O regolito é o manto do intemperismo existente sobre as rochas. Este manto pode ser constituído estruturalmente por três entidades distintas denominadas, solo, sedimento e saprolito. Ambas são produtos da intemperização das rochas. No entanto, o saprolito é definido como o único produto não transportado da intemperização isovolumétrica do litotipo originário. Diferente dos solos, dos sedimentos ou das rochas, não existe uma ciência específica para o estudo dos saprolitos. A saprolitologia não existe oficialmente, porém, pode ser implicitamente encontrada em trabalhos científicos de todo o mundo. No primeiro capítulo da tese, apresenta-se o estado da arte dos estudos dos saprolitos e sugere-se a consolidação da saprolitologia com o intuito de incentivar o incremento das pesquisas voltadas a esta entidade ainda pouco conhecida. De fato, os processos relacionados à intemperização isovolumétrica das rochas ainda não foram completamente compreendidos. Neste contexto, o Estado de Pernambuco, no nordeste do Brasil, apresenta condições geomorfológicas e climáticas propícias ao estudo da formação de saprolitos. No segundo capítulo da tese, demonstra-se que o intemperismo isovolumétrico de treze rochas cristalinas foi mais influenciado pelas condições microambientais, a exemplo da dinâmica da água através da microestrutura, do que pelas condições macroambientais. Posteriormente ao intemperismo isovolumétrico, diferenças morfológicas e geoquímicas ocorrem durante a evolução vertical do regolito. Entretanto, os domínios da saprolitogênese e da pedogênese são difíceis de diferenciar. No terceiro capítulo da tese, avaliou-se a evolução morfológica, estrutural e geoquímica de treze perfis formados por sistemas solo-saprolitos derivados do embasamento cristalino do Estado de Pernambuco. Anomalias nos índices de mensuração do intemperismo demonstram que o aumento gradual do grau de intemperização dos horizontes mais superficiais em relação aos horizontes inferiores não é a regra durante a evolução vertical do regolito. Em adição, a geoquímica e a morfologia dos perfis estudados indicam que alguns sistemas solo-saprolitos desenvolveram-se de forma interligada e outros apresentam evidências de que a formação do saprolito pode ter ocorrido após a formação do solo sobrejacente. Durante a evolução do regolito, o solo e o saprolito influenciam processos essenciais ao meio ambiente. No quarto capítulo da tese, descrevem-se as implicações agrícolas e ambientais dos treze perfis descritos no terceiro capítulo. Os resultados sugerem que os processos geoquímicos existentes nos sistemas solo-saprolitos, a exemplo da \"mineral carbonation\", influenciam o fluxo de elementos através do ecossistema circundante e demonstram que os saprolitos possuem importância agrícola e ambiental análoga à dos solos, influenciando processos de relevância agroambientais tais como a dinâmica da água, a retenção e transporte de nutrientes e/ou a retenção e transporte de contaminantes ou poluentes. / The regolith is the mantle of weathering above the rocks. This mantle may consist of three structurally distinct entities denominated sediment, soil and saprolite. All are products of rock weathering. Saprolite is defined as the product of in situ, isovolumetric weathering of the lithotype. Unlike the soils, sediments or rocks, there is no specific science dedicated to the study of saprolite. The saprolihtology does not exist formally. However, it can implicitly be found in scientific papers from around the world. The first chapter of the thesis presents the state of the art of saprolite studies and suggests the consolidation of saprolithology in order to encourage the development of research focused in this entity poorly known. In fact, the processes related to the isovolumetric weathering of rocks are not yet fully understood. In this context, the Pernambuco State in Northeastern Brazil have geomorphological and climatic conditions prone to the study of the saprolite formation and evolution. The second chapter of this thesis demonstrates that the isovolumetric weathering of the thirteen crystalline rocks was more influenced by microenvironmental conditions, such as the water dynamics through the microstructure, than the macro-environmental conditions. Subsequent to isovolumetric weathering, morphological and geochemical differenciation occur during the vertical evolution of regolith. However, it is difficult to differentiate the domains of saprolithogenesis and pedogenesis. The third chapter of the thesis reports the morphological, structural and geochemical evolution of the thirteen profiles formed by soil-saprolite systems derived from the crystalline basement of the Pernambuco State. Anomalies in the weathering measurement indexes showed that the gradual increase in the degree of weathering from the surface horizons towards the subsurface horizons is not the rule for the vertical development of regolito. In addition, the geochemistry and the morphology of the studied profiles indicate that some soil-saprolite systems evolved in an interconnected way and others provide evidence that the formation of saprolite may have occurred after the formation of the overlying soil. During the regolith evolution, soil and saprolite influence key environmental processes. The fourth chapter describes the agricultural and environmental implications of the processes acting in the thirteen profiles described in the third chapter. The results suggest that existing processes in geochemical soil-saprolite systems, such as the mineral carbonation, have influenced the elements flow through the surrounding ecosystem and demonstrate that saprolites have agricultural and environmental importance analogous to soil, influencing processes such as water fluxes, retention and transport of nutrients and/or of contaminants or pollutants.

En l’espace de cinquante ans l’exploitation minière d’uranium en France a généré 163 millions de tonnes de stériles miniers à l’échelle du territoire. Ces stériles, stockés sous forme de verses sont sujets à une altération météorique accrue par rapport à un massif granitique naturel. Dans le cadre du plan de gestion des matériaux et déchets radioactifs (PNGMDR) les stériles miniers sont l’objet d’une attention particulière visant à caractériser leur impact environnemental. Cette étude précise la géostructure des verses à stériles avec le développement d’un modèle structural typique pour aboutir à une caractérisation géochimique et minéralogique de ces stériles et permettre d’évaluer la stabilité de l’uranium. De cette étude, il apparaît très clairement que l’uranium est principalement associé aux phosphates, dans des phases héritées telles que les monazites ou sous formes d’uranyle-phosphates secondaires. Lorsque l’U est associé à des oxyhydroxydes de fer amorphes, le phosphore est également présent. Cette étude illustre le rôle majeur que peuvent jouer les oxyhydroxydes de fer et le phosphore dans le piégeage de l’uranium. Ces phases constituent un piège efficace et relativement stable, permettant de limiter les concentrations en uranium en solution à condition que les conditions environnementales restent stables. Quand bien même des changements d’équilibre auraient lieu, la présence de smectite dans les échantillons de la verse à stériles présente une barrière supplémentaire à la diffusion de l’uranium dans l’environnement. / In a time span of 50 years uranium mining in France generated 163 Mt of waste rocks. These form waste rocks piles which are subjected to enhanced weathering compared to natural granitic outcrops. Therefore, as part of the French radioactive waste and material management plan (PNGMDR), waste rocks are studied in order to assess their potential environmental impact. This study specifically focuses on the internal structure of waste rock piles complemented by geochemistry and mineralogical data, in order to develop a model that assesses the waste rock pile’s weathering state and uranium’s stability. Results show uranium (U) is mainly associated to phosphates, either in primary accessory minerals, such as monazites, or crystallized in secondary uranyl-phosphates. When U is associated to amorphous iron oxyhydroxides, phosphorous is also associated. The importance of iron oxyhydroxides and phosphorous in uranium trapping is clearly demonstrated. Both iron oxyhydroxides as well as uranyl-phosphates form efficient and stable U traps, limiting U dissolution as long as pH, redox and temperature parameters remain stable. In case of variable conditions, smectite identified in the waste rock pile might also play a role in preventing further uranium diffusion.

<p>Relict non-glacial surfaces occur in many formerly glaciated landscapes, where they represent areas that have escaped significant glacial modification. Frequently distinguished by blockfield mantles, relict non-glacial surfaces are important archives of long-term weathering and landscape evolution processes. The aim of this thesis is to examine the distribution, weathering, ages, and formation of relict non-glacial surfaces in the northern Swedish mountains.</p><p>Mapping of surfaces from aerial photographs and analysis in a GIS revealed five types of relict non-glacial surfaces that reflect differences in surface process types or rates according to elevation, gradient, and bedrock lithology. Clast characteristics and fine matrix granulometry, chemistry, and mineralogy reveal minimal chemical weathering of the blockfields.</p><p>Terrestrial cosmogenic nuclides were measured in quartz samples from two blockfield-mantled summits and a numerical ice sheet model was applied to account for periods of surface burial beneath ice sheets and nuclide production rate changes attributable to glacial isostasy. Total surface histories for each summit are almost certainly, but not unequivocally, confined to the Quaternary. Maximum modelled erosion rates are as low as 4.0 mm/kyr, which is likely to be near the low extreme for relict non-glacial surfaces in this landscape.</p><p>The blockfields of the northern Swedish mountains are Quaternary features formed through subsurface physical weathering processes. While there is no need to appeal to Neogene chemical weathering to explain blockfield origins, these surfaces have remained continuously regolith-mantled and non-glacial since their inception. Polygenetic surface histories are therefore indicated, where the large-scale surface morphologies are potentially older than their regolith mantles.</p>

<p>The properties of Mercury's regolith have been investigated at optical and near-infrared wavelengths with high-resolution imaging, photometric, and spectroscopic observations with the Swedish Vacuum Solar Telescope and the Nordic Optical Telescope. </p><p>A new global optical map at a spatial resolution of 200 km shows that the well known (from Mariner 10) and poorly known hemispheres are indistinguishable with respect to the distribution, number density, and morphological parameters of bright albedo features. This indicates a globally uniform recent (<3 Gyr) geologic evolution, a compositionally very homogeneous surface and the absence of a lunar-like mare–terrae albedo dichotomy.</p><p>It is found that the spectrum of Mercury is linear, strongly sloped, lacks detectable absorption features and displays a unique relation between the continuum slope and photometric geometry. Mercury has a photometrically smoother surface than the average near-side Moon, and is 10–15% fainter and 50% more back scattering in the V-band. Unlike the case for the Moon, the average single-particle backscattering anisotropy increases with wavelength.</p><p>Intimate regolith mixing models are used to determine a probable surface composition of predominantly Ca-rich labradorite plagioclase feldspar with minor low-iron enstatitic orthopyroxene, and rule out high-iron pyroxenes or olivines as other than insignificant constituents. Abundances of FeO ~1.2 wt%, TiO₂ ~0 wt%, and submicroscopic metallic iron ~0.1–0.3 wt% are found for the average surface. This implies an optically active grain size of 15–30 μm that is a factor of two smaller than for the Moon.</p><p>A numerical integration study shows that hermeocentric orbits with semi-major axes <30 mercurian radii for elliptic retrograde, and circular prograde, object are stable for durations in excess of 4.5 Myr. The weak gravitational scattering effect of Mercury indicates that re-impacting particles may have been important for the early evolution of its crust.</p>

Relict non-glacial surfaces occur in many formerly glaciated landscapes, where they represent areas that have escaped significant glacial modification. Frequently distinguished by blockfield mantles, relict non-glacial surfaces are important archives of long-term weathering and landscape evolution processes. The aim of this thesis is to examine the distribution, weathering, ages, and formation of relict non-glacial surfaces in the northern Swedish mountains. Mapping of surfaces from aerial photographs and analysis in a GIS revealed five types of relict non-glacial surfaces that reflect differences in surface process types or rates according to elevation, gradient, and bedrock lithology. Clast characteristics and fine matrix granulometry, chemistry, and mineralogy reveal minimal chemical weathering of the blockfields. Terrestrial cosmogenic nuclides were measured in quartz samples from two blockfield-mantled summits and a numerical ice sheet model was applied to account for periods of surface burial beneath ice sheets and nuclide production rate changes attributable to glacial isostasy. Total surface histories for each summit are almost certainly, but not unequivocally, confined to the Quaternary. Maximum modelled erosion rates are as low as 4.0 mm/kyr, which is likely to be near the low extreme for relict non-glacial surfaces in this landscape. The blockfields of the northern Swedish mountains are Quaternary features formed through subsurface physical weathering processes. While there is no need to appeal to Neogene chemical weathering to explain blockfield origins, these surfaces have remained continuously regolith-mantled and non-glacial since their inception. Polygenetic surface histories are therefore indicated, where the large-scale surface morphologies are potentially older than their regolith mantles.

The properties of Mercury's regolith have been investigated at optical and near-infrared wavelengths with high-resolution imaging, photometric, and spectroscopic observations with the Swedish Vacuum Solar Telescope and the Nordic Optical Telescope. A new global optical map at a spatial resolution of 200 km shows that the well known (from Mariner 10) and poorly known hemispheres are indistinguishable with respect to the distribution, number density, and morphological parameters of bright albedo features. This indicates a globally uniform recent (&lt;3 Gyr) geologic evolution, a compositionally very homogeneous surface and the absence of a lunar-like mare–terrae albedo dichotomy. It is found that the spectrum of Mercury is linear, strongly sloped, lacks detectable absorption features and displays a unique relation between the continuum slope and photometric geometry. Mercury has a photometrically smoother surface than the average near-side Moon, and is 10–15% fainter and 50% more back scattering in the V-band. Unlike the case for the Moon, the average single-particle backscattering anisotropy increases with wavelength. Intimate regolith mixing models are used to determine a probable surface composition of predominantly Ca-rich labradorite plagioclase feldspar with minor low-iron enstatitic orthopyroxene, and rule out high-iron pyroxenes or olivines as other than insignificant constituents. Abundances of FeO ~1.2 wt%, TiO2 ~0 wt%, and submicroscopic metallic iron ~0.1–0.3 wt% are found for the average surface. This implies an optically active grain size of 15–30 μm that is a factor of two smaller than for the Moon. A numerical integration study shows that hermeocentric orbits with semi-major axes &lt;30 mercurian radii for elliptic retrograde, and circular prograde, object are stable for durations in excess of 4.5 Myr. The weak gravitational scattering effect of Mercury indicates that re-impacting particles may have been important for the early evolution of its crust.

Increasing concerns over future anthropogenic effects on climate change as a result of increasing greenhouse gases generate concomitant efforts to better characterize recent climate in order to more accurately predict climate in the future. To this end, a multiproxy study of climate variability in western Ireland from lacustrine sediment was undertaken. The interpretation of paleoclimate records derived from lacustrine carbonate minerals is difficult without a good understanding of the mechanisms that generate variation in isotope values of modern surface waters. Variation in surface waters are ultimately incorporated into lacustrine sediment records conflated by temperature. Therefore, a study of the spatial distribution of ä¹⁸O and äD values of lake and river waters from 144 locations in Ireland has been conducted to provide insight into the behavior of lakes and rivers in Ireland, including source, recycling and loss through evapotranspiration. A 7.6 m sediment core was recovered from Lough Inchiquin that provides evidence for rapid and long-term climate change from the Late Glacial to the Holocene. This was determined using carbon and oxygen isotope analyses of lacustrine calcite as well as carbon from bulk organic sediment fractions. Several significant climate perturbations were identified in the ä¹⁸O_calcite record such as the Oldest Dryas, Younger Dryas, and the 8.2 ka cold event. A previously undescribed climate anomaly between 7,300 to 6,700 cal. yr B.P. characterized by low ä¹⁸O</span>_calcite values with high frequency variability. Variations in carbon isotopes of calcite and bulk organics from the Late Glacial to the Holocene are significant in magnitude (~12) and have similar trends that record temporal shifts in the relative contributions of carbon from the weathering of limestone versus the weathering of terrestrial organic matter. ä¹³C_calcite and ä¹³C_org suggest a rapid recovery of terrestrial vegetation following the Younger Dryas. Change in Ää¹³C_{calcite - org} documents a rapid increase in exogenous fluxes of carbon into the lake at ~9 ka.

Increasing concerns over future anthropogenic effects on climate change as a result of increasing greenhouse gases generate concomitant efforts to better characterize recent climate in order to more accurately predict climate in the future. To this end, a multiproxy study of climate variability in western Ireland from lacustrine sediment was undertaken. The interpretation of paleoclimate records derived from lacustrine carbonate minerals is difficult without a good understanding of the mechanisms that generate variation in isotope values of modern surface waters. Variation in surface waters are ultimately incorporated into lacustrine sediment records conflated by temperature. Therefore, a study of the spatial distribution of ä¹⁸O and äD values of lake and river waters from 144 locations in Ireland has been conducted to provide insight into the behavior of lakes and rivers in Ireland, including source, recycling and loss through evapotranspiration. A 7.6 m sediment core was recovered from Lough Inchiquin that provides evidence for rapid and long-term climate change from the Late Glacial to the Holocene. This was determined using carbon and oxygen isotope analyses of lacustrine calcite as well as carbon from bulk organic sediment fractions. Several significant climate perturbations were identified in the ä¹⁸O_calcite record such as the Oldest Dryas, Younger Dryas, and the 8.2 ka cold event. A previously undescribed climate anomaly between 7,300 to 6,700 cal. yr B.P. characterized by low ä¹⁸O</span>_calcite values with high frequency variability. Variations in carbon isotopes of calcite and bulk organics from the Late Glacial to the Holocene are significant in magnitude (~12) and have similar trends that record temporal shifts in the relative contributions of carbon from the weathering of limestone versus the weathering of terrestrial organic matter. ä¹³C_calcite and ä¹³C_org suggest a rapid recovery of terrestrial vegetation following the Younger Dryas. Change in Ää¹³C_{calcite - org} documents a rapid increase in exogenous fluxes of carbon into the lake at ~9 ka.

The Savannah River Site (SRS) deposits in the Southeastern US between 30-45 m of depth are calcium carbonate-rich, marine-skeletal, Eocene-aged sediments with varying clastic content and extensive diagenetic alteration, including meter-sized caves that coexist with brittle and hard limestone. An experimental investigation including geotechnical (P- and S-wave velocities, tensile strength, porosity) and geochemical (EDS, XRD, SEM, N2-adsorption, stable isotopes, K-Ar age dating, ICP-assisted solubility, groundwater) studies highlighted the contrast between hard and brittle limestones, their relationship with cave formation, and allowed calculation of parameters for geochemical modeling. Results demonstrate that brittle and hard limestones bear distinct geochemical signatures whereby the latter exhibits higher crystallinity, lower clastic load, and freshwater-influenced composition. Results also reveal carbonate diagenesis pathways likely driven by geologic-time seawater/freshwater cycles, microorganism-driven micritization, and freshwater micrite lithification. The second section of this investigation dealt with SRS surface soils which are largely coarse-grained and rich in iron oxides with various degrees of maturity. These soils were simulated in the laboratory using Ottawa sands that were chemically coated with goethite and hematite. Surface (SEM, AFM, N2-adsorption) and geotechnical properties (fabric, small-strain stiffness, shear strength) were investigated on the resulting "soil analog". Results indicate that iron-oxide coated sands bear distinct inherent fabric and enhanced small-strain stiffness and critical state parameters when compared to uncoated sands. Contact mechanics analyses suggest that iron oxide coatings yield an increased number of grain-to-grain contacts, higher surface roughness, and interlocking, which are believed to be responsible for the observed properties.

<p>Coatings for exterior wood have two basic functions. One isto give an aesthetically acceptable surface appearance andcolour. The other is to provide protection against wooddegradation by microbiological or physical attack. Theseprotective properties, often called the barrier properties,play an important role in the selection of proper material forsupreme durability. The assessment of these barrier propertiesis of great importance. Within the CEN Technical Committee 139,Working Group 2, Coatings for exterior wood test methods andperformance specifications have been established. Forassessment of water protection efficiency a standard testprocedure, EN 927-5, has been launched. The present work hasfocused on its applicability in assessing water protectionefficiency in relation to the degradation of coatings duringexposure.</p><p>Assessments according to EN 927-5 is shown to givesignificant differences in water absorption values fordifferent types of coatings on wood. The proposed performancespecifications in ENV 927 - 2 for the water absorption valuesfor coatings to be used in different constructions seem to beset at acceptable levels. It has been shown that there is agood correlation between the level of water absorption andpractical experience of the performance of paints inScandinavia. However, it has also been shown that thecombination of a standard procedure for water absorptionmeasurement and an artificial weathering procedure gives moreinformation regarding expected durability and longtermperformance than a single measurement of water absorption onfresh, unweathered coated wood. A combination of waterabsorption measurement and artificial weathering could become auseful tool in product development as well as in benchmarking.Together with statistical tools, such as reliability-basedservice life prediction methodologies for predicting theservice life of coating systems a reduction in testing timesmay be achieved.</p><p>Surface-active substances in coatings have a negative effecton the coatings ability to prevent water ingress, which mostprobably is due to the hydrophilic character of thesesubstances. The presence of these substances, which are commonin waterborne coatings, alters the moisture sorptioncharacteristics of wood. Considering that these substancesoccur in waterborne coatings, may be mobilised during and afterfilm formation and accumulate at the coating/substrateinterface, there is a great probability that these substanceschange the moisture sorption characteristics of the woodsubstrate in an unfavourable way and create unexpected dynamicmoisture conditions at the coating/wood interface.</p><p>Computerized tomography has been found to be a valuable,non-destructive tool for visualising the spatial moisturedistribution of water and moisture in coated wood panels. Themethod is suitable for recurrent testing of a specimen exposedto a series of processes of wetting, drying. This thesis showsthat high moisture contents occur locally at and around cracks.In these areas there is an increased risk of internal tensionand stress resulting in crack initiation and propagation andthat high moisture contents may occur in the first fewmillimetres under waterborne coatings despite intact coatingfilms. Even with good barrier properties of the coating,moisture may accumulate by water-vapour absorption in air gapsbehind the cladding thus causing favourable conditions formicrobiological colonization.</p><p>The work that has been carried out regarding assessment ofthe water protection efficiency shows promising resultsregarding the possibility to use reliability-based service lifeprediction methodology for the assessment. The aim of futurework will be to establish more reliable techniques andprotocols for assessing service life expectancy and durability,especially for waterborne coatings with special focus ontendencies to early failure and robustness of the coatingsystems.</p><p><b>Keywords:</b>Coatings, surfactants, water absorption value,EN 927, paint, additives, moisture dynamics, absorption,desorption, artificial weathering, artificial exposure,computerized tomography, MRI.</p>