1.3 Basic experimental techniques 13
scintillation counters (see e.g. Knoll, 1989 for a general discussion). One
of the most commonly used sources of positrons in lifetime studies is
the
22
Na radioisotope, a simplified decay scheme for which is shown in
Figure 1.4(b). The β
+
branching ratio for this isotope is around 90% and
the positron emission is followed promptly by a gamma-ray of energy 1.274
MeV. This gamma-ray is used to register the positron’s birth by starting
the timing sequence. In addition,
22
Na has a conveniently long half-life
of around 2.6 years, and is commercially available in a form suitable for
many applications.
The annihilation gamma-rays, at energies of 511 keV and below (see
section 1.2 for a discussion of the various possible annihilation modes),
are registered by a second scintillation counter. The start and stop
signals are usually processed by a pair of discriminators, and the simplest
arrangement, shown in Figure 1.4(a), consists of two constant-fraction
discriminators, which combine good timing characteristics with the ability
to set upper and lower limits on the pulse height accepted by the instru-
ment. Thus, the higher energy ‘start’ gamma-ray can easily be selected.
After the insertion of an appropriate delay, to introduce a minimum fixed
time between the start and stop signals, the pulses are fed to the inputs
of a time-to-amplitude converter. The output of this module, which is
proportional to the length of time between the start and stop signals, and
thus to the individual positron lifetime, is then stored using a multichannel
analyser. A lifetime spectrum is thereby built up, frequently containing
10
6
–10
7
events, from which various lifetimes, principally those due to free
positron and ortho-Ps annihilation, along with several other parameters,
can be extracted. Numerous examples of results obtained using this kind
of instrumentation are described in Chapters 6 and 7.
Another useful lifetime system, though less frequently encountered, is
the so-called β
+
–gamma system. A variant of this technique was used
in some of the pioneering measurements of positron–atom total collision
cross sections described in Chapter 2. The annihilation gamma-ray still
provides the stop signal, but the start signal is derived via the energy
deposited by the positrons as they traverse a thin (typically 0.1–0.3 mm)
scintillator. This method of start detection has a high efficiency, usually
around 50%, which permits the use of a relatively weak radioactive source,
resulting in a superior signal-to-background ratio.
Numerous technical descriptions of various aspects of lifetime apparatus
can be found (e.g. MacKenzie, 1983, and references therein), and a number
of sophisticated data analysis and fitting procedures have been developed
to analyse the data collected (e.g. Coleman, Griffith and Heyland, 1974;
Coleman, 1979; Kirkegaard, Pedersen and Eldrup, 1989), but detailed
discussion of these topics is beyond the scope of the present treatment.