Stellar Q&A: Unraveling Fusion Mysteries, Martian Caves & Solar Cycles

Stellar Q&A: Unraveling Fusion Mysteries, Martian Caves & Solar Cycles

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Cosmic Queries: Unraveling Stellar Mysteries In this enlightening Q&A episode of Space Nuts, hosts Andrew Dunkley and Professor Jonti Horner tackle a trio of intriguing questions from listeners. From the complexities of hydrogen fusion to the potential for life in Martian caves and the mysteries of stellar activity, this episode is a deep dive into the cosmos.
Episode Highlights:
Hydrogen to Helium Fusion: Ken from Maroochydore seeks clarity on the fusion process in stars, questioning why the mass of helium appears greater than the sum of its hydrogen components. Jonty explains the concept of binding energy and how it plays a crucial role in energy production during fusion, demystifying this fundamental stellar process.
Caves on Mars: Mark from Brisbane wonders about the possibility of limestone caves on Mars and whether they could support life with a stable atmosphere. The hosts discuss the geological differences between Earth and Mars, the challenges of oxygen presence, and the implications for future human habitation in Martian caves.
Understanding Stellar Activity: Casey from Colorado inquires about the changing activity levels of stars and solar cycles. Jonty elaborates on the magnetic forces driving solar cycles, the variability of different stars, and the fascinating world of asteroseismology, revealing how stars can change over time and what that means for our understanding of the universe.

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Stay curious, keep looking up, and join us next time for more stellar insights and cosmic wonders. Until then, clear skies and happy stargazing.

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- Introduction to Hydrogen Fusion
- The Binding Energy Explained
- Potential for Life in Martian Caves
- The Nature of Stellar Activity
- Understanding Solar Cycles and Variability


00:00:00 --> 00:00:02 Andrew Dunkley: Hi there. Thanks for joining us. This is a Q

00:00:02 --> 00:00:04 and A edition of Space Nuts. My name is

00:00:04 --> 00:00:07 Andrew Dunkley. Thanks for your company. Uh,

00:00:07 --> 00:00:09 coming up, we're going to answer audience

00:00:09 --> 00:00:12 questions. Um, one from Ken. Uh,

00:00:12 --> 00:00:14 I'm going to paraphrase his 500 word

00:00:14 --> 00:00:16 question by saying, why don't the numbers add

00:00:16 --> 00:00:18 up when turning hydrogen into helium?

00:00:19 --> 00:00:22 Also, a question from Mark about caves on

00:00:22 --> 00:00:25 Mars and Casey wants

00:00:25 --> 00:00:28 to talk about changes in stars.

00:00:28 --> 00:00:30 That's all coming up on this Q and A edition

00:00:30 --> 00:00:33 of space nuts. 15 seconds. Guidance is

00:00:33 --> 00:00:36 internal. 10, 9,

00:00:36 --> 00:00:38 ignition sequence start. Space nuts.

00:00:39 --> 00:00:40 Jonti Horner: 5, 4, 3, 2.

00:00:40 --> 00:00:43 Andrew Dunkley: 1. 2, 3, 4, 5, 5, 4, 3,

00:00:43 --> 00:00:44 2, 1.

00:00:44 --> 00:00:45 Jonti Horner: Space nuts.

00:00:45 --> 00:00:47 Andrew Dunkley: Astronauts report it feels good.

00:00:48 --> 00:00:50 I just got a text to say my car's been

00:00:50 --> 00:00:52 serviced, so I'll be back in about 20 minutes

00:00:52 --> 00:00:53 if you just want to. Hang on. I'm kidding.

00:00:54 --> 00:00:56 Uh, joining us to answer all those questions

00:00:56 --> 00:00:58 is Professor Jonty Horner, professor of

00:00:58 --> 00:01:00 Astrophysics at the University of Southern

00:01:00 --> 00:01:01 Queensland. Hi, Jonty. Good day.

00:01:01 --> 00:01:02 Jonti Horner: How are you going to.

00:01:03 --> 00:01:05 Andrew Dunkley: I am m. All right. Good to see you again.

00:01:05 --> 00:01:06 Jonti Horner: It's good to be back. I was going to say the

00:01:06 --> 00:01:08 amount I've been talking too much. You've

00:01:08 --> 00:01:11 probably got time to go and get the car and I

00:01:11 --> 00:01:11 could probably

00:01:11 --> 00:01:14 Andrew Dunkley: ask you a question, bolt down and get the car

00:01:14 --> 00:01:17 and come back just in time to hear the end

00:01:17 --> 00:01:18 of the first sentence.

00:01:18 --> 00:01:20 Jonti Horner: Yes, and I do apologise to listeners if I've

00:01:20 --> 00:01:23 rambled on too much, but it's when you get to

00:01:23 --> 00:01:24 talk about your hobby and people have to

00:01:24 --> 00:01:26 listen, it's, you know, hard not to get

00:01:26 --> 00:01:28 excited and it is, isn't it?

00:01:28 --> 00:01:28 Andrew Dunkley: It is.

00:01:29 --> 00:01:31 Let's get, uh, straight into our first

00:01:31 --> 00:01:34 question. Hi, Andrew and Jonty. I'm going to

00:01:34 --> 00:01:35 say it's not what he wrote, but anyway, it

00:01:35 --> 00:01:38 doesn't matter. Ken, uh, from Maroochydore,

00:01:38 --> 00:01:40 longtime listener and fan and love the way

00:01:40 --> 00:01:43 you make complex issues sound simple. I am

00:01:43 --> 00:01:45 trying to understand the basic fusion

00:01:45 --> 00:01:47 reaction that both me and my accountant are

00:01:47 --> 00:01:50 struggling with. Uh, the basic fusion

00:01:50 --> 00:01:52 reaction in our sun converts hydrogen to

00:01:52 --> 00:01:55 helium. To summarise the reaction, four

00:01:55 --> 00:01:58 hydrogen nuclei, I.e. four protons,

00:01:58 --> 00:02:01 go through two steps to create one

00:02:01 --> 00:02:04 helium nucleus containing two neutrons

00:02:04 --> 00:02:06 and two protons. Additionally, gamma rays,

00:02:06 --> 00:02:09 neutrinos and positrons are released.

00:02:09 --> 00:02:12 My anatomy textbook tells me that about

00:02:12 --> 00:02:14 600 million tonnes of hydrogen convert to

00:02:14 --> 00:02:17 596 million tonnes of helium every

00:02:17 --> 00:02:20 second. The 4 million tonnes is

00:02:20 --> 00:02:23 conveyed to energy as per E equals

00:02:23 --> 00:02:26 MC squared. If neutrons had a lower

00:02:26 --> 00:02:28 mass than protons it would all make perfect,

00:02:28 --> 00:02:31 perfect sense, but they don't. They have a

00:02:31 --> 00:02:34 higher mass. So the mass of the helium

00:02:34 --> 00:02:37 nucleus is higher than the mass of the four

00:02:37 --> 00:02:39 protons. All the explanations I've read

00:02:39 --> 00:02:42 sound pretty dodgy, and my accountant says he

00:02:42 --> 00:02:44 could never get away with such, such

00:02:44 --> 00:02:46 explanations with the tax department.

00:02:47 --> 00:02:49 Could you please explain the devil in the

00:02:49 --> 00:02:52 detail that I'm missing? I, uh, love it.

00:02:52 --> 00:02:54 That's a great question. And thanks for the

00:02:54 --> 00:02:56 research, Ken. Hope all is well in

00:02:56 --> 00:02:58 Maroochydore. Not far from you, just a bit

00:02:58 --> 00:02:59 further up the coast.

00:02:59 --> 00:03:02 Jonti Horner: Yes, out to the coast and up a bit north of

00:03:02 --> 00:03:04 Brisbane, up on the sunshine course, which is

00:03:04 --> 00:03:05 kind of lovely area.

00:03:05 --> 00:03:08 Andrew Dunkley: It's kind of, it's only kind of lovely.

00:03:08 --> 00:03:09 Jonti Horner: Yeah, only kind of lovely. It's getting,

00:03:09 --> 00:03:11 getting very aggressively more and more

00:03:11 --> 00:03:13 touristed. Tracks a slightly different

00:03:13 --> 00:03:15 tourist demographic to the Gold coast, which

00:03:15 --> 00:03:18 is south of Brisbane, um, but is still

00:03:18 --> 00:03:20 a little bit more touristy than you'd like

00:03:20 --> 00:03:22 it. It's a little bit like hippie central,

00:03:22 --> 00:03:25 but not to the level of Byron nuts.

00:03:25 --> 00:03:27 Andrew Dunkley: Yeah, I get you. Yeah, yeah, yeah.

00:03:27 --> 00:03:30 Byron is the hippie, uh, capital of the, of

00:03:30 --> 00:03:33 the country, I think. Or to, to

00:03:33 --> 00:03:36 be more like Nimbin a bit further down.

00:03:36 --> 00:03:38 That's, that's very, very hippie.

00:03:39 --> 00:03:41 Anyway, um, so,

00:03:41 --> 00:03:43 yeah, he doesn't understand the balance. It

00:03:43 --> 00:03:46 doesn't. It doesn't. To paraphrase, why don't

00:03:46 --> 00:03:48 the numbers add up when turning hydrogen into

00:03:48 --> 00:03:50 helium? That's the short version of the

00:03:50 --> 00:03:51 question.

00:03:51 --> 00:03:52 Jonti Horner: And I totally get that. Because if you look

00:03:52 --> 00:03:55 at the masses of protons and

00:03:55 --> 00:03:58 neutrons in isolation and add them together,

00:03:58 --> 00:04:01 helium is two protons, two neutrons. Add them

00:04:01 --> 00:04:04 together, taking the mass of a proton and the

00:04:04 --> 00:04:06 mass of a neutron, and you get a given value

00:04:06 --> 00:04:09 for the mass of a helium nucleus. And

00:04:09 --> 00:04:10 then you look at the mass of a helium nucleus

00:04:10 --> 00:04:13 and it isn't that mass. And that doesn't make

00:04:13 --> 00:04:15 sense because if you've got four nucleons

00:04:16 --> 00:04:19 together, surely the mass of the nucleus is

00:04:19 --> 00:04:21 the four nucleons added together. And that's

00:04:21 --> 00:04:23 effectively the fundamental of what's being

00:04:23 --> 00:04:26 said here. Added to which a, uh,

00:04:26 --> 00:04:29 hydrogen nucleus is a proton, a deuterium

00:04:29 --> 00:04:30 nucleus is a proton and a neutron, but

00:04:30 --> 00:04:33 hydrogen nucleus is a proton. Four hydrogen

00:04:33 --> 00:04:36 nuclei go together to make a helium nucleus,

00:04:36 --> 00:04:38 which is 2 protons, 2 neutrons and M. In the

00:04:38 --> 00:04:40 process, you kick a few things out and do a

00:04:40 --> 00:04:43 few weird things, surely. Therefore,

00:04:43 --> 00:04:46 four hydrogen nuclei have the mass of

00:04:46 --> 00:04:49 four protons. One helium nucleus has a mass

00:04:49 --> 00:04:51 of two Protons plus two neutrons. And when

00:04:51 --> 00:04:53 you get the numbers off Wikipedia, that would

00:04:53 --> 00:04:55 suggest that the helium nucleus should be

00:04:55 --> 00:04:57 more massive than hydrogen and you should

00:04:57 --> 00:05:00 lose energy rather than create it, because

00:05:00 --> 00:05:02 you've had to create mass. Fundamentally in

00:05:02 --> 00:05:04 actuality though, the mass of the helium

00:05:04 --> 00:05:07 nucleus is lower than the mass of two

00:05:07 --> 00:05:10 protons plus two neutrons. And that's

00:05:10 --> 00:05:12 where the misunderstandings coming in, or not

00:05:12 --> 00:05:14 really misunderstanding, that's where the

00:05:14 --> 00:05:16 complexity and the confusion comes in

00:05:17 --> 00:05:19 and takes everybody a little bit to get your

00:05:19 --> 00:05:20 head around this when you first come across

00:05:20 --> 00:05:23 it. Helium nucleus, quite rightly is

00:05:23 --> 00:05:25 made of two protons and two neutrons. But

00:05:25 --> 00:05:28 those two protons and neutrons are held

00:05:28 --> 00:05:30 together. They're bound together by the

00:05:30 --> 00:05:32 nuclear force, held in strongly enough that

00:05:32 --> 00:05:34 the repulsion from the two positively charged

00:05:34 --> 00:05:37 things don't blow it apart. So there is

00:05:37 --> 00:05:38 something going on called the binding energy.

00:05:39 --> 00:05:41 And the binding energy is the amount of

00:05:41 --> 00:05:43 energy you would have to throw at a helium

00:05:43 --> 00:05:46 nucleus to separate the two protons and

00:05:46 --> 00:05:48 the two neutrons and make them fly through

00:05:48 --> 00:05:51 space separately. Again with the energy and

00:05:51 --> 00:05:54 mass equivalence. If you were to do that,

00:05:54 --> 00:05:57 you would then have 4, 4 nucleons

00:05:57 --> 00:05:58 independently of each other, which would have

00:05:58 --> 00:06:01 the mass we've just calculated. But you've

00:06:01 --> 00:06:03 had to add energy and energy is equivalent to

00:06:03 --> 00:06:06 mass. So what it's saying is that the mass of

00:06:06 --> 00:06:09 a helium nucleus is lower than the

00:06:09 --> 00:06:11 mass you would expect from the four nucleons

00:06:11 --> 00:06:13 because of the effect of this binding energy

00:06:13 --> 00:06:15 that's in there. And that binding energy is

00:06:15 --> 00:06:18 something we can calculate. It's helium is

00:06:18 --> 00:06:20 remarkably high compared to the things on

00:06:20 --> 00:06:22 either side of it. Helium 3 hydrogen, 3

00:06:22 --> 00:06:25 lithium, and that is incredibly tightly

00:06:25 --> 00:06:27 bound. That binding energy

00:06:28 --> 00:06:30 is what leads to the little bit of mass

00:06:30 --> 00:06:32 deficit with the helium atom being lighter

00:06:32 --> 00:06:34 than the four nucleons that went to make it.

00:06:35 --> 00:06:37 And it's that energy that's released. Now

00:06:37 --> 00:06:40 this is why nuclear fusion can work, because

00:06:40 --> 00:06:43 if you put four nucleons

00:06:43 --> 00:06:45 together from hydrogen atoms and make ah,

00:06:45 --> 00:06:48 from hydrogen nuclei to make a helium nuclei

00:06:48 --> 00:06:50 with the binding energy, it means you get

00:06:50 --> 00:06:53 more energy out than you get in. You produce

00:06:53 --> 00:06:56 energy. And that's true if you fuse

00:06:56 --> 00:06:58 helium. Helium is difficult. You can't fuse

00:06:58 --> 00:07:01 it to anything until carbon because

00:07:01 --> 00:07:04 lithium, beryllium, boron have a

00:07:04 --> 00:07:06 lower binding energy per nucleon than helium

00:07:06 --> 00:07:09 does. So you actually have to put energy in

00:07:09 --> 00:07:11 to fuse helium to those things rather than

00:07:11 --> 00:07:13 getting energy out. So that doesn't happen.

00:07:13 --> 00:07:16 Helium can fuse to carbon, but you need

00:07:16 --> 00:07:18 three helium nuclei to collide at once.

00:07:19 --> 00:07:22 Which is hard. From then on, from carbon

00:07:22 --> 00:07:23 upwards, you can get a little bit of energy

00:07:24 --> 00:07:25 from fusing heavier and heavier things

00:07:25 --> 00:07:28 together until you get to iron. Iron 56

00:07:28 --> 00:07:31 has the highest amount of binding energy per

00:07:31 --> 00:07:34 nucleon. So if you try and fuse

00:07:34 --> 00:07:36 hydrogen, fuse iron atoms to make a heavier

00:07:36 --> 00:07:39 atom than iron, you have to put more energy

00:07:39 --> 00:07:42 in than you get out. And that's what causes

00:07:42 --> 00:07:44 stars fundamentally to go supernova, is that

00:07:44 --> 00:07:46 they fuse heavier and heavier things to iron

00:07:46 --> 00:07:48 and then the fuel sources cut off suddenly,

00:07:49 --> 00:07:51 they then collapse. You get a boom because of

00:07:51 --> 00:07:54 the shockwave going bouncy, bouncy. Some of

00:07:54 --> 00:07:56 the energy from that supernova,

00:07:56 --> 00:07:59 uh, gets taken up in the fusion of iron to

00:07:59 --> 00:08:01 make heavier elements and gets sunk into

00:08:01 --> 00:08:03 that, which is where we get all the elements

00:08:03 --> 00:08:05 heavier than iron, everything up to uranium

00:08:05 --> 00:08:08 and beyond those things heavier than

00:08:08 --> 00:08:11 iron, the binding energy per nucleon gets

00:08:11 --> 00:08:13 lower and lower the further up you go. Which

00:08:13 --> 00:08:16 is why for things heavier than iron,

00:08:16 --> 00:08:19 nuclear fusion costs energy, but nuclear

00:08:19 --> 00:08:22 fission liberates energy because you're going

00:08:22 --> 00:08:24 back up the slope again. So uranium

00:08:24 --> 00:08:26 fissioning to be become lighter elements

00:08:26 --> 00:08:28 gives off energy because of that binding

00:08:28 --> 00:08:30 energy difference. It's all part of the same

00:08:30 --> 00:08:32 thing. Now I, I understand that

00:08:32 --> 00:08:35 intuitively this really isn't a

00:08:35 --> 00:08:37 satisfying answer because this binding energy

00:08:37 --> 00:08:39 sounds a bit like your accountant thinking

00:08:39 --> 00:08:41 you've got a tax dodge. It's a bit like

00:08:41 --> 00:08:43 capital gains tax or fringe benefits or, or

00:08:43 --> 00:08:46 uh, what is it? Negative gearing? Binding

00:08:46 --> 00:08:48 energy may well be the negative gearing of

00:08:48 --> 00:08:50 the cosmos because it's when you put four

00:08:50 --> 00:08:51 nucleons together, they're wear less than

00:08:51 --> 00:08:53 they would do on their own.

00:08:53 --> 00:08:56 Um, it's ultimate waste loss plan. But it is

00:08:56 --> 00:08:58 this bind that leads to the mass you

00:08:58 --> 00:09:01 would measure for a helium nucleus being less

00:09:01 --> 00:09:03 than the mass you would measure for hydrogen

00:09:03 --> 00:09:06 nuclei. And it's a mass as you measure, not

00:09:06 --> 00:09:08 the masses of the individual components. If

00:09:08 --> 00:09:10 you took them out and put them on their own,

00:09:10 --> 00:09:13 that is the important thing. This is usually

00:09:13 --> 00:09:15 skipped in the explanations. And this is

00:09:15 --> 00:09:17 where the challenges come in. Because in the

00:09:17 --> 00:09:20 explanations you just say a helium atom is

00:09:20 --> 00:09:22 less massive than four hydrogen atoms.

00:09:23 --> 00:09:25 Ergo some mass has been lost. Therefore

00:09:25 --> 00:09:28 energy is produced by equals MC squared. And

00:09:28 --> 00:09:30 it skips all this discussion of the particle

00:09:30 --> 00:09:32 physics underpinning it on um, this binding

00:09:32 --> 00:09:35 energy. As always, there is a fairly

00:09:35 --> 00:09:37 detailed discussion of this in the wikipedia

00:09:37 --> 00:09:39 page for Helium 4. Talking about the

00:09:39 --> 00:09:41 stability and that's got the binding energy

00:09:41 --> 00:09:43 curve in. There is also discussions of

00:09:43 --> 00:09:45 binding energy and that out there. And

00:09:45 --> 00:09:48 particle Physics out there. It is basically

00:09:48 --> 00:09:50 though, that the binding energy causes this

00:09:50 --> 00:09:52 mass deficit. And it's that mass deficit that

00:09:52 --> 00:09:55 has been converted to energy that it's

00:09:55 --> 00:09:58 in liberated in fusion. So I

00:09:58 --> 00:10:00 appreciate it is not the most satisfying

00:10:00 --> 00:10:03 answer, but that's our

00:10:03 --> 00:10:06 understanding of the why behind all of this.

00:10:06 --> 00:10:08 And the proof is in the pudding. Fusion

00:10:08 --> 00:10:11 happens. It produces energy at the

00:10:11 --> 00:10:13 right level that we calculate that all, all

00:10:13 --> 00:10:15 of our models suggest it should do. So it

00:10:15 --> 00:10:17 seems that this is a very accurate

00:10:18 --> 00:10:21 representation of how the world works, even

00:10:21 --> 00:10:23 if it doesn't immediately feel

00:10:23 --> 00:10:26 satisfying and commonsensical. And uh,

00:10:26 --> 00:10:28 part of that is that common sense we've

00:10:28 --> 00:10:31 developed based on the experience of the

00:10:31 --> 00:10:33 world around us at our scales, at macroscopic

00:10:33 --> 00:10:34 scales. And the further you go from the

00:10:34 --> 00:10:37 conditions in this room, the less accurate

00:10:37 --> 00:10:39 modern sense, common sense is at predicting

00:10:39 --> 00:10:42 the outcomes of things. And that's why

00:10:42 --> 00:10:44 it's hard to work these things out.

00:10:45 --> 00:10:48 Andrew Dunkley: Yeah, it's like, I mean, listening

00:10:48 --> 00:10:50 to your explanation would be the same as me

00:10:50 --> 00:10:53 trying to explain to a kangaroo how to use

00:10:53 --> 00:10:55 a pedestrian crossing. So, you know,

00:10:55 --> 00:10:58 it's. I can understand Ken's

00:10:58 --> 00:11:01 frustration. Um, but

00:11:02 --> 00:11:05 if I understand your explanation thoroughly,

00:11:05 --> 00:11:08 um, Ken, what, what Jonty was saying

00:11:08 --> 00:11:09 was that shift happens.

00:11:11 --> 00:11:14 That's basically it, I think. But thanks for

00:11:14 --> 00:11:17 the question. Great to hear from you. This is

00:11:17 --> 00:11:18 a Q and A edition of Space Nuts with Andrew

00:11:18 --> 00:11:20 Dunkley and Professor Johnty Horner.

00:11:25 --> 00:11:26 Jonti Horner: Space Nuts.

00:11:26 --> 00:11:29 Andrew Dunkley: Okay, Jonty, our next question says,

00:11:29 --> 00:11:31 uh, Fred Watson was talking about caves on

00:11:31 --> 00:11:34 Mars and that got me thinking. The caves on

00:11:34 --> 00:11:36 Earth are, uh, primarily made of limestone,

00:11:36 --> 00:11:39 which has high concentrations of CO2

00:11:39 --> 00:11:42 that was locked in by millions of years of

00:11:42 --> 00:11:44 sea creatures popping into the sea, creating

00:11:44 --> 00:11:46 a layer on the seabed that could be,

00:11:47 --> 00:11:50 uh, um, seabed. Could it be the same effect

00:11:50 --> 00:11:53 on Mars? No. Punctuation caught me out

00:11:53 --> 00:11:55 there. If so, I need to ask, ah,

00:11:56 --> 00:11:58 the question. Um, you get,

00:11:58 --> 00:12:01 uh. If

00:12:01 --> 00:12:04 so, I don't need to ask the next question.

00:12:04 --> 00:12:06 Um, you get what I mean. But the next

00:12:06 --> 00:12:09 question is, if caves are deep enough,

00:12:09 --> 00:12:12 could it be possible that the atmosphere at

00:12:12 --> 00:12:15 the base of these caves could be dense enough

00:12:15 --> 00:12:17 to create a stable atmosphere with higher

00:12:17 --> 00:12:19 concentrations of oxygen for life? And could

00:12:19 --> 00:12:22 that life be looking at Earth with

00:12:22 --> 00:12:23 envious eyes?

00:12:23 --> 00:12:24 Jonti Horner: Yeah, very funny.

00:12:24 --> 00:12:27 Andrew Dunkley: Hope not. Uh, Mark? Uh, thank you, Mark.

00:12:27 --> 00:12:30 So, um, caves on Earth, we. Yeah, not all of

00:12:30 --> 00:12:31 them, but uh, quite a lot of them are

00:12:31 --> 00:12:34 limestone. Um, could it be the

00:12:34 --> 00:12:37 same way as caves were created

00:12:37 --> 00:12:40 on Mars? I think that's the initial question.

00:12:40 --> 00:12:43 Jonti Horner: So I'd stress here, I'm Not a geophysicist,

00:12:43 --> 00:12:45 but the limestone we get on Earth is stuff

00:12:45 --> 00:12:47 that is now above sea level that was once

00:12:47 --> 00:12:49 below sea level. You had all these calcium

00:12:49 --> 00:12:52 shelled creatures die and fall to the bottom

00:12:52 --> 00:12:54 of the, uh, ocean and then get compacted over

00:12:54 --> 00:12:57 millions of years to form this rock. And then

00:12:57 --> 00:12:59 plate tectonics lifted the rock above the

00:12:59 --> 00:13:01 surface of the ocean. I guess on Mars you'd

00:13:01 --> 00:13:03 probably argue the oceans went away. There's

00:13:03 --> 00:13:05 not plate tectonics to lift things up, but

00:13:05 --> 00:13:07 the places that were ocean now no longer

00:13:08 --> 00:13:10 are. Ah, this is

00:13:11 --> 00:13:13 predisposed on the idea that you develop

00:13:13 --> 00:13:16 things with enough calcium

00:13:16 --> 00:13:18 to be able to make shells and stuff like

00:13:18 --> 00:13:21 that. Um, I believe, and I stand to

00:13:21 --> 00:13:23 be corrected on this, that the things that

00:13:23 --> 00:13:25 make calcium are typically

00:13:25 --> 00:13:28 oxygen breathers, not carbon dioxide

00:13:28 --> 00:13:30 breathers. But I may be wrong on that. Um,

00:13:30 --> 00:13:32 they die, they precipitate stuff out. Now,

00:13:32 --> 00:13:34 the first point is whether they could be

00:13:34 --> 00:13:36 limestone caves on Mars. Ah, now that would

00:13:36 --> 00:13:39 be predisposed on the appropriate

00:13:39 --> 00:13:42 evolution of life to get to the point where

00:13:42 --> 00:13:43 you have things that could leave fossils,

00:13:43 --> 00:13:45 that could leave shells and stuff. And we

00:13:45 --> 00:13:48 haven't yet found any fossils of such life on

00:13:48 --> 00:13:51 Mars. And without such life, you couldn't get

00:13:51 --> 00:13:53 limestone. I think think will be an open

00:13:53 --> 00:13:54 question. I suspect if we got Earth, uh,

00:13:54 --> 00:13:56 scientists and stuff like that in on the

00:13:56 --> 00:13:59 show, they'd have good reasons why limestone

00:13:59 --> 00:14:01 will be unlikely to be common on Mars.

00:14:01 --> 00:14:04 Because, yes, you did have oceans and lakes,

00:14:04 --> 00:14:07 but was there, ah, enough time for

00:14:07 --> 00:14:09 enough deposits to be made of shelled

00:14:09 --> 00:14:12 creatures which we don't even know evolved?

00:14:12 --> 00:14:14 So there's a lot of complexity there. It's

00:14:14 --> 00:14:16 obviously something, I don't know for

00:14:16 --> 00:14:19 definite whether you could have limestone

00:14:19 --> 00:14:22 on Mars. Um, I haven't heard of it being

00:14:22 --> 00:14:25 detected on Mars, but absence of evidence

00:14:25 --> 00:14:26 is not evidence of absence. But I don't

00:14:26 --> 00:14:28 believe it is common, otherwise we'd be

00:14:28 --> 00:14:30 fairly well aware of it. But there are other

00:14:30 --> 00:14:32 ways you can get caves on Earth. And I mean,

00:14:32 --> 00:14:35 we've got lava tubes and lava caves up

00:14:35 --> 00:14:37 in North Queensland in Uladulla. We've got

00:14:37 --> 00:14:39 similar things have been found on the Moon

00:14:39 --> 00:14:42 and Mars. There are skylights and lava tubes

00:14:42 --> 00:14:44 on Mars that people have even suggested could

00:14:44 --> 00:14:47 be suitable places for humans to

00:14:47 --> 00:14:49 go and live. Because if you're underground,

00:14:49 --> 00:14:51 you're shielded from radiation. And of

00:14:51 --> 00:14:53 course, if you're in a cave, you can seal the

00:14:53 --> 00:14:56 entrance and fill it with air, which would be

00:14:56 --> 00:14:58 good. Now that kind of links to the second

00:14:58 --> 00:15:01 part of the question here from Mark, which is

00:15:01 --> 00:15:02 if you have caves deep enough, could you have

00:15:02 --> 00:15:04 enough atmosphere in those caves to have

00:15:05 --> 00:15:08 atmospheric pressure? I think that's

00:15:08 --> 00:15:10 unlikely here because those cave

00:15:10 --> 00:15:13 systems would probably be connected to the

00:15:13 --> 00:15:16 surface and air would diffuse out of

00:15:16 --> 00:15:18 them. So you equilibriate and you don't

00:15:18 --> 00:15:21 go into the cave in the lava tube on Earth,

00:15:21 --> 00:15:24 and suddenly it's 3 atmospheres. Because if

00:15:24 --> 00:15:25 it was 3 atmospheres, the air would be pushed

00:15:25 --> 00:15:28 out the entrance. So I don't

00:15:28 --> 00:15:30 think you get to atmospheric pressure in

00:15:30 --> 00:15:33 these caves unless they were very, very deep

00:15:33 --> 00:15:35 and were sealed and the air was sealed in

00:15:35 --> 00:15:37 from when the atmospheric pressure was higher

00:15:37 --> 00:15:39 and it hadn't escaped. But with the porosity

00:15:39 --> 00:15:40 of the rocks, I think that would be very

00:15:40 --> 00:15:43 unlikely. The next thing is about there being

00:15:43 --> 00:15:46 oxygen in those caves. And I think of all of

00:15:46 --> 00:15:48 these things, that is the least likely

00:15:48 --> 00:15:50 because Mars

00:15:51 --> 00:15:54 doesn't have much, if any free oxygen

00:15:54 --> 00:15:56 in the atmosphere, because oxygen reacts with

00:15:56 --> 00:15:59 everything. And on Mars, there are bits of

00:15:59 --> 00:16:00 methane being produced. We're not quite sure

00:16:00 --> 00:16:03 what's going on there, but the oxygen, free

00:16:03 --> 00:16:06 oxygen from Mars has been very

00:16:06 --> 00:16:08 effectively absorbed into the surface through

00:16:08 --> 00:16:11 chemistry. Um, big part of why Mars looks

00:16:11 --> 00:16:12 red, of course, is that you can effectively

00:16:12 --> 00:16:15 say the surface is rusted iron

00:16:15 --> 00:16:18 oxide. The oxygen in the air has reacted with

00:16:18 --> 00:16:19 the iron in the surface and

00:16:19 --> 00:16:22 Andrew Dunkley: been locked up like a lot of Australia.

00:16:22 --> 00:16:25 Jonti Horner: Yes. Um, now you can produce some oxygen in

00:16:25 --> 00:16:28 Mars's atmosphere. If you get water into the

00:16:28 --> 00:16:30 atmosphere, and there is a very small amount,

00:16:30 --> 00:16:32 traces of ox of water in Mars's atmosphere,

00:16:32 --> 00:16:35 we do get water clouds there. Without an

00:16:35 --> 00:16:37 ozone layer, some of that water, particularly

00:16:37 --> 00:16:38 the water that gets highest in the

00:16:38 --> 00:16:41 atmosphere, will get dissociated. It will get

00:16:41 --> 00:16:43 broken into hydrogen and oxygen by

00:16:43 --> 00:16:46 ultraviolet radiation and the hydrogen will

00:16:46 --> 00:16:48 then escape because hydrogen atoms travel so

00:16:48 --> 00:16:50 quickly that Mars gravity can't hold them,

00:16:50 --> 00:16:52 which means the hydrogen goes away and the

00:16:52 --> 00:16:55 oxygen is left behind. So you will be

00:16:55 --> 00:16:57 producing small trace amounts of oxygen in

00:16:57 --> 00:16:59 Mars's atmosphere all the time. But then the

00:16:59 --> 00:17:02 oxygen would then be used up in chemistry and

00:17:02 --> 00:17:04 removed. So in order to have large amounts of

00:17:04 --> 00:17:06 oxygen in one of these caves, you'd need a

00:17:06 --> 00:17:09 source of oxygen, and you'd need that source

00:17:09 --> 00:17:11 to provide enough oxygen that the oxygen can

00:17:11 --> 00:17:13 overcome everything that's trying to remove

00:17:13 --> 00:17:16 it. Now, on Earth, it took a

00:17:16 --> 00:17:18 huge fraction of Earth's life before you got

00:17:18 --> 00:17:20 the great oxidation event for life to

00:17:20 --> 00:17:21 actually get to the point where it could

00:17:21 --> 00:17:23 produce more oxygen than the Earth, uh,

00:17:23 --> 00:17:26 system could absorb. So to have abundant

00:17:26 --> 00:17:28 oxygen on Mars, uh, strikes me as Very

00:17:28 --> 00:17:31 unlikely. Maybe possible that in the future

00:17:31 --> 00:17:32 that will change though, because if we went

00:17:32 --> 00:17:35 to Mars, then one of the ways people are

00:17:35 --> 00:17:37 thinking the first human habitats will be

00:17:37 --> 00:17:39 built will be to go to the caves in the lava

00:17:39 --> 00:17:42 tunnels and live there. And then you can make

00:17:42 --> 00:17:44 a sealed environment that you can then pump

00:17:44 --> 00:17:46 with an artificial atmosphere. So it could be

00:17:46 --> 00:17:49 that if you ask that question in 20 years

00:17:49 --> 00:17:52 time, Mark, the answer would be yes. There

00:17:52 --> 00:17:53 are caves with high enough atmospheric

00:17:53 --> 00:17:56 concentrations for life. We've put them

00:17:56 --> 00:17:58 there. Would they be looking back at Earth

00:17:58 --> 00:18:00 with anxious eyes, with envious eyes? I guess

00:18:00 --> 00:18:02 it depends on the person who's emigrated

00:18:02 --> 00:18:05 there. There's these fabulous ideas of what

00:18:05 --> 00:18:07 humanity will look like when we're a multi

00:18:07 --> 00:18:09 planet species. But the thing that stuck with

00:18:09 --> 00:18:11 me more than anything else was this amazing

00:18:11 --> 00:18:14 Talk from a doctor in 2012, 2013,

00:18:14 --> 00:18:16 2014 at one of our space research conferences

00:18:17 --> 00:18:19 who basically talked about the difficulty

00:18:19 --> 00:18:22 humans have reproducing when you go even

00:18:22 --> 00:18:24 very slightly away from standard temperature

00:18:24 --> 00:18:26 pressure at sea level. Talked about the

00:18:26 --> 00:18:29 challenges at invaders had into South

00:18:29 --> 00:18:30 America when they reached the high Andes.

00:18:30 --> 00:18:32 They couldn't colonise there because they

00:18:32 --> 00:18:35 weren't able to reproduce. Talking about very

00:18:35 --> 00:18:37 slight changes in conditions being enough to

00:18:37 --> 00:18:39 render our ability to have children

00:18:40 --> 00:18:42 null and void. On Mars you've got one third

00:18:42 --> 00:18:45 gravity. Unless you get dystopian science

00:18:45 --> 00:18:48 fiction future where women enter

00:18:48 --> 00:18:50 centrifuges for nine months in order to carry

00:18:50 --> 00:18:52 a child to term, in order to simulate one

00:18:52 --> 00:18:55 ghost. The perspective is at least in the

00:18:55 --> 00:18:58 relatively near future, humanity on the

00:18:58 --> 00:19:00 moon, humanity on Mars will be

00:19:01 --> 00:19:03 not self sustaining. We won't be able to have

00:19:03 --> 00:19:05 children there. And so it may well be that

00:19:05 --> 00:19:08 Mars becomes a interplanetary retirement

00:19:08 --> 00:19:11 home. People sow their wild oats, live their

00:19:11 --> 00:19:13 lives and then go to Mars later in life for

00:19:13 --> 00:19:15 the adventure. And then would they look back

00:19:15 --> 00:19:17 with envy? Well, they'd probably look back

00:19:17 --> 00:19:18 with a little bit of longing, but also they'd

00:19:18 --> 00:19:20 have the excitement of where they are are.

00:19:20 --> 00:19:22 So it could be that in 20 years time, 30

00:19:22 --> 00:19:25 years time, there will be life in the caves

00:19:26 --> 00:19:28 with artificially enhanced oxygen levels.

00:19:29 --> 00:19:31 Looking back at Earth, watching the news and

00:19:31 --> 00:19:33 all the rest of it, but I don't think at the

00:19:33 --> 00:19:34 minute that that's the case.

00:19:35 --> 00:19:38 Andrew Dunkley: Okay, fair enough. Uh, and uh, just one

00:19:38 --> 00:19:40 more point, Mark. I just did a quick search

00:19:40 --> 00:19:42 about could there be limestone on Mars? And

00:19:42 --> 00:19:44 according to an article in Science

00:19:44 --> 00:19:46 AstroDailyPod which dates back nearly 20

00:19:46 --> 00:19:49 years now, uh, yes, limestone, specifically

00:19:49 --> 00:19:51 carbonate minerals likely exist on Mars, but

00:19:53 --> 00:19:55 probably not in massive thick sedimentary

00:19:55 --> 00:19:58 beds found On Earth, while early Mars was

00:19:58 --> 00:20:00 warmer and wetter, supporting the potential

00:20:00 --> 00:20:03 for carbonate formation, the planet lacked

00:20:03 --> 00:20:05 the extensive oceans and tectonic plate

00:20:05 --> 00:20:07 activity required to build large limestone

00:20:07 --> 00:20:10 deposits. So there you are. They

00:20:10 --> 00:20:13 think there possibly is limestone

00:20:13 --> 00:20:16 on Mars, but not uh, enough to do

00:20:16 --> 00:20:18 what we've seen on Earth. Uh,

00:20:18 --> 00:20:21 but great question and uh, certainly food for

00:20:21 --> 00:20:24 thought, uh, and appreciate it. Mark, thanks

00:20:24 --> 00:20:25 for sending it in.

00:20:25 --> 00:20:27 This is Space Nuts. Andrew Dunkley here with

00:20:27 --> 00:20:28 Professor Jonty Horner.

00:20:33 --> 00:20:34 Jonti Horner: M. Space Nuts.

00:20:34 --> 00:20:37 Andrew Dunkley: And you're listening to a Q and A edition.

00:20:37 --> 00:20:39 We've got one more question to tackle. Hello,

00:20:39 --> 00:20:42 this is Casey from Colorado, she's one of our

00:20:42 --> 00:20:45 regular contributors. I have some questions

00:20:45 --> 00:20:47 about stars. Why do the activity levels of

00:20:47 --> 00:20:50 stars change? What causes solar cycles?

00:20:50 --> 00:20:53 Does every type of star go through solar

00:20:53 --> 00:20:56 cycling? Love the show, Hope you're both

00:20:56 --> 00:20:58 well. Uh, thanks Casey from Colorado.

00:20:59 --> 00:21:01 Um, it's a good question because we don't

00:21:01 --> 00:21:03 really talk about this sort of thing much,

00:21:03 --> 00:21:06 but uh, we're just about to go out of

00:21:06 --> 00:21:09 uh, the peak of solar activity

00:21:09 --> 00:21:12 in our own Solar System, the 11 year cycle

00:21:12 --> 00:21:15 that they talk about. Uh, so that's probably

00:21:15 --> 00:21:17 where we should start. We know the sun goes

00:21:17 --> 00:21:20 through an 11 year cycle and um,

00:21:22 --> 00:21:24 and we witness different things during those

00:21:24 --> 00:21:27 11 years because it's constantly changing.

00:21:27 --> 00:21:29 Jonti Horner: Yeah, it's worth stressing Shreya, that

00:21:29 --> 00:21:32 uh, effectively all stars are uh,

00:21:32 --> 00:21:35 inherently variable to some degree. And

00:21:35 --> 00:21:37 our sun is actually incredibly low

00:21:37 --> 00:21:39 variability compared to many stars.

00:21:40 --> 00:21:43 The solar cycle we observe is

00:21:43 --> 00:21:45 arguably a 22ish year cycle with

00:21:45 --> 00:21:48 two peaks and two minima. And the subtlety

00:21:48 --> 00:21:50 there is we get solar maximum when there are

00:21:50 --> 00:21:52 lots of sunspots, lots of activity, more

00:21:52 --> 00:21:55 aurora and solar minimum when we've got fewer

00:21:55 --> 00:21:57 sunspots, less activity, fewer aurora.

00:21:58 --> 00:22:00 And we get those on and about an 11 year

00:22:00 --> 00:22:02 cycle from one peak to the next, sometimes a

00:22:02 --> 00:22:05 bit shorter, sometimes a bit longer. But the

00:22:05 --> 00:22:08 origin of the solar cycles with the

00:22:08 --> 00:22:10 sun is the Sun's magnetic field. The sun

00:22:11 --> 00:22:13 has a magnetic field that runs from the North

00:22:13 --> 00:22:15 Pole to the South Pole. And it

00:22:15 --> 00:22:18 rotates in such a way that the rotation

00:22:18 --> 00:22:20 period at the equator and the rotation period

00:22:20 --> 00:22:22 at the poles are different rotates as a fluid

00:22:22 --> 00:22:25 body. So the time it takes the Sun's equator

00:22:25 --> 00:22:27 to rotate is a couple of days quicker than

00:22:27 --> 00:22:30 the poles. The magnetic field lines running

00:22:30 --> 00:22:32 from the North Pole to the South Pole get

00:22:32 --> 00:22:34 hooked up in the material and gradually get

00:22:34 --> 00:22:36 wound up a bit like an elastic band. And so

00:22:36 --> 00:22:38 the Sun's magnetic field gets more and more

00:22:38 --> 00:22:41 complicated through the 11 years, starts to

00:22:41 --> 00:22:42 get kinks and the kinks break through the

00:22:42 --> 00:22:44 surface. So you get locations where the

00:22:44 --> 00:22:46 magnetic field comes out of the surface,

00:22:46 --> 00:22:48 loops up and goes back down. And in the

00:22:48 --> 00:22:50 places where it's nearly vertical, it cools

00:22:50 --> 00:22:52 the surface of the sun because it suppresses

00:22:52 --> 00:22:53 convection of new energy from, from

00:22:53 --> 00:22:55 underneath, leading to cooler spots which

00:22:55 --> 00:22:58 look darker and therefore are sunspots. And

00:22:58 --> 00:22:59 gradually the sun gets more and more wound

00:22:59 --> 00:23:02 up. Sunspot activity begins at high latitudes

00:23:02 --> 00:23:04 and works its way down towards the equator

00:23:04 --> 00:23:07 and eventually around solar maximum, you get

00:23:07 --> 00:23:09 the field line starting to snap and break and

00:23:09 --> 00:23:12 you get a polar reversal happen. The north

00:23:12 --> 00:23:14 pole becomes a south pole and the south pole

00:23:14 --> 00:23:16 becomes a north pole and then it all begins

00:23:16 --> 00:23:18 again. So the reason we talk about a 22 year

00:23:18 --> 00:23:21 cycle is you get solar maximum

00:23:21 --> 00:23:23 with north pole to the north, well, north

00:23:23 --> 00:23:25 pole to the top, and then a minimum, then

00:23:25 --> 00:23:27 solar maximum with the south pole to the top,

00:23:27 --> 00:23:29 then a minimum, then you're back to where you

00:23:29 --> 00:23:32 started from. Roughly. Those

00:23:32 --> 00:23:35 cycles are driven by the magnetic activity of

00:23:35 --> 00:23:37 the sun and they vary the brightness of our

00:23:37 --> 00:23:39 star, um, by a vanishingly small amount. It's

00:23:39 --> 00:23:42 an incredibly stable star. I think you're

00:23:42 --> 00:23:44 talking about variability on the level, about

00:23:44 --> 00:23:47 one part in 2, 10, something

00:23:47 --> 00:23:49 like that. Now that is such a low level of

00:23:49 --> 00:23:51 variability that if we were observing an

00:23:51 --> 00:23:54 other star, we probably wouldn't be able to

00:23:54 --> 00:23:56 pick up the variability in the total

00:23:56 --> 00:23:58 brightness, but we would be able to pick up

00:23:58 --> 00:24:00 the magnetic activity. And this is magnetic

00:24:00 --> 00:24:03 activity. And star spots are uh, one of the

00:24:03 --> 00:24:05 challenges for people trying to find

00:24:05 --> 00:24:08 exoplanets because a star spot can mimic as

00:24:08 --> 00:24:10 an exoplanet and stellar activity like the

00:24:10 --> 00:24:13 Sun's magnetic cycle and the star. So SAR

00:24:13 --> 00:24:16 spots that go with it can actually be mimic

00:24:16 --> 00:24:17 a radial velocity planet. So there's a lot of

00:24:17 --> 00:24:20 work done in when we think we've got a signal

00:24:20 --> 00:24:22 confirming that it is actually a planet and

00:24:22 --> 00:24:24 not a star spot. So you've got that kind of

00:24:24 --> 00:24:25 stellar activity.

00:24:25 --> 00:24:28 Now most stars are significantly, uh, more

00:24:28 --> 00:24:29 variable than the sun. And there's a lot of

00:24:29 --> 00:24:31 other ways stars can vary. We think that

00:24:32 --> 00:24:35 most sun like stars will have sunspot cycles

00:24:35 --> 00:24:36 like the sun, and it's due to the structure

00:24:36 --> 00:24:39 of the convective and the radiative zones and

00:24:39 --> 00:24:41 all the rest of it. The internal structure of

00:24:41 --> 00:24:42 the sun, a bit like the Earth, has a crust, a

00:24:42 --> 00:24:45 mantle and a car. The magnetic field in the

00:24:45 --> 00:24:47 top layer of the sun can get tangled up.

00:24:49 --> 00:24:50 Stars of different masses have a bit of a

00:24:50 --> 00:24:52 different structure, but there's A lot of

00:24:52 --> 00:24:55 other ways that stars can be variable. And so

00:24:55 --> 00:24:57 we have a very wide variety of different

00:24:57 --> 00:24:59 types of variable stars. There are flare

00:24:59 --> 00:25:01 stars like Proxima Centauri, which have

00:25:02 --> 00:25:04 stellar activity that can occasionally be a

00:25:04 --> 00:25:06 super flare that can cause the star's

00:25:06 --> 00:25:07 brightness to change by almost a factor of

00:25:07 --> 00:25:10 100. And I normally talk about Proxima

00:25:10 --> 00:25:12 Centauri being 100 times too fancy with the

00:25:12 --> 00:25:14 naked eye, but in one mega flare it had a few

00:25:14 --> 00:25:16 years ago, it almost reached the edge of

00:25:16 --> 00:25:18 naked eye visibility. That flare was that

00:25:18 --> 00:25:21 intense. You've then got a, ah, large number

00:25:21 --> 00:25:23 of stars that vary in brightness. Bixa

00:25:23 --> 00:25:26 pulsate Bixa size changes fundamentally

00:25:26 --> 00:25:29 and usually these are stars coming towards

00:25:29 --> 00:25:30 the end of the life entering a bit of

00:25:30 --> 00:25:33 instability for various reasons. Some of them

00:25:33 --> 00:25:35 are only just moving off the main sequence or

00:25:35 --> 00:25:38 are very young. Others are super giant stars

00:25:38 --> 00:25:41 with different kinds of variability. But

00:25:41 --> 00:25:43 that variability causes their

00:25:43 --> 00:25:46 diameter to change, causes them to pulsate.

00:25:46 --> 00:25:47 And that's because they're just slightly out

00:25:47 --> 00:25:49 of equilibrium. When they're at their

00:25:49 --> 00:25:52 smallest they get hotter, they're putting out

00:25:52 --> 00:25:54 more energy because they're a bit hotter.

00:25:55 --> 00:25:57 Um, the surface layers therefore are pushed

00:25:57 --> 00:26:00 outwards with more force than gravity can

00:26:00 --> 00:26:02 push them in and they start to expand, they

00:26:02 --> 00:26:04 go through the equilibrium point but because

00:26:04 --> 00:26:06 they're still expanding they keep going. As

00:26:06 --> 00:26:08 the stars outer layers get bigger and bigger,

00:26:09 --> 00:26:12 the star cools. Because when you

00:26:12 --> 00:26:14 take a gas and you increase its volume,

00:26:14 --> 00:26:16 you lower the pressure and you lower the

00:26:16 --> 00:26:18 temperature so that material cools

00:26:19 --> 00:26:21 and eventually is giving out less energy

00:26:22 --> 00:26:25 than gravity pulling in would cause and it

00:26:25 --> 00:26:27 starts to collapse again. So instead of like

00:26:27 --> 00:26:29 the sun staying at that very fixed radius

00:26:29 --> 00:26:31 because gravity and radiation are balanced

00:26:31 --> 00:26:33 perfectly, you can get this oscillating

00:26:33 --> 00:26:34 behaviour where you overshoot in both

00:26:34 --> 00:26:37 directions. And um, sometimes that's fairly

00:26:37 --> 00:26:39 small, sometimes that's fairly large. And it

00:26:39 --> 00:26:41 happens at different phases of stars lives in

00:26:41 --> 00:26:43 different ways. One of the most famous types

00:26:43 --> 00:26:45 of variable stars are known as the Cepheid

00:26:45 --> 00:26:48 variable stars. And um, these are somewhat

00:26:48 --> 00:26:50 evolved stars coming towards the end of their

00:26:50 --> 00:26:52 life where the pulsation period

00:26:53 --> 00:26:56 is directly linked to how luminous a star is.

00:26:58 --> 00:27:00 So two similar stars, but one's brighter than

00:27:00 --> 00:27:03 the other intrinsically, put them at the same

00:27:03 --> 00:27:04 distance, one's more luminous, looks

00:27:04 --> 00:27:06 brighter, they will pulsate with different

00:27:06 --> 00:27:08 periods. And if you can measure the period,

00:27:08 --> 00:27:11 you can measure how luminous that star is.

00:27:11 --> 00:27:13 And that makes Cepheid variables an excellent

00:27:13 --> 00:27:16 step on our distance ladder. Because you see

00:27:16 --> 00:27:17 a star that's a certain Brightness, you don't

00:27:17 --> 00:27:19 really know how far away it is. But if you

00:27:19 --> 00:27:21 can measure the period of the Cepheid

00:27:21 --> 00:27:23 variable pulsating, that tells you

00:27:23 --> 00:27:26 intrinsically how luminous that star is,

00:27:26 --> 00:27:28 which means we can work out its distance. So

00:27:28 --> 00:27:29 they're really useful.

00:27:30 --> 00:27:32 Some stars are astonishingly variable.

00:27:33 --> 00:27:35 Um, among the stars with the biggest

00:27:35 --> 00:27:37 variation in brightness from brightest to

00:27:37 --> 00:27:40 faintest, um, are known as the Myra stars.

00:27:40 --> 00:27:43 Ah, Myra, the archetypal one is known as

00:27:43 --> 00:27:45 Myra, the wonderful Myra at its brightest

00:27:45 --> 00:27:48 is easily visible with a naked eye at

00:27:48 --> 00:27:50 its fantasy, you need a telescope to see it.

00:27:50 --> 00:27:52 And a few of these stars have

00:27:53 --> 00:27:54 amplitudes, the difference in brightness

00:27:54 --> 00:27:57 between the brightest and faintest that are

00:27:57 --> 00:27:58 such that they vary in brightness by more

00:27:58 --> 00:28:01 than a factor of 10. Um, a couple of

00:28:01 --> 00:28:04 examples here, Chi Cygni, which at its

00:28:04 --> 00:28:06 brightness is a magnitude 3.3 star, so

00:28:06 --> 00:28:08 comfortable with the naked eye, but not that

00:28:08 --> 00:28:10 bright at, ah, its Faintest is magnitude

00:28:10 --> 00:28:13 14.2. Um, that is

00:28:13 --> 00:28:16 a factor of about 25 in brightness

00:28:16 --> 00:28:18 between brightest and faintests. That is

00:28:19 --> 00:28:21 so long a period that that was discovered,

00:28:21 --> 00:28:24 that variability back in 1686.

00:28:25 --> 00:28:27 You've got a wide variety of mirror type

00:28:27 --> 00:28:29 stars dominating the stars with the biggest

00:28:29 --> 00:28:31 variability. But there are other type ones in

00:28:31 --> 00:28:34 there. Arcarona Borealis is a famous one in

00:28:34 --> 00:28:36 the bowl of the northern crown, normally only

00:28:36 --> 00:28:39 barely visible with the naked eye. So carbon

00:28:39 --> 00:28:42 star, where the mirror stars

00:28:42 --> 00:28:44 have a periodic variation, they're pulsating

00:28:44 --> 00:28:47 in a broadly periodic way with periods of a

00:28:47 --> 00:28:49 year or more. Acherona

00:28:49 --> 00:28:51 Borealis is different. It shines along,

00:28:51 --> 00:28:52 shines along, shines along and then suddenly

00:28:52 --> 00:28:54 it's like somebody drops a curtain in front

00:28:54 --> 00:28:57 of it and its brightness plunges and then it

00:28:57 --> 00:28:59 gradually brightens up again. And that is not

00:28:59 --> 00:29:01 exactly periodic. It's known as a carbon

00:29:01 --> 00:29:03 star. And what's happening is that, ah,

00:29:03 --> 00:29:05 occasionally it's got a huge amount of carbon

00:29:05 --> 00:29:08 in its atmosphere. Occasionally the carbon

00:29:08 --> 00:29:10 condenses into soot, blocking the light from

00:29:10 --> 00:29:12 underneath. That cools the outer layers,

00:29:12 --> 00:29:14 which gets this runaway condensation of

00:29:14 --> 00:29:16 carbon carbon into soot. That traps the

00:29:16 --> 00:29:19 radiation from inside, so the heat builds up

00:29:19 --> 00:29:20 inside until eventually the carbon gets

00:29:20 --> 00:29:22 turned back into a gas again. The clouds

00:29:22 --> 00:29:24 clear and the star brightens again.

00:29:24 --> 00:29:26 Andrew Dunkley: So that's, I was, I was just going to

00:29:26 --> 00:29:28 stupidly suggest that it was soot.

00:29:28 --> 00:29:31 Jonti Horner: Yeah, it is, it's a carbon star. And a Corona

00:29:31 --> 00:29:34 Borealis is the archetypal, most

00:29:34 --> 00:29:36 famous one. It's described as a low mass

00:29:36 --> 00:29:38 yellow supergiant. So again, it's a star

00:29:38 --> 00:29:39 coming towards the end of its life,

00:29:40 --> 00:29:43 um, every so often can be after just

00:29:43 --> 00:29:45 a few months, or it can be a few years. It

00:29:45 --> 00:29:48 can dim by as much as a factor of 10

00:29:48 --> 00:29:51 because it kind of suits up, clouds up.

00:29:51 --> 00:29:53 And if you look at the light curve of that.

00:29:53 --> 00:29:54 If you're bored, have a look at the light

00:29:54 --> 00:29:57 curve on Wikipedia, because it's really

00:29:57 --> 00:29:59 head scratching. It shows you how random this

00:29:59 --> 00:30:01 is and how hard it must have been for people

00:30:01 --> 00:30:04 to understand. Um, there was an incredible

00:30:04 --> 00:30:06 deep minimum that happened in the, the

00:30:06 --> 00:30:09 mid-2010s, I think it was, where it

00:30:09 --> 00:30:11 dimmed and then it stayed dim for ages.

00:30:12 --> 00:30:13 Normally it's bright and then it dims for a

00:30:13 --> 00:30:15 bit and then it brightens up fairly quickly.

00:30:16 --> 00:30:19 But fundamentally, there's a huge variety of

00:30:19 --> 00:30:21 ways in which stars can vary intrinsically

00:30:21 --> 00:30:24 themselves. Their brightness can vary. It

00:30:24 --> 00:30:27 is known from discussions with the

00:30:27 --> 00:30:28 traditional owners of the land here in

00:30:28 --> 00:30:30 Australia that the variability of

00:30:30 --> 00:30:32 Beetlejuice, Nal, Deborah, and two bright red

00:30:32 --> 00:30:34 giant, giant red supergiant stars in our

00:30:34 --> 00:30:37 summer sky, Northern Hemisphere winter sky,

00:30:37 --> 00:30:39 are variable. We saw that with the great

00:30:39 --> 00:30:41 dimming of Beetlejuice about a decade ago.

00:30:41 --> 00:30:44 Now, that kind of variability has been known

00:30:44 --> 00:30:46 for hundreds, if not thousands of years among

00:30:46 --> 00:30:48 traditional owners around the world who look

00:30:48 --> 00:30:50 at the night sky so that stars

00:30:50 --> 00:30:53 varying intrinsically in brightness, the star

00:30:53 --> 00:30:56 itself varying. And, um, it's a wonderful

00:30:56 --> 00:30:57 rabbit hole for people to wander down. It's

00:30:57 --> 00:30:59 another area of astronomy where amateur

00:30:59 --> 00:31:02 astronomy contribute a lot because there's

00:31:02 --> 00:31:04 very active variable star observers who will

00:31:04 --> 00:31:05 go out there and measure the brightness of

00:31:05 --> 00:31:08 stars repeatedly to track when they vary.

00:31:08 --> 00:31:10 We get a lot of that knowledge. You've then

00:31:10 --> 00:31:12 got a second type of stellar variability

00:31:12 --> 00:31:15 which is not intrinsic, but is extrinsic.

00:31:15 --> 00:31:18 What I mean by that is an intrinsically

00:31:18 --> 00:31:20 variable star is a star itself changing. An

00:31:20 --> 00:31:23 extrinsic variation is something else causing

00:31:23 --> 00:31:25 the brightness of the star to change. You

00:31:25 --> 00:31:27 know, put your hand in front of the star. The

00:31:27 --> 00:31:28 stars dissipate because your hand's

00:31:28 --> 00:31:31 absorbing. All the lights disappeared. We

00:31:31 --> 00:31:33 have multiple star systems where we have

00:31:33 --> 00:31:36 eclipsing binaries. Algol is possibly the

00:31:36 --> 00:31:38 most famous of these. The winking demon star,

00:31:38 --> 00:31:40 whose brightness drops by about a factor of

00:31:40 --> 00:31:43 three every couple of days. And that

00:31:43 --> 00:31:46 star is bright enough to be easily visible

00:31:46 --> 00:31:48 with the naked eye. And, um, the

00:31:48 --> 00:31:50 variability in its brightness is sufficiently

00:31:50 --> 00:31:52 large that it's easily noticeable with the

00:31:52 --> 00:31:55 naked eye. So its brightness varies. I

00:31:55 --> 00:31:57 think it's every 70 hours or so. I just want

00:31:57 --> 00:31:59 to cheque it out. Um,

00:32:01 --> 00:32:03 no, it's less often Than that. Algol's

00:32:03 --> 00:32:06 brightness varies every 2.86 days.

00:32:07 --> 00:32:10 So every 2.86 days, the brightness of

00:32:10 --> 00:32:13 the star drops from magnitude 2.1 to 3.4.

00:32:13 --> 00:32:15 That's a brightness change of about a factor

00:32:15 --> 00:32:18 of three times, roughly. And, uh, it dims for

00:32:18 --> 00:32:20 about 10 hours and then brightens up again.

00:32:20 --> 00:32:23 Became known as a winking demon star that has

00:32:23 --> 00:32:26 been known to be variable since prehistory.

00:32:26 --> 00:32:29 In reality, there's allegations

00:32:29 --> 00:32:31 that perhaps an Egyptian calendar that talked

00:32:31 --> 00:32:32 about unlucky days may have been linked to

00:32:32 --> 00:32:35 that. That's questionable. Where it is

00:32:35 --> 00:32:37 really interesting, though, is the

00:32:37 --> 00:32:40 variability of Algol was first explained

00:32:40 --> 00:32:43 by John Goodrich, who is one of

00:32:43 --> 00:32:45 those heroes of astronomy you don't hear

00:32:45 --> 00:32:47 about very often, mainly because he lived a

00:32:47 --> 00:32:50 very short life. He presented findings in May

00:32:50 --> 00:32:53 1783 to suggest that the

00:32:53 --> 00:32:55 variability, the periodic variability of

00:32:55 --> 00:32:58 Algol was caused by a dark body or a dimmer

00:32:58 --> 00:33:01 body passing in front of it every 2.86 days.

00:33:01 --> 00:33:04 He was awarded a medal for this, I believe.

00:33:04 --> 00:33:06 He never got to receive the medal because he

00:33:06 --> 00:33:09 died, as I say, very, very young. Died at the

00:33:09 --> 00:33:12 age of 21. Got the Copley Medal in

00:33:12 --> 00:33:14 1783, I think he was. Uh, passed away

00:33:14 --> 00:33:17 three years after that. So in just 21 years

00:33:17 --> 00:33:20 old, he contributed hugely to our modern

00:33:20 --> 00:33:22 knowledge of variable stars. And, um, you

00:33:22 --> 00:33:24 know, it's very unfortunate that he passed

00:33:24 --> 00:33:26 away at such a young age, but he was able to

00:33:26 --> 00:33:28 explain this variability that had been

00:33:28 --> 00:33:30 clearly known for a very long time. It's

00:33:30 --> 00:33:32 obvious to the naked eye that this star gets

00:33:32 --> 00:33:35 dimmer. It's not a subtle effect, but he

00:33:35 --> 00:33:37 was the one who was able to explain it.

00:33:38 --> 00:33:41 Despite his challenges. He was someone with

00:33:41 --> 00:33:44 certain physical disabilities. He was someone

00:33:44 --> 00:33:46 who had a very difficult life. But he had

00:33:46 --> 00:33:48 such a visionary intellect at the time to

00:33:48 --> 00:33:50 come up with the explanation that this

00:33:50 --> 00:33:52 periodic variability and the style of it and

00:33:52 --> 00:33:55 the frequency and the depth of it being so

00:33:55 --> 00:33:57 repeatable was because this was actually

00:33:57 --> 00:34:00 two objects going around each other. Ties in

00:34:00 --> 00:34:02 with the exoplanet chat we had earlier,

00:34:02 --> 00:34:04 because in a way, this is the indirect

00:34:04 --> 00:34:07 discovery of the binarity of Algol.

00:34:07 --> 00:34:09 You don't know that there are two stars there

00:34:09 --> 00:34:10 because you t two stars separately. They're

00:34:10 --> 00:34:13 circles close together. You can't separate

00:34:13 --> 00:34:16 them with telescopes, modular, hugely massive

00:34:16 --> 00:34:18 interferometers we have today. But you can

00:34:18 --> 00:34:20 infer the two stars there by the

00:34:20 --> 00:34:23 extrinsic variability, the variability of the

00:34:23 --> 00:34:25 light we receive because one blocks light

00:34:25 --> 00:34:28 from the other, fundamentally. So that also

00:34:28 --> 00:34:31 causes cyclical variations in

00:34:31 --> 00:34:33 brightness. But it's not the star in this

00:34:33 --> 00:34:36 case varying. It's a result of the

00:34:36 --> 00:34:38 environment around the star blocking some of

00:34:38 --> 00:34:38 the light.

00:34:39 --> 00:34:42 Andrew Dunkley: Yeah. Okay, so the answer to

00:34:42 --> 00:34:44 Casey's questions are, uh, fundamentally,

00:34:44 --> 00:34:46 yes, um,

00:34:46 --> 00:34:49 stars. Most stars probably have some sort of

00:34:49 --> 00:34:52 variability, some more than others. Uh, the

00:34:52 --> 00:34:55 solar cycles are caused by the buildup

00:34:55 --> 00:34:57 of, um, activity

00:34:59 --> 00:35:01 and um. Yeah. Does every type of

00:35:01 --> 00:35:03 star go through solar cycling?

00:35:03 --> 00:35:05 Jonti Horner: Probably. Does it? It's one of. Like I said,

00:35:05 --> 00:35:06 it's one of the big challenges for us with

00:35:06 --> 00:35:08 our radial velocity work. Looking for planet

00:35:08 --> 00:35:11 trans is filtering out the stellar

00:35:11 --> 00:35:12 cycles and that's particularly a problem for

00:35:12 --> 00:35:14 finding planets like Jupiter on a Jupiter

00:35:14 --> 00:35:17 like orbit. Jupiter goes around the sun every

00:35:17 --> 00:35:19 11.86 years. The solar cycle is about

00:35:19 --> 00:35:22 11 years. It's m hard to disentangle the two.

00:35:23 --> 00:35:25 There's also a fascinating branch of science

00:35:25 --> 00:35:27 and one of my colleagues at Uni SQ is one of

00:35:27 --> 00:35:29 the world's experts in this. Um, Professor

00:35:29 --> 00:35:32 Simon Murphy. This is a discipline called

00:35:32 --> 00:35:35 asteroseismology. We know about the

00:35:35 --> 00:35:37 Earth's interior because of earthquakes. We

00:35:37 --> 00:35:39 can figure out the crust, the core, the

00:35:39 --> 00:35:41 mantle by how different types of seismic

00:35:41 --> 00:35:43 waves pass through the Earth's interior. So

00:35:43 --> 00:35:44 we'll listen to the Earth ringing like a bell

00:35:44 --> 00:35:46 after an earthquake and we can use that

00:35:46 --> 00:35:48 information to sense what the interior

00:35:48 --> 00:35:51 structure is and how it varies. The science

00:35:51 --> 00:35:53 of astroseismology is doing the same kind of

00:35:53 --> 00:35:55 thing with stars, looking at how they wibble

00:35:55 --> 00:35:58 and wobble to map out their interior and

00:35:58 --> 00:35:59 understand it. And that's fundamentally tied

00:35:59 --> 00:36:02 to the variability. Now Simon's got a couple

00:36:02 --> 00:36:04 of PhD students working with him and doing

00:36:04 --> 00:36:06 some fabulous work, um, including

00:36:07 --> 00:36:09 Guy, um, called Tom Love, who's down in New

00:36:09 --> 00:36:10 Zealand, who's an amateur astronomer there,

00:36:10 --> 00:36:13 doing a PhD, just finishing up with us. Where

00:36:13 --> 00:36:15 they're looking with Simon at these

00:36:15 --> 00:36:18 asteroseismology, wibbly wobbliness and also

00:36:18 --> 00:36:20 at the variability of stars. Looking

00:36:20 --> 00:36:23 at a group of stars called the Delta Scuti

00:36:23 --> 00:36:25 stars, which are a particular type of

00:36:25 --> 00:36:28 oscillating, varying vibrating

00:36:28 --> 00:36:31 star, looking at how their interiors behave,

00:36:31 --> 00:36:33 looking at how old they are. So we can better

00:36:33 --> 00:36:36 understanding of the physics going on and a

00:36:36 --> 00:36:38 better understanding of where these stars sit

00:36:38 --> 00:36:41 in the storey of stellar lives. So this kind

00:36:41 --> 00:36:44 of question is one that leads

00:36:44 --> 00:36:46 to whole, uh, rafts of amazing science that's

00:36:46 --> 00:36:47 been done. And I think like everything we

00:36:47 --> 00:36:50 discuss on the show, these questions are all,

00:36:50 --> 00:36:52 all entryways to rabbit holes that can go as

00:36:52 --> 00:36:53 deep as you want to.

00:36:54 --> 00:36:57 Andrew Dunkley: Yes, absolutely. There you are,

00:36:57 --> 00:36:59 Casey. Thanks for the question, really, uh,

00:36:59 --> 00:37:01 really interesting. And um, yeah, it's

00:37:01 --> 00:37:02 fascinating.

00:37:02 --> 00:37:04 Stars. I, I've been spending a lot of time

00:37:04 --> 00:37:07 outside of my telescope recently, uh, and

00:37:07 --> 00:37:09 photographing where I can

00:37:11 --> 00:37:13 some of the, the big stars that are visible.

00:37:13 --> 00:37:16 Um, um, I think I did I get serious

00:37:16 --> 00:37:18 recently. I can't remember. I've got a couple

00:37:18 --> 00:37:20 of good ones. I got Alpha Centauri the other

00:37:20 --> 00:37:23 night, which turned out really well. Uh, but

00:37:23 --> 00:37:24 yeah, thanks for the question, Casey. If you

00:37:24 --> 00:37:27 have questions for us, please send them in

00:37:27 --> 00:37:29 via our website spacenutspodcast.com

00:37:30 --> 00:37:32 and click on the Ask me anything button at

00:37:32 --> 00:37:35 the top. It's labelled ama. You can leave

00:37:35 --> 00:37:37 text or audio messages. If you've got a

00:37:37 --> 00:37:39 device with a microphone, you're all set.

00:37:39 --> 00:37:41 Such as a, I don't know, cell phone, mobile

00:37:41 --> 00:37:44 phone, um, tablet, anything like that.

00:37:44 --> 00:37:47 Or your computer. The got built in mics

00:37:47 --> 00:37:49 these days and just tell us who you are and

00:37:49 --> 00:37:51 where you're from and we'd be happy to try

00:37:51 --> 00:37:53 and solve your riddles. Uh, and have a

00:37:53 --> 00:37:55 look around while you're there. Cheque out

00:37:55 --> 00:37:56 the shop. Cheque out. Uh, Astronomy

00:37:56 --> 00:37:58 AstroDailyPod. Maybe sign up for your daily

00:37:58 --> 00:38:01 feed of astronomical news and

00:38:01 --> 00:38:03 click the supporter tab if you'd like to help

00:38:03 --> 00:38:06 us out. That is totally optional. Uh, and

00:38:06 --> 00:38:08 thank you Jonty for all your help today.

00:38:08 --> 00:38:09 Jonti Horner: Absolute pleasure. It's always good to have a

00:38:09 --> 00:38:10 chat.

00:38:10 --> 00:38:12 Andrew Dunkley: We'll see you soon when we talk, uh,

00:38:12 --> 00:38:15 Astrobiology Part two.

00:38:15 --> 00:38:17 Uh, that is Professor Johnty Horner from the

00:38:17 --> 00:38:20 University of Southern Queensland. And uh,

00:38:20 --> 00:38:23 thanks to Huw in the studio, couldn't uh, be

00:38:23 --> 00:38:26 with us today? Huw? Um, he's an ex radio

00:38:26 --> 00:38:28 guy so he thinks he's a star,

00:38:28 --> 00:38:31 uh, which means his equator rotates more than

00:38:31 --> 00:38:33 his north and south and he's back in hospital

00:38:33 --> 00:38:36 with a twisted bow. And from me, Andrew

00:38:36 --> 00:38:38 Dunkley. Terrible. Thanks for your company.

00:38:38 --> 00:38:40 We'll catch you on the next episode of Space

00:38:40 --> 00:38:41 Network Nuts. Bye bye.

00:38:43 --> 00:38:45 Jonti Horner: You've been listening to the Space Nuts

00:38:45 --> 00:38:48 podcast available at

00:38:48 --> 00:38:50 Apple Podcasts, Spotify,

00:38:50 --> 00:38:53 iHeartRadio or your favourite podcast

00:38:53 --> 00:38:55 player. You can also stream on

00:38:55 --> 00:38:56 demand@bytes.com.

00:38:57 --> 00:38:59 Andrew Dunkley: this has been another quality podcast

00:38:59 --> 00:39:01 production from bytes.com.