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This is a reprint of R. de L. Kronig's paper 'On the Theory of Dispersion of X-Rays' (J.O.S.A. & R.S.I., vol. 12, June 1926). It summarizes Kramers' quantum theory of dispersion, derives the index of refraction from the atomic absorption coefficient and critical frequencies, and applies it to x-rays. It also discusses electron-group coupling and the origin of Compton-shifted radiation. It sits in the Spectral Theory Book downloads folder, apparently as background reading.
AI-written summary; may contain errors.
Extracted text (machine-read; may contain errors)
Journal of the
Optical Society of America and
Review of Scientific Instruments
Vol. 12 JUNE, 1926 Number 6
ON THE THEORY OF DISPERSION OF X-RAYS
BY R. DE L. KRONIG
ABSTRACT
After a brief summary of the ideas underlying the quantum theory of dispersion it is shown
that it can be applied to the refraction of x-rays, although the assumption that the number of
atoms in a wave length cube is large is no longer satisfied. A general formula for the index
of refraction in terms of the atomic absorption coefficient α and the critical frequencies
is given. From the condition, experimentally verified, that the electrons in the atom for im
pressed frequencies, large compared to their natural frequencies, shall act like free electrons
as far as the index of refraction is concerned, a relation is obtained for a. From the failure
of this relation when applied to the groups of electrons separately, conclusions are drawn as
to the coupling of the groups. Some considerations on the origin of the Compton shifted
radiation are added, from which it appears that in the wave description this radiation must
be regarded as coming from all the atoms and as being coherent with the incident waves; a
result suited to stress the difficulty of harmonizing the wave picture with that of quantum pro
cesses in the atoms.1
1. THE GENERAL DISPERSION THEORY
As is well known, a great many features of the phenomena arising
from the action of external radiation upon matter in bulk can be
qualitatively described by the classical theories. It is there assumed
that all the atoms contain electric charges elastically and, in general,
isotropically bound to equilibrium positions, having a damping pro
portional to their velocity. Under the influence of the radiation the
resonators perform forced oscillations with the impressed frequency.
On account of these oscillations they will emit spherical wavelets, their
induced electric moment being parallel to, and almost in phase with,
the electric field of the incident waves as long as the impressed frequency
is sufficiently remote from any of the natural frequencies of the reson-
1 As Professor Kramers kindly informs me, he too has obtained most of the results derived
in 3. (To be published shortly.)
547
548 R. DE L. KRONIG [J.O.S.A. & R.S.I., 12
ators. These wavelets represent the scattered radiation, and by their
interference with the primary waves they give rise to the retardation
or acceleration of phase which causes the phenomenon of dispersion.
When one of the natural frequencies of the resonators is approached
by the impressed frequency, the amplitude of the forced oscillations
becomes very large, and, moreover, they will be considerably out of
phase with the electric field of the incident waves. The scattering
increases markedly (resonance), and due to the phase shift, the wavelets
produce a diminution of the amplitude of the incident wave (absorp
tion). Finally, when the impressed frequency gets much greater than
the natural frequency of a resonator, its charge will act as if free.
The induced electric moment of an atom containing charges e1, e2,
. . . . e1, e2,. . . ef of mass m1, m2, . . . . mf and capable of performing free
oscillations about an equilibrium position with frequencies ω1, ω2,
. . . . ωf respectively is known to be
if the impressed field at the point of the atom is given by
and v is sufficiently different from the ωi. The total amount of energy
absorbed on the average by a resonator in a time dt from a radiation
field, whose density p(v) does not vary appreciably in the neighborhood
of the natural frequency ωi, is given by
where c is the velocity of light and αi may be called the total atomic
absorption coefficient for the resonator i.2 Hence (1) may be written
The wave theory seems to be the only picture which affords an
adequate description of the phenomenon of dispersion and its connec
tion with absorption.3 Its ideas are therefore utilized in the quantum
2 αi is then the integral of the absorption coefficient over all frequencies, considering the
absorption curve as approaching zero on both sides of the natural frequency. In reality the
absorption coefficient at large frequencies approaches a small positive value corresponding to
the scattering of a free charge. This part of the absorption coefficient has to be subtracted.
3 N. Bohr, Zs. f. Phys. 13, p. 161; 1923.
June, 1926] X-RAY DISPERSION THEORY . 549
theory of dispersion by ascribing also here a scattering moment to
every atom. Since, however, according to our knowledge of atomic
structure, the picture of elastically and isotropically bound charges
in the atom is not to be harmonized with other facts, Kramers4 investi
gated the perturbations arising in a multiply periodic system under
the influence of an external field of the form (2) and found an expression
for the induced scattering moment of an atom by introducing for the
quantities characteristic of the multiply periodic system their quantum
analogues. In the case of a large number of atoms in their normal state,
oriented at random and having absorption lines at the frequencies ωi,
his general expression for the average scattering moment per atom
reduces to5
Here e and m are respectively the charge and mass of an electron, so
that the atom acts as if containing resonators of charge ƒie and mass
fim. Kramers' expression for ƒi may be written
where h is Planck's constant and bi is defined by
Pidt denotes the probability of an atom being lifted from the normal
state to the state i in the time dt under the influence of a radiation field
whose energy density between frequencies ωi and ωi+dω is p(ωi)dω.
bihωip(ωi)dt represents the energy absorbed on the average per atom in
the time dt and may hence be put equal to αicp(ωi)dt. This gives
Introducing in (4) leads to the old expression (3) for the scattering
moment of an atom. In fact, equation (4) was first derived by Laden-
4 H. A. Kramers, Nature, 113, p. 673; 114, p. 310, 1924; H. A. Kramers and W. Heisen-
berg, Zs. f. Phys., 31, p. 681; 1925. See also M. Born, Zs. f. Phys., 26, p. 379; 1924 and J. H.
van Vleck, Phys. Rev., 24, p. 344; 1924.
5 This is identical with a formula obtained previously by R. Ladenburg, Zs. f. Phys., 4,
p. 451; 1921 in a different way; see also R. Ladenburg and F. Reiche, Naturwiss., 11, p. 584;
1923.
550 R. DE L. KRONIG [J.O.S.A. & R.S.I., 12
burg from the viewpoint of the very intimate connection between
dispersion and absorption inherent in the wave picture.
2. CALCULATION OF THE INDEX OF REFRACTION
On account of what follows, it will be necessary to recall how the
expression for the index of refraction can be derived from (4). Consider
an infinite slab of the substance perpendicular to the direction of
propagation Z of the incident waves and of thickness dz, small compared
to the wave length λ, so that all the resonators inside will be practically
in phase, say dz = qλ, where q is a small fraction. Take a point P a
distance l away from the slab and put the Z-axis through it. The slab
may be divided into circular zones by cylinders about Z of radius p.
Let the breadth of such a zone be dp. We now investigate the resultant
electromagnetic field at P produced by the superposition of the spherical
wavelets originating from the atoms in the slab under the influence
of a plane wave. For this purpose we must make the breadth of the
zones such that waves coming from atoms on the inner and outer
boundaries of the zone are still practically in phase; i.e., dr = qλ, where
r is the distance from P to the zone. But pdp=rdr = rqλ≥lqλ. Now
the total volume of a zone is 2πpdpdz ≥2πlq2λ2. But in order that one
may be able, in computing the field at P, to integrate, it is necessary
that in the volume 2πlq2λ2 there is a considerable number n of atoms.
This gives the condition for l
where N is the number of atoms per unit volume.
Using for the scattering moment of an atom the expression (4), one
easily finds by integrating over all the radiation fields of the oscillating
moments that at distances greater than l the wavelets emitted by the
slab under the influence of the incident wave have been ironed out by
interference approximately into a plane wave. If we regard the refract
ing medium as made up of such slabs, we can neglect the effect on the
motion of the resonators in a slab of the waves coming backwards from
the following slabs, provided the polarization produced in the medium
by the field E of the incident wave is small compared to E (i.e., /µ — 1/
< <1). Then the retardation in phase of the incident wave in going
June, 1926] X-RAY DISPERSION THEORY 551
through a slab, produced by the wave from the slab, corresponds to
an-index of refraction µ given by
if all the atoms are of the same kind.
In the theory of dispersion in the optical region it is always assumed
that there is a large number of atoms in a volume whose linear dimen
sions are of the same order of magnitude as the wave length, a condition
generally satisfied in this region. The reason for the assumption is that,
if the polarization of the substance is comparable to the electric field,
then the only simple way of taking the effect of this polarization on an
atom into account consists in imagining a sphere around the atom cut
out of the substance. If the sphere can be so chosen that it contains
many atoms, and yet its radius is small compared to the wave length,
then the formulas for the polarization of a sphere in a uniform electric
field can be applied. If, however, the polarization is very small so that
it may be neglected, i.e., if µ does not differ much from unity, the
preceding analysis shows that the above assumption no longer is
necessary.6 Equation (7) then holds even if there are few atoms in a
wave length cube, but it must be remembered that if actual refraction
is to take place, the optical path of the beam under investigation must
be greater than l.
3. APPLICATION TO THE DISPERSION OF X-RAYS
In case a substance composed of atoms in their normal state is
illuminated by x-rays, we meet a problem with a number of interesting
features. In the first place, there are very few atoms in a wave length
cube, both the wave length and the distances between atoms being of
the order of 1ÅU. Nevertheless, the formula given for the index of
refraction will apply since µ-1 = δ is found to be of the order 10–6, and
l according to (6) ranges for solids around 10–3 cm if we assume as
reasonable values for q and n q = 1/25, n = 25; while the actual path of
the beam in a spectrometer is several cm. Further we have a contin
uous manifold of excited stationary states instead of a discrete sequence.
Consider an electron in one of the inner orbits of the atom, say an
nk orbit. Upon its removal the electron may have any velocity v.
6 For an elaborate mathematical discussion of the case of few atoms in a wavelength cube
leading to the same conclusion the reader is referred to F. Reiche, Ann. d. Phys. 50, pp. 1
and 121, 1916.
552 R. DE L. KRONIG [J.O.S.A. & R.S.I., 12
The ionized atom will in general be capable of two states7 whose energy
difference obeys the relacivistic doublet formula, and which may be
distinguished by a third quantum number j; when k = 1, the ionized
atom is capable of one state only. Thus if an electron be removed from
a 11 orbit, the atom remains in the state designated as K, while if an
electron be removed from a 22 orbit, the atom may remain either in
the state LII or LIII, forming the relativistic L-doublet, these two
states having the values j = 1 and j = 2 respectively.8 We may, therefore,
characterize an excited state by (v,nkj), or using as abbreviation for
the combination nkj the letter r, we can denote it by (v,r). Finally, we
may call it (ω,r), where ω is the frequency corresponding to a transition
from the normal state to the state (v,r). The continuous manifold of
states (v,r) or (ω,r), where r is given and v variable, corresponds to an
absorption band extending from the critical frequency ωr toward larger
frequencies.
With a frequency interval dω of the continuous absorption band r
there is to be associated a resonator of charge fr(ω)dω • e and mass
fr(ω)dω . m, where fr(ω)dω according to (5) is given by
Here αr(ω) is the atomic absorption coefficient at the frequency ω
due to transfer of atoms to the state r. In the expression (7) for the
index of refraction we have now instead of a summation an integration
by ω, extending over the absorption band r from ωr to ∞, and a sum
mation over the various bands r and in addition terms corresponding
to the lines associated with the transfer of outer electrons to higher
stationary states. These latter each belong to a definite series limit
at which an absorption band r begins and we may include them sym
bolically in the integration by extending it from 0 to ∞. For a sub
stance composed of atoms of one kind, one finds from (7) and (8)
This expression will hold even on the short wave length side of the
absorption edges except in their immediate neighborhood, although
then some of the resonators have frequencies nearly coinciding with v.
7 Disregarding the different possible orientations of the orbits of the valence electrons.
8 These are the values customarily used in x-ray notation; their ratio is that of the statis
tical weights of the two states.
June, 1926] X-RAY DISPERSION THEORY 553
The reason is that the resonators in the narrow region from v to v+Δω,
in which the damping would become of importance, have their con
tribution almost canceled by the resonators from v— Δω to v. This is
no longer true at the edge, where the damping must be taken into
account. For compounds or mixtures the value of δ will be found
additively from the values due to the components.
To proceed further it is necessary to know something about αr(ω).
The general result of the investigations on the true absorption co
efficients of elements of atomic number Z not too low and for wave
lengths in the region from 0.1 Å U to 1 ÅU appears to be9 that this
coefficient is approximately expressible in the form
Cr being a constant more or less independent of the substance. Such
expressions have been found to hold both on the short and long wave
length side of the K-absorption limit, i.e., for the absorption due to
the K-and L-electrons. The experimental data10 on the refraction of
x-rays have been obtained with frequencies v large compared to the
frequencies of most of the electrons in the atom. Since according to
(10)αr(ω) decreases rapidly with ω, it is easily seen from (9) that the
9 For a detailed discussion of the experimental evidence and references to the literature
see H. A. Kramers, Phil. Mag., 46, p. 836; 1923; see also F. K. Richtmyer, Phys. Rev., 27,
p. 1; 1926.
10 Bergen Davis and H. M. Terrill, Proc. Nat. Ac, 8, p. 537; 1922;
A. H. Compton, Phil. Mag., 45, p. 1121; 1922;
C. C. Hatley and Bergen Davis, Phys. Rev., 23, p. 290; 1924;
Bergen Davis and R. von Nardroff, Phys. Rev., 23, p. 291; 1924; Piroc. Nat. Ac, 10,
p. 60, 384; 1924;
C. C. Hatley, Phys. Rev., 24, p. 486; 1924;
R. von Nardroff, Phys. Rev., 24, p. 143; 1924;
E. Hjalmar and M. Siegbahn, Nature, 115, p. 85; 1925;
A. Larsson, M. Siegbahn and T. Waller, Phys. Rev., 25, p. 235; 1925.
Bergen Davis and C. M. Slack, Phys. Rev., 25, p. 881; 1925;
M. Siegbahn, Journ. de Phys., 6, p. 228; 1925;
Bergen Davis and C. M. Slack, Phys. Rev., 27, p. 18; 1926.
A. Larson, Zs. f. Phys. 35, p. 401; 1926;
I am indebted to Professor Davis and Mr. Slack for some additional unpublished material.
This deals with the refraction of X-rays in silver on the long wavelength side of the K-limit.
Below are given the values of δ.106 as observed and as computed from the Lorentz formula and
from (9) respectively: .707 Å.U.; -5.3±.6, -5.7, -6.0; .515 Å.U.; –3.0 ± .4, –2.1,
-3.1; .500 Å.U., –2.5±.3, –1.0, –2.9; .485 Å.U., -2.2±.3, 16.4, -2.5.
554 R. DE L. KRONIG [J.O.S.A. & R.S.I., 12
contribution to δ of an absorption band due to such loosely bound
electrons reduces very nearly to
If v is large compared to all the critical frequencies of the atom, then
Now the experimental values for δ in this case are found to check well
with the value obtained by the classical theory on the assumption that
all electrons act as if free:
where Z is the number of electrons per atom. From comparison there
follows
This is a special case of a general condition formulated by Kuhn11
and Thomas.12 Kuhn, moreover, suggests from a consideration of the
scattering activity of atoms at very high impressed frequencies that the
sum of the charges fie of the resonators associated with the absorption,
which arises from transitions of electrons in a given kind of orbit of
the normal state of the atom, is equal to the sum of the charges of
these electrons. One thus would have from (11) in the case of the
inner electrons which give rise only to continuous absorption
where pnk is the number of electrons in the atom in its normal state
occupying nk orbits. For the K-electrons αk(ω) according to various
observers9 is given by (10) with CK about 0.02. This leads to a value
11 W. Kuhn, Zs. f. Phys., 33, p. 408; 1925.
12 W. Thomas, Natuπviss., 13, p. 627; 1925. See also F. Reiche and W. Thomas, Zs. f.
Phys., 34, p. 510; 1925.
June, 1926] X-RAY DISPERSION THEORY 555
for the above integral of about 0.025, while the right-hand side is about
0.05, pK being equal to 2. The discrepancy between these values appears
to indicate that the individual groups of electrons in the atom cannot
be treated independently as regards the connection between their
scattering activity at high frequencies and their absorbing properties.
The experimental data on refraction for an impressed frequency
near one of the frequencies corresponding to an absorption edge are
still too meager and too inaccurate to base any binding conclusions
upon, especially so, since a large part of the refraction comes from the
lightly bound electrons.
It may be remarked here that as regards the constants Cr in (10)
corresponding to absorption edges which form a relativistic doublet
some further information can be obtained from considerations similar
to those applied by Heisenberg13 for an explanation of the summation
rules in multiplets. For when an atom is transferred by removal of an
inner electron from the normal state to either one of two higher states
forming a relativistic doublet, the initial state is the same in both cases.
The total radiative activity of the final states too may be expected to
be the same, for in both the number of electrons in the different nk
orbits is the same. This leads by the familiar argument to the conclusion
that the ratio of the constants C of the two absorption bands, dis
regarding quantities of the order Δω/ω, is that of the statistical weights
j of the final states, a result arrived at by Stoner14 in a different way.
4. THE NATURE OF THE COMPTON SCATTERED RADIATION
If the refracting medium is a light substance, and hard x-radiation
be used, a considerable portion of the scattered radiation appears with
its wave length shifted according to Compton's equation, the relative
intensity of the shifted to the unshifted radiation increasing as the
incident radiation is made harder, while the total amount of radiation
is about what may be expected on the classical theory if all the electrons
in the subsjance were free. This scattering, as is well known, is accom
panied by recoil electrons. The question arises whether the shifted
radiation, in the wave picture, must be considered as coming from the
electrons undergoing recoil, the electrons thus affected radiating very
strongly, or whether all the atoms must be considered as participating
equally in its production, radiating weakly. In actual experiments
13 W. Pleisenberg, Zs. f. Phys., 31 p. 617; 1925.
14 E. C. Stoner, Phil. Mag., 48, p. 719; 1924.
556 R. DE L. KRONIG [J.O.S.A. & R.S.I., 12
carried out here on the index of refraction of carbon for molybdenum
K-radiation, the intensity of the x-rays was at most of the order of
magnitude 1 erg/cm2sec. As approximately 50 per cent of the scattered
radiation is shifted, such an intensity would give rise to about 107 recoil
electrons per cm3 per sec. Since the frequency of the incident radiation
is about 4 • 1018, and there will hardly be more than 106 waves in a wave
train, the time during which an electron is engaged in a scattering
process is not more than 10–12 sec. But if the shifted radiation came only
from the electrons undergoing recoil, the above number of scattering
processes would lead to the result that per cm3 at any time there are very
few electrons or none at all engaged in this kind of scattering. The
Compton shifted radiation could therefore not possibly contribute to
the index of refraction by interference. Since, however, more and more
of the scattered radiation becomes shifted radiation as the frequency
increases, while at these high frequencies the index of refraction appears
always to be what one would expect from the scattering of free electrons
on the classical theory, it is evident that the shifted radiation, too,
must in the wave picture be considered as coming from all the atoms,
and that it must be coherent15 with the incident radiation. This is a case
similar to that of the resonance radiation in atomic gases and vapors.
There, too, the question arises if this resonance radiation, in the wave
description, is to be considered as coming from all the atoms, being
completely coherent with the incident light, or whether at least part
of it comes from atoms in the upper stationary state, emitting strong
radiation with no phase relation to the primary waves. From analogy
one may be inclined to adopt the former view.
This state of affairs is particularly suited to accentuate the difficulties
which one encounters in trying to connect the wave description with
the appearance of the elementary processes, in our case the production
of recoil electrons. These difficulties are all the greater since the experi
ments of Geiger and Bothe16 and of Compton and Simon17 have made
15 The shifted radiation can be considered, as far as the variation of its frequency with the
angle of observation is concerned, as coming from sources moving in the direction of the inci
dent beam with a velocity depending on the frequency of this beam (see A. H. Compton,
Phys. Rev., 21, p. 483; 1923). With coherence of the shifted radiation we mean that, if by a
Lorentz transformation we go to a coordinate system in which the sources are at rest, then in
this system the radiation coming from them has a definite phase relation to the incident
waves. The fact that one does not observe selective reflection in crystals at angles correspond
ing to the shifted radiation does not contradict this, as the moving sources need not start
moving all at the same time so that they no longer form a lattice.
16 W. Bothe and H. Geiger, Zs. f. Phys., 32, p. 639; 1925.
17 A. H. Compton and A. W. Simon, Phys. Rev., 26, p. 289; 1925.
June, 1926] X-RAY DISPERSION THEORY 557
it likely that giving up energy and momentum conservation in the
individual processes, as suggested by Bohr, Kramers, and Slater,18
is not a feasible way out of the dilemma.
DEPARTMENT OF PHYSICS,
COLUMBIA UNIVERSITY,
NEW YORK CITY.
JANUARY 29, 1926.
18 Bohr, Kramers and Slater, Phil. Mag., 47, p. 785, 1924; Zs. f. Phys., 24, p. 69; 1924.