Bell, William Terence
Description
This thesis is presented in two parts: Part I dealing with the theory of the thermoluminescence phenomenon and with the origins and effects of the natural radiation environment; and Part II dealing with three
applications of the TL dating method to archaeological sites in Australia.
The first chapter describes the theories and mechanisms thought responsible for the thermoluminescence phenomenon. The application of these theories to the principles of age determination using quartz is explained...[Show more] and a review of the thermoluminescent properties of quartz itself is given. Nothing further has been added to knowledge already extant in these areas as the purpose of this chapter is to lay the foundation for the work found
later in the thesis. A full description of the setting up and calibration of the TL
dating equipment, including the alpha counter, is given in the second
chapter. The third chapter deals with the passage of alpha particles through
matter. The theory of Howarth (1965) is modified in this chapter so as to
quantify the absorbed dose from alpha particles passing through a 105 micron
quartz grain and to describe the alpha dose reduction due to HF etching. The results are significantly different from the "first order approximation" given by Fleming (1969, 19 70). In the fourth chapter the theoretical approach of Charlton (1970)
for solving the problem of the energy dissipation of electrons passing
through matter is discussed. This method is modified in this chapter to be applicable to a quartz grain irradiated by the natural radioactive series. The contribution from the internal conversion electrons is included in the dose attenuation factors. The assessment of the dose dilution resulting
from etching the grains in HF is then given.
The fifth chapter describes qualitatively the interaction of gamma radiation with matter. The concept of energy-absorption buildup factors is described and is used in the evaluation of the absorbed dose from an
overlying clay layer. The dependence of the TL response on both the photon energy and the particle size is explained and a method for formulating a general solution of this problem is put forward. Specific solutions for the samples to be dated in Part II of this thesis are obtained. Chapter six presents detailed radiation data concerning the naturallyoccurring radioactive series. Tables giving the energy released during
every transition of every radioisotope are given. These data are used to evaluate dose-rate conversion factors from ppm of the parent and from the alpha activity of the sample to mrad/yr. The information given in this chapter has been published.
The seventh chapter commences Part II of the thesis and it is concerned with the TL dating of ancient Aboriginal fireplaces from Lake Mungo in western New South Wales. The inclusion technique of TL dating is used
but particular attention is paid to the assessment of the alpha particle
contribution to the dose-rate because of the irregularity of the etching of quartz grains in HF acid. Other complicating factors which are also considered in detail are the saturation of the electron traps, the internal radioactivity of the quartz grains, and the gamma dose from an overlying
stratigraphic layer of much higher radioactive content than the fireplaces
themselves. The ages of the Mungo fireplaces range from 31,400 to 36,400 years which confirms the antiquity of the site as suggested previously by radiocarbon age determinations on charcoal from the fireplaces. The radiocarbon ages are given in the eighth chapter and a small
systematic discrepancy of between 10 and 15% appears to exist between them and the TL ages, with the TL ages being the older in each case. A full description of possible sources of error in the radiocarbon method is
presented and one of these, the variations in the Earth's geomagnetic field,
is put forward as a possible reason for the TL/C-14 age differences. The ninth chapter describes a further application of the inclusion technique, as modified in the seventh chapter, to Aboriginal fireplaces from Lake Jindabyne in New South Wales. The ages of these fireplaces lie between
2000 and 3000 years. In the tenth chapter the TL dating of cooking stones from New
Guinea is described. Large uncertainties in the ages for these stones were encountered and an impurity analysis of the samples suggests that this is due to the high level of impurity diffusion into the quartz grains. The pre-dose technique of Fleming (1973) was used for this investigation and
the results given in this chapter have been published.
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