Hydrogen and water vapour effects on oxygen solubility and diffusivity in high temperature Fe-Ni alloys

It is a worldwide priority to reduce emissions of greenhouse gases such as CO2. One solution for reducing these emissions is to improve the efficiency of energy production units by increasing their operating temperature. However, in order to increase operating temperature, new austenitic materials based on the Fe-Ni-Cr system have to be designed. In addition, these materials need to exhibit good protection against high temperature oxidation, which is achieved by the formation of a slow growing chromium oxide or alumina scale on the metal. However, to predict the formation of a protective scale, knowledge of the oxygen permeability, the product of oxygen solubility and diffusivity, in the base alloy is required. The objective of this study is to measure the permeability, solubility and diffusivity of oxygen in Fe- Ni alloys at temperatures above 1,000°C. In order to obtain the best results, the formation of an external oxide layer during the experiment has to be avoided. To achieve this, the oxygen partial pressure was fixed at the Fe/FeO equilibrium pressure in all experiments. In addition, two types of atmospheres were used: one dry and one wet, in order to investigate the effect of water vapour on oxygen permeability, solubility and diffusivity. The dry atmosphere was achieved using the Rhines Pack technique. The samples were oxidised in vacuum-sealed quartz capsules, which contained a mixture of powdered iron and wüstite. The humid atmosphere was obtained by using H2/H2O gas mixtures with the appropriate water vapour to hydrogen ratio to fix oxygen partial pressure at the Fe/FeO equilibrium. The maximum oxygen solubility was found in pure iron, and decreased continuously with nickel additions to the alloy. The dependence of solubility on alloy composition is non-ideal, and cannot be predicted from simple models. Moreover, the presence of water vapour in the atmosphere seems to increase the solubility by a factor of 2 in alloys with nickel content lower than 80 at.% at temperatures near 1,000°C. However, at 1,150°C the solubility of the oxygen is independent of the environment. The oxygen permeability was determined by measuring the internal oxidation kinetics of Fe-Ni-Cr alloy. These kinetics were evaluated by measuring the internal oxidation zone depth by optical microscopy, or by continuous and discontinuous thermogravimetry. Results showed that the oxygen permeability exhibits the same variation with alloy composition as the oxygen solubility, independent of the atmosphere. In particular, no significant effect of water vapour on oxygen permeability values was observed. In the present study, the oxygen diffusion coefficient was also determined using permeability, in addition to the independent measurement of the oxygen solubility carried out in the present study. For temperature above 1,000°C, the variation of oxygen diffusion coefficient with the alloy composition is similar in all environments tested, and a maximum is observed for alloys with a nickel content of 40 at.%. However, for a given nickel content up to 60 at.%, the presence of water vapour in the atmosphere decreases the value of the oxygen diffusion coefficient by a factor of 2-3 at 1,000°C. In addition, this difference between diffusion coefficients measured in a dry and wet atmosphere increases as the temperature decreases. Overall, it was found that the water vapour has no effect on the way in which oxygen permeability, solubility and diffusivity vary with the alloy composition. However, the presence of water vapour in the environment appears to increase the oxygen solubility and decrease the oxygen diffusivity in iron-rich alloys, the effect being more significant at low temperatures. These results suggest further research into interactions between O, H and metal vacancies, particularly for temperature around 1,000°C and below, as the latter defect is thought to change the diffusion and solubility properties of interstitial species

Contribution à la prise en charge nutritionnelle et comportementale du chat obèse

Après avoir rappelé le comportement alimentaire puis étudié la mise en place de l’état d’obésité, ses méthodes d’évaluation et ses conséquences sur l’état de santé du chat, l’auteur s’est intéressée aux causes médicales, alimentaires et comportementales de l’obésité féline ainsi qu’aux méthodes de prise en charge disponibles à ce jour pour le vétérinaire praticien. Puis, une étude expérimentale a été menée sur 14 chats obèses suivis en consultation de nutrition à l’ENVT et ne présentant aucun trouble médical pouvant expliquer la prise de poids. Après évaluation de l’anxiété et du comportement de chaque chat, des adaptations alimentaires et environnementales ont été proposées afin d’améliorer globalement l’hygiène de vie des animaux. Les résultats de cette étude montrent que l’identification et le traitement d’un trouble comportemental chez le chat obèse sont essentiels dans la gestion de l’obésité. Enfin, cette étude a permis de construire deux outils destinés à la gestion de l’obésité : une grille d’évaluation de l’anxiété du chat et un arbre décisionnel tenant compte des diverses étiologies de l’obésité pour guider le vétérinaire dans sa prise en charge du chat obèse

The effect of hydrogen in the HIP treatment of additive manufactured IN718

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Sur La Structure Du Bulbe D'une Orchidée Exotique De La Tribu Des Aréthusées

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Impact of the clusterization on the solubility of oxygen and vacancy concentration in nickel: A multi-scale approach

Combining thermodynamic concepts with first-principles calculations, we study the solubility of oxygen atoms (O) in nickel. In our approach, we include the possible formation of oxygen clusters (On) and vacancies-oxygens clusters (VOn and V2On). We show that the vacancy-oxygens interactions are strong (approximately 1 eV) and would induce a large concentration of clusters in fcc-Ni. The use of a thermodynamic model, within a grand canonical approach, allows calculation of the vacancy concentration, including these VOn clusters, as a function of O concentration, for different temperatures. We find that at low temperatures (below 600 K), a small content of oxygen (in appm) strongly modifies the vacancy concentration, increasing the total vacancy concentration in the metal by many orders of magnitude more than the thermal vacancy concentration. The vacancy concentration is thus directly controlled by the oxygen content in the metal. At high temperatures, the effect is reduced, becoming negligible near the melting point. These results show the strong impact of interstitial atoms on the vacancy concentration. The influence of the vacancy formation energy is also discussed

Internal oxidation in dry and wet conditions for oxygen permeability of Fe–Ni alloys at 1150 and 1100 °C

The design of new austenitic alloys based on the Fe–Ni–Cr system requires knowledge of their oxygen permeability. Data are available for pure Fe and Ni but not for Fe–Ni alloys. Wagner’s model for internal oxidation is used to evaluate the oxygen permeability in Fe–Ni alloys. Internal oxidation of Fe–Ni–Cr alloys carried out at 1150 and 1100 °C in Rhines packs and H2/H2O mixtures is described. Internal oxidation produces zones of FeCr2O4 and Cr2O3 precipitates, according to parabolic kinetics. Permeabilities are deduced taking into account interfacial diffusion contributions. Oxygen permeability decreases with nickel addition in a non-ideal way, and oxygen permeability in nickel-rich alloys is independent of the studied environments. However, the oxygen permeability in iron at the highest temperature studied is increased in H2/H2O

Theoretical study of oxygen insertion and diffusivity in the g-TiAl L10 system

This work is a first-principles study of the insertion and diffusivity of oxygen in the -TiAl L10 system. Five interstitial positions were identified as stable. One, however, the 2h site a pyramid composed of a Ti square topped by an Al atom, was found more stable than the others. The oxygen interactions with the TiAl system were thus studied and analyzed in detail using vibrational, elastic and electronic properties. The results show that the O atom prefers to be surrounded by Ti atoms and tries to minimize the number of bonds with aluminum. The diffusion mechanism is subsequently studied at the atomic scale, by analyzing displacements between stable interstitial sites. The oxygen diffusivity is found to be anisotropic and the components in the x and z direction, Dx and Dz, are then calculated and compared with those of O diffusion into other Ti–Al alloys. The analysis of results shows two effects. First, the stability of sites is related to the number of O–Al bonds, the fewer there are, the more stable the site is, and second, the diffusion is faster when the content of interstitial sites composed of many Ti atoms is lo

Oxygen permeability of Fe-Ni-Cr alloys at 1100 and 1150 °C under carbon-free and carbon-containing gases

Wagner's model of internal oxidation allows the prediction of an alloy's critical concentration of oxide forming metal required to achieve a protective oxide scale at high temperatures. The model depends on oxygen permeability in the alloy, but this parameter has not been evaluated for the Fe-Ni system, and the influence of carbon-bearing gases is unknown. Oxygen permeability measurement by internal oxidation of Fe-Ni-Cr alloys, reacted at 1100 and 1150 8C is described. Exposures in Rhines packs and flowing CO-CO2 gas mixtures serve to assess the influence of carbon on oxygen permeability at the Fe-FeO equilibrium oxygen potential. Oxygen permeability in Fe-Ni increases with iron content in a non-ideal manner in both gas environments. Higher permeability is found in carbon bearing gases for iron-rich alloys, and the size of this effect increases with temperature

Effets de l'hydrogène et de la vapeur d'eau sur la solubilité et la diffusion de l'oxygène à haute température dans les alliages Fe-Ni

Les matériaux basés sur le système Fe-Ni-Cr utilisés à haute température doivent présenter une bonne résistance à l'oxydation, généralement obtenu par la croissance lente d’une couche d’oxyde de chrome à la surface de ces alliages. Pour prédire la formation d'une couche d’oxyde protectrice la perméabilité de l'oxygène dans l’alliage doit être connue, la perméabilité étant définie comme le produit de la solubilité et du coefficient de diffusion de l’oxygène. L'objectif de nos travaux est de mesurer la perméabilité, la solubilité et la diffusivité de l'oxygène dans des alliages Fe-Ni pour des températures supérieures à 1000°C. Afin d'obtenir les meilleurs résultats,la formation d'une couche externe d'oxyde pendant les expériences doit être évitée. Pour cela, la pression partielle d'oxygène a été fixée à la pression d'équilibre Fe/FeO dans toutes les expériences. En outre, afin d'étudier l'effet de la vapeur d'eau sur la perméabilité, la solubilité et la diffusivité de l’oxygène, deux atmosphères ont été utilisées: l’une considérée comme sèche et l’autre comme humide. L'atmosphère sèche a été obtenue en utilisant la technique du « pack de Rhines »: les échantillons sont oxydés dans des capsules en quartz sous vide qui contiennent un mélange de poudre de fer et de wüstite. L'atmosphère humide a quant à elle été obtenue en utilisant des mélanges gazeux H2/H2O avec un ratio approprié de vapeur d'eau et d’hydrogène afin de fixer la pression partielle d’oxygène à la pression d’équilibre Fe/FeO. Les mesures de solubilité réalisées dans ce travail ont montré que celle-ci atteint son maximum dans le fer pur et diminue avec l’ajout de nickel. Cependant, la dépendance de la solubilité avec la composition de l’alliage Fe-Ni n'est pas idéale et ne peut être prédite à partir de modèles simples. De plus, les résultats obtenus sous atmosphère humide suggèrent que la présence de vapeur d'eau dans l'atmosphère augmente la solubilité de l'oxygène d’un facteur 2 dans les alliages avec une concentration en nickel inférieure ou égale à 60 at.% pour des températures proches de 1000°C,tandis qu'à 1150°C, la solubilité de l'oxygène est indépendante de l'environnement. La perméabilité de l'oxygène a été déterminée en mesurant la cinétique d'oxydation interne d'alliages Fe-Ni-Cr. Les résultats ont montré que la perméabilité de l'oxygène présente les mêmes variations avec la composition de l’alliage que la solubilité de l'oxygène, indépendamment de l'atmosphère.De plus, aucun effet significatif de la vapeur d'eau sur les valeurs de perméabilité de l'oxygène n'a été observé. Le coefficient de diffusion de l'oxygène a également été déterminé en utilisant les résultats précédents, c’est à dire la perméabilité et la solubilité de l’oxygène mesurées dans notre étude. Pour une température supérieure à 1000°C, la variation du coefficient de diffusion de l'oxygène avec la composition de l'alliage est similaire dans tous les environnements testés et un maximum est observé pour les alliages avec une teneur en nickel de 40 at.%. Cependant, la présence de vapeur d'eau dans l'atmosphère diminue les valeurs du coefficient de diffusion de l'oxygène, par un facteur 2-3 à 1000°C, pour les alliages avec une concentration en nickel inférieure ou égal à 60 at.%. De plus, il a été trouvé que la différence entre les coefficients de diffusion mesurés dans l’atmosphère sèche et humide augmente à mesure que la température diminue. En conclusion, il a été constaté que la vapeur d'eau n'a aucun effet sur la manière dont la perméabilité, la solubilité et la diffusivité de l'oxygène varient avec la composition des alliages Fe-Ni. Cependant, la présence de vapeur d'eau dans l'environnement semble augmenter la solubilité de l'oxygène et diminuer sa diffusivité dans les alliages riches en fer. De plus, l’effet de la vapeur d’eau apparaît plus important aux plus basses températures étudiées.It is a worldwide priority to reduce emissions of greenhouse gases such as CO2. One solution for reducing these emissions is to improve the efficiency of energy production units by increasing their operating temperature. However, in order to increase operating temperature, new austenitic materials based on the Fe-Ni-Cr system have to be designed. In addition, these materials need to exhibit good protection against high temperature oxidation, which is achieved by the formation of a slow growing chromium oxide or alumina scale on the metal. However, to predict the formation of a protective scale, knowledge of the oxygen permeability, the product of oxygen solubility and diffusivity, in the base alloy is required. The objective of this study is to measure the permeability, solubility and diffusivity of oxygen in Fe- Ni alloys at temperatures above 1,000°C. In order to obtain the best results, the formation of an external oxide layer during the experiment has to be avoided. To achieve this, the oxygen partial pressure was fixed at the Fe/FeO equilibrium pressure in all experiments. In addition, two types of atmospheres were used: one dry and one wet, in order to investigate the effect of water vapour on oxygen permeability, solubility and diffusivity. The dry atmosphere was achieved using the Rhines Pack technique. The samples were oxidised in vacuum-sealed quartz capsules, which contained a mixture of powdered iron and wüstite. The humid atmosphere was obtained by using H2/H2O gas mixtures with the appropriate water vapour to hydrogen ratio to fix oxygen partial pressure at the Fe/FeO equilibrium. The maximum oxygen solubility was found in pure iron, and decreased continuously with nickel additions to the alloy. The dependence of solubility on alloy composition is non-ideal, and cannot be predicted from simple models. Moreover, the presence of water vapour in the atmosphere seems to increase the solubility by a factor of 2 in alloys with nickel content lower than 80 at.% at temperatures near 1,000°C. However, at 1,150°C the solubility of the oxygen is independent of the environment. The oxygen permeability was determined by measuring the internal oxidation kinetics of Fe-Ni-Cr alloy. These kinetics were evaluated by measuring the internal oxidation zone depth by optical microscopy, or by continuous and discontinuous thermogravimetry. Results showed that the oxygen permeability exhibits the same variation with alloy composition as the oxygen solubility, independent of the atmosphere. In particular, no significant effect of water vapour on oxygen permeability values was observed. In the present study, the oxygen diffusion coefficient was also determined using permeability, in addition to the independent measurement of the oxygen solubility carried out in the present study. For temperature above 1,000°C, the variation of oxygen diffusion coefficient with the alloy composition is similar in all environments tested, and a maximum is observed for alloys with a nickel content of 40 at.%. However, for a given nickel content up to 60 at.%, the presence of water vapour in the atmosphere decreases the value of the oxygen diffusion coefficient by a factor of 2-3 at 1,000°C. In addition, this difference between diffusion coefficients measured in a dry and wet atmosphere increases as the temperature decreases. Overall, it was found that the water vapour has no effect on the way in which oxygen permeability, solubility and diffusivity vary with the alloy composition. However, the presence of water vapour in the environment appears to increase the oxygen solubility and decrease the oxygen diffusivity in iron-rich alloys, the effect being more significant at low temperatures. These results suggest further research into interactions between O, H and metal vacancies, particularly for temperature around 1,000°C and below, as the latter defect is thought to change the diffusion and solubility properties of interstitial species

Sur La Formation Et La Germination Des Spores Des Urocystis (Ustilagin\ue9es)

Volume: 27Start Page: 204End Page: 20