Studies in thermoluminescence dating in Australia
Creators: name: Bell, William Terence
Publisher: name: The Australian National University
Year: 1978

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 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.