if we disregard (the minor) changes in the backscattering factor; the experimental ratio
is (I
A
/I
p
) for a multilayer divided by (I
A
/I
p
) for a ML. Here we assume that there are N
1
atoms in the first layer, N
2
in the second and so on, and their spacing is d. Then we can
work out the signals at a coverage
u
between n and n11 ML from both the layers and
the substrate, as sums which take into account the attenuation. For example, if n51,
and we neglect attenuation within the first layer
N
e
5N
1
[(22
u
)1(
u
21)exp(2d/
l
cos
u
e
)]1N
2
, (3.15)
where the first (second) term in square brackets correspond to the proportion of the
first layer which is uncovered (covered) by the second layer, and so on. This relation
leads to a series of straight lines, often plotted as a function of deposition time, from
which the
l
can be deduced in favorable cases.
The simplest case, where there are the same numbers of atoms in each completed
ML, can be worked out explicitly. In that case, the slope of the second ML line ratioed
to that of the first ML gives exp(2d/
l
cos
u
e
), from which d/
l
can be extracted if the
effective analyzer angle
u
e
is known. This effective angle is given by
cos
u
e
5(1/
V
a
)
兰兰
cos
u
a
·sin
u
a
d
u
a
d
f
a
, (3.16)
with the integrals taken over the analyzer acceptance. For detailed studies, it is advis-
able to construct computer programs which take the analyzer geometry into account,
and then perform the angular integration numerically. There has been much discussion
over what
l
really is in such experimental comparisons; it is now accepted to be the
attenuation length (AL), which is shorter than the imfp due to elastic (wide angle) scat-
tering (Dwyer & Matthew 1983, 1984, Jablonski 1990, Matthew et al. 1997, Cumpson
& Seah 1997). However, as pointed out by the last authors, unless the integration of
(3.16) is performed separately (as implied here), the AL also depends on the type of
analyzer used and the angular range accepted; thus in some papers the AL is not a
material constant, and one should beware of using published values uncritically.
There are many layer growth analyses in the literature, in some cases with a large
number of data points showing relatively sharp break points at well-defined coverage,
such as for Ag/W(110) (Bauer et al. 1977). Experiments with fewer data points can still
lead to firm conclusions, using the comparison with a layer growth curve of the type
reported here. Such an analysis is shown in figure 3.20, which shows both the Auger
spectra for a series of Ag deposits on Si(001) and the corresponding Auger curves as a
function of coverage at both room and elevated temperature (Hanbücken et al. 1984,
Harland & Venables 1985). This is a case where growth more or less follows the ‘layer
plus island’, or Stranski–Krastanov (SK) mode, discussed in more detail in chapter 5.
From the Auger curves we see that at room temperature, layer growth is followed for
approximately 2 ML, but then experiment diverges from the model, indicating rough-
ening or islanding. The high temperature behavior is much more extreme, as the first
layer is #0.5 ML thick, and islands grow on top of, and in competition with, this dilute
layer (Luo et al. 1991, Hembree & Venables 1992, Glueckstein et al. 1996).
The Ag/Si(111) and Ag/Ge(111) systems have also been studied, with the 冑3 recon-
structed layer at high temperatures having a thickness of around 1 ML. The exact
3.4 Quantification of Auger spectra 93