Atom probe field ion microscope measurements of carbon segregation at an a:a grain boundary and service failures by intergranular stress corrosion cracking

This work reports on a critical measurement to understand the intergranular stress corrosion cracking (IGSCC) of pipeline steels: the atom probe field ion microscope (APFIM) measurement of the carbon concentration at a grain boundary (GB). The APFIM measurement was related to the microstructure and to IGSCC observations. The APFIM indicated that the GB carbon concentration of X70 was similar to 10 at% or less, which correlated with a high resistance to IGSCC for X70. (C) 2005 Elsevier Ltd. All rights reserved.

The distribution of grain boundary and interface plane orientations in transformed microstructures

The properties of interfaces depend not only on the lattice misorientation, but also on the interface plane orientation. Extensive studies of grain boundaries led to the conclusion that in systems evolving by grain growth, the relative areas of different grain boundary planes are inversely correlated to their relative energies. In other words, the low energy grain boundary planes make up a larger part of the population than the higher energy grain boundary planes. The hypothesis of this work is that the interface plane orientation distribution in transformed microstructures depends more on the mechanism of formation than on the relative energy. After a discussion of methods for measuring interface plane orientations, results will be presented for lath martensite in a low carbon steel and for martensite in a Ti-6Al-4V alloy processed in two different ways to promote a displacive transformation in one case and a diffusional transformation in the other.

The role of thermomechanical routes on the distribution of grain boundary and interface plane orientations in transformed microstructures

In the current study, a series of thermomechanical routes were used to produce different microstructures (i.e., ferrite and martensite) in low-carbon low alloy steels. The five-parameter grain boundary character distribution was measured for all microstructures. The thermomechanical processing route altered the texture of the fully ferritic microstructure and significantly influenced the anisotropy of the grain boundary character distribution. Generally, the population of (111) planes increased with an increase in the γ-fiber texture for the ferritic microstructure, but it did not change the shape of the grain boundary plane distribution at specific misorientations. The most commonly observed boundaries in the fully ferritic structures produced through different routes were {112} symmetric tilt boundaries with the Σ3 = 60 deg/[111] misorientation; this boundary also had a low energy. However, the grain boundary plane distribution was significantly changed by the phase transformation path (i.e., ferrite vs martensite) for a given misorientation. In the martensitic steel, the most populous Σ3 boundary was the {110} symmetric tilt boundary. This results from the crystallographic constraints associated with the shear transformation (i.e., martensite) rather than the low-energy interface that dominates in the diffusional phase transformation (i.e., ferrite).

Thermal Stability of Spherical Nanoporous Aggregates and Formation of Hollow Structures by Sintering-A Phase-Field Study

Nanoporous structures are widely used for many applications and hence it Is important to investigate their thermal stability. We study the stability of spherical nanoporous aggregates using phase-field simulations that explore systematically the effect of grain boundary diffusion, surface diffusion, and grain boundary mobility on the pathways for microstructural evolution. Our simulations for different combinations of surface and GB diffusivity and GB mobility show four distinct microstructural pathways en route to 100% density: multiple dosed pores, hollow shells, hollow shells with a core, and multiple interconnected pores. The microstructures from our simulations are consistent with experimental observations in several different systems. Our results have important implications for rational synthesis of hollow nanostructures or aggregates with open pores, and for controlling the stability of nanoporous aggregates that are widely used for many applications.

大别山硬玉石英岩带中的水

The Dabie Mountains is a collisional orogenic belt between the North China and Yantze Continental plates. It is the eastern elongation of the Tongbai and Qingling orogen, and is truncated at its east end by the Tan-Lu fault. Jadeite-quartzite belt occurs in the eastern margin of UHPMB from the Dabie Mountains. Geochemical features indicate that the protoliths of the jadeite-quartzite and associated eclogite to be supracrustal rocks. The occurrence of micro-inclusions of coesite in jadeite and garnet confirmed that the continental crust can be subducted to great depth (8 0-100km) and then exhumed rapidly with its UHP mineral signature fairly preserved. Therefore, study of UHP jadeite-quartzite provides important information on subduction of continental crustal rocks and their exhumation histories, as well as the dynamics of plate tectonic processes at convergent margins. The purpose of this paper is to investigate the presence of hydrous component in the jadeite-quartzite belt, significant natural variations in the hydrous component content of UHP minerals and to discuss the role of water in petrology, geochemistry and micro-tectonic. On the basis of our previous studies, some new geological evidences have been found in the jadeite-quartzite belt by researches on petrography, mineralogy, micro-tectonic, hydrous component content of UHP minerals and combined with the study on rheology of materials using microprob, ER, TEM. By research and analysis of these phenomenona, the results obtained are as follows: 1. The existence of fluid during ultra-high pressure metamorphic process. Jadeites, omphacite, garnet, rutile, coesite and quartz from the jadeite-quartzite belt have been investigated by Fourier transform infrared spectrometer and TEM. Results show that all of these minerals contain trace amount of water which occur as hydroxyl and free-water in these minerals. The two-type hydrous components in UHP minerals are indicated stable in the mantle-depth. The results demonstrated that these ultra-high pressure metamorphic minerals, which were derived from continental crust protoliths, they could bring water into the mantle depth during the ultra-high pressure metamorphism. The clusters of water molecules within garnet are very important evidence of the existence of fluid during ultra-high pressure metamorphic process. It indicated that the metamorphic system was not "dry"during the ultra-high pressure stage. 2.The distribution of hydrous component in UHP minerals of jadeite-quartzite. The systematic distribution of hydrous components in UHP minerals are a strong indication that water in these minerals, are controlled by some factors and that the observed variations are not of a random nature. The distribution and concentration of hydrous component is not only correlated with composition of minerals, but also a function of geological environment. Therefore, the hydrous component in the minerals can not only take important part in the UHP metamorphic fluid during subduction of continental crustal rocks, but also their hydroxyl transported water molecules with decreasing pressure during their exhumation. And these water molecules can not only promote the deformation of jadeite through hydrolytic weakening, but also may be the part of the retrograde metamorphic fluid. 3.The role of water in the deformed UHP minerals. The jadeite, omphacite, garnet are strong elongated deformation in the jadeite-quartzite from the Dabie Mountains. They are (1) they are developed strong plastic deformation; (2) developed dislocation loop, dislocation wall; (3) the existence of clusters of water molecular in the garnet; and (4) the evolution of micero-tectonic from clusters of water molecular-dislocation loop in omphacite. That indicated that the water weakening controlled the mechanism of deformed minerals. Because the data presented here are not only the existence of clusters of water molecular in the garnet, but also developed strong elongation, high density of dislocation and high aspect ratios, adding microprobe data demonstrate the studied garnet crystals no compositional zoning. Therefore, this indicates that the diffusion process of the grain boundary mobility did not take place in these garnets. On the basis of above features, we consider that it can only be explained by plastic deformation of the garnets. The clusters of water molecules present in garnet was directly associated with mechanical weakening and inducing in plastic deformation of garnet by glissile dislocations. Investigate of LPO, strain analysis, TEM indicated that these clinopyroxenes developed strong elongation, high aspect ratios, and developed dislocation loop, dislocation wall and free dislocations. These indicated that the deformation mechanism of the clinopyroxenes plastically from the Dabie Mountains is dominant dislocation creep under the condition of the UHP metamorphic conditions. There are some bubbles with dislocation loops attached to them in the omphacite crystal. The bubbles attached to the dislocation loops sometimes form a string of bubble beads and some loops are often connected to one another via a common bubble. The water present in omphacite was directly associated with hydrolitic weakening and inducing in plastic deformation of omphacite by dislocations. The role of water in brittle deformation. Using microscopy, deformation has been identified as plastic deformation and brittle deformation in UHP minerals from the Dabie Mountains. The study of micro-tectonic on these minerals shows that the brittle deformation within UHP minerals was related to local stresses. The brittle deformation is interpreted as being caused by an interaction of high fluid pressure, volume changes. The hydroxyl within UHP minerals transported water molecules with decreasing pressure due to their exhumation. However, under eclogite facies conditions, the litho-static pressure is extreme, but a high fluid pressure will reduce the effective stress and make brittle deformation possible. The role of water in prograde metamorphism. Geochemical research on jadeite-quartzite and associated eclogite show that the protoliths of these rocks are supracrustal rocks. With increasing of temperature and pressure, the chlorite, biotite, muscovite was dehydrous reaction and released hydrous component during the subduction of continental lithosphere. The supracrustal rocks were transformed UHP rocks and formed UHP facies assemblage promotely by water introduction, and was retained in UHP minerals as hydrous component. The water within UHP minerals may be one of the retrograde metamorphic fluids. Petrological research on UHP rocks of jadeite-quartzite belt shows that there was existence of local fluids during early retrograde metamorphism. That are: (1) coronal textures and symplectite around relict UHP minerls crystals formed from UHP minerls by hydration reactions; (2) coronal textures of albite around ruitle; and (3) micro-fractures in jadeite or garnet were filled symplectite of Amp + PI + Mt. That indicated that the reactions of early retrograde metamorphism dependent on fluid introduction. These fluids not only promoted retrograde reaction of UHP minerals, but also were facilitate to diffuse intergranular and promote growth in minerals. Therefore, the hydrous component in the UHP minerals can not only take important part in the UHP metamorphic fluid during subduction of continental crustal rocks, but also their hydroxyl transport water molecules with decreasing pressure and may take part in the retrograde metamorphic fluid during their exhumation. 7. The role of water in geochemistry of UHP jadeite-quartzite. Geochemical research show that there are major, trace and rare earth element geochemical variations in the jadeite-quartzite from the Changpu district of Dabie Mountains, during retrograde metamorphic processes from the jadeite-quartzite--gneiss. The elements such as SiO_2、FeO、Ba、Zr、Ga、La、Ce、PTN Nd% Sm and Eu increase gradually from the jadeite-quartzite to retrograded jadeite-quartzite and to gneiss, whilst TiO_2. Na_2CK Fe2O_3、Rb、Y、Nb、Gd、Tb、Dy、Ho、Er、Tm、Yb decrease gradually. And its fO_2 keep nearly unchanged during early retrograde metamorphism, but decreased obviously during later retrograde metamorphism. These indicate that such changes are not only controlled by element transformation between mineralogical phases, but also closely relative to fluid-rock interaction in the decompression retrograde metamorphic processes.

Microstructure design of Titanate-based electroceramics

Electrocerâmicos são uma classe de materiais avançados com propriedades eléctricas valiosas para aplicações. Estas propriedades são geralmente muito dependentes da microestrutura dos materiais. Portanto, o objectivo geral deste trabalho é investigar o desenho da resposta dieléctrica de filmes espessos obtidos por Deposição Electroforética (EPD) e cerâmicos monolíticos, através do controlo da evolução da microestrutura durante a sinterização de electrocerâmicos à base de titanatos. Aplicações sem fios na indústria microelectrónica e de comunicações, em rápido crescimento, tornaram-se um importante mercado para os fabricantes de semicondutores. Devido à constante necessidade de miniaturização, redução de custos e maior funcionalidade e integração, a tecnologia de filmes espessos está a tornar-se uma abordagem de processamento de materiais funcionais cada vez mais importante. Uma técnica adequada neste contexto é EPD. Os filmes espessos resultantes necessitam de um passo subsequente de sinterização que é afectada pelo substrato subjacente, tendo este um forte efeito sobre a evolução da microestrutura. Relacionado com a miniaturização e a discriminação do sinal, materiais dieléctricos usados como componentes operando a frequências das microondas em aplicações na industria microelectrónica de comunicações devem apresentar baixas perdas dieléctricas e elevadas permitividade dieléctrica e estabilidade com a temperatura. Materiais do sistema BaO-Ln2O3- TiO2 (BLnT: Ln = La ou Nd), como BaLa4Ti4O15 (BLT) e Ba4.5Nd9Ti18O54 (BNT), cumprem esses requisitos e são interessantes para aplicações, por exemplo, em estações de base para comunicações móveis ou em ressonadores para telefones móveis, onde a miniaturização dos dispositivos é muito importante. Por sua vez, o titanato de estrôncio (SrTiO3, STO) é um ferroeléctrico incipiente com constante dieléctrica elevada e baixas perdas, que encontra aplicação em, por exemplo, condensadores de camada interna, tirando partido de fronteiras de grão altamente resistivas. A dependência da permitividade dieléctrica do campo eléctrico aplicado torna este material muito interessante para aplicações em dispositivos de microondas sintonizáveis. Materiais à base de STO são também interessantes para aplicações termoeléctricas, que podem contribuir para a redução da actual dependência de combustíveis fósseis por meio da geração de energia a partir de calor desaproveitado. No entanto, as mesmas fronteiras de grão resistivas são um obstáculo relativamente à eficiência do STO para aplicações termoeléctricas. Para além do efeito do substrato durante a sinterização constrangida, outros factores, como a presença de fase líquida, a não-estequiometria ou a temperatura de sinterização, afectam significativamente não apenas a microestrutura dos materiais funcionais, mas também a sua resposta dieléctrica. Se adequadamente compreendidos, estes factores podem ser intencionalmente usados para desenhar a microestrutura dos electrocerâmicos e, desta forma, as suas propriedades dieléctricas. O efeito da não-estequiometria (razão Sr/Ti 0.995-1.02) no crescimento de grão e resposta dieléctrica de cerâmicos de STO foi investigado neste trabalho. A mobilidade das fronteiras de grão aumenta com a diminuição da razão Sr/Ti. A resistividade do interior dos grãos e das fronteiras de grão é sistematicamente diminuída em amostras não-estequiométricas de STO, em comparação com o material estequiométrico. O efeito é muito mais forte para as fronteiras de grão do que para o seu interior. Dependências sistemáticas da não-estequiometria foram também observadas relativamente à dependência da condutividade da temperatura (muito mais afectada no caso da contribuição das fronteiras de grão), à capacitância do interior e fronteiras de grão e à espessura das fronteiras de grão. Uma anomalia no crescimento de grão em cerâmicos de STO ricos em Ti foi também observada e sistematicamente analisada. Foram detectadas três descontinuidades na dependência do tipo Arrhenius do crescimento de grão relativamente à temperatura com diminuições no tamanho de grão a temperaturas em torno de 1500, 1550 e 1605 °C. Além disso, descontinuidades semelhantes foram também observadas na dependência da energia de activação relativamente à condutividade das fronteiras de grão e na espessura das fronteiras de grão, avaliadas por Espectroscopia de Impedância. Estas notáveis coincidências suportam fortemente a formação de diferentes complexos de fronteira de grão com transições entre os regimes de crescimento de grão observados, que podem ser correlacionados com diferentes mobilidades de fronteira de grão e propriedades dieléctricas. Um modelo é sugerido, que se baseia na diminuição da fase líquida localizada nas fronteiras de grão, como o aumento da temperatura de sinterização, um cenário compatível com um fenómeno de solubilidade retrógrada, observado anteriormente em metais e semicondutores, mas não em cerâmicos. A EPD de filmes espessos de STO em substratos de folha de Pt e a sinterização constrangida dos filmes fabricados foram também preliminarmente tratadas. Filmes espessos de STO foram depositados com êxito por EPD sobre substratos de Pt e, depois de sinterizados, atingiram densidades elevadas. Um aumento da densificação e do tamanho de grão assim como o alargamento da distribuição de tamanho do grão foram observados com a diminuição da razão Sr/Ti, tal como anteriormente observado em amostras cerâmicas. Grãos equiaxiados foram observados para todas as composições, mas um certo grau de anisotropia na orientação dos poros foi detectado: os poros revelaram uma orientação vertical preferencial. Este trabalho focou-se também na sinterização constrangida do sistema BLnT (Ln = La ou Nd), nomeadamente de filmes espessos de BLT e BNT sobre substratos de folha de platina, e na relação do desenvolvimento de anisotropia microestrutural com as propriedades dieléctricas. As observações durante a sinterização constrangida foram comparadas com cerâmicos monolíticos equivalentes sinterizados livremente. Filmes espessos de BLnT (Ln = La ou Nd) com elevada densidade foram obtidos por EPD e subsequente sinterização constrangida. A anisometria cristalográfica do material em conjunto com um passo de sinterização constrangida resultou em grãos alongados e microestruturas anisotrópicas. O efeito do stress do substrato durante a sinterização constrangida originou graus mais elevados de anisotropia (grãos e poros alongados e orientação preferencial, bem como textura cristalográfica) nos filmes sinterizados relativamente aos cerâmicos equivalentes sinterizados livremente, não obstante o estado equivalente das amostras em verde. A densificação dos filmes de BLnT (Ln = La ou Nd) é retardada em comparação com os cerâmicos, mas depois de longos tempos de sinterização densidades semelhantes são obtidas. No entanto, em oposição a observações na sinterização constrangida de outros sistemas, o crescimento do grão em filmes de BLnT (Ln = La ou Nd) é favorecido pelo constrangimento causado pelo substrato. Além disso, grãos e poros alongados orientados paralelamente ao substrato foram desenvolvidos durante a sinterização constrangida de filmes espessos. Verificou-se uma forte correlação entre a evolução de grãos e poros, que começou assim que o crescimento do grão se iniciou. Um efeito da tensão do substrato no aumento do crescimento de grão, bem como um forte “Zener pinning”, origina microestruturas altamente texturizadas, o que também é observado a nível cristalográfico. Efeitos marcantes da anisotropia microestrutural foram também detectados nas propriedades dieléctricas dos filmes de BLnT (Ln = La ou Nd). Juntamente com o aumento da razão de aspecto dos grãos, do factor de orientação e do grau de textura cristalográfica, a permitividade relativa é ligeiramente diminuída e o coeficiente de temperatura da permitividade evolui de negativo para positivo com o aumento do tempo isotérmico de sinterização. Este trabalho mostra que a não-estequiometria pode ser usada para controlar a mobilidade das fronteiras de grão e, portanto, desenhar a microestrutura e as propriedades dieléctricas de electrocerâmicos à base de STO, com ênfase nas propriedades das fronteiras de grão. O papel da não-estequiometria no STO e dos complexos de fronteira de grão no desenvolvimento microestrutural é discutido e novas oportunidades para desenhar as propriedades de materiais funcionais são abertas. As observações relativamente à sinterização constrangida apontam para o efeito de tensões mecânicas desenvolvidas devido ao substrato subjacente no desenvolvimento da microestrutura de materiais funcionais. É assim esperado que a escolha adequada de substrato permitia desenhar a microestrutura de filmes espessos funcionais com desempenho optimizado. “Stress Assisted Grain Growth” (SAGG) é então proposto como uma técnica potencial para desenhar a microestrutura de materiais funcionais, originando microestruturas anisotrópicas texturizadas com propriedades desejadas.

Application of identification techniques to determine effect of carbon content in steels on rheological parameters during hot deformation

The objective of the present work is searching for the correlation between the carbon content in steels and the parameters of the rheological models, which are used to describe the materials behavior during hot plastic deformation. This correlation can be expected in the internal variable models, which are based on physical phenomena occurring in the material. Such a model, based on the dislocation density as the internal variable, is investigated in this work. The experiments including hot torsion tests are used for the analysis.
The procedure is composed of three parts. Plastometric tests were performed for steels with various carbon content. Optimization techniques were applied next to determine the coefficients in the internal variable rheological model for these steels. Two versions of the model are considered. One is based on the average dislocation density and the second accounts for the distribution of dislocation densities. Evaluation of correlation between carbon content and such coefficients in the models as activation energy for self diffusion, activation energy for recrystallization, grain boundary mobility, recovery coefficient etc. was the main objective of the work. In consequence, the model which may be used for simulation of hot forming processes for steels with various chemical compositions, is proposed.

Carrier mobility in polycrystalline semiconductors

This letter presents a modified version of the grain boundary barrier model for polycrystalline semiconductors which takes into account the carrier transport in the bulk of the grain and the dynamic process of capture and release of free carriers by the grain boundary traps.

Influence of grain boundaries on the vibrational properties of silver nanowires

Metal and semiconductor nanowires (NWs) have been widely employed as the building blocks of the nanoelectromechanical systems, which usually acted a resonant beam. Recent researches reported that nanowires are often polycrystalline, which contains grain boundaries (GBs) that transect the whole nanowire into a bamboo like structure. Based on the larger-scale molecular dynamics (MD) simulations, a comprehensive investigation of the influence from grain boundaries on the vibrational properties of doubly clamped Ag NWs is conducted. It is found that, the presence of grain boundary will result in significant energy dissipation during the resonance of polycrystalline NWs, which leads a great deterioration to the quality factor. Further investigation reveals that the energy dissipation is originated from the plastic deformation of polycrystalline NWs in the form of the nucleation of partial dislocations or the generation of micro stacking faults around the GBs and the micro stacking faults is found to keep almost intact during the whole vibration process. Moreover, it is observed that the closer of the grain boundary getting to the regions with the highest strain state, the more energy dissipation will be resulted from the plastic deformation. In addition, either the increase of the number of grain boundaries or the decrease of the distance between the grain boundary and the highest strain state region is observed to induce a lower first resonance frequency. This work sheds lights on the better understanding of the mechanical properties of polycrystalline NWs, which benefits the increasing utilities of NWs in diverse nano-electronic devices.

Analysis and prediction of the critical current density across [001]-tilt YBa2Cu3O7- grain boundaries of arbitrary misorientation angles

A qualitative analysis of the expected dilatation strain field in the vicinity of an array of grain-boundary (GB) dislocations is presented. The analysis provides a basis for the prediction of the critical current densities (jc) across low-angle YBa2Cu3O7- (YBCO) GBs as a function of their energy. The introduction of the GB energy allows the extension of the analysis to high-angle GBs using established models which predict the GB energy as a function of misorientation angle. The results are compared to published data for jc across [001]-tilt YBCO GBs for the full range of misorientations, showing a good fit. Since the GB energy is directly related to the GB structure, the analysis may allow a generalization of the scaling behavior of jc with the GB energy. © 1995 The American Physical Society.

Graphene ripples generated by grain boundaries in highly ordered pyrolytic graphite

Atomic scale periodic ripples that extend for several nanometers on the surface of adjacent graphitic grains have been observed for the first time on highly ordered pyrolitic graphite by UHV-STM. The ripples emanate from a grain boundary, and are explained in terms of a mechanical deformation due to the elastic strain accumulated along the GB, which is relieved out-of-plane in the topmost graphene layer. We present a molecular dynamics model that accounts for the formation of similar ripples as result of the lattice mismatch induced by two different grain orientations.

Energetic and thermal properties of tilt grain boundaries in graphene/hexagonal boron nitride heterostructures

Graphene/hexagonal boron nitride (G/h-BN) heterostructure has attracted tremendous research efforts owing to its great potential for applications in nano-scale electronic devices. In such hybrid materials, tilt grain boundaries (GBs) between graphene and h-BN grains may have unique physical properties, which have not been well understood. Here we have conducted non-equilibrium molecular dynamics simulations to study the energetic and thermal properties of tilt GBs in G/h-BN heterostructures. The effect of misorientation angles of tilt GBs on both GB energy and interfacial thermal conductance are investigated.

A Method for the Deposition of Transparent Conducting Thin-Films of Tin Oxide

A modified method has been developed for the deposition of transparent semiconducting thin films of tin oxide, involving the chemical vapour phase oxidation of tin iodide. These films show sheet resistances greater than 100 Ω/□ and an average optical transmission in the visible range exceeding 80%. The method avoids uncontrolled contamination, resulting in better reproducibility of the films. The films showed direct and indirect transitions and the possibility of an indirect forbidden transition. X-ray diffraction studies reveal that the films are polycrystalline. The low mobility values of the films have been attributed to the grain boundary scattering effect.