The focus of this study was analytical investigations of Egyptian paintings, mainly Coptic icons and Islamic wooden ceilings, dating from 1300-1900 using multiinstrumental techniques. Twenty three Coptic icons and three wooden ceilings dated from different periods and painted by different painters in case of icons were examined. The materials used including pigments, media, varnishes, ground layers and gold layers. The surface stratigraphy of paint samples, their layered structured and the composition of materials used in each layer were analysed. Variations in painting techniques, pigments palettes, paint media and varnishes applied in Egyptian paintings according to painters, time and type of paintings were revealed. A total of twenty-eight organic and inorganic pigments were identified in this study, of which nine have never been previously included as a part of the Egyptian pigment palettes, namely; smalt, lapis lazuli, indigo, pararealgar, Prussian blue, chrome yellow, barium yellow, barium white and hydromagnesite. The identification of hydromagnesite, which has never been to date considered as a pigment either in Egypt or elsewhere and the identification of smalt from the mid-14th century, whose reported earliest large scale use was in the 16th century. Two types of resins were identified as a constituent of the oil/resin varnish applied on Coptic icons of which Venice turpentine has been identified for the first time as an ingredient of Egyptian varnishes. The identification of mosaic gold in an 18th C. icon, a novel usage of dammar resin and the multilayered structure of the white ground layers were revealed. / Egyptian Ministry of Higher Educations

This thesis describes the development and use of a computer-automated microscopy routine for characterization of respirable dust particles from coal mines. Respirable dust in underground coal mining environments has long been known to pose an occupational health hazard for miners. Typically following years of exposure, coal workers' pneumoconiosis (CWP) and silicosis are the most common disease diagnoses. Although dramatic reductions in CWP and silicosis cases were achieved across the US between about 1970-1999 through a combination of regulatory dust exposure limits, improved ventilation and dust abatement practices, a resurgence in disease incidence has been noted more recently – particularly in parts of Appalachia. To shed light on this alarming trend and allow for better understanding of the role of respirable dust in development of disease, more must be learned about the specific characteristics of dust particles and occupational exposures. This work first sought to develop an automated routine for the characterization of respirable dust using scanning electron microscopy with energy dispersive x-ray (SEM-EDX). SEM-EDX is a powerful tool that allows determination of the size, shape, and chemistry of individual particles, but manual operation of the instrument is very time consuming and has the potential to introduce user bias. The automated method developed here provides for much more efficient analysis – with a data capture rate that is typically 25 times faster than that of the manual method on which it was based – and also eliminates bias between users. Moreover, due to its efficiency and broader coverage of a dust sample, it allows for characterization of a larger and more representative number of particles per sample. The routine was verified using respirable dust samples generated from known materials commonly observed in underground coal mines in the central Appalachian region, as well as field samples collected in this region. This effort demonstrated that particles between about 1-9μm were accurately classified with respect to defined chemical categories, and suggested that analysis of 500 particles across a large area of a sample filter generally provides representative results. The automated SEM-EDX routine was then used to characterize a total of 210 respirable dust samples collected in eight Appalachian coal mines. The mines were located in three distinct regions (i.e., northern, mid-central and south-central Appalachia), which differed in terms of primary mining method, coal seam thickness and mining height, and coal and/or rock mineralogy. Results were analyzed to determine whether number distributions of particle size, aspect ratio, and chemistry classification vary between and within distinct mine regions, and by general sampling location categories (i.e., intake, feeder, production, return). Key findings include: 1) Northern Appalachian mines have relatively higher fractions of coal, carbonate, and heavy mineral particles than the two central Appalachian regions, whereas central Appalachian mines have higher fractions of quartz and alumino-silicate particles. 2) Central Appalachian mines tended to have more mine-to-mine variations in size, shape, and chemistry distributions than northern Appalachian mines. 3) With respect to particle size, samples collected in locations in the production and return categories have the highest percentages of very small particles (i.e., 0.94-2.0μm), followed by the feeder and then the intake locations. 4) With respect to particle shape, samples collected in locations in the production and return categories have higher fractions of particles with moderate (i.e., length is 1.5 to 3x width) to relatively high aspect ratios (i.e., length is greater than 3x width) compared to feeder and intake samples. 5) Samples with relatively high fractions of alumino-silicates have higher fractions of particles with moderate aspect ratios than samples with low alumino-silicate fractions. 6) Samples with relatively high fractions of quartz particles have higher fractions of particles with moderate aspect ratios and higher percentages of very small particles than samples with no identified quartz particles. 7) Samples with high fractions of carbonates have higher percentages of particles with relatively low aspect ratios (i.e., length and width are similar) than samples with no identified carbonate particles. / Master of Science

Le platine (Pt), le palladium (Pd) et le rhodium (Rh), font partie des Eléments du Groupe du Platine (EGP), utilisés dans les catalyseurs automobiles. En raison de leur émission dans l'environnement, ces éléments peuvent aujourd'hui être considérés comme des contaminants émergeants et traceurs de la contamination automobile. Cette étude porte sur la dispersion des EGP depuis leur source (monolithes et émission à l'échappement) jusqu'au champ proche (atmosphère, poussières de chaussées, eaux de ruissellement, sédiment,sol de bord de route). Leur mobilité à partir de monolithes a été étudiée en présence d'eau de ruissellement et de molécules organiques. Leur spéciation a été évaluée dans les poussières de chaussées et les sédiments. Les teneurs en EGP dans les monolithes étudiés montrent le remplacement de Pt par Pd dans les catalyseurs récents. L'abondance relative des EGP dans les échantillons environnementaux est Pd > Pt > Rh. Les expérimentations de mobilisation montrent que la mobilisation des EGP est plus significative au contact des molécules organiques, est dépendante du pH de la solution et augmente avec l'âge du monolithe. Rh est l'élément le plus mobilisable dans les monolithes. La spéciation montre que les EGP sont peu mobiles. Dans la part mobilisable, ils sont majoritairement liés à la fraction dite organique. / Platinum (Pt), palladium (Pd) and rhodium (Rh) (platinum-group elements; PGEs),are used in automotive catalytic converters to remove harmful emissions from exhaust gas. Nevertheless, nowadays, the PGEs are emerging as new environmental emission contaminators due to their increasing use. The goal of this research is to study the distribution of PGEs from the source (i.e. automotive catalytic converters and exhaust gas) to the environmental samples (i.e. atmospheric particles, road dust,storm water, pond sediments, and road-side soil). The mobility of PGEs from the converters in contact with run off water and natural complexing agents were studied. Also, the speciation of PGEs was investigated in road dust and pond sediments. Comparison of PGE contents in different catalysts confirms the replacement of Pt by Pd in more recent converters. Besides, the relative abundance of PGEs in environmental samples shows higher concentration of Pd compared toPt and Rh (i.e. Pd>Pt>Rh). The results of testing PGEs mobilization in catalytic converters demonstrate more significant mobilization by organic molecules as compared to run off water. Our results also show the dependency of PGEs mobilization on pH and on catalyst age. Among the PGEs, Rh was the most mobilized element in catalytic converters. More importantly, the speciation test shows that while PGEs are low mobile elements, in the mobilizable fraction, PGEs are in the organic fraction.

[pt] Este trabalho teve como objetivo caracterizar química e morfologicamente material particulado (PM2.5 e PM10) coletado na zona sul e oeste da cidade de Rio de Janeiro e na região metropolitana, utilizando técnicas como a Cromatografia de íons (CI), Espectrometria de Massas com Plasma Indutivamente Acoplado (ICPMS) e a Microscopia Eletrônica de Varredura acoplada ao Espectrômetro de RaiosX por Dispersão de Energia (MEV-EDX). Além disso, foram realizados ensaios toxicológicos com C. elegans para avaliar os efeitos da exposição ao material particulado (MP), nas diferentes frações de tamanho. Concentrações médias anuais de PM2.5 entre 7,40 +/- 3,96 (micrograma)m-3 e 17,4 +/- 7,38 (micrograma) m-3 foram medidas durante os anos 2015 e 2018, as quais foram inferiores ao padrão intermediário da qualidade do ar, estabelecido pelo CONAMA, registando-se as maiores médias anuais durante o 2016, ano em que foram realizados os Jogos Olímpicos. Resultados das análises químicas mostraram que o MP em todos os pontos de coleta estava constituído principalmente por espécies iônicas como Cl- , NO3 - , Na+ e SO4 2- e elementos como V, Ni, Cu, Cd, Sn e Pb, sendo determinadas apenas variações significativa (p menor que 0,05) nas concentrações de SO4 2- , NO3 - , Na+ , Cu e Sn, entre os períodos estudados. Através dos resultados das análises de MEV-EDX as partículas atmosféricas se classificaram segundo sua morfologia – Fuligem, esféricas, biológica e minerais- e segundo sua composição elementar – partículas com teor de enxofre, de cloro e de ferro -. Finalmente, efeitos tóxicos foram observados pela exposição ao PM10 e PM2.5 em organismos C. elegans, alterando parâmetros fisiológicos (e.g. crescimento e reprodução) e promovendo respostas dos mecanismos antioxidantes, como resultado do estresse oxidativo gerado por espécies presentes no MP. / [en] This work aimed to characterize chemically and morphologically particulate matter (PM2.5 and PM10) collected in the south and west zones of the city of Rio de Janeiro and in the metropolitan region, using techniques such as ion chromatography (IC), inductively coupled plasma mass spectrometry (ICP-MS) and Scanning electron microscopy- energy dispersive spectrometry (SEM-EDX). Annual mean concentrations of PM2.5 between 7,40 +/- 3,96 microgram m-3 e 17,4 +/- 7,38 microgram m-3 were measured during the years 2015 and 2018, which were lower than the intermediateair quality standard established by CONAMA, with the highest annual averages recorded during 2016, the year in which the Olympic Games were held. In addition, toxicological tests were performed with C. elegans to evaluate the effects of exposure to particulate matter (PM) in the different size fractions. Results of the chemical analysis showed that PM at all collection sites consists mainly of ionic species such Cl- , NO3 - , Na+ and SO4 2- and elements such as V, Ni, Cu, Cd, Sn and Pb, being determined only significant variations (p less than 0,05) in the concentrations of SO4 2- , NO3 - , Na+ , Cu, and Sn, between the studied periods. Based on the results of the SEM-EDX analysis, atmospheric particles were classified according to their morphology – Soot, spherical, biological and minerals- and according to their elemental composition – particles with sulfur, chlorine and iron content. Finally, toxic effects were observed by exposure C. elegans organisms to PM10 and PM2.5, altering physiological parameters (e.g growth and reproduction) and promoting antioxidant mechanisms responses, as a result of oxidative stress generated by compounds present in the PM.

Traditionally archaeology has referred to the anthropic sediments accumulated around prehistoric settlements with the blanket term ‘midden’. This is now recognised as an inadequate term to describe the complex formation processes and functions represented in these sediments. This thesis reviewed the body of evidence accumulated over the past century of research into Neolithic and Bronze Age settlements on the islands of the Scottish North Atlantic seaboard and extrapolated the many occurrences of ‘midden’. Several contexts emerged for these sediments including interior floors, hearths, exterior occupational surfaces, dumped deposits, building construction materials and abandonment infill. In addition, ‘midden’ is described added to cultivated soils to form fertile anthrosols. The way in which prehistoric communities exploited this material for agriculture and construction has been described through geoarchaeological research which implied that to past communities ‘midden’ was a valuable resource. This led to the formation of a model based upon a human ecodynamics framework to hypothesise sediment formation pathways. Rescue excavation at the Links of Noltland, Westray provided an opportunity to conduct a holistic landscape and fine resolution based study of Neolithic and Bronze Age settlement to test this model. The research incorporated auger survey, archaeological and geoarchaeological excavation, thin section micromorphology and SEM EDX analyses. Sediments identified in literature review and recovered from the field site were described using this toolkit and set within a cultural and environmental context. Results demonstrate that anthropic materials were incorporated into all contexts examined. Discrete burning and maintenance activities were found to have taken place during the gradual accumulation of open-air anthropic sediments whilst incorporation of fuel residues and hearth waste into floors lead to the gradual formation of ‘living floors’ inside structures. An unexpected discovery was evidence of animal penning within late Neolithic/Early Bronze Age settlement and the in situ burning of stabling waste. Three types iv | P a g e of land management strategy which relied upon the input of anthropic sediments were evidenced and the range and extent of anthropic inclusions in the landscape recorded. Spatial interpolation of auger survey data utilised a new sub-surface modelling technique being developed by the British Geological Survey to explore soil stratigraphic relationships in 3D. SEM EDX analysis supported micromorphological analysis providing chemical data for discrete inclusions and assisting in the identification of herbivore dun ash and the Orcadian funerary product ‘cramp’. SEM EDX analysis was also applied to fine organo-mineral material for statistical testing of nutrient loadings across context groups. It was found that anthropic sediments were enriched in macro and intermediate plant nutrients Mg, P, K, S and Ca compared to geological controls, and the application of anthropic material to cultivated soils improved soil fertility for the three observed land management practices. The versatility of anthropic sediments was explored through discussion of context groups based upon the results of this research and the potential significance of this material to prehistoric communities is explored.

The focus of this work is to investigate the dissolution of MW25, a non-radioactive simulant of UK high-level nuclear waste borosilicate glass, and to predict its performance in the near field of a geological repository. A single-pass flow-through (SPFT) experimental system was used to measure the forward dissolution rates of MW25. Experiments were conducted in two parts. Experiment Part 1 considers the dissolution of the waste glass in deionised water at 40 and 90 oC and circum-neutral pH. Experiment Part 2 considers the dissolution of the waste glass in simulant groundwaters, with similar compositions to groundwaters of Callovo-Oxfordian clay (lower-strength sedimentary rock (LSSR)) and Borrowdale Volcanic Group rocks (higher-strength rock (HSR)), at 40 oC and pH 7. The forward dissolution rate measured in deionised water was found to be approximately one order of magnitude higher at 90 oC than at 40 oC. A similar release was observed for Si, Mg and Al at 40 oC and 90 oC, whereas the B, Cs, Na, Li and Mo showed an order of magnitude increase when the temperature was increased from 40 to 90 oC for low q/S values. The activation energy (Ea) of the reactions shows that the dissolution process is a surface phenomenon. At 90 oC the net effect of the processes governing MW25 dissolution led to the preferential release of boron and alkali metals relative to the release of Si during the transient dissolution stage, accompanied by an increase in the concentration of silicic acid. This suggests that the solution activity of silicic acid at a higher temperature has a weak influence on the release of the mobile elements. The forward dissolution rate measured in LSSR simulant groundwater was found to be slightly higher than that measured in HSR simulant groundwater. The dissolution behaviour of MW25 in both groundwaters is consistent with its behaviour in deionised water at 40 oC, with the dissolution rates of elements increasing as flow rates were increased. However, forward dissolution rates measured in the simulant groundwaters were lower than the forward dissolution rates measured in deionised water under these experimental conditions. This is attributable to the interaction of the components of the simulant groundwaters with the glass, as revealed by post-reaction surface analyses, and a consequential lower alkalinity of the leachates collected in the experiments with simulant groundwater than in deionised water. Reactive chemical transport simulations of waste glass dissolution and radionuclide release in a hypothetical near field were conducted over a time span of a million years with GoldSim. The results showed that enclosing the waste glass in a steel canister covered by a copper canister and emplacing the waste package in a granite host rock is optimal for the long-term isolation of the radionuclides. The waste glass was found to play a significant role in the overall performance of the near field. This study features a new method for estimating the surface area of reacted glass powder more accurately than the geometric surface area estimate, which is the preferred standard method among researchers.

The Sámi’s past activities have been documented historically from a European perspective, and more recently from an anthropological viewpoint, giving a generalised observation of the Sámi, during the study period of AD200-AD1800, as semi-nomadic hunter gatherers, with several theories suggesting that interaction with Europeans, through trade, led to the adoption of European activities by certain groups of the Sámi (Eiermann, 1923; Paine, 1957; Manker and Vorren, 1962; Bratrein, 1981; Mathiesen et al, 1981; Meriot, 1984). However, there is almost no information on the impact the Sámi had on the landscape, either before or after any adoption of European activities, and none investigating what cultural footprint or indicators would remain from Sámi or European occupation and/or activity within the typically podzolic soils of Northern Sweden. Consequently the thesis aims to contribute to the gap in knowledge through the formation of a podzol model identifying the links between anthropogenic activity and the alteration of podzol soils, and through the creation of soils based models which identify the cultural indicators associated with both Sámi and European activity; formed from the identification of cultural indicators retained within known Sámi and European sites. The methods used to obtain the information needed to achieve this were the pH and magnetic susceptibility from bulk soil samples and micromorphological and chemical analysis of thin section slides through the use of standard microscopy and X-ray fluorescence from a scanning electron microscope. The analysis revealed that the Sámi had an extremely low impact on the landscape, leaving hard to detect cultural indicators related to reindeer herding in the form of reindeer faecal material with corresponding phosphorous peaks in the thin section slides. The European footprint however, was markedly different and very visible even within the acidic soil environment. The European indicators were cultivation based and included phosphorous and aluminium peaks as well as a deepened, highly homogenised plaggen style anthropogenic topsoil rich in ‘added’ materials. An abandoned European site which visibly and chemically shows the formation of a secondary albic horizon within the anthropogenic topsoil also provides an insight into the delicate balance of cultivated soil in northern Sweden, whilst reinforcing the outputs identified in the podzol model. Due to the almost invisible Sámi footprint on the landscape, areas of overlap were impossible to identify however, there was no evidence of the adoption of European cultivation activities at any of the Sámi sites investigated. The only known area of interaction between the two cultures was an official market place which had been a Sámi winter settlement prior to its use as a market site. This site showed none of the reindeer based Sámi indicators or the cultivation based European indicators, but did contain pottery fragments which could be linked to trade or occupation. Overall, the thesis reinforces the low impact expected of the semi-nomadic Sámi and sheds light on the underlying podzolic processes influencing the anthropogenically modified soils of Northern Sweden. The podzol model is reinforced by several findings throughout the thesis and the soils based cultural indicator models for both Sámi and European activity have been successfully tested against independent entomological and palynological data and therefore provide reliable reference material for future studies.