Chapter 7

Rutherford’s Scattering Formula

The experiment told us how the scattered α particles are distributed. Here we derive that distribution from the Schrödinger equation, extended to three dimensions, and compare the result with the measurements.

The Schrödinger equation in three dimensions and probability flux.

The Schrödinger equation in three dimensions can be obtained by retracing exactly the same steps we followed to obtain the one-dimensional one, with the only nuisance of having to use a somewhat heavier formalism. The result is formally analogous:

iddtψ=Hψi\hbar\frac{d}{dt}|\psi\rangle=H|\psi\rangle

with

H=qV(X,Y,Z)+12m(Px2+Py2+Pz2)H=qV(X,Y,Z)+\frac{1}{2m}(P_x^2+P_y^2+P_z^2)
Px=iDxi/xP_x=-i\hbar D_x\equiv-i\hbar\,\partial/\partial x, similarly for yy and zz

and

ψψ(x,y,z,t)|\psi\rangle\equiv\psi(x,y,z,t)

The operator V(X,Y,Z)V(X,Y,Z) is defined on the basis of the Taylor formula for functions of several variables and in practice one has V(X,Y,Z)ψV(x,y,z)ψ(x,y,z,t)V(X,Y,Z)|\psi\rangle\leftrightarrow V(x,y,z)\psi(x,y,z,t).

The function ψ(x,y,z,t)\psi(x,y,z,t) is a vector in “3\infty^3 dimensions” that depends on time. We have in fact three indices corresponding to three observable quantities, that is, the three coordinates that identify the position of the particle. So one can say that the function ψ(x,y,z,t)\psi(x,y,z,t) is the distribution of probability amplitudes for the triple of random variables (x,y,z)(x,y,z); the dependence on time indicates that the distribution can vary with time. If we want to calculate the probability distribution we must take the squared moduli:

p(x,y,z,t)=ψ(x,y,z,t)2=ψ(x,y,z,t)ψ(x,y,z,t)\begin{aligned} p(x,y,z,t) & =|\psi(x,y,z,t)|^2 \\ & =\psi^*(x,y,z,t)\psi(x,y,z,t) \end{aligned}

For example, if we consider a volume Ω and want to determine the probability that the particle is found in the volume Ω, then we must compute the integral:

Ωp(x,y,z,t)dxdydz=Ωψ(x,y,z,t)ψ(x,y,z,t)dxdydz\iiint_\Omega p(x,y,z,t)\:dxdydz=\iiint_\Omega\psi^*(x,y,z,t)\psi(x,y,z,t)\:dxdydz

In general, when we have a distribution of a certain physical quantity — for example mass or charge — we also have the flux-density vector of that same quantity, for example the mass-flux-density vector or the charge-flux-density vector. In our case we have a probability distribution, and we expect that a probability-flux-density vector can be defined such that a continuity equation holds, similar to the one valid for any other physical quantity:

ddtΩpdΩ=ΣΩsn^dΣ-\frac{d}{dt}\iiint_\Omega p\:d\Omega=\oiint_{\Sigma_\Omega}\overline{s}\cdot\hat{n}\:d\Sigma

That is, the decrease of the probability contained in Ω equals the outgoing flux of the probability-flux-density vector s\overline{s} through the surface ΣΩ\Sigma_\Omega that bounds the volume Ω.

As is well known, this equation can also be written in differential form:

pt=s=sxx+syy+szz\begin{aligned} -\frac{\partial p}{\partial t} & =\nabla\cdot\overline{s} \\ & =\frac{\partial s_x}{\partial x}+\frac{\partial s_y}{\partial y}+\frac{\partial s_z}{\partial z} \end{aligned}

Now, on the basis of the Schrödinger equation and the continuity equation, let us try to find an explicit formula for s\overline{s}:

t(ψψ)=ψψtψψt=ψψtψ(ψt)\begin{aligned} -\frac{\partial}{\partial t}(\psi^*\psi) & =-\psi^*\frac{\partial\psi}{\partial t}-\psi\frac{\partial\psi^*}{\partial t} \\ & =-\psi^*\frac{\partial\psi}{\partial t}-\psi{\left(\frac{\partial\psi}{\partial t}\right)}^* \end{aligned}

On the basis of the Schrödinger equation we can write

ψt=iHψ=i(qV+12mP2)ψ=i(qV22m2)ψsubstituting P=i=iqVψ+i2m2ψ\begin{aligned} \frac{\partial\psi}{\partial t} & =-\frac{i}{\hbar}H\psi \\ & =-\frac{i}{\hbar}\left(qV+\frac{1}{2m}{\overline{P}}^2\right)\psi \\ & =-\frac{i}{\hbar}\left(qV-\frac{\hbar^2}{2m}\nabla^2\right)\psi && \text{substituting }\overline{P}=-i\hbar\nabla \\ & =-\frac{i}{\hbar}qV\psi+\frac{i\hbar}{2m}\nabla^2\psi \end{aligned}

Substituting, we have

t(ψψ)=ψ(iqVψ+i2m2ψ)ψ(iqVψ+i2m2ψ)=ψ(iqVψ+i2m2ψ)ψ(iqVψi2m2ψ)=iψqVψi2mψ2ψiψqVψ+i2mψ2ψ=i2m(ψ2ψψ2ψ)=imiIm{ψ2ψ}=mIm{ψ2ψ}=mIm{ψ2ψ}\begin{aligned} -\frac{\partial}{\partial t}(\psi^*\psi) & =-\psi^*\left(-\frac{i}{\hbar}qV\psi+\frac{i\hbar}{2m}\nabla^2\psi\right)-\psi{\left(-\frac{i}{\hbar}qV\psi+\frac{i\hbar}{2m}\nabla^2\psi\right)}^* \\ & =-\psi^*\left(-\frac{i}{\hbar}qV\psi+\frac{i\hbar}{2m}\nabla^2\psi\right)-\psi\left(\frac{i}{\hbar}qV\psi^*-\frac{i\hbar}{2m}\nabla^2\psi^*\right) \\ & =\frac{i}{\hbar}\psi^*qV\psi-\frac{i\hbar}{2m}\psi^*\nabla^2\psi-\frac{i}{\hbar}\psi qV\psi^*+\frac{i\hbar}{2m}\psi\nabla^2\psi^* \\ & =\frac{i\hbar}{2m}\left(\psi\nabla^2\psi^*-\psi^*\nabla^2\psi\right) \\ & =\frac{i\hbar}{m}i\operatorname{Im}\left\{\psi\nabla^2\psi^*\right\} \\ & =-\frac{\hbar}{m}\operatorname{Im}\left\{\psi\nabla^2\psi^*\right\} \\ & =\frac{\hbar}{m}\operatorname{Im}\left\{\psi^*\nabla^2\psi\right\} \end{aligned}

By the product rule for derivatives we can write

(ψψ)=ψ2ψ+ψψ=ψ2ψ+ψ2\begin{aligned} \nabla\cdot(\psi^*\nabla\psi) & =\psi^*\nabla^2\psi+\nabla\psi^*\cdot\nabla\psi \\ & =\psi^*\nabla^2\psi+|\nabla\psi|^2 \end{aligned}

Taking the imaginary part of both sides we have the equality

Im{(ψψ)}=Im{ψ2ψ}+Imψ2=Im{ψ2ψ}\begin{aligned} \operatorname{Im}\left\{\nabla\cdot\left(\psi^*\nabla\psi\right)\right\} & =\operatorname{Im}\left\{\psi^*\nabla^2\psi\right\}+\operatorname{Im}{\left|\nabla\psi\right|}^2 \\ & =\operatorname{Im}\left\{\psi^*\nabla^2\psi\right\} \end{aligned}

Substituting the term Im{ψ2ψ}\operatorname{Im}\{\psi\nabla^2\psi^*\} into the formula for (ψψ)/t\partial(\psi^*\psi)/\partial t we have

t(ψψ)=mIm{(ψψ)}=[mIm{ψψ}]\begin{aligned} -\frac{\partial}{\partial t}(\psi^*\psi) & =\frac{\hbar}{m}\operatorname{Im}\left\{\nabla\cdot(\psi^*\nabla\psi)\right\} \\ & =\nabla\cdot\left[\frac{\hbar}{m}\operatorname{Im}\left\{\psi^*\nabla\psi\right\}\right] \end{aligned}

Comparing this last one with the continuity equation in local form (ψψ)/t=p/t=s-\partial(\psi^*\psi)/\partial t=-\partial p/\partial t=\nabla\cdot\overline{s}, we can extrapolate a possible formula for s\overline{s}:

s=mIm{ψψ}\overline{s}=\frac{\hbar}{m}\operatorname{Im}\{\psi^*\nabla\psi\}

To better understand the analytical meaning of this formula, let us try to express the complex function ψ\psi in terms of modulus and phase: ψ=peiφ\psi=\sqrt{p}e^{i\varphi}. Substituting into the formula for s\overline{s} we have:

s=mIm{ψψ}=mIm{peiφ(peiφ)}=\begin{aligned} \overline{s} & =\frac{\hbar}{m}\operatorname{Im}\left\{\psi^*\nabla\psi\right\} \\ & =\frac{\hbar}{m}\operatorname{Im}\left\{\sqrt{p}e^{-i\varphi}\nabla\left(\sqrt{p}e^{i\varphi}\right)\right\}= \end{aligned}

=mIm{peiφ[eiφ(p)+p(eiφ)]}=mIm{p(p)+peiφ(eiφ)}==-\frac{\hbar}{m}\operatorname{Im}\left\{\sqrt{p}e^{-i\varphi}\left[e^{i\varphi}\nabla\left(\sqrt{p}\right)+\sqrt{p}\nabla\left(e^{i\varphi}\right)\right]\right\}=-\frac{\hbar}{m}\operatorname{Im}\left\{\sqrt{p}\nabla\left(\sqrt{p}\right)+pe^{-i\varphi}\nabla\left(e^{i\varphi}\right)\right\}=The underlined term simplifies because it is purely real

=mpIm{eiφ(eiφ)}applying the formula for the derivative=mpIm{eiφdeiφdφφ}=mpIm{eiφ(ieiφ)φ}=mpIm{iφ}=mpφ\begin{aligned} & \\ & =\frac{\hbar}{m}p\operatorname{Im}\{e^{-i\varphi}\nabla(e^{i\varphi})\} && \text{applying the formula for the derivative} \\ & =\frac{\hbar}{m}p\operatorname{Im}\left\{e^{-i\varphi}\frac{de^{i\varphi}}{d\varphi}\nabla\varphi\right\} \\ & =\frac{\hbar}{m}p\operatorname{Im}\{e^{-i\varphi}(ie^{i\varphi})\nabla\varphi\} \\ & =\frac{\hbar}{m}p\operatorname{Im}\{i\nabla\varphi\} \\ & =\frac{\hbar}{m}p\nabla\varphi \end{aligned}

So we can write

s=mIm{ψψ}=mpφ\begin{aligned} \overline{s} & =\frac{\hbar}{m}\operatorname{Im}\{\psi^*\nabla\psi\} \\ & =\frac{\hbar}{m}p\nabla\varphi \end{aligned}

This last formula shows us that the probability-flux-density vector at a given point is proportional to the probability density at that point and to the gradient of the phase φ\varphi of the distribution of probability amplitudes.

Rutherford's scattering formula.

Consider an α particle that strikes a gold foil, and suppose we want to determine the probability distribution p(ϑ)p(\vartheta) that the particle is deflected through an angle ϑ.

First of all we observe that there can be no diffraction phenomena, because the wavelength associated with an α particle is much smaller than the interatomic distance of the crystal lattice of gold; indeed:

pλ=hλ=hp=hmv\begin{aligned} p\lambda & =h\Rightarrow \\ \lambda & =\frac{h}{p} \\ & =\frac{h}{mv} \end{aligned}

substituting the values h=6.61034 joule×sh=6.6\cdot10^{-34}\ \text{joule}\times s, m=6.71027kgm=6.7\cdot10^{-27}\:\text{kg} and v=1.6107 m/sv=1.6\cdot10^7\ \mathrm{m}/\mathrm{s}

λ=6.610346.71027×1.61070.61014m<<1010m\begin{aligned} \lambda & =\frac{6.6\cdot10^{-34}}{6.7\cdot10^{-27}\times1.6\cdot10^7} \\ & \cong0.6\cdot10^{-14}\:m<<10^{-10}\:m \end{aligned}

To set up the scattering problem with the Schrödinger equation we would have to specify the initial “wave packet”, that is, the initial distribution of probability amplitudes ψt0=ψ(x,y,z,t0)|\psi t_0\rangle=\psi(x,y,z,t_0), and moreover we would have to specify the electric potential V(x,y,z)V(x,y,z) present inside the gold foil.

We note that already at this point we have made a considerable simplification; indeed the gold foil is a complex system made of an aggregate of gold nuclei and electrons. Despite this simplification the problem remains very complicated and we must find a strategy to get around it.

Experimentally we saw that almost all the particles undergo small deflections (say, less than 15°), while only a small percentage undergoes larger deflections. This means that it is very improbable to have a “close collision”, that is, it is very improbable that the wave packet passes close enough to a nucleus to be deflected by an angle greater than 15°.

We can conclude that, if it is improbable to have a collision with a deflection angle greater than 15°, then it is even more improbable that there are two consecutive collisions both with an angle greater than 15°. So we can assume that the particles deflected at large angles undergo a single collision while crossing the gold foil. More correctly, we can say that they undergo a single collision of significant magnitude, plus many small collisions with zero average effect.

On the basis of the previous hypothesis we will study the scattering due to a single atom, and we will compare the theoretical and experimental results only for large angles.

To set up the problem it remains to define the initial wave packet. The simplest condition is to assume that a plane wave of the type ei(kzωt)e^{i(kz-\omega t)} comes from the direction Z=Z=-\infty. After determining the solution in this particular case, we can use the linearity of the Schrödinger equation and build other solutions by superposing those already found. In particular, by suitably choosing the superposition, we can obtain the solution for any initial packet; indeed Fourier's theorem guarantees that any complex function can be obtained as a superposition of functions of the type eikxe^{ikx}, eikye^{iky} and eikze^{ikz}.

Now let us do the calculations:

We must solve the Schrödinger equation with the condition that

ψ(x,y,z,t)z    ei(kzωt)\psi(x,y,z,t)\to_{z\to-\infty\;}^{\;}e^{i(kz-\omega t)}

First of all we observe that it must be ω=k2/2m\omega=\hbar k^2/2m because the function ei(kzωt)e^{i(kz-\omega t)} must satisfy the Schrödinger equation in the space zz\to-\infty where V=0V=0

itei(kzωt)=22m2ei(kzωt)i(iω)ei(kzωt)=22m(ik)2ei(kzωt)ω=2k22mω=k22m\begin{aligned} i\hbar\frac{\partial}{\partial t}e^{i(kz-\omega t)} & =-\frac{\hbar^2}{2m}\nabla^2e^{i(kz-\omega t)}\Longleftrightarrow \\ i\hbar(-i\omega)e^{i(kz-\omega t)} & =-\frac{\hbar^2}{2m}(ik)^2e^{i(kz-\omega t)}\Longleftrightarrow \\ \hbar\omega & =\frac{\hbar^2k^2}{2m}\Longleftrightarrow \\ \omega & =\frac{\hbar k^2}{2m} \end{aligned}

Now, to solve our problem, let us try to separate the space variables from the time variables with functions of the type ψ(x,y,z,t)=ψ(x,y,z)eiωt\psi(x,y,z,t)=\psi(x,y,z)e^{-i\omega t}; substituting into the Schrödinger equation we have:

itψeiωt=qVψeiωt22m2ψeiωti\hbar\frac{\partial}{\partial t}\psi e^{-i\omega t}=qV\psi e^{-i\omega t}-\frac{\hbar^2}{2m}\nabla^2\psi e^{-i\omega t}\Leftrightarrow
iψ(iω)eiωt=qVψeiωt22m(2ψ)eiωtωψ=qVψ22m2ψ\begin{aligned} \Leftrightarrow i\hbar\psi(-i\omega)e^{-i\omega t} & =qV\psi e^{-i\omega t}-\frac{\hbar^2}{2m}(\nabla^2\psi)e^{-i\omega t}\Leftrightarrow \\ \hbar\omega\psi & =qV\psi-\frac{\hbar^2}{2m}\nabla^2\psi\Leftrightarrow \end{aligned}2ψ+2mωψ=2mq2Vψ2ψ+k2ψ=2mq2Vψwith ω=k22m\begin{aligned} \Leftrightarrow\nabla^2\psi+\frac{2m\omega}{\hbar}\psi & =\frac{2mq}{\hbar^2}V\psi \\ \nabla^2\psi+k^2\psi & =\frac{2mq}{\hbar^2}V\psi && \text{with }\omega=\frac{\hbar k^2}{2m} \end{aligned}

So we must solve the problem:

{2ψ+k2ψ=2mq2Vψwith ψ(x,y,z)zeikz\left\{\begin{gathered}\nabla^2\psi+k^2\psi=\frac{2mq}{\hbar^2}V\psi \\\text{with }\psi(x,y,z)\underset{z\to-\infty}{\longrightarrow}e^{ikz}\end{gathered}\right.

The equation of this problem cannot be solved in analytical form, so we will find an approximate solution using an iterative method.

First we choose a function ψ0\psi_0 that approximates the equation and the boundary condition well. Then we substitute this function into the right-hand side of the equation and solve for the unknown that has remained on the left-hand side:

2ψ+k2ψ=2mq2Vψ0\nabla^2\psi+k^2\psi=\frac{2mq}{\hbar^2}V\psi_0

In this way we find a first solution ψ1\psi_1; to proceed we substitute ψ1\psi_1 into the right-hand side and find a second solution ψ2\psi_2. One proceeds by iterating this operation until a satisfactory approximation is reached.

Actually we perform only one step and as the initial function we choose ψ0(x,y,z)=eikz\psi_0(x,y,z)=e^{ikz}. So we have:

{2ψ+k2ψ=2mq2V(r)eikzwith ψ(x,y,z)zeikz\left\{\begin{gathered}\nabla^2\psi+k^2\psi=\frac{2mq}{\hbar^2}V(r)e^{ikz} \\\text{with }\psi(x,y,z)\underset{z\to-\infty}{\longrightarrow}e^{ikz}\end{gathered}\right.

The general solution of this problem is (see appendix 1):

ψ(r)=eikz14πAll Spaceeikrrrr2mq2V(r)eikzdΩ\psi(\vec{r})=e^{ikz}-\frac{1}{4\pi}\iiint_{\text{All Space}}\frac{e^{ik|\vec{r}-\vec{r}{\:}'|}}{|\vec{r}-\vec{r}{\:}'|}\frac{2mq}{\hbar^2}V(r')e^{ikz'}\:d\Omega'

The term V(r)V\left(r\right) vanishes far from the nucleus, so it is as if the integral were extended to a limited neighbourhood; on the other hand, the points r\overline{r} at which we are interested in determining the solution are very far from the atom, so we can say that rrr\gg r'. On the basis of these considerations we can approximate the term rr|\vec{r}-{\vec{r}}'|. For the denominator we can write rrr\left|\vec{r}-\vec{r}{\:}'\right|\cong r; while for the argument of the exponential we can write rrrrr^\left|\overline{r}-{\overline{r}}'\right|\cong r-{\overline{r}}'\cdot\hat{r} (fig. 15).

Geometry of the scattering.
Fig. 15Geometry of the scattering.

Moreover we can write z=rz^z'=\overline{r}\cdot\hat{z}.

Substituting these expressions we have:

ψ(r)=eikz14πAll Spaceeik(rrr^)r2mq2V(r)eikrz^dΩ=eikzmq2π2eikrrAll Spaceeikr(z^r^)V(r)dΩ\begin{aligned} \psi(\vec{r}) & =e^{ikz}-\frac{1}{4\pi}\iiint_{\text{All Space}}\frac{e^{ik(r-{\vec{r}}'\cdot\hat{r})}}{r}\frac{2mq}{\hbar^2}V(r')e^{ik{\vec{r}}'\cdot\hat{z}}\:d\Omega' \\ & =e^{ikz}-\frac{mq}{2\pi\hbar^2}\frac{e^{ikr}}{r}\iiint_{\text{All Space}}e^{ik{\vec{r}}'\cdot(\hat{z}-\hat{r})}V(r')\:d\Omega' \end{aligned}

To compute the integral we must choose a coordinate system; the most sensible choice is a polar coordinate system (α,β,r)(\alpha,\beta,r'), with the axis in the direction z^r^\hat{z}-\hat{r}. Indeed, in this way we have r(z^r^)=rz^r^cosαr'\cdot\left(\hat{z}-\hat{r}\right)=r'|\hat{z}-\hat{r}|\cos\alpha, and since z^r^=2sinϑ2|\hat{z}-\hat{r}|=2\sin\frac{\vartheta}{2} we can write the integral in the form:

All Spaceeikr(z^r^)V(r)dΩ=02πdβ0πdα0+e2ikrcosαsinϑ2V(r)r2sinαdr\begin{aligned} & \iiint_{\text{All Space}}e^{ikr'\cdot(\hat{z}-\hat{r})}V(r')d\Omega' \\ & \qquad=\int_0^{2\pi}d\beta\int_0^\pi d\alpha\int_0^{+\infty}e^{2ikr'\cos\alpha\sin\frac{\vartheta}{2}}V(r')r^{'2}\sin\alpha dr' \end{aligned}

The integrand does not contain the variable β, so the integration with respect to β is trivial and gives a term 2π. The integration with respect to α is done by substitution, setting y=cosαdy=sinαdαy=\cos\alpha\Rightarrow dy=-\sin\alpha\:d\alpha; in this way we have:

2π11dy0+e2ikrysinϑ2V(r)r2dr=2π0+e2ikrsinϑ2e2ikrsinϑ22ikrsinϑ2V(r)r2dr=2π0+sin  (2krsinϑ2)ksinϑ2V(r)rdr=2πksinϑ20+sin  (2krsinϑ2)V(r)rdr\begin{aligned} & -2\pi\int_1^{-1}dy\int_0^{+\infty}e^{2ikr'y\sin\frac{\vartheta}{2}}V(r')r^{'2}dr' \\ & \qquad=2\pi\int_0^{+\infty}\frac{e^{2ikr'\sin\frac{\vartheta}{2}}-e^{-2ikr'\sin\frac{\vartheta}{2}}}{2ikr'\sin\frac{\vartheta}{2}}V(r')r^{'2}dr' \\ & \qquad=2\pi\int_0^{+\infty}\frac{\sin\;\left(2kr'\sin\frac{\vartheta}{2}\right)}{k\sin\frac{\vartheta}{2}}V(r')r'dr' \\ & \qquad=\frac{2\pi}{k\sin\frac{\vartheta}{2}}\int_0^{+\infty}\sin\;\left(2kr'\sin\frac{\vartheta}{2}\right)V(r')r'dr' \end{aligned}

At this point, to complete the calculation of the integral, we must introduce the potential V(r)V(r). We could insert V(r)=Q/(4πε0r)V(r')=Q/(4\pi\varepsilon_0 r'), where ϱ\varrho is the charge of the nucleus, but in this way we obtain an “oscillating” integral that cannot be computed; this problem arises because we placed ourselves in an ideal situation when we considered a plane wave as the incident packet. However, this difficulty is easily overcome if one considers V(r)=Qer/a/(4πε0r)V(r')=Qe^{-r'/a}/(4\pi\varepsilon_0 r'); in this formula the exponential represents the screening effect due to the charge of the electrons, and a is the radius of the “electron cloud”. Actually the screening effect should be determined with precise calculations, but in any case the exponential approximation is very good, and moreover the result does not change much if we choose other forms.

Substituting the formula for the potential we have:

12ε0ksinϑ20+sin(2krsinϑ2)Qrerardr=Q2ε0ksinϑ20+sin(2krsinϑ2)eradr=Q2ε0ksinϑ22ksinϑ2(2ksinϑ2)2+(1a)2=Q/ε0(2ksinϑ2)2+(1a)2\begin{aligned} & \frac{1}{2\varepsilon_0k\sin\frac{\vartheta}{2}}\int_0^{+\infty}\sin\left(2kr'\sin\frac{\vartheta}{2}\right)\frac{Q}{r'}e^{-\frac{r'}{a}}r'dr' \\ & \qquad=\frac{Q}{2\varepsilon_0k\sin\frac{\vartheta}{2}}\int_0^{+\infty}\sin\left(2kr'\sin\frac{\vartheta}{2}\right)e^{-\frac{r'}{a}}dr' \\ & \qquad=\frac{Q}{2\varepsilon_0k\sin\frac{\vartheta}{2}}\frac{2k\sin\frac{\vartheta}{2}}{{\left(2k\sin\frac{\vartheta}{2}\right)}^2+{\left(\frac{1}{a}\right)}^2} \\ & \qquad=\frac{Q/\varepsilon_0}{{\left(2k\sin\frac{\vartheta}{2}\right)}^2+{\left(\frac{1}{a}\right)}^2} \end{aligned}

Since k=2πλ1ak=\frac{2\pi}{\lambda}\gg\frac{1}{a} we can neglect the term (1a)2{\left(\frac{1}{a}\right)}^2 in the denominator and obtain for the integral the formula:

=Q4ε0k2sin2ϑ2\iiint=\frac{Q}{4\varepsilon_0k^2\sin^2\frac{\vartheta}{2}}

Substituting into the formula for ψ\psi we have:

ψ(r)=eikzmq2π2eikrrQ4ε0k2sin2ϑ2=eikzmqQ8πε02k21sin2ϑ2eikrr\begin{aligned} \psi(\vec{r}) & =e^{ikz}-\frac{mq}{2\pi\hbar^2}\frac{e^{ikr}}{r}\frac{Q}{4\varepsilon_0k^2\sin^2\frac{\vartheta}{2}} \\ & =e^{ikz}-\frac{mqQ}{8\pi\varepsilon_0\hbar^2k^2}\frac{1}{\sin^2\frac{\vartheta}{2}}\frac{e^{ikr}}{r} \end{aligned}

At this point we have determined the distribution of probability amplitudes; now we must interpret it and calculate the probability flux.

Originally we had a plane wave coming from the direction Z=Z=-\infty; the result, as figure 16 shows, is a plane wave going towards Z=+Z=+\infty plus a diverging spherical wave whose amplitude depends on the angle ϑ.

Incident plane wave → plane wave plus outgoing spherical wave.
Fig. 16Incident plane wave → plane wave plus diverging spherical wave.

In physical reality we will not have an infinitely extended plane wave but, as figure 17 shows, a narrow beam, very similar to a plane wave, but with a finite transverse size.

A narrow beam: only the spherical wave reaches the detector.
Fig. 17A narrow beam: only the spherical wave reaches the detector.

Under these conditions only the spherical wave can reach the detector, so it is only the spherical wave that we must consider to calculate the probability flux.

Now we move on to the calculation of the flux by means of the formula s=mpφ=mψψφ\overline{s}=\frac{\hbar}{m}p\nabla\varphi=\frac{\hbar}{m}\psi^*\psi\nabla\varphi. The phase φ is the one found in the term eikre^{ikr} and is φ=kr\varphi=kr, so we have φ=r^(kr)/r=r^k\nabla\varphi=\hat{r}\,\partial(kr)/\partial r=\hat{r}k.

Substituting the various terms into the formula, we obtain for the modulus of the scattered flux-density vector:

sd=mψψφ=m(mqQ8πε02k21sin2ϑ2eikrr)(mqQ8πε02k21sin2ϑ2eikrr)k=mq2Q264π2ε023k31sin4ϑ21r2\begin{aligned} s_d & =\frac{\hbar}{m}\psi^*\psi\nabla\varphi \\ & =\frac{\hbar}{m}{\left(-\frac{mqQ}{8\pi\varepsilon_0\hbar^2k^2}\frac{1}{\sin^2\frac{\vartheta}{2}}\frac{e^{ikr}}{r}\right)}^*\left(-\frac{mqQ}{8\pi\varepsilon_0\hbar^2k^2}\frac{1}{\sin^2\frac{\vartheta}{2}}\frac{e^{ikr}}{r}\right)k \\ & =\frac{mq^2Q^2}{64\pi^2\varepsilon_0^2\hbar^3k^3}\frac{1}{\sin^4\frac{\vartheta}{2}}\frac{1}{r^2} \end{aligned}

For the incident flux density due to the wave eikze^{ikz} we have:

si=meikzeikzzkz=mk\begin{aligned} s_i & =\frac{\hbar}{m}e^{ikz}e^{-ikz}\frac{\partial}{\partial z}kz \\ & =\frac{\hbar}{m}k \end{aligned}

The scattered flux density for a unit incident flux density is given by the ratio:

sdsi=m2q2Q264π2ε024k41sin4ϑ21r2\frac{s_d}{s_i}=\frac{m^2q^2Q^2}{64\pi^2\varepsilon_0^2\hbar^4k^4}\frac{1}{\sin^4\frac{\vartheta}{2}}\frac{1}{r^2}

If we multiply this term by a surface dS we obtain the flux through dS. If we want to calculate the flux associated with a solid angle dΩ we must consider the surface subtended by the angle dΩ, which is dS=r2dΩdS=r^2d\Omega. So the flux entering dΩ is:

wdΩ=m2q2Q264π2ε024k41sin4ϑ21𝔯2dS=m2q2Q264π2ε024k41sin4ϑ21𝔯2r2dΩ=m2q2Q264π2ε024k41sin4ϑ2dΩ\begin{aligned} wd\Omega & =\frac{m^2q^2Q^2}{64\pi^2\varepsilon_0^2\hbar^4k^4}\frac{1}{\sin^4\frac{\vartheta}{2}}\frac{1}{𝔯^2}\:dS \\ & =\frac{m^2q^2Q^2}{64\pi^2\varepsilon_0^2\hbar^4k^4}\frac{1}{\sin^4\frac{\vartheta}{2}}\frac{1}{𝔯^2}\:r^2d\Omega \\ & =\frac{m^2q^2Q^2}{64\pi^2\varepsilon_0^2\hbar^4k^4}\frac{1}{\sin^4\frac{\vartheta}{2}}d\Omega \end{aligned}

If we substitute k=2πλ=2π(h/p)=2πhp=p=mvk=\frac{2\pi}{\lambda}=\frac{2\pi}{(h/p)}=\frac{2\pi}{h}p=\frac{p}{\hbar}=\frac{mv}{\hbar} we obtain Rutherford's scattering formula:

w=q2Q2/(64π2ε02m2v4sin4(ϑ/2))w=q^2Q^2/(64\pi^2\varepsilon_0^2m^2v^4\sin^4(\vartheta/2))

This formula gives us the scattered flux density per solid angle, from a single atom, when the incident flux has unit density.

Comparison between theory and experiment.

First of all we observe that Rutherford's formula diverges for ϑ=0\vartheta=0, so for small angles there can be no experimental agreement; we expected this because we made approximations valid only for fairly large angles.

As for the dependence on 1/sin4(ϑ/2)1/\sin^4(\vartheta/2), figures 18 and 19 report the comparison between the values obtained experimentally and those calculated with the suitably scaled formula; figure 18 is on a linear scale, while figure 19 is on a logarithmic scale; the circles represent the measured points and the triangles represent the calculated points.

Comparison of measurement and theory on a linear scale.
Fig. 18Comparison between measurements and theory on a linear scale.
Comparison of measurement and theory on a logarithmic scale.
Fig. 19Comparison between measurements and theory on a logarithmic scale.

As can be seen, there is agreement for angles greater than 10°.

Now we will see how the nuclear charge can be determined by applying the complete Rutherford formula w=q2Q2/(64π2ε02m2v4sin4(ϑ/2))w=q^2Q^2/(64\pi^2\varepsilon_0^2m^2v^4\sin^4(\vartheta/2)).

As we have already said, this formula gives us the distribution of the probability flux, scattered by a single atom and for a unit incident flux density. To apply it to our case we must first multiply it by the actual flux density, and then multiply it by the actual number of atoms that contribute to the scattering process:

wEffective=(Effective flux density)×(Number of scattering atoms)×wUnitw_{\text{Effective}}=\left(\text{Effective flux density}\right)\times\left(\text{Number of scattering atoms}\right)\times w_{\text{Unit}}

To obtain the number of scattering atoms we must consider the volume of gold struck by the beam and multiply it by n, the number of atoms per unit volume. The volume of gold struck by the beam can be calculated by multiplying the cross-section of the beam by the thickness s of the gold foil, so we have:

wEffective=(Effective flux density)×(Beam cross-section)×s×n×wUnitw_{\text{Effective}}=\left(\text{Effective flux density}\right)\times\left(\text{Beam cross-section}\right)\times s\times n\times w_{\text{Unit}}

The product of the flux density and the beam cross-section gives us the total incident flux, which we will denote by F, so we have:

wEffective=F×s×n×wUnit=Fsnq2Q264π2ε02m2v41sin4ϑ2\begin{aligned} w_{\text{Effective}} & =F\times s\times n\times w_{\text{Unit}} \\ & =Fsn\frac{q^2Q^2}{64\pi^2\varepsilon_0^2m^2v^4}\frac{1}{\sin^4\frac{\vartheta}{2}} \end{aligned}

This formula gives us the probability flux per solid angle. If we want to calculate the flux of particles, we must consider that the passage of a particle is equivalent to the passage of a “unit of probability”, that is, when a unit of probability moves from one place to another it means that a particle has moved between these two places; so the formula that gives us the probability flux also gives us the flux of particles without needing to be corrected.

If we assume that the detector subtends a solid angle dΩ, then we can calculate the number of particles per unit time that are detected:

NΔt=wEffectivedΩ=Fsnq2Q264π2ε02m2v41sin4ϑ2dΩ\begin{aligned} \frac{N}{\Delta t} & =w_{\text{Effective}}d\Omega \\ & =Fsn\frac{q^2Q^2}{64\pi^2\varepsilon_0^2m^2v^4}\frac{1}{\sin^4\frac{\vartheta}{2}}d\Omega \end{aligned}

To be able to apply this formula it remains to determine the total incident flux F. To determine this quantity we must compute the integral of the distribution obtained experimentally. The integral must be computed taking into account that the curve actually represents a surface, obtained by rotating the curve about the ordinate axis; so we do not have a simple integral, but a double integral. However, to obtain a rough estimate we will do the calculation based on the approximation shown in figure 20, that is, we will approximate the surface with a cylinder of base radius 10° and height equal to the maximum height of the surface, 27 particles per second in the solid angle dΩ.

Approximation of the surface by a cylinder.
Fig. 20Approximation of the surface of revolution with a cylinder.

So for the total flux we have:

F=(Particles per unitof time in dΩ)×(Total solidangle)dΩF=\left(\begin{gathered}\text{Particles per unit} \\ \text{of time in }d\Omega\end{gathered}\right)\times\frac{\left(\begin{gathered}\text{Total solid} \\ \text{angle}\end{gathered}\right)}{d\Omega}

For the total solid angle we have (Fig. 21):

Solid angle of the detector.
Fig. 21Solid angle of the detector.
(Total solid angle)=Sr2=π(rsin10)2r2=πsin210\begin{aligned} \left(\text{Total solid angle}\right) & =\frac{S}{r^2} \\ & =\frac{\pi(r\sin10^\circ)^2}{r^2} \\ & =\pi\sin^210^\circ \end{aligned}

so:

F=(Particles per unit of time in dΩ)×πsin210dΩ=27×πsin210dΩ2.5dΩ\begin{aligned} F & =\left(\text{Particles per unit of time in }d\Omega\right)\times\frac{\pi\sin^210^\circ}{d\Omega} \\ & =27\times\frac{\pi\sin^210^\circ}{d\Omega} \\ & \approx\frac{2.5}{d\Omega} \end{aligned}

Substituting this value of F into the formula for the number of particles detected per unit time we have:

NΔt=2.5dΩsnq2Q264π2ε02m2v41sin4ϑ2dΩ=2.5snq2Q264π2ε02m2v41sin4ϑ2\begin{aligned} \frac{N}{\Delta t} & =\frac{2.5}{d\Omega}sn\frac{q^2Q^2}{64\pi^2\varepsilon_0^2m^2v^4}\frac{1}{\sin^4\frac{\vartheta}{2}}d\Omega \\ & =2.5sn\frac{q^2Q^2}{64\pi^2\varepsilon_0^2m^2v^4}\frac{1}{\sin^4\frac{\vartheta}{2}} \end{aligned}

For n, the number of atoms per unit volume, we can make an estimate considering that an atom has a radius of about 1 Å (1010m10^{-10}m), so it occupies a volume of about (21010m)3=81030m3(2\cdot10^{-10}\:m)^3=8\cdot10^{-30}\:m^3; thus we have n(81030)11029n\approx{\left(8\cdot10^{-30}\right)}^{-1}\approx10^{29}.

Substituting the following values into the formula:

n1029 atoms per m3n\simeq10^{29}\ \text{atoms per}\ m^3

we have:

NΔt=2.5(2106)1029(3.21019)2Q2643.142(8.81012)2(6.71027)2(1.6107)41sin4ϑ241029Q2sin4ϑ2 atoms per s\begin{aligned} \frac{N}{\Delta t} & =2.5\left(2\cdot10^{-6}\right)10^{29}\frac{{\left(3.2\cdot10^{-19}\right)}^2Q^2}{64\cdot3.14^2\cdot{\left(8.8\cdot10^{-12}\right)}^2{\left(6.7\cdot10^{-27}\right)}^2{\left(1.6\cdot10^7\right)}^4}\frac{1}{\sin^4\frac{\vartheta}{2}} \\ & \cong4\cdot10^{29}\frac{Q^2}{\sin^4\frac{\vartheta}{2}}\ \text{atoms per s} \end{aligned}

At this point we must find the charge Q that makes this theoretical distribution coincide with the experimental distribution; for Q=1351019CQ=135\cdot10^{-19}\:C we have the comparison shown in figure 22.

Final comparison of theory and measurement.
Fig. 22Final comparison between the theoretical distribution and the measurements.

So our estimate for the charge of the gold nucleus is Q=1351019CQ=135\cdot10^{-19}\:C, corresponding to 1351.6=84\frac{135}{1.6}=84 electrons.

More precise measurements lead to a charge equal to 79 times that of the electron.

We did not want to carry out a very precise measurement; our aim was only to show how it is possible to determine the nuclear charge and the number of electrons contained in an atom.

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