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Manuel Retana arrived in the U.S. at 15 years old, unable to speak English and with nothing but a dream and $200 in his pocket. Now, he plays a crucial role implementing life support systems on spacecraft that will carry humans to the Moon and, eventually, Mars—paving the way for the next frontier of space exploration. 

A project manager for NASA’s Johnson Space Center Life Support Systems Branch in Houston, Retana helps to ensure astronaut safety aboard the International Space Station and for future Artemis missions. His work involves tracking on-orbit technical issues, managing the cost and schedule impacts of flight projects, and delivering emergency hardware. 

Manuel Retana stands in front of NASA’s Space Launch System rocket at Kennedy Space Center in Florida.

One of his most notable achievements came during the qualification of the Orion Smoke Eater Filter for the Artemis II and III missions. The filter is designed to remove harmful gases and particulates from the crew cabin in the event of a fire inside the spacecraft. Retana was tasked with creating a cost-effective test rig – a critical step for making the filter safe for flight. 

Retana’s philosophy is simple: “Rockets do not build themselves. People build rockets, and your ability to work with people will define how well your rocket is built.” 

Throughout his career, Retana has honed his soft skills—communication, leadership, collaboration, and conflict resolution—to foster an environment of success. 

Retana encourages his colleagues to learn new languages and share their unique perspectives. He even founded NASA’s first Mariachi ensemble, allowing him to share his cultural heritage in the workplace. 

He believes diversity of thought is a key element in solving complex challenges as well as creating an environment where everyone feels comfortable sharing their perspectives. 

“You need to be humble and have a willingness to always be learning,” he said. “What makes a strong team is the fact that not everyone thinks the same way.” 

Manuel Retana, center, performs with the Mariachi Ensemble group at NASA’s Johnson Space Center in Houston.

For the future of space exploration, Retana is excited about the democratization of space, envisioning a world where every country has the opportunity to explore. He is eager to see humanity reach the Moon, Mars, and beyond, driven by the quest to answer the universe’s most enigmatic questions. 

To the Artemis Generation, he says, “Never lose hope, and it is never too late to start following your dreams, no matter how far you are.” 

AI fights conspiracy theories, Massachusetts leads the way on waste reduction, and more in this week’s science news roundup

Continuous human habitation of the Moon is the state aim of many major space-faring nations in the coming decades. Reaching that aim requires many tasks, but one of the most fundamental is feeding those humans. Shipping food consistently from Earth will likely be prohibitively expensive shortly, so DLR, Germany’s space agency, is working on an alternative. This semi-autonomous greenhouse can be used to at least partially feed the astronauts in residence on the Moon. To support that goal, a team of researchers from DLR released a paper about EVE, a robotic arm intended to help automate the operations of the first lunar greenhouse, at the IEEE Aerospace conference in March.

The EDEN Versatile End-effector (or EVE) is only possibly named as an homage to the life-seeking robot from WALL-E. But it is designed to interface with the EDEN LUNA greenhouse, a project at DLR meant to result in a fully functional greenhouse for use on the lunar surface. The advantages of such a greenhouse have been discussed in other articles, but needless to say, the EDEN LUNA is the best-supported project that will likely result in a fully functional system on the Moon when the time is right.

But as any gardener would tell you, greenhouses are a lot of work. And any time an astronaut spends on greenhouse maintenance is time they can’t spend doing other tasks, like scientific research. So, it would be extremely beneficial if there was a robot to assist with greenhouse operations, even if that robot had to be remotely controlled by an operator back on Earth.

Fraser discusses how to grow crops on the Moon.

Enter EVE, which consists of three main components. The transport rails allow the robot to move to the correct location in the greenhouse. Its robotic “arm” enables the robot to position itself effectively to complete its assigned task, and the end effector can push, pull, pick up, or perform other manual tasks. The system uses about 700W and weighs about 170 kg fully installed.

First, let’s look at the transport trails. It’s actually an off-the-shelf commercial system for use in industrial automation. The eXtended Transport System, made by Beckhoff, an industrial automation company, can be mounted in different configurations. It allows whatever is attached to it to be driven to various locations based on a series of signals that control the “mover” to which the robotic arm would be connected.

The robotic arm is based on DLR’s “This Is Not an Arm” (TINA) project. It has seven degrees of freedom, which allows for precise positioning of its end effector. Each of its three joints has around three electronic controllers for motor control, power management, and communication. It’s supported by a camera system that senses its surroundings and allows remote operators to tell where the end effector is positioned.

Isaac Arthur discusses how the Moon could support a biosphere.
Credit – Isaac Arthur YouTube Channel

The Compliant Low-Cost Antagonistic Servo Hand (CLASH) is the end effector. It has two “fingers” and a “thumb” to grip soft objects using force feedback sensors in its fingertips. It can also sense pressure from other components, such as the hand’s “tendons” and thumb and figure position.

These positioning and end-effector systems can work effectively together to perform the greenhouse’s daily maintenance tasks. For now, at least, it will require a skilled operator to do so, but that operator doesn’t have to be co-located with the greenhouse on the Moon – it could be back on Earth or even on the Lunar Gateway station orbiting above the lunar surface. Continuous operation is essential, though, as the first stages of the permanent occupation of the Moon involve temporary stays, where there will be long stretches with no human inhabitants.

DLR is fully backing the development of the EDEN LUNA greenhouse and the EVE robotic arm. Later this year, EVE will be fully integrated into the greenhouse at the Institute of Space Systems in Bremen, followed by a specially designed facility for the greater LUNA project of ESA/DLR in Cologne. As of now, both EVE and EDEN LUNA seem on track to be put through their paces before officially supporting the continual human occupation of the Moon within the next decade.

Learn More:
Prince et al. – EDEN Versatile End-effector (EVE): An Autonomous Robotic System to Support Food Production on the Moon
UT – Plants Could Grow in Lunar Regolith Using Bacteria
UT – A Greenhouse on the Moon by 2014?
UT – Practical Ideas for Farming on the Moon and Mars

Lead Image:
Greenhouse concept art on the Moon.
Credit – DLR

The post Can a Greenhouse with a Robotic Arm Feed the Next Lunar Astronauts? appeared first on Universe Today.

Of all the mysteries facing astronomers and cosmologists today, the “Hubble Tension” remains persistent! This term refers to the apparent inconsistency of the Universe’s expansion (aka. the Hubble Constant) when local measurements are compared to those of the Cosmic Microwave Background (CMB). Astronomers hoped that observations of the earliest galaxies in the Universe by the James Webb Space Telescope (JWST) would solve this mystery. Unfortunately, Webb confirmed that the previous measurements were correct, so the “tension” endures.

Since the JWST made its observations, numerous scientists have suggested that the existence of Early Dark Energy (EDE) might explain the Hubble Tension. In a recent study supported by NASA and the National Science Foundation (NSF), researchers from the Massachusetts Institute of Technology (MIT) suggested that EDE could resolve two cosmological mysteries. In addition to the Hubble Tension, it might explain why Webb observed as many galaxies as it did during the early Universe. According to current cosmological models, the Universe should have been much less populated at the time.

The research was led by Xuejian Shen and his colleagues from the Department of Physics and the Kavli Institute for Astrophysics and Space Research (MTK) at MIT. They were joined by researchers from the NSF AI Institute for Artificial Intelligence and Fundamental Interactions (IAIFI) at MIT, the University of Texas at Austin, and the Kavli Institute for Cosmology (KICC) and Cavendish Laboratory at the University of Cambridge. The paper detailing their findings was recently published in the Monthly Notices of the Royal Astronomical Society.

The Cosmic Distance Ladder, which relies on different methods to gauge distance, has led to the realization that measurements of cosmic expansion don’t agree. Credit: NASA/ESA/A. Feild (STScI)/A. Riess (STScI/JHU)

To recap, Dark Energy is the theoretical form of energy that is believed to be driving the expansion of the Universe today. The theory first emerged in the 1990s to explain observations by the venerable Hubble Space Telescope, which showed that cosmic expansion appeared to be accelerating over time. EDE is similar but is thought to have briefly appeared shortly after the Big Bang, which disappeared after influencing the expansion of the early Universe. Like Dark Energy, this force would have counteracted the gravitational pull of early galaxies and temporarily accelerated the expansion of the Universe.

The existence of this energy would also explain why measurements of the Hubble Constant are inconsistent with each other. Short of General Relativity being wrong (despite being proven repeatedly for over a century), EDE is considered the most likely solution to the Hubble Tension. Similarly, Webb’s 2023 observations uncovered a surprising number of bright galaxies just 500 million years after the Big Bang that were comparable in size to the modern Milky Way. These findings challenge conventional models of galaxy formation, which predict that galaxies take billions of years to form and grow.

For their study, the team focused on the formation of “Dark Matter Halos,” the hypothetical region that allows protogalaxies to accumulate gas and dust, leading to star formation and growth. As when said in a recent MIT News story:

“The bright galaxies that JWST saw would be like seeing a clustering of lights around big cities, whereas theory predicts something like the light around more rural settings like Yellowstone National Park. And we don’t expect that clustering of light so early on. We believe that dark matter halos are the invisible skeleton of the universe. Dark matter structures form first, and then galaxies form within these structures. So, we expect the number of bright galaxies should be proportional to the number of big dark matter halos.”

Early Dark Energy could have caused early seeds of galaxies (depicted at left) to sprout many more bright galaxies (at right) than theory predicts. Credit: Josh Borrow/Thesan Team

The team developed an empirical framework for early galaxy formation that incorporated the six main “cosmological parameters”—the basic mathematical terms that describe the evolution of the Universe. This includes the Hubble Constant, which describes cosmic expansion, while parameters describe density fluctuations immediately after the Big Bang, from which dark matter halos formed. The team theorized that if EDE affects early cosmic expansion, it could also affect other parameters that might explain the appearance of many large galaxies shortly thereafter.

To test their theory, the team modeled the formation of galaxies within the first few hundred million years of the Universe. This model incorporated EDE to determine how early dark matter structures evolved and gave rise to the first galaxies in the Universe. As study co-author Rohan Naidu, a postdoc with MKI, explained:

“You have these two looming open-ended puzzles. We find that in fact, early dark energy is a very elegant and sparse solution to two of the most pressing problems in cosmology. What we show is, the skeletal structure of the early universe is altered in a subtle way where the amplitude of fluctuations goes up, and you get bigger halos, and brighter galaxies that are in place at earlier times, more so than in our more vanilla models. It means things were more abundant, and more clustered in the early universe.”

“We demonstrated the potential of early dark energy as a unified solution to the two major issues faced by cosmology,” added co-author Mark Vogelsberger, an MIT professor of physics. “This might be an evidence for its existence if the observational findings of JWST get further consolidated. In the future, we can incorporate this into large cosmological simulations to see what detailed predictions we get.”

Further Reading: MIT News, MNRAS

The post Early Dark Energy Could Resolve Two of the Biggest Mysteries in Cosmology appeared first on Universe Today.

Optical interferometry has been a long-proven science method that involves using several separate telescopes to act as one big telescope, thus achieving more accurate data as opposed to each telescope working individually. However, the Earth’s chaotic atmosphere often makes achieving ground-based science difficult, but what if we could do it on the Moon? This is what a recent study presented at the SPIE Astronomical Telescopes + Instrumentation 2024 hopes to address as a team of researchers propose MoonLITE (Lunar InTerferometry Explorer) as part of the NASA Astrophysics Pioneers program. This also comes after this same team of researchers recently proposed the Big Fringe Telescope (BFT), which is a 2.2-kilometer interferometer telescope to be built on the Earth with the goal of observing bright stars.

Here, Universe Today discusses MoonLITE with Dr. Gerard van Belle, who is an astronomer at the Lowell Observatory in Flagstaff, Arizona, regarding the motivation behind proposing MoonLITE, the science they hope to achieve, lunar surface location preference, the cost of MoonLITE, and next steps to make MoonLITE a reality. Therefore, what is the motivation behind proposing MoonLITE?

“The real barrier to doing super sensitive high resolution optical interferometry is the Earth’s atmosphere,” Dr. van Belle tells Universe Today. “It’s a boiling, turbulent medium that means the exposure time of your telescope is ultimately limited to less than a millisecond or so. Telescopes that expose longer than that can achieve greater sensitivity, but at the expense of angular resolution – things smear out. MoonLITE, with two-inch (50mm) apertures, would be more than a thousand times more sensitive than terrestrial apertures is 8-meter collecting apertures, because it can stare for many minutes at a time. In comparison to millisecond exposure times on the Earth, the amount of light grabbed by these tiny dime-store sized telescopes exceeds giant industrial facility telescopes within the first second of having the shutter open.”

Much like with the recently proposed BFT, MoonLITE has a number of scientific objectives it hopes to accomplish, as the study notes three science cases, including studying the radii of low-mass stars (M-dwarfs) and brown dwarfs, young stellar objects (YSOs), and active galactic nuclei (AGN). For the M-dwarfs and brown dwarfs, the team aspires to obtain long-sought data regarding their sizes and temperatures since observing them from ground-based telescopes has proven difficult.

For YSOs, the researchers hope to gain greater understanding of the formation and evolution of habitable exoplanets within the protoplanetary disks of pre-main sequence stars, with MoonLITE being capable of ascertaining the inner regions of these stars and the star sizes, as well. For AGNs, the researchers aspire to learn more about supermassive black holes, and specifically the jets that emanate from them, with MoonLITE being able to observe these objects in optical wavelengths for the first time. But what else can we learn from these three science cases?

“So, we actually have more science cases than that – so many, in fact, that we realized the new capabilities of MoonLITE were beyond our collective imagination for covering all the bases,” Dr. van Belle tells Universe Today. “So, we built into the program a 20% slice of the overall observing time to put up for competitive selection by the community – you know, crowdsource for the really creative ideas. The three we wrote up were just what we felt highlighted what one could do with greater sensitivity from the Earth’s surface. For example, the stars that are the smallest – 10% the size of our sun – are also the faintest. And measuring the sizes of those is out of reach of terrestrial interferometers. Same for YSOs and AGNs – there’s a few that can be done from Earth, but for more general samples – ones that represent the more typical objects, not the super-bright oddballs – you need lots of sensitivity.”

Diagram conveying the setup for MoonLITE on the lunar surface, beginning with a lander being delivered by NASA’s Commercial Lunar Payload Services (1), which unrolls a fiber umbilical over 100 meters (328 feet) (2), concluding with deploying the siderostat station (3). Science operations begin once instrument calibration is performed. (Credit: van Belle et al. (2024))

One of the unique aspects of MoonLITE is it could be brought to the lunar surface via NASA’s Commercial Lunar Payload Services (CLPS), which is a collaboration with the private sector to deliver scientific and technical payloads to the Moon to test technologies that can help with both human missions as part of the Artemis Program, and scientific missions to further our understanding of the universe, like MoonLITE. Examples of companies participating in upcoming CLPS missions include Intuitive Machines, Astrobiotic, Firefly Aerospace, and Draper, all of which are delivering payloads to various locations on the lunar surface. But is there a specific location where MoonLITE would work best?

“We designed MoonLITE to be entirely site agnostic,” Dr. van Belle tells Universe Today. “For a small experiment like this, it’s going to catch a ride on board a NASA CLPS lander as a minor guest – and putting a minimal number of requirements on your ride improves one’s chances of getting a ride assignment. So polar or equatorial latitudes both work, as well as nearside versus farside.”

As noted, this same team of researchers recently proposed the Big Fringe Telescope, which is slated to be a 2.2-kilometer interferometer telescope comprised of 16 smaller telescopes that are 0.5-meters in diameter. Along with conducting cutting-edge science, including observing binary star systems and making exoplanet transit “movies”, one of the most notable features of the BFT is its extremely low cost compared to current optical interferometers around the world, coming with an approximate price tag of $28,496,000.

In contrast, the cost of the European Southern Observatory’s Very Large Telescope Interferometer (VLTI), which is comprised of four 8.2-meter telescopes and four movable 1.8-meter telescopes, has been estimated in the hundreds of millions of dollars. Therefore, what is the potential cost for MoonLITE compared to other Earth-based interferometers?

“MoonLITE was designed to work within the cost box for the NASA Pioneers call for proposals,” Dr. van Belle tells Universe Today. “This CfP [Call for Projects] stipulates a couple of things: a $20M cost cap, including a 25% uncommitted reserve, so the actual budgeted level of activities and hardware was $15M. The CfP does let you request some things – first off, a CLPS ride, though you have to then fit within the CLPS mass cap of 50kg. The notional CLPS lander in the CfP was to provide some other things as well – power, communications, mobility with a rover. So, there’s actually quite a bit of in-kind support wrapped up in that CLPS ride.”

Submitting a proposal to NASA is a very in-depth process involving several steps, also known as phases, resulting in a very small acceptance rate, often with several rejections and improvements before being accepted. These proposals range from CubeSats to full-blown, multi-billion-dollar space missions, with most taking years to become real-world missions even after selection, if at all. For example, of the four proposals selected for further development in January 2021 Astrophysics Pioneers Program, (Aspera, Pandora, StarBurst, and PUEO), only two of them have definitive launch dates (StarBurst in 2027 and PUEO in 2025). Therefore, if MoonLITE is to be selected for advancement, it could be years, or even decades, before it officially lands on the lunar surface to conduct science. Unfortunately, while Dr. van Bells says the 2024 Pioneers proposal term was canceled due to federal budget issues, what are the next steps to make MoonLITE a reality?

“We submitted for the 2023 NASA Pioneers call and got turned down,” Dr. van Belle tells Universe Today. “But we got a good review and have been encouraged to improve things, address perceived issues, and resubmit. We’re trying to reduce risk by doing some lab and ground-based tests. This is another nice element of MoonLITE – we can just build a representative system on the ground and test it straight up here. We don’t get the exquisite sensitivity like we would on the moon, but otherwise it’ll work just the same – we just need to look at bright things here from Earth. So, we’re keen to address some of these issues from the review panel and resubmit for 2025.” 

As NASA prepares to send humans back to the Moon with the Artemis Program for the first time since 1972, the level of science that can be achieved on the lunar surface is unprecedented. This is specifically evident given the lack of a Moon’s atmosphere, allowing for more accurate data to be obtained and potentially providing scientists with a greater understanding of our universe, and our place in it. With MoonLITE, scientists hope to gain insight into low-mass stars and brown dwarfs, young stellar objects, and active galactic nuclei from potentially anywhere on the lunar surface, allowing for greater diversity is site selection and what celestial objects can be observed.

Dr. van Belle concludes by telling Universe Today, “MoonLITE is super exciting, not just because it’s a really high-impact experiment in a remarkably affordable package – but because it will show the whole approach works and can be taken much, much further. As an example, high precision astrometry from a lunar interferometer could characterize the masses of terrestrial-scale extrasolar planets. Mass measures are needed in advance of the Habitable Worlds Observatory of the 2040’s, to understand the spectral HWO will get, and disentangle those spectra for signs of life.”

How will MoonLITE contribute to optical interferometry on the lunar surface in the coming years and decades? Only time will tell, and this is why we science!

As always, keep doing science & keep looking up!

The post Studying Stars from the Lunar Surface with MoonLITE, Courtesy of NASA’s Commercial Lunar Payload Services appeared first on Universe Today.

If you could fly over Mars, what might you see?

Using a phenomenon known as gravitational lensing, it might be possible to use the sun as a gigantic telescope to peer deep into space.

The four Polaris Dawn astronauts splashed down safely off the coast of Florida today (Sept. 15), bringing an end to their historic commercial mission.

After five days in space aboard a SpaceX Crew Dragon, the crew of Polaris Dawn will return to Earth early TKday, and you can watch the landing live.

Earlier this year, NASA selected a rather interesting proposal for Phase I development as part of their NASA Innovative Advanced Concepts (NIAC) program. It’s known as Swarming Proxima Centauri, a collaborative effort between Space Initiatives Inc. and the Initiative for Interstellar Studies (i4is) led by Space Initiative’s chief scientist, Marshall Eubanks. The concept was recently selected for Phase I development as part of this year’s NASA Innovative Advanced Concepts (NIAC) program.

Similar to other proposals involving gram-scale spacecraft and lightsails, the “swarming” concept involves accelerating tiny spacecraft with a laser array to up to 20% the speed of light. This past week, on the last day of the 2024 NASA Innovative Advanced Concepts (NIAC) Symposium, Eubanks and his colleagues presented an animation illustrating what this mission will look like. The video and their presentation provide tantalizing clues as to what scientists expect to find in the closest star system to our own. This includes Proxima b, the rocky planet that orbits within its parent star’s circumsolar habitable zone (CHZ).

As we addressed in previous articles, the Swarming Proxima Centauri concept has evolved significantly over the past few years. The concept emerged in 2017 as a proposal by the i4is named Project Lyra, which aimed to send tiny spacecraft to catch up with the interstellar object (ISO) ‘Oumuamua. However, it has since evolved into a collaborative effort between the i4is and Space Initiatives Inc., a Florida-based aviation and aerospace component manufacturer dedicated to developing gram-based “femtospacecraft” – i.e., even tinier than nanospacecraft!

Not long ago, Eubanks and his colleagues produced research papers addressing some big questions about interstellar exploration, including communications and what we might learn from a flyby of Proxima b. During the 2024 NIAC Symposium, which took place from September 10th to 12th in Pasadena, California, Eubanks and his colleagues had the opportunity to present their latest findings. As the video illustrates, the swarm they envision will consist of a thousand “picospacecraft” (between nano and femto), which they’ve named “Coracles” (a small, rounded, lightweight boat).

The probes are solid, armored on one side, and covered with optical annuli (reflective material) on the other. They measure about two centimeters thick (0.8 inches) and four meters (about 13 feet) in diameter and weigh no more than a few grams each. According to their NIAC proposal, these will be accelerated by a ~100 gigawatt (GW) laser array that will be available by mid-century. The probes are also equipped with side-mounted lasers to facilitate communications between them and mission controllers back on Earth.

As Eubanks indicated during the presentation, there are actually a thousand probes in the animation and an artistically accurate depiction of the Proxima Centauri system. The red dwarf is shown prominently as the probes approach the Proxima b, while Alpha Centauri AB is visible in the far background. Once the probes pass by the planet, we also get an accurate depiction of many scientists they expect to find:

“This is real-time. This is more or less what you would see expect for a redshift, a blushift, and then a redshift. And we had the artists do the planet as an ‘eyeball planet,’ where you have a central warm spot surrounded by a cold zone because we think this planet’s probably rotationally locked.”

Team member Robert Kennedy III posing in front of an 88% size mock-up of the Coracle sail. Credit: 2024 NIAC/i4is/Interstellar Initiatives Inc.

As Eubanks further explained, their collaboration has already produced prototypes of their Coracle spacecraft. One was recently showcased at the World Science Fiction Convention in Glasgow, while another is currently in Pasadena. While providing a run-down on the design of the individual spacecraft, Eubanks emphasized the importance of coherence and how the swarm’s configuration will facilitate communications and cohesion:

“Operational coherence is essential to making this mission work. By operational coherence, we mean that the whole set of probes acts as a unit. Now I notice that doesn’t mean photonic phase coherence – we won’t be able to do that. But if we have good enough clocks and we have range measurement by lasers, we can determine where we are to a few centimeters. We can determine what the relative clocks are to more or less the same level. And [they] can then act as one thing.

“And the crucial part of that is we can do that with a lot of things, like taking pictures of the planet and so on. But the crucial part of that is what we call the wall of light. The wall of light is when all the probes send one coherent set of photons back to Earth so they can be received altogether. We think we can get one kilobit per second data rate back, and we can, therefore, send something like four gigabytes a year back to Earth. And that’s enough to get good data and really understand the system.”

While the Swarming Proxima Centauri concept did not receive Phase II or III funding from the NIAC this year, it remains a project worthy of study and further development. Like Breakthrough Starshot and other lightsail proposals, it showcases what interstellar missions will look like in the coming decades. In that respect, ideas like this also indicate that we are at a point in our history where exploring the nearest star systems is no longer considered a far-off idea that requires serious technological innovations to happen first.

Further Reading: 2024 NIAC Symposium

The post New Video Shows How Tiny Spacecraft Will “Swarm” Proxima Centauri appeared first on Universe Today.

ESA scientists have successfully demonstrated 3D printing of a metal part in space for the first time.

On Episode 128 of This Week In Space, Rod and Tariq talk about what's going on with Boeing's Starliner CST-100 spacecraft.

The most distant object easily visible to the unaided eye is

Cosmic dust may have helped to kick-start life on Earth, new research suggests. The findings challenge a widely held assumption that this was not a plausible explanation.

A team of scientists presented a new gravity map of Mars at the Europlanet Science Congress 2024. The map shows the presence of dense, large-scale structures under Mars’ long-gone ocean and that mantle processes are affecting Olympus Mons, the largest volcano in the Solar System.

The new map and analysis include data from multiple missions, including NASA’s InSIGHT (Interior Exploration using Seismic Investigations, Geodesy and Heat Transport) mission. They also use data from tiny deviations in satellites as they orbit Mars. The paper “The global gravity field of Mars reveals an active interior” will be published in an upcoming edition of JGR: Planets. The lead author is Bart Root of the Delft University of Technology. Some of the results go against an important concept in geology.

Geologists work with a concept called flexural isostasy. It describes how a planet’s outer rigid layer responds to large-scale loading and unloading. The layer is called the lithosphere and consists of the crust and the uppermost part of the mantle. When something heavy loads the lithosphere, it responds by sinking. On Earth, Greenland is a good example of this, where the massive ice sheet puts downward pressure on it. As its ice sheets melt due to global warming, Greenland will rise.

This downward bending often causes an uplift in surrounding areas, though the effect is slight. The more massive the load is, the more pronounced the downward bending, although it also depends on the lithosphere’s strength and elasticity. Flexural isostasy is a critical idea for understanding glacial rebound, mountain formation, and sedimentary basin formation.

The authors of the new paper say scientists need to rethink how flexural isostasy works on Mars. This is because of Olympus Mons, the largest volcano in the Solar System, and the entire volcanic region called Tharsis Rise, or Tharsis Montes. Tharsis Montes is a vast volcanic region that holds three other enormous shield volcanoes: Arsia Mons, Pavonis Mons, and Ascraeus Mons.

This colourized image of the surface of Mars was taken by the Mars Reconnaissance Orbiter. The line of three volcanoes is the Tharsis Montes, with Olympus Mons to the northwest. Valles Marineris is to the east. Image: NASA/JPL-Caltech/ Arizona State University

Flexural isostasy states that this massive region should force the planet’s surface downward. But the reverse is true. Tharsis Montes is much more elevated than the rest of Mars’ surface. NASA’s InSIGHT lander also told scientists a lot about Mars’ gravity, and together, it’s forcing researchers to reconsider how this all works on Mars.

“This means we need to rethink how we understand the support for the big volcano and its surroundings,” the authors write. “The gravity signal of its surface fits well with a model that considers the planet as a thin shell.”

The research shows that active processes in the Martian mantle are boosting Tharsis Montes upward. “There seems to be a big mass (something light) deep in Mars’ layer, possibly rising from the mantle,” the authors write. “It shows that Mars might still have active movements happening inside it, making new volcanic things on the surface.”

The researchers found an underground mass around 1750 kilometres across and at a depth of 1100 kilometres. They suspect that it’s a mantle plume rising under Tharsis Montes and strong enough to counteract the downward pressure from all the mass. “This suggests that a plume head is currently flowing upward towards the lithosphere to generate active volcanism in the geological future,” the authors write in their paper.

There’s debate about how volcanically active Mars is. Although there are no active volcanic features on the planet, research shows that the Tharsis region has resurfaced in the near geological past within the last few tens of millions of years. If there is a mantle plume under Tharsis Montes, could it eventually reach the surface? That’s purely speculative, and more research is needed to confirm these findings.

The researchers also found other gravitational anomalies. They found mysterious, dense structures under Mars’ northern polar plains. They’re buried under a thick, smooth sediment layer that was likely deposited on an ancient seabed.

This map from the study highlights the dense gravitational structures in the northern hemisphere. The regions marked with black lines are high-mass anomalies that do not show any correlation with geology and topography. These hidden subsurface structures are covered by sediments from an old ocean, and their origin is still a mystery. Credit: Root et al.

The anomalies are approximately 300–400 kg/m3 denser than their surroundings. Earth’s Moon has gravitational anomalies that are associated with giant impact basins. Scientists think that the impactors that created the basins were denser than the Moon, and their mass has become part of the Moon.

These maps show the gravitational anomalies at the surface of the Moon. Some of the gravity anomalies are clearly associated with large impact basins. On Mars, the anomalies have no corresponding surface features. Image Credit: By Mark A. Wieczorek – Own work, CC BY 2.5, https://commons.wikimedia.org/w/index.php?curid=1381260

Impact basins on Mars also show gravity anomalies. However, the anomalies in Mars’ northern hemisphere show no traces of them on the surface.

This image from the research shows the gravitational structures in Mars’ northern polar region on a topographical map. There’s no correlation between the deep structures and the surface. Image Credit: Root et al.

“These dense structures could be volcanic in origin or could be compacted material due to ancient impacts. There are around 20 features of varying sizes that we have identified dotted around the area surrounding the north polar cap—one of which resembles the shape of a dog,” said Dr. Root. “There seems to be no trace of them at the surface. However, through gravity data, we have a tantalizing glimpse into the older history of the northern hemisphere of Mars.”

The only way to understand these mysterious structures and Mars’ gravity in general is with more data. Root and his colleagues are proponents of a mission that could gather the needed data.

It’s called the Martian Quantum Gravity (MaQuls) mission. MaQuls would be based on the same technology used in the GRAIL (Gravity Recovery and Interior Laboratory) and GRACE (Gravity Recovery and Climate Experiment) missions, which mapped the Moon’s and Earth’s gravity, respectively. MaQuls would feature two satellites trailing each other and connected by an optical link.

A grainy yet illustrative image of how the MaQuls mission would work. MaQuls would investigate the gravitational field of Mars and study static and dynamic processes on and under the surface. MaQuls would measure Mars’s gravitational field with the highest precision yet. Image Credit: Worner et al. 2023.

“Observations with MaQuIs would enable us to better explore the subsurface of Mars. This would help us to find out more about these mysterious hidden features and study ongoing mantle convection, as well as understand dynamic surface processes like atmospheric seasonal changes and the detection of ground water reservoirs,” said Dr. Lisa Wörner of DLR, who presented on the MaQuIs mission at EPSC2024 this week.

The post A Gravity Map of Mars Uncovers Subsurface Mysteries appeared first on Universe Today.

The success of the all-civilian spacewalk on SpaceX’s Polaris Dawn mission shows that private space flight is starting to catch up with government space agencies

The success of the all-civilian spacewalk on SpaceX’s Polaris Dawn mission shows that private space flight is starting to catch up with government space agencies

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Sols 4304-4006: 12 Years, 42 Drill Holes, and Now… 1 Million ChemCam Shots! In celebration of ChemCam’s milestone, here is a stunning image from its remote micro imager, showing details in the landscape far away. This image was taken by Chemistry & Camera (ChemCam) onboard NASA’s Mars rover Curiosity on Sol 4302 — Martian day 4,302 of the Mars Science Laboratory mission — on Sept. 12, 2024, at 09:20:51 UTC. NASA/JPL-Caltech

Earth planning date: Friday, Sept. 13, 2024

Today, I need to talk about ChemCam, our laser and imaging instrument on the top of Curiosity’s mast. It one of the instruments in the “head” that gives Curiosity that cute look as if it were looking around tilting its head down to the rocks at the rover’s wheels. On Monday, 19th August the ChemCam team at CNES in France planned the 1 millionth shot and Curiosity executed it on the target Royce Lake on sol 4281 on Mars. Even as an Earth scientist used to really big numbers, this is a huge number that took me a while to fully comprehend. 1 000 000 shots! Congratulations, ChemCam, our champion for getting chemistry from a distance – and high-resolution images, too. If you are now curious how Curiosity’s ChemCam instrument works, here is the NASA fact sheet. And, of course, the team is celebrating, which is expressed by those two press releases, one from CNES in France and one from Los Alamos National Laboratory, the two institutions who collaborated to develop and build ChemCam and are now running the instrument for over 12 years! And the PI, Dr Nina Lanza from Los Alamos informs me that the first milestone – 10000 shots was reached as early as Sol 42, which was the sol the DAN instrument used its active mode for the first time. But before I am getting melancholic, let’s talk about today’s plan!

The drive ended fairly high up in the terrain, and that means we see a lot of the interesting features in the channel and generally around us. So, we are on a spot a human hiker would probably put the backpack down, take the water bottle out and sit down with a snack to enjoy the view from a nice high point in the landscape. Well, no such pleasures for Curiosity – and I am pretty sure sugar, which we humans love so much, wouldn’t be appreciated by rover gears anyway. So, let’s just take in the views! And that keeps Mastcam busy taking full advantage of our current vantage point. We have a terrain with lots of variety in front of us, blocks, boulders, flatter areas and the walls are layered, beautiful geology. Overall there are 11 Mastcam observations in the plan adding up to just about 100 individual frames, not counting those taken in the context of atmospheric observations, which are of course also in the plan. The biggest mosaics are on the targets “Western Deposit,” “Balloon Dome,” and “Coral Meadow.” Some smaller documentation images are on the targets “Wales Lake,” “Gnat Meadow,” and “Pig Chute.”

ChemCam didn’t have long to dwell on its milestone, as it’s busy again today. Of course, it will join Mastcam in taking advantage of our vantage point, taking three remote micro imager images on the landscape around us. LIBS chemistry investigations are targeting “Wales Lake,” “Gnat Meadow,” and “Pig Chute.” APXS is investigating two targets, “College Rock” and “Wales Lake,” which will also come with MAHLI documentation. With all those investigations together, we’ll be able to document the chemistry of many targets around us. There is such a rich variety of dark and light toned rocks, and with so much variety everywhere, it’s hard to choose and the team is excited about the three targeted sols … and planning over 4 hours of science over the weekend!

The next drive is planned to go to an area where there is a step in the landscape. Geologists love those steps as they give insights into the layers below the immediate surface. If you have read the word ‘outcrop’ here, then that’s what that means: access to below the surface. But there are also other interesting features in the area, hence we will certainly have an interesting workspace to look at! But getting there will not be easy as the terrain is very complex, so we cannot do it in just one drive. I think there is a rule of thumb here: the more excited the geo-team gets, the more skills our drivers need. Geologists just love rocks, but of course, no one likes driving offroad in a really rocky terrain – no roads on Mars. And right now, our excellent engineers have an extra complication to think about: they need to take extra care where and how to park so Curiosity can actually communicate with Earth. Why? Well, we are in a canyon, and those of you liking to hike, know what canyons mean for cell phone signals… yes, there isn’t much coverage, and that’s the same for Curiosity’s antenna. This new NASA video has more information and insights into the planning room, too! So, we’ll drive halfway to where we want to be but I am sure there will be interesting targets in the new workspace, the area is just so, so complex, fascinating and rich!

And that’s after Mars for you, after 12 years, 42 drill holes, and now 1 Million ChemCam shots. Go Curiosity go!!!

Written by Susanne Schwenzer, Planetary Geologist at The Open University

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Sep 13, 2024

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In 2003, strange features on Mars’s surface got scientists’ “spidey senses” tingling when they saw them. That’s when unusual “anareiform terrain” landforms appeared in images from the Mars Reconnaissance Orbiter. They’ve returned each year, spreading across the southern hemisphere surface.

At first, nobody knew what caused these weird wrinkly spider-like formations. Now, NASA researchers have duplicated them in the lab to explain their existence. No doubt about it, though, these Mars spiders look weird. Some of them stretch across a kilometer and generally appear in clusters.

Since discovering them in 2003 via images from orbiters, scientists have marveled at these Mars spiders sprawled across the southern hemisphere of Mars. No one is entirely sure how these geologic features are created but lab simulations may provide clues. Credit: NASA/JPL-Caltech/University of Arizona

Since carbon dioxide is common on Mars, scientists figured it had something to do with creating these weird formations. They used the “Kieffer model” to delve into the history of Mars spiders. That model explains how carbon dioxide ice slabs under the surface trap gas as it sublimates (turns to gas), usually during southern hemisphere spring.

Sunlight heats the surface and shines through transparent slabs of carbon dioxide. Those ice layers build up each winter. The soil beneath the ice absorbs heat from the Sun and causes the ice closest to it to sublimate. Gas pressure builds up, which cracks the ice and allows gas to escape. As it seeps upward, the gas takes with it a stream of dark dust and sand from the soil that lands on the surface of the ice. Those deposits take the form of spidery landforms.

Confirming Mars Spiders

To see if that process is what’s creating Mars spiders, NASA JPL scientists, led by Lauren McKeown, decided to simulate Mars conditions in their lab. “The spiders are strange, beautiful geologic features in their own right,” said McKeown. “These experiments will help tune our models for how they form.”

The DUSTIE chamber at JPL. This is where scientists simulated the surface conditions under which Mars spiders form. Credit: NASA/JPL-Caltech.

Not that it’s easy to replicate Mars on Earth, even in strict laboratory conditions. For Mc Keown and her team, the hardest part was re-creating conditions found on the Martian polar surface. That region experiences extremely low air pressure. Seasonal changes bring the air and surface temperatures down to a chilly -301 degrees Fahrenheit (minus 185 degrees Celsius). To make it work, the team used a liquid-nitrogen-cooled test chamber at JPL—the Dirty Under-vacuum Simulation Testbed for Icy Environments, or DUSTIE.

“I love DUSTIE. It’s historic,” Mc Keown said, noting that the wine barrel-size chamber was used to test a prototype of a rasping tool designed for NASA’s Mars Phoenix lander. For their experiment, the team chilled Martian soil simulant in a container dipped into a nitrogen bath. Then they put the whole thing into DUSTIE and replaced Earth-normal pressure with Mars air pressure. Carbon dioxide gas flowed in and condensed to ice. The next step was to put a heater inside to simulate Martian conditions in early spring. The team did this several times before the experiment created simulated “spiders” similar to those on Mars.

Mars spider-like formations in soil simulant created during experiments at NASA/JPL in the DUSTIE chamber. Credit: NASA/JPL-Caltech. The Next Steps

That simulation created plumes of carbon dioxide gas escaping from the soil simulant. It’s close to what happens on Mars, but not quite. So, the next step is to do the same experiment and use a simulated Sun to heat the surface materials. If that produces the same results, then the team has a good chance of proving this is what happens on Mars.

However, Mars being what it is—there are still a lot of questions about why the spiders only form in the southern hemisphere at spring. Since subsurface carbon dioxide ice isn’t limited to that region of the planet, why don’t spiders form in other places? One possibility is that these aren’t recent features. They could be left over from a more active time in the planet’s past. Maybe the climate was very different when they formed. Or something catastrophic happened to enable the formation and growth of spiders in the southern hemisphere.

The study at JPL is a good step forward in understanding the Martian terrain. It confirms several formation processes described by the Kieffer model. Of course, it would be really cool to visit those spiders someday. For now, however, lab work is as close as it gets to explaining them. Future rovers and landers could be used to study those landforms up close and personal. However, there aren’t any planned in the near future, and no other spacecraft has landed in the spider-rich southern hemisphere region. For now, scientists will continue testing the lab to understand the conditions that make these strange-looking features.

For More Information

NASA Scientists Re-Create Mars ‘Spiders’ in a Lab for the First Time
A Lab-scale Investigation of the Mars Kieffer Model

The post Scientists Recreate Mars Spiders in the Lab appeared first on Universe Today.