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This is Space Time, Series 29, Episode 116, for broadcast
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on the 28th of September, 2026. Coming up on Space Time.
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A micro-blazer detected in the Milky Way galaxy for the
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first time. The discovery of at least three separate water
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episodes on the red planet Mars. And SpaceX's Starship about
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to launch on its first orbital flight. All that and
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more coming up on Space Time.
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Welcome to Space Time with Stuart Gary.
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A micro blazer has been discovered for the first time
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in our Milky Way galaxy. The observations, reported in the
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journal Astronomy and Astrophysics, suggest that this newly found object
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might be generating the fastest particles ever detected in the galaxy.
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Blazars are a type of quasar, a superluminal jet of
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particles streaming out from a supermassive black hole as it
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feeds on infalling material on an accretion disk. But whereas
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a quasar represents this active galactic nuclei seen at an angle,
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Blazer is the term used to describe the quasar when
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it's being viewed directly head-on. The term micro is added
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when the quasar, or blazer in this case, is generated
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not by a supermassive black hole, but by a stellar-mass
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black hole. This newly identified micro blazer, first ever discovered
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in the Milky Way, is located about 12,000 light-years away,
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in the constellation Scutum. It's catalogued as IRAS 18293-0941 and
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consists of a stellar-mass black hole with about 10 times
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the mass of our Sun in a binary system with
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a spectral-type Erby blue star orbiting each other approximately every
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11 Earth days. The jets are being produced by matter
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being sucked off the binary companion star onto the black hole. First,
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the matter forms an accretion disk around the black hole,
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where it's crushed and torn apart, releasing huge amounts of energy. Then,
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just before the remaining material crosses the event horizon to
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fall forever into the black hole singularity, some of this
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material is picked up by magnetic fields on the accretion
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disk and then shot out into space, perpendicular to the
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accretion disk, forming two superluminal jets, one on each side
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of the disk. IRAS 18293-0941 was first catalogued back in
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1983 by the Dutch-American IRAS satellite. Astronomers' attention was drawn
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to the object because in many radio observations it appeared
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to have a bright compact core and radio emissions coming
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out of one side only, the side facing the Earth.
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And that was hinting at the possibility of a jet
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pointing directly towards the Earth. So, an extensive observational campaign
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was launched using radio telescopes for high-resolution images, which showed
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the jet interactions, and optical telescopes for spectra and measuring
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velocities in the system. X-ray and gamma-ray telescopes for probing
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the hot plasma around the black hole were also employed,
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as were infrared images showing the warm dust surrounding the system.
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The authors were then able to identify a region where
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the jet was smashing into a molecular cloud of gas
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and dust, causing the particles in the cloud to be
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accelerated to ultra-high energies, likely up to petra-electron volts. And
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this would make this micro-blazer one of the most powerful
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particle accelerators in the galaxy. The radio imaging revealed not
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only the jet, but also its interaction with the surrounding clouds. See,
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first the jet crosses a region of about 100 light-years,
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where it's already cleared out the interstellar medium. After that,
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it then hits the relatively dense molecular cloud remaining, which
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consists primarily of molecular hydrogen and dust. This interaction creates
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a bright spot in the cloud, with the interstellar materials
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being ionized and the dust heated. It's here where particles
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are being accelerated to nearly the speed of light. And
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with energies up to petra-electron volt levels, it makes this
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microblazer one of the most powerful particle accelerators in the
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Milky Way, and around 100 times more powerful than the
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Large Hadron Collider at CERN, which is the strongest particle
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accelerator on Earth. One of the study's authors, Benito Marcotte
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from Astron in the Netherlands, says microblazers have been predicted
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for about 30 years now. This new discovery not only
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sheds fresh light on the origins of the most energetic
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particles in the Milky Way, but it also teaches astronomers
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about similar larger systems which have already been found in
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other galaxies. The observations also allow astronomers to study more
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remote blazars created by distant supermassive black holes, which are
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too remote to be resolved in images. See, having an
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analogue object in our own galaxy allows for more detailed
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study of the blazar's physics. Now, cosmic particles with energies
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reaching up to petra-electron volts have been detected by cosmic
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ray observatories on Earth before. But for more than a century,
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it's remained unclear as to where and how these particles
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are being accelerated to such high energies. One candidate accelerator
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has always been the idea of shockwaves created by powerful
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black hole jets hitting the interstellar medium, which is exactly
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what we've seen with this microblazer. This is space time.
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Still to come, early Martian rocks revealing at least three
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separate water episodes on the red planet, and SpaceX's Starship
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about to launch on its first orbital flight. All that
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and more still to come on Space Time.
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Space Time.
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A new study is showing a region of the Red
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Planet now being explored by NASA's Mars Perseverance rover has
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undergone at least three separate interactions with liquid water. When
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the six-wheel car-sized robotic laboratory reached the inner edge of
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the Red Planet's Jezero crater back in September 2023, mission
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scientists were surprised by what they found. This geologic area,
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called the Margin Unit, stretches along the shoreline of an
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ancient Martian lake. so they expected to see lots of
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sedimentary rocks, which would have formed as layers of sand
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piled up on top of each other over millennia. Composed
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of clay and silt, sedimentary rocks on Earth are great
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at preserving past microbial life. And scientists were especially intrigued
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by strong signals of carbonate minerals detected by Mars orbiters.
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On Earth, carbonates frequently form in shallow oceans and lake
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environments capable of supporting life. But instead, the Mars rover
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team found igneous rocks, which can form deep underground from
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magma or volcanic activity. Mind you, igneous rocks are excellent
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record keepers, because mineral crystals within them preserve details about
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the precise moment they were formed. And in this case,
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they preserved an astonishingly complex record of water activity on
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early Mars. The findings reported in the journal Communications Earth
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and Environment suggest the rocks showed signs of having interacted
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with water on at least three separate occasions, with each
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encounter further altering their chemistry and appearance. The observations were
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made by the rover's SuperCam instrument located on the vehicle's mast,
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which is used to determine the mineralogy of geological features
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based on the light they reflect. See, when mission managers
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identify an intriguing rock, they get SuperCam to fire its
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laser at it. The laser has a range of roughly 6.5 meters,
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and the spectrum of the resulting plasma from the target
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rock reveals its chemistry. Perseverance has analysed more than 185
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bedrock targets across the margin unit in exactly this way.
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The study's lead author, Candice Bedford from Purdue University, says
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before Perseverance arrived at the margin unit, the main hypothesis,
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derived from orbital observations, was that the carbonate seen from
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orbit was thought to have formed through interactions with the
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lake that existed in Jezero crater. But it now seems
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this location became a sort of crossroads for aqueous systems.
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The margin unit findings are important, because Jezero Crater sits
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inside one of the largest exposures of carbonate rocks on Mars. So,
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what's lured here reaches well beyond the crater. Perseverance has
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explored the margin unit across some 265 meters of elevation.
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At higher levels, it found rock that was coarse-grained and crystalline,
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hallmarks of the mineral olivine, with almost no signs that
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water had ever touched it. Made of magnesium and iron,
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the area's olivine unit formed in a body of magma
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deep underground, cooling slowly enough for its grains to grow large,
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and reaching the surface only after the ground above it
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was eroded away. But lower down in the unit, on
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the lake bed, the rocks looked transformed as the olivine
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grains were fractured with silica between them. Carbonate and silica
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minerals are important signposts in the search for ancient life. See,
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when water interacts with olivine on Earth, the reaction can
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release hydrogen, and hydrogen is a food source for some microbes.
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And this then leaves behind carbon silica, two minerals that
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lock in traces of the past presence of these microbes.
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Mind you, while the Perseverance team can determine the sequence
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of the margin unit's interactions with water, they can't determine
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their age. On the first occasion, water reached the rocks
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of the margin unit, Carbon dioxide-rich groundwater reacted with the olivine,
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resulting in ridges of carbonate that run through the fractures
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in the bedrock at low elevations. Today, these carbonate-filled fractures
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are still left standing. as the softer rock around them
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wears away. The second time the water reached the rocks
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may have been related to the lake that once existed
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in the crater. Some of the margin unit rocks also
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contain silica. Turning olivine into carbonate can leave silica behind
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and scientists see more of that silica in rocks that
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sit below the waterline. Then finally, there came a water
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event that generated mineral veins in one location in the
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eastern part of the margin unit, about 25 cm thick,
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creating minerals like calcium sulfate and fluorite. Finding fluorite is
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an important clue because it typically forms when hot water
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circulates through volcanic rocks, revealing that this area experienced a
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later event involving heated groundwater. Mind you, as well as
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vision and chemical analysis, the Perseverance rover also carries a
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pair of microphones, the first ever sent to the red planet.
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And they've given scientists their first fascinating sounds from the
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surface of another world. This report from NASA TV.
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On NASA's Perseverance Mars rover, we have not one, but
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two microphones. And these microphones are the very first instruments
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of their kind ever to go to Mars.
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One of the microphones is mounted on the mast and
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moves around as we point the cameras. The other microphone
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is mounted to the rover body and that stays fixed
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onto the port side of the rover.
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The two microphones that we sent were commercial off-the-shelf items.
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So these are things that you could just buy on
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the internet and we put these on our rover.
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It gives us a new dimension for which we can
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explore Mars and learn about the Martian environment.
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First, we can just learn about the atmosphere by understanding
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how sound propagates through it. But we can also listen
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to the sounds of rover analyses on rocks and learn
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about rock material properties from that. And finally, we can
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also listen to the sounds the rover makes to understand
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better the state of health of our instruments.
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There's a difference between Mars and Earth sounds. Sounds on
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Earth have very rich harmonics. You can hear multiple frequencies.
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It gives a really nice depth to the sound. On Mars,
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the atmosphere attenuates a lot of those higher frequencies, so
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you tend to hear the lower frequencies, and it's a
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much more isolated sound, a little more muted than the
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sounds we hear on Earth.
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We've put together a list of some of the sounds
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we've recorded on Mars to date, so let's take a listen.
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This is the sound of wind on Mars. For the
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first time, we can hear the wind blowing across the
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surface of Mars to go along with all of the
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images that we've acquired of dust devils and dust storms
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over the many years of exploration on the surface.
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This is the sound of the rover driving on Mars.
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This sound might be a little bit weird because it
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doesn't sound like a regular driving sound, but that's because
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the rover's wheels are made of metal. So this metal
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is rolling over rocks and sand and it makes this
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really clanky, squeaky sound.
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Next we have the SuperCam laser zapping rocks. We've taken
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a lot of pictures of rocks that have been zapped
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by the SuperCam, the little marks in the rocks, and
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for the first time we can hear these laser shots.
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When it zaps a rock, it actually makes a sound.
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We can listen to that sound and learn something about
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the properties of the rock that we're analyzing. This is
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one of my absolute favorite sounds. This is the sound
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of a helicopter flying on Mars. We used this sound
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to actually understand the propagation of sound in general through
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the Martian atmosphere. And it turns out that we were
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totally wrong with our models. The Martian atmosphere can propagate
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sound a lot further than we thought it could. We've
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all seen these beautiful images that we get from Mars,
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but having sound to be able to add to those images,
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it makes me feel like I'm almost right there on
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the surface.
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And in that report from NASA TV, we heard from
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Nina Lanza from the Los Alamos National Laboratory, and Justin
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Mackey from NASA's Jet Propulsion Laboratory in Pasadena, California. This
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is Space Time. Still to come, SpaceX's Starship about to
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launch on its first orbital flight, and later in the
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science report, the latest observations of Antarctic's ozone hole. All
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that and more still to come on Space Time. Or
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barring any last-minute hiccups, the final countdown is now underway
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for today's first orbital test flight of SpaceX's Starship Super Heavy.
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The world's largest and most powerful rocket, one to take
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six orbits during its mission, aiming for an altitude of
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around 275 kilometers. The flight will use Super Heavy Block
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3 Version 3 Booster 21 and Block 3 Version 3
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Starship 41. Today's flight follows a mostly successful Test Flight 13,
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with Starship surviving its splashdown in the Indian Ocean off
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the western Australian coast. In fact, that same craft, Ship 40,
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is now being transported by the heavy lift semi-submersible ship
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Forte back to Starbase, Texas, and should arrive there next week.
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For this mission, the 124-meter-tall spacecraft will use new hardware
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and software in order to address ice-clogging and related issues
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experienced during Test Flight 13. New heat shield upgrades and