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O trabalho apresenta procedimentos e resultados referentes à análise de solos, rejeitos ferrosos de origem mínero-metalúrgica, ligas ferrosas e minérios ferrosos por espectroscopia de fluorescência de raios X com dispersão de energia (EDXRF), com vistas especialmente à identificação e quantificação de metais pesados em ensaios realizados com equipamento portátil. Para solos e lamas, foram realizados estudos com e sem o recurso de adições de padrões internos. Em ambos os casos, foram ignorados os teores de elementos leves importantes como alumínio e silício. Sem a adição de padrões internos, não se obtiveram resultados absolutos, e os teores dos elementos claramente identificados eram expressos de modo relativo. Com a adição de padrões internos, foi possível expressar os teores daqueles elementos como valores absolutos. Para a análise de ligas ferrosas e minérios, utilizou-se o recurso da fluorescência secundária com alvo de ferro, para aumentar a excitação dos elementos mais leves que o ferro e diminuir a intensidade dos picos de escape da família Fe-K. Com este recurso, obteve-se uma elevada correlação entre as áreas dos picos destes elementos e seus teores nominais. Para determinação dos elementos mais pesados que o ferro, utilizou-se o feixe direto. Foi elaborada metodologia para conciliar os resultados obtidos com feixe direto e os obtidos com fluorescência secundária, obtendo-se uma boa aderência aos valores dos teores nominais. Complementarmente o trabalho apresenta uma forma alternativa de estimar erros quantitativos, baseando-se em simulações de espectros, e traz uma forma de visualizar o espectro sob o domínio da frequência para encontrar e remover ruído. / The work presents procedures and results concerning the analysis of soils, ferrous wastes of mineral-metallurgical origin, ferrous alloys and ferrous minerals by Energy-Dispersive X-ray Fluorescence spectroscopy (EDXRF), with a special focus on the identification and quantification of heavy metals in tests performed with portable equipment. For soils and sludges, studies were carried out with and without the use of additions of internal standards. In both cases, the contents of important light elements such as aluminum and silicon were ignored. Without the addition of internal standards, no absolute results were obtained, and the contents of the clearly identified elements were expressed in relative terms. With the addition of internal standards, it was possible to express the contents of these elements as absolute values. For the analysis of ferrous alloys and ores, the secondary fluorescence with iron target was used to increase the excitation of lighter elements than iron and to reduce the intensity of the escape peaks of the Fe-K family. With this feature, a high correlation was obtained between the areas of the peaks of these elements and their nominal contents. To determine the elements heavier than iron, the direct beam was used. A methodology was developed to reconcile the results obtained with direct beam and those obtained with secondary fluorescence, obtaining a good adhesion to the values of the nominal values. In addition, the work presents an alternative way of estimating quantitative errors, based on spectra simulations, and provides a way to visualize the spectrum under the frequency domain to find and remove noise.

Fused glass beads as a sample preparation method for X-ray Fluorescence spectroscopy (XRF) were introduced in 1957 by Claisse; it soon became the preferred method to introduce oxide samples to the spectrometer, because heterogeneity, mineralogical and particle size effects are eliminated during the fusion process. Matrix effects are largely reduced by the resulting dilution. With the recent advances in XRF spectrometers, instruments with enhanced generator and temperature stability, improved sensitivity (even for light elements), and effective matrix correction software are available. Consequently, the largest proportion of analytical error results from the sample preparation step. Sampling error will always contribute the largest overall error but that is not the topic of this discussion. After more than 50 years of fused bead use in XRF analysis, certain matrices remain problematic. Although many fusion methods for chromite-, sulphide- and cassiterite-rich materials have been published, easily reproduced, routine methods for these still elude analytical chemists. Lengthy fusions at temperatures higher than 1100ºC are often prescribed for refractory materials and ores, and until recently one of the biggest challenges was a metal-bearing sample e.g. contained in slags or certain refractory materials. This study was conducted to identify and elucidate the reactions occurring in the formation of a lithium borate glass, but also between the lithium borate and oxides during glass formation. Different analytical techniques were used to investigate the reactions occurring during the fusion process based on theoretical glass-making principles. As a starting point, Thermo Gravimetric Analysis (TGA) and Differential Thermal Analysis (DTA) were used jointly to evaluate the reactions occurring during the fusion of lithium borate glasses, and at a later stage, oxide/flux mixtures. When a different TGA instrument was used, Differential Scanning Calorimetry (DSC) was used in conjunction with the TGA. Observed reactions were modelled in a muffle furnace to produce identical material in larger quantities, and this material was then investigated using X-ray Powder Diffractometry (XRD), Raman Spectroscopy and Electron Microprobe Analysis (EPMA). The most enlightening result from the TGA/DSC results was the large mass loss above 1050 ºC. Literature often prescribes prolonged fusions at elevated temperatures for certain fusions, but it was proved beyond reasonable doubt that this practise causes volatilisation of the flux and leads to erroneous analytical results. The next analytical technique applied to the flux and flux/oxide samples was XRD. Where pre-fused fluxes were investigated, the XRD data served as confirmation of the glassy state of the pre-fused flux as a broad humpy scan indicative of an amorphous material was seen in stead of a diffractogram with sharp, well defined peaks. After heating to above the temperature of re-crystallisation, the phases present could be identified from the diffractogram. Provisional results using the in-situ, high temperature stage point towards the possibility of using this technique to great effect to investigate the presence of different phases formed at high temperatures. Flux-oxide mixtures were measured on the high temperature stage and after cooling a new phase was observed indicating that new phases formed during a fusion reaction. As the heating stage is slow-cooled, the chance of crystallisation in the glass is good, providing the possibility for investigating this formation of new phases at elevated temperatures further with a more suitable heating element that will contain the material. Raman spectroscopy was subsequently used to gain information about the bonds within the flux. Pure lithium tetraborate and lithium metaborate fluxes were analysed as well as flux oxide mixtures. The vibrations could not be predicted from first principles as band broadening occurs in glasses that makes theoretical predictions very difficult. The data obtained was compared to similar studies in literature and good agreement was found. In oxide-flux mixtures definite new bands were observed that was not part of the flux or oxide spectrum. EPMA results allowed calculation of the maximum solubilities of an oxide in a specific flux. It was done using Cr2O3 and ZrO2 and compared well with experimental values obtained from literature. The microscope images revealed some new insights into the theory of XRF fusions. It could clearly be seen that dissociation of the minerals in the sample occurred, thus proving that no mineralogical effects exist in a fused glass bead, and it could be observed that the flux oxide mixture devitrify when over saturated. / Dissertation (MSc)--University of Pretoria, 2010. / Chemistry / unrestricted

The study aims to achieve an understanding of the artist’s materials and techniques used by Lucky Madlo Sibiya when he created his carved and painted wood panel artworks. A survey of the artist’s materials and techniques is of great importance, because he is represented in multiple institutional, corporate and private collections – including the University of Pretoria. His carved and painted wood panel artworks are also reaching an age (at least 20 years old, as 2019 is the twentieth anniversary of his death) when they would soon require conservation and restoration, if not stored and displayed according to sound conservation conditions and standards. For best-practice conservation and restoration, in-depth knowledge of the materiality of an artwork is needed. In order to reach an in-depth knowledge of the materiality of Sibiya’s carved and painted wood panel artworks, the survey intends to examine and document through the combination of various historical, visual and analytical techniques artworks with unrefuted provenance. The analytical techniques used are popular in heritage conservation, because they are non-invasive and non-destructive. They include provenance studies, visual examination, technical photography, X-ray Fluorescence and Fourier-transform Infrared Spectroscopy. In combination, the techniques should reveal the materials and techniques Sibiya employed. This knowledge will be used to safeguard and preserve this part of South African art heritage. / Mini Dissertation (MSocSci)--University of Pretoria, 2020. / Tangible Heritage Conservation / MSocSci (Tangible Heritage Conservation) / Unrestricted

Sediment records of two Italian subalpine lakes (Lake Garda and Lake Ledro) were analyzed in order to reconstruct their ecological evolution over the past several hundred years. A multi-proxy and multi-site approach was applied in order to disentangle the effects of local anthropogenic forcings, such as nutrients, and climate impacts on the two lakes and their catchments. Biological indicators (sub-fossil pigments, diatoms and Cladocera) were used to reconstruct changes in the aquatic food web and to define the lake reference conditions, while geochemical methods, i.e. wavelength-dispersive X-ray fluorescence spectroscopy (WD-XRF), were used to provide quantitative information on the different physical or chemical processes affecting both lake and catchment systems. Sub-fossil pigments and diatoms, together with their respective inferred TP values, suggested very stable oligotrophic conditions in both lakes until the 1960s. The period following was affected by nutrient enrichment, which led to a drastic shift in the phytoplanktonic community. The response of sub-fossil pigments and diatoms to major climatic anomalies such as the Medieval Climatic Anomaly (MCA) and the Little Ice Age (LIA) were not pronounced, and the taxonomic composition remained relatively stable. On the contrary, these proxies showed an indirect response to climate variability since the beginning of the nutrient enrichment phase in the 1960s. In Lake Garda, the winter temperature regulates the water column mixing, which in its turn controls the degree of nutrient fertilization of the entire water column, and the related phytoplankton growth. In Lake Ledro a rapid reorganization of planktonic diatoms was observed only during the temperature recovery after the LIA, while recent temperature effects are masked by the prevailing nutrient effects. In Lake Garda, Cladocera remains responded in quantitative and qualitative terms to climatic changes, whereas in Lake Ledro they appeared to be mainly affected by variations in hydrological regimes, i.e. flood events. Cladocera remains corroborated the nutrient enrichment after the 1960s in both lakes as inferred by diatoms and pigments. In Lake Garda, the geochemical data showed a pronounced shift in elemental composition since the mid-1900s, when major elements and lithogenic tracers started to decrease, while some elements related to redox conditions and other (contaminant) trace elements increased. The general trends since the mid-1900s agree with the biological records. However, some differences recorded in the two different basins of Lake Garda reflected the effects of local conditions, both related to hydrology and sedimentation patterns. Lake Ledro showed higher short-term variability for most elements, even though some features were comparable to Lake Garda. The geochemical record of Lake Ledro revealed a major influence of human-induced lake-level fluctuations and catchment properties. This paleolimnological study allows us to place temporally restricted limnological surveys into a longer-term secular perspective, which is highly valuable for the definition of lake reference conditions. Because the restoration targets are usually based on the lake reference conditions, this study highlighted also the necessity to pay particular attention to the lake-specific sensitivity patterns. The multi-proxy and multi-site approach showed that the lake conditions of large and deep lakes in northern Italy, such as Lake Garda, are mainly driven by nutrient enrichment and/or climate change. In contrast, smaller lakes with larger catchment areas, such as Lake Ledro, are seemingly more impacted by conditions and processes occurring in the drainage basin.

The elemental analysis of soil is useful in forensic and environmental sciences. Methods were developed and optimized for two laser-based multi-element analysis techniques: laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS) and laser-induced breakdown spectroscopy (LIBS). This work represents the first use of a 266 nm laser for forensic soil analysis by LIBS. Sample preparation methods were developed and optimized for a variety of sample types, including pellets for large bulk soil specimens (470 mg) and sediment-laden filters (47 mg), and tape-mounting for small transfer evidence specimens (10 mg). Analytical performance for sediment filter pellets and tape-mounted soils was similar to that achieved with bulk pellets. An inter-laboratory comparison exercise was designed to evaluate the performance of the LA-ICP-MS and LIBS methods, as well as for micro X-ray fluorescence (μXRF), across multiple laboratories. Limits of detection (LODs) were 0.01-23 ppm for LA-ICP-MS, 0.25-574 ppm for LIBS, 16-4400 ppm for µXRF, and well below the levels normally seen in soils. Good intra-laboratory precision (≤ 6 % relative standard deviation (RSD) for LA-ICP-MS; ≤ 8 % for µXRF; ≤ 17 % for LIBS) and inter-laboratory precision (≤ 19 % for LA-ICP-MS; ≤ 25 % for µXRF) were achieved for most elements, which is encouraging for a first inter-laboratory exercise. While LIBS generally has higher LODs and RSDs than LA-ICP-MS, both were capable of generating good quality multi-element data sufficient for discrimination purposes. Multivariate methods using principal components analysis (PCA) and linear discriminant analysis (LDA) were developed for discriminations of soils from different sources. Specimens from different sites that were indistinguishable by color alone were discriminated by elemental analysis. Correct classification rates of 94.5 % or better were achieved in a simulated forensic discrimination of three similar sites for both LIBS and LA-ICP-MS. Results for tape-mounted specimens were nearly identical to those achieved with pellets. Methods were tested on soils from USA, Canada and Tanzania. Within-site heterogeneity was site-specific. Elemental differences were greatest for specimens separated by large distances, even within the same lithology. Elemental profiles can be used to discriminate soils from different locations and narrow down locations even when mineralogy is similar.

Submitted by Eunice Novais (enovais@uepg.br) on 2018-06-28T19:18:21Z No. of bitstreams: 2 license_rdf: 811 bytes, checksum: e39d27027a6cc9cb039ad269a5db8e34 (MD5) Talita Rosas Ferreira.pdf: 3918159 bytes, checksum: 3af8401f079b1540a49f10a3f6fd3b2d (MD5) / Made available in DSpace on 2018-06-28T19:18:21Z (GMT). No. of bitstreams: 2 license_rdf: 811 bytes, checksum: e39d27027a6cc9cb039ad269a5db8e34 (MD5) Talita Rosas Ferreira.pdf: 3918159 bytes, checksum: 3af8401f079b1540a49f10a3f6fd3b2d (MD5) Previous issue date: 2018-04-23 / No presente estudo, foram investigados os efeitos da calagem superficial sobre: os atributos químicos, as propriedades de interação com a radiação e a estrutura (sistema poroso) de um Cambissolo Háplico alumínico. A estrutura do solo foi analisada em escala micrométrica, considerando monólitos (8×8×8 cm) e pequenos agregados do solo (2-4 e 1-2 mm de diâmetro). O experimento consistia de cinco faixas, uma delas em área de pasto, considerada como referência (REF) e representando as condições do solo antes da implementação do sistema de plantio direto (SPD), e as demais, sob SPD, receberam as seguintes doses de calcário: 0 (C0), 10 (C10), 15 (C15) e 20 (C20) t ha-1 aplicadas na superfície do solo. A coleta das amostras se deu aos trinta meses após o procedimento de calagem, nas camadas 0-10 cm (A) e 10-20 cm (B). Os atributos químicos do solo foram caracterizados de acordo com procedimentos experimentais padrões e a composição de óxidos do solo, obtida por meio de análise de espectroscopia de fluorescência de raios X (FRX), foi usada para o cálculo do coeficiente de atenuação de massa do solo (μm), por meio do código computacional XCOM, para as energias de ≈ 60 keV (241Am) e ≈ 662 keV (137Cs). Os valores de μm foram utilizados para calcular as demais propriedades de interação da radiação com o solo e para simular as variações causadas na densidade (D) e porosidade total (Pt) do solo. Para a análise da estrutura do solo, foram utilizadas imagens 3D de microtomografia computadorizada de raios X (μTC), com resolução espacial de 60 μm (monólitos), e de μTC utilizando radiação síncrotron (μTC-RS), com resolução espacial de 1,64 μm (agregados). A visualização, processamento e análise das imagens foram realizadas com o software Avizo Fire. Foram determinadas as seguintes propriedades micromorfológicas e geométricas: porosidade baseada na imagem (P’), número de poros (NP), distribuições de P’ e NP em função de intervalos de volume, comprimento, alongamento, formato, conectividade e tortuosidade dos poros (monólitos); e: P’, distribuições de P’ e NP em função de intervalos de volume, conectividade, tortuosidade e dimensão fractal (agregados). Complementarmente, a composição elementar dos agregados do solo foi avaliada por meio de medidas de FRX. Na maioria dos casos, os efeitos da calagem concentraram-se na camada A, onde houve melhora nos atributos químicos e, portanto, no grau de acidez do solo, bem como houve aumento nas propriedades de interação da radiação em função das doses de calcário. O aumento nas propriedades de interação da radiação foi mais acentuado para a energia de ≈ 60 keV em relação a ≈ 662 keV e, no primeiro caso, as mudanças causadas em μm promoveram variação considerável na D e Pt do solo, demonstrando a relevância do estudo. A exemplo dos efeitos da calagem sobre o sistema poroso de monólitos do solo, na camada A, ressalta-se o aumento de P’ e do número de poros em que o poro principal foi separado, os quais foram identificados como sendo mais alongados e mais conectados devido à calagem. A calagem promoveu ainda alterações no arranjo dos poros separados, em ambas as camadas, com a formação de poros cilíndricos na direção horizontal, o que pode ser atribuído ao estímulo da atividade da fauna do solo. Para os agregados de solo, na camada A, a porcentagem de cálcio foi elevada a um valor mais alto em agregados de 1-2 mm em comparação com aqueles de 2-4 mm, em função das doses de calcário. A calagem afetou negativamente a estrutura de pequenos agregados do solo, diminuindo a P’ e aumentando a tortuosidade de poros para agregados de 1-2 mm. Além disso, a calagem reduziu a dimensão fractal em agregados de ambas as classes de tamanhos, em acordo com o fato de que, com a calagem, poros maiores foram substituídos por poros menores em agregados de 1-2 mm, conforme análises de natureza quantitativa e qualitativa. / In the present study, effects of surface liming on: chemical attributes, soil-radiation interaction properties and the structure (porous system) of a Dystrudept soil were investigated. The soil structure was analyzed in micrometric scale, considering monoliths (8×8×8 cm) and tiny aggregates (2-4 and 1-2 mm in diameter). The trial consisted of five stripes, one of them under pasture, considered here as reference (REF), representing the soil conditions before the no-till system (NTS) implementation, and the remaining, under NTS, received the following lime rates: 0 (C0), 10 (C10), 15 (C15) and 20 (C20) t ha-1 on the soil surface. Samples were collected thirty months after the liming procedure, at the 0-10 cm (A) and 10-20 cm (B) soil layers. The soil chemical attributes were characterized according to standard experimental procedures and the soil oxide composition, obtained by X-ray fluorescence spectroscopy (XRF), was used for the calculation of the soil mass attenuation coefficient (μm), by means of the computer code XCOM, for the energies of ≈ 60 keV (241Am) amd ≈ 662 keV (137Cs). The μm values were used to calculate the remaining soil-radiation interaction properties and to simulate variations caused on soil density (D) and total porosity (Pt). For the soil structure analysis, 3D images of X-ray computed microtomography (μCT), with spatial resolution of 60 μm (monoliths), and 3D images of synchrotron radiation based X-ray computed microtomography (SR-μCT), with spatial resolution of 1,64 μm (aggregates) were used. The image visualization, processing and analysis were performed in the Avizo Fire software. The following micromorphological and geometrical properties were determined: image-based porosity (P’), number of pores (NP), distributions of P’ and NP as function of volume intervals, length, elongation, shape, connectivity, and tortuosity of pores (monoliths); and: P’, distributions of P’ and NP as function of volume intervals, connectivity, tortuosity, and fractal dimension (aggregates). Additionally, the elemental composition of the soil aggregates was evaluated by XRF. In the majority of cases, liming effects were concentrated at layer A, where there was an improvement of soil chemical attributes and, therefore, of soil acidity level, as well as there was an increase in the soil-radiation interaction properties as function of lime rates. The increase in soil-radiation interaction properties was more accentuated for the energy of ≈ 60 keV in relation to ≈ 662 keV and, in the former case, the μm variation promoted considerable variation in D and Pt, demonstrating the relevance of the study. Highlighted instances of liming effects on the porous system of the soil monoliths, at layer A, were an increase in P’ and in the number of pores into which the main soil pore was separated, which were identified as being longer and more connected due to liming. Moreover, liming promoted changes in the arrangement of the separated pores, at both soil layers, with the formation of cylindrical pores in the horizontal orientation, which can be attributed to stimulation of the soil fauna activity. Regarding the soil aggregates, at layer A, calcium was raised to a higher percentage in aggregates of 1-2 mm when compared to those of 2-4 mm, as function of the lime rates. Liming affected negatively the structure of the soil tiny aggregates, decreasing P’ and increasing the tortuosity of pores for 1-2 mm aggregates. Besides, liming decreased the fractal dimension in aggregates from both size classes, in accord to the fact that, with liming, larger pores were replaced by smaller ones in 1-2 mm aggregates, as both quantitatively and qualitatively analyzed.