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This article was downloaded by: [Pennsylvania State University]On: 25 September 2013, At: 06:22Publisher: Taylor & FrancisInforma Ltd Registered in England and Wales Registered Number: 1072954 Registered office:Mortimer House, 37-41 Mortimer Street, London W1T 3JH, UK
Contemporary PhysicsPublication details, including instructions for authors and subscriptioninformation:http://www.tandfonline.com/loi/tcph20
Thin film analysis with nuclear methodsKlaus-Peter LiebPublished online: 08 Nov 2010.
To cite this article: Klaus-Peter Lieb (1999) Thin film analysis with nuclear methods, Contemporary Physics,40:6, 385-413
To link to this article: http://dx.doi.org/10.1080/001075199181297
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Thin ® lm analysis with nuclear methods
KLAUS-PETER LIEB
Nuclear physics provides a number of unique methods to analyse thin ® lms in the range of
tens to hundreds of nanometres thickness. This article ® rst describes the basics and recent
applications of the most prominent ion-beam analysis techniques, such as Rutherford
backscattering, nuclear reaction analysis, elastic recoil detection, ion channelling, and
particle induced X-ray emission. The use of microbeams in thin- ® lm analysis will be
sketched. In addition, some nuclear techniques using (implanted ) radioactive probe nuclei
will be shortly described, such as emission channelling, conversion electron MoÈ ssbauer
spectroscopy and perturbed gamma-ray angular correlations. Mainly, such examples have
been selected where combinations of these analysing techniques illustrate their respective
power and limitations.
1. Introduction
The decade leading into the next millenium is that of thin
® lms, be they optical, hard or wear- and corrosion-resistant
coatings, multilayer electronic chips, magnetic or chemical
sensors, nanometre-to-micrometre biological structures,
just to mention a few examples. Such modern materials
are often too complicated in their compositions and
structures so that a single method rarely allows one to
fully characterize their properties and to monitor wanted or
unwanted changes of them during manufacturing or use.
For that reason, the full arsenal of solid-state spectroscopic
tools is being tested to provide the `best’ (most sensitive,
most direct, non-destructive, cheapest ) ways of analysis.
Nuclear physics along its way to investigate subatomic
structures, has developed and optimized a number of rather
simple analysing methods in thin ® lm technology which are
particularly sensitive to properties such as element compo-
sition, crystallinity, lattice locations, defect structures, and
phases. These methods can be used, to monitor the ® lm
properties during manufacturing (quality control ), but also
to investigate changes of the ® lms due to external
in¯ uences, as for example wear, corrosion, ion impact or
laser treatments. It is the aim of the present article to
describe in section 2 the most common nuclear and ion-
beam analytical methods such as Rutherford backscatter-
ing (RBS ), nuclear reaction analysis (NRA ), elastic recoil
detection analysis (ERDA ), channelling, and particle
induced X-ray emission (PIXE ). The basics, advantages
and limitations, as well as some recent applications will be
reviewed in section 2. This section also highlights develop-
ments in microbeam analysis. In section 3, shorter accounts
will be given, concerning methods using implanted radio-
active tracer ions, such as emission channelling, perturbed
gamma-ray angular correlations (PAC ) and conversion
Electron (or X-Ray ) MoÈ ssbauer spectroscopy (CEMS,
CXMS ). Among the powerful and widely used `nuclear’
methods of analysis in thin ® lms, we also have to mention
radiotracer diŒusion, neutron diŒraction, scattering and
capture, nuclear magnetic resonance, positron annihilation,
accelerator mass spectrometry, or muon spin resonance,
which are not the focus of the present survey.
As the ® eld to be covered in this rather short article has
become very broad, care has been taken to ® rst introduce,
for each method, the basic idea, to highlight its application
in one or several examples (many of them selected from
very recent work carried out at GoÈ ttingen University ), and
to ® nally summarize its bene® ts and shortcomings. We
hope that readers having specialized in one ® eld, ® nd this
presentation useful to consider supplementary analysing
methods. For more detailed information they should refer² Author’ s address: II. Physikalisches Institut, UniversitaÈ t GoÈ ttingen,
Bunsenstr. 7-9, D-37073 GoÈ ttingen, Germany.
Contemporary Physics, 1999, volume 40, number 6, pages 385± 413
Contemporary Physics ISSN 0010-7514 print/ISSN 1366-5812 online Ó 1999 Taylor & Francis Ltdhttp://www.tandf.co.uk/JNLS/cph.htm
http://www.taylorandfrancis.com/JNLS/cph.htm
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to [1-6] and to the original papers listed at the end of this
article.
2. Ion beam analysis with stable projectiles
Modern thin-® lm materials are often made up of many
components and tailored in complicated (multilayer )
geometries. For that reason, combinations of ion-beam
analytical and other methods are being employed to
characterize the materials. Figure 1 illustrates a typical
multi-purpose experimental equipment for ion-beam ana-
lysis: the high-vacuum or UHV target chamber is connected
to an ion-accelerator beam and equipped with detectors
suitable for RBS, NRA, ERDA and PIXE and possibly
also ion channelling. In most cases, the accelerator will be
either a Cockcroft± Walton machine, a single-ended or a
tandem van de GraaŒ accelerator, or a cyclotron which
provides well focused, mono-energetic beams of light
particles (protons, deuterons, a -particles ) and possibly
heavy ions (6 ,7Li,
12C,
16 ,1 8O,
35Cl,
40Ar,
58Ni,...).
2.1. Rutherford backscattering spectroscopy (RBS )
2.1.1. Principle. RBS is the most commonly used
nuclear method for elemental depth analysis of nm-to- l m
thin ® lms [6, 7]. It is based on the elastic scattering of a
beam of monochromatic ions (typically 1 ± 3 MeV a -
particles ) at the Coulomb potential of the target nuclei,
and the known energy loss of the beam, D E in , and of the
scattered projectiles, D Eout, on their way into and out of the
target. The principle of RBS is sketched in ® gure 2 (a ): the
beam of projectile ions (nuclear mass M 1 , element number
Z1 , ion energy E1 ) hits the sample at normal incidence. If
the scattering occurs at the depth x from the surface, the
energy E f of the backscattered particles measured at the
angle h relative to the direction of the incoming beam, is
given by
E f 5 k [E 1 2 D E in (x) ] 2 D E out (x) . (1)
The kinematical factor
k 5 [M2 cos h 1 (M 22 2 M 2
1 sin2h )
1 /2]2/[M1 1 M2]
2(2)
depends on the mass (es ) M 2 of the target nuclei. Knowing
the stopping power dE1/dx of the projectile in the material,
the combined energy loss D E in (x )+ D Eo ut (x ) is a measure of
the depth x. The diŒerential cross-section for Rutherford
scattering in a laboratory system for the projectile energy at
depth x, E1 ¢ = E1- D E in (x )= E1-o & X (dE1/dx ¢ ) dx ¢ ,
d r /d R 5 [Z1Z2e2/2 E 1 sin2
h ]2 D x , (3)
depends on the nuclear charge (s ) Z 2e of the target nuclei.
Here multiple scattering and energy straggling of the
Figure 1. Typical experimental set-up for ion beam analysis
providing detectors for charged particles (Rutherford back-
scattering spectrometry= RBS, elastic recoil detection analysi-
s= ERDA, nuclear reaction analysis= NRA ), X-rays (PIXE:
Si ± Li detector ) and c -rays (PIGE: Ge-HP ). The acronym PIGE
stands for proton-induced gamma-ray emission, Ge-HP for high-
purity germanium detector. The analysing beam enters from the
right.
Figure 2. (a ) Geometry of RBS analysis. (b ) Geometry of
RNRA analysis using a proton beam and a Ge detector.
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projectiles have been neglected. The factor
D x 5 [(1 2 (M1 sin h /M2)2)1 /2 1 cos h ]
2/
[1 2 (M1 sin h /M2)2) ]
1 /2(4)
approaches 4 cos4 (h /2 ) in the limit M 1 < < M 2 , in which
case one obtains k ® 1 and
d r /d R 5 [Z1Z2e 2 /4 E ¢1]2
sin 2 4( h /2) . (5)
For a given number of projectile ions, the yield and energy
spectrum of the backscattered particles (RBS spectrum dN /dE f ) depend on the concentration pro® le of the target
atoms, c2 (x ). Several computer codes are available [8,9] to
deconvolute RBS spectra. Evidently, the dependence of the
cross-section on Z22
enhances the detection sensitivity to
heavy elements, while the dependence of the kinematical
factor k on M 2 shifts the signals from the heavy elements to
the upper part of the spectrum where they overlap least
with the lighter mass components.
2.1.2. Examples. The ® rst example selected refers to the
analysis of polycrystalline Ag± Fe bilayers deposited onto Si
wafers and their behaviour under irradiation with Xe ions
(ion beam mixing ). This system oŒers a high dynamic
contrast, due to the large diŒerence in mass and element
numbers of the three components (Ag: Z2 = 47, M 2 »108 amu; Fe: Z2 = 26, M 2 » 56 amu; Si: Z2 = 14; M 2 »28 amu ). The signals from all three components are well
separated in the backscattering spectra taken with 0.9 MeV
a -particles as shown in ® gure 3 (a ). When irradiating such
multilayers with 750 keV Xe+ +
-ions at 77 K, one notes
that the edges of the concentration pro® les at the Ag± Fe
interface get less and less steep with the increase of the ion
¯ uence U . From this observation, one was tempted to
conclude that the Ag± Fe interface roughens, due to the
mutual ion-induced transport of Ag atoms into the Fe layer
and vice versa (ion beam mixing ). However, on the basis of
STM analyses of the Ag surface, Crespo-Sosa et al. [10,11]
realized that the ion irradiation roughens the surface and
leaves the Ag ± Fe ¯ at! Indeed as shown in ® gure 3 (b ), the
diŒerence of variances measured via RBS and STM,
d r 2 (U ) º D r R BS2 (U )- D r S TM
2 (U ), is consistent with zero.
This phenomenon can be understood if we assume that
the elements in the ballistically mixed Ag± Fe interface zone
segregate as a consequence of local thermal spikes initiated
Figure 3. Athermal mixing of an Ag ± Fe bilayer via a 750 keV
Xe+
-ion beam [10, 11]. (a ) RBS spectra taken with a 0.9 MeV
a -particle beam before and after a Xe irradiation at 77 K. Note
the reduction of the thickness of the Ag top layer due to
sputtering and its increase of the variance of the Ag layer
thickness. (b ) DiŒerence of the ion-induced variances in the Ag
layer thickness obtained via RBS and STM, d r 2= D r R B S
2±
D r S T M2, as a function of the ion ¯ uence U . The three curves refer
to sequential (top ) or single irradiations (middle ) at 77 K and
single irradiations at 300 K (bottom ). As d r 2is consistent with
zero and less than the prediction of the ballistic model (dashed
lines ), it must be concluded that the Ag/Fe interface stays ¯ at
and that the Ag surface roughens.
Thin film analysis with nuclear methods 387
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by the energetic Xe ions [12 ± 14]. Note that Ag and Fe are
not thermally miscible. The increase of the variance
D r ST M2 (U ) indicates an ion-induced roughening and grain
growth at the surface of the Ag layer [11].
The second example refers to a recent study by Schaaf
and co-workers [15 ± 18] on the laser nitriding of armco iron
via short pulses of a XeCl excimer laser (pulse duration
55 ns, average energy density 2 ± 8 J cmÐ 2 ). Many facets of
this complicated and technically important process have
been understood on the basis of nuclear techniques such as
RBS, RNRA and MoÈ ssbauer spectroscopy (see [18] and
below ). The high energy density of the laser beam melts
about a 1 l m thick surface layer and may lead to several
transport processes such as turbulent ¯ ow, ablation and
ejection of the melt by the plasma pressure. These transport
properties have been made visible through RBS by
introducing a 10 nm thin Au layer into the Fe sample at a
depth of 60 nm below the surface, before laser irradiation.
Figure 4 illustrates RBS spectra taken at 0.9 MeV a -particle
energy before and after applying 1 and 4 laser pulses:
clearly, already the ® rst laser pulse fully dissolves the Au
marker layer and leads to a uniform distribution of the
marker, as can be seen by the ¯ at Au distribution between
690 and 830 keV a -energy in the RBS spectrum [15].
2.1.3. Depth and mass resolutions, eŒects of roughness.
The depth resolution D x » D E (dE/dx )Ð 1
to be achieved in
RBS depends on the energy precision of the primary beam,
r 12, the energy straggling of the beam on its way into and
out of the target, r S2, the variation of the backscattering
energy due to the ® nite solid angle of the detector, r X2, and
the energy resolution of the detector, r det2:
D E » ( r 21 1 r 2
S 1 r 2 1 r 2de t)
1/2. (6)
For a well-stabilized, low-energy Cockcroft± Walton accel-
erator, r 1 is of the order of 0.05 ± 0.15 keV at E1 < 0.5 MeV
[19], while for a 2 ± 5 MeV van de GraaŒ or tandem
accelerator, r 1 » 1 keV. Electronic straggling, r S2, can be
estimated via Bohr’ s expression [20],
r2S » 4p e 2
Z21 Z2 N2 x(1 1 1 /cos h ) , (7)
where N2 denotes the atomic density of target atoms and x
the depth of the scattering process in the ® lm; the quantity
x (1+ 1/cos h ) is then the full path length traversed by the
projectile. For a -backscattering from a Fe ® lm (Z2 = 26,
M 2 » 56 amu, h = 165 8 ), r S increases as 12 from about
2 keV for x = 10 nm to some 10 keV at 200 nm.
The main contribution to the depth resolution there-
fore is usually derived from the energy resolution of the
detector, r d et. For the most commonly employed Si
surface barrier detectors having a very thin ion-
implanted Au top layer towards the target, r det = 11 ±
13 keV. Alternative solutions to improve the detector
resolution have been developed by using electrostatic or
magnetic spectrometers [21,22]. In the best cases, an
energy resolution as small as < 1 keV has been achieved
Figure 4. RBS spectra and deduced Au depth distributions of an armco Fe sample containing a 10 nm Au marker layer at a depth of
60 nm and irradiated with 1 or 4 pulses of a XeCl excimer laser [15].
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using a magnetic analyser, which leads to a depth
resolution of about a monolayer at the surface of the
sample [22,23].
RBS averages with respect to the ¯ uctuations in ® lm
thickness and density over the spot size of the analysing
beam (typically 1 ± 5 mm2
if no microbeam is used ). As a
consequence, the tails of the edges in the RBS spectrum
directly re¯ ect these ¯ uctuations, but they do not allow one
to distinguish between surface roughness and interface
roughness if the thin ® lm is deposited on another thin ® lm
or on a substrate. The eŒect of surface roughness has
recently been studied by Metzner et al. [24,25] for
polycrystalline, 10 ± 500 nm thick In ® lms deposited via
evaporation from a Knudsen cell onto nanometre smooth
Si wafers. Figure 5 illustrates RBS spectra obtained at 0.9
a -energy for two rather thick samples. A scanning electron
microscopy (SEM ) analysis showed the presence of In
droplets of several hundred nanometre diameter on the
surface of sample #12. An analytical description of this
surface topography has been inferred by assuming a height
probability function p (h ) which is composed of two
fractions: the droplet part pD (h ) is represented via hemi-
spheres of radius R , pD (h )= (4fD / p R2 ) (R
2± h
2 )12, while the
non-structured part of the ® lm is approximated by a
Gaussian distribution (fraction fG = 1 ± fD , average thick-
ness < h> , variance r h2 ). Fits to the RBS spectra gave the
parameters listed in table 1. A comparison of the spectra
taken at 0.9 and 2.0 MeV a -energy and the errors given in
table 1 shows that the lower a -energy provides better depth
resolution, while the higher a -energy provides better mass
resolution. This diŒerence is due to the variation of the a -
particle stopping power.
Figure 5. RBS spectra obtained at 0.9 MeV a -particle energy from two thick In ® lms deposited via evaporation onto Si substrates. The
inserts illustrate the height distributions p (h ) whose parameters are listed in table 1 [25].
Thin film analysis with nuclear methods 389
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2.2. Nuclear reaction analysis (RNRA )
2.2.1. Principle. While Rutherford scattering enhances
the heavy components of the target to be analysed, nuclear
reaction analysis (NRA ) induced by protons or a -particles
of some 100 keV up to several MeV is most useful for depth
pro ® ling the light components of ® lms. Since almost all
modern ceramic materials contain carbon, nitrogen and
oxygen, NRA, in particular in combination with proton-
induced resonance reactions (RNRA ), has become very
popular for depth pro® ling these light components. Since
RNRA is not only depth sensitive, but selects particular
target isotopes, this technique opens the way to detailed
isotope-sensitive studies (we mention corrosion in18
O-
enriched gases or ¯ uids [26] and nitriding in15
N-enriched
atmospheres [27] ).
In ® gure 2 (b ), the basic principle of RNRA is sketched
for a reaction having a narrow resonance at energy ER and
total resonance width C , in the laboratory frame. Neglect-
ing any non-resonant processes and the dependence of the
resonance width parameters on the beam energy, the cross-
section over the resonance follows the Breit± Wigner
formula
r (E 1) 5 r 0 G in G out /[(E 1 2 E R )2 1 G 2 /4], (8)
where r 0 is a constant and C in and C out denote the partial
widths of the entrance and exit channel of the resonance,
respectively. The yield of the resonance reaction can be
monitored by measuring the emitted charged particles and/or subsequent c -radiation of the ® nal nucleus. Generally,
the analysing beam (say protons at energy E1 ) hits the
sample at normal incidence. In ® rst approximation, if
E1 = ER , the resonance reaction evidently selects nuclei
located at the surface. If E1 > ER , the resonance occurs at
the depth x = (E 1 ± ER ) (dE 1/dx )Ð 1
. By measuring the yield
function Y (E1 ) for constant projectile number (accumu-
lated charge ) and varying the beam energy E1 in small
steps, the yield function Y (E1 ) can be deconvoluted into the
desired concentration pro® le c2 (x ). Of course, the ® nite
resonance width C , the beam spread of the accelerator and
the energy straggling of the projectiles in the target have to
be considered in the analysis. A survey of reactions suitable
for NRA is given in [28 ± 30]. Table 2 lists some useful low-
energy proton-induced resonance reactions (E 1 < 0.5 MeV )
whose resonance parameters ER and C have been measured
at the GoÈ ttingen high-resolution implanter IONAS and
which are appropriate for depth-pro® ling the isotopes14 ,1 5
N,18
O,19
F,23
Na,24 ± 26
Mg and27
Al [19].
2.2.2. Examples. Important details of the laser nitriding
process [16, 18] already discussed in section 2.1 have been
revealed by RNRA using the prominent15
N (p, a c )12C
resonance at 430 keV for depth-pro® ling the nitrogen
isotope15
N (see table 2 ). The 4.43 MeV c -radiation in12
C emitted in this reaction is recorded in a 12 cm long,
16 cm wide NaI detector and the 2.0 l A proton beam is
scanned in 5 keV steps over the resonance. When
deconvoluted, the c -ray yield curve Y c (E1 ) provides the
desired15
N concentration pro® le. Usually, the 0.37%
abundance of the isotope15
N present in natural nitrogen
is su� cient for such analyses. If the laser nitriding process
is carried out in atmospheres of enriched15
N content, the
eŒect of single laser pulses within a series of multiple
irradiations can be highlighted [15,17,27]. Figure 6 illus-
trates nitrogen depth pro® les obtained when irradiating the
Fe sample with up to 256 pulses of a homogeneous XeCl
excimer laser beam at an average energy density of
4.0 J cm2
[17]. While the ® rst pulse induces a more or less
exponential nitrogen pro® le and very little nitriding, each
subsequent pulse increases the nitrogen content at depths
larger than 20 nm, until a saturation pro® le develops after
some 128 pulses, equivalent to cN (x )= 12 at.% at depths
x> 100 nm. At the surface, saturation is already reached
Table 1. Fit parameters of rough In layers deposited onto Si
wafers and covered with hemispherical in droplets [25].
Sample Ea
(MeV )
fD
(% )
R
(nm )
< h>
(nm )r h
(nm )
hm
(nm )
#11
#12
#12
0.9
0.9
2.0
58 (2 )
68 (1 )
68 (3 )
460 (12 )
217 (1 )
208 (4 )
614 (1 )
277 (1 )
261 (4 )
71 (1 )
54 (2 )
54 (4 )
492 (1 )
224 (1 )
205 (4 )
Table 2. Useful proton resonances for RNRA below
E1= 500 keV.
Reaction ER (keV )a G (eV )a W (eV )b Reference
14N (p, c )1 5
O15
N (p, a c )12C
18O (p, a )15
N19
F (p, a c )16O
23Na(p, c )24
Mg24
Mg (p, c )25Al
24Mg (p, c )26
Al
26Mg (p, c )27
Al27
Al (p, c )28Si
277.60 (27 )
429.57 (9 )
150.97 (26 )
223.99 (7 )
340.46 (4 )
483.91 (10 )
308.75 (6 )
222.89 (8 )
316.16 (11 )
389.24 (11 )
434.85 (12 )
496.75 (12 )
292.06 (9 )
222.82 (10 )
293.08 (8 )
326.97 (5 )
405.44 (10 )
446.75 (15 )
1115 (15 )
125 (16 )
178 (30 )
985 (20 )
2340 (40 )
903 (30 )
< 36
< 32
< 37
< 4
< 44
< 51
< 37
< 34
59
< 38
< 42
40 (5 )
60 (5 )
53 (5 )
48 (5 )
62 (5 )
72 (5 )
64 (5 )
52 (5 )
68 (5 )
82 (5 )
85 (5 )
95 (7 )
69 (5 )
57 (5 )
70 (5 )
73 (5 )
87 (5 )
96 (6 )
c
[31]c
[19]
[19]
[32]
[19]
[19]
[19]
aEnergies ER and G in the laboratory system.
bBeam ripple and Doppler broadening at room temperature.
cK. P. Lieb, private communication.
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after 8 laser pulses. On the basis of the depth and lateral
nitrogen pro® les and other quantities like surface pro® le
and hardness, Schaaf and co-workers [15, 16] developed a
scenario which accomodates various aspects of the laser±
plasma± melt± solid interactions, the nitriding eŒect and
other transport processes due to laser irradiation.
The second example presented refers to the analysis of
magnetron-sputtered FeN layers, a recently identi ® ed phase
in the otherwise well-documented Fe± N phase diagram
[33,34]. This system can be ideally analysed by combining
RBS, which is sensitive to the Fe concentration pro® le,
and RNRA, again using the15
N (p, a c )12C resonance
reaction for depth pro® ling the N concentration. Figures
7 (a ) and (b ) illustrate the N and Fe depth pro® les
obtained in this way [35], together with the depth pro® les
of all elements deduced from an ERDA analysis (® gure 7
(b ), see section 2.3 ). The relative calibrations of the two
methods pose a certain problem. In the case of RNRA
one may use stoichiometric CrN or TiN ® lms. As long as
only Fe and N are present in the ® lms, this combination
of methods works very well and the typical error of
stoichiometry amounts to 1 ± 2% . If additional (light )
elements such as carbon or oxygen are present in the
® lms, one cannot quantitatively determine their contents
via RBS, while RNRA would require appropriate
resonance reactions for each element. Under such condi-
tions, ERDA oŒers an elegant alternative for multi-
element analysis (see ® gure 7 (b ) and section 2.3 ).
2.2.3. Depth resolution and sensitivity. The depth resolu-
tion of RNRA, D x » D E (dE /dx )Ð 1
, depends on similar
quantities as for RBS. The achievable energy resolution D E
is again in¯ uenced by the energy precision of the beam, r 1 ,
and the straggling of the projectile, r S, on its way from the
surface to the depth x, where the nuclear reaction takes
place. In addition, the Doppler broadening due to the
thermal motion of the capturing target nuclei, r D op p, and
the resonance width C in¯ uence the energy resolution:
D E » ( r 21 1 r 2
Dopp 1 G 2 1 r 2S )
1/2. (9)
Using a highly stabilized proton beam (e.g. that of IONAS )
and the very narrow resonances listed in table 2, the energy
ripple of the beam and the Doppler broadening at room
temperature, W = (r 12+ r D o pp
2 )12 increase from 50 eV to
100 eV for E 1 = 100 ± 500 keV [19]. Therefore, the energy
resolution D E mainly re¯ ects the energy straggling r S of the
proton beam in the target, leading to depth resolutions of
some 10 ± 20 nm at x » 100 ± 300 nm. If straggling can be
avoided, i.e. when using RNRA at the surface, the depth
resolution can be reduced to less than 1 nm and RNRA has
even been used to study, e.g. atoms adsorbed at surfaces
[37].
Figure 6. Laser nitriding of armco iron by a XeCl excimer laser
beam. The curves represent the nitrogen depth pro® les for n= 1
up to n= 256 laser pulses obtained via RNRA by means of the
reaction15
N (p, a c )12C [17].
Figure 7. Analysis of magnetron-sputtered FeN ® lms on Si
substrates highlighting the depth pro® les of various elements in
the sample [35,36]. (a ) N depth pro® le obtained from RNRA and
the reaction15
N (p, a c ); (b ) TOF-ERDA analysis using a 37 MeV197
Au beam and glancing geometry. Note the contents of carbon
and oxygen not observed in (a ) nor in (c ); Fe depth pro® le
obtained from RBS using 0.9 MeV a -particles.
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2.3. Elastic recoil detection analysis (ERDA )
2.3.1. Principle. This ion-beam technique, which was
pioneered in the seventies mainly for the purpose of
hydrogen pro® ling [38 ± 42], has very much developed in
thin-® lm analysis during the last decade, especially for
depth pro® ling of light and medium-mass elements, and
some very sophisticated instrumentation has been designed.
The recent review by Tirira et al. [43] covers these
developments. The main diŒerence between ERDA and
RBS and NRA is the use of heavy projectiles M 1 > M 2 . Due
to energy and momentum transfer during the nuclear two-
body collision with the target nucleus (scattering or
reaction ), a pair of energetic ions is produced and either
the scattered ion (Z1, M 1 ) or the ejected recoil atom (M 2 ,
Z2 ), or both, may leave the sample and are analysed. In the
case of an appropriate geometry (see ® gure 8 ), both
particles may be measured in coincidence. Again, the
energy losses of the projectile before, during and after the
collision and the stopping of the associated recoil atom on
the way out of the sample determine site x of the reaction
within the target.
Figure 8 illustrates the two basic experimental set-ups
used in ERDA [44]. In order that both particles can be
observed, the technique is either used for thin, self-
supporting ® lms (transmission geometry ) or at very small
incidence and ejection angles with respect to the ® lm
normal (glancing geometry ). For pure Rutherford scatter-
ing, the diŒerential cross-section for recoil mass M 2 at an
angle / with respect to the direction of the primary beam is
given in the laboratory frame as
d rrec
/d R 5 [Z1Z2e 2 /2E ¢1 ]
2[M1 1 M2) /M2]
2cos 2 3 u ,
(10)
where E1 ¢ again denotes the projectile energy just before the
collision.
As in RBS, the simplest way to use ERDA is the
measurement of the projectile and/or recoil energy spec-
trum Y (E f ) which contains information about the concen-
tration depth pro® les c2 (x ) within the analysed ® lm and can
be deconvoluted in a similar manner. However, as long as
one does not diŒerentiate between the projectile and the
ejected (recoil ) species, there exists an ambiguity concerning
the fractions of energy shared between both partners.
Depending on their masses M 1 and M 2 , particles from
diŒerent depths can have the same energy. This leads to a
mass± depth ambiguity or, in the forward direction, to a
recoil± projectile ambiguity [44].
Several remedies have been tested to solve this problem.
The simplest solution is the use of absorber foils in which
the diŒerent ions experience diŒerent energy losses,
depending on their mass, element number and energy.
High-resolution magnetic spectrometers, combinations of
Figure 8. Typical set-ups of ERDA in glancing and transmission geometry used to depth-pro® le hydrogen via impact with a4He beam
[43].
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electric and magnetic ® elds (ExB ® lters ) or a gas ionization
chamber in conjunction with the silicon surface barrier
energy detector have also been used for particle identi ® ca-
tion [45 ± 47]. A quite universal and experimentally still
straightforward version of ERDA which oŒers mass and
element identi ® cation, is sketched in ® gure 9. Via a time-of-
¯ ight spectrometer (mass ), combined with a D E -E telescope
(element number, energy ), all three quantities can be
determined. This technique is called TOF-ERDA. The
¯ ight path is de® ned by an electrostatic start detector,
usually a thin carbon foil emitting secondary electrons
during the very short passage time of the ion. These
electrons are collected via an arrangement of electric ® elds
and mirrors and guided to a microchannel plate where they
produce a nanosecond sharp time mark. As stop detector,
one can either use a similar electrostatic detector or directly
the thin D E surface barrier Si detector of the telescope.
2.3.2. Examples. The example for ERDA with coinci-
dence spectroscopy shown in ® gure 10 refers to the analysis
of self-supporting polycarbonate foils (C16O3H14 ) by means
of a 2 MeV a -beam [49]. In order to remove the projectile ±
recoil ambiguity, coincidences were required between the
forward-scattered a -particles (h = 70 8 ) and the O and C
recoil atoms (/ = 48 8 ). Figures 10 (a ) and (b ) illustrate the
3-dimensional energy± energy-intensity histogram, and a
projection of it onto the energy± energy plane, which the
distribution of oxygen and carbon in the foil can be
deduced from.
The properties of magnetron-sputtered FeN layers have
been studied by Rissanen et al. [35, 36] via glancing ERDA
(as well as RBS, RNRA and MoÈ ssbauer spectroscopy, see
sections 2.2 and 3.2 ). The stoichiometries of the ® lms and
the occurrence of contaminants were investigated, depend-
ing on the deposition parameters in the HF magnetron (gas
mixture, substrate temperature, HF power ). The analysis of
light elements was carried out by means of a TOF-ERDA
spectrometer [48] set up at the University of Helsinki
tandem accelerator using a 37 MeV197
Au beam (see ® gure
9 ). The element depth pro® les of a nearly stoichiometric
FeN ® lm on a Si substrate containing very few contami-
nants of carbon and oxygen are plotted in ® gure 7 (b ). When
comparing the bene® ts and limitations of RBS, RNRA and
ERDA in this particular example, one clearly would prefer
ERDA as long as depth resolution is not the critical
parameter.
2.3.3. Depth and mass resolution, sensitivity, limitations.
The wide range of target± projectile combinations and
geometries in ERDA usually does not provide a general
estimate of the achievable depth and mass resolutions [43].
With 3 MeV a -particles, depth resolutions of 10 ± 40 nm
have been reported for H-pro® ling in silicon [50, 51]. Using
a 60 MeV12
C beam of the Munich tandem accelerator and
a Q3D magnetic spectrograph, Dollinger et al. [45] recently
achieved atomic resolution for the (0002 ) layers of a highly
oriented pyrolytic graphite (HOPG ) crystal, in glancing
geometry (h = 96 8 ). As mentioned before, one can orient
the sample in such a way as to allow both the projectile and
recoil to travel out of it so that their energies (and masses )
can be measured in coincidence. Whenever the sample can
be manufactured as a self-supporting thin foil, the
transmission geometry is preferred for the following
reasons [44].
(a ) It facilitates coincidence measurements with large
detector solid angles.
(b ) The maximum probing depth is larger than in
glancing ERDA, since the analysing beam enters at
normal incidence.
(c ) The depth resolution does not depend on the surface
roughness (which is a very important limitation in
glancing geometry ), but rather on the homogeneity
of the ® lm.
(d ) The mass resolution d = d E2/ d M2 of the device is
de ® ned via the energy diŒerence d E2 of recoil atoms
after the collision, when two types of atoms diŒer by
the quantity d M 2. The calculated mass resolution din transmission ERDA [43] as a function of M 2 is
plotted in ® gure 11 for the four projectile beams4He,
16O,
35Cl and
58Ni, which all are easily available
at tandem accelerators. One notes the poor resolu-
tion for M 1 = M 2 . This graph shows that4He beams
are best suited to diŒerentiate between the hydrogen
isotopes and in the mass range M 2 = 10 ± 30 amu,
while16
O ions are recommendable for pro® ling
heavier nuclei (M 2 = 30 ± 80 amu ).
2.4. Ion channelling
2.4.1. Principle. While RBS, NRA and ERDA generally
determine the concentration pro® les of elements or isotopes
in thin ® lms, channelling uses well focused ion beams for
getting information on the crystallinity of the sample and/
Figure 9. Time-of-¯ ight ERDA arrangement [48].
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or the lattice locations of dopants or self-atoms. Channel-
ling rests on the intuitive idea that positive ions, mostly
protons, a -particles and other light ions, travelling along an
`open’ (axial or planar ) channel in a crystal experience
fewer collisions and therefore a reduced energy loss. What
is more important, the channelled ions are focused by the
ion cores aligned along the boundary atomic rows of the
channels. Any atom located within the channel therefore
constitutes a collision centre (for reactions or backscatter-
ing ) and in this way adds to the stopping process [52 ± 56].
The theory of channelling was ® rst worked out, for
example, by Lindhard and by Leibfried [56] in the limit of
the `continuum channel potential’ (see ® gure 12 )
Ua (r ) » (Z1Z2e 2 /d) ln (3a /r )2 1 1]. (11)
Here the quantity d denotes the distance of neighbouring
Figure 10. Coincidence ERDA analysis of a self-supporting polycarbonate ® lm with a 4 MeV4He
+ +beam in transmission geometry
[49]. (a ) Histogram of the energies of recoil atoms (Ereco il ) and scattered He-projectiles (EH e ). (b ) Projection of the histogram shown in(a ) onto the Erec o il-EH e plane.
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atoms in the row, a the Thomas± Fermi screening length
and r the distance of the moving ion Z 1 from the row. This
potential gives rise to a critical tilt angle w c (relative to the
channel direction ) up to which the incoming ions are being
axially guided (transmitted ) within the channel:
c 5 (Z1Z2e 2/E
¢1 d )
1 /2|ln [3a / q )2 1 1]|1 /2
. (12)
The quantity q is approximately 2/3 of the mean square,
lattice vibrational amplitude and E1 ¢ is the energy of the
impinging ion inside the crystal:
E ¢1 5 Ua (r ) 1 (p1^ 2 /2M1) 1 (p15
2 /2M1) , (13)
where p1 ^ and p1 | | denote the transversal and long-
itudinal components of the projectile momentum relative
to the channel axis. For 1.0 MeV a -particles incident
onto Si < 110> at room temperature, the calculated
critical tilt angle is w c = 0.65 8 which compares fairly
well with the measured value w c = 0.55 8 [55]. Similar
Figure 11. Mass resolution d j /dM 2 calculated as function of M 2 , for analysing beams of4He,
16O,
35Cl,
58Ni and
63Cu [43].
Figure 12. The ion beam entering from the left is partly transmitted through the crystal channel and partly rescattered from surface
atoms (shadow cone ).
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expressions have also been derived for planar ion
channelling conditions.
2.4.2. Examples. Figure 13 shows an example illustrat-
ing the lattice locations of Yb impurity atoms in silicon which
have been implanted at 60 keV and 450 8 C, at a ¯ uence of
5 ´ 1014
ions cmÐ 2
. The normalized backscattering yield of
1.0 MeV a -particles is plotted versus the tilt angle h relative
to the < 110> channel. The Si signal (full line ) shows the
expected channelling dip proving the crystalline structure of
the matrix after implantation, while the Yb signal (broken
line ) indicates a ¯ ux peaking eŒect arising from the
interstitial lattice location of the implanted Yb ions [52].
The second example refers to the solid phase epitaxial
regrowth (SPEG ) of ion-irradiated SiO2 (a -quartz ) sam-
ples. Even small ion ¯ uences are known to damage
monocrystalline SiO2 to such an extent as to destroy the
long-range crystalline order. For instance, 50 keV20
Ne
ions produce a coherent amorphized layer at a ¯ uence of
only 1 ´ 1014
ions cm2
[57]. On the other hand, the short-
range order of Si and O atoms, i.e. the degree of
connectivity, is usually preserved up to much higher ion
¯ uences and even for ions as heavy as Xe. For this reason,
the conventional method of solid-phase epitaxial regrowth
via post-annealing of the irradiated samples in vacuum has
never been successful [58, 59]. Bolse and co-worker [60 ± 62]
have recently solved this longstanding problem and, indeed,
succeeded in preserving or achieving full recrystallization of
ion-beam amorphized SiO2. In all these studies, RBS
channellng was the key method of investigation of the
crystalline structure of the amorphized and recrystallized
SiO2 surface layers.
Dahr et al. [60] investigated SPEG of Ne-irradiated a -
quartz via dynamic annealing up to 980 K, by searching for
the balance between damage accumulation and annealing,
as a function of the ion ¯ uence U and the sample
temperature T. Figure 14 illustrates RBS-channelling
spectra taken after implanting 1 ´ 1015 20
Ne ions cmÐ 2
at
50 keV and for the substrate temperatures indicated. One
notes that the damage (degree of amorphization ) decreases
for increasing substrate temperature and that all damage
completely disappears at the critical temperature
Tc » 970 K. If one applies lower ion ¯ uences, SPEG can
be achieved at lower temperatures. Figure 15 displays the
temperature dependence of the critical ¯ uence U c , i.e. that
of Ne-ion ¯ uence at which defect production accumulates
to form an amorphous layer. One notes that at T » 980 K,
F c steeply increases, indicating that SPEG wins over
amorphization at any ion ¯ uence. The temperature
dependence of the critical ¯ uence U c can be parametrized
by the defect out-diŒusion model by Morehead and
Crowder [63] and is compatible with an activation energy
of Ea = 0.28 (2 ) eV. (In passing we note that the back-
scattering spectra from both the virgin and fully recrys-
tallized samples show a small peak at the surface. This peak
arises from the non-channelled scattering of the a -particles
at the surface Si atoms; it depends on the propeties of the
bulk surface and contains information about reconstruc-
tion and relaxation of the surface and adsorbed atoms or
molecules. )
While dynamic annealing tries to avoid damage accu-
mulation during the process of implantation, Roccaforte
and cok-workers [61, 62] studied the epitaxial recrystallisa-
tion of alkaline-ion irradiated a -quartz in air. In these
experiments, single-crystalline (0001 ) a -quartz samples were
irradiated at 77 K with 250 keV Cs+
ions to a ¯ uence of
2.5 ´ 1016
ions/cm2. The c axis of the crystal was misaligned
Figure 13. Channelling analysis of a Si sample doped with
5 ´ 1014
Yb-ions cmÐ 2
via 60 keV ion implantation at 450 8 C.
The a -particle backscatter yields from Si and Yb as function of
the tilt angle relative to the < 110> channel direction in the Si
matrix are shown. The yield functions demonstrate that the Yb
implants are located on intersitial sites, while the Si matrix has
stayed single-crystalline [52].
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by 6 8 relative to the beam direction to prevent channelling
eŒects during implantation. Isochronal annealings (1 h )
either in an air furnace or in vacuum at 2 ´ 10Ð 6
mbar were
carried out at 500 ± 900 8 C. An important result of these
measurements is illustrated in ® gure 16, which shows RBS-
channelling spectra of Cs-irradiated samples individually
heated in air to the temperatures indicated: the recrystalli-
zation process starts around 800 8 C and is fully completed
at 875 8 C where the backscatter spectrum cannot be
distinguished any more from that of a virgin single crystal.
As shown in ® gure 16 (bottom ), the recrystallization speed
v (T ) follows an Arrhenius dependence governed by an
activation energy of Ea = 2.83 (20 ) eV. Also indicated in
® gure 16 (top ) is the RBS signal of the pro ® le of the
implanted Cs which shows its migration during annealing:
the as-implanted Gaussian pro® le broadens to a box-like
shape at 700 8 C, with Cs penetrating deeper into the sample
until reaching the amorphous± crystalline interface around
800 8 C. Finally, all Cs migrates to the surface and leaves the
sample at 875 8 C, where complete recrystallization of the
matrix was achieved. Previously, SPEG of Si- and O-
irradiated Brasilian quartz was observed by Devaud et al.
[64] to occur around 1050 8 C under air. Similar self-
implantation experiments in a -quartz did not show any
recrystallization up to 875 8 C [61]. Control experiments
were also carried out with132
Xe,23
Na and7Li ions. While
annealing in air of the alkali-ion irradiated samples resulted
in SPEG, no epitaxial recrystallization was observed after
the Xe implantations nor after annealing in vacuum.
The peculiar in¯ uence of Cs (or other alkali ions studied
such as Li and Na ) on the recrystallization process of a -
quartz can be explained by topological arguments. Amor-
phous and crystalline SiO2 consist of networks of corner-
Figure 14. RBS-channelling spectra from single-crystalline SiO2 samples obtained after 50 keV Ne+
implantations at a ¯ uence of
1 ´ 1015
ions cmÐ 2
, measured at the substrate temperatures indicated [60].
Figure 15. Temperature dependence of the critical ¯ uence U c
for amorphization of SiO2 (a -quartz ) via 50 keV20
Ne ion
bombardment [60]. At 970 K, recrystallization balances amor-
phization at any ¯ uence. The ® t to the data is based on the model
of Morehead and Crowder [63] and corresponds to the values of
the activation energy Ea and critical temperature Tc indicated.
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sharing [SiO4] tetrahedra, having four oxygen vortices, each
of them common to two adjacent [SiO4 ] tetrahedra. Recent
theoretical modelling of the network structure [65] suggests
that SiO2 is fully connected in the ordered and in the
amorphous phase. The ability of a random network to
epitaxially recrystallize strongly depends on the connectiv-
ity of the tetrahedra. The introduction of alkali ions into
the SiO2 matrix, regarded as network modi® ers, breaks up
the network, generates non-connected tetrahedon corners
and increases the recrystallization probability. Most likely,
the role of oxygen during annealing relies on the formation
and disintegration of alkali oxides. This hypothesis can be
checked by annealing the samples in enriched18
O and
measuring the18
O concentration pro® les, via ERDA or the18
O (p, a ) resonance reaction [62].
2.5. Particle induced X-ray emission (PIXE )
2.5.1. Principle. In the true sense, PIXE is not a
nuclear technique, since the ionization of the atoms of a
thin-® lm sample by charged-particle impact (electrons,
protons, ions ) and the subsequent emission of character-
istic X-rays are purely atomic electromagnetic processes.
Furthermore, only under very special conditions PIXE
provides information on depth pro® les of the elements
within the sample. Nonetheless, PIXE ranges among the
most common ion-analytical methods of thin ® lms, as it
provides detailed information about the (generally aver-
age ) element composition of the sample and is able to
detect elements at the sub-ppm concentration level. For
that reason a short outline of PIXE is being included in
this article.
PIXE has been widely documented, and we refer to some
recent survey articles [66 ± 69]. In general, one uses a proton
beam at an energy E1 close to the Coulomb barrier EC » Z 2/M 2
1 /3 of the lightest element (Z 2 ,M 2 ) to be detected in order
to avoid nuclear reactions taking place. A more recent
development of PIXE in thin ® lm analysis, called diŒer-
ential PIXE [31], uses the strong decrease of the K-hole
production cross-section r K toward smaller proton energies
which restricts X-ray emission to the top layer of the ® lm or
substrate. Figure 17 (a ) shows the normalized K-ionization
cross section r K (EK 2/Z1 )2 as a function of the proton
energy E1/EK 2 [67], normalizd to the K-shell binding energy
EK 2 of the matrix atom. As the K a X-ray emission strongly
competes with the emission of Auger electrons in low-Z2
substrates and therefore gives a ¯ uorescence yield x X < 1,
the K a X-ray yield rises sharply with the proton energy, but
Figure 16. Solid state epitaxial recrystallisation of SiO2
irradiated with 250 keV Cs+
ions at ¯ uences of
2.5 ´ 1015
ions cmÐ 2
and 77 K [61]. (a ) RBS-channelling spectra
after 1 h annealings at the temperatures given; (b ) Arrhenius plot
of the recrystallization speed v (T ).
Figure 17. Normalized K-hole production cross section r (EK 2/Z1 )2 after proton bombardment of light and medium-mass
elements (Z2= 6 ± 28 ), plotted versus the reduced proton energy
E1/EK 2 . The quantity EK 2 denotes the K-shell ionization energy
of the target. The full line is the prediction of the binary
encounter theory [67].
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then decreases at higher proton energies. Figure 17 (b )
illustrates the energy dependence of the K a X-ray emission
cross-section r K x X for various elements [69].
2.5.2. Examples. The ® rst example selected illustrates
the use of diŒerential PIXE in analysing TiN coatings on
steel [31, 70]. Figure 18 (a ) shows the X-ray spectrum taken
for a 500 keV proton beam impinging onto a 30 nm thin
TiN layer deposited on 1 mm stainless steel. One discerns
the K a and K b X-ray lines of the elements Ti, Cr, Fe, and
Ni. The relatively large yield of the Ti K-radiation is due to
the fact that the cross-section for K-hole production rises
steeply with the proton energy (see ® gure 17 (a )), thus
enhancing X-ray emission in the top (TiN ) layer of the
sample relative to the deeper (steel ) layers. For that reason,
even modi® cations of the top TiN layer, e.g. by ion-induced
sputtering, can be measured: ® gure 18 (b ) illustrates a scan
of the Ti X-ray yield over the implantation spot of 1016
Kr
ions cmÐ 2
. The reduction in the Ti K a yield in the
implantation spot illustrates the reduction of the TiN layer
thickness, due to sputtering, and can be used to measure the
sputtering coe� cient.
Measurements of trace elements in tree rings illustrate
the power of the PIXE method in analysing biomaterials
[71]. Figure 19 (a ) illustrates the X-ray spectrum obtained
in a Si (Li ) detector when bombarding a sample of kaki
wood with a 4 ´ 4 mm2
proton beam at 2.0 MeV energy
and 20 ± 50 nA current. The detector was covered with
two absorbing foils, 16 l m mylar and 58 l m Al, in order
to enhance the signals of the heavier elements in the
spectrum. One discerns the K a lines from elements
between potassium and strontium. Figure 19 (b ) shows
the variations of the Cu, Zn, Rb and Sr contents in the
rings of a sugi stem over the years 1920 ± 1991 ; the
concentrations run between 1 and 20 ppm. While the
measurement and analysis of such spectra are quite
simple, their calibration concerning sub-ppm concentra-
tions can pose some problems. In the presented case, ® lter
papers were prepared which had absorbed standard
element solutions before drying.
2.6. Microbeam Analysis
So far, we have stressed the capacities of nuclear and/or
ion-beam analytical methods concerning their depth
resolution (RBS, NRA, ERDA ), their isotope and/or
element sensitivity (RNRA, ERDA, PIXE ), and their
sensitivity to lattice structures or immediate atomic
surroundings (ion channelling ). The choice of some of the
examples has highlighted that the combination of several
analysing techniques (in addition to conventional surface
and solid state methods ), indeed, can provide detailed
information on rather complicated processes and structures
in thin ® lms. At the end of this section, the ever growing use
of microbeams in thin ® lm analysis will be documented
brie¯ y. These techniques oŒer high lateral resolution in the
l m or sub- l m range [72 ± 74] .
2.6.1. Principle. When keeping the current density at a
`reasonable’ level, only analysing methods having an
`atomic’ cross-section (> 10Ð 20
cm2 ) appear to be useful
for microprobe analysis, i.e. PIXE, RBS, ERDA, and
possibly also RBS-channelling. For these applications,
microbeams in the 100 pA domain are considered to be
standard. For much lower beams in the 1 pA range, novel
techniques such as ion beam induced charge (IBIC ) [75] and
scanning transmission ion microscopy (STIM ) [76] have
Figure 18. PIXE analysis of a 30 nm TiN/steel bilayer sample
irradiated with 2.1 ´ 1017
Kr+
ions cmÐ 2
and analysed with a
0.4 MeV proton beam [70]. (a ) X-ray spectrum showing the K a
and K b radiations of the layer elements Ti, Cr, Fe and Ni; (b ) If
the radiations from the layer elements are partly absorbed in a
0.2 mm Al absorber, one also discerns the K a and K b lines of the
implanted Kr; (c ) Lateral scan of the Ti K-line intensity over the
Kr implantation spot showing the reduction of the TiN ® lm
thickness due to sputtering [70].
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been invented which are able to create direct pictures of
thin ® lm structures.
A comparison of X-ray microprobe methods using
synchrotron radiation, electrons or ions (including their
bene® ts and shortcomings ) has been given by Butz and
Legge [77] (see table 3 ). Watt et al. [78] recently surveyed
the state of the art performance of nuclear microprobe
analysis using proton and a beams; their results are
summarised in table 4. With the most widely used MeV
proton beams, the best high-current (> 100 pA ) and low-
current (< 0.1 pA ) performances were achieved at 2 ±
3 MeV giving lateral resolutions in the 50 ± 400 nm range.
Similar ® gures have also been reached with beams of few
MeV a -particles. Watt et al. [78] also discussed the various
limitations aŒecting the attainment of small spot sizes: in
the case of PIXE and RBS, the major factors in focusing
Figure 19. PIXE elemental analysis of kaki and sugi tree rings [71]. (a ) X-ray spectrum obtained from a 1 mm thick sample of kaki
wood. (b ) Distribution of the elements Cu (h ), Zn (j ), Rb (o ) and Sr (· ) in a sugi stem.
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the beam are the quality of the lens system and optimiza-
tion of system aberrations.
2.6.2. Examples. The two examples selected for microp-
robe element analysis illustrate the performance of a proton
beam for PIXE [84] and of an a -particle microbeam for
RBS [85]. Furthermore, we illustrate the use of a focused
proton beam for maskless micro-machining in three
dimensions [86].
The Oxford group recently contributed to medical
diagnosis by performing a PIXE microprobe study on hair
which was taken from a patient known to have clinical
symptons of lead poisoning [84]. The 3 MeV and 200 pA
proton microbeam was used to create elemental maps
across the section of the sample, a 42 l m thick hair. In
® gure 20 concentration scans of sulphur (which is a major
component of the base material, keratin ) and lead are
shown. The non-uniform pro® le of the latter element,
showing pronounced maxima at the perimeter, may be
associated with the metabolic transcellular transport
mechanism of heavy metals.
Intercalating of Ag into a layered crystal of TiS2
schematically explained in ® gure 21 (a ) was recently studied
by Heitmann and collaborators, using the 2 MeV He+
microbeam of the MARC scanning microprobe facility at
the University of Melbourne [85]. The ion beam was
focused to a 4 l m beam spot and the backscattered ions
were detected in a telescope positioned at 35 8 to the beam.
The samples were scanned in three dimensions by mapping
the Ag content after electrolytic intercalation. Figure 21 (b )
illustrates an Ag map obtained after 2.5 h, which indicates
regions diŒering in their Ag content (A, B, C ). The
corresponding RBS spectra of these regions shown in
® gure 21 (c ) exhibit the Ag, Ti and S pro® les (for decreasing
channel number ). The large kinematical contrast of the
Table 4. High-performance nuclear microprobe facilities [78].
Site Beam Resolution Reference
Oxford SPM Unit
National University, Singapore
Max Planck Institut, Heidelberg
TIARA, Takasaki
MARC, Melbourne
3 MeV protons , 100 pA
2 MeV protons , < 0.1 pA
2 MeV proton s
2 MeV a -particles, 100 pA
2 MeV a -particles
400 nm
100 nm
400 nm
70 nm
[79]
[80]
[81]
[82]
[83]
Table 3. Comparison of features of X-ray microprobes using
ions, electrons and synchrotron radiation [77].
Property Ions Electrons Synchrot ron
radiation
Depth sensitivity
Element speci® c
Quantitation
Background
Sensitivity
Depth resolution
Versatility
Cost
yes
yes
good
low
very good
100 nm± 1 l m
high
high
poor
yes
moderate
high
good
1 nm ± 1 l m
moderate
intermediate
no
yes
good
very low
very good
few l m
limited
very high
Figure 20. Relative X-ray yields of S and Pb measured with a
proton microbeam across a hair of a person showing symptons of
lead poisoning [84].
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three elements involved makes RBS analyses particularly
sensitive in this case.
The use of microbeams is not restricted to resolving
lateral structures in thin ® lm analysis, but can be extended
to fabricate 3-dimensional microstructures. A very ® ne
example was recently communicated by de Kerckhove et
al. [86] who etched microturbines in polymethylmethacry-
late (PMMA ). The spot size of the Oxford SPM Unit
3 MeV proton beam was about 1 l m and the range in
PMMA some 125 l m; the necessary dose was 1 pC l mÐ 2
.
Figure 22 shows a microturbine manufactured with the
proton beam tilted by 10 8 with respect to the sample
normal, for every blade. The three photographs were taken
with increasing spatial resolution and illustrate the micro-
turbine, details of a blade and further details of one of the
edges of a blade.
Figure 21. (a ) Intercalation of Ag into layers of TiS2 [85]; (b ) Map of the Ag content after a 2.5 h electrolytic intercalation; (c ) RBS
spectra taken with a 4- l m wide 2-MeV4He microbeam in the regions A, B and C shown in (b ).
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2.7. Synopsis of ion beam analytical method
At the end of this section, we present a synopsis of the
various methods discussed so far and summarize their
advantages and disadvantages.
2.7.1. Rutherford backscattering spectroscopy. RBS with
1 ± 3 MeV a -particles is a precise, simple and rather
convenient depth pro® ling method in thin-® lm technology
of nanometre depth resolution, mainly for heavy elements.
It is best applicable whenever the multi-element composi-
tion of the ® lm (s ) shows a large contrast in mass number
M 2 which means that the mass resolution of RBS is rather
limited. In most applications, the depth and mass resolu-
tion are limited by the energy resolution of the detection
system. Monolayer depth resolution at surfaces has been
achieved when using an appropriate magnetic or electro-
static analyser for the scattered particles. In the case of bi-
or multilayers, RBS determines the eŒective ® lm thick-
ness (es ) and requires surface-sensitive methods such as
STM, AFM or SEM to distinguish between surface and
layer interface properties. RBS is non-destructive in most
cases, due to the low analysing beam current required.
2.7.2. Resonant nuclear reaction analysis. RNRA is a
depth- and isotope-sensitive pro® ling method of high
resolution at or near the surface (< 1 ± 10 nm ), and still
rather good depth resolution in the interior of the ® lm.
Besides depth resolution, its main advantage is the high
isotope sensitivity which facilitates the detection of isotope
concentrations as low as 100 ppm for strong nuclear
resonances. The disadvantages of this technique to be
mentioned here are that it is rather time-consuming, due to
the small nuclear cross-sections, and that it is not always
non-destructive in the strict sense. In the case of proton
resonances, large amounts of hydrogen are injected into the
sample which may modify some properties of the ® lms.
Possible ® lm deterioation during particle bombardment
may be due to defect production, surface sputtering, or
surface deposition of contaminants under non-UHV
irradiation conditions.
2.7.3. Elastic recoil detection analysis. The main advan-
tage of ERDA in thin-® lm analysis arises from the
possibility to depth pro® le simultaneously many or even
all (light and medium-mass ) elements within the ® lms. For
small Z 2, one even may distuinguish between the diŒerent
isotopes, in particular when selecting beams of diŒerent
masses M 1 . For elastic scattering, the cross-section d rrec
/d X R scales with (Z1 Z2 )2 cos
Ð 3/ (see equation (10 )) and
can therefore be quite high at large angles / and for
appropriate projectiles Z 1, even for low values of Z 2. For
pro® ling medium-mass elements, the use of energetic heavy
projectiles of tens of MeV often still guarantees pure
Coulomb interactions, due to the large mass ratio M 1/M 2
and the correspondingly reduced projectile energy in the
centre-of-mass system. The main disadvantage of ERDA
with heavy ions appears to be that it may in¯ ict radiation
damage in the samples, in particular in insulators and
semiconductors.
Figure 22. Microturbine etched with a 3 MeV proton microbe-
am in PMMA [86]. The blades are tilted by 10 8 relative to the
normal of the sample. (a ) Micrograph taken at 45 8 ; (b )
Micrograph showing the tilt on a blade; (c ) Details of the blade.
The scale bar in each ® gure is 10 l m long.
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2.7.4. Ion channelling. Ion channelling (in connection
with RBS ) is a very useful ion beam analytical method for
testing the crystallinity of thin ® lms and to identify lattice
locations of (mainly interstitial ) self-atoms or dopants. The
sensitive depth is up to several hundred nanometres, the
precision in lattice locations down to a few picometres. The
method is also accessible to NRA to analyse light elements
using strong nuclear resonance reactions.
2.7.5. Particle-induced X-ray emission. Over the last
decade, the ever growing importance of PIXE for elemental
analysis in thin coatings on archeological objects (pottery,
metals, ¯ ints ), antiques (paintings, laquers, vases, hand-
written manuscripts ), biological and medical samples
(tooth inlays, tree-ring dating ), environmental pollution
(aerosols, limnology ) etc. has led to an enormous expansion
and re® nement of this technique [68]. The use of microbe-
ams and the combination of PIXE with RBS and NRA will
further promote this versatile method.
3. Methods using implanted radioactive probes
The methods presented in section 2 all use scattering or
reactions induced by well focused beams of stable isotopes.
The somewhat more exotic, but still manageable analysing
methods which will be sketched in section 3, use radio-
tracers. In the case of emission channelling and perturbed
c -ray angular correlations (PAC ), the radiotracers are ion-
implanted, diŒused or deposited in the ® lms to be analysed,
while MoÈ ssbauer spectroscopy generally uses radioactive
sources outside the samples. The information obtained
from the last two methods is complementary to that gained
in ion beam analysis insofar as they give access to phases
and defect structures, within thin layers, surfaces and
interfaces.
3.1. Emission channelling
3.1.1. Principle. Depth pro® ling of the constituents of
thin ® lms via elastic scattering or nuclear reactions with
beams of stable isotopes, mainly protons and a -particles, is
the most common method. The information obtained
relates to the concentration pro® les and, if used under
channelling conditions, to the crystalline order or disorder
of the samples. Lattice site locations can also be determined
from channelling measurements of a -decay particles or b -
decay positrons and electrons emitted from implanted
radioactive sources. These measurements, in addition to
radiotracer diŒusion measurements, have become quite
important nuclear techniques of thin-® lm analysis.
Emission channelling is, cum grano salis, the reverse of
ion-beam induced channelling described in section 2.4. If
the source nucleus emitting a positively charged particle
(positron, a -particle ) is located at a substitutional lattice
site, the corresponding channel directions and planes are
blocked and one will observe minima of the channelling
yields. If on the other hand, the source nucleus emits its
positive particle from an interstitial site, the corresponding
emisson directions will show channelling peaks. For the
emission of b -decay electrons, the very opposite is true: the
ion cores along the lattice rows will guide and focus
electrons emitted from a substitutional source nucleus
along these lattice directions and produce channelling
peaks, but will not do so if the source is situated within a
channel. The analytical treatment of emission channelling
of massive particles very much follows the line of
argumentation presented in section 2.4 [87, 88].
3.1.2. Example. The example chosen describes work by
HofsaÈ ss et al. [89] who investigated the role of Li doping of
III ± V semiconductors. In particular, the lattice locations of8Li-ions in InSb single crystals were studied in that work.
8Li b -decays with a half-life of 0.84 s to a state of
8Be,
which breaks up, within 4 ´ 10Ð 22
s, into two mono-
energetic a -particles and can thus be used for a channeling
analysis. The emitted a -particles were recorded in a two-
dimensional, position-sensitive Si-detector having a
10 ´ 10 mm2
active area centred under 28 8 to the implanta-
tion direction.
The aim of the study was to identify the original
implantation site (s ) and their changes due to thermal
transport up to room temperature. Figure 23 illustrates
two-dimensional a -particle yield patterns taken around
< 211 > at substrate temperatures of 110 K, 170 K and
295 K during 60 keV implantation into n-InSb. Evidently
the pattern obtained at 295 K indicates that both the {111}
and {110} channel planes are blocked, visible in the low a -
particle yields in these directions. It must be concluded that8Li has reached substitutional positions in the zincblende
structure of InSb, possibly by migrating to and combining
with an In-vacancy within its 0.84 s lifetime. At the
implantation temperature of 110 K, the emission channel-
ling pattern is quite diŒerent: only the {110} plane is
blocked, while yield maxima are seen along the {111} and
{311} planes, indicating that the8Li atoms are implanted
on tetrahedral interstitial lattice sites. The 170 K channel-
ling pattern is typical for an intermediate situation, i.e.
{110} blocking, but neither blocking nor channelling along
the other planes [89].
3.1.3. Summary. The example presented refers to the
rare case of a -particle emission channelling [90], while the
majority of such studies deals with emission channelling of
positrons or electrons following the b -decays of implanted
radioactive nuclei. Fortunately almost all elements have
such b -decaying isotopes which have proper lifetimes and
can be produced abundantly via nuclear reactions (® ssion,
proton spallation, heavy-ion reactions ). These tracer
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isotopes can be either recoil-implanted during the nuclear
reaction itself or implanted oŒ-line by means of an ion
implanter (ISOLDE [87, 88] ). In this respect, emission
channelling is quite versatile. Furthermore, the necessary
number of radioactive tracer usually is quite small, typically
1011
tracers cmÐ 2
. On the other hand, the need of precise
goniometers and position-sensitive two-dimensional detec-
tors and the doping of the ® lms with appropriate sources
makes emission channelling a rather delicate method.
3.2. MoÈ ssbauer spectroscopy
Through the hyper® ne interactions of radioactive isotopes,
important information can also be gained on defect
structures, phases and interface properties in thin ® lms.
For that reason, we illustrate here a few applications of
conversion electron (and X-ray ) MoÈ ssbauer spectroscopy
(CEMS, CXMS ) and, in section 3.3 of perturbed angular
correlation (PAC ) spectroscopy in the analysis of nano-
metre ® lms. These techniques often complement (and
a emission channeling spectrafrom 8Li-implanted p-InSb T = 110K
Tilt angle / deg-2
-1
0
1
2
Tilt an
gle / d
eg
-2
-1
0
1
2
0.6
0.8
1.0
1.2Norm
alized yield
T = 170 K
-2
-1
0
1
2
Tilt an
gle / d
egTilt angle / deg
-2
-1
0
1
2
0.6
0.8
1.0
1.2Norm
alized yield
-2
-1
0
1
2
Tilt an
gle /
degTilt angle / deg
-2
-1
0
1
2
0.6
0.8
1.0
1.2Norm
alized yield
T = 295 K
{111}
{311}
{110}{311}
{111} {110}
{111}
{311}
{110}
{311}
Figure 23. a -emission channelling yields from the decay of8Li which was implanted at 60 keV and 110 K, 170 K and 295 K in p-InSb.
For details see text [89].
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compete with ) transmission electron microscopy and X-ray
diŒraction.
3.2.1. Principle of CEMS and CXMS . The principles
and applications of MoÈ ssbauer investigations have been
described extensively [91 ± 93], and there is no need to give a
general introduction here. Resonant c -ray excitations of
nuclear levels can be used for thin ® lm analysis through the
observation of conversion electrons and/or characteristic
X-rays following the electromagnetic decays of the
MoÈ ssbauer state. In the case of the 14.4 keV 3/2 ® 1/2transition in
57Fe, populated in the electron capture decay
of57
Co with a hal¯ ife of 270 d, the electron conversion
coe� cient is a = 8.2. The conversion electrons have an
initial kinetic energy of 0.6 ± 14.3 keV, while the photon
energy of the emitted K a -radiation is 6.4 keV. These two
energies determine the sensitivity range of CEMS to
roughly 150 nm and that of CXMS to the absorption
length of the K a X-rays of some 10 l m. Without any
additional energy selection of the conversion electrons,
CEMS and CXMS therefore are able to distinguish
properties of the ® lms on these length scales. In thin-® lm
MoÈ ssbauer analysis, the simultaneous recording of trans-
mission (TM ), conversion electron (CEM ) and X-ray
(CXM ) spectra may be desirable, and spectrometers have
been designed to allow such measurements. Figure 24
illustrates the design of a triple-beam MoÈ ssbauer spectro-
meter [94]. The conversion electrons are recorded in a gas-
® lled proportional chamber in which the sample is housed,
while the X-rays are detected in a toroidal gas detector
adjacent to it and separated by a thin window.
Being a hyper® ne interaction method, MoÈ ssbauer
spectroscopy provides information on the isomer shift
(IS, electric monopole interaction ), magnetic hyper® ne
® elds B~
h f and electric ® eld gradient tensors V ik (electric
quadrupole splitting QS ) of the probe nuclei in the matrix
[91]. Typical CEMS spectra for57
Fe are sketched in ® gure
25. Usually, one needs good calibrations to interpret these
hyper® ne parameters and to associate them with de® nite
microsurroundings.
3.2.2. Examples. MoÈ ssbauer eŒect studies in thin ® lms
or multilayers are quite common and there are many
examples for their power and versatility [95,96]. Our ® rst
example selected refers to a CEMS experiment performed
by Sauer et al. [97]. It aimed at measuring the variation of
the magnetic hyper® ne ® eld B~
hf within a Fe/Cr bilayer, as a
function of the distance from the interface. As shown in
® gure 26, an isotopic57
Fe marker ® lm of 2 monolayers
(MLS ) thickness (in order to enhance the sensitivity ) was
placed within a Fe± Cr bilayer epitaxially grown on GaAs;
the57
Fe marker layer was embedded within the Fe ® lm, at a
distance d from the Fe ± Cr interface. The hyper® ne ® eld B~ hf
as measured via CEMS and extrapolated to T = 0 K, was
found to increase to Ð 35.0 T at d » 2 ML from the
interface and to reach the bulk value of B~
h fbulk
= Ð 33.3 T
already at the fourth ML.
Returning to laser nitriding of armco iron, CEMS and
CXMS helped to identify the phases developing near the
surface during the multiple-pulse excimer laser irradiations
Figure 24. Sketch of an apparatus for transmission (TM ),
conversion electron (CEM ) and conversion X-ray (CXM )
MoÈ ssbauer spectroscopy [94] and typical spectra obtained for
each mode of operation. The sample is contained in the
proportional chamber for electron detection (CEMS ), while X-
rays are recorded in a toroidal proportional counter (CXMS ).
Figure 25. The hyper® ne eŒects in the CEM spectra due to the
isomer shift, quadrupole and magnetic splitting are indicated.
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[16,18]. Figure 27 shows CEM and CXM spectra taken
after 64 pulses of a XeCl excimer laser hit the surface at an
average energy density of 4 J cmÐ 2
and at a nitrogen
pressure of 1.5 bar. While the CXM spectrum closely
resembles that of pure Fe showing mainly the a -phase and
little c -Fe (N ), the CEM spectrum is very diŒerent and
con® rms the formation of various iron nitrides in the top
150 nm layer (a ¢ -FeN, c -Fe (N ), e -Fe2N 1-x ). Since the laser-
molten and nitrided coating is roughly 1 l m thick and the
nitrogen content decreases within the ® rst 300 nm (see
® gure 6 ), the two MoÈ ssbauer spectra complement each
other as well as the nitrogen pro® les obtained via RNRA
(see section 2.2 ). Table 5 lists the hyper® ne parameters and
phase fractions deduced from both spectra.
3.2.3. Summary on bene® ts and limitations. The greatest
bene® t of MoÈ ssbauer spectroscopy is possibly the simple
investigation of stable, non-radioactive samples without the
need for special sample preparation. The high resolution
allows easy phase and site analysis via distinct ®̀ nger-
prints’ . Information on the magnetic orientation, magnetic
moments, site occupations, ordering of substitutional and
interstitial sites, etc. can be gained from MoÈ ssbauer spectra.
Even dynamic processes such as superparamagnetism,
diŒusion, or site hopping, can be investigated. The isomer
shifts allow one to diŒerentiate between various cubic non-
magnetic phases which is not possible with most other
hyper® ne methods. More than 100 MoÈ ssbauer isotopes can
be used for the analysis of almost any material. In thin-® lm
analysis, diŒerential CEMS, which selects the conversion
electrons according to their energies, has been developed to
sub-nanometre resolution. The biggest problem of MoÈ ss-
bauer spectroscopy is the Debye± Waller factor, which is
generally not known and assumed to be equal for all phases
and sites. Its strong decrease with increasing temperature
hinders measurements at higher temperatures (up to
1200 K in Fe and up to 100 K in Ni ).
3.3. Perturbed c -ray angular correlations (PAC )
3.3.1. Principle. The application of the perturbed angu-
lar correlation technique in thin ® lm and surface analysis is
rather novel, but may have high potential for further
Bh
f / T
No. of Molecular Layers
Figure 26. Magnetic hyper® ne ® eld Bh f of a stack of 30 nm56
Fe/2 ML57
Fe/d ML56
Fe/4 nm Cr, epitaxially grown on
GaAs < 110> , measured as function of the distance d (in
monolayers ) between the57
Fe marker and the Fe ± Cr interface
[97].
Figure 27. CEM (a ) and CXM (b ) spectra of an armco Fe
sample after laser nitriding with 64 pulses of a XeCl excimer
laser beam. The diŒerences between the two spectra highlight the
formation of the iron nitride phases a ¢ -Fe, c -Fe (N ) and e -Fe2N1 -x
near the surface (a ), while the a -Fe phase in the deeper layers is
not aŒected (b ) [17].
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developments. In PAC, a radioactive nucleus b -decays to a
daughter probe nucleus which contains a c -ray cascade
populating and de-exciting the intermediate, hyper® ne-
sensitive nuclear level. If this nuclear state has a known
magnetic dipole and/or electric quadrupole moment and a
lifetime of the order of ns to l s, one is able to time-
diŒerentially measure the precession of the c -ray angular
correlation, due to the magnetic hyper® ne ® eld (s ) and/or
electric quadrupole tensor (s ) acting on the probe nucleus in
its sensitive state. Extensions of the method to time-integral
PAC measurements for shorter-lived states (down to a few
picoseconds ) are also known. Time-diŒerential or time-
integral measurements of in-beam perturbed c -ray angular
distributions (PAD ), in which the probe nuclei are directly
produced and recoil-implanted into the matrix via a nuclear
reaction, are other important extensions of the PAC
method.
The basic theoretical concept of PAC has been presented
in many treatises [91, 98, 99], and numerous applications to
various situations have been worked out (static magnetic or
electric interaction, superpositions of static magnetic or
electric interactions, superposition of both interactions,
time-dependent hyper® ne ® elds ). In order to enhance the
sensitivity of the experimental set-up, one uses 4 or 6 c -ray
detectors (mainly NaI or BaF2 scintillators ) arranged in a
symmetric planar (4 ) or cube (6 ) geometry and facing the
source which is placed in the centre. For a two-step c -ray
cascade, each detector can record either the start or stop c -
ray, giving a total of 12 or 30 coincidence combinations in
the planar or cube geometry, respectively. Each event of
these combinations is electronically labelled by the two c -
ray energies, detector numbers/positions and the time
diŒerence between the start and the stop signal and thus
provides the (perturbed ) correlation function R (t ). Its
Fourier transform contains the desired hyper® ne interac-
tion (s ). In the case of a static distribution of magnetic
hyper® ne ® elds B~ hf, one derives the ® rst two moments,
namely the centre Larmor precession frequency < x L >and the width d x L , and possibly the orientation of B
~h f
relative to the detectors and/or the sample.
3.3.2. Examples. The ® rst example presents the result of
PAC measurements concerning the magnetic hyper ® ne
interaction of111
Cd nuclei in iron ® lms. The 130 nm thin
Fe ® lm was deposited on either a Si or a SiO2 backing and
doped with a total of some 1012
radioactive111
In tracer
atoms via ion implantation at 280 keV [100]. The111
In
nuclei decay, with a hal¯ ife of 2.8 d via electron capture to
the daughter nuclei111
Cd. Each such decay is followed by
the emission of a two-step c -ray cascade of 171 and
245 keV photon energy and involves an intermediate state
in111
Cd having a hal¯ ife of 85 ns and a magnetic moment
of Ð 0.7656 (25 ) nuclear magnetons (see ® gure 28 ). Figure
29 shows two perturbation functions
R (t) 5 [N ( p , t) 2 N ( p /2, t) ] /[N ( p , t) 1 N ( p /2, t) ], (14)
where N (h , t ) denotes the coincidence rate with the two
detectors forming an angle h , and t being the time diŒerence
between the start and stop signals. The two peaks in each
Fourier spectrum A (x ) of this ® lm (right-hand side )
correspond to the Larmor frequency x L = 0.53 GHz and
its ® rst harmonic, 2 x L , of111
Cd tracer nuclei on substitu-
tional Fe sites. The data in ® gure 29 (a ) reveal that the
magnetic polarization is distributed uniformly within the
plane of the Fe foil. If one now irradiates this foil with
6 ´ 1015
Xe+
-ions cmÐ 2
at 450 keV (having an ion range
Table 5. Hyper® ne parameters of a laser-nitrided Fe sample
measured via CEMS and CXMS [17].
IS
(mm s± 1 )
QS
(mm s± 1 )
B~
h f
(T )
G ¢(mm s
± 1 )
Fraction
(% )
Phase
CEMS
± 0.04 (2 )
0.12 (2 )
0.37 (2 )
0
0.21 (4 )
0.40 (3 )
0.33 (6 )
0.37 (1 )
0.30 (1 )
0
0
0.10 (2 )
± 0.11 (1 )
32.9 (2 )
26.6 (3 )
19.9 (2 )
12.8 (3 )
0.36 (1 )
0.36 (1 )
0.33 (2 )
0.66 (4 )
0.80 (6 )
0.80 (6 )
0.80 (6 )
13 (2 )
12 (2 )
9 (3 )
20 (4 )
15 (2 )
23 (2 )
8 (1 )
cce
a , a ¢eee
CXMS
0.05 (3 )
0.11 (4 )
0
0.40 (5 )
0 33 (2 )
0.33 (1 )
0.33 (1 )
0.33 (1 )
4 (1 )
7 (1 )
89 (2 )
cca
IS= Isomer shift, relative to a -Fe.
QS= Quadrupole splitting.
B~
hf= magnetic hyper® ne ® eld.
G ¢ = line width.
Figure 28. Properties of the PAC source111
In/111
Cd. The
perturbation of the 171/245 keV c -ray cascade in111
Cd involving
the isomeric 245 keV state serves to measure the hyper® ne
interaction (s ) (see [91], chap. 5 ).
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about half the thickness of the Fe ® lm ), a dramatic
polarization of the magnetic hyper® ne ® eld can be
observed, since now the 2 x L component is much stronger
than the x L component (® gure 29 (b )). The origin of this
strong polarization eŒect is not fully understood.
An important information on the athermal ion-mixing
processes in Ag/Fe bilayers has been gained by PAC. As
deduced from the combined RBS and STM analyses and
discussed in section 2.1, the Xe-irradiations at 77 K lead to
a roughening of the Ag surface and induce very little net
atomic transport across the Ag± Fe interface (ion-beam
mixing ). This observation was explained by the existence of
local thermal spikes which produce segregation of Ag and
Fe in the interface zone, after the ballistic intermixing
processes in the collision cascade have taken place. By
means of PAC, Neubauer et al. [101 ± 103] recently
obtained a detailed picture of the stages of the interface
mixing process in this system and were even able to
estimate the average size of the local spikes. In these
studies,111
In tracer ions were introduced either by ion
implantation or deposited as marker layers in the samples
[104].
For measuring the average size of thermal spikes, the
trick was to deposit a submonolayer of111
In tracer atoms
[104], at a variable distance x from the Ag± Fe interface
(x = 0 ± 17 nm ), and to monitor the fraction fA g of111
In
tracers being transferred into Ag during the Xe irradiation
via PAC. Hence, the fraction fA g is characterized by the
absence of any hyper® ne perturbation, due to the fact that
probe nuclei on substitutional, defect-free lattice sites in the
fcc structure do not experience any electric ® eld gradient.
Figure 30 (c ) illustrates the layer geometry, while ® gures 30
(a ) and (b ) display two PAC spectra and their Fourier
transforms taken at the distances x = 0 and x = 1.4 nm
before the ion irradiations. The two sharp peaks in the
Fourier spectrum for x = 1.4 nm again correspond to the
Larmor frequency x L and its ® rst harmonics, 2 x L , of111
Cd
tracer nuclei on substitutional, defect-free Fe sites in Fe
bulk. The Fourier spectrum taken at x = 0, on the other
hand, exhibits two broad distributions of Larmor frequen-
cies centred around x L /2 and x L , which are due to the
smaller magnetic hyper® ne ® elds (and to the possible
existence of electric ® eld gradients ) acting on111
Cd probe
nuclei at the Ag± Fe interface [103,105]. The unperturbed
fraction fA g vanishes in both cases, as no111
In atoms are
located in the Ag layer.
After irradiating these bilayers with 450 keV Xe ions at
¯ uences of 3 ´ 1015
and 6 ´ 1015
ions cmÐ 2
at 77 K, the
fraction fA g is seen. This fraction, which is plotted in ® gure
31 as a function of the distance x, decreases exponentially
on a length scale of about 2.5 nm. However, as shown in
the inset of ® gure 31 (a ), its amount is not reproduced by
the ballistic model. On the other hand, we can apply the
concept of local thermal spikes to explain it: on the basis of
Figure 29. Perturbation functions R (t ) and Fourier transforms A (x ) of111
Cd on substitutional, defect-free sites in Fe, exhibiting the
Larmor frequency x L and twice its value, (a ) in an as-deposited Fe ® lm; (b ) after implanting 6 ´ 1015
450 keV Xe ions cmÐ 2
at 80 K.
Note the change of the relative fractions at the two frequencies indicating a strong net polarization of the magnetic hyper® ne ® eld Bh f in
the ® lm [100].
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tracer diŒusion data and the energy distribution in the
spike, one can estimate the time tS and the mean
temperature TS of the spike necessary to achieve a
su� ciently large diŒusion coe� cient for111
In atoms to
migrate into the Ag layer (see ® gure 30 (c )). It is an
interesting observation that for TS » 2000 K, i.e. just above
the melting temperature of Fe, the experimental and
calculated diŒusion lengths < xD > agree with each other
and with the average spike radius < rS > » 2.5 nm. This
series of experiments constitutes a direct experimental
estimate of the size of ion-induced thermal (droplet ) spikes
[10, 14, 101, 103].
Nonetheless, a small fraction of Ag atoms stays in the Fe
matrix after Xe-irradiations and their microsurroundings
have also been identi ® ed using PAC. As the111
In tracers
occupy substitutional Fe sites, any replacements of Fe
atoms in the neighbourhood of the111
In tracers by injected
Ag atoms lead to decreasing hyper® ne ® elds B~
h f, relative to
that of an inert Fe surrounding. According to calibration
measurements in laser-deposited AgzFE1 -z ® lms (z < 30
at.% ), B~
hf decreases linearly with the number of Ag atoms
in the nearest and next-nearest neighbourhood [106]. PAC
(and CEMS ) measurements of ion-mixed bilayers indicate a
stochastic occupation probability of the Fe lattice sites with
1 or 2 Ag atoms after ion-beam mixing. Athermal ion beam
mixing of Ag± Fe bilayers thus oŒers a particularly
convincing example of the power of nuclear methods
(RBS, PAC, CEMS ) to characterize a complicated ion-
beam induced transport process with nanometre resolution.
3.3.3. Bene ® ts and limitations. As in MoÈ ssbauer spectro-
scopy, the bene® ts of PAC lie in the high local sensitivity of
this method which can give access to structures on an
atomic scale. As long as the hyper® ne interaction is static
during the observation time, i.e. within the lifetime of the
nuclear level chosen, PAC depicts this interaction and is
able to resolve diŒerent static probe surroundings. The
method can be extended to dynamic processes on the
nanosecond time scale [107]. PAC is able to distinguish
between (static ) magnetic hyper® ne ® elds, electric ® eld
gradients and superpositions of both. Moreover, it provides
information about the orientation of such internal vector or
Figure 30. The two PAC spectra shown in (a ) and (b ) refer to
distances of x= 0 and 1.4 nm between the111
In marker layer and
the Ag ± Fe interface. The spectra were accumulated before the
Xe-ion irradiation. (c ) Layer geometry of the samples [103].
Figure 31. Top: fraction fA g of111
In probe atoms which have
migrated to substitutional, defect-free lattice sites in Ag,
measured as function of the distance x between the111
In marker
layer and the Ag ± Fe interface, after 450 keV Xe+
irradiations
at 77 K and for ¯ uences of U = 3 ´ 1015
and 6 ´ 1015
ions cmÐ 2
.
Note that the ballistic model does not reproduce this fraction(inset ). Bottom: spike temperature TS (a ) and experimental and
calculated eŒective diŒusion length < xD > (b ) as function of the
spike radius rS [103].
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tensor ® elds relative to crystallographic axes. In compar-
ison with MoÈ ssbauer spectroscopy, PAC is more favour-
able at higher temperatures, since it does not depend on a
Debye± Waller type factor. A further advantage of PAC is
the very small number of radiaoctive tracer atoms
necessary which, in general, do not in¯ uence the (macro-
scopic ) properties of the matrix.
The limitations of PAC derive from
(1 ) the small number of appropriate nuclear probe
nuclei available;
(2 ) the necessity to introduce the radioactivity into the
sample to be studied;
(3 ) the need to calibrate the observed hyper® ne ® elds;
(4 ) the modi® cations which the probe atoms (which
usually are impurities ) may exert onto the local
environment, either due to the chemical nature of the
probe atoms or, in the case of implantation, the
radiation damage.
3.3.4. Summary. Perturbed angular correlation spectro-
scopy bene® ts from the fact that, when using modern, large-
solid-angle gamma detector arrays, a large fraction of the
nuclear decays gives access for investigating the hyper® ne
interaction. Therefore, the density and total number of the
radioactive tracers necessary can be very small (< 1 ppm,
some 1012
tracer nuclei in total ). The short-range nature of
hyper® ne interactions makes this method very sensitive to
local structures such as point defects, atomic con® gurations,
local chemical reactions and phase transitions. The poten-
tial of PAC in thin-® lm analysis has not been fully exploited
yet, but despite the disadvantages mentioned above, PAC
oŒers some unique possibilities.
Acknowledgements
It is a pleasure to thank Tilmann Butz, Sankar Dhar, Lucie
Hamdi, Hans HofsaÈ ss, Andrea Jungclaus, Diane de
Kerckhove, Felix Landry, Momir Milosavljevic, Fabrizio
Roccaforte, Peter Schaaf and Michael Uhrmacher for their
suggestions and comments or for allowing me to quote
some unpublished results. This work was supported by
Deutsche Forschungsgemeinschaft (DFG ).
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Physics, edited by E. A. GoÈ rlich, and K. Latka, (Krakow ), p. 56.
[103] Neubauer, M., Lieb, K. P., Uhrmacher, M., and Wodniecki, P., 1998,
Europhys. Lett., 43, 177.
[104] Uhrmacher, M., Neubauer, M., Bolse, W., Ziegeler, L., Lieb, K. P.,
1998, Nucl. Instr. Meth., B139, 306.
[105] Runge, B. U., Dippel, M., FilleboÈ ck, C., Jacobs, K., Kohl, U. and
Schatz, G., 1997, Phys. Rev. Lett., 79, 3054.
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M., Wenzel, T. and ISOLDE-Collaboration, 1996, Phys. Rev., B54,
871; Lupascu, D., Neubauer, M., Wenzel, T., Uhrmacher, M., Lieb,
K. P., 1996, Nucl. Instr. Meth. B113, 507.
Klaus-Peter Lieb was born 1939 in Germany. He
studied physics in Basel and Freiburg (1958± 67 ).
He holds diploma and doctoral theses (1964,
1966 ) in experimental nuclear physics, Universi-
taÈ t Freiburg. He has held postdoctoral position s
at the Universities of Freiburg (1966± 67 ), Texas
at Austin (1967± 69 ), Bogota/Colom bia (1969± 71 )
and KoÈ ln (1971± 73 ) and Associate Professor
UniversitaÈ t zu KoÈ ln (1973± 79 ). He currently hold
the position Full Professor UniversitaÈ t GoÈ ttingen
(since 1979 ). His research topics include: nuclear
spectroscopy of neutron and heavy ion reactions;
measurements of lifetimes and magnetic mo-
ments; EUROBALL spectrometer; applied nucle-
ar physics: ion beam implantation, mixing and
analysis, hyper® ne interactions, thin ® lms, laser
nitriding and corrosion . He has authored some
420 refereed articles in journals and books: editor
and author of textbook Experimental Physics:
Atoms, Molecules, Nuclei, Particles (1997 ).
Thin film analysis with nuclear methods 413
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