Thesis (Doctor)--Technische Universiteit Delft, 2006. / Includes bibliography (p. 134-136).

published_or_final_version / abstract / Earth Sciences / Doctoral / Doctor of Philosophy

The objective of this project is to apply the Optical Stimulated Luminescence (OSL) technique to date the palaeo sediment from Mu Us Desert, part of the Inner Mongolia in northern China and reconstruct the palaeo environment. Five OSL samples were collected from Dagouwan, Salawusu River Valley at Inner Mongolia by Dr S. H. Li and his team in 2009. Extraction of 150μm to 180μm silt-size feldspar from collected dune sand, lacustrine facies and fluvial facies samples and running of luminescence dating therefore to obtain the age from 50ka to 90ka. Climate proxies - magnetic susceptibility, grain size, fossil vertebrates and fossil pollens have been analyzed and it is concluded that significant climate change occurred within this period, which change from domination of warm, humid and rainy summer monsoons (before 70ka) to cold, wind, windy strengthened dry winter wind and back to warm and humid again after 55ka. / published_or_final_version / Applied Geosciences / Master / Master of Science

Thesis (Ph. D.)--University of Hong Kong, 2008. / Also available in print.

Thesis (M. Phil.)--University of Hong Kong, 2008. / Also available in print.

Carbon-doped aluminium oxide, α-Al₂O₃:C, is a ultra-sensitive dosimeter of topical research interest. The aim of this project was to investigate the dynamics of luminesce in this material. The methods of investigation consisted of thermoluminescence and time-resolved optical stimulation. Thermoluminescence measurements provide information on trap distribution and kinetic parameters of the traps involved in luminescence whereas time-resolved optical stimulation is a handy technique in investigation of luminescence lifetimes and provides an insight into the charge transitions between traps and recombination centres. Measurements were made on samples annealed at a nominal temperature of 900⁰C for 15 minutes. The material shows the presence of five thermoluminescence peaks at 37⁰C, 160⁰C, 300⁰C 410⁰C, and 480⁰C at a heating rate of 0.03k/s when irradiated to 6.0 Gy of beta. The main peak at 160⁰C, shows a linear dose response for doses between 0.1 Gy and 10 Gy and then goes sublinear above 10 Gy, the peak at 37⁰C shows a sublinear dose response for doses between 0.1 Gy and 10 Gy and appears to saturate thereafter, whereas the dose response of the peak at 300⁰C goes from linear to supralinear then apparently quadratic behaviour in the dose range of 0.1 Gy to 16.0 Gy. The trap depth of the main peak, that is, its activation energy as determined below the conduction band, has been approximated at 1.3 eV with a kinetic order of approximately 1.2. Time-resolved optical stimulation has been used to investigate luminescence lifetimes. The mean luminescence lifetime obtained for the sample at ambient temperatures is 35.0±1.0 ms. The investigations of the dependence of luminescence lifetimes on measurement temperature show that the material suffers from thermal quenching effects at measurement temperatures above 140⁰C with the activation energy of thermal quenching estimated at 1.045±0.002 eV. Shallow traps i.e. traps lying close to the conduction band, seem to elongate the lifetimes of optically stimulated luminescence in the material at temperatures between 30⁰C - 80⁰C due to charge retrapping. The material exhibits both fading and recuperation of the optically stimulated luminescence signal with storage time.

This study used OSL dating to examine the chronological relationship between two adjacent archaeological sites at the Hare Hammock complex in northwest Florida. High-resolution vertical sampling was performed at 10cm intervals in profiles, one corresponding to a Swift Creek burial mound, and the other to a Weeden Island ring midden. This was done in order to determine the timing of occupations at the sites and look for patterns in radiation dosimetry. The Swift Creek mound was found to have a mean OSL age of 1835 +/- 68 years, consistent with archaeological expectations of the site and the accepted range of Swift Creek culture. The subsequent Weeden Island occupation was also found to have OSL ages within expectations, with a mean age of 1049 +/- 43 years that overlies a single age of 1511 +/- 372 years, corresponding to the Late and Early Weeden Island periods, respectively. The general coherence with radiocarbon dates and ceramic chronologies affirms the veracity of these OSL ages, which were obtained using a very recently developed dosimetric technique that applies Al2O3:C cylinders as in-situ dosimeters. These dosimeters indicated that the sediments at Hare Hammock contain significant heterogeneity in beta dose rates. This study finds that, under these circumstances, the best age results are obtained when applying the refined dosimetric technique which combines the beta dose rate from NAA/DNC and gamma dose rate from Al2O3:C dosimetry. / Thesis / Master of Science (MSc)

published_or_final_version / abstract / Earth Sciences / Master / Master of Philosophy

Reconstruction of former Central Asian glaciers extents can provide valuable information about past atmospheric circulation variations. These extents, often marked by terminal moraines, need to be chronologically constrained. Cosmogenic nuclide exposure (CNE) dating is widely used to directly date moraines. In addition, there is increasing interest on using optically stimulated luminescence (OSL) techniques for dating glacial landforms. This thesis focuses on the methodological aspects of directly dating glacial landforms to perform paleoglacial reconstructions in Central Asia, with an emphasis on OSL dating. For OSL dating of sediments from glacial settings, it is important to measure the luminescence signal at the single grain scale, because the sediments are likely affected by partial bleaching due to short light exposure during glacial or glaciofluvial transport. The use of an Electron Multiplying Charges Coupled Device (EMCCD)-based imaging system for single grain OSL measurements would offer larger flexibility in light stimulation and sediment type, compared to the current Single Grain Risø reader. An automated image processing procedure has been developed to compensate for sample carrier displacement over repeated measurements and for attributing pixels to each grain for signal integration when using this imaging system. However, significant cross talk contamination, demonstrated by laboratory and simulation experiments, prohibits accurate single grain luminescence measurements. Preliminary experiments using a basic image processing algorithm show good potential for software correction solutions. Paleoglacial reconstructions conducted in the Altai Mountains, Central Asia, using both CNE and OSL dating demonstrate that luminescence measurements of glaciofluvial sediments performed at the multi-grain scale result in large age overestimates, and that single grain measurements allow for more accurate dating of glacial landforms. However, uncertainties remain that are related to the model used for extracting equivalent doses for well-bleached grains and to fading corrections when using feldspar minerals. The timing of glaciation can be inferred from scattered CNE moraine boulder ages if most of the ages are concentrated within a few thousand years, with only few ages clearly older or younger. Overall, combining CNE and OSL techniques for dating a glacial landform is a powerful approach for producing robust glacial chronologies, despite uncertainties inherent to each technique. Paleoglacial reconstructions from the Altai Mountains indicate Marine Isotope Stage (MIS) 2 and MIS 4/late MIS 5 local Last Glacial Maximums. In Central Asia, in addition to a regional MIS 2 glaciation, previous studies indicate a period of major glacial advances during MIS 3 that is out of phase with global ice volume records. However, most MIS 3 glacial chronologies from Central Asia are based on too few or too heavily scattered CNE data sets, or on OSL or Electron Spin Resonance (ESR) ages for which partial bleaching has not been properly investigated. Hence, at this stage, chronological evidence is insufficient to demonstrate a regional MIS 3 glaciation in Central Asia. Surge-related glacial features identified in the Russian Altai also highlight the importance of conducting detailed geomorphology and sedimentology studies to understand former ice dynamics, which is essential for inferring appropriate paleoclimate information from paleoglacial reconstructions. / <p>At the time of the doctoral defense, the following paper was unpublished and had a status as follows: Paper 4: Manuscript.</p>

A radiação ionizante é amplamente utilizada em diversas áreas na indústria e na medicina. No campo da medicina, a radiação ionizante é utilizada tanto para fins terapêuticos como para fins diagnósticos, abrangendo assim um grande intervalo de doses de diferentes tipos de radiações. Para certificar que a finalidade da prática esteja sendo alcançada, são necessários estudos detalhados de detectores e dispositivos que atendam aos diferentes tipos de radiações. Neste trabalho foi realizado um estudo das características dosimétricas de amostras de BeO em feixes padronizados de radiodiagnóstico convencional, mamografia e tomografia computadorizada, utilizando as técnicas de termoluminescência (TL) e luminescência opticamente estimulada (OSL) e propondo um sistema adequado para sua utilização em dosimetria de feixes. Os principais resultados obtidos foram: alta sensibilidade à luz branca durante a irradiação, boa reprodutibilidade das respostas TL e OSL (coeficientes de variação inferiores a 5%), parâmetros cinéticos correspondentes aos valores obtidos em todos os métodos testados, sem fading dentro do período estudado para ambas as técnicas. As características dosimétricas obtidas neste trabalho mostram a possibilidade de aplicação das amostras de BeO em dosimetria da radiação X, considerando os intervalos de dose empregados, pelas técnicas de TL e OSL. Assim, as amostras de BeO apresentaram sua utilização potencial para dosimetria de feixes de radiodiagnóstico convencional, mamografia e tomografia computadorizada. / The ionizing radiation is widely used in several areas in industry and medicine. In the field of medicine, the ionizing radiation is used both for therapeutic purposes and for diagnostic purposes, thus covering a wide range of doses of different types of radiation. To certify that the goal of practice is being achieved detailed studies of detectors and devices that respond to different types of radiation are required. In this work, a study of dosimetric characteristics of BeO samples was performed in standard beams of conventional diagnostic radiology, mammography and computed tomography, using the techniques of thermoluminescence (TL) and optically stimulated luminescence (OSL), and proposing a suitable system for its use in beam dosimetry. The main results obtained were: high sensitivity to white light during the irradiation, good reproducibility of responses TL and OSL (coefficients of variation of less than 5%), and kinetics parameters corresponding to the values obtained in all of the tested methods, without fading within the observed period for both techniques. The dosimetric characteristics obtained in this work show the possibility of application of BeO samples for dosimetry of X radiation, considering the tested dose interval, by the TL and OSL techniques. Thus, the BeO samples presented potential use for dosimetry of conventional diagnostic radiology, mammography and computed tomography beams.