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So I come back to this lecture about -- potentials.

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So in the previous lecture, I have just given you the solution to this for General Maxwell's equations

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and the solutions are these -- potentials.

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But in reality, it's very difficult to find out that these are really the solutions and that this solution

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here is true.

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So this lecture is optional, and this is because you will not really learn new physics here, because

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I already told you that these are the solutions, we just have to verify it.

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And furthermore, this proof is rather difficult, mathematically speaking.

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So if you're not really that interested in the mathematics, you can go ahead and skip this video and

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go to the next video.

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But I think it's really worth the effort to go through this video because you'll learn some new cool

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tricks about mathematics.

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And we will also learn about the so-called Delta distribution, which is a very important concept in

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theoretical physics.

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So I will only prove one half of this part.

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I will only prove that this electrostatic potential with this -- time here solves this Maxwell

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equation here.

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And then afterwards, if you want, you could verify also that the vector potential solves the other

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Maxwell equation.

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But the steps on the method in terms of the mathematics, they are very similar.

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OK, so let us get started.

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So first of all, we must realize that this large class operator acting on the electrostatic potential

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is just the divergence of the gradient.

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And so we go step by step and first calculate the gradient of fire before we calculate the plaza operator.

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Now, since we have here this are ministers, other aren't here as well.

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And always we only consider distance might introduce a new variable, which just is Capital R, which

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describes this distance here.

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And of course, if I don't write it bold, not as a vector, then I mean this absolute value.

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So let us calculate the gradient of the electrostatic potential.

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So this is a pretty factor and we can also switch around the integration and the differentiation.

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So we just have to differentiate this integration to you.

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We have to calculate the gradient.

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Now, of course, here we have to are dependent terms.

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We have to charge density, which depends on R because we have here in this time argument the R and

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then we have here another R, so it's a quotient.

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Or you could also say a product of two functions that are dependent.

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Now another comment, this KNOBLER operator here, this gradient is typically with respect to this position

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vector, but since they are linear to each other, it's the same.

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If we also write it here with respect to this capital R so we can just differentiate with respect to

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this R here.

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OK, let's do this.

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So we have here this product of these two are dependent functions, so we get a sum of two terms.

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The first term here is just this one here times the derivative of one over R, so the derivative of

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one of our is of course one of our square then the minus sign.

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And we also need to consider the inner derivative, which is the gradient of our.

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Then the other term, we know we have to apply the naval operators to discharge density and just have

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to multiply by these other functions, so we have to gradient over divided by R.

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Now we have to calculate what is the gradient of our I think you know this already, but here I have

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written it down once again.

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So a comment you could do this much more elegantly if you would use spherical coordinates.

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But this in itself is also a bit difficult because then you first have to learn about spherical coordinates.

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So in principle, you can also do it in Cartesian coordinates, as you can see here.

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But then you need several steps and you need to be very, very careful that you do not miss any any

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in a derivative so that you do not miss this term here, for example.

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And you will see that this is just are divided by ah, OK.

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This means we have now this term here.

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So we still need this one, the gradient of the charge density.

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And to you we have to gradient with respect to capital R and this coordinate enters this -- time

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argument.

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So what we have to do is we have to first calculate the outer derivative which is charged density divided

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with respect to this argument.

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And then we have to multiply and calculate the inner derivative, which is the gradient of this argument.

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So we have here robots, there's just a shorthand notation, as you typically use it in physics, and

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then for the for the inner derivative, we have the gradient of the argument, which is the gradient

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of tea, which gives zero and then the gradient of minus are divided by.

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So this in a derivative is the gradient of ah and then times minus one divided by C and the gradient

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of are we know already we have it here.

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This is the vector are divided by the absolute value of R, so this is our final result for this one

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here.

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So now let's take these two terms here, this one and that one and put them into our our gradient here.

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And this is what we get for the gradient of fire.

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We get two terms and they look kind of similar.

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But here we have a dependent's one of our square until one of our to the power of three.

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And here we get a row until we get the time derivative of row.

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So this is what we have, but what we want to calculate is the plant's operator.

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So now we need to calculate the divergence of this term.

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So we have now these two terms and we need to calculate the divergence of both of these terms.

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And now, of course, you can see we have here three functions, Row R and R Square, and here also

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three functions that all depend on R.

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So we need to use the product rule many times and let us start by calculating these two terms and write

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them down.

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First of all, I used to the product rule here.

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So I write down real dot, for example.

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rawData times the divergence of dysfunction here.

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So that's done divergence of this one plus the other way around this function, then the scale of products

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times the gradient of row dot, and then similarly I do it for this term to get these two terms.

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But here we are not finished, I want to go one step further, I have to apply the product rule also

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to this term here and to this term, because here we have also the product of two are dependant functions,

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so we get even more terms.

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So, for example, from this one here, we get these two terms.

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And then from this one here, we get these two terms.

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Now, this is what we have for our the plant operator and this is what we get for the integrity.

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So now we need to simplify all of these six terms.

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So let's get started with the first term.

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Of course, here the only difficulty is calculating the divergence of R, but actually it's it's not

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at all difficult because you can imagine the operator is a vector of the partial derivatives and you

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calculate the scale of product with this position vector itself.

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So you calculate basically derivative of respect to X of X, which is one plus derivative of Y with

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respect to Y, which is one plus the derivative of Z with respect to Z, which is also one.

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So we get for this term here three.

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So the answer is three times robots divided by C are square.

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Now the second term you can see already highlighted that's red.

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So we will get a similar functional dependence.

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This a bit more difficult.

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So here we have to calculate the gradient of one of our square, which is a bit similar to what we previously

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did when we already calculated.

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So what we what we get here is first we have to construct the outer derivative, which is our to the

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power of three.

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So one divided by R to the poor three times minus two, which comes from this two here.

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But then please do not forget about the inner derivative, which is the gradient of arm.

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Now the gradient of are we have also already calculated this was the arbiter divided by R so this is

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what we get in total.

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And now you can see when we only look at these vectors here, our thoughts are, is of course the absolute

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value of our square so we can get rid of the Spectre's here and just right our square and we divide

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by our to the power of four.

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So we end up with one divided by R to the power of two.

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And then all of these three factors, of course, and you can see it's exactly the same dependence here.

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But here we have this term three times and here we have it minus two times.

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So these two will simplify already.

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Now here we get a different turn here.

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We have to calculate the gradient of DOT.

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And this is, of course, very, very simple because on the previous slide, we have already calculated

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the gradient of row.

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And so we can just take our solution from the gradient of row.

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But instead of getting here what we get now, roadable dot.

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But besides that, it's the same thing.

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And we need to consider here also this in a derivative, which is, of course, are divided by R and

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then we get here also this minus one A.

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So if you don't remember how it is done and if you can't do it yourself, just skip a few minutes back

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where we have already calculated this gradient of row.

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Now here we get the same thing.

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We get again, our dot are where we can just ride our square.

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And here in the denominator we have our to the power of two times.

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Ah.

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So we end up with one of our and then these three factors here.

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So this is a different dependent's.

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So we cannot cancel this term with the other two two terms.

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Now, here we get another term here we have to calculate again the divergence of our which is three.

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So this one is very simple.

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Here we have to calculate the Dow and sorry, the gradient of one of our to the power of three.

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So if we know what the gradient of one of our square is, we also know what the gradient of one of our

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to the power of three is.

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We just get here are to depart four instead of three, and here we get minus three instead of minus

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two, which comes, of course, from these three instead of this two.

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And then again, we have the derivative, which is the gradient of art, which simplifies to this one

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here.

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So as a total result here, we get minus three times row divided by R to the point of three.

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So you see, it's again very similar here.

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We get to minus three instead of two, minus two, and here the three instead of the two.

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And see that it's the same functional dependence as this one here.

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And in fact, these two terms even cancel out.

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So that's really cool, which means we do not have these two terms here anymore because they are exactly

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the same for the last term.

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We have something here are times the gradient of row and we already know what the gradient of row is.

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This is, of course, this minus one of a sea times.

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Roedad times are divided by are we have calculated this on the previous slide.

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So again, we get our times are, which is our square.

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So we get here from this arg to power for only are to the power of two.

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And as you can see, this term once again has the same functional dependence as these two terms here.

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And furthermore, you can see that all of these terms compensate and that all of these blue terms compensate.

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So all of these difficult looking derivation letters to one single term.

162
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So we have that the entire rent is equal to minus roadable dots divided by sea squared times are.

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So we have that our the class operator is the integral of this expression here.

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Now, what we can do next is we can write down this road double dots as the second order, time to time

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derivative, which.

166
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Yeah, second order a time derivative of rope.

167
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And we can then switch around the derivative and integration.

168
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So we write down the second or the time derivative.

169
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Of this integral of roll over are we can do this because these are here is not time dependent and Rose

170
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was the only time dependent thing in his intake around here.

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Now, another thing is that I have used this square here in the Integral and have put it outside of

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this term here.

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And so here you see, I have already introduced these two brackets to highlight this term here.

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And if you remember really well what this term was, this was our electrostatic potential from the beginning

175
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to look here.

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If you're introduced as are you get the same thing for this term and for this term here.

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So what we have here is one of a C Square, the second order time derivative of the electrostatic potential.

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So what we wanted to show is that this class operator is equal to one of us square the second or third

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time derivative of five, which is this one here.

180
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But there is this term missing here.

181
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Here.

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We wanted to also show that we have another term, which is minus one of Epsilon zero.

183
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So I think given the fact that this whole derivation was kind of difficult, it's a good first step

184
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that we have to as a result.

185
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But then again, where is this term?

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It cannot cannot be missing.

187
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And the reason why it is missing is that we made a small mistake in the derivation.

188
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So our derivation is only valid when are equal or is only valid when R is not equal to zero.

189
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This is because we divide by art in many different locations.

190
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So whenever we have divided by hour or derivation is in fact wrong, and we need to be much more careful

191
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for the case where ours is equal to zero.

192
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So now, um, what what this means is that this expression here is only true if R is different from

193
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zero.

194
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So this means if R is equal to zero, which is, of course the case, and we also have to integrate

195
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it, this means we get here additional terms that we have been lacking so far.

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And so let's go back to this slide here where I have written down all of these different terms.

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And I want to tell you which of the terms gives us additional results that we have been missing so far.

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And it turns out that all of these four terms here give us nothing new except for this single term here,

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which corresponds to these two terms.

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00:16:51,400 --> 00:16:57,220
So this term for our equals zero gives us another thing and let's look at what it is.

201
00:16:58,690 --> 00:17:06,040
So first of all, we need to, again, remind ourselves that when we straightforwardly calculate this

202
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divergence of this function here, we get these two terms and we get that at zero.

203
00:17:12,160 --> 00:17:16,090
And it's zero for every are different from zero.

204
00:17:17,910 --> 00:17:24,540
But we can also do a different thing, we can just take this term here, so not this role, but this

205
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divergence of are divided by the power of three and we integrate over the whole three dimensional space.

206
00:17:31,800 --> 00:17:38,850
And if we want to calculate this integral, we can use Goussis Theorem as we did before, and transformed

207
00:17:38,850 --> 00:17:45,090
this integration to a surface integral where we integrate not over the divergence, but just over this

208
00:17:45,090 --> 00:17:48,240
function here of our divided by our to the power of three.

209
00:17:49,110 --> 00:17:51,620
And then this one here is this.

210
00:17:52,420 --> 00:17:52,690
Yeah.

211
00:17:52,800 --> 00:18:01,110
Just this element, which is which is a surface and its orientation is normal to the surface.

212
00:18:01,830 --> 00:18:03,880
So it's always in radial direction.

213
00:18:03,900 --> 00:18:09,330
So this one here is actually parallel to our if we consider a sphere.

214
00:18:10,050 --> 00:18:15,600
So what we are doing here is we want to calculate over the whole three dimensional space, which is

215
00:18:15,600 --> 00:18:22,590
infinitely large, and then he on the right hand side, we must integrate over the surface of the three

216
00:18:22,590 --> 00:18:29,100
dimensional space, which is not really possible, of course, because what is the surface of something

217
00:18:29,100 --> 00:18:30,140
infinitely large?

218
00:18:30,930 --> 00:18:32,220
So we must use a trick here.

219
00:18:32,520 --> 00:18:40,620
We must consider a finite sphere at first and what the radius are, and then we must take the limit

220
00:18:40,620 --> 00:18:42,920
of this radius which goes to infinity.

221
00:18:43,230 --> 00:18:48,840
And if we do this, we get an infinitely large sphere, which is of course equal to this whole three

222
00:18:48,840 --> 00:18:49,740
dimensional space.

223
00:18:51,320 --> 00:18:59,880
OK, so we have transformed this one here to this one, which is with just me, which just means that

224
00:18:59,880 --> 00:19:07,860
we take a sphere, we integrate over the surface of the sphere with Radius R and afterwards we make

225
00:19:07,860 --> 00:19:09,540
the radius infinitely large.

226
00:19:10,500 --> 00:19:18,480
And then here, since we have used the sphere, now this surface element here, this orientation is

227
00:19:18,480 --> 00:19:26,490
parallel to our so we get to your unit vector R and then this is given by our square synesthete ADT

228
00:19:26,490 --> 00:19:27,450
to define.

229
00:19:30,630 --> 00:19:34,840
So now let's use this relation here that these two are parallel to each other.

230
00:19:35,190 --> 00:19:41,280
So this just gives us ah, so we get ah to the power of three divided by ah to the power of three.

231
00:19:42,390 --> 00:19:43,980
And that's the whole trick here.

232
00:19:44,800 --> 00:19:48,510
It means that our integration's is not dependent on.

233
00:19:48,510 --> 00:19:56,640
Ah, so this means it doesn't matter how large our sphere is now we can just take the limit ah to infinity

234
00:19:56,940 --> 00:20:00,560
and it will change nothing that will just give us this term here.

235
00:20:01,890 --> 00:20:04,840
And when we calculate this term, this is really easy for us.

236
00:20:04,850 --> 00:20:09,740
First, we can solve this integration with respect to PHI because there is no fi here.

237
00:20:10,170 --> 00:20:16,500
So we just get the function or we just get to the difference of this integration boundary.

238
00:20:16,530 --> 00:20:23,640
So we get two PI times this integration and this integration we can solve by.

239
00:20:24,090 --> 00:20:29,970
Yeah, calculating minus cosine theta from the uh from the boundaries.

240
00:20:30,210 --> 00:20:31,370
So zero to pi.

241
00:20:32,280 --> 00:20:38,190
And so if you do this you get minus minus one, minus minus one, so you get two.

242
00:20:38,730 --> 00:20:43,440
And so our total integral here is equal to four pi.

243
00:20:45,190 --> 00:20:46,960
So what does this mean?

244
00:20:47,380 --> 00:20:56,530
It means that this this term, he had divergence of are divided by R to the power of three is zero everywhere

245
00:20:56,530 --> 00:20:59,070
besides the position are equal to zero.

246
00:21:00,370 --> 00:21:07,180
But if we integrate this term over the whole three dimensional space, which basically means we add

247
00:21:07,180 --> 00:21:12,830
up this expression here at every possible position, it gives us four pi.

248
00:21:14,080 --> 00:21:16,630
So this means at the position R equals zero.

249
00:21:16,810 --> 00:21:24,400
There must be a very large signal or a very large term that gives rise to this integration that gives

250
00:21:24,400 --> 00:21:25,130
for PI.

251
00:21:26,710 --> 00:21:30,310
And so this is something that has bothered physicists for a long time.

252
00:21:30,310 --> 00:21:36,760
And it's really hard to comprehend because it's a bit counterintuitive that you just have a single point

253
00:21:36,760 --> 00:21:40,360
of which you integrate and you get some finite signal.

254
00:21:41,920 --> 00:21:50,170
But this has led to the introduction of the so-called Delta distribution function and this Delta distribution

255
00:21:50,170 --> 00:21:58,420
function you can write here as Delta are, and in very simple terms, which are not really correct.

256
00:21:58,420 --> 00:22:09,310
You could say that the Delta function is zero for everything different from R equals zero and it's infinitely

257
00:22:09,310 --> 00:22:11,960
large for our equals zero.

258
00:22:12,850 --> 00:22:16,540
So this means you really get only a signal from this point.

259
00:22:16,540 --> 00:22:19,980
R equals zero by this definition is not really correct.

260
00:22:20,530 --> 00:22:27,370
The real definition is that when you write it in an integral, you can get rid of the integer and just

261
00:22:27,370 --> 00:22:30,240
take this other function here that you're right as a product.

262
00:22:30,580 --> 00:22:37,480
So you take this function here, which is just for PI and take the argument are at the position zero,

263
00:22:38,080 --> 00:22:42,570
which in this case just gives for PI because there is no argument.

264
00:22:42,580 --> 00:22:44,190
Ah, OK.

265
00:22:44,200 --> 00:22:51,910
This may sound a bit confusing to you maybe, but on the next, on one of the next slides I will show

266
00:22:51,910 --> 00:22:53,640
you a bit more about the Delta distribution.

267
00:22:53,650 --> 00:23:00,490
Then this may become clearer, but the important thing is we can write down that this divergence of

268
00:23:00,490 --> 00:23:05,860
R divided by R to typeof three is given by four PI times the Delta function.

269
00:23:06,460 --> 00:23:15,550
And this also includes our previous results that for a position where R is different from zero, then

270
00:23:15,550 --> 00:23:17,230
this whole divergence is zero.

271
00:23:17,950 --> 00:23:23,230
And it also includes that when we integrate over this term, we do not get zero.

272
00:23:23,440 --> 00:23:26,730
We get a finite term, which is four pi in this case.

273
00:23:27,610 --> 00:23:35,320
So we get our new term here, which is four PI Delta times zero, which you must not forget because

274
00:23:35,320 --> 00:23:36,850
here we have to zero also.

275
00:23:38,270 --> 00:23:44,520
It's now since this Delta distribution is a bit, yeah, difficult to imagine and a bit counterintuitive,

276
00:23:44,520 --> 00:23:49,680
I think here I have prepared one more slide that I want to show you.

277
00:23:50,130 --> 00:23:57,840
And there exists some kind of continuous transformation of this function here that approximates the

278
00:23:57,840 --> 00:24:02,400
Delta distribution very well if you take the limit of eight to zero.

279
00:24:03,360 --> 00:24:10,320
So this function here is a Gorshin function, which is basically x e to the power of minus X square.

280
00:24:11,180 --> 00:24:16,650
And you have here in this argument also some parameter aid and also here you have a perimeter.

281
00:24:17,990 --> 00:24:24,260
And now if you take this parameter eight to zero, you will see that this prefecture becomes infinitely

282
00:24:24,260 --> 00:24:29,840
large and also that this Gorshin function becomes infinitely narrow.

283
00:24:30,620 --> 00:24:33,890
So those are not Desharnais animation on Wikipedia about this.

284
00:24:34,430 --> 00:24:41,060
So you can see here for smaller values of a this peak in the middle becomes larger and larger.

285
00:24:41,510 --> 00:24:47,590
And the yeah, the broadness of the Delta function also becomes more narrow.

286
00:24:48,410 --> 00:24:55,370
And the important thing is that when you take the limit to infinity, you will see that the value of

287
00:24:55,370 --> 00:24:57,470
this function here becomes zero.

288
00:24:57,680 --> 00:25:05,330
It becomes zero everywhere except for the position X equal to zero, and therefore the value will become

289
00:25:05,330 --> 00:25:06,470
infinitely large.

290
00:25:07,430 --> 00:25:14,840
And also, this may be hard to see, but maybe you can imagine this when you integrate over this area

291
00:25:14,840 --> 00:25:19,940
here below this curve, this will give you the same value for every value of a.

292
00:25:20,870 --> 00:25:27,320
So when you have some some final value of A, you can just calculate the integral and it will give you

293
00:25:27,320 --> 00:25:27,830
a number.

294
00:25:28,880 --> 00:25:34,010
Now, if you make a smaller and smaller, this this number stays the same.

295
00:25:34,700 --> 00:25:41,360
And so this means also for the limit of eight to zero, where you could say that this function is zero

296
00:25:41,360 --> 00:25:47,010
everywhere and it's infinitely large at zero, he will still get the same area.

297
00:25:47,960 --> 00:25:55,700
And so this is the whole important thing about this data distribution, that when you integrate a function

298
00:25:55,700 --> 00:26:01,690
times this Delta function or Delta distribution, then you will get a finite value.

299
00:26:02,270 --> 00:26:07,610
And in fact, you will get the value of this function at the position of zero.

300
00:26:08,810 --> 00:26:14,690
And if this data function is not centered around zero, as in this case, where it's centered around

301
00:26:14,840 --> 00:26:19,340
X zero, then you will get the function at the position X zero.

302
00:26:21,430 --> 00:26:28,360
So in our case, this is very similar here, we have an integral role like this and we have shown that

303
00:26:28,360 --> 00:26:30,760
we can transform it to this expression here.

304
00:26:31,570 --> 00:26:38,320
So this means when we integrate over this function, which is just four PI times Delta distribution,

305
00:26:38,680 --> 00:26:41,880
we get this function at the position are equals zero.

306
00:26:42,310 --> 00:26:47,130
And since this does not have any dependence, we just get for PI.

307
00:26:48,010 --> 00:26:54,740
And so this means we can really express this divergence here in terms of this Delta function.

308
00:26:57,350 --> 00:27:04,600
OK, that was really difficult, but this is only one of two occasions where we will use the Delta distribution

309
00:27:04,600 --> 00:27:05,900
throughout this whole course.

310
00:27:06,340 --> 00:27:12,130
So this is why I decided to not spend too much time on the Delta distribution, because for our purposes,

311
00:27:12,130 --> 00:27:13,740
it's not that important.

312
00:27:14,350 --> 00:27:21,250
We could say it's for us just a mathematical trick to write down the things in an elegant way.

313
00:27:22,170 --> 00:27:28,140
But what's important is that, you know, what this Delta function does, and this is when you integrate

314
00:27:28,140 --> 00:27:31,020
over overhead, you get a finite value.

315
00:27:32,430 --> 00:27:38,850
OK, so we have now here over the plant operator and we have transformed our integrations and have found

316
00:27:38,850 --> 00:27:45,690
that it's actually not just a single term, but that there is another term which becomes only important

317
00:27:45,690 --> 00:27:47,310
when R is equal to zero.

318
00:27:49,110 --> 00:27:55,050
So this means when we write it down like this, we get to hear this new term, previously we only had

319
00:27:55,050 --> 00:27:59,430
this term and this term transformed to this term here.

320
00:27:59,460 --> 00:28:00,600
We have shown this already.

321
00:28:01,680 --> 00:28:07,140
Now, the other term here, we have this Delta distribution.

322
00:28:08,270 --> 00:28:12,560
And on the previous slide, we have already learned what the standard distribution does.

323
00:28:13,630 --> 00:28:24,460
It sets the the argument are to this argument are with this dash here, so this means as the integral

324
00:28:24,460 --> 00:28:34,840
here, we get this function, which is for pay roll at or for the case where R is equal to this are

325
00:28:34,840 --> 00:28:35,210
here.

326
00:28:35,770 --> 00:28:44,260
So this means we get no here an hour and we get here a zero, which means we have finally got rid of

327
00:28:44,260 --> 00:28:45,550
the retardation effect.

328
00:28:46,300 --> 00:28:54,580
So this means this integral here is for Pirjo and the arguments are R and T now these four pieces here,

329
00:28:54,580 --> 00:29:03,490
they cancel out and we just get minus one of Epsilon zero zero of our N t and this is exactly this term

330
00:29:03,490 --> 00:29:04,690
here that was missing.

331
00:29:06,130 --> 00:29:12,340
Sort of all this means after this long time, after this difficult lecture, we have finally proven

332
00:29:12,700 --> 00:29:18,120
that indeed this -- scalar potential solves this Maxwell equation.

333
00:29:19,180 --> 00:29:21,640
And now I told you, it is already in the beginning.

334
00:29:22,090 --> 00:29:26,130
You can do a very similar derivation for the vector potential.

335
00:29:27,190 --> 00:29:29,260
So the mathematics is really similar.

336
00:29:29,620 --> 00:29:35,860
But again, it's quite an effort, maybe even more, because this is here a vector and this was only

337
00:29:35,860 --> 00:29:36,400
a scalar.

338
00:29:36,970 --> 00:29:41,500
But I think if you really take your time, you could do it yourself.

339
00:29:41,500 --> 00:29:45,520
If you follow along the steps that I have just shown you for this Caillat potential.
