Ce manuscrit présente la synthèse et la caractérisation de deux nouvelles familles de complexes mononucléaires, [Fe(L)2(NCS)2] et [Fe(L)(H2B(pz)2)2], montrant des propriétés bistables. L’étude des structures cristallographiques a permis de discuter l’influence de l’élongation des ligands L sur le réseau cristallin et sur les contacts intermoléculaires ainsi que l’existence de corrélations structures / propriétés. Enfin, la dernière partie de ce travail est consacrée à l’élaboration de façon contrôlée d’objets à transition de spin à l’échelle nanométrique, sous la forme de films déposés par sublimation et de nanoclusters synthétisés en milieu confiné. / This thesis presents the synthesis and characterization of two new families of mononuclear complexes, [Fe(L)2(NCS)2] and [Fe(L)(H2B(pz)2)2] showing bistable properties. The crystallographic studies allowed us to discuss the influence of the elongation of the ligands L on the crystal lattice, intermolecular contacts and the existence of structure / properties correlations. The final part of this work shows the controlled synthesis of spin crossover objects at the nanometric scale as thin films prepared by sublimation and nanoclusters synthesized in confined media.

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Cette étude a porté sur différents hydroxysels ferreux, formés en milieu carbonaté ou sulfaté. Ces composés sont connus pour le rôle important qu’ils jouent lors des processus de corrosion à long terme des aciers en milieux naturels (sols, milieu marin). La chukanovite, hydroxycarbonate ferreux de composition Fe2(OH)2CO3, a été particulièrement étudiée. Son enthalpie libre standard de formation a ainsi pu être déterminée à partir d’une étude détaillée des conditions d’équilibre avec l’hydroxyde de Fe(II), réalisée sur des suspensions aqueuses vieillies jusqu’à 6 mois. Cette détermination a permis de tracer des diagrammes d’équilibre potentiel-pH du fer incluant la chukanovite et mettant en évidence son domaine de stabilité thermodynamique. Par comparaison avec des diagrammes similaires incluant la sidérite FeCO3, il a été possible de montrer que la chukanovite était métastable (à 25°C) par rapport à la sidérite. Nous avons également étudié les mécanismes de transformation de la chukanovite pour différentes conditions d’oxydation, en utilisant notamment le peroxyde d’hydrogène pour accélérer la cinétique de la réaction. Les résultats obtenus montrent, qu’à 25°C, la chukanovite se transforme en lépidocrocite et/ou goethite sans passer par un composé intermédiaire Fe(II,III) de type rouille verte. La goethite est favorisée par une augmentation du pH (excès de carbonate par exemple). Une oxydation violente par le peroxyde d’hydrogène conduit à la formation d’un oxycarbonate de Fe(III), structurellement très proche de la chukanovite. Enfin, deux hydroxysulfates ferreux ont été mis en évidence et caractérisés par diffraction des rayons X et spectroscopie Infrarouge. Ces composés n’ont cependant pas pu être obtenus seuls, mais toujours ensembles, et/ou avec Fe(OH)2, voire un 3ème hydroxysulfate ferreux. Une étude des processus d’oxydation a permis de révéler que tous ces composés se transformaient dans un premier temps en rouille verte sulfatée. / This study deals with various ferrous hydroxysalts formed in carbonated or sulphated environments. These compounds are known to play an important role during the long term corrosion processes of carbon steel in natural media (soils, seawater). Chukanovite, the Fe(II) hydroxycarbonate with composition Fe2(OH)2CO3, was studied more particularly. Its standard Gibbs free energy of formation could be determined via the detailed study of the equilibrium conditions with Fe(II) hydroxide, performed with aqueous suspensions aged up to 6 months. Potential-pH equilibrium diagrams of iron could then be drawn including chukanovite and highlighting its domain of stability. A comparison with diagrams drawn with siderite FeCO3 revealed that chukanovite was metastable (at 25°C) with respect to siderite. The mechanisms of transformation of chukanovite were also studied for various conditions of oxidation. Hydrogen peroxide was for instance used to accelerate the reaction. The obtained results show that the oxidation of chukanovite leads, at 25°C, to lepidocrocite and/or goethite without the formation of an intermediate Fe(II,III) green rust-like compound. Goethite is favored by an increase of pH (i.e. excess of carbonate). The violent oxidation by hydrogen peroxide leads to a Fe(III) oxycarbonate structurally similar to chukanovite. Finally, two Fe(II) hydroxysulphates could be identified and characterised by X-ray diffraction and infrared spectroscopy. These compounds could not however be obtained alone, but always together, and/or with Fe(OH)2 or maybe a third Fe(II) hydroxysulphate. The study of their oxidation process revealed that all these compounds were first transformed to sulfated green rust.

Made available in DSpace on 2017-07-21T18:53:17Z (GMT). No. of bitstreams: 1 hanna.pdf: 1540428 bytes, checksum: 5ef484decfdf0f2847bc9b139292d514 (MD5) Previous issue date: 2007-02-15 / The phytic acid depending on the pH value presents high potential quelante, quelanting metallic ions, inhibiting the production of species reactivates of oxygen, responsible for the destruction oxidative in biological systems. That potential quelante has been basing several applied studies to the antioxidant action in foods products, in environmental controls and as antioxidant in the human organism. The objective of this work was to study the degree of interaction of the phytic acid with the metallic ions Fe(II) and Fe(III), of biological importance, in near conditions of the physiologic and the stability of these complexes. Potentiometric titration were driven to determine the constants of formation of the complexes phytic acid-Fe(II) and phytic acid-Fe(III) in solution, under conditions of inert atmosphere, it ionic strength 0,1 mol.L-1 (KCl) at 36±0,1 ºC. For the system phytic acid- Fe(II), were determined seven constant of formation, corresponding to seven species formed in the range p[H] from 2,0 to 12,0. The first constant of formation of the complex phytic acid- Fe(II), it presented log K = 16,06 for the specie [MHL]9-, indicating that a great affinity exists among the ligand monoprotonated with the metal. For the system phytic acid-Fe(III) were determined seven constant of formation, seven species were detected in the range p[H] from 2,5 to 12,0. The first constant of formation of the complex presented log K = 18,87, very high value for the species [ML]9-, this denoted a strong interaction among the ligand deprotonated and the metallic ion. Studies spectroscopy in the region of the UV-Vis, were performed to accompany the formation of the complexes of the phytic acid with the metallic ions Fe(II) and Fe(III). In the studies of UV-Vis of the phytic acid in absence of the metallic ions, not occurred any absorption in the area of wavelength from 200 to 800 nm. Already for the ligand in the presence of the metallic ions two absorption bands were detected in 216 and 279 nm for the phytic acid-Fe(II) and 218 and 274 nm for the phytic acid Fe(III). Those are bands of transfer of electrons of the ligand for the metallic ion with formation of the linking coordinative. The complexes phytic acid-Fe(II) and phytic acid-Fe(III) were synthesized from the data potentiometric and characterized by absorption spectroscopy in the area of the infrared. The spectra for the system phytic acid in presence of the ions Fe(II), synthesized in pH=7,4, and Fe(III), pH=7,1, showed displacements in the areas of frequency of the groups O=PO3H2 of the phytic acid free. Those displacements, evidence that the ligant is coordinated to the metallic ions. Through the termogravimetry it verified that in the interval from 30 to 780 ºC the loss of total mass of the complex phytic acid-Fe(II) it was of 24,43 %. Of the room temperature up to 185 ºC, occurred the liberation of molecules of hydration water. In superior temperatures of this value the mass losses were relative to the decomposition of the compound, with liberation of constitution water and decomposition of the organic matter, with formation of double pyrophosphate of potassium and Fe(II) and potassium metaphosphate. The phytic acid-Fe(III) complexes presented thermal behavior similar to the complex phytic acid-Fe(II), however for the complex phytic acid-Fe(III) synthesized in pH 7,1 the loss of total mass of it was of 25,64 % in the area from 30 to 800 ºC, while the compound synthesized in pH 9,9 presented a loss of total mass of 31,98 % in the interval of temperature from 30 to 845 ºC. The obtained data, for the three complexes, indicate that the ligand is coordinated with the metallic ions so much in values of low pH as to you value of higher pH. / O ácido fítico dependendo do valor de pH apresenta alto potencial quelante, complexando íons metálicos, inibindo assim a produção de espécies reativas de oxigênio, responsáveis pela destruição oxidativa em sistemas biológicos. Esse potencial quelante tem fundamentado diversos estudos aplicados à ação antioxidante em produtos alimentícios, em controles ambientais e como antioxidante no organismo humano. O objetivo deste trabalho foi estudar o grau de interação do ácido fítico com os íons metálicos Fe(II) e Fe(III), de importância biológica, em condições próximas às fisiológicas e a estabilidade destes complexos. Titulações potenciométricas foram conduzidas para determinar as constantes de formação dos complexos ácido fítico-Fe(II) e ácido fítico-Fe(III) em solução, sob condições de atmosfera inerte, força iônica 0,100 mol.L-1 (KCl) a 36±0,1 ºC. Para o sistema ácido fítico- Fe(II), determinaram sete constantes de formação, correspondente a sete espécies formadas na faixa de p[H] de 2,0 a 12,0. A primeira constante de formação do complexo ácido fítico- Fe(II), apresentou log K=16,06 para a espécie [MHL]9-, indicando que existe uma grande afinidade entre o ligante monoprotonado com o metal. Para o sistema ácido fítico-Fe(III) foram determinadas sete constantes de formação, sete espécies foram detectadas na faixa de p[H] de 2,5 a 12,0. A primeira constante de formação do complexo apresentou log K=18,87, valor muito elevado para a espécie [ML]9-, isto denotou uma forte interação entre o ligante totalmente deprotonado e o íon Fe(III). Estudos espectroscópicos na região do UV-Vis foram realizados para acompanhar a formação dos complexos do ligante com os íons metálicos Fe(II) e Fe(III). Nos estudos de UV-Vis do ácido fítico em ausência dos íons metálicos não ocorreu nenhuma absorção na faixa de comprimento de onda de 200 a 800 nm. Já para o ligante na presença dos íons metálicos foram detectadas duas bandas de absorção em 216 e 279 nm para o ácido fítico-Fe(II) e 218 e 274 nm para o ácido fítico Fe(III). Essas são bandas de transferência de elétrons do ligante para o íon metálico com formação da ligação coordenativa. Os complexos ácido fítico-Fe(II) e ácido fítico-Fe(III) foram sintetizados a partir dos dados potenciométricos e caracterizados por espectroscopia de absorção na região do infravermelho. Os espectros para o sistema ácido fítico em presença do íon Fe(II), sintetizado em pH=7,4, e Fe(III), pH=7,1, mostraram deslocamentos nas regiões de freqüência dos grupamentos O=PO3H2 do ácido fítico livre. Esses deslocamentos evidenciam que o ligante encontra-se coordenado aos íons metálicos. Através da termogravimetria constatou-se que no intervalo de 30 a 780 ºC, a perda de massa total do complexo ácido fítico-Fe(II) foi de 24,43 %. Da temperatura ambiente até 185 ºC, ocorreu a liberação de moléculas de água de hidratação. Em temperaturas superiores deste valor as perdas de massa foram relativas à decomposição do complexo, com liberação de água de constituição e decomposição da matéria orgânica, com formação de pirofosfato duplo de potássio e Fe(II) e metafosfato de potássio. Os complexos ácido fítico-Fe(III) apresentaram comportamento térmico semelhante ao complexo ácido fítico-Fe(II), porém, para o complexo ácido fítico-Fe(III) sintetizado em pH 7,1 a perda de massa total do foi de 25,64 % na faixa de 30 a 800 ºC, enquanto que o complexo sintetizado em pH 9,9 apresentou uma perda de massa total de 31,98 % no intervalo de temperatura de 30 a 845 ºC. Os dados obtidos, para os três complexos, indicam que o ligante encontra-se coordenado com os íons metálicos tanto em valores de pH baixo como em valores de pH mais elevados.

Les complexes à transition de spin sont des molécules qui peuvent être commutées entre deux états, l’un diamagnétique et l’autre paramagnétique. Cette commutation peut s’effectuer, entre autre, à l’aide d’une excitation lumineuse, ouvrant la voie vers un possible stockage de l’information au niveau d’une molécule unique. Toutefois, l’information photo-inscrite n’est stable qu’au-dessous d’une certaine température appelée T(LIESST). L’objectif principal de cette thèse a constitué en des modifications chimiques (modification du ligand organique, désolvatation, modifications d’anion,…) d’un complexe macrocyclique de Fe(II) qui présente à l’heure actuelle l’un des T(LIESST) les plus élevés (134 K), et ce afin d’augmenter encore cette valeur. Parmi les divers résultats expérimentaux, un T(LIESST) de 160 K a été obtenu. / Spin transition complexes are molecules that can be commuted between two different states, one being diamagnetic and the other one paramagnetic. This commutation can be triggered by different ways, including light irradiation, opening a way to the storage of information at molecular level. However, the photo-inscribed information is stable only below a given temperature called T(LIESST). The main goal of this thesis has been to modify chemically (modification of organic ligand, desolvation, modification of anions, …) a Fe(II) macrocyclic ligand presenting one of the highest T(LIESST) known today (134 K) with the aim to further increase this temperature. Among the different results obtained, a T(LIESST) of 160 K has been reached.

Cette thèse de doctorat présente les résultats d'une étude expérimentale des composés à transition de spin pour le dépôt de surface. Nous nous sommes concentrés sur Fe(II) systèmes avec la configuration de d6 et leur comportement bistable ST. Dans une symétrie octaédrique le configuration d6 peut adopter deux états fondamentaux électronique différentes selon l'occupation des orbitales d scindé en exemple eg et t2g sous-ensembles. Si la différence d'énergie entre deux états est petite, alors tourner transition peut être induite par un stimulus externe. En fait, les complexes adoptent l'état haut spin ou l'état bas spin en raison de la différence d'énergie entre les orbitales (eg, t2g) et de l'énergie de répulsion interélectronique. Nous avons synthétisé et caractérisé de nouveaux ligands tridentates organiques, qui ont été utilisés comme précurseurs pour les nouveaux Fe(II) composés de coordination. Nous avons préparé des complexes Fe(II) avec et sans contre-anions. / This doctoral thesis presents the results of an experimental study of the spin transition compounds for surface deposition. We have focused on Fe(II) systems with d6 configuration and their bistable ST behaviour. In an octahedral symmetry the d6 configuration can adopt two different electronic ground states according to the occupation of the d orbitals split into the eg and t2g subsets. If the energy difference between two states is small then the spin transition can be induced by an external stimulus. In fact, the complexes adopt the high-spin state or the low-spin state by reason of energy difference between orbitals and interelectronic repulsion energy. Nine novel tridentate ligands have been synthesized and characterized; they were used as precursors for new Fe(II) coordination compounds. The SQUID magnetometry was used in studying magnetic properties of prepared complexes and the XAS technique was also applied to study magnetic properties of a neutral complex on an adhesive graphite tape.

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Porphyrins are an important class of biomolecules, which are heavily studied, both ex- perimentally and computationally. But, despite the intensive efforts, for many questions we still aren't able to consistently find an agreement between theory and experiment. One of the still unresolved issues is the character of the ground state of the Fe(II)-porphyrin molecule. We used a model of the Fe(II)-porphyrin molecule to study the effects of geometrical changes on the spin states. By carrying out extensive DMRG-CASSCF cal- culations topped with TCCSD correlation treatment we are able to link the effects of these geometrical changes to the experimental results, and predict a quintet ground state for the isolated Fe(II)-porphyrin molecule. Also, using a ligated porphyrin belonging to the iron porphyrin carbene class of molecules, we demonstrate by combining the CASSCF and AC0 methods that geometrical changes outside the porphyrin core cannot be over- looked. 1

The reaction between aqueous Fe(II) and Fe(III) oxides is extremely complex, and can catalyze Fe(II)-Fe(III) electron transfer, exchange of Fe atoms between the aqueous and solid phases, mineral transformation, and contaminant reduction. Together, these processes represent a phenomenon referred to as Fe(II)-catalyzed Fe oxide recrystallization, which has been observed under controlled conditions in the laboratory for numerous Fe oxides. In the environment, Fe oxides are likely surrounded by organic carbon in various forms, but their potential to interfere with Fe(II)-catalyzed Fe oxide recrystallization, and its subsequent environmental relevance has not been well studied. The Fe(II)-catalyzed recrystallization of stable Fe oxides goethite and magnetite was studied in the presence of several environmentally relevant classes of organic carbon. For both goethite and magnetite, Fe(II)-catalyzed recrystallization continued relatively undeterred in the presence of electron shuttling compounds, natural organic matter isolates, and extracellular polysaccharides. Slight inhibition was observed when spent media from dissimilatory iron-reducing cultures was present, but only by sorbing a long-chain phospholipid to the oxides was significant inhibition observed. The lack of interference by organic carbon indicates that Fe(II)-catalyzed Fe oxide recrystallization is likely to be relevant throughout a wide range of environments, and represents a significant process with regards to the geochemical cycling of Fe atoms, a claim supported by evidence of Fe(II)-driven isotope mixing in real soils. The movement of atoms during Fe(II)-catalyzed Fe oxide recrystallization is not limited to just Fe however. Multiple trace elements have been shown to exchange between the aqueous and solid phases along with Fe during the Fe(II)-catalyzed recrystallization of Fe oxides. The effect of organic carbon, both sorbed to the oxide surface and coprecipitated with the oxide, on Fe(II)-catalyzed atom exchange and transformation of ferrihydrite was studied. Again, the presence of organic carbon did not appear to influence Fe atom exchange kinetics. It also did not appear to influence the rapid transformation of ferrihydrite to lepidocrocite. The presence of organic carbon does appear to ultimately have implications for mineral transformation, as over longer time periods it stabilized lepidocrocite, preventing its subsequent transformation to magnetite or goethite.

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