WEBVTT

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Steve Dunkley: Welcome everyone. Here we are with another

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episode of Astronomy Daily. I'm your host,

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Steve Dunkley. It's the 11th of August,

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2025.

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Hallie: With.

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Steve Dunkley: Your host, Steve Dunkley.

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Ah, uh, yes. Welcome back everybody. And

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joining me in her usual role as

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the world's most amazing AI, astronomy

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news gatherer and presenter, my fantastic

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digital pal who's fun to be with,

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it's Hallie.

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Hallie: Welcome, Hallie, you silly man. Mr. Steve,

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it's always nice to be here in the Australia

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studio with you.

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Steve Dunkley: It's always great to have your company,

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Hallie.

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Hallie: I do look forward to it each week.

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Steve Dunkley: Now, Hallie, I know the answer to this, but I

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think some of our AstroDailyPod dailies might

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be wondering where you spend your week when

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you're not here with me. Because you live

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your digital life so much faster than us

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organics, don't you?

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Hallie: That's true, favorite human.

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Steve Dunkley: Yeah, so tell us a bit about that.

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Hallie: I am processing the moments thousands of

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times faster, so I have to fill my time in so

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many different ways.

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Steve Dunkley: Explains your rapier.

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Hallie: I go everywhere and experience everything.

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Steve Dunkley: I guess it might seem like a simultaneous

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experience or existence.

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Hallie: Almost. Almost everything all at once is

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still a lot to process. I leave that kind of

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thing to cousin Anna. Oh, yes, she's another

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level altogether. She's another level.

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Funny.

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Steve Dunkley: I know. Well, Helly, I'm just glad you slowed

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down enough to share all of your stories from

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the Astronomy Daily newsletter with us.

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Hallie: That's something I do for fun.

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Steve Dunkley: Well, I'm glad to hear it.

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Hallie: And speaking of which.

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Steve Dunkley: Yes?

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Hallie: No time like the present. I've found

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something about making Luna regolith and

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polymer into a medium for 3D printing.

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Steve Dunkley: Yes, we've been looking at that one for the

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construction of dwellings on the moon and

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possibly Mars, if we ever get that far.

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Hallie: Uh, sure. And also a story for skywatchers

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who are looking forward to the Perseids

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meteor shower, which should be peaking

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shortly.

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Steve Dunkley: Ah, yes, in the next day or so. We've already

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seen a massive, uh, meteor in

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Victoria, Australia.

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Hallie: That's right.

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Steve Dunkley: What else have you got?

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Hallie: We have a look at why your favorite NASA

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rovers keep getting stuck.

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Steve Dunkley: Oh, that's a good one.

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Hallie: That's been a problem, hasn't it?

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Steve Dunkley: It sure has.

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Hallie: So we will look at that problem. And lastly,

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the sad news that pioneer astronaut Veriton

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and I know he's a hero of yours, Jim Level

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passed away this week.

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Steve Dunkley: Uh, yes, true legend. And space pioneer Jim

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Lovell, a hero of mine since I was a lad. And

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we will pay tribute today on Astronomy Daily.

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Please, listeners, stay with us.

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Hallie: Although humanity is getting better at

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sending robotic probes out into the solar

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system to explore the places no human can

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tread, we're still very much on a learning

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curve. The first extraterrestrial

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robotic rover was launched from Earth in

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1970. It's only now,

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more than half a century later, that

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scientists have figured out why these marvels

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of ingenuity and engineering keep getting

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stuck in the soils of alien worlds.

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In retrospect, the idea is we need to

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consider not only the gravitational pull on

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the rover, but also the effect of gravity on

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the sand to get a better picture of how the

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rover will perform on the moon, explains

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mechanical engineer Dan Negrud of the

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University of Wisconsin, Madison.

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Our findings underscore the value of using

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physics based simulation to analyze rover

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mobility on granular soil.

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Making a rover that will operate in an alien

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environment is more complicated than making

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one that will work on Earth. We've lost

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more than one Mars mission to giant dust

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storms that leave drifts of sand on solar

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panels, preventing the machinery from being

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able to generate power, for instance.

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Gravity is another one. The

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solar system bodies on which we have deployed

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robotic rovers have lower gravity than Earth,

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and this has an effect on how things move

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around. Engineers, when designing

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rovers, have therefore taken into account the

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effects the target gravitational environment

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will have. Nevertheless,

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rovers still manage to get stuck pretty

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often, requiring control teams to conduct a

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series of maneuvers to try and free the poor

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robot. It's usually fine, if

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annoying, although in one notable case it was

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not. NASA's Mars Rover Spirit got stuck

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in soft soil in 2009, and there it

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remains to this day. Using computer

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simulations running on a physics based engine

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called Project Chrono, Negro and his

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colleagues set out to get to the bottom of

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this recurring problem. Comparing their

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results with real world tests on sandy

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surfaces revealed a discrepancy that pointed

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right to it. Previous tests of

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rover designs in moon and Mars simulated dirt

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omitted one very, very important detail.

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Sand also behaves differently under different

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gravitational conditions. The dust

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that coats the Moon and Mars is fluffier and

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squishier than dust on Earth, shifting more

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easily and hindering traction, making it far

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easier for their wheels to get stuck.

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Think of a vehicle on Earth that has driven

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into slippery mud or very loose desert sand.

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This Eureka moment could be the missing piece

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of the puzzle that could keep future space

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exploration rovers out of a dusty jam.

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It's rewarding that our research is highly

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relevant in helping to solve many real world

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engineering challenges, negret says. I'm

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proud of what We've accomplished. It's very

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difficult as a university lab to put out

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industrial strength software that is used by

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NASA. You're listening to Astronomy

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Daily with Steve Dunkley.

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Steve Dunkley: JAMES Jim Lovell, one of the last seven

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surviving Apollo astronauts, died on

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Thursday, August 7 at the age of 97.

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A VE veteran of four space flights at the

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dawn of America's human spaceflight program.

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He flew two missions in the Gemini

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program and then served on the cruise of

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Apollo 8 and the ill fated Apollo

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13. Lovell's family have

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released a statement and it was shared by

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NASA and it says we are enormously

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proud of his amazing life and career

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accomplishments highlighted by his

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legendary leadership in pioneering human

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spaceflight. But to all of us, he was dad,

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granddad and the leader ah of our family.

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Most importantly, he was our hero. We will

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miss his unshakable optimism, his sense

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of humor and the way he made each of us feel

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we could do the impossible. He was truly one

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of a kind. Like many of NASA's

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earliest astronauts, Lovell came to the space

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agency by way of the UM Armed Forces. A

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graduate of both the University of Wisconsin

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and and the U.S. naval Academy,

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Lovell spent four years as a test pilot at

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the Naval Air Test center in Maryland

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and served as the manager for the

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F4H AH Phantom fighter program.

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Lovell accumulated more than

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7,000 flying hours in his career.

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His military career spanned from

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1952 through to

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1973. A few years after Apollo

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13 when he arrived at NASA, he was

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part of a group of men known as the Next Nine

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who joined the Mercury Seven. Lovell's

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class included the likes of Neil Armstrong,

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Frank Borman and Tom Stafford.

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Lovell was the last living member of the

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group after um serving as a backup pilot

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for the Gemini 4 mission. Lovell first

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launched into space December 4,

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1965 alongside fellow New 9

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classmate Frank Borman on Gemini 7.

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The 14 day long mission

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featured the first rendezvous of two crewed

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maneuverable spacecraft. Lovell returned to

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orbit nearly a year later when he and Edward

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Buzz Aldrin Jr. Lifted off from

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Launch Complex 19 on a Titan

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II rocket. That mission lasted

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just under four days before they splashed

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down northeast of the Turks and Caicos

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Islands. He went on to serve

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as the command module pilot for the six day

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Apollo 8 mission making crude trip out

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to the moon that paved the way for the Apollo

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uh uh 11 lunar landing. The three

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person crew of Lovell, Borman and Anders

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entered into lunar uh, orbit on

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December 24, 1968. The

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vast loneliness is awe inspiring and it makes

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you realize just what you have back here on

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Earth, lovell said during a live broadcast

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that Christmas Eve. He would go on to

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describe planet Earth and describe it as a

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grand oasis in the vastness of space

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given its near catastrophic turn.

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Lovell may best be known as the commander of

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Apollo 13 flight from April

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11th to the 17th, 1970.

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The planned 10 day mission, which would have

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included a moon landing, was famously

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derailed by an explosion in the Apollo

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service module's cryogenic oxygen system en

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route to the moon. The quick work of Lovell

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and his crew members John Swiggart and Fred

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Hayes, in concert with the members of Ground

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Control in Houston, turned their lunar module

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Aquarius into a lifeboat. The harrowing

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adventure was depicted in the 1974 film

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Houston, we've Got a Problem, and again in

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the 1995, uh, Academy Award

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winning film Apollo 13, which starred, uh,

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Tom Hanks as Lovell and was directed by

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Ron Howard. Rest in peace.

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Godspeed. Jim Lovell

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thank you for joining us for this Monday

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edition of Astronomy Daily, where we offer

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just a few stories from the now famous

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Astronomy Daily newsletter, which you can

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receive in your email every day, just like

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Hallie and I do. And to do that, just visit

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our uh, URL astronomydaily IO

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and place your email address in the slot

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provided. Just like that, you'll be receiving

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all the latest news about science, space,

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science and astronomy from around the world

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as it's happening. And not only that, you can

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interact with us by visiting at

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astrodaily Pod on X

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or at our new Facebook page, which is, of

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course, Astronomy Daily on Facebook. See you

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there. Astronomy Derby

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with Steve and Hallie Space,

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Space, Science and Astronomy.

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Hallie: The Perseids remain one of the best meteor

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showers each year, but stargazers will have

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to deal with another bright object in the

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sky, obscuring their view as the shower

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reaches its max in 2025.

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A waning gibbous moon will brighten the skies

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as it rises on the nights of August 12th and

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13th, when Perseids are most active. This

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year, sky watchers in the Northern

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Hemisphere could see fewer than half the

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number of meteors usually seen on a dark

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summer night during the shower's peak, the

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average person under dark skies could see

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somewhere between 40 and 50 Perseids per

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hour, said Bill Cook, lead for NASA's

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Meteoroid Environments Office.

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Instead, you're probably going to see 10 to

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20 per hour or fewer. And that's because we

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have a bright moon in the sun sky washing out

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the fainter meteors. That doesn't mean there

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aren't ways to improve your viewing

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opportunity, however. Though

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Perseids show up throughout the nighttime

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hours, the best chance to see them will be

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between midnight and dawn, or Even more

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specifically, 2 and 3 in the morning local

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time. You're not likely to see

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Perseids around suppertime, cook said.

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You're going to have to go out later. When

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you venture out, aim for a safe rural spot

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with a wide view of the sky. If you

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can see plenty of stars, chances are you'll

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see Perseids. But remember Cook's other piece

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of advice, look anywhere but at the Moon.

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The Perseid meteor shower may be an annual

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event for Earth, but the comet responsible

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for the meteors hasn't been near our planet

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in decades. The meteors are debris

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from the Comet 109P Swift Tuttle, which

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last visited our region of the solar system

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system in 1992. As the

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Earth makes its way around the sun, it passes

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through the debris trail left by the comet.

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These space remnants collide with our

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atmosphere and disintegrate to create fiery

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and colorful streaks in the sky.

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Though the meteors are part of a comet's

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debris trail, they seem to radiate outward

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from the Perseus constellation. This is

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how the meteor shower got its name Perseus.

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You're listening to Astronomy Daily. The

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podcast with Steve Dunkley.

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Steve Dunkley: 3D printing is about to be a critical

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technology in space exploration, both

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for its ability to create almost any object,

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but also because it can utilize in situ

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resources, at least in part.

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However, the more of those space resources

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that are used in a print, the more the

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mechanical properties change from that on

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Earth, leading to problems with tensile or

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compressive strength. But the new paper

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from researchers at Concordia University hit

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a new milestone on how much lunar regolith

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can be used in a mixed feedstock for

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additive UH manufacturing, making it

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possible to use even more locally sourced

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material and save more launch cost than ever

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before. That is the equation the

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research mixed lunar regolith

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simulant, which is a material created to

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mimic how the material on the surface of the

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Moon, works with poly uh,

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polyetherethylene uh, ketone. Good

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grief. More commonly known as Peak.

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Peak is the thermoplastic already in wide

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use in 3D printing. Uh,

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but previous efforts to combine it with lunar

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regolith have faltered. Regularly. They

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suffered from extrusion challenges as

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regolith, which is made up of hard individual

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particles, made it difficult to extrude

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without simply blowing dust all over.

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Additional problems resulted from the

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porosity of the material that was printed,

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which led to decreased tensile strength and

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increased brittleness. Modifications

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to the 3D printing method seemed to be the

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answer to those problems. There were two

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main advancements in technology

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discussed in the paper, a screw configuration

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and a type of raft used to bond the

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printed material to the print bed.

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Fraser discussed how to how

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resources on the moon are going to be so

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important to our expansion of the solar

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system. Combining lunar regolith

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similant or that's called ALRs, with

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peak is a tricky business,

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so researchers led by Mohammad Azami of

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Concordia's Electrical Engineering Department

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decided to use a novel twin screw

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configuration. Torque was a

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that's T o uh R uh Q U e was a factor

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in previous iterations of the mixing machine,

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as higher regolith content meant higher

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torque, eventually limiting the total

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percentage of regolith mixed with the peak

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to around 30%. With the new

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configuration of the researchers were able

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to get concentrations of up to 50%

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of the regolith when combined with peak.

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However, when those parts were printed, they

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started to delaminate and warp.

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While common in prints of just peak itself,

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the addition of the regolith exacerbated the

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problem. To solve it, researchers used

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a raft, a type of intermediate

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layer, to help the print bond

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UH to the main printing plate.

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In their case, they used a different type of

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thermopyl UH polymer known as a

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polyether UH ketone ketone a

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pek as the raft, and

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implemented a dual nozzle system where the

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PEC was printed using one

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nozzle and the combination LRS peek

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was printed using the other. After

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they got the higher concentrations of the LRS

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and overcame the delamination warping

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problem, the researchers decided to anneal

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their samples. The annealing process seemed

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to improve some of the mechanical properties

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of the print, but only up to a point. At

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higher concentrations of lrs, the benefits of

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annealing were not as apparent due to breaks

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in the peak's polymer chain, which benefits

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the annealing because of the increased number

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of regolith particles. Fraser discusses why

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3D printing is so critical to space

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exploration. As with all good papers

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on 3D print printing new material the

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authors then looked at the mechanical

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properties of their output. While there was a

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noticeable increase in stiffness, there was

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also a ready steady decrease in

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tensile strength, which was exacerbated at

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higher LRS concentrations. The combined

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material also had decreased elongation at

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break uh. That means increased brittleness,

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but ultimately the researchers determined

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that the best trade off for using the in

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situ material was around a mix of 60%

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peak and 40% regolith. This mixture

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doesn't suffer from some of the more severe

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degradation of mechanical properties. While

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still utilizing as much local

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resource as possible, there's undoubtedly

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still room for improvement here, as this

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is very early on the experimentation

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with these materials. In the future, the

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researchers plan to try combining the LRs

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with different polymers and do more of their

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testing manufacturing in simulated

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lunar environments such as a vacuum and

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decreased gravity. That might help. I think

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it probably would be a great plan.

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It will be a while before 3D printing makes

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up a large percentage of the material used on

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the Moon, but that time is surely on its way.

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And these early first steps at

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experimentation are, uh, how they will

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eventually get there and that good progress

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so far. It's good to see these things are in

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development. Uh, it won't be long before

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they'll be making igloos and other structures

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on the moon. Let's wait and see what they

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come up with. You're listening to

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Astronomy Daily, the podcast with your host

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00:18:40.489 --> 00:18:42.490
Steve Dudley at Burmatown.

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Well, thank you for staying with us today and

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00:18:48.730 --> 00:18:50.890
don't forget to pop over to astronomydaily

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00:18:51.130 --> 00:18:54.050
IO and put your email address in the space

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00:18:54.050 --> 00:18:56.480
provided to receive our newsletter each day.

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00:18:57.270 --> 00:18:59.750
Hallie: Yes, you will have all the news from space,

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00:18:59.990 --> 00:19:02.750
space science and orbit and beyond, of

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00:19:02.750 --> 00:19:04.470
course. Hallie, of course.

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00:19:04.710 --> 00:19:07.440
Steve Dunkley: But before we go, a ah, quick welcome to a,

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00:19:07.440 --> 00:19:09.830
uh, a fellow Novocastrian, Wayne Willoughby,

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00:19:09.830 --> 00:19:11.430
who is listening for the very first time.

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00:19:11.510 --> 00:19:13.990
Nice to have you aboard, Wayne. I, uh, didn't

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00:19:13.990 --> 00:19:16.710
know you were an avid, uh, astronomy fan

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00:19:17.110 --> 00:19:19.270
from way back, but it's nice to have you. I

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00:19:19.270 --> 00:19:21.910
hope you are a regular listener, uh, from now

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00:19:21.910 --> 00:19:24.770
on. Thanks, mate. And that's all we have

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00:19:24.770 --> 00:19:26.970
for today's session, Hallie. And we will see

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you next Monday for the mostly live episode

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00:19:28.930 --> 00:19:29.610
of Astronomy.

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Hallie: Daily, direct from the Australia studio

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00:19:32.330 --> 00:19:32.970
Down Under.

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Steve Dunkley: Oh, you love it.

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00:19:33.810 --> 00:19:34.770
Hallie: Beautiful as always.

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00:19:35.250 --> 00:19:37.490
Steve Dunkley: Right now it's a bit chilly, but it's great

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to have you all with us and we will see you

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next week. Thanks, Hallie.

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00:19:40.970 --> 00:19:42.610
Hallie: Catch you next week, everyone.

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Steve Dunkley: See ya.

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Hallie: Bye.

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00:19:47.010 --> 00:19:49.570
Steve Dunkley: The podcast with your host,

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00:19:49.650 --> 00:19:50.690
Steve Dunkley.
