Placeholder Image

字幕列表 影片播放

  • The following content is provided under a Creative

  • Commons license.

  • Your support will help MIT OpenCourseWare

  • continue to offer high-quality educational resources for free.

  • To make a donation or to view additional materials

  • from hundreds of MIT courses, visit MIT OpenCourseWare

  • at ocw.mit.edu.

  • PROFESSOR: OK, guys.

  • We're actually slightly ahead of where

  • I thought we'd be at this point, so I'm only

  • going to spend about half of today's lecture

  • finishing up some new material on mass parabolas

  • and stability.

  • I also got a comment in through the anonymous box

  • that said please leave a little bit of time

  • after class for questions.

  • So you can get them out right away, because I'm usually

  • running off to teach some other class at, like,

  • the IDC or some other building.

  • So from now on, I'll try and leave

  • about five minutes at the end of class

  • for questions on today's material,

  • and we'll make up with the second half-hour or 25 minutes

  • of this class being for all the questions on the material

  • so far in the first two weeks.

  • But first I wanted to give a quick review of where

  • we were Wednesday and launch back into mass parabolas, which

  • are ways of looking at nuclear stability in relative numbers

  • and even or oddness of nuclei.

  • So you saw last time we intuitively

  • derived the semi-empirical mass formula

  • as a sum of volume, surface, coulomb, asymmetry,

  • and pairing, or whether things are even-even or odd-even terms

  • with the coefficients in MeV gleaned from data,

  • and the forms of the-- and the exponents right here gleaned

  • from intuition.

  • Here we assume that the nucleus can

  • be thought of like a big drop of liquid with some charged

  • particles in it.

  • And so the droplet should become more stable

  • the more nuclei there are-- or the more nucleons there are.

  • But then you have some more outside

  • on the surface that aren't bonded to the others.

  • All of the protons are repelling each other over linear length

  • scales, because the radius of this liquid drop

  • would scale like A to the 1/3.

  • There's an asymmetry term, which means if the neutrons

  • and protons are out of balance, there's

  • going to be some less binding energy.

  • And then there's this extra part that

  • tells you whether the nuclei are even-even or odd-odd.

  • And this works pretty well.

  • If you remember, we looked at theory versus experiment

  • where all the red points here are theoretical predictions,

  • and all the black points are experimental predictions.

  • And for the most part, they look spot-on.

  • It generates the classic binding energy per nucleon

  • curve that you see in the textbook

  • and can predict from the semi-empirical mass formula.

  • Zooming in and correcting for, let's say,

  • just getting absolute values of errors,

  • you can see that, except for the very small nuclei

  • and a few peaks, which we explained

  • by looking even closer, the formula, well,

  • it predicts nuclear stability quite well on average.

  • Again, this line right here, if there's

  • a dot that lies on this blue line,

  • it means that theory and experiment agree.

  • And a deviation by a few MeV here and there, not too bad.

  • But we started also looking at different nuclear stability

  • trends, and we noticed that for odd mass number nuclei,

  • there's usually only one or sometimes none stable isotopes

  • per Z, whereas for even ones, there's quite a few more.

  • And we're going to be now linking up

  • the stability of nuclei versus what mode of decay

  • they will take in order to find a more stable configuration.

  • We looked quickly at the number of stable nuclei with even

  • and odd Z and noted that these places right here where

  • there are no stable nuclei correspond to technetium

  • and promethium.

  • There's no periodic table on the back of this wall,

  • but behind my back on the other wall,

  • there's that periodic table where

  • you can see the two elements that are fairly

  • light with no stable isotopes.

  • That's what those correspond to.

  • And the peaks correspond to what we call magic numbers

  • or numbers of protons or neutrons

  • where all available states at some energy

  • are pretty much filled.

  • And this goes for both protons and neutrons.

  • So something with a magic number for both n, number of neutrons,

  • and Z, number of protons, is going

  • to be exceptionally stable.

  • And we'll see how that's used as a tool

  • to synthesize the super heavy elements that we believe

  • should exist.

  • And finally we got into these mass parabolas.

  • I found this to be a particularly difficult concept

  • to just get mathematically.

  • If you remember, we wrote out the semi-empirical mass formula

  • and said if you take the derivative with respect to Z,

  • as we did it, you would get the most stable z for a given A.

  • And we started graphing for a equals 93

  • where niobium is stable.

  • That was just the one I had on the brain from some failures

  • in lab earlier this week.

  • We started plotting where those nuclei--

  • what is it-- the relative masses are for a fixed A. So

  • let's regenerate that one right now,

  • because we were a little fast at the end of last lecture.

  • Then I want to generate one for a equals 40.

  • And you'll see something kind of curious.

  • I'm going to leave this up here for a sec.

  • If you notice, for odd A nuclei, there's

  • only one parabola, whereas for even A, there are two.

  • Why that is, we're going to see when we

  • look at the table of nuclides.

  • But notice this nucleus right here

  • can decay by either positron emission or beta emission

  • to get to a more stable form.

  • And there are many real examples,

  • and I'm going to show you how to find them.

  • So let's start off by going back to the table of nuclides,

  • finding niobium-93.

  • Just go up one more chunk.

  • And there we are.

  • Niobium-93 is a stable isotope.

  • And if you want to see where it came from,

  • you can scroll down a little bit and see its possible parent

  • nuclides right here.

  • So let's say that niobium--

  • we'll draw it right there--

  • is stable.

  • We'll put it at the bottom of this parabola.

  • And let's work down in Z. So we'll move to zirconium.

  • Zirconium-93 ostensibly has a very similar atomic mass.

  • But if you remember that 93 AMU is a rather poor approximation

  • for the actual mass of all nuclei with A equals 93.

  • In fact, if you look very closely at the atomic masses,

  • zirconium-93 is 92.90.

  • Niobium-93, well, it looks like we

  • have to go all the way to another digit there.

  • 92.906.

  • You have to go to, like, even more digits 92.906375,

  • 92.906475.

  • So we go down in Z, and we've actually

  • gone up in mass by looks like the sixth or seventh digit

  • in AMU.

  • If we go up in mass, we go down in binding energy.

  • That tells us that there's something that's less stable.

  • And if you notice, we went down by a very small--

  • or we went up by a very small amount of mass.

  • Notice also that its beta decay energy is really, really small,

  • 91 kiloelectron volts.

  • So why don't we put zirconium just above?

  • And we note that that decay will happen

  • by beta, where the beta, let's say

  • if we have an isotope with mass number A, protons Z,

  • and let's just call it symbol question mark.

  • In beta decay, we have the same A.

  • We'll have a different Z. We're going

  • to have to give these symbols.

  • Let's call this parent, and we'll call that daughter.

  • Plus a beta, plus an electron antineutrino.

  • And what has to happen to that Z in order for everything

  • to be conserved?

  • It's the same reaction that we've got here for--

  • I'm sorry-- for zirconium.

  • So you'd have to have one fewer proton to release one electron.

  • And so that becomes same A but different Z.

  • And this is the beta decay reaction.

  • Let's go back a little farther.

  • We'll look at the possible parent nuclide for--

  • did anyone have a question?

  • AUDIENCE: Don't you need one more proton [INAUDIBLE]??

  • PROFESSOR: Let's see.

  • Which direction are we going in Z here?

  • That goes to yttrium.

  • It actually looks like it's going down.

  • Oh, yeah, for beta decay.

  • I'm thinking-- I have the reaction backwards.

  • Sorry.

  • I need one more proton to account

  • for the extra negative charge.

  • You're right.

  • OK.

  • Yep, I was thinking backwards, because we're now

  • climbing up the decay chain in reverse order.

  • So this could have come from yttrium-93 with a much

  • higher energy of three MeV.

  • So let's put yttrium right here.

  • That gives a beta decay.

  • And we'll just go one more back to strontium-93 Has

  • an even higher beta decay energy.

  • So let's put that up here.

  • And let's take a look at its mass real quick.

  • The mass of strontium-93, 92.914 AMU.

  • If we go back to niobium-93, now it's

  • noticeably different to, like, four significant digits

  • instead of six.

  • 92.914 versus 92.906.

  • And so that shows you that a tiny bit of mass and AMU

  • corresponds to a pretty significant change

  • in binding energy by that same conversion factor

  • that we've been using everywhere.

  • 931.49 AMU per big MeV per C squared.

  • Let's see.

  • Yeah.

  • OK.

  • So let's go now in the other direction, in the positron

  • direction.

  • Niobium can also be made by electron capture

  • from molybdenum.

  • So let's put molybdenum right here.

  • Let's say that around half an--

  • what did we have here?

  • It was like half an MeV.

  • Like that.

  • And let's see.

  • Molybdenum-93 could have been made by electron capture

  • from technetium-93 with an energy of 3.201 MeV,

  • even more extreme.

  • We'll go back one more, because there's a trend that I want

  • you guys to be able to see.

  • And this could have come from electron capture

  • from ruthenium.

  • I think I may have said rubidium last time,

  • but Ru is ruthenium-93.

  • And that 6.3 MeV, something like that.

  • And this is where we got to yesterday.

  • Now I'd like us to take a closer look at the decay

  • diagrams, which tells us what possible decay reactions can

  • happen in each of these reactions.

  • Since we're right here on the chart,

  • let's take a look at ruthenium turning into technetium by what

  • it says, electron capture.

  • So note that on the table, you can click on electron capture,

  • and if it's highlighted, then the decay diagrams are known.

  • It's not known for every isotope,

  • but for a lot of the ones you'll be dealing with, it is.

  • And you get something I have to zoom out for--

  • a lot, a lot of different decays.

  • What I want you to look at is this one here on the bottom

  • that I'll zoom in to.

  • That should be a little more visible.

  • So notice that if you want to go down the entire 6.4-something

  • MeV, it usually proceeds by B-plus or positron decay,

  • by either method.

  • And as you go up the chain, as these energy differences get

  • smaller, look what happens to the probability

  • of getting positron decay.

  • It shrinks lower and lower and lower.

  • So there's a trend that the larger the decay

  • energy for this type of reaction, the more likely

  • you're going to get positron decay.

  • And in fact, where we left off last time is in order

  • to get positron decay, the Q value of the reaction

  • has to be at least 1.022 MeV, better known

  • as at least two times the rest mass of the electron,

  • because in this case, to conserve charge and energy,

  • you shoot out a positron, and you also

  • have to eject an electron in order

  • to conserve all the charge going on here.

  • So there you have it.

  • Now let's look at the lower energy decay of technetium

  • to molybdenum, which had something

  • like 3 MeV associated with it.

  • So we'll click on technetium, and its energy is 3.2 MeV.

  • Let's take a look at its electron capture.

  • Significantly simpler.

  • Already what do you notice about these positron

  • to electron capture ratios?

  • Anyone call it out.

  • AUDIENCE: Electron capture is much more likely.

  • PROFESSOR: Indeed.

  • When the energy of the decay goes down--

  • notice that only these decays are allowed--

  • The electron capture suddenly becomes much more likely.

  • But notice that it does not let you go directly

  • from 3.2 MeV to 0.

  • There is no allowable decay here.

  • So this is probably a change of-- that's 3.2.

  • That's 1.3.

  • A little less than 2 MeV.

  • All of a sudden, electron capture

  • becomes much more likely, but positron decay

  • is not disallowed yet.

  • So we can say electron capture or positron decay right there.

  • Everyone with me so far?

  • So let's go to the really low energy one.

  • We'll click on molybdenum-93 and see

  • how it decays with an energy of 0.405 MeV to niobium.

  • Anyone want to guess what's allowed?

  • AUDIENCE: Electron capture only.

  • PROFESSOR: Electron capture only.

  • There's not enough energy for positron decay.

  • And, indeed, it draws funny, because there's

  • a metastable state.

  • But if you scroll down here, there

  • are two pathways allowed, both of which by electron capture.

  • Decay diagram's quite a bit simpler.

  • So we leave this one here by saying it can only

  • decay by electron capture.

  • Any questions on the odd A before we

  • move on to the even, which is a little more interesting?

  • Cool.

  • OK.

  • Let's move on to the even case.

  • So for here, I'm going to go back

  • to the overall picture of the table of nuclides.

  • Click on around where I think potassium-40 is.

  • Looks like I got there.

  • And I want to point out one of these features.

  • If you wanted to undergo decay change

  • and maintain the same mass number,

  • that's diagonally from upper left to lower right.

  • See how all the isotopes here have a 40 in front of them.

  • The really interesting part is as you cross this line,

  • you go from stable to unstable to stable to unstable again.

  • The colors here is dark blue represents stable,

  • and dark gray represents long lifetimes

  • of over 100,000 years.

  • So this is one of the reasons you find potassium-40

  • in the environment.

  • In fact, 0.011% of all potassium in you and everything

  • is potassium-40.

  • It's what's known as a primordial nuclide.

  • It's not stable, but its half-life

  • is so long that there's still some

  • left since the universe began or whatever

  • supernova that formed Earth got accumulated into the earth.

  • But notice it can come from--

  • it can decay by a couple of different methods.

  • So let's pick one of those stable isotopes, calcium-40,

  • and put that as the bottom of the parabola on this diagram.

  • So we'll put calcium here.

  • And in a relative sense, we'll put a calcium point right there

  • for its total mass.

  • And it could have come from beta decay

  • from potassium-40 or electron capture from scandium-40 40.

  • So let's look at potassium-40.

  • It can beta decay for about, oh, 1.3 MeV.

  • So potassium is right here.

  • Let's say it could beta decay with about 1.3 MeV.

  • And we'll trace potassium back a little bit,

  • figure out where would it have come from.

  • Interesting.

  • Doesn't tell us.

  • OK, forget that.

  • Let's trace calcium back and say there's scandium-40.

  • And scandium-40 can decay with-- wow--

  • an enormous 14.32 MeV.

  • Let's put that like here.

  • Anyone want to guess which mode, electron capture or positrons,

  • much more likely?

  • AUDIENCE: I think positrons.

  • PROFESSOR: Probably positron.

  • Let's take a look.

  • Oh boy.

  • Another complicated one.

  • But the whole way down, positron, positron,

  • positron for all the most likely decays.

  • You won't find a drawing to every single line.

  • I believe that they know that at some point,

  • drawing extra lines is futile, and they just all overlap

  • each other.

  • So I don't know exactly how the algorithm works,

  • but it does draw up to some number of possible decay

  • chains.

  • If you want to see every single one,

  • they are tabulated in a very, very long list down below.

  • I'm never going to ask you to do something with all of these,

  • because that would be insane unless it's

  • a relatively simple decay, like that

  • has two or three possibilities.

  • And let's see.

  • This could have come from electron capture

  • from titanium-40 with 11.68 MeV.

  • Wow.

  • OK.

  • Up here.

  • And there's titanium.

  • And let's go in the other direction.

  • So I do know that potassium-40 can decay into argon-40.

  • So let's jump there.

  • Argon is a stable isotope too.

  • So potassium-40 can decay into argon-40 by electron capture.

  • OK, good.

  • A more respectable 1.505 MeV.

  • Is positron decay allowed?

  • AUDIENCE: Yes.

  • PROFESSOR: Yes.

  • Why is that?

  • AUDIENCE: [INAUDIBLE]

  • PROFESSOR: Over 1.022 MeV.

  • Yeah.

  • Anyone have a question?

  • No?

  • OK.

  • So we've got kind of a kink in our mass parabola.

  • Yeah?

  • AUDIENCE: Actually, yeah, so it's

  • possible if it's over 1.022, but it's still very unlikely.

  • PROFESSOR: That's correct.

  • AUDIENCE: Until we get to these higher orders, like 10.

  • PROFESSOR: Yep, so once the Q value's satisfied,

  • it is technically possible.

  • But if you had something with the decay

  • energy of, like, 1.023 MeV, it would be exceedingly unlikely.

  • So in fact, we can take a look at this.

  • This, I would say, is also going to be

  • on the exceedingly unlikely level, and we can take a look.

  • So if we look at the decay diagram,

  • we know it makes positrons.

  • They're not even really listed.

  • Interesting.

  • So that process would not be allowed,

  • but this one, because that's about 1.5 MeV,

  • should be allowed.

  • But since that branch ratio or the probability

  • of that happening is already so low, I wonder if it even says.

  • Yep, beta ray with a max or average energy of 482.8 MeV.

  • We're going to go over why that energy is so low when

  • we talk about decay next week.

  • With the relative intensity of something with a lot of zeros

  • before the decimal place.

  • So there you go.

  • Like you said, energies near 1.022 MeV, slightly above it,

  • are extremely unlikely but possible and measurable.

  • Cool.

  • And then let's see what could have made argon 40.

  • Could have been beta decay from chlorine-40.

  • So chlorine maybe was here.

  • And I don't think I have to draw any more.

  • So we've got a funny-looking parabola with a kink in it,

  • because really, you have two mass parabolas overlapping.

  • I'm going to go back to the screen

  • so that the diagram from the notes

  • makes a little more sense.

  • What we've kind of traced out here

  • is that there's two overlapping parabolas here.

  • There's the one with the-- what is

  • it-- the odd Z and the even Z.

  • So there you go.

  • Just like the one on here, which I think

  • is for a different mass number.

  • Yep.

  • 102.

  • We get the same kind of behavior where things will mostly

  • follow the lower mass parabola, but sometimes if something

  • gets stuck here, it can go either way to get more stable.

  • So I want to stop here for new stuff,

  • because this is precisely where I thought

  • we'd be at the end of the week.

  • And in the next half an hour, I'd

  • like to open it up to questions or working things

  • out together on the board or anything else

  • you might have had.

  • Yeah?

  • AUDIENCE: I have a question about the parabola things.

  • PROFESSOR: Sure.

  • AUDIENCE: There's-- you said multiple paths,

  • so it doesn't have to do the little peak in the middle?

  • Like, could it follow the lower parabola or the upper,

  • or does it have to jump over?

  • PROFESSOR: It's going to go in whatever

  • way makes it more stable.

  • So you're never going to have a nucleus that's

  • going to spontaneously gain mass in order

  • to get to a different path.

  • You can only go down on the mass axis.

  • But let's say you happen to be starting here at potassium-40.

  • You can go down via either mechanism to the next mass

  • parabola down.

  • AUDIENCE: But if you were argon, you would go up.

  • That's what you would do.

  • PROFESSOR: That's right.

  • If you're at argon, you're stuck.

  • And in fact, if you want to take a look,

  • what do I mean scientifically by "stuck"?

  • I mean stable.

  • Argon-40 is a stable nucleus that

  • comprises 99.6% of the argon.

  • So that's what I mean by "stuck" is stable.

  • And if we look at the rest of the table of nuclides

  • for similar-looking places--

  • so let's hunt near potassium-40.

  • So notice potassium-40 right here

  • has got stable isotopes to the upper left and the lower right.

  • If we look back over here, manganese-54.

  • Same deal.

  • It's got a stable isotope to the upper left and a stable one

  • to the lower right.

  • How much you want to bet that when we click on manganese-54,

  • it's got two possible parent nuclides--

  • or I'm sorry, two possible decay methods.

  • So let's take a look.

  • Manganese-54 can either electron capture and positron decay

  • to chromium-54 or beta decay to iron-54.

  • Let's take a look at one more to hammer the point home,

  • and I think that'll probably be enough.

  • Cobalt-58 right near nickel-58 and iron-58.

  • Interesting.

  • That one's not allowed unless there's more down here.

  • So you can electron capture to iron-58,

  • but there's no allowed decay to--

  • what was it?

  • Nickel-58.

  • OK.

  • Let's look for more.

  • Chlorine-36 has argon and sulfur on either side.

  • There it is.

  • Beta decay and electron capture.

  • And how much you want to bet there's basically never

  • a positron here?

  • But basically, not actually never.

  • So you get a positron 0.01% of the time and electron

  • capture 1.89% of the time.

  • Where is the other 98-and-change percent?

  • Right here in the beta decay.

  • So in this case, chlorine-36 will preferentially beta decay.

  • If you also notice, it's a--

  • let's see.

  • I don't know if that actually matters.

  • But I am going to say it's more likely to beta decay.

  • So when you sum these up, you get

  • 100% of the possible decays.

  • Let's see how many energy levels there are there too.

  • Hopefully not too many.

  • That qualifies as not too many.

  • Yeah?

  • Sean?

  • AUDIENCE: Are the changes in mass always going

  • to be attributed to beta decays or electron

  • captures or positron [INAUDIBLE]??

  • PROFESSOR: They'll be due to those as well

  • as some other processes, which we're going to cover on decay.

  • But if you notice, I've been giving you

  • a lot of flash-forwards in this class.

  • We've introduced cross-sections as a thing,

  • the proportionality constant between interaction

  • probabilities.

  • We're going to hit them hard later.

  • I've also been kind of introducing or flash-forwarding

  • different methods of decay.

  • So there's also alpha decay.

  • There's also isomeric transition or gamma emission.

  • There's also spontaneous fission.

  • This is the whole basis behind how

  • fission can get working without some sort

  • of kick-starting element.

  • So maybe now's a good time to show you.

  • Let's go to uranium-235 and see how it decays.

  • It goes alpha decay to thorium-231 most of the time.

  • And if you look how, it's not terrible.

  • We can make sense of this.

  • It also undergoes SF, which stands for spontaneous fission.

  • So one out of every seven--

  • what is it?

  • Seven out of every billion times,

  • it will just spontaneously fizz into two fission products.

  • And this is why if you put enough uranium-235 together

  • in one place, you can make a critical reactor.

  • In reality, you don't tend to want

  • to put enough U-235 together to just spontaneously go critical.

  • We use other isotopes as kickstarters.

  • For example, californium, I think it's 252.

  • Let's take a quick look.

  • There we go.

  • Californium-252 undergoes spontaneous fission 3%

  • of the time.

  • It's even heavier, even more unstable.

  • So there is a reactor called HFIR,

  • or the high flux isotope reactor at Oak Ridge National Lab.

  • One of its main outputs is californium kickstarters

  • for reactors.

  • So to get things going, you put a little bit of californium

  • in as a gigantic neutron source, and then you don't really

  • need it anymore once it gets going.

  • So it's one of the safer ways of starting up

  • a reactor is put in a crazy neutron source,

  • and then once it gets going, take it out or leave it in

  • and burn it.

  • I'm not actually sure which one they do.

  • Yep?

  • AUDIENCE: Is the name californium

  • based on California?

  • PROFESSOR: It is.

  • When we get to--

  • now is a good time to introduce the super heavy elements

  • since you asked.

  • So a lot of these older elements were named after--

  • actually this is kind of a hobby of mine.

  • So I don't know if you guys saw the periodic table outside.

  • I collect elements, because if you're

  • going to collect something, you might

  • as well collect everything that everything else is made of.

  • It's the same reason I went into nuclear energy.

  • I started off course 6, or 6.1, specifically electrical.

  • And I was like, well, I could be designing, like,

  • the next screen for a cell phone,

  • or we could solve the energy problem,

  • which is the problem all others are based off of.

  • So my whole life theme has been go to the source.

  • That's why I came here in high school and never left.

  • That's why I declared course 22.

  • That's why I collect elements and probably is

  • the reason for many other things which only a psychiatrist could

  • diagnose.

  • But let's look at some of the other elements.

  • For example, yttrium.

  • I think it has a isotope 40.

  • Anyone know-- no, it doesn't have a 40.

  • What about a 50?

  • 60?

  • 100?

  • Whatever.

  • At least it knew that Y was yttrium.

  • Anyone know--

  • AUDIENCE: 89.

  • PROFESSOR: --where this is coming from?

  • 89?

  • Seems high.

  • Oh my god.

  • You're right.

  • AUDIENCE: I work with it.

  • PROFESSOR: OK.

  • Gotcha.

  • You work with it.

  • Awesome.

  • Anyone know what this is all about, yttrium?

  • There's a town called Ytterby in Sweden

  • where large deposits of yttrium and ytterbium, or Yb,

  • tend to be found or Db, named for dubnium.

  • So let's say the really basic elements tend

  • to come from Latin.

  • Fe stands for iron, which actually stands for ferrum.

  • Lead is plumbum.

  • Gold is aurum.

  • Silver, Ag, is argentium.

  • I don't know if I'm saying that right.

  • I never took Latin, and I've never

  • heard it spoken, of course.

  • And then a lot of the heavier and heavier elements as we go

  • are being named for more and more famous

  • scientists or places where they tend to be made like Db.

  • I'm going to guess 260 for a mass there.

  • Oh, nice.

  • For Dubna in Russia that has got one

  • of the few gigantic super heavy element colliders where they're

  • constantly synthesizing and characterizing

  • these super heavy elements.

  • So finally they said, you know what?

  • They've made enough of these in Dubna.

  • Let's name one of the elements after them.

  • Or Sg, seaborgium, for Glenn Seaborg.

  • Or No, nobelium, for Alfred Nobel.

  • Yep?

  • AUDIENCE: I just have a question for the actual mass parabola.

  • PROFESSOR: Uh-huh.

  • AUDIENCE: Like, do the parabolas ever, like, reach each other?

  • PROFESSOR: Do they intersect?

  • AUDIENCE: Yeah.

  • PROFESSOR: I've never seen a case where they intersect.

  • That would make for a crazy situation indeed.

  • However, part of what the homework assignment's about

  • is to derive an analytical form for a mass parabola

  • and then check the data to see how well it works.

  • So for any cases where you have an even mass number,

  • and you have either odd-odd or even-even nuclei,

  • you can check those equations analytically

  • to see if they'll intersect.

  • AUDIENCE: And for the case of A equals 40,

  • I'm not really sure what the top parabola is.

  • PROFESSOR: So the top parabola for potassium-40--

  • let's take a quick look at how many protons and neutrons it

  • has.

  • Potassium has a proton number of 19, which means

  • it has a neutron number of 21.

  • So the top parabola is odd N and odd Z,

  • where the bottom one is even N and even Z.

  • Whereas for odd mass number nuclei,

  • it has to be either odd-even or even-odd,

  • else it would be even, which is a funny sentence when

  • you say it all out loud.

  • Yeah.

  • So that's the idea here is that notice

  • that the even-even parabola tends to be further down.

  • All those nuclear magic numbers, 2, 8, 20, 28--

  • I'm not going to quote the rest.

  • Those the little ones I know.

  • All even numbers.

  • So any other questions on these mass

  • parabolas before we launch into super heavy elements?

  • Yeah?

  • AUDIENCE: [INAUDIBLE] the bump on the right?

  • PROFESSOR: Uh-huh.

  • AUDIENCE: How do you know that that's where [INAUDIBLE]??

  • PROFESSOR: Analytically or experimentally?

  • Which question?

  • AUDIENCE: Analytically.

  • PROFESSOR: So analytically.

  • Analytically there should be some isotope

  • of-- well, not potassium.

  • That wouldn't be allowed.

  • So in this case, the stable element positions

  • have got to kind of switch off, shouldn't they?

  • So if that's potassium-40, that would still

  • have to be potassium.

  • You don't really have another choice.

  • There isn't really a position there, is there, analytically?

  • That's the interesting thing is that you can either

  • be odd-odd or even-even for an even mass number.

  • But you can't just take off one neutron from potassium-40,

  • and then you've got potassium-39.

  • Then you're on a different mass number.

  • Or if you exchange a proton and a neutron,

  • which you pretty much do in either of these directions.

  • There's no way to get straight down here.

  • AUDIENCE: Right.

  • PROFESSOR: Yeah?

  • AUDIENCE: For odd-odd, delta is negative, right?

  • PROFESSOR: For odd what?

  • For-- sorry?

  • AUDIENCE: For odd-odd, delta is negative?

  • PROFESSOR: Yeah, let's go back to that slide

  • just to make sure.

  • You mean the pairing term in the semi-empirical mass formula?

  • AUDIENCE: Yeah.

  • PROFESSOR: Yeah, so for odd-odd nuclei,

  • indeed, delta's negative, which means lower binding energy,

  • which means higher mass.

  • And that's why we see it bump up on the mass right here.

  • Yeah?

  • And do you have a second part of the question?

  • AUDIENCE: It was more so how to relate

  • [INAUDIBLE] like the binding energy to that mass parabola.

  • PROFESSOR: We can actually relate--

  • so we can relate the binding energy

  • to the mass and the mass parabola analytically,

  • because the binding energy is equal to Z times protons plus N

  • times mass of neutron minus the actual mass

  • of that same nucleus, A comma Z. So they're actually directly

  • related, just negatively.

  • So something with a higher mass is

  • going to have a low binding energy, which means it's

  • less bound and less stable.

  • And indeed, the further up the mass scale we go,

  • the higher those beta or electron

  • capture or positron energies are.

  • And there's another thing you can check too,

  • which is the half-life.

  • Half-life is what we'll be talking about on Tuesday.

  • It's how long before an average amount of a substance

  • has undergone radioactive decay.

  • So let's look at some of these isotopes

  • and start looking at half-life trends

  • as another measure of stability.

  • So potassium-40 has an exceptionally long half-life.

  • So it's relatively stable.

  • Let's take a look not at either the stable isotopes,

  • but let's go up the mass parabola

  • chain in one direction.

  • Calcium-40, scandium-40.

  • So let's take a look at scandium-40.

  • Scandium-40 has a half-life less than a second.

  • And it's got quite a high decay energy by whatever method

  • you want to use.

  • Let's go up to titanium-40.

  • Anyone want to guess?

  • Do you think the half-life is going to go up or down?

  • Let's see if the half-life goes down.

  • We know the decay energy goes up.

  • Indeed.

  • Half-life goes down from 182 milliseconds to 50

  • milliseconds.

  • And let's say titanium-40 could have come from-- wow.

  • Two proton decay from Cr-42 with a half-life of 350 nanoseconds.

  • So as we go up the mass ladder and down the stability ladder,

  • the half-life decreases, which kind of follows intuitively.

  • Something that's exceptionally stable

  • should have a half-life of infinity,

  • and something that's exceptionally unstable

  • should just blow apart instantly.

  • Like, remember the first week of class,

  • we talked about helium-4 grabbing a neutron,

  • becoming helium-5, and instantaneously going back

  • to helium-4.

  • If you look at helium-5, its half-life

  • is measured in MeV, or 7 times 10 to the minus 7 femtoseconds.

  • So if helium-4 absorbs a neutron,

  • it simply doesn't want it and gets rid of it

  • in 10 to the minus 7 femtoseconds, which

  • would tell us that it's exceptionally unstable.

  • So I hope that's a long-winded answer

  • to that question about what does it mean to be going up

  • in the mass levels.

  • Any other questions on mass parabolas or the liquid drop

  • model or stability in general?

  • Yes.

  • AUDIENCE: For something that goes upwards [INAUDIBLE]

  • just because the mass [INAUDIBLE]..

  • PROFESSOR: So if you're changing one neutron

  • to a proton in each case, you're switching back and forth

  • from the odd-odd to the even-even mass parabolas.

  • So if I were to redraw these dots more to scale,

  • this would have to be on the odd-odd.

  • And, well, let me draw them a little better.

  • Yep.

  • AUDIENCE: OK.

  • PROFESSOR: That's on the odd-odd,

  • and that's on the even-even.

  • AUDIENCE: OK.

  • PROFESSOR: Yeah.

  • So excuse my poor drawing skills.

  • But if you're switching one proton to a neutron

  • or vice-versa, by definition, you're

  • jumping back and forth between these parabolas.

  • AUDIENCE: OK, thank you.

  • PROFESSOR: That's a good question for clarification.

  • You had a question too?

  • AUDIENCE: Yeah, about the semi-empirical mass formula.

  • When do you use that to find binding energy as opposed

  • to, like, any of the other ways?

  • PROFESSOR: I'm sorry.

  • The semi-empirical mass formula is a good way

  • to get an analytical guess at most of them.

  • If you want an exact answer, always

  • use the actual binding energy.

  • AUDIENCE: So, like, how often is it used now?

  • PROFESSOR: I would not say it's used much now except--

  • well, that's going to be one of your homework questions

  • is this formula predicts that as you get heavier and heavier

  • and heavier, nuclei should just continuously get less stable.

  • And that was, as of when this was derived,

  • let's say decades ago, we now know something different

  • is happening.

  • So if you look at the table of nuclides,

  • you can sort of see some swells in the number of black pixels

  • until it cuts off.

  • And this region actually where we think super heavy elements

  • happen, I want to jump to the actual table of nuclides, which

  • I'll say is our snapshot of knowledge today,

  • and go all the way to the top.

  • And our knowledge kind of cuts off at these elements, which

  • are, for now, temporarily named in a very uncreative way.

  • We don't even know anything about them.

  • Uun is probably going to have a proton number of what?

  • 110.

  • I don't know what the prefixes are,

  • but UUU would be un-un-un 111.

  • Probably has 111 protons.

  • Beyond here, off the screen or probably up into the next room,

  • it's predicted that once you approach the next magic number

  • in nuclei, there should be an island of stability

  • where it may not necessarily be totally stable,

  • but the half-lives should go up again.

  • And we should be able to synthesize super heavy matter.

  • And if you actually graph neutron number

  • versus half-life-- so notice how we were looking at half-life

  • as a measure of stability.

  • It starts to go up, then comes down, and then,

  • to the extent of our knowledge, it

  • is going back up again to the next predicted magic number.

  • So what we think should be happening

  • is half-lives should be continuously going up.

  • And yeah?

  • You had a question?

  • AUDIENCE: Like, what do we do with these weird things?

  • PROFESSOR: Well, whatever you want.

  • It's going to be--

  • it should be dense as all heck, because nuclear matter is quite

  • a bit denser than ordinary matter,

  • and quite a bit is quite an understatement.

  • So what would you do with super heavy matter?

  • A lot of it could be used to probe the structure of matter.

  • There's a lot about how the nucleus is

  • constructed that we don't know.

  • And beyond the scope of this course

  • would also be an understatement.

  • There's folks that are making their careers now

  • on figuring out what are the forces between nucleons?

  • Why do things spontaneously fizz at the rates that they do?

  • You'll even hit a little bit of this in 22.02

  • when you can calculate the rough half-life for alpha decay using

  • quantum tunneling through the potential barrier in a nucleus.

  • And so the more nuclei we have to mess around with,

  • the more data and real examples we have to study.

  • But practical applications, well, I could imagine,

  • we might find something denser than osmium.

  • Osmium right now has a density of about 22 grams

  • per cubic centimeter.

  • This stuff, zirconium, is about 6.9 or so.

  • Steel is like 8.

  • Lead's like 11.

  • Mercury is like 19.

  • Have any of you ever played with liquid mercury before?

  • This is a "don't try this at home, kids" kind of moment.

  • My grandfather happened to be a dentist,

  • so we happened to have a lot of mercury to mess around with.

  • And it's, like, unintuitively heavy.

  • It's unbelievable.

  • A 1-pound jar is about that big.

  • I think it would be cool if we could

  • find something even denser.

  • And then really, really dense matter

  • happens to make really, really good photon shields and gamma--

  • not the Star Trek thing.

  • I mean this in the actual nuclear physics sense.

  • The best way to stop gamma rays for gamma shielding

  • is just put more matter in front of it.

  • And if we find a denser state of matter that's earth stable,

  • you then have a smaller gamma shield.

  • So there are practical applications too in radiation

  • shielding.

  • They also might make awesome nuclear fuel,

  • because you better believe they're

  • going to fizz like crazy.

  • So who knows?

  • Maybe we can-- I don't think that would be cost-effective,

  • but it would probably work.

  • So the way they're doing this is actually

  • slamming calcium 48 nuclei into other super heavy elements

  • that have exceptionally long half-lives.

  • So if you can't read what the screen says,

  • this here is berkelium, for Berkeley,

  • with proton number 97, mass number 249.

  • Let's take a look at the Bk-249, which happens

  • to be way beyond uranium.

  • So it's definitely not a stable isotope,

  • but it has a half-life of 320 days.

  • That means you can make a bunch of it,

  • chemically separate it, make it into a target,

  • and fire calcium-48 nuclei into it.

  • Anyone want to guess, why do we use calcium-48?

  • And I'll give you a hint and write the proton number

  • for calcium.

  • The isotope that we use is calcium-28--

  • or calcium-48.

  • Anyone want to take a guess?

  • Why start here?

  • Why not just smash two berkeliums into each other?

  • Calcium 48 happens to be exceptionally stable,

  • because it's got two magic numbers.

  • Its proton number is 20, one of those peaks of stability.

  • And its neutron number is 28.

  • So start with something super stable,

  • something with a lot more binding energy to begin with,

  • and you maximize your chance of making something

  • with more binding energy that won't just spontaneously

  • disappear.

  • So there are reasons calcium 48 was chosen

  • and not something heavier or lighter.

  • If we go back to that article, you

  • can see what happens here is you make some element 117, which

  • has yet to be made, and it undergoes alpha decay until it

  • reaches some rather stable--

  • you know, 17 seconds.

  • That's pretty exceptional.

  • And if you notice the trends here, as you decay,

  • the alpha energy steadily goes down,

  • and the half-life steadily goes up.

  • And so what you do is you make a super, super heavy element,

  • hoping that it will decay and rest

  • in one of these islands of stability

  • beyond the magic numbers that we know right now.

  • Which I thought this was super cool,

  • because this is actually happening now.

  • Like, new elements are made.

  • I think we've been seeing one a year

  • or so for the past few years on average.

  • There might have been a year when there was more than one

  • announced recently.

  • There's only a few places in the world doing them,

  • but you can start to-- already with two weeks of 22.01,

  • you can start to get a handle for why

  • do they use the nuclei they do, and then what sort of things

  • are you looking for?

  • Decays with lower and lower energy

  • mean you're already starting to get less steep on whatever

  • imaginary mass parabola.

  • Don't quite know how to draw this one,

  • because it's beyond anything we know.

  • And as the half-lives keep going up,

  • you can tell that it's reaching a measure of stability.

  • However, to get you started on the homework,

  • for the open-ended ended problem--

  • I think I'll bring it up right now

  • so you guys can take a look.

  • So let's go to the Stellar site.

  • Hopefully it doesn't call me.

  • Good.

  • And two problem set two.

  • This is the way I know that everyone's

  • seen the P set seven days before it's due, because I'm going

  • to put it up on the screen so you can

  • see it all the way at the end.

  • Predicting the island of stability.

  • Does the semi-empirical mass formula

  • predict the island of stability?

  • Well, let's start you off with the easier

  • part of the question, which is yes or no.

  • And I'm going to leave you to the why and the how.

  • If we graph binding energy per nucleon versus mass number,

  • the semi-empirical mass formula predicts something like this.

  • What happens as we go beyond the realm of known mass numbers?

  • Anyone?

  • How should I extend this curve?

  • What did you say, Alex?

  • AUDIENCE: I don't know.

  • PROFESSOR: Just keep going.

  • Yeah.

  • Does this predict an island of stability?

  • I don't think so.

  • So that's one of the few questions I'm

  • asking you in this homework.

  • And it's up to you guys.

  • Use your creativity.

  • Again, this is an open-ended problem.

  • I'm not looking for a specific answer.

  • I want to see how you think and how

  • you would change this formula to account

  • and actually predict the island of stability while still

  • satisfying the mostly correct predictions from the elements

  • we know.

  • So-- sorry, go ahead.

  • AUDIENCE: So should it, like, converge a little bit?

  • PROFESSOR: Well, you're on the right track.

  • If you want to show stability, you'd

  • want it to maybe have a higher value right here.

  • Higher binding energy per nucleon

  • would correspond to a lower mass, which would

  • correspond to higher stability.

  • So how would you predict this island of stability?

  • And then more specifically, how would you

  • reconcile the inaccuracies in the semi-empirical mass

  • formula?

  • Because we know it doesn't work very well for all cases.

  • There are some cases like right around here where it works

  • great, and there's some like right here and right here where

  • it really doesn't.

  • You can get things wrong by like 10 MeV,

  • which is pretty significant.

  • You know, that's like four digits on the mass scale, like,

  • the fourth decimal place.

  • That's huge to a nuclear engineer.

  • So that's something to get thinking about.

  • And remember I did tell you that there will

  • be some open-ended problems.

  • I'm going to mark them as open-ended

  • so you actually know.

  • We're not looking for a right or wrong answer.

  • This is one of those kinds of things

  • where we want to see how you think

  • and what do you think is missing.

  • There's other hard problems where we give you the answer,

  • because I'm not interested in you deriving some insane

  • expression and getting it right.

  • I'm interested in the derivation process.

  • What are the steps you choose?

  • What sort of assumptions do you make?

  • What sort of terms can you neglect and say,

  • that's in the ninth decimal place.

  • I'm going to forget it.

  • So in this case, we give you the answer,

  • because we're going to grade you on the process.

  • And you can use the answer to check your process

  • and see if you're on the right track or not.

  • For the skill-building questions,

  • we actually do want you to come up

  • with some sort of an answer like explaining

  • the terms in the semi-empirical mass formula

  • or modifying an equation to calculate something else.

  • We will be looking for a right answer there.

  • But those are questions to make sure that you

  • get the basics of the material.

  • If you can answer all of the questions in the first half

  • of these P sets fairly quickly, let's say in three or four

  • hours, you're totally on the right track.

  • The hard ones is because this is MIT.

  • And we want you to think beyond just

  • knowing what's in the Turner book or the Yit book.

  • Like I said, you guys are the leaders of this field.

  • So any other questions on stability in general?

  • Yes?

  • AUDIENCE: Just a real quick reminder.

  • When you say, like, even-even, are you

  • talking protons, neutrons?

  • PROFESSOR: Correct.

  • So that would be even N and even Z or odd N

  • and odd Z like in the reading and like

  • on these mass parabolas.

  • Yep.

  • Any other questions?

  • Yes.

  • AUDIENCE: Is the only proof or reason

  • that we say that there's an island of stability

  • because the mass increases up to the point of unknown?

  • PROFESSOR: There's a few--

  • so the question was, is the only reason

  • people think there will be super heavy elements because the mass

  • increases, right?

  • AUDIENCE: Yeah.

  • PROFESSOR: So in this case, the mass will always--

  • are you talking about now the total mass or--

  • AUDIENCE: Why is the idea that there

  • is this island of stability?

  • PROFESSOR: Ah, OK.

  • AUDIENCE: If this doesn't prove it,

  • do we have other reasons [INAUDIBLE]??

  • PROFESSOR: We have a few things to go on.

  • There are a number of different aspects of nuclear stability

  • that are all pointing to the same conclusion.

  • One of them, you can see on this graph here.

  • If you look at the alpha decay half-life

  • as a function of neutron number, it

  • doesn't just increase or decrease monotonically.

  • It swells up and down.

  • And it reaches a relative maximum

  • near certain magic numbers.

  • We can confirm that with the lower mass nuclei.

  • It doesn't work for really low mass,

  • because tiny things don't tend to undergo alpha decay.

  • But there are patterns that we're simply

  • recognizing and saying, well, if this is the next magic number,

  • it should continue to increase.

  • And I should mention too, this scale is logarithmic.

  • So the top right here is like 10 to the 4 seconds.

  • Just so you know, there are 86,400 seconds

  • in-- what is it-- a day.

  • And 3 times 10 to the 7 seconds in a year.

  • So if this graph--

  • let's say for Z 111--

  • were to continue on its track, it

  • should reach like 10 to the 9 or 10

  • to the 10, which could be like 100-year lifetimes

  • or 100-year half-lives, which means definitely you

  • can chemically separate them and do things with them.

  • I don't know if they would be safe enough to deal with.

  • But we also don't really know what's going to happen.

  • You can see that there is some uncertainty,

  • and things don't always follow the trend.

  • Even the error bars are outside the dashed lines.

  • But so we have this to go on.

  • We have the alpha decay half-life.

  • We also have the alpha decay energy.

  • As you approach an island of stability,

  • something that's more stable won't give off

  • as much kinetic energy to its alpha particle.

  • There is also-- for the ones that you can actually

  • measure that live long enough, you

  • can measure their mass to charge ratio

  • and actually get a good picture of their actual mass.

  • So we would expect the mass defect

  • to follow a certain trend as we go up.

  • The mass is always going to increase.

  • If you add more nucleons, it's going to increase.

  • But the mass defect, which is the real mass

  • minus the atomic number mass--

  • if stability were to increase, do you

  • think the mass defect would increase or decrease

  • with more stability?

  • Let's take a quick look at this.

  • If A were to stay the same, a shrinking real mass--

  • and remember, lower mass means more stability--

  • would mean a higher or a low mass defect?

  • It would mean a lower mass defect or a lower excess mass

  • as you'd call it.

  • So in this case, you would expect the mass of the nucleus

  • to be smaller than its A if it was going more stable.

  • And all of these trends work in the same direction,

  • which is saying, OK, so we have the alpha energy.

  • We have the mass defect.

  • We have the half-life all pointing to the same thing

  • that something should be more stable.

  • And we have some patterns to go on,

  • but our understanding is kind of incomplete.

  • So-- yeah?

  • AUDIENCE: So if there's super heavy elements,

  • do they exist somewhere in space,

  • or do stars make them, possibly?

  • PROFESSOR: Ooh.

  • AUDIENCE: Or are they--

  • PROFESSOR: Good question.

  • AUDIENCE: --currently made?

  • PROFESSOR: So the question is, if super heavy elements exist,

  • do they exist out there in space?

  • I think there would be a couple places they would exist.

  • The source of most of the elements beyond iron

  • is supernovas, where regular old fusion doesn't cut it anymore.

  • When you hit the maximum of this binding energy per nucleon

  • curve, you're at about iron 56.

  • That's why stars tend to form a core of iron

  • before it goes really bad in whatever way it

  • does for a star.

  • There are multiple ways.

  • When you get a supernova, you have an insane explosion,

  • and the core gets compressed from

  • the outside, forcing fusion of heavy elements to happen.

  • That's because you're putting in extra kinetic energy.

  • So it's like you have an endothermic reaction where

  • if Q is less than zero, how do you make that reaction happen?

  • Add kinetic energy, which can come

  • from a tremendous explosion outside of the outer regions

  • of the star.

  • So who's to say that some of these super heavy elements

  • aren't formed in supernovas?

  • I think they would be.

  • But would they actually make it out to be part of Earth

  • and then, let's say, live the 5 billion years that Earth's

  • been around?

  • We don't know if their half-lives are long enough.

  • There very well may have been some 5 billion years ago

  • or when the supernova was made.

  • But we haven't detected any here on Earth.

  • So we know that they're not 5 billion years stable.

  • Rather, I wouldn't even say we know that,

  • but we have a pretty good idea.

  • That's a great question is like, are they naturally made?

  • Probably.

  • Yeah.

  • Any other questions?

  • I like these outside the material ones.

  • We can take things beyond our known universe,

  • start to explain them.

The following content is provided under a Creative

字幕與單字

單字即點即查 點擊單字可以查詢單字解釋

B1 中級

5.品質拋物線的連續性、穩定性和半衰期。 (5. Mass Parabolas Continued, Stability, and Half Life)

  • 3 0
    林宜悉 發佈於 2021 年 01 月 14 日
影片單字