2.7 Partitioning of the total cross section 89
2.3. It is immediately apparent that the total cross section does not show
a dramatic rise or change of slope as the impact energy is raised through
the threshold for positronium formation. This is in marked contrast to
the results for the other gases discussed so far in this section and for the
noble gases, discussed in subsections 2.5.1 and 2.5.2. In fact, following
an initial decline from approximately 2 ×10
−15
cm
2
at1eVto7×10
−16
cm
2
at 5 eV, σ
T
remains nearly constant up to 20 eV (there is a gradual
decline at higher energies). The apparent dearth of positronium formation
may, however, be an illusion resulting from the behaviour of the elastic
scattering cross section near this threshold (see sections 3.3 and 4.4 and
the discussion of Meyerhof et al., 1996). There have, thus far, been no
direct studies of positronium formation in water, although a study of low
energy positron impact with an ice surface found abundant positronium
emission (Eldrup et al., 1985). In positron lifetime studies in other gases
with high dipole moments (e.g. NH
3
,CH
3
Cl), high positronium formation
probabilities have been found (Heyland et al., 1982).
2.7 Partitioning of the total cross section
In this, the concluding section of this chapter, we present a discussion of
the partitioning of the positron and electron total cross sections for helium
gas, based upon the work of Campeanu et al. (1987) for positron scattering
and of de Heer and Jansen (1977) for electron scattering. This target has
been chosen because it has been the subject of extensive theoretical and
experimental study. A similar exercise has also recently been undertaken
by Zhou et al. (1997) in connection with their measurements of σ
T
for
atomic hydrogen, and by Sueoka and Mori (1994) for helium, neon and
argon gases.
The presentation of positron and electron data in sections 2.5 and
2.6 has illustrated that there are often large differences between the two
total cross sections, both in magnitude and energy dependence, although
sometimes the converse is true, with the behaviour being remarkably
similar. In an effort to understand some of these effects it is necessary
to probe deeper into the total cross section by splitting it up into its
partial contributions, taking the most reliable data from both theory
and experiment. In so doing, one may also hope to gain some degree
of self-consistency. Detailed discussions of the processes which make the
major contributions to σ
T
are contained in Chapters 3–5, and one of our
purposes here is to set the scene for these.
The earliest attempts to partition σ
T
for positron–helium scattering
were those of Griffith et al. (1979b), before the advent of any partial
cross section measurements, and of Coleman et al. (1982), when the first
inelastic scattering data became available. The most detailed study is