For the American contribution to the human journey to the beginning of space and time
Space news (Space economics: American contributions; NASA’s 2018 budget) NASA’s released documents covering American economic contributions, future strategic plans, and current performance during this phase of the human journey to the beginning of space and time. Below you’ll find links to each.
The United States isa leader during the human journey to the beginning of space and time and 2018’s shaping up to be an exciting year. Curiosity will continue to travel across the Red Planet searchingfor signs of water and life, while NASA continues with plans for humans to stand upon Mars sometime in 2030s.
Check out NASA’s 2018 budget and strategic plans to spend the money invested in our desire to reach the stars and the vast beyond. America’s spending a lot of your moneyto expandthespace frontier each year. You might want to check out their progress and work. It couldbe important for the future of your kids and generations of human beings to come.
Follow the human journey to the beginning of space and time at NASA.
Space news (The search for life beyond Earth) – An artist’s rendition of the Europa spacecraft orbiting Jupiter–
NASA’s Jet Propulsion Laboratory released this artist‘s rendering of the Europa spacecraft, which is set to head to Jupiter sometime in the 2020s. The Europa Mission spacecraftconfiguration in early 2016 is shown in this image. The final spacecraft configuration at launch could easily be different, so stay tuned here for more news. The position of Jupiter in the sky relative to Europa and the spacecraftare also off in this drawing.
Two large solar arrays are shown extending from the sides of the Europa spacecraft to which the ice-penetrating radar antennas are attached in this artist’s rendition. On the side of the craft, a saucer-shaped high gain antenna is depicted next to a magnetometer boom. On the forward section is a remote-sensing palette with the remaining science instruments.
The Europa Mission profile has a very capable, radiation-resistant spacecraft traveling to Jupiter, where it enters into a long, looping orbit of the giant planet in order to perform at least 45 repeated flybys of Europa at altitudes ranging from 1700 miles to 16 miles (2700 kilometers to 25 kilometers) above its surface. Planetary scientists want to take a closer look at the evidence for an ocean of liquid water beneath its icy shell. An ocean of liquid water that could be the habitat of alien lifeforms we want to get to know better.
One of the oldest regions of the Red Planet discovered, an ancient Martian lake, or the site of an ancient hot spring first explored by NASA’s Spirit rover
Space news (The Journey to Mars: Mars 2020; possible landing sites) – Northeast Syrtis: Jerero crater; or Columbia Hills, on the Red Planet –
Planetary scientists and other scientists attending the third landing site workshop hosted by NASA in order to determine the best place for its Mars 2020 rover to land recommend three places. NASA’s been using the Mars Reconnaissance Orbiter to search for suitable sites since about 2006 and to help in the identification, study, and verification of possible future landing sites for coming manned missions during most recent history. Data and observations provided by the MRO also helped participants narrow down the choices to three during the workshop.
“From the point of view of evaluating potential landing sites, the Mars Reconnaissance Orbiter is the perfect spacecraft for getting all the information needed,” said the workshop’s co-chair, Matt Golombek of NASA’s Jet Propulsion Laboratory, Pasadena, California. “You just can’t overstate the importance of MRO for landing-site selection.”
“Missions on the surface of Mars give you the close-up view, but what you see depends on where you land. MRO searches the globe for the best sites,” said MRO Deputy Project Scientist Leslie Tamppari of JPL.
“Whether it is looking at the surface, the subsurface or the atmosphere of the planet, MRO has viewed Mars from orbit with unprecedented spatial resolution, and that produces huge volumes of data,” said MRO Project Scientist Rich Zurek of JPL.“These data are a treasure trove for the whole Mars scientific community to study as we seek to answer a broad range of questions about the evolving habitability, geology, and climate of Mars.”
The Journey to the Red Planet
The human journey to the beginning of space and time will be making a stop on Mars sometime in the 2030s if everything goes as planned with NASA’s Journey to Mars. Mars 2020 is expected to launch aboard the Atlas V 541 rocket from Space Launch Complex 41 at Cape Canaveral Air Force Station in Florida around July 2020. After a journey of millions of miles across the solar system to the Red Planet, the Mars 2020 rover will land at one of three possible sites.
Images of the first possible landing site in the Northeast part of Syrtis Major showEarly Noachian bedrock planetary scientists would like to have a closer look at for signs of possible life. An excellent place for study and exploration of the past of the Red Planet, scientists are currently studying whether it’s safe for Mars 2020 to land. There could be too many boulders or even steep slopes unidentified in the initial analysis of images of this region making landing problematic at best. There’s also always the possibility of something we haven’t thought of. If the site is safe, it will be considered for the final choice, and possibly even for the rovers planned by Europe and NASA sometime around 2018.
This part of the Red Planet was once warmed by volcanoes, so planetary scientists want to look for ancient hot springs and even surface ice melt where liquid water could have flowed. Liquid water’s one of the catalysts-of-life planetary scientists look for in the search for extraterrestrial life. The layered terrain of Northeast Syrtis could hold a record of ancient simple life forms that existed on Mars during its early history. At the very least it should tell us more about interactions between water and minerals over successive parts of the Red Planet when it was young. This site we should definitely take a look at.
Rewind time 3.5 billion years in Jezero crater, to when river channels spilled over the crater wall and formed a lake. Planetary scientists see evidence water from this lake carried clay minerals from the lake bed after this body of water dried up. Scientists want to explore the crater for signs microbial life once lived here during events such as this when Jezero crater was a little wetter. For the remains of ancient life in the lakebed sediments.
Columbia Hills, Mars
After additional study planetary scientists and geochemists agree mineral springs once bubbled up from the rocks of Columbia Hills in Gusev crater on the Red Planet. Originally, the Spirit rover found no clear signs water flowed over or existed in the rocks of this region of Mars, but the discovery hot springs once existed here has scientists thinking a shallow lake may have once formed for a time. Warm, inviting waters microbial life could have evolved in, exobiologists are keen to examinesoils and lakebed sediments of Gusev crater for their remains.
The Final Landing Site of the Mars 2020 rover
Possible landing sites of NASA’s Mars 2020 rover may change as the mission goes forward, the science mission and even engineering considerations of achieving their goals could change as they learn more. Ultimately, NASA will decide on a landing site with geology indicating a wetter past that also meets all criteria. Stay tuned to the human journey to the beginning of space and time during the months and years ahead to learn more.
To study ways to protect future astronauts as they prepare and one day travel to the other planets and throughout the solar system
Space news (NASA initiatives: The Transitional Research Institute (NTRI); researching and developing innovative approaches to decrease risks for humans associated with traveling and living in space) – Texas Medical Center Innovation Institute in Houston, Texas –
During the next few decades human beings will travel to parts of the solar system never visited before and the journey is expected to be dangerous, yet awe-inspiring. In order to reduce the risks associated with traveling and living in space, NASA has announced the formation of a partnership with Baylor College of Medicine in Houston. Plans are to operate a new institute charged with researching and developing innovative approaches designed to help keep astronauts alive and healthy during long-term voyages to Mars and beyond.
Men and women react differently to the environment called space and research can differ between the two. This diagram shows key differences between men and women in cardiovascular, immunologic, sensorimotor, musculoskeletal, and behavioral adaptations to human spaceflight. Credits: NASA
Called the NASA Transitional Research Institute (NTRI), the new institute will implement a bench-to-spaceflight strategy. Their main goals to produce new treatments, countermeasures, and technologies with practical applications towards known spaceflight health risks. Medical problems like visual impairment intracranial pressure (VIIP) Syndrome, which was identified in 2005, and is currently NASA’s number one spaceflight-related health risk for astronauts. Plans are for the work to be done at the Texas Medical Center Innovation Institute in Houston, Texas.
“It’s fitting on the 47th anniversary of humanity’s first moon landing that we’re announcing a new human spaceflight research institute that will help reduce risks for our astronauts on the next giant leap – our Journey to Mars,” said Marshall Porterfield, NASA’s director of Space Life and Physical Sciences Research and Applications.
Time to get to work
Astronauts will be happy to hear this news and it has the potential to enable mankind’s journey to Mars and beyond to the beginning of space and time. The NASA Transitional Research Institute willhelp form relationships between scientists and medical laboratories and institutes looking to reduce health risks and performance barriers for humans traveling and living in space. It will also keep astronauts healthier during their space missions during the decades ahead.
In order to better understand intricate operations and detailed planning needed to capture multi-ton boulder from asteroid surface
Space news (Asteroid Redirect Mission: testing of prototype of robotic capture module system) – The Robotic Operations Center of NASA’s Goddard Space Flight Center –
Inside the Robotic Operations Center (ROC) of NASA’s Goddard Space Flight Center engineers are at work preparing the robotic section of the Asteroid Redirect Mission (ARM). The most recent work involved testing a prototype of the asteroid capture system with a mock boulderbuilt by NASA and students from West Virginia University. This work will help engineers learn more about the intricate operations needed to capture a multi-ton boulder from the surface of an asteroid. The robotic section of ARM is targeted for a 2021 launch window.
The capability built into the ROC allows engineers to create a simulation of the capture of a boulder from the surface of an asteroid. Here they can also simulate servicing of the satellite, fine tuning of systems and controllers, and even optimize all performance factors for future repairs and refueling. An important capabilitywhen building spacecraft worth hundreds of millions of dollars and even more. One that saves money and time.
The report reflects the findings of a two-month study conducted by members of the Small Bodies Assessment Group (SBAG). It explains many of ARM’s potential contributions to the future of the human journey to the beginning of space and time.
“This report is an important step in identifying ways that ARM will be more scientifically relevant as we continue mission formulation for the robotic and the crew segments,” said Gates. “We’re currently in the process of selecting hosted instruments and payloads for the robotic segment, and hope to receive an updated analysis from the SBAG after we announce those selections in spring 2017.”
During the same relative time period, other clues indicate more oxygen was present in the atmosphere thanfound currently
Space news (planetary science: Martian rocks containing manganese oxide minerals; indicating a wetter surface with more atmospheric oxygen than presently found on Mars) – Mars (the Red Planet), 154 million miles (249 kilometers) from Sol, or 141 million miles (228 million kilometers) from Earth, on average –
NASA’s Curiosity Mars rover has found rocks at a place called Windjana containing manganese oxide minerals according to reports from planetary scientists studying samples from the region. On Earth rocks of this type formed during the distant past in the presence of abundant water and atmospheric oxygen. This news added to previous reports of ancient lakes and other groundwater sources during Mar’s pastpoints to a wetter environment in the study region Gale Crater during this time.
Planetary scientists used the laser-firing instrument on the Curiosity Mars rover to detect high levels of manganese-oxide in mineral veins found at Windjana. “The only ways on Earth that we know how to make these manganese materials involve atmospheric oxygen or microbes,” said Nina Lanza, a planetary scientist at Los Alamos National Laboratory in New Mexico. “Now we’re seeing manganese oxides on Mars, and we’re wondering how the heck these could have formed?”
Planetary scientists are looking at other processes that could create the manganese-oxide they found in rocks in Mar’s Gale Crater region. Possible culprits at this point include microbes, but even optimistic planetary scientists are finding little fan fair accompanyingtheir ideas. Lanza said, “These high manganese materials can’t form without lots of liquid water and strongly oxidizing conditions. Here on Earth, we had lots of water but no widespread deposits of manganese oxides until after the oxygen levels in our atmosphere rose.”
Geologists have found high concentrations of manganese oxide minerals is an important marker of a major shift in Earth’s atmospheric composition, from relatively low oxygen levels during the distant past, to the oxygen-rich environment we live in today. Planetary scientists studying the rocks they found in Gale Crater suggest the presence of these materials indicates oxygen levels on Mars rose also, before declining to the present low levels detected. The question is how was Mar’s oxygen-rich atmosphere formed?
“One potential way that oxygen could have gotten into the Martian atmosphere is from the breakdown of water when Mars was losing its magnetic field,” said Lanza. “It’s thought that at this time in Mars’ history, water was much more abundant. Yet without a protective magnetic field to shield the surface, ionizing radiation started splitting water molecules into hydrogen and oxygen. Because of Mars’ relatively low gravity, the planet wasn’t able to hold onto the very light hydrogen atoms, but the heavier oxygen atoms remained behind. Much of this oxygen went into rocks, leading to the rusty red dust that covers the surface today. While Mars’ famous red iron oxides require only a mildly oxidizing environment to form, manganese oxides require a strongly oxidizing environment, more so than previously known for Mars.“
Lanza added, “It’s hard to confirm whether this scenario for Martian atmospheric oxygen actually occurred. But it’s important to note that this idea represents a departure in our understanding for how planetary atmospheres might become oxygenated. Abundant atmospheric oxygen has been treated as a so-called biosignature or a sign of extant life, but this process does not require life.“
The Curiosity rover has been investigating Gale Crater for around four years and recent evidence supports the possibilityconditions needed to form these deposits were present in other locations. The concentrations of manganese oxide discovered were found in mineral-filled cracks in sandstones in a region of the crater called “Kimberley”. NASA’s Opportunity rover has been exploring the surface of the planet since 2004 and recently reported similar high manganese deposits in a region thousands of miles away. Supporting the idea environments required to form similar deposits could be found well beyond Gale Crater.
What’s next for Curiosity?
NASA’s Curiosity rover’s currently collecting drilled rock powder from the 14th drill site called the Murray formation on the lower part of Mount Sharp. Plans call for NASA’s mobile laboratory to head uphill towards new destinations as part of a two-year mission extension starting near the beginning of October.
The rover will go forward about a-mile-and-a-half (two-and-a-half-kilometers) to a ridge capped with material rich in the iron-oxide mineral hematite first identified by observations made with NASA’s Mars Reconnaissance Orbiter. Just beyond this area, there’s also a region with clay-rich bedrock planetary scientists want to have a closer look.
NASA has been exploring these key exploration sites on lower Mount Sharp as part of an effort to investigate evidence the Red planet was once a much wetter environment, which contrasts with the pictures of Mars we have received from our orbiters and rovers. A wetter environment where life could have taken root and grown.
“We continue to reach higher and younger layers on Mount Sharp,” said Curiosity Project Scientist Ashwin Vasavada, of NASA’s Jet Propulsion Laboratory, Pasadena, California. “Even after four years of exploring near and on the mountain, it still has the potential to completely surprise us.”
Planetary scientists found the Murray formation consists primarily of mudstone, which on Earth would form from mud accumulated on the bottom on an ancient lake. This seems to indicate any lake environment that existed on the Red Planet lasted awhile, but we’ll need to investigate this possibility more. Plans are for Curiosity to investigate the upper regions of the Murray formation, ahead, for at least one year of the mission.
“We will see whether that record of lakes continues further,”Vasavada said. “The more vertical thickness we see, the longer the lakes were present, and the longer habitable conditions existed here. Did the ancient environment change over time? Will the type of evidence we’ve found so far transition to something else?”
Vasavada said, “The Hematite and the Clay units likely indicate different environments from the conditions recorded in the older rock beneath them and different from each other. It will be interesting to see whether either or both were habitable environments.”
Most isolated young star discovered launching jets of material into surrounding gas and dust
Space news (astrophysics: massive, young stars in star-forming regions; unusual, isolated young star baffles astronomers) – approximately 27,000 light-years from Earth in an isolated region of the bulge of the Milky Way –
Astronomers surveying the universe looking for unusual celestial objects to study to add to human knowledge and understanding have found something they haven’t seen before. Unusual celestial object CX 330 was first noticed in data obtained during a survey of the bulge of the Milky Way in 2009 by NASA’s Chandra X-ray Observatory as a source of X-ray light. Additional observations of the source showed italso emitted light in optical wavelengths, but with so few clues to go on, astronomers had no idea what they were looking at.
During morerecent observations of CX 330 during August of 2015, astronomers discovered it had recently been active, launching jets of material into gas and dust surrounding it. During a period from 2007 to 2010, ithad increased in brightness by hundreds of times, which made scientists curious to examine previous data obtained from the same region of the bulge.
Looking atdata obtained by NASA’s Wide-field Infrared Survey Explorer (WISE) in 2010, theyrealized the surrounding gas and dust was heated to the point of ionization. Comparing this data to observations taken with NASA’s Spitzer Space Telescope in 2007, astronomers determined they were looking at a young star in an outburst phase, forming in an isolated region of the cosmos.
“We tried various interpretations for it, and the only one that makes sense is that this rapidly growing young star is forming in the middle of nowhere,” said Chris Britta postdoctoral researcher at Texas Tech University in Lubbock, andlead author of a study on CX330 recently published in the Monthly Notices of the Royal Astronomical Society.
By combining this data with observations taken by a variety of both ground and space-based telescopes they were able to get an even clearer picture of CX330.An object very similar to FU Orionis, but likely more massive, compact, and hotter, and lying in a less populated region of space. Launched faster jets of outflow that heated a surrounding disk of gas and dust to the point of ionization, and increased the flow of material falling onto the star.
“The disk has probably heated to the point where the gas in the disk has become ionized, leading to a rapid increase in how fast the material falls onto the star,” said Thomas Maccarone, study co-author and associate professor at Texas Tech.
The fact CX 330 lies in an isolated region of space, unlike the previous nine examples of this type of star observed during the human journey to the beginning of space and time, tweaks the interest of astronomers. The other nine examples all lie in star-forming regions of the Milky Way galaxy with ample material for new stars to form from, but the closest star-forming region to this young star is over 1,000 light-years away.
“CX330 is both more intense and more isolated than any of these young outbursting objects that we’ve ever seen,” said Joel Green, study co-author and researcher at the Space Telescope Science Institute in Baltimore. “This could be the tip of the iceberg — these objects may be everywhere.”
We really know nothing about CX 330. More observations are required to determine more. It’s possible all young stars go through a similar outburst period as observed in the case of CX 330. The periods are just too brief in cosmological time for astronomers to observe with current technology. The real clue’s the isolation of this example as compared to previous models.
How did CX 330 become so isolated? One idea often floated is the possibility it formed in a star-forming region, before being ejected to a more isolated region of space. This seems unlikely considering astronomers believe this young star’s only about a million years old. Even if this age’s wrong, this star’s still consuming its surrounding disk of dust and gas and must have formed near its current location. It just couldn’t have traveled the required distance from a star-forming region to its current location, without completely stripping away its surrounding disk of gas and dust.
Astronomers are learning more about the formation of stars studying CX 330, that’s for sure. Using two competing ideas, called “hierarchical” and “competitive” models, scientists search for answers to unanswered questions concerning CX 330. At this point, they favor the chaotic and turbulent environment of the “hierarchical” model, as a better fit for the theoretical formation of a lone star.
It’s still possible material exists nearby CX 330, such as intermediate to low-mass stars, that astronomers haven’t observed, yet. When last viewed in August 2015, this young star was still in an outburst phase. During future observations planned with new telescopes in different wavelengths, we could get a better picture of events surrounding this unusual celestial object. Stay tuned to this channel for more information.
For people wondering if planets could form around this young star? Some astronomers are hopingplanets will form from the disk of CX 330, they’ll be able to examine closer for the chemical signature of the scars left by the outbursts observed. Unfortunately, at the rate this star’s consuming its surrounding disk of gas and dust, having enough left over for the formation of planets seems unlikely.
“You said you like it hot, right!” If CX 330’s a really massive star, which seems likely. It’s short, violent lifespan would be a truly hot time for any planet and inhabitants.