slips past the shade.


 Searching For New Earths

In 1995 a Swiss team scanning the Milky Way discovered 51 Pegasi b, the first known exoplanet orbiting a sunlike star. Since then, scientists using ground-based and space telescopes have found more than 500 exoplanets in the galaxy. Currently only one, Gliese 581 d is considered a potential Earth analogue—it may even have oceans—but the number will grow. Kepler, a photometric telescope that points toward the constellations Cygnus and Lyra, could find as many as 3,000 new worlds by the end of the decade.

 Do Good, Find Aliens



In April, after the National Science Foundation and the state of California cut funding for radio astronomy, the Allen Telescope Array (ATA) at Hat Creek Radio Observatory, the SETI Institute’s primary listening post, went dark for the first time in nearly four years. The ATA scans deep space for alien radio signals, which some scientists say could be our best chance of finding intelligent life.


To replace the estimated $5 million it will cost to get the ATA back online full time for two years, SETI introduced a new program called SETIStars in June. For $15, donors can sponsor three-minute blocks of telescope data. In March, SETI launched the beta version of another program, a citizen-science application called setiQuest Explorer. Amateur alien hunters will be able to analyze radio-telescope data for signs of contact on their computers, tablet or mobile phone. The institute’s public outreach is paying off. By August, SETIStars had generated more than $200,000, enough to turn the ATA back on, at least for a little while.
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Space Weather Is Getting Worse



Our sun has been more active lately as it enters a new phase in its 11-year cycle, which is one reason we’ve seen a bunch of enormous coronal mass ejections and solar explosions in the past few months. But it’s actually a pretty weak solar maximum, as solar maximums go, so heliophysicists believe the sun is entering a prolonged hibernation unseen since the 17th century. This has some major implications for climate changes — on Earth and in the heavens, according to one new study.


A chilled-out sun would spew fewer particles into space, meaning the sun’s protective moat around the solar system would be less powerful. Galactic cosmic rays could have an easier time getting through, which means they could pose an increased radiation risk to astronauts and air passengers. Under these space weather conditions, a crewed asteroid or Mars mission would be far more dangerous, if not impossible.

This makes sense, given the sun’s role in shielding Earth from invading galactic particles. Charged particles from the sun encase the entire solar system in a protective sheath called the heliosphere. Scientists believe frothy bubbles of charged particles create a moat at the border between the sun's sphere of influence and that of interstellar space; cosmic rays from other stars have a hard time getting across. But when the sun is less active, this moat, called the heliosheath, is weaker. 




To test whether this is really happening, you would need to study galactic cosmic ray penetration over the centuries. Michael Lockwood and colleagues at the University of Reading in the United Kingdom looked at a 9,300-year record from ice core samples from the north and south poles. 


Galactic cosmic rays and solar energetic particles tend to channel at the poles, and Lockwood et. al looked for different chemicals that serve as a proxy for cosmic ray and SEP abundance. They found in times of low solar activity, more galactic cosmic rays reach the Earth, and there were fewer SEP events, according to ScienceNow. But in an odd twist, they also noted that the SEP events were more intense. This was especially true during transition times — just like the one we’re thought to be in right now. So just as the sun is letting more particles cross its moat, it, too, is spewing out more harmful stuff. 


The study was published in the journal Geophysical Research Letters.

Solar physicists say this could expose astronauts to unsafe levels of radiation, especially astronauts leaving the protective influence of Earth’s own magnetic field. Lockwood believes radiation exposure could increase two-fold during this solar hibernation, according to ScienceNow. And that hibernation could last between 40 and 200 years, so a Mars mission might be even further out than we all hoped.



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NASA Will Take Astronauts To Mars And Never To Return



The mission is to boldly go where no man has gone before – on a flight to Mars.
The snag is that you’d never come back.
The U.S. space agency Nasa is actively investigating the possibility of humans colonising other worlds such as the Red Planet in an ambitious project named the Hundred Years Starship.

The settlers would be sent supplies from Earth, but would go on the understanding that it would be too costly to make the return trip.
NASA Ames Director Pete Worden revealed that one of NASA’s main research centres, Ames Research Centre, has received £1million funding to start work on the project.
The research team has also received an additional $100,000 from Nasa.

 Astronauts would be marooned on the planet's surface and would never be able to return home due to cost.



‘You heard it here,” Worden said at ‘Long Conversation,’ an event in San Francisco. ‘We also hope to inveigle some billionaires to form a Hundred Year Starship fund.’
He added: ‘The human space program is now really aimed at settling other worlds. Twenty years ago you had to whisper that in dark bars and get fired.’ 

Worden said he has discussed the potential price tag for one-way trips to Mars with Google co-founder Larry Page, telling him such a mission could be done for $10 billion.
He said said: ‘His response was, “Can you get it down to $1 [billion] or $2billion?” So now we're starting to get a little argument over the price.’ 

Depending on the position of Mars in its orbit around the sun, its distance from Earth varies between 34million and 250million miles.
The most recent unmanned mission there was Nasa’s Phoenix lander, which launched in August 2007 and landed on the planet’s north polar cap in May the following year.

Experts say a nuclear-fuelled rocket could shorten the journey to about four months.
Of all the planets in the solar system, Mars is the most likely to have substantial quantities of water, making it the best bet for sustaining life. But it is a forbidding place to set up home.

Temperatures plummet way below freezing in some parts. The thin atmosphere would be a problem as it is mostly carbon dioxide, so oxygen supplies are a must.
Worden also suggested that new technologies such as synthetic biology and alterations to the human genome could also be explored ahead of the mission.

And he said that he believed the mission should visit Mars’ moons first, where scientists can do extensive telerobotics exploration of the planet. He claims that humans could be on Mars' moons by 2030.

News of the Hundred Years Starship comes as new research found that a one-way human mission to Mars is technologically feasible and would be a cheaper option than bringing astronauts back.
Writing in the Journal of Cosmology, scientists Dirk Schulze-Makuch and Paul Davies, say that the envision sending four volunteer astronauts on the first mission to permanently colonise Mars.

They write: ‘A one-way human mission to Mars would not be a fixed duration project as in the Apollo program, but the first step in establishing a permanent human presence on the planet.’
The astronauts would be sent supplies from Earth on a regular basis but they would be expected to become self-sufficient on the red planet’s surface as soon as possible.

They say: There are many reasons why a human colony on Mars is a desirable goal, scientifically and politically. The strategy of one-way missions brings this goal within technological and financial feasibility.

‘Nevertheless, to attain it would require not only major international cooperation, but a return to the exploration spirit and risk-taking ethos of the great period of Earth exploration, from Columbus to Amundsen, but which has nowadays being replaced with a culture of safety and political correctness.’

 An artist's impression of the 100 Year Starship, the craft that would take astronauts to colonise other planets


NASA's Mars Exploration Rover Spirit work on the planet's surface. One day humans could be working alongside the robotic probe

They admit that the mission would come with ‘ethical considerations’ with the general public feeling that the Martian pioneers had been abandoned to their fate or sacrificed.
But they argue that these first inhabitants of Mars would be going in much the same spirit as the first white settlers of North America – travelling to a distant land, knowing that they will never return home.  

They say: ‘Explorers such as Columbus, Frobisher, Scott and Amundsen, while not embarking on their voyages with the intention of staying at their destination, nevertheless took huge personal risks to explore new lands, in the knowledge that there was a significant likelihood that they would perish in the attempt.’

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To The Moon with NASA Twin Science Probes


An unmanned Delta 2 rocket blasted off from Cape Canaveral Air Force on Saturday to send a pair of NASA science probes on their way to the moon.

After being delayed two days by poor weather and to review technical data after Thursday’s launch scrub, the 124-tall rocket bolted off its seaside pad at 9:08 a.m. EDT on Saturday, darting through partly cloudy skies as it headed into orbit.

The twin satellites, each weighing 677 pounds, are headed to a point in space about 1.5 million kilometers (932,0570 miles) away where gravitational pull from the sun and Earth balances out.


From there, the Gravity Recovery and Interior Laboratory, or GRAIL, satellites will make a long, slow approach to the moon, arriving on Dec. 31 and Jan 1.

More than 100 spacecraft already have been to the moon, including six with U.S. astronauts, but one key piece of information about Earth’s natural satellite is still missing -- what’s inside. That’s the focus of the GRAIL mission.

After a few months to maneuver into the proper orbit, the pair will spend 82 days flying over the lunar poles, linked by radio waves.

When one spacecraft flies over a region of higher gravity, it will speed up, momentarily changing the distance between itself and its sibling probe. Less dense regions likewise will impact the satellites’ positions. Using the radio waves as a ruler, changes as tiny as a micron -- the width of a red blood cell -- can be detected.

The gravity maps will be compared with topographical features and other data to piece together the moon's history.


Overall, the moon has about one-sixth the gravity of Earth, but it is not evenly distributed. On the moon, a mountain actually might be a molehill, gravitationally speaking.

“Sometimes you’ll see a big mountain and you’d expect a high gravity signal, but in reality you get no (extra) gravity signal,” said Sami Asmar, GRAIL deputy project scientist at NASA’s Jet Propulsion Laboratory in Pasadena, Calif.

“That’s where it gets interesting,” he added. “The planet (moon) has compensated for the weight of this load for a net zero effect.”

Likewise, gravity maps of lunar flatlands show unexplained pockets of extra heft, an indication of subterranean deposits or structures. Learning the interior structure of the moon is considered critical to piecing together the story about what happened to the moon since its formation some 4.5 billion years ago.

Scientists believe the moon’s building blocks were large chunks of debris jettisoned from Earth after a collision with an object as big as Mars. In addition to unraveling the moon's history, GRAIL scientists expect to extrapolate their findings to other rocky bodies, both in our solar system and eventually to those beyond.

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