Prediction of deviations from the Rutherford formula for low-energy Coulomb scattering of wavepackets
Scott E. Hoffmann

TL;DR
This paper investigates how wavepacket scattering from a Coulomb potential deviates from Rutherford's formula at low energies and angles, revealing measurable effects and theoretical insights into wavepacket behavior in long-range potentials.
Contribution
It introduces a wavepacket-based approach to Coulomb scattering, enabling finite probability calculations and analysis of deviations from Rutherford's formula at low energies.
Findings
Deviations from Rutherford formula occur at low angles and energies.
Low-energy scattering shows a measurable shadow zone around the forward direction.
Wavepacket analysis extends partial wave analysis to infinite-range potentials.
Abstract
We calculate the nonrelativistic scattering of a wavepacket from a Coulomb potential and find deviations from the Rutherford formula in all cases. These generally occur only at low scattering angles, where they would be obscured by the part of the incident beam that emerges essentially unscattered. For a model experiment, the scattering of helium nuclei from a thin gold foil, we find the deviation region is magnified for low incident energies (in the keV range), so that a large shadow zone of low probability around the forward direction is expected to be measurable. From a theoretical perspective, the use of wavepackets makes partial wave analysis applicable to this infinite-range potential. It allows us to calculate the everywhere finite probability for a wavepacket to wavepacket transition and to relate this to the differential cross section. Time delays and advancements in the…
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Prediction of deviations from the Rutherford formula for low-energy
Coulomb scattering of wavepackets
Scott E. Hoffmann
School of Mathematics and Physics
The University of Queensland
Brisbane, QLD, 4072
Australia
Abstract
We calculate the nonrelativistic scattering of a wavepacket from a Coulomb potential and find deviations from the Rutherford formula in all cases. These generally occur only at low scattering angles, where they would be obscured by the part of the incident beam that emerges essentially unscattered. For a model experiment, the scattering of helium nuclei from a thin gold foil, we find the deviation region is magnified for low incident energies (in the keV range), so that a large shadow zone of low probability around the forward direction is expected to be measurable.
From a theoretical perspective, the use of wavepackets makes partial wave analysis applicable to this infinite-range potential. It allows us to calculate the everywhere finite probability for a wavepacket to wavepacket transition and to relate this to the differential cross section. Time delays and advancements in the detection probabilities can be calculated. We investigate the optical theorem as applied to this special case.
I Introduction
It is well known that many of the methods of nonrelativistic scattering theory, methods that can be applied successfully to short-range potentials (those that fall off with radial distance, faster than ), encounter divergences when applied to the infinite-range Coulomb potential. The first Born approximation applied to the Coulomb problem produces the Rutherford differential scattering cross section (6), while the second approximation to the wavefunction diverges for all scattering angles Dalitz1951 . Using partial wave analysis, the sum over the angular momentum quantum number, does not converge. Using formal scattering theory, the transition matrix element beween free momentum eigenvectors diverges when the energy is on shell Dettmann1971 . Furthermore, as pointed out by Taylor Taylor1974 , the usual asymptotic condition is not applicable and the standard definitions of the scattering amplitude and the phase shifts are not applicable.
Other authors have shown that a wavepacket treatment can be used to regularize these divergences Dettmann1971 ; Kroger1984 but did not use the technique of partial wave analysis. Dettmann Dettmann1971 used wavepackets with the divergent matrix elements of formal Coulomb scattering theory to find the accepted Rutherford differential cross section. In Section IX we will discuss his results. Kroger and Slobodrian Kroger1984 discretized the Coulomb problem by using a finite basis of wavepacket state vectors described by non-overlapping step functions in momentum magnitude multiplied by spherical harmonics. The Hamiltonian used was approximate, being the projection of the full Hamiltonian onto this discrete basis. They calculated one -wave element of the matrix for the Coulomb interaction, not enough to allow comparison with our results. Dollard Dollard1964 replaced the usual asymptotic condition by a weaker, more general condition that includes the Coulomb case. We will not find it necessary to use his method.
Our treatment of the nonrelativistic scattering of a wavepacket (representing a charged, spinless particle) from a Coulomb potential uses a basis of eigenvectors of total energy and total angular momentum. As such, it is a combination of a wavepacket treatment and partial wave analysis. We find that the modified sum over converges to a result finite everywhere.
Boris *et al. Boris1993 *used both a wavepacket treatment and partial wave analysis to give a spatial visualization of the scattering process. In Section IX we will discuss their results.
Our method involves first finding the change of basis from free momentum eigenvectors, , to free eigenvectors of the magnitude, , of the momentum and the angular momentum quantum numbers and , denoted These are simply related to eigenvectors of energy, , and angular momentum by (9). This is done in Section II. Then we change the representation of a free initial wavepacket state vector from (7) to (8). This is not an exact result but the leading asymptotic approximation for a small fractional momentum spread. This is done in Section III.
Then we use the technique from partial wave analysis, as is done for short-range potentials, of adjusting the phase of this free wavefunction to give a representation of the incoming state vector. Our wavepacket method involves replacing a limit as time with a limit as the momentum spread to define the correspondence between free and incoming state vectors. This is done in Section IV. We will discuss the role of the logarithmic phase in (39).
We use the antiunitary time reversal operator to construct the outgoing state vectors. The measurement is modelled as the projection onto these outgoing state vectors.
In Section V we derive the connection, for Gaussian wavepackets, between finite probabilities and the differential cross section.
In Section VI we evaluate an integral over momentum magnitude and numerically evaluate a sum over the angular momentum quantum number to find the finite amplitude for the process. We explore the parameter space and present our results in Section VII, with consideration of the possibility of experimental measurement of the phenomena we predict.
In Section VIII we present an integral relation satisfied by our scattering probability that represents the conservation of total probability. We use this as a check on our results. We also discuss the optical theorem in the context of Coulomb wavepacket scattering.
In Section IX we compare our results with those of other authors. Conclusions are presented in Section X.
For the nonrelativistic scattering of a spinless, charged particle in a static Coulomb field, the time-independent Schrödinger equation, with Hamiltonian in the representation
[TABLE]
can be solved to find an energy eigenvector of the form
[TABLE]
as done in standard textbooks Messiah1961 ; Merzbacher1998 . The asymptotic form of this wavefunction as then gives the scattering amplitude
[TABLE]
(Throughout this paper, we use Heaviside-Lorentz units, in which .) The momentum magnitude, in terms of the energy, is The scattered wave is observed at the scattering angle to the incident direction. The dimensionless quantity is
[TABLE]
where is the atomic number of the Coulomb field, is the atomic number of the incident particle, and is the nonrelativistic form of the speed of the incoming particle of mass . The quantity is the fine structure constant . The phase shifts for general are defined by (40).
To make contact with experiment, the Rutherford differential cross section is then given by
[TABLE]
Rutherford used an entirely classical treatment of Coulomb scattering of point particles to obtain, remarkably, the same result as the later quantum calculation Rutherford1911 . The experimental verification of this cross section formula is routinely done as a laboratory activity in undergraduate physics courses.
This scattering amplitude (3) is not an amplitude of the type for which the modulus-squared is a probability less than or equal to unity. For a start it is not dimensionless, instead having the dimensions of length. Furthermore it diverges in the forward direction, , for all momenta, and as for all scattering angles.
One purpose of this paper is to find the relation between the scattering amplitude and what we will call the finite amplitude for this scattering process, which is simply the matrix element between normalized wavepacket state vectors, and as such must be less than or equal to unity in magnitude. This relation, which we will derive for Gaussian wavepackets in Section V, will, in the case of more general interactions, only hold for scattering angles sufficiently far from the forward direction.
II The change of improper basis vectors
We first need to change the representation of a free wavepacket state vector, normalized to unity, from
[TABLE]
to
[TABLE]
where the are eigenvectors of the magnitude of momentum () and angular momentum (the familiar quantum numbers and taking only integer values). Note that eigenvectors of energy () and angular momentum are simply related to these by a change of normalization:
[TABLE]
We start with the improper basis vectors. The basis transformation is derived by Sakurai Sakurai1994 and agrees with our calculation. We want the to have the orthonormality relation
[TABLE]
and the to obey the orthonormality relation
[TABLE]
The result is
[TABLE]
with , with a choice of global phase.
III Basis transformation for a free wavepacket state vector
The free state vector that will be modified to become the incoming state vector is chosen as the Gaussian wavepacket Schrödinger picture state vector
[TABLE]
The average momentum is The standard deviation of momentum in all directions is . We are going to choose a well-resolved momentum,
[TABLE]
and we will only need the leading asymptotic approximation to the wavefunction in powers of , as will be explained shortly. The average position at is The standard deviation of position in all directions at is with
The distance, , from the center of the Coulomb potential at must be large so that the corresponding interacting state vector is effectively free at that time, and so that we can apply an approximation in Section V. However there must be a limit on the size of In our scattering geometry, over the time of the experiment, the incoming wavepacket will traverse a distance of about We demand that the spreading of the wavepacket be negligible over this time. The nonrelativistic law for spreading of Gaussian wavepackets is Merzbacher1998
[TABLE]
where is the time measured from minimality. We see that spreading becomes significant for If we instead choose a particular dependence of on and
[TABLE]
we will still have a very large initial distance for , much larger that the initial spread, but wavepacket spreading will be negligible over the time of the experiment. We note that the dependence on of the probability that we calculate (90) will only influence the time shifts, and with only a logarithmic dependence. For short-range potentials, the absence of the logarithmic phase will mean that the time shifts are independent of
Now we transform the wavefunction. Using (7),(8) and (12), we find the transformation
[TABLE]
again with and with .
The spherical harmonic is
[TABLE]
where
[TABLE]
are Wigner rotation matrices Messiah1961 .
The integral is simply
[TABLE]
We have
[TABLE]
To eventually calculate an amplitude for the scattering process, we will be evaluating an integral over in which a factor will appear, where
[TABLE]
This factor is sharply peaked in with a width of . We will repeatedly find integrands similarly dominated by narrow factors, including the integral over , which contains the factor
[TABLE]
This function is sharply peaked at with a width of order We need to find the leading approximation to such integrals for along with an estimate of the remainder. We use the technique of expanding the exponents (and more slowly varying factors) in powers of treating this as a quantity of and in powers of treating this as a quantity of We then evaluate the integrals to lowest order and estimate that the fractional remainder is no larger than uniform in the remaining variables.
With this method, we find
[TABLE]
Similarly, we find that we can replace
[TABLE]
using our scheme to avoid wavepacket spreading. Here cannot be replaced by
With these approximations, we need to evaluate the integral (after using )
[TABLE]
We cannot use a power series in for the Wigner rotation matrix, , as for large it will have rapid variation on the region . Instead, we use an approximation, from a paper by the author in preparation, valid for small uniform in :
[TABLE]
(This result has been checked numerically.) Then the integral evaluates to Gradsteyn1980
[TABLE]
Finally the leading asymptotic approximation to the representation of the free state vector is given by the wavefunction (normalized up to corrections)
[TABLE]
Note that a narrow distribution in angle produces a wide distribution in angular momentum.
IV Construction of the incoming and outgoing state vectors
We will be considering a range of different incident momentum magnitudes, . In each case, we require that the fractional momentum spread, , be small. The simplest scheme is to make this quantity a constant independent of momentum:
[TABLE]
It will also become necessary to impose a lower limit on momentum for a given , thereby imposing an upper limit on the quantity , in (53) below. Note that we can still consider arbitrarily small momentum magnitudes, but only by decreasing . In our numerical calculations, we will use which gives , sufficiently small for our purposes.
In scattering theory Newton1982 ; Taylor1974 , we define two mappings from free state vectors to interacting state vectors, provided by the Møller operators and It is supposed that for an arbitrary free state vector, an interacting state vector can always be constructed that behaves in an essentially free manner at very early times, with properties matching those of the free state vector at those early times. We say that this interacting state vector is the incoming state vector corresponding to that free state vector, and write
[TABLE]
It should be clear that this correspondence only makes physical sense for wavepacket state vectors, where there is a position distribution that may be localized far from the scattering center at very early times. However, once it is constructed, the Møller operator will have matrix elements between plane-wave improper state vectors.
The other Møller operator, maps from free to outgoing state vectors, such that the latter are essentially free as
The incoming correspondence is defined by requiring
[TABLE]
In contrast, in our method we only need to find the free to interacting correspondence for two particular sets of state vectors, namely
[TABLE]
and
[TABLE]
where the latter will be defined below. We consider the incoming case first.
Since, for small , the free wavepacket is already localized far from the scattering centre at we argue that the interacting state vector should be essentially free at not just as This leads to two constraints. The probability distribution in and is independent of time for the interacting system, so it must be equal to its value as when we argue that it must take its free value exactly (for negligible bound state content in the attractive case). Hence
[TABLE]
(The modifications imposed by the logarithmic phase in (39) will not negate this argument.) In practice we equate to the leading asymptotic approximation as of given by (29), with the knowledge that the error is negligible for the value of that we consider.
We will find that it is not possible for the phases as well as the magnitudes of the incoming and free position probability amplitudes to be equal in the limit (32). Instead we propose that it is sufficient to require that the position probability density at approach its free form in the limit as
[TABLE]
(This argument will need to be modified when taking into account the effect of the logarithmic phase.) Compared to (32), there is no need here to evolve the wavefunctions towards infinite times.
The first of these equations implies that the interacting and free wavefunctions can only differ by a phase factor
[TABLE]
The fact that is independent of follows from the extra physical requirement that rotations commute with the Møller operators. (The phase factor from is physically relevant and will be retained.)
Now we impose the constraint (36) on the incoming position probability amplitude,
[TABLE]
It is clear that for large we can use an approximation for large if the incoming probability density is to have a similar form to the free density. We use the known solutions Messiah1961 (with continuum normalization similar to (11)) with asymptotic form as
[TABLE]
where the Coulomb phase shifts, , are defined implicitly by
[TABLE]
In contrast, the free spherical waves have the asymptotic form
[TABLE]
and the free position probability amplitude is
[TABLE]
which evaluates to
[TABLE]
Note that for short-range potentials, there will be different phase shifts instead of and the logarithmic phase term will be absent.
In
[TABLE]
with
[TABLE]
only the integral over containing will be significant on So the relevant phase to consider is
[TABLE]
in comparison with
[TABLE]
which leads to a peak probability density at
We would like to be able to choose to cancel both the Coulomb phase shifts and the logarithmic phase. This is not possible, since the latter is a function of and cannot depend on Instead, we choose
[TABLE]
and investigate the physical effects of the logarithmic phase.
We expand in powers of :
[TABLE]
The remainder is found to be negligible for and (see (53) below).
The first term in (49) is independent of so merely contributes an -dependent phase factor to the position wavefunction. The second term produces a spatial shift of the peak of the position wavefunction away from its free value of To see this, we note that is stationary in at the peak, for satisfying
[TABLE]
Inverting for large gives the asymptotic behaviour
[TABLE]
with
[TABLE]
(It will be easily seen that the same result will hold for the outgoing state vectors.)
We suppose that could be as large as without affecting the negligibility of wavepacket spreading or the requirement that the mean initial radial distance of the wavepacket grow as for given momentum. This leads to
[TABLE]
for .
So, with our choice of phase (48) to define the incoming state vector corresponding to a free state at average radial position the actual average position of the incoming state vector is at radius It is clear that the incoming state can never be considered entirely free, since evolution over short times will always give
[TABLE]
We argue that this is the correct physical behaviour for a particle in a Coulomb field because very similar behaviour is seen in the classical case at large distances from the origin. A straightforward calculation of the classical trajectories for a head-on collision shows that if free motion is defined as
[TABLE]
where is the finite limit of momentum magnitude far from the origin, then the actual position of the particle has the asymptotic form for large
[TABLE]
in asymptotic agreement with the quantum calculation as .
A longitudinal spatial shift will not change the probability density, so the conclusion (35) stands. We now see how the constraint (36) must be modified to
[TABLE]
Clearly this result is satisfied in our case.
Our final result for the wavefunction of the incoming state vector is
[TABLE]
We use the antiunitary time reversal operator, to construct the outgoing state vector as the time reversal of an incoming state vector is an outgoing state vector. It can be shown Merzbacher1998 that the transformation law of the interacting eigenvectors is
[TABLE]
Starting with
[TABLE]
and applying a time reversal, a rotation by about the axis and then a further rotation by about the axis gives
[TABLE]
so
[TABLE]
We have chosen
[TABLE]
So
[TABLE]
Calculation of involves the factor and arrives at the same result (51,52) for the shift due to the logarithmic phase term.
Our scattering geometry is shown in Figure 2.
V Connection between finite amplitudes, scattering amplitudes and
matrix elements
From the way we have defined the incoming and outgoing state vectors, as illustrated in Figure 1, we see that we need to apply a time shift of (for low interaction strength ) to the incoming state vector to align the wavepackets and maximize the scattering probability. Then both wavepackets are expected to be localized around the origin at time We leave as a variable, a parameter of the incoming state vector. Later we will scan in (or rather as defined in (85,86) below) to see the time delays or advancements away from free evolution caused by the interaction. So we have the incoming and outgoing state vectors
[TABLE]
respectively.
The quantity that we call a finite amplitude is just an matrix element between normalized free wavepacket state vectors
[TABLE]
We used the definition of the matrix Newton1982
[TABLE]
Note that matrix elements (and thus the cross section) are independent of Schrödinger picture evolution time,
[TABLE]
since the matrix commutes with the full Hamiltonian. This, in turn, follows from the fact that the action of the Møller operators is to simply multiply by phase factors that depend only on and .
For state vectors normalized to unity, the Schwartz inequality Messiah1961 guarantees
[TABLE]
which is why we call these “finite amplitudes”.
matrix elements between momentum eigenvectors are related to scattering amplitudes by (see Wichmann Wichmann1965 for a derivation using wavepackets)
[TABLE]
With we can find the matrix element between our Gaussian wavepacket state vectors, by approximating the integrals for , to give
[TABLE]
(The average positions of the wavepackets are not important to this calculation, but will be relevant later.)
Then we find the differential cross section to be (using (5)), for ,
[TABLE]
In Section VIII we will discuss how the separation of the matrix gives physically relevant results for short-range potentials, where the probability is always found to have a peak in the forward direction of height slightly less than unity and width (produced by the 1 term) and scattering in other directions at a much smaller probability (produced by the term). Then the expression (72) is appropriate for short-range () potentials. We will find for Coulomb scattering that this separation does not produce physically meaningful terms, and that (except at very low interaction strengths/high energies) there is no narrow forward peak. Then it is more appropriate to combine the terms and write
[TABLE]
or
[TABLE]
There is a simple way to see how the powers of and arise. The area of the incoming wavepacket perpendicular to the average momentum direction scales as The final state solid angle element scales as Then the probability of the event is
[TABLE]
so
[TABLE]
VI Evaluation of the finite amplitude and extraction of the scattering
amplitude
We now have the finite amplitude, using (58,64) and a Legendre polynomial,
[TABLE]
where the phases are
[TABLE]
The time shift phase factor is
[TABLE]
with the average speed of the wavepacket.
We also expand the Coulomb phase shifts in powers of :
[TABLE]
A numerical investigation shows that the remainder, is negligible on our parameter space.
So we can find the leading approximation to the integral for small ,
[TABLE]
(with negligible error from extending the lower limit of the integral to ), to give
[TABLE]
with
[TABLE]
Taking into account the spatial shifts caused by the logarithmic phase, the time it would take a free particle to start at radius be deflected at the origin without time shift and finish at radius would be with
[TABLE]
For the actual interacting evolution, we define the spatial displacement ( times the time delay) as a function of the shift time, , in units of as
[TABLE]
Then the Gaussian factor dependent on becomes
[TABLE]
with
[TABLE]
We used
[TABLE]
The form on the right-hand side is more advantageous for computation.
Note that if the interaction made any change to the free spreading formula (15), it would be caused by a phase proportional to Since in the expansions of the logarithmic phase (49) and the Coulomb phase shift (80), we found those second-order terms to be negligible with our choice of parameters, there is effectively no spreading over the course of the experiment.
Now we numerically evaluate the series in
[TABLE]
to find the probability of the process. In practice we scan in to find the peak. The equation for the differential cross section is then
[TABLE]
with the warning, discussed earlier, that if this result produces a peak of width around the forward direction, we must use the methods of Section VIII to separate the peak from the scattering.
Note that this formula (90) can be used for any short-range central potential with the replacements
[TABLE]
where are the phase shifts for that potential and there are no logarithmic phase contributions to
VII Results and discussion of measurability
Now we calculate the probability as given by (90,88,40), for several cases.
We choose the momentum resolution parameter mostly for illustration purposes, as it is much less than unity, and to limit computation time. There is a sense in which the “true” differential cross section is the limit of our results as However, we will find that there is not uniform convergence in scattering angle, or strength parameter, Yet is a physical parameter, the width in momentum of the wavepacket. To provide a realistic description of a scattering experiment would require an estimate of this parameter.
We consider radioactive and accelerator sources. If alpha particles were emitted from Radium-226 with a momentum spread determined by the natural linewidth (the reciprocal of the decay lifetime as determined by the Heisenberg uncertainty principle) the value of would be so small (of order ) that deviations from the Rutherford formula could never be observed. However physical effects broaden the linewidth from a solid sample. Again for radioactive emission of alpha particles, using extremely thin samples to reduce broadening effects, linewidths as small as have been observed Pomme2015 . For the emission of Radium-226, this would give assuming that the actual energy width of the wavepackets could be smaller than the observed linewidth.
In accelerator experiments, the energy resolution of the beam is well controlled, so it should be possible to put an upper bound on This matter requires further consideration for a specific experiment.
In Figure 2 we plot the angular dependence of the probability for the particular choice then the dependence of the probability on for the scattering angle In both cases we choose not attempting to find the maxima of the probabilities. For comparison we plot the Rutherford “probability”,
[TABLE]
which we obtain by naïvely converting the Rutherford differential cross section (122) into a probability using (74). Of course this is not a true probability since it rises above unity and diverges at
In Figure 2(a) we see excellent agreement with the Rutherford formula over almost the entire range of angles, but a deviation at low angles. The probability we calculate cannot rise above unity, so a deviation is to be expected. In Figure 2(b) we see deviations from the Rutherford formula at high energies (low ) and at low energies (large ). We assume that the first of these is due to numerical error, but we do not investigate further in this paper. The deviation at low energies will be investigated shortly with a special treatment of the phase shifts, where we conclude that there is a physical effect.
We find that the timing varies significantly with scattering angle. First we calculate the probability in the forward direction, for as a function of the scaled spatial shift . This shows a maximum at corresponding to a time delay. We find later that the peak probability as a function of angle occurs at around The profile in for this angle is shown in Figure 3(a). We find the maximum probability for this angle is at corresponding to a time delay. We will discuss the measurability of time shifts shortly. Then we calculate the angular distribution, for this value of , shown in Figure 3(b). We see deviations from the Rutherford formula for scattering angles less than about There is a shadow zone of low probability of angular width around the forward direction.
We have found that as is decreased, the region of violation of the Rutherford formula becomes smaller (in approximately direct proportion).
We repeat this procedure for an attractive interaction () and find the profile in for scattering angle shown in Figure 4(a). We see a peak at corresponding to an advancement in time. Then we set and obtain the probability shown in Figure 4(b). The results are very similar to the case The Rutherford probability for these two cases () is identical.
We consider weaker interactions () with probability results shown in Figure 5, only focussing on low angles. For we see a strong forward peak and takes its maximum at For we find takes its maximum at . The probability profile in Figure 5(b) is essentially that expected for no interaction, proportional to (dot-dashed) with a peak probability very close to unity. Thus we see more deviations from the Rutherford formula, at low interaction strengths. The calculation shown in Figure 2(b) for low is attempting to calculate an extremely small probability at , leading us to the conclusion that we are encountering numerical errors in this region.
Our numerical investigations and the result (106) that we obtain in Section VIII suggest that the angular width of the shadow zone will increase as increases (incident momentum, decreases). To investigate scattering at very large values of for numerical stability in our computation, it was necessary to obtain an asymptotic approximation of the Coulomb phase shifts,
[TABLE]
with This then leads to
[TABLE]
The experiment we envision, that we wish to describe with this calculation, is the scattering of alpha particles () by a thin gold () foil, similar to the original experiments of Rutherford, Geiger and Marsden Rutherford1911 ; Geiger1909 . The energies of alpha particles emitted by radioactive sources are too large for our purposes. The emission of Radium-226 with gives and a very small deviation region that would be obscured by the unscattered particles. So we suggest that a helium nucleus accelerator Anokhin2013 could be configured to produce sufficiently low energies.
In Section IV we imposed a bound on the strength parameter, to satisfy physical constraints. So we consider first the case ( with the above experimental parameters). Figure 6 shows the predicted differential cross section compared to the Rutherford formula (6). We see a cross section dominated by backscattering, with a shadow zone almost to , in agreement with the Rutherford formula only at Even with a beam width of obscuring the forward direction (see discussion at the end of this Section), this shadow zone would be clearly observable. We find takes its maximum at
We examine the range of energies over which this shadow zone could be observed. We choose an observation angle of There should no difficulty ensuring a beam width sufficiently narrow that the essentially unscattered particles do not obscure the signal. For this scattering angle, we calculate the ratio of predicted to Rutherford differential cross sections
[TABLE]
We sampled the scaled spatial shifts at several energies and found a best fit The results are shown in Figure 7. We see that the ratio rises rapidly with energy. The potentially most definitive measurements would be on the region We note
Since this example has the largest scaled spatial shift encountered, we calculate the time delay in seconds for this case and find not easily measured.
Wigner Wigner1955 reasoned that the spatial shift for -wave scattering would be twice the derivative of the phase shift with respect to . This is precisely what we have found, after taking into account the time shifts caused by the logarithmic phase. Wigner was considering in what way the classical concept of causality could be extended to the quantum domain, but his reasoning was based on the assumption of a potential of finite range.
The form of our results should be cause for concern. In addition to the violations of the accepted Rutherford formula at low angles, we see (except at low energies) no strong forward peak as usually expected in a scattering experiment and the very low scattering in the forward direction raises questions about violation of the optical theorem.
On the first of these points, our scattering model has a special geometry, that of a head-on collision of wavepackets. In a real scattering experiment, the projectiles approach the targets with a distribution of impact parameters, displacements perpendicular to the incoming momentum direction. The physical expectation is that wavepackets with sufficiently large impact parameters will pass through essentially unscattered. These events will build up the strong, narrow peak around zero scattering angle that we expect. We will examine the effects of nonzero impact parameters on Coulomb scattering in a future work.
We consider the optical theorem as applied to our system in the next Section.
VIII Conservation of probability and the optical theorem
We find a simple integral relation satisfied by the probabilities that expresses conservation of total probability. Starting from (90) and using the orthogonality of the Legendre polynomials and the normalization integral for a shifted Gaussian, it is easily shown that
[TABLE]
This relation holds for all interactions, including the free case with
[TABLE]
For the Coulomb interaction, we have cases with no narrow peak with probability close to unity around the forward direction that we would expect for short-range potentials. So the relation (74) between the probability and the differential cross section can be used for all angles. Then we find another integral relation
[TABLE]
We hesitate to call this the “total cross section” for the Coulomb interaction, as it is independent of the strength parameter, and diverges as the momentum width For all potentials we find the sum rule
[TABLE]
with including the forward peak and the scattering. The forward peak dominates this normalization integral for short-range potentials, which does not give the total scattering cross section. A separation of the forward peak and the scattering is necessary to define the differential scattering cross section in these cases, as we do below.
Our result for the Coulomb case differed most dramatically from the expected form for short-range potentials. We would like to be confident that the total probability in our final states is unity. We found a best fit for after finding the values of where the probability took its maximum value for several sampled values of Then we approximated the integral over as a discrete sum with 200 intervals and found
[TABLE]
We can use the integral relation (98) to find an estimate of the angular size of the region where the Rutherford formula is violated. In our numerical investigations, we have found that the probability factorizes in the form
[TABLE]
to a very good approximation. Clearly the way to extract the maximum probability is by the integral
[TABLE]
Then suppose the shadow region had vanishing probability, on and took the Rutherford form (94) at higher angles. Then we would have the integral relation
[TABLE]
For which includes the cases other than that we have been considering, we find
[TABLE]
This gives , . From Figures 3 and 4, these estimates are seen to give good characterizations of the regions of violation. For the case there is a narrow forward peak instead of a shadow zone, so an estimate of is not appropriate.
We derive an optical theorem using partial wave analysis (as done by Newton Newton1982 ), modified to take into account amplitudes that depend on as well as We start by defining an amplitude with a definite phase, as necessary for a relation between an amplitude and a phase-independent total cross section, by
[TABLE]
so that Then we apply the identity
[TABLE]
with the intention of separating the amplitude into a part that describes the narrow forward peak and a remaining part that we identify as the scattering. This is equivalent to separating the transition matrix, from the matrix by This gives
[TABLE]
with
[TABLE]
Using this separation, we define a scattering amplitude, a function of only, by integrating over :
[TABLE]
with the prefactor chosen to be consistent with (74). Then we find
[TABLE]
Similarly, we define the total cross section as another integral over and an integral over all scattering directions:
[TABLE]
Now we point out the great distinction between the Coulomb case and that of a short-range potential. In the latter case, converges to a narrow function peaked at with height less than unity by (These results were tested numerically on the finite-range spherical square well potential Messiah1961 .) The sums in (113) and (115) converge without the need of the Gaussians in to
[TABLE]
The scattering amplitude, is finite for all angles (for the spherical square well) and has no narrow peak at so the separation (108) achieves the intended goal of separating the forward peak from the scattering. We note that there is a computational benefit in using the form (111) instead of (107) if we are not interested in calculating the forward peak: the sums over can be taken to a cutoff value much lower than when the form (107) is used.
Then the optical theorem,
[TABLE]
follows immediately from (116) and (117).
We see that our method can be recast into the familiar results of partial wave analysis, for short-range potentials, with two benefits: the regularization of the forward peak and the ability to calculate time shifts.
For the Coulomb potential, taking as an example, we find that both and the imaginary part of have narrow peaks around both of the form
[TABLE]
while the real part of takes much smaller values. So using these separated amplitudes, the observed low value of the probability close to comes about partly from a near cancellation of two very similar terms in
[TABLE]
We see that the separation (108), in the Coulomb case, does not separate the amplitude into a forward peak and a scattering term, justifying our choice not to apply it.
Even the case which shows a forward peak in the probability close to unity, gives unintuitive results when the separation (108) is applied. In that case all three of and show narrow peaks close to unity.
As for the possibility of an optical theorem in the Coulomb case, we plot the ratio
[TABLE]
for a range of values of (and for ) in Figure 8. We see that nowhere does it take the value unity. Furthermore, we have seen that the quantities in the ratio do not have the physical meanings of their counterparts for short-range potentials.
IX Comparison with other works
Boris et al. Boris1993 numerically evolved wavepackets in a Coulomb potential. For an initial wavepacket state vector, , they numerically calculated the amplitudes on the interacting basis vectors ,
[TABLE]
where the are simply related to the energy and angular momentum eigenvectors of the full Coulomb Hamiltonian (by (9)). Then they plotted the position probability density, where
[TABLE]
However, they did not extract the differential cross section or calculate time shifts.
Their Figure 15, for the scattering of a wavepacket by a repulsive Coulomb potential, shows a shadow zone around the forward direction. However that was for a wavepacket with a nonzero impact parameter, as they were investigating whether wavepackets would follow classical trajectories. Since they did not consider the head-on (zero impact parameter) case, direct comparison with our results is not possible. Also, their wavepackets spread noticeably over the course of their numerical experiments, so they appear not to be in the regime It would be of value to repeat their simulations with our parameters to allow direct comparison.
We are also interested in whether wavepackets follow classical trajectories, and will investigate this in a future work.
Several authors Nutt1968 ; Dettmann1971 have used wavepackets to deal with the divergence of the matrix in formal scattering theory applied to the Coulomb interaction Schwinger1964 . Dettmann Dettmann1971 was able to reproduce the Rutherford formula but, crucially, he did not calculate the modulus-squared of the matrix elements for final momenta close to the initial momentum. It would be of value to repeat his calculation in that region to allow direct comparison with our results.
X Conclusions
The inclusion of wavepackets into the description of a scattering experiment does not merely smear the scattering amplitude over a small angular width. Instead, for Coulomb scattering, we predict a finite probability of scattering into the forward direction, where the Rutherford formula diverges. Generally we find excellent agreement with the Rutherford formula except for small angles around the forward direction. We conclude that these deviations would not have been observable in previous experiments. However, consideration of low incident energies shows the deviation to be magnified and raises the possibility of experimental observation of a shadow zone.
We note that the existence of a shadow zone is consistent with the view of a scattering process as the diffraction of a wave, in the appropriate parameter regime.
A wavepacket treatment also implies, and allows the calculation of, time shifts in the detection probabilities. However, these are generally very small for Coulomb scattering.
From a theoretical perspective, a wavepacket description allows the technique of partial wave analysis from scattering theory to be applied to the long-range Coulomb potential. We use a formalism that allows treatment of the logarithmic phase in (39), a consequence of the infinite range of the Coulomb potential. This phase alters the long-distance trajectory of the wavepacket, in close agreement with the corresponding classical trajectory.
Our method involves the calculation of probabilities for wavepacket to wavepacket transitions and then relates these to the differential cross section. That fact that a probability must be finite leads directly to our prediction of deviations from the Rutherford formula for the differential cross section.
This method is made possible by the availability of the exact solutions for the energy angular momentum eigenfunctions. To apply the method to other central potentials would require the phase shifts for those potentials. Phase shifts have been calculated for the Yukawa Hamzavi2012 , Morse Rawitscher2002 and spherical well Messiah1961 potentials, for example. Note that Rawitscher et al. Rawitscher2002 calculated the motion of a wavepacket at a resonance using a partial wave method. There are numerical methods available to calculate phase shifts in other cases Klozenberg1974 .
We note that partial wave analysis is widely used in nuclear physics, where a Coulomb interaction is often present in addition to short-range nuclear forces Bertulani2004 . The Coulomb amplitude (3) is usually inserted to avoid the divergent partial wave series. The method presented here may allow the inclusion of the Coulomb force into the partial wave analysis.
The method could be extended to two-particle scattering by forming the eigenvectors of total energy, momentum and centre-of-mass frame angular momentum Jacob1959 ; Macfarlane1962 . Particles with spin are not an obstacle. If relativistic interactions are to be investigated, it is not widely known that there are relativistic probability amplitudes for particles of any spin, as discussed by Fong and Rowe Fong1968 . For the electron, these are two-component rather than four-component objects.
The reference list from the paper itself. Each links out to its DOI / PubMed record.
- 1(1) Dalitz RH. On higher Born approximations in potential scattering. Proc Roy Soc Lond A: Math, Phys and Eng Sci. 1951;206(1087):509–520.
- 2(2) Dettmann K. Wave packet theory of Coulomb scattering. Zeitschrift für Physik. 1971;244(1):86–93. Available from: http://dx.doi.org/10.1007/BF 01394875 . · doi ↗
- 3(3) Taylor JR. A new rigorous approach to Coulomb scattering. Il Nuovo Cimento B (1971-1996). 1974;23(2):313–334. Available from: http://dx.doi.org/10.1007/BF 02723639 . · doi ↗
- 4(4) Kröger H, Slobodrian RJ. Coulomb scattering of wave packets. Phys Rev C. 1984 Nov;30:1390–1402. Available from: http://link.aps.org/doi/10.1103/Phys Rev C.30.1390 .
- 5(5) Dollard JD. Asymptotic Convergence and the Coulomb Interaction. Journal of Mathematical Physics. 1964;5(6):729–738. Available from: http://scitation.aip.org/content/aip/journal/jmp/5/6/10.1063/1.1704171 .
- 6(6) Boris SD, Brandt S, Dahmen HD, Stroh T, Larsen ML. Quantum-mechanical motion of Gaussian wave packets on elliptical and hyperbolic Kepler orbits in the Coulomb field. Phys Rev A. 1993 Oct;48:2574–2585. Available from: http://link.aps.org/doi/10.1103/Phys Rev A.48.2574 .
- 7(7) Messiah A. Quantum Mechanics. vol. 1 and 2. North-Holland, Amsterdam and John Wiley and Sons, N.Y.; 1961.
- 8(8) Merzbacher E. Quantum Mechanics. 3rd ed. John Wiley and Sons, Inc.; 1998.
