Cette étude est une contribution à l'étude de la dépollution des sols à l'aide d'une modélisation expérimentale. L'objectif du travail est d'étudier les processus physico-chimiques intervenant au cours du transport de polluants métalliques toxiques dans les sols soumis à un champ électrique. Les essais sont réalisés en laboratoire avec des sols obtenus à partir d'un mélange d'un sable de Fontainebleau avec une solution cationique de polluant. Les polluants étudiés sont des métaux amphotères dont le plomb(II), le chrome(III) et le zinc(II), avec des concentrations initiales variant de 0,1 à 10 g/l. Une tension électrique constante est appliquée au dispositif pendant un temps déterminé. L'analyse des teneurs de polluant sur différents endroits de la cuve à l'arrêt du traitement dans le sol montre que la répartition du polluant varie en fonction de la nature et de la concentration initiale du polluant utilisé. Ainsi, dans le cas du plomb, nous avons observé trois cas de figure : - une distribution plutôt homogène du plomb dans la cuve pour une concentration initiale de 0,1 g de Pb2+/1, consécutive à un faible déplacement du polluant, - un appauvrissement des zones anodique et cathodique, par rapport à la teneur initiale, avec accumulation du polluant au centre de la cuve pour 1 g de Pb2+/1, - un appauvrissement important des zones anodiques avec accumulation du polluant à la cathode pour 10 g de Pb2+/1. Les mesures de pH réalisées sur le sol et sur l'eau interstitielle à différents intervalles de temps ont mis en évidence deux mécanismes à l'origine du transport du plomb : un transport cationique à l'anode en présence de pH acides, suivi d'un transport anionique à la cathode pour des pH basiques. En effet, certains hydroxydes métalliques peuvent, sous des conditions de pH basiques, former des anions par réactions de dissolution. Cette propriété permet alors de « remobiliser » le plomb précipité à la cathode sous forme d'anions plombates et de concentrer le polluant dans les zones centrales du dispositif. L'action combinée de ces deux mécanismes de transport concentre la pollution, soit au centre de la cuve, soit à la cathode suivant la concentration initiale. Selon les cas, l'action d'un champ électrique permettrait de restreindre le volume de sol pollué à traiter ultérieurement ou à excaver. La mesure de la conductivité électrique de l'eau interstitielle met en évidence des variations de la concentration ionique dans le milieu liées au déplacement du polluant ou à sa précipitation. Les concentrations utilisées dans le cas du chrome et du zinc ont mis en évidence un transport sous une forme cationique. Aucun phénomène de « remobilisation » n'a pu être observé car les pH mesurés à la cathode ne favorisaient pas un transport important du polluant sous forme d'anions.

The current study therefore aims to provide a comprehensive characterisation of weathered dry disposed ash cores, to reveal mobility patterns of chemical species as a function of depth and age of ash, with a view to assessing the potential environmental impacts. Fifty-nine samples were taken from 3 drilled cores obtained respectively from the 1 year, 8 year and 20-year-old sections of sequentially dumped, weathered, dry disposed ash in an ash dump site at Tutuka - a South African coal burning power station.

<p>The management and disposal of huge volumes of coal combustion by products such as fly ash has constituted a major challenge to the environment. In most cases due to the inadequate alternative use of coal fly ash, the discarded waste is stored in holding ponds, slag heaps, or stock piled in ash dumps. This practice has raised concerns on the prospect of inorganic metals release to the surface and groundwater in the vicinity of the ash dump. Acceptable scientific studies are lacking to determine the best ash disposal practices. Moreover, knowledge about the mobility patterns of inorganic species as a function of mineralogical association or pH susceptibility of the dry disposed ash dump under natural weathering conditions are scarce in the literature. Fundamental understanding of chemical interactions of dry disposed ash with ingressed CO2 from atmosphere, percolating rain water and brine irrigation within ash disposal sites were seen as key areas requiring investigation. The mineralogical association of inorganic species in the dry disposed ash cores can be identified and quantified. This would provide a basis for understanding of chemical weathering, mineralogical transformations or mobility patterns of these inorganic species in the dry ash disposal scenario. The current study therefore aims to provide a comprehensive characterisation of weathered dry disposed ash cores, to reveal mobility patterns of chemical species as a function of depth and age of ash, with a view to assessing the potential environmental impacts. Fifty-nine samples were taken from 3 drilled cores obtained respectively from the 1 year, 8 year and 20-year-old sections of sequentially dumped,&nbsp / weathered, dry disposed ash in an ash dump site at Tutuka - a South African coal burning power station. The core samples were characterized using standard analytical procedures viz: X-ray fluorescence (XRF), X-ray diffraction (XRD), Fourier transforms infrared (FTIR) techniques, Scanning electron microscopy/energy dispersive spectroscopy (SEM/EDS) and Acid neutralisation capacity (ANC) test. A modified sequential extraction (SE) method was used in this study. The chemical partitioning, mobility and weathering patterns in 1 year, 8 year and 20-year-old sections of the ash dump were respectively investigated using this modified sequential extraction scheme. The sequence of the extractions was as follows: (1) water soluble, (2) exchangeable, (3) carbonate, (4) iron and manganese and (5) residual. The results obtained from the 5 steps sequential extraction scheme were validated with the total metal content of the original sample using mass balance method. The distribution of major and trace elements in the different liquid fractions obtained after each step of sequential extraction of the 59 drilled core samples was determined by inductively coupled plasma mass spectrometry (ICPMS). The data generated for various ash core samples were explored for the systematic analysis of mineralogical transformation and change in ash chemistry with ageing of the ash. Furthermore, the data was analyzed to reveal the impact of ingressed CO2 from atmosphere, infiltrating rain water and brine irrigation on the chemistry of ash core samples. Major mineral phases in original ash core samples prior to extraction are quartz (SiO2) and mullite (3Al2O3&middot / 2SiO2). Other minor mineral phases identified were hematite (Fe2O3), calcite (CaCO3), lime (CaO), anorthite (CaAl2Si2O8), mica (Ca (Mg, Al)3 (Al3Si) O10 (OH)2), and enstatite (Mg2Si2O6). X-ray diffraction results show significant loss of crystallinity in the older ash cores. The presence of minor phases of calcite and mica in dry disposed ash cores are attributed to reduction in the pore water pH due to hydration, carbonation and pozzolanic reactions. The X-ray diffraction technique was unable to detect Fe-oxyhydroxide phase and morealuminosilicate phases in ash core samples due to their low abundance and amorphous character. X-ray fluorescence results of the original ash core samples showed the presence of major oxides, such as SiO2, Al2O3, Fe2O3, while CaO, K2O, TiO2, Na2O, MnO, MgO, P2O5, and SO3 occur in minor concentrations. The ratio of SiO2/Al2O3 classified the original core samples prior to extraction as a silico-aluminate class F fly ash. The ternary plot of major elements in 1-year-old ash core samples was both sialic and ferrocalsialic but 8 year and 20-year-old ash core samples were sialic in chemical composition. It is noteworthy that the mass % of SiO2 varies through the depth of the core with an increase of nearly 3 %, to 58 mass % of SiO2 at a depth of 6 m in the 1-year-old core whereas in the case of the 8-year-old core a 2 % increase of SiO2 to a level of 57.5 mass % can be observed at levels between 4-8 m, showing dissolution of major components in the matrix of older ash cores.. The Na2O content of the Tutuka ash cores was low and varied between 0.6-1.1 mass % for 1-year-old ash cores to around 0.6-0.8 mass % for 8-year-old ash cores. Sodium levels were higher in 1-year-old ash cores compared to 8 year and 20-year-old ashcores. Observed trends indicate that quick weathering of the ash (within a year) leached out Na+ from the ash dump. No evidence of Na+ encapsulation even though the ash dump was brine irrigated. Thus the dry disposal ash placement method does not result in a sustainable salt sink for Na-containing species over time. The total content of each of the elements in 1 year and 20-year-old ash cores was normalised with their total content in fresh ash from same power station to show enrichment and depletion factor. Major elements such as K+, Mn showed enrichment in 1-year-old ash cores whereas Al, Si, Na+, Ti, Ca, Mg, S and Fe showed depletion due to over time erosion. Trace elements such as Cr, Sr, P, Ba, Pb, V and Zn showed enrichment but Ni, Y, Zr showed depletion attributed to over time erosion. In 20-year-old ash cores, major elements such as Al, Na+ and Mn showed enrichment while Si, K+, Fe, Mg and Ca showed depletion highlighting their mobility. Trends indicated intensive flushing of major soluble components such as buffering constituents (CaO) by percolating rain water. The 1-year-old and 20-year-old coal ash cores showed a lower pH and greater loss/depletion of the soluble buffering constituents than the 2-week-old placed ash, indicating significant chemical weathering within a year. Based&nbsp / on ANC results the leaching behaviours of Ca, Mg, Na+, K+, Se, Cr, and Sr were found to be controlled by the pH of the leachant indicating high mobility of major soluble species in the ash cores when in contact with slightly acid rain water. Other investigated toxic metals such as As, Mo and Pb showed amphoteric behaviour with respect to the pH of the leachant. Chemical alterations and formation of transient minor secondary mineral phases was found to have a significant effect on the acid susceptibility and depletion pattern of chemical species in the core ash samples when compared to fresh ash. These ANC results correlated well with the data generated from the sequential extraction scheme. Based on sequential extraction results elements, showed noticeable mobility in the water soluble, exchangeable and carbonate fractions due to adsorption and desorption caused by variations in the pore water pH. In contrast, slight mobility of elements in the Fe and Mn, and residual fractions of dry disposed fly ashes are attributed to the co-precipitation and dissolution of minor amount of less soluble secondary phase overtime. The 1-year-old dry disposed ash cores were the least weathered among the 3 drilled ash cores. Therefore low concentration of toxic metals in older ash cores were ascribed to extensive weathering with slower release from residual mineral phases over time. Elements were found to associate with different mineral phases depending on the age or depth of the core samples showing greater heterogeneity in dispersion. For instance the average amount of total calcium in different mineral associations of 1-year-old ash cores is as follows / water soluble (10.2 %), exchangeable (37.04 %), carbonate (37.9 %), Fe and Mn (7.1 %) and residual (2.97 %). The amount of total Na+ in different mineral phases of 1-year-old ash cores followed this trend: water soluble (21 %), exchangeable (11.26 %), carbonate (2.6 %), Fe and Mn (4.7 %) and residual (53.9 %). The non-leachable portion of the total Na+ content (namely that contained in the residual fraction) in the 1-year-old ash core samples under conditions found in nature ranged between 5-91 %. This non-leachable portion of the Na+ showed the metastability of the mineral phases with which residual Na+ associates. Results showed older ash cores are enriched in toxic elements. Toxic elements such as As, B, Cr, Mo and Pb are enriched in the residual fraction of older ash cores. For instance As concentration in the residual fraction varied between 0.0003- 0.00043 mg kg-1 for 1-year-old ash cores to around 0.0003-0.0015 mg kg-1 for 20-year-old ash cores. This suggests that the older ash is enriched in toxic elements hence dust from the ash dump would be toxic to human health. The knowledge of mobility and ecotoxicological significance of coal fly ash is needed when considering its disposal or reuse in the environment. The mobility and ecotoxicology of inorganic metals in coal fly ash are determined by (i) mineralogical associations of inorganic species (ii) in-homogeneity in the ash dumps (iii) long and short term exposure to ingress CO2 and percolating rain water. Management issues such as inconsistent placement of ash in the dumps, poor choice of ash dump site, in-homogeneity in brine irrigation, no record of salt load put on the ash dumps and lack of proper monitoring requires improvement. The thesis provides justification for the use of the modified sequential extraction scheme as a predictive tool and could be employed in a similar research work. This thesis also proved that the dry ash disposal method was not environmental friendly in terms of overall leaching potential after significant chemical weathering. Moreover the study proved that the practice of brine co-disposal or irrigation on ash dumps is not sustainable as the ash dump did not act as a salt sink.</p>

Dans un contexte où l’approvisionnement énergétique mondial du 21e siècle est un enjeu majeur, le développement de sources d’énergie renouvelables suscite l’attention croissante de la communauté scientifique et industrielle. L’énergie solaire est définitivement l’une des meilleures alternatives aux combustibles fossiles en tant que source d’énergie du monde de demain. Ce mémoire traite donc du développement de nouveaux matériaux organométalliques pour des applications de photorécoltage d’énergie en photovoltaïque et en production d’hydrogène. Le premier chapitre présente la synthèse assistée par microondes de quatre nouveaux complexes de Co(II), Ni(II), Cu(II) et Zn(II) basés sur le ligand tétra-p-méthoxyphényl-azadipyrrométhène (ADPM) avec des rendements variant de 89% à quantitatif. Ces complexes sont mis en relation avec d’autres complexes homoleptiques connus portant le tétraphényl-ADPM comme ligand ainsi qu’avec leurs chélates de BF2+ pour une meilleure compréhension des tendances engendrées par la substitution de l’agent coordonnant et/ou des substituants p-méthoxy. Pour ce faire, le comportement électrochimique et photophysique est présenté. De façon générale, la présence des quatre groupements p-méthoxy semble rendre les dérivés de cet ADPM plus susceptibles à la dégradation électrochimique en conditions d’oxydation et induire un déplacement bathochromique des propriétés optiques d’absorption et d’émission. Les structures rayons X du ligand tétra-p-méthoxyphényl-ADPM et de son complexe homoleptique de Co(II) sont aussi discutées. Cette étude a été effectuée dans l’espoir de fournir des informations utiles sur la stabilité des ADPM aux chercheurs du domaine photovoltaïque en quête de nouveaux chromophores dans le proche infrarouge (NIR). Le deuxième chapitre présente quant à lui les propriétés de senseur envers les anions F-, OAc- et H2PO4- de deux nouveaux complexes neutres de Re(I) de type mono- et dinucléaire basés sur une phénanthroline substituée en position 5 contenant un récepteur thio-urée. Ces composés ont été obtenus dans des rendements de 81% et 60%, respectivement. L’effet de la formation de ponts hydrogène lors de l’ajout d’anions versus la déprotonation du récepteur a été évalué par des titrations UV/Vis et RMN 1H et semble indiquer que la formation de la base conjuguée du récepteur est favorisée pour ce type de système. De plus, la structure rayons X d’un des précurseurs est présentée et permet une discussion sur la chiralité des complexes mono- et dinucléaire obtenus. L’obtention d’un complexe bimétallique par autoassemblage ouvre la voie à la préparation d’antennes moléculaires pour des systèmes de photosynthèse artificielle. / The world's energy supply is rapidly becoming the major issue of the 21st century. Instead of the status quo approach of finding and extracting more hydrocarbons from the ground, the development of renewable energy sources is attracting much interest from both the scientific and industrial communities. Solar energy is definitively one of the best sources to power the World of tomorrow. In such a framework, this dissertation discusses the development of new organometallic materials able to harvest solar energy for photovoltaic or H2 photoproduction applications. The first chapter presents the synthesis by a microwaves-assisted methodology of four new homoleptic complexes of Co(II), Ni(II), Cu(II) and Zn(II) based on the tetra-p-methoxyphenyl-azadipyrromethene (ADPM) ligand in yields ranging from 89% to quantitative. Those complexes are put in relation with already known ADPM homoleptic complexes of the same M(II) series and related BF2+ chelates (Aza-BODIPY) for a better understanding of trends arising from substitution of the chelate and/or electron-donating effect of the p-methoxy substituents. This is achieved by the study of electrochemical behavior of the compounds and their photophysical properties. From a general point of view, the presence of the four p-methoxy substituents leads to an electrochemical decomposition of the derivatives based on that ADPM in oxidative conditions, along with a bathochromic shift of the optical properties. X-Ray structures for the tetra-p-methoxyphenyl-ADPM ligand and related Co(II) complex are also discussed. Hopefully, this study will provide useful insights to researchers on the substituents to install for stable ADPM derivatives in their quest for NIR chromophores utilizable for photovoltaic application. The second chapter report anion sensing properties toward F-, OAc- and H2PO4- of new neutral mononuclear and dinuclear Re(I) complexes based on a 5-substituted phenanthroline moiety bearing a thiourea hydrogen-bonding receptor. Those complexes were obtained in 81% and 60% yields, respectively. The effect of hydrogen-bonding versus deprotonation of the thiourea receptor upon addition of the anions was also evaluated by UV/vis and 1H NMR titration techniques. Observations made support the hypothesis that formation of the conjugated base of the receptor is favored. In addition, an X-ray structure of the Re(I) precursor complex is reported and the chirality of the mononuclear and dinuclear complexes is discussed. Achievement of a bimetallic complex by self-assembly paves the way for the preparation of light-harvesting molecular antennae utilizable in artificial photosynthesis systems.

<p>The management and disposal of huge volumes of coal combustion by products such as fly ash has constituted a major challenge to the environment. In most cases due to the inadequate alternative use of coal fly ash, the discarded waste is stored in holding ponds, slag heaps, or stock piled in ash dumps. This practice has raised concerns on the prospect of inorganic metals release to the surface and groundwater in the vicinity of the ash dump. Acceptable scientific studies are lacking to determine the best ash disposal practices. Moreover, knowledge about the mobility patterns of inorganic species as a function of mineralogical association or pH susceptibility of the dry disposed ash dump under natural weathering conditions are scarce in the literature. Fundamental understanding of chemical interactions of dry disposed ash with ingressed CO2 from atmosphere, percolating rain water and brine irrigation within ash disposal sites were seen as key areas requiring investigation. The mineralogical association of inorganic species in the dry disposed ash cores can be identified and quantified. This would provide a basis for understanding of chemical weathering, mineralogical transformations or mobility patterns of these inorganic species in the dry ash disposal scenario. The current study therefore aims to provide a comprehensive characterisation of weathered dry disposed ash cores, to reveal mobility patterns of chemical species as a function of depth and age of ash, with a view to assessing the potential environmental impacts. Fifty-nine samples were taken from 3 drilled cores obtained respectively from the 1 year, 8 year and 20-year-old sections of sequentially dumped,&nbsp / weathered, dry disposed ash in an ash dump site at Tutuka - a South African coal burning power station. The core samples were characterized using standard analytical procedures viz: X-ray fluorescence (XRF), X-ray diffraction (XRD), Fourier transforms infrared (FTIR) techniques, Scanning electron microscopy/energy dispersive spectroscopy (SEM/EDS) and Acid neutralisation capacity (ANC) test. A modified sequential extraction (SE) method was used in this study. The chemical partitioning, mobility and weathering patterns in 1 year, 8 year and 20-year-old sections of the ash dump were respectively investigated using this modified sequential extraction scheme. The sequence of the extractions was as follows: (1) water soluble, (2) exchangeable, (3) carbonate, (4) iron and manganese and (5) residual. The results obtained from the 5 steps sequential extraction scheme were validated with the total metal content of the original sample using mass balance method. The distribution of major and trace elements in the different liquid fractions obtained after each step of sequential extraction of the 59 drilled core samples was determined by inductively coupled plasma mass spectrometry (ICPMS). The data generated for various ash core samples were explored for the systematic analysis of mineralogical transformation and change in ash chemistry with ageing of the ash. Furthermore, the data was analyzed to reveal the impact of ingressed CO2 from atmosphere, infiltrating rain water and brine irrigation on the chemistry of ash core samples. Major mineral phases in original ash core samples prior to extraction are quartz (SiO2) and mullite (3Al2O3&middot / 2SiO2). Other minor mineral phases identified were hematite (Fe2O3), calcite (CaCO3), lime (CaO), anorthite (CaAl2Si2O8), mica (Ca (Mg, Al)3 (Al3Si) O10 (OH)2), and enstatite (Mg2Si2O6). X-ray diffraction results show significant loss of crystallinity in the older ash cores. The presence of minor phases of calcite and mica in dry disposed ash cores are attributed to reduction in the pore water pH due to hydration, carbonation and pozzolanic reactions. The X-ray diffraction technique was unable to detect Fe-oxyhydroxide phase and morealuminosilicate phases in ash core samples due to their low abundance and amorphous character. X-ray fluorescence results of the original ash core samples showed the presence of major oxides, such as SiO2, Al2O3, Fe2O3, while CaO, K2O, TiO2, Na2O, MnO, MgO, P2O5, and SO3 occur in minor concentrations. The ratio of SiO2/Al2O3 classified the original core samples prior to extraction as a silico-aluminate class F fly ash. The ternary plot of major elements in 1-year-old ash core samples was both sialic and ferrocalsialic but 8 year and 20-year-old ash core samples were sialic in chemical composition. It is noteworthy that the mass % of SiO2 varies through the depth of the core with an increase of nearly 3 %, to 58 mass % of SiO2 at a depth of 6 m in the 1-year-old core whereas in the case of the 8-year-old core a 2 % increase of SiO2 to a level of 57.5 mass % can be observed at levels between 4-8 m, showing dissolution of major components in the matrix of older ash cores.. The Na2O content of the Tutuka ash cores was low and varied between 0.6-1.1 mass % for 1-year-old ash cores to around 0.6-0.8 mass % for 8-year-old ash cores. Sodium levels were higher in 1-year-old ash cores compared to 8 year and 20-year-old ashcores. Observed trends indicate that quick weathering of the ash (within a year) leached out Na+ from the ash dump. No evidence of Na+ encapsulation even though the ash dump was brine irrigated. Thus the dry disposal ash placement method does not result in a sustainable salt sink for Na-containing species over time. The total content of each of the elements in 1 year and 20-year-old ash cores was normalised with their total content in fresh ash from same power station to show enrichment and depletion factor. Major elements such as K+, Mn showed enrichment in 1-year-old ash cores whereas Al, Si, Na+, Ti, Ca, Mg, S and Fe showed depletion due to over time erosion. Trace elements such as Cr, Sr, P, Ba, Pb, V and Zn showed enrichment but Ni, Y, Zr showed depletion attributed to over time erosion. In 20-year-old ash cores, major elements such as Al, Na+ and Mn showed enrichment while Si, K+, Fe, Mg and Ca showed depletion highlighting their mobility. Trends indicated intensive flushing of major soluble components such as buffering constituents (CaO) by percolating rain water. The 1-year-old and 20-year-old coal ash cores showed a lower pH and greater loss/depletion of the soluble buffering constituents than the 2-week-old placed ash, indicating significant chemical weathering within a year. Based&nbsp / on ANC results the leaching behaviours of Ca, Mg, Na+, K+, Se, Cr, and Sr were found to be controlled by the pH of the leachant indicating high mobility of major soluble species in the ash cores when in contact with slightly acid rain water. Other investigated toxic metals such as As, Mo and Pb showed amphoteric behaviour with respect to the pH of the leachant. Chemical alterations and formation of transient minor secondary mineral phases was found to have a significant effect on the acid susceptibility and depletion pattern of chemical species in the core ash samples when compared to fresh ash. These ANC results correlated well with the data generated from the sequential extraction scheme. Based on sequential extraction results elements, showed noticeable mobility in the water soluble, exchangeable and carbonate fractions due to adsorption and desorption caused by variations in the pore water pH. In contrast, slight mobility of elements in the Fe and Mn, and residual fractions of dry disposed fly ashes are attributed to the co-precipitation and dissolution of minor amount of less soluble secondary phase overtime. The 1-year-old dry disposed ash cores were the least weathered among the 3 drilled ash cores. Therefore low concentration of toxic metals in older ash cores were ascribed to extensive weathering with slower release from residual mineral phases over time. Elements were found to associate with different mineral phases depending on the age or depth of the core samples showing greater heterogeneity in dispersion. For instance the average amount of total calcium in different mineral associations of 1-year-old ash cores is as follows / water soluble (10.2 %), exchangeable (37.04 %), carbonate (37.9 %), Fe and Mn (7.1 %) and residual (2.97 %). The amount of total Na+ in different mineral phases of 1-year-old ash cores followed this trend: water soluble (21 %), exchangeable (11.26 %), carbonate (2.6 %), Fe and Mn (4.7 %) and residual (53.9 %). The non-leachable portion of the total Na+ content (namely that contained in the residual fraction) in the 1-year-old ash core samples under conditions found in nature ranged between 5-91 %. This non-leachable portion of the Na+ showed the metastability of the mineral phases with which residual Na+ associates. Results showed older ash cores are enriched in toxic elements. Toxic elements such as As, B, Cr, Mo and Pb are enriched in the residual fraction of older ash cores. For instance As concentration in the residual fraction varied between 0.0003- 0.00043 mg kg-1 for 1-year-old ash cores to around 0.0003-0.0015 mg kg-1 for 20-year-old ash cores. This suggests that the older ash is enriched in toxic elements hence dust from the ash dump would be toxic to human health. The knowledge of mobility and ecotoxicological significance of coal fly ash is needed when considering its disposal or reuse in the environment. The mobility and ecotoxicology of inorganic metals in coal fly ash are determined by (i) mineralogical associations of inorganic species (ii) in-homogeneity in the ash dumps (iii) long and short term exposure to ingress CO2 and percolating rain water. Management issues such as inconsistent placement of ash in the dumps, poor choice of ash dump site, in-homogeneity in brine irrigation, no record of salt load put on the ash dumps and lack of proper monitoring requires improvement. The thesis provides justification for the use of the modified sequential extraction scheme as a predictive tool and could be employed in a similar research work. This thesis also proved that the dry ash disposal method was not environmental friendly in terms of overall leaching potential after significant chemical weathering. Moreover the study proved that the practice of brine co-disposal or irrigation on ash dumps is not sustainable as the ash dump did not act as a salt sink.</p>

The current study therefore aims to provide a comprehensive characterisation of weathered dry disposed ash cores, to reveal mobility patterns of chemical species as a function of depth and age of ash, with a view to assessing the potential environmental impacts. Fifty-nine samples were taken from 3 drilled cores obtained respectively from the 1 year, 8 year and 20-year-old sections of sequentially dumped, weathered, dry disposed ash in an ash dump site at Tutuka - a South African coal burning power station.

Die vorliegende Arbeit beschäftigt sich mit der Herstellung von funktionellen Magnetit-Nanokompositen durch Sprühtrocknung für die Anwendung in der Bioseparation. Dabei liegen die Schwerpunkte auf der Anwendung von Polyelektrolyten als Ionenaustauscher sowie auf der Nachhaltigkeit des Herstellungsprozesses. Basierend auf einem existierenden Herstellungsprozess wurde die Aufgabenstellung konkretisiert. Es wurden Möglichkeiten zur nachhaltigen Prozessgestaltung der Synthese von kationischen bzw. anionischen magnetischen Funktionspartikeln zur Proteinabtrennung vorgestellt. Als magnetische Komponente wurde Magnetit verwendet. Aufgrund seines pseudo-amphiphilen Charakters und seiner besonderen Eigenschaften in Bezug auf die Stabilisierung von Magnetit-Kolloiden wurde Polyvinylbutyral (Mowital B 30T) als Matrixpolymer bei der Sprühtrocknung benutzt. Für die nachhaltige Prozessgestaltung wurden Isopropanol und Tetrahydrofuran als Dichlormethan-Ersatz bei der Sprühtrocknung verwendet. Bei der Synthese kationischer Magnetic Beads wurden verzweigtes Polyethylenimin und lineares Poly(Allyamin) als Anionenaustauscher verwendet. Beide Polykationen sind schwache Polyelektrolyte mit Aminogruppen. Für die Verarbeitung der Polykationen als funktionelle Liganden in magnetischen Funktionspartikeln wurde zwei Herstellungsmethoden vorgestellt: eine Synthese ohne Oberflächenmodifizierung, wobei die mechanische und chemische Stabilität der Funktionspartikeln einzig von der chemischen Struktur der eingesetzten Materialien bzw. vom Matrixpolymer abhängt, und eine Synthese mit Oberflächenmodifizierung. Die Synthese mit Oberflächenmodifizierung ist gekennzeichnet durch die kovalente Bindung von Polyethylenimin bzw. Poly(Allyamin) an der Oberfläche der Funktionspartikeln (Polyvinylbutyral). Dafür wurde 1,1’-Carbonyldiimidazol als „zero length“-Crosslinker benutzt. Die nach beiden Methoden hergestellten Funktionspartikeln wurden charakterisiert, um ihre technische Eignung beurteilen zu können. Für die Charakterisierung der sorptiven Eigenschaften wurde unter anderem der Bowman-Birk Inhibitor (BBI) verwendet. Das Protein ist ein Sojaprodukt und für seine krebsvorbeugende Wirkung bekannt. Um die Selektivität der Abtrennung zu untersuchen, wurden BBI-Produkte mit unterschiedlichen Reinheitsgraden benutzt. Durch die zwei vorgestellten Methoden konnten kationische magnetische Funktionspartikeln erfolgreich hergestellt werden. Alle Funktionspartikeln sind superparamagnetisch, und der Medianwert ihrer Partikelgrößenverteilung liegt im einstelligen Mikrometerbereich. Aufgrund eines höheren Polykationanteils ist die Bindungskapazität der Funktionspartikeln ohne Oberflächenmodifizierung um den Faktor 2,4 größer als die BBI-Bindungskapazität der Funktionspartikeln mit Oberflächenmodifizierung (Qmax=322 mg/g). Das Fehlen eine feste Anbindung des funktionellen Liganden an den Funktionspartikeln ohne Oberflächenmodifizierung verleiht jedoch diesen eine sehr schlechte chemische Stabilität in Lösungen. Es wurde auch gezeigt, dass oberflächenmodifizierte Funktionspartikeln mit ähnlichen Eigenschaften durch den Einsatz von Dichlormethan bzw. Tetrahydrofuran als Lösungsmittelersatz während der Sprühtrocknung hergestellt werden können. Durch den Einsatz von mit Poly(allylamin) oberflächenmodifizierten Funktionspartikeln konnte BBI von technischen Sojamolken unterschiedlicher Reinheitsgrade erfolgreich abgetrennt werden. Anionische Magnetic Beads wurden mit Kationenaustauscherharz als funktionellem Ligand hergestellt. Dabei wurde Isopropanol als organisches Lösungsmittel während der Sprühtrocknung verwendet. Die Synthese wurde analog zur Synthese der kationischen Magnetic Beads ohne Oberflächenmodifizierung durchgeführt. Es wurde auch hier gezeigt, dass anionische magnetische Funktionspartikeln mit guten sorptiven Eigenschaften durch den Einsatz von Isopropanol als organisches Lösungsmittel hergestellt werden können. Die anionischen Funktionspartikeln besitzen im Vergleich zu Literaturwerten höhere Bindungskapazitäten (bis 280 mg/g; ermittelt mit Lysozym). Im letzten Kapitel wird der kritische Prozessschritt des Lösungsmittelaustausches behandelt. Nach dem Lösungsmittelaustausch sollten die Magnetitnanopartikeln in der organischen Phase stabil sein. Dies ermöglicht sowohl eine homogene Verteilung der Nanopartikeln in der Matrix als auch deren bessere Verkapselung während der Sprühtrocknung. Es wurde festgestellt, dass sich eine vollständige Abtrennung von Dichlormethan durch die angewendete Destillationsmethode nicht erreichen lässt. Anhand von zwei Modellsystemen — Rizinolsäure- und Ölsäure-beschichteten Magnetitnanopartikeln — und Lösungsmittelgemischen wurde die Stabilität von sterisch stabilisierten Magnetitpartikeln in binären Lösungsmittelgemischen untersucht. Der Fokus bei dieser Untersuchung lag auf der Untersuchung der Stabilität der beschichteten Magnetitnanopartikeln in einer möglichst Dichlormethan- bzw. Isooktan-freien organischen Phase. Als zweites Lösungsmittel (als Lösungsmittelersatz betrachtet) wurden neben Tetrahydrofuran und Isopropanol technisch verbreitete Lösungsmittel wie Isooktan und 1-Butanol eingesetzt. Die Untersuchungsergebnisse zeigen, dass die Anwendung der technischen Rizinolsäure bzw. Ölsäure einen zusätzlichen Einfluss auf die Stabilität der Magnetitpartikeln hat, da diese aus anderen Fettsäuren mit unterschiedlichen chemischen Strukturen bestehen. Die Diskrepanz zwischen der berechneten HANSEN-Distanzen und der Stabilität der Magnetitnanopartikeln mit reinen Fettsäuren lässt vermutet, dass die Zusammensetzung der Lösungsmittelgemische an der fest/flüssig-Grenzfläche anders ist als im freien Volumen. Ein Modell zur Beschreibung der Stabilität der Nanopartikeln, das auf einer Anreicherung des Ausgangslösungsmittels an der Grenzfläche basiert, wurde postuliert. Solange die Diffusion des zweiten Lösungsmittels in die Adsorptionsschicht nicht ausreichend genug ist, um die Löslichkeit der Fettsäureketten entscheidend zu reduzieren und somit einen Abfall der Abstoßungskräfte zwischen der Partikeln hervorzurufen, bleiben alle beschichteten Magnetitnanopartikeln stabil im Lösungsmittelgemisch. Dies ist der Fall für die mit der reinen Rizinolsäure beschichteten Magnetitnanopartikeln in allen verwendeten Lösungsmittelgemischen mit 0,5 Vol. % DCM in der kontinuierlichen Phase. Durch die vorgestellten Herstellungsmethoden wurde gezeigt, dass magnetische Funktionspartikeln sowohl mit festen partikelförmigen Ionenaustauschern als auch mit flüssigen schwachen Polyelektrolyten erfolgreich synthetisiert werden können. Eine nachhaltige Prozessgestaltung durch die Reduzierung der Dichlormethanmenge im Sprühtrocknungsprozess ist auch möglich. Für eine erfolgreiche industrielle Anwendung der Funktionspartikeln müssen aber ihre chemischen sowie mechanischen Eigenschaften deutlich verbessert werden. Dies könnte z.B. durch die Verwendung eines anderen Matrixpolymers oder durch die Entfernung von nicht gebundenen Bestandteilen durch gezielte Waschung der Funktionspartikeln erfolgen. Die Bindungskapazität sowie die Selektivität der oberflächenmodifizierten Funktionspartikeln sollte ebenfalls verbessert werden. Dafür wurde einen Ansatz durch die Quaternisierung der Aminogruppen präsentiert. Schließlich würde die Untersuchung der Stabilität der beschichteten Magnetitnanopartikeln in einphasigen reinen Lösungsmitteln nähere Erkenntnisse über das postulierte Modell der Anreicherung von Dichlormethan in der Adsorptionsschicht erbringen. Dabei könnte die Dichlormethanmenge durch mehrstufige Destillation bzw. Rektifikation beim Lösungsmittelaustausch entfernt werden. Eine vollständige Untersuchung dieses Effekts würde zusätzlich eine Antwort auf zahlreiche Fragestellungen der Kolloidchemie in Bezug auf das Stabilitätsverhalten von Pigmentdispersionen (Lacke) oder von beschichteten Nanopartikeln in Polymerlösungen erbringen.

L’any 2002 tres grups de recerca, entre ells el nostre grup, van demostrar teòricament que la interacció entre anions i anells aromàtics electrodeficients, anomenada interacció anió–, era favorable. Des de llavors s’ha dut a terme un intens estudi de la seva naturalesa física fins la total comprensió. Aquesta tesi es basa amb l’estudi de la interacció anió– des de tres punts de vista. Primerament, la investigació es basa en el disseny teòric de motius estructurals per donar lloc a un receptor on la interacció anió– siga molt favorable, per posteriorment avaluar la força de la interacció experimentalment en dissolució. A continuació, es va analitzar la interrelació entre un gran nombre de combinacions d’interaccions no covalents. A partir d’aquest estudi es defineixen nous conceptes i es proposen diferents formules per calcular efectes de cooperativitat. Finalment, hem anat un pas més enllà en l’estudi de la interacció analitzant: 1) l’impacte de la interacció anió– a sistemes biològics; 2) la influència de modificacions a l’anió sobre la naturalesa física de la interacció. / In 2002 three research groups, among them our research group, theoretically demonstrated that the interaction between anions and electron-deficient aromatic rings, named anion– interaction, was favourable. Since then, an intense study of its physical nature has been performed to understand it completely. This thesis is based on the study of the anion– interaction from three points of view. Firstly, theoretical design of binding units to build a receptor and to obtain the most favourable binding based on anion– interactions. The binding properties of these receptors have been experimentally assessed in solution. Secondly, we have studied the interplay between a great combination of noncovalent interactions. From this study, new concepts and formula to calculate cooperativity effects have been described. Finally, we have study one step further the anion– interaction analysing: 1) the impact of anion– interaction in biological systems; 2) how the modifications in the anion influence the physical nature of the interaction.

La conception et la préparation de réseaux moléculaires organiques et hybrides à l’état cristallin ont été envisagées par un processus itératif d’auto-assemblage entre des briques de construction moléculaires préprogrammées et complémentaires appelées tectons. Cette approche est basée sur la reconnaissance moléculaire de modules dicationiques, donneurs de liaisons hydrogène, et d’unités anioniques, accepteurs de liaisons hydrogène. Ainsi, la combinaison des tectons moléculaires de la famille des bis-benzimidazoliums, intrinsèquement luminescents, avec des anions polycyanométallates conduit à la formation de réseaux moléculaires hybrides luminescents à l’état cristallin. Il a été procédé à l'étude des propriétés photophysiques de ces réseaux à l'état solide. De même, l’association de bis-amidiniums,briques dicationiques, à des anions de type azodibenzoates mène à des assemblages cristallins possédant la propriété de photo-commutation, c’est-à-dire conduisant à une isomérisation sous stimulus lumineux. / The design and synthesis of organic and hybrid molecular networks in the crystalline state has been investigated using iterative self-assembly processes involving preprogrammed complementary molecular building blocks called tectons. This approach is based on molecular recognition events between dicationic hydrogen bond donors and anionic hydrogen bond acceptors tectons. Thus, the combination of intrinsically luminescent molecular tectons belonging to the family of cationic bis-benzimidazoliums with polycyanometallates anions leads to the formation of luminescent hybrid molecular networks in the crystalline state. Their optical properties have been studied in the solid state. Similarly, the association of bis-amidiniums, dicationic bricks, to azodibenzoates type anions leads to crystalline assemblies presenting photo-switching property, i.e. the ability to isomerise under light stimulus.

Philosophiae Doctor - PhD / The management and disposal of huge volumes of coal combustion by products such as fly ash has constituted a major challenge to the environment. In most cases due to the inadequate alternative use of coal fly ash, the discarded waste is stored in holding ponds, slag heaps, or stock piled in ash dumps. This practice has raised concerns on the prospect of inorganic metals release to the surface and groundwater in the vicinity of the ash dump. Acceptable scientific studies are lacking to determine the best ash disposal practices. Moreover, knowledge about the mobility patterns of inorganic species as a function of mineralogical association or pH susceptibility of the dry disposed ash dump under natural weathering conditions are scarce in the literature. Fundamental understanding of chemical interactions of dry disposed ash with ingressed CO2 from atmosphere, percolating rain water and brine irrigation within ash disposal sites were seen as key areas requiring investigation. The mineralogical association of inorganic species in the dry disposed ash cores can be identified and quantified. This would provide a basis for understanding of chemical weathering, mineralogical transformations or mobility patterns of these inorganic species in the dry ash disposal scenario. The current study therefore aims to provide a comprehensive characterisation of weathered dry disposed ash cores, to reveal mobility patterns of chemical species as a function of depth and age of ash, with a view to assessing the potential environmental impacts. Fifty-nine samples were taken from 3 drilled cores obtained respectively from the 1 year, 8 year and 20-year-old sections of sequentially dumped, weathered, dry disposed ash in an ash dump site at Tutuka - a South African coal burning power station. The core samples were characterized using standard analytical procedures viz: X-ray fluorescence (XRF), X-ray diffraction (XRD), Fourier transforms infrared (FTIR) techniques, Scanning electron microscopy/energy dispersive spectroscopy (SEM/EDS) and Acid neutralisation capacity (ANC) test. A modified sequential extraction (SE) method was used in this study. The chemical partitioning, mobility and weathering patterns in 1 year, 8 year and 20-year-old sections of the ash dump were respectively investigated using this modified sequential extraction scheme. The sequence of the extractions was as follows: (1) water soluble, (2) exchangeable, (3) carbonate, (4) iron and manganese and (5) residual. The results obtained from the 5 steps sequential extraction scheme were validated with the total metal content of the original sample using mass balance method. The distribution of major and trace elements in the different liquid fractions obtained after each step of sequential extraction of the 59 drilled core samples was determined by inductively coupled plasma mass spectrometry (ICPMS). The data generated for various ash core samples were explored for the systematic analysis of mineralogical transformation and change in ash chemistry with ageing of the ash. Furthermore, the data was analyzed to reveal the impact of ingressed CO2 from atmosphere, infiltrating rain water and brine irrigation on the chemistry of ash core samples. Major mineral phases in original ash core samples prior to extraction are quartz (SiO2) and mullite (Al2O3·2SiO2). Other minor mineral phases identified were hematite (Fe2O3), calcite (CaCO3), lime (CaO), anorthite (CaAl2Si2O8), mica (Ca (Mg, Al)3 (Al3Si) O10 (OH)2), and enstatite (Mg2Si2O6). X-ray diffraction results show significant loss of crystallinity in the older ash cores. The presence of minor phases of calcite and mica in dry disposed ash cores are attributed to reduction in the pore water pH due to hydration, carbonation and pozzolanic reactions. The X-ray diffraction technique was unable to detect Fe-oxyhydroxide phase and morealuminosilicate phases in ash core samples due to their low abundance and amorphous character. X-ray fluorescence results of the original ash core samples showed the presence of major oxides, such as SiO2, Al2O3, Fe2O3, while CaO, K2O, TiO2, Na2O, MnO, MgO, P2O5, and SO3 occur in minor concentrations. The ratio of SiO2/Al2O3 classified the original core samples prior to extraction as a silico-aluminate class F fly ash. The ternary plot of major elements in 1-year-old ash core samples was both sialic and ferrocalsialic but 8 year and 20-year-old ash core samples were sialic in chemical composition. It is noteworthy that the mass % of SiO2 varies through the depth of the core with an increase of nearly 3 %, to 58 mass % of SiO2 at a depth of 6 m in the 1-year-old core whereas in the case of the 8-year-old core a 2 % increase of SiO2 to a level of 57.5 mass % can be observed at levels between 4-8 m, showing dissolution of major components in the matrix of older ash cores.. The Na2O content of the Tutuka ash cores was low and varied between 0.6-1.1 mass % for 1-year-old ash cores to around 0.6-0.8 mass % for 8-year-old ash cores. Sodium levels were higher in 1-year-old ash cores compared to 8 year and 20-year-old ashcores. Observed trends indicate that quick weathering of the ash (within a year) leached out Na+ from the ash dump. No evidence of Na+ encapsulation even though the ash dump was brine irrigated. Thus the dry disposal ash placement method does not result in a sustainable salt sink for Na-containing species over time. The total content of each of the elements in 1 year and 20-year-old ash cores was normalised with their total content in fresh ash from same power station to show enrichment and depletion factor. Major elements such as K+, Mn showed enrichment in 1-year-old ash cores whereas Al, Si, Na+, Ti, Ca, Mg, S and Fe showed depletion due to over time erosion. Trace elements such as Cr, Sr, P, Ba, Pb, V and Zn showed enrichment but Ni, Y, Zr showed depletion attributed to over time erosion. In 20-year-old ash cores, major elements such as Al, Na+ and Mn showed enrichment while Si, K+, Fe, Mg and Ca showed depletion highlighting their mobility. Trends indicated intensive flushing of major soluble components such as buffering constituents (CaO) by percolating rain water. The 1-year-old and 20-year-old coal ash cores showed a lower pH and greater loss/depletion of the soluble buffering constituents than the 2-week-old placed ash, indicating significant chemical weathering within a year. Based on ANC results the leaching behaviours of Ca, Mg, Na+, K+, Se, Cr, and Sr were found to be controlled by the pH of the leachant indicating high mobility of major soluble species in the ash cores when in contact with slightly acid rain water. Other investigated toxic metals such as As, Mo and Pb showed amphoteric behaviour with respect to the pH of the leachant. Chemical alterations and formation of transient minor secondary mineral phases was found to have a significant effect on the acid susceptibility and depletion pattern of chemical species in the core ash samples when compared to fresh ash. These ANC results correlated well with the data generated from the sequential extraction scheme. Based on sequential extraction results elements, showed noticeable mobility in the water soluble, exchangeable and carbonate fractions due to adsorption and desorption caused by variations in the pore water pH. In contrast, slight mobility of elements in the Fe and Mn, and residual fractions of dry disposed fly ashes are attributed to the co-precipitation and dissolution of minor amount of less soluble secondary phase overtime. The 1-year-old dry disposed ash cores were the least weathered among the 3 drilled ash cores. Therefore low concentration of toxic metals in older ash cores were ascribed to extensive weathering with slower release from residual mineral phases over time. Elements were found to associate with different mineral phases depending on the age or depth of the core samples showing greater heterogeneity in dispersion. For instance the average amount of total calcium in different mineral associations of 1-year-old ash cores is as follows; water soluble (10.2 %), exchangeable (37.04 %), carbonate (37.9 %), Fe and Mn (7.1 %) and residual (2.97 %). The amount of total Na+ in different mineral phases of 1-year-old ash cores followed this trend: water soluble (21 %), exchangeable (11.26 %), carbonate (2.6 %), Fe and Mn (4.7 %) and residual (53.9 %). The non-leachable portion of the total Na+ content (namely that contained in the residual fraction) in the 1-year-old ash core samples under conditions found in nature ranged between 5-91 %. This non-leachable portion of the Na+ showed the metastability of the mineral phases with which residual Na+ associates. Results showed older ash cores are enriched in toxic elements. Toxic elements such as As, B, Cr, Mo and Pb are enriched in the residual fraction of older ash cores. For instance As concentration in the residual fraction varied between 0.0003- 0.00043 mg kg-1 for 1-year-old ash cores to around 0.0003-0.0015 mg kg-1 for 20-year-old ash cores. This suggests that the older ash is enriched in toxic elements hence dust from the ash dump would be toxic to human health. The knowledge of mobility and ecotoxicological significance of coal fly ash is needed when considering its disposal or reuse in the environment. The mobility and ecotoxicology of inorganic metals in coal fly ash are determined by (i) mineralogical associations of inorganic species (ii) in-homogeneity in the ash dumps (iii) long and short term exposure to ingress CO2 and percolating rain water. Management issues such as inconsistent placement of ash in the dumps, poor choice of ash dump site, in-homogeneity in brine irrigation, no record of salt load put on the ash dumps and lack of proper monitoring requires improvement. The thesis provides justification for the use of the modified sequential extraction scheme as a predictive tool and could be employed in a similar research work. This thesis also proved that the dry ash disposal method was not environmental friendly in terms of overall leaching potential after significant chemical weathering. Moreover the study proved that the practice of brine co-disposal or irrigation on ash dumps is not sustainable as the ash dump did not act as a salt sink. / South Africa