- Mass defect and binding energy
- Nuclear stability and nuclear equations
- Types of decay
- Writing nuclear equations for alpha, beta, and gamma decay
- Half-life and carbon dating
- Half-life plot
- Exponential decay formula proof (can skip, involves calculus)
- Exponential decay problem solving
- More exponential decay examples
- Exponential decay and semi-log plots
We can use half-lifes of radioactive substances to determine how old something is. Using your calculus skills, learn how to use the N(t)=Ne^(-kt) exponential decay equation to measure the amount of a radioactive substance we have at time T. Created by Sal Khan.
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- what is mean by lambda(13 votes)
- How did the scientists calculate the half life of an element ?(6 votes)
- We measure the decay constant, which can be done in a lab fairly easily. This is the constant we would normally use in computations, not the half-life. However, the half-life can be calculated from the decay constant as follows:
half-life = ln (2) / (decay constant).
To measure the decay constant, we take a sample of known mass and measure the number of radioactive decays per second as a function of time. Then we do a little bit of math to get the decay constant.(14 votes)
- How do people really determine the half life of elements or compounds which have have great half life periods? Like C-14, how is it really done?(8 votes)
- how did we know that there is such a thing as a half-life in the first place? as compared to say, a quartet-life or a sixtet-life? how did we realise in the very beginning that radioactive decay always conforms to such an intriguing exponential pattern that is dependent on its half-life?(1 vote)
- I did not get why the rate of decay is dependent on the amount of substance we already have. How does a nucleus "know" that it is surrounded by more nuclei and it is supposed to decay faster than another nucleus that is surrounded by lesser number of nuclei?(3 votes)
- The disintegration process is completely random. A given nucleus Doesn't know when its supposed to decay, but the rate evens out when you have billions of billions of atoms.
If you take a piece of uranium, it will decay at a certain rate.
If you divide it into two pieces but keep them together. you will still get the same number of disintegrations per second.
If you take only one piece (half the size), you will get half the disintegrations per second (the other piece is giving off the other half, but you aren't counting them).
Thus, the observed rate of decay depends on the amount of substance you have.(4 votes)
- How do you get to know which Carbon to use @ time.. C12 or C14 ?(4 votes)
- C14 is a radioactive isotope of carbon, while C12 is just a stable isotope. Only radioactive isotopes can undergo radioactive decay.(1 vote)
- why carbon 14 changed with nitrogen 14??(2 votes)
- Carbon-14 is a radioactive isotope of carbon. It has 6 protons and 8 neutrons. One of the neutrons turns into a proton by emitting an electron. The atom is now Nitrogen-14 because it has 7 protons and 7 neutrons.(3 votes)
- Is activity in Becquerels the same as the decay constant? Say I was given a radioactive compound with an activity of 10 Bq, could I just slot '10' in for lambda?(2 votes)
- No, they are not the same. The decay constant is mass independent, but the activity (which is measured in Becquerels) is not.
So, the equation is:
A (in Becquerels) = λN
where N is the number of atoms of the substance(3 votes)
- At11:28, I don't understand how Sal interpreted the answer as, 1.2 * 10^-4. Why isn't is 1.2 * e^-4?(1 vote)
- You misunderstood a common notation: 1.2e-4 means 1.2 x 10⁻⁴. You will sometimes (not commonly) see this written as 1.2EE-4
To indicate something to the power of e, you would write 1.2exp(-4) which does mean 1.2 * e⁻⁴(4 votes)
- why is e to the ln(N) equal to N?(1 vote)
- because the natural log, by definition, is the inverse of raising e to a power.
Sal has vids about logarithms that you can watch if you need to review the properties of logs.(3 votes)
- Why radioactive element take infinite time to decay? Mathematical and physical answer?(1 vote)
- Since radioactive decay is random we define the decay rate in a probabilistic way by using a half-life so you have the amount remaining R = 1/(2^n) O where O is the original amount and n is the number of half-lives.
For any positive real number for n the result will never be 0. Realistically once there have been enough half-lives that you have 1 particle left you then have a chance of that particle to not having decayed is again 1/(2^n) so you can't say that there is a point in time that you can be 100% sure that it is all decayed.(3 votes)
SAL: The notion of a half-life is useful, if we're dealing with increments of time that are multiples of a half-life. For example, where time equals zero, we have 100% of our substance. Then after time equals one half-life, we'd have 50% of our substance. At time is equal to two half-lives, we'd have 25% of our substance, and so on and so forth. So if I say that three half-lives have gone by-- in the case of carbon that would be, what, roughly 15,000 years-- I can tell you roughly, or almost exactly, what percentage of my original element I still have. In the case of carbon-14, I'll tell you what percentage of my original carbon-14 has not decayed into nitrogen, as yet, nitrogen-14. And that's useful, but what if I care about how much carbon I have after 1/2 a year, or after 1/2 a half life, or after three billion years, or after 10 minutes? What if I want a general function. A general function, as a function of time, that tells me the number, or the amount, of my decaying substance I have. So that's what we're going to do in this video. And it's going to be a little mathy, but I think the math is pretty straightforward, especially if you've taken a first-year course in calculus. And this is actually a pretty neat application of it. So let's just think a little bit about the rate of change, or the probability, or the number particles that are changing at any given time. So if we say, the difference or change in our number of particles, or the amount of particles, in any very small period of time, what's this going to be dependent on? This is the number particles we have in a given period time. This is our rate of change. So one thing, we know that our rate of change is going down. We know it's a negative number. We know that, in the case of radioactive decay, I could do the same exercise with compounding growth, where I would say, oh no, it's not a negative number, that our growth is dependent on how much we have. In this case the amount we're decaying is proportional, but it's going to be the negative of how much of the actual compound we already have. Let me explain that. So what I'm saying is, look, our amount of decay is proportional to the amount of the substance that we already are dealing with. And just to maybe make that a little bit more intuitive, imagine a situation here where you have 1 times 10 to the 9th. You have a billion carbon atoms. And let's say over here you have 1 times 10 to the 6th carbon atoms. And if you look at it at over some small period of time, let's say, if you look at it over one second, let's say our dt. dt as an infinitesimally small time, but let's say it's a change in time. It's a delta t. And let's say over one second, you observe that this sample had, I don't know, let's say you saw 1000 carbon particles. You really wouldn't see that with carbon-14, but this is just for the sake of our intuition. Let's say over one second you saw 1000 carbon particles per second here. Well here you have 1000th of the number particles in this sample as this one. So, for every thousand particles you saw decaying here, you'd really expect to see one carbon particle per second here. Just because you have a smaller amount. Now I don't know what the actual constant is. But we know that no matter what substance we're talking about, this constant is dependent on the substance. Carbon's going to be different from uranium, is going to be different from, you know, we looked at radon. They're all going to have different quantities right here. And we can see that. We'll actually do it in the next video, you can actually calculate this from the half-life. But the rate of change is always going to be dependent on the number of particles you have, right? I mean, we saw that here with half-life. When you have 1/2 the number of particles, you lose 1/2 as much. Here, if we start with 100 particles here, we went to 50 particles, then we went to 25. When you start with 50, in a period of time you lose 25. When you start with 100, you lose 50. So clearly the amount you lose is dependent on the amount you started with, right? Over any fraction of time, and here it's a very small fraction. So what I set up here is really fairly simple, but it doesn't sound so simple to a lot of people if you say it's a differential equation. We can actually solve this using pretty straightforward techniques. This is actually a separation of variables problem. And so, what can we do? Let's divide both sides by N. We want to get all the N's on this side and all the t stuff on the other side. So if we have 1 over N, dN over dt is equal to minus lambda. I just divided both sides of this by N. And then I can multiply both sides of this by dt, and I get 1 over N dN is equal to minus lambda dt. Now I can take the integral of both sides of this equation. And what do I get? What's the antiderivative? I'm taking the indefinite integral or the antiderivative. What's the antiderivative of 1 over N? Well that's the natural log of N plus some constant-- I'll just do that in blue-- plus some constant. And then that equals-- What's the antiderivative of just some constant? Well it's just that constant times the derivative, the variable. We're taking the antiderivative with respect to. So minus lambda, times t, plus some constant. These are different constants, but they're arbitrary. So if we want, we can just subtract that constant from that constant, and put them all on one side and then we just get another constant. So this boils down to our solution to our differential equation is the natural log of N is equal to minus lambda-t, plus some other constant, I call it c3, it doesn't matter. And now if we want to just make this a function of N in terms of t, let's take both of these, or both take e to the power of both sides of this. You can view that as kind of the inverse natural log. So e to the power of ln of N, ln of N is just saying what power do you raise e to to get to N? So if you raise e to that power, you get N. So I'm just raising both sides of this equation. I'm raising e to both sides of this equation. e to the ln of N is just N. And that is equal to e to the minus lambda-t, plus c3. And now this can be rewritten as, N is equal to e to the minus lambda-t, times e to the c3. And now once again this is an arbitrary constant, so we can just really rename that as, I don't know, let me rename it as c4. So, our solution to our differential equation, N, as a function of t, is equal to our c4 constant, c4e to the minus lambda-t. Now let's say, even better, let's say is N equals 0. Let's say that N equals 0. We have N sub 0 of our sample. That's how much we're starting off with. So let's see if we can substitute that into our equation to solve for c4. So we said N sub-0 is equal to, let's put 0 in here, so let's see, that's equal to N sub naught. And that's equal to c4 times e to the minus lambda, times 0. Well, minus anything times 0 is 0. So it's e to the 0. So that's just 1. So c4 is equal to N naught, our starting amount for the sample. So we've actually got an expression. We have the number of particles, or the amount as a function of t, is equal to the amount that we start off with, at time is equal to 0, times e to the minus lambda, times time. And we just have to be careful that we're always using the time constant when we solve for the different coefficients. So this seems all abstract. How does this relate to half-life? Well let's try to figure out this equation for carbon. This'll be true for anything where we have radioactive decay. If we actually had a plus sign here it'd be exponential growth as well. We know that carbon, c-14, has a 5,700-year half-life. So the way you could think about it, is if at time equals 0 you start off with t-- So time equals 0. t equals-- let me write that down. If at N of 0 is equal to-- and we could write 100 there if we want. Actually why don't we do that? If N of 0 we start off with 100. And then at N of 5,700 years-- so we're going to take t to be in years, you just have to be consistent with your units-- how much will we have left? We'll have 50 left. We could have written x and x over two here, and it would have all have worked out in the end. So let's see, let's apply that to this equation and try to solve this for lambda. So we know N of 0 is equal to 100. So we immediately know that we can write this equation as N of t is equal to 100e, to the minus lambda-t, at least in this exact circumstance. And we also know that N of 5,700-- so that means, N of 5,700-- that is equal to, we just said, that's one half-life away. So we have 1/2 as much of our compound left. That's equal to 50, which is equal to the 5,700th power times lambda. So it's equal to 100 times e, to the minus lambda, times 5,700. And now we just solve for lambda. Then we'll have a general equation for how much carbon we have at any given moment in time. So if you divide both sides of this by 100. What do we get? We get 0.5, we have 1/2, is equal to e to the-- let me just write minus 5,700 lambda, and then we could take the natural log of both sides. So then we get-- scroll down a bit-- the natural log of 1/2 is equal to the-- the natural log of this is just minus 5,700 lambda. To solve for lambda, you get lambda is equal to the natural log of 1/2, over minus 5,700. So let me see what that is. Let's see what that is. So 0.5 natural log is that, divided by minus 5,700. 5,700 negative is equal to 1.2 times 10 to the negative 4. Is equal to 1.21 times 10 to the minus 4. So there you have it, we figured out our lambda. So the general equation for how much carbon-14 we can expect at any moment in time, t, where t is in years, is N of t is equal to the amount of carbon we start off with, times e to the minus lambda. The minus lambda is 1.21 times 10 to the minus 4, times t in years. So now if you say after 1/2 a year, you just plug it in and, you have to tell me how much you started off with, and then I can tell you how much you have after 1/2 a year, or after a billion years, or after a gazillion years. And we'll do a lot more of these problems in the next video.