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1.
A new technique has been used for the early stages of crystallization of amorphous materials, like metallic alloys. In situ X-ray diffraction has been performed during the early stages of crystallization of Fe80B20. The samples are resistively heated to 600°C in a customized vacuum chamber. A programmable charge-coupled device detector records simultaneously the evolution of the three phases: -Fe, Fe3B and Fe2B in the minute scale. This is the first in situ X-ray diffraction study of this system in these temperature and time scales. Interesting behaviours have been seen: appearance and disappearance of phases, -Fe supersaturation solution in boron (found for the first time in this compound), and migration of B out of the -Fe matrix. The two-dimensional diffraction pictures show topography irregularities indicating crystallite inhomogeneties.  相似文献   

2.
Crystallization behaviour of amorphous Fe80(C1–x B x )20 alloys, obtained by splat-cooling technique, for x values ranging from zero to unity has been investigated mainly by transmission electron microscopy. The crystalline phase which first appeared in the amorphous matrix was -Fe for all alloys studied. However, the morphology of -Fe phase changed from a spherical shape for low x values to a watch-glass shape for intermediate x values and to dendritic for large x values. The nucleation of -Fe crystals was homogeneous for low x samples while preferred nucleation on edges and surfaces was noted for samples with higher x values. The final volume fraction of -Fe phase before the appearance of the second crystalline phase increased with the increase in x.  相似文献   

3.
Ultrafine Fe-Si-C powders were prepared from mixed gases of SiH4-CH4-Fe(CO)5 using a newly developed thermal-plasma apparatus with a dual-radio-frequency-coupled-plasma-torch system. The phases of the powders prepared were classified into two groups; one composed of -FeSi2 which was prepared by rapid quenching, while the other was composed of -Fe, Fe3Si, Fe5Si3, FeSi, -SiC and amorphous Si, which were prepared by slow quenching. The diameters of these powders were in the range 5–50 nm. The catalytic activities of these powders for Fischer-Tropsch synthesis were examined. The ultrafine -FeSi2 powder was very active for the selective formation of olefin. On the other hand, powders of -Fe, Fe3Si and Fe5Si3 were low in their selectivity but gave high CO conversion. Relations between the plasma conditions for the preparation of ultrafine Fe-Si-C powders and their catalytic properties are discussed.  相似文献   

4.
Crystallization of amorphous Fe78B13Si9 has been investigated using a combination of differential scanning calorimetry (DSC) and conventional and high-resolution transmission electron microscopy. The crystallization mechanisms and crystalline products are sensitive to the annealing temperature. At 450C, crystallization takes place by the growth of b c c -Fe (Si) dendrites, while at 510 and 515C there are three simultaneous reactions to form dendritic b c c -Fe (Si), elliptical crystals of b c t Fe3B and lamellar eutectic spherulites of b c c -Fe (Si) and b c t Fe3B. Quantitative TEM shows that the b c c -Fe (Si) dendrites and b c c -Fe (Si)-b c t Fe3B spherulites both form with constant nucleation and growth rates, in agreement with previous. DSC measurements of an Avrami exponent of 4.  相似文献   

5.
Single crystals of -Al2O3 were implanted with iron ions at room temperature to fluences ranging from 4×1016 Fe cm–2 to 1×1017 Fe cm–2. The microstructure and composition in the implanted region were examined using analytical electron microscopy techniques. Special emphasis was placed on monitoring the microstructural changes which take place during post-implantation annealing. Clusters of metallic -Fe were identified in the specimen after implantation to a dose of 1×1017 Fe cm–2. Analytical electron microscopy of implanted specimens annealed in oxygen revealed the redistribution of the implanted iron and the formation of surface precipitates of -Fe2O3, subsurface precipitates of various forms of spinel, and, in some cases, subsurface precipitates of iron, depending on the annealing temperature. Examination of implanted specimens annealed under reducing conditions revealed the presence of precipitates of -Fe.  相似文献   

6.
The microstructure and properties of NdFeB sintered permanent magnets were analysed by different methods. Samples analysed were sintered and thermally treated. The hard magnetic Nd2Fe14B phase and amorphous neodymium-rich phase were observed by TEM. The neodymium-rich phase contained iron and boron, in elemental and in B2O3 form, which is known as a glass former. At the sintering temperature, Nd2Fe14B and the neodymium-rich phase are supersaturated with iron, which should be dissolved at the annealing temperature to react with neodymium and boron and form additional Nd2Fe14B phase. Iron precipitates of size up to 2 nm were detected in the Nd2Fe14B phase. These superparamagnetic precipitates of -Fe could affect the hard magnetic properties of NdFeB magnets.  相似文献   

7.
The crystallization process of amorphous Fe80B20–x Si x (x=0, 2, and 8) ferromagnetic alloys has been studied by using 57Fe Mössbauer spectroscopy and X-ray diffraction studies. Results for samples heat treated at different temperatures for different times show that the crystallization of Fe80B20–x Si x samples having x=0 and 2 leads to -Fe and t-Fe3B, while for x=8, it leads to -Fe, t-Fe2B, and perhaps Fe-Si. It is further observed that the addition of silicon to the Fe-B system improves the thermal stability of the system.  相似文献   

8.
Inal  O. T.  Keller  L.  Yost  F. G. 《Journal of Materials Science》1980,15(8):1947-1961
Samples of 0.003 in. round Fe80B20 amorphous wires were annealed in vacuo for 1 sec to 8 h periods at 780° C and the crystallinity induced in these wires from this heat treatment was studied through X-ray diffraction and field-ion microscopy. X-ray diffraction studies indicate that complete crystallinity is produced following 1 sec anneal at 780° C. However, the initial product is a primitive-tetragonal Fe3B phase unlike the body-centred tetragonal Fe3B observed in low-temperature isothermal transformation studies with this alloy. The Fe3B phase is seen to persist in the diffraction patterns for annealing durations of up to 15 min. Upon annealing for periods of up to 1 h, an intermediate three-phase structure consisting of -Fe, Fe3B, and Fe2B is seen to result with a gradual decrease in the Fe3B phase corresponding to longer annealing durations. Anneals of more than 1 h at 780° C are seen to result in the disappearance of the Fe3B phase producing a two-phase microstructure consisting of -Fe(b c c) and Fe2B (b c t). Field-ion-microscopy with a pure neon imaging gas at 78 K likewise indicates that existence of a three-stage phase structural change during the isothermal anneals, and the atomic arrangement of the various species are quite readily discernible because of the different symmetries contained in the three distinct phases.  相似文献   

9.
The crystallization behaviour of amorphous Fe93 – x Zr7B x (x = 3, 6, 12 at.%) alloys, the microstructures of the primary crystallization products of stable and metastable phases and the subsequent transformations, have been studied using a combination of differential scanning calorimetry, differential thermal analysis, X-ray diffraction and transmission electron microscopy, including microdiffraction. It has been found that, for x = 3 and 6 at.%, the sole product of primary crystallization is the bcc -Fe phase and the average grain sizes of the crystalline phase were 14 nm and 12 nm for the two alloys, respectively. However, when x = 12 at.%, primary crystallization results in more than one crystalline phase, and a metastable phase with the cubic Fe12Si2ZrB structure is the major crystallization product after the primary crystallization reaction, accompanied by the -Fe phase. The average grain size of this metastable phase was 35 nm for the alloy heated to 883 K at 20 K/min. Isothermal heat treatments at 873 K and 973 K confirm that after being heated for 240 h, this metastable phase transforms into equilibrium phases: bcc -Fe, hcp ZrB2 and probably hcp Fe2Zr. The apparent activation energies for the primary crystallization reaction during continuous heating for these three alloys are 4.4 ± 0.2 eV, 3.5 ± 0.2 eV and 6.9 ± 0.3 eV, respectively.  相似文献   

10.
A detailed study of the process of crystallization in amorphous Fe25Sc75, Fe28 Sc72 and Fe25Sc45Zr30 alloys has been carried out using differential scanning calorimetry, X-ray diffraction and Mössbauer spectroscopic techniques. The complex multi-stage transformation process in Fe25Sc75 and Fe28Sc72 is understood in terms of polymorphous formation of an intermediate metastable crystalline phase of orthorhombic structure (a = 0.521 nm, b = 0.648 nm and c = 1.212 nm) and of likely Sc3Fe stoichiometry, before final eutectic crystallization to stable Fe2Sc and -Sc.  相似文献   

11.
It is suggested that the formation of ice layers should be regarded as a consequence of a loss of stability of the motion of the freezing front. The kinetics of the freezing process is investigated and a stability criterion is obtained.Notation s(t) coordinate of the moving front - L length of the specimen - k moisture conductivity - W moisture content - heat of phase transition - WH amount of unfrozen water - q flow of moisture from the melted zone into the frozen zone - v velocity of motion of the front - Ti temperature - Qi heat flux - i thermal conductivity - ai thermal diffusivity (i=1 is the frozen zone and i=2 is the melted zone) - mass transfer coefficient - TH the initial temperature Translated from Inzhenerno-Fizicheskii Zhurnal, Vol. 39, No. 1, pp. 96–101, July, 1980.  相似文献   

12.
The formation regions of Fe7C3 and Fe3C were determined at high temperature and high pressure in the iron-graphite system. Fe7C3 formed at relatively higher pressures and Fe3C at lower pressures. Both Fe7C3 and Fe3C were isolated from coexisting excess carbon powders by a magnetic method. Fe7C3 had a Curie point of 250° C and a saturation magnetization of 120 emu g–1 at room temperature and Fe3C had those of 210° C and 125 emu g–1. Fe7C3 decomposed to Fe3C and carbon at 600° C, but to -Fe and carbon at 700° C at atmospheric pressure, and Fe3C to -Fe and carbon at 700° C. The substitution of other metals (Cr, Mo and W) for iron in these carbides leads to changes in the thermal stabilities and the magnetic properties.  相似文献   

13.
We study the structure and chemical composition of the reaction products formed in the process of contact of -Fe and 20Kh13 steel with oxygen-containing stagnant lead melts (600–700°C, 3000 h, C O[Pb] (1–4) · 10–5 wt.%). It is shown that a heterogeneous structure is formed in the interaction zone. This structure consists of an external intermediate layer (with low hardness, the same composition as the matrix, and lead accumulated on the grain boundaries) and a thin oxide film (Fe3O4 for -Fe and FeCr2O4 and Cr2O3 for 20Kh13 steel), which separates the intermediate layer from the internal porous suboxide layer of the matrix and blocks the process of penetration of lead into the matrix.  相似文献   

14.
The magnetic state of -Fe particles and the behaviour of nitrogen and zirconium during annealing in Fe96N4 and Fe85.6Zr7.6N6.8 magnetic thin films have been studied by conversion electron Mössbauer spectroscopy for 57Fe. The crystalline phases present in the Fe-N annealed films were -Fe and -Fe4N, and those in the Fe-Zr-N annealed films were -Fe and ZrN. In the Fe-N films annealed below 300°C, about 60% nitrogen is incorporated interstitially into -Fe and the rest is used for the formation of -Fe4N. In the Fe-N film annealed at 500°C, almost all nitrogen participates in the formation of -Fe4N, leading to the grain growth of -Fe particles and an increase in coercive force. The values (291–325 kOe) of internal magnetic field of iron sites in -Fe in the Fe-Zr-N films are much smaller than that (333 kOe) of the iron site in pure -Fe. Even if the Fe-Zr-N films were annealed at 500–700°C, some zirconium and nitrogen is still incorporated substitutionally and interstitially into -Fe, respectively. In particular, the substitutional zirconium depresses the grain growth of -Fe particles, perhaps due to a chemical interaction between zirconium and iron.  相似文献   

15.
Amorphous Fe-17 at %B alloy prepared by a splat-quenching technique was annealed at temperatures ranging from 250 to 500° C for different periods. A time-temperature transformation diagram has been constructed from X-ray diffraction examination of annealed samples. On annealing the alloy at a pressure of 50 kbar, an appreciable retardation of crystallization was observed. The crystalline phase precipitated first from the amorphous matrix at 1 bar. This was -Fe containing a small amount of boron, but at 50 kbar this was a mixture of -Fe(B) and intermetallic phase Fe3B. Under the increased pressure of 100 kbar the mode of the crystallization was further changed and Fe3B became the first precipitating phase. Preferential formation of Fe3B under pressure can be explained assuming a modified dense-random packing model for the amorphous structure.On leave from Institute of Physics, Academia Sinica, Beijing, China.  相似文献   

16.
As a catalyst, partially crystallized Fe78Si12B10 alloy shows a three times higher activity than totally crystallized Fe78Si12B10 in the hydrogenation of CO. High-resolution electron microscopy (HREM) reveals that the catalyst contains a great number of minute (less than 10 nm), highly dispersed -Fe particles which act as the major active component. Many tiny B and Si oxide clusters also exist in the amorphous matrix. After being rinsed by a NaOH solution, the catalyst exhibits a decreasing selectivity to methane due to the dissolution or aggregation of B and Si species. After reaction, the sizes of the active particles increase and an overlayer of B or Si species is found over the surface of some -Fe particles. This coverage is thought to be the primary origin of the deactivation of the catalyst.  相似文献   

17.
Co : Al2O3nanocermets are synthesized by co-reducing Co2+-cations dispersed in a mesoporous AlO(OH) · H2O matrix (amorphous) in a pure H2atmosphere at 850–1150 K. The dispersed Co2+-cations in pores co-reduce to separated Co-particles of controlled size, as small as 50 nm, encapsulated in thin Al2O3films, which are formed in-situ by molecular decomposition of the matrix, 2AlO(OH) · H2O Al2O3+ (2 + 1)H2O. The Al2O3film which coats Co-particles has an amorphous structure. This is possible only if it is extremely thin limited to a thickness of t< 2r c, with r c 1.9 nm the critical size of its nucleation and growth into a stable crystallite. The thin Al2O3surface film supports the formation and existence of Co-particles in a modified FCC or BCC crystal structure. As a result, unusually, large crystallites of an average 100 nm diameter could be observed. Normally, such large particles of pure Co-metal exist in an HCP structure which undergoes a reversible martensitic transformation to FCC structure at 695 K. The results are analyzed and discussed in terms of microstructure, x-ray diffraction and XPS studies of nanocermets prepared under selected conditions.  相似文献   

18.
Fe57 transmission Mössbauer spectroscopy, supported by metallography, SEM and X-ray diffraction analysis, has been employed to study the oxidation of Fe-Ni alloys at 535 and 635° C in 1 atm. of air. With increasing Ni content of the alloy, the composition of the scale changed and the oxidation rate decreased. For an alloy containing 0.9% Ni, the oxide scale produced at 535° C was Fe3O4 covered by a thin outer layer of-Fe2O3, while at 635° C FeO was additionally present as a major phase. The scale formed on a 10% Ni alloy at both 535 and 635° C was similar to that observed for the 0.9% Ni alloy oxidized at 535° C (i.e. of Fe3O4 and-Fe2O3), although the-Fe2O3 layer tended to be relatively thicker. For a 49% Ni alloy, the scale at both 535 and 635° C comprised an inner layer of Ni x Fe3–x O4 (withx0.5, on average) and an outer layer of-Fe2O3, of similar thickness. Finally, on an 83% Ni alloy oxidized at 635° C, the scale consisted of roughly equally thick layers of NiO (next to the metal) and NiFe2O4, and a thin outer covering of-Fe2O3. The decrease in oxidation rate with increasing Ni content of the alloy is discussed briefly in relation to the changing composition of the scale and diffusion in the alloy.  相似文献   

19.
The galssy ferromagnets Fe81.5B14.5Si4 and Fe40Ni40B20 have been studied by Mössbauer spectroucopy from 77.5 up to 650 and 680K, respectively, In the glassy state, the average magnetic hyperfine field decreases with increasing temperature due to a distribution of exchange inter-actions. At low temperatureH(T)/H(0) has a temperature dependence (1 -BT /32 -CT /52) whereB andC are constants, indicative of spin-wave excitations in glassy ferromagnets. The value of B/32) = 0.40 = 0.05 is almost four times larger than those of crystalline iron and nickel. On the other hand, fluctuations of the exchange interaction constant are found to decrease with increasing temperature. The Curie temperaturesT c - 608 K for the glassy Fe81.5B14.5Si4 andT c = 583K for the glassy Fe40Ni40B20 are found to be well defined. AtT close toT c H(T) behaves as a power law with critical exponent = 0.3. The crystallizationT cr glassy Fe81.5B14.5Si4 was found to be 645K. The crystalline material obtained contains three different phases, namely -Fe, Fe2B and Fe-8% Si.  相似文献   

20.
Iron-polyvinylalcohol (Fe-PVA) complexes have been pyrolysed at the temperatures up to 1000 K, and the iron-carbon composites formed have been characterized. The yield of carbon was much higher for the complexes than for PVA alone. The degree of carbon graphitization and the chemical form of iron species were dependent on the pyrolysis temperature. About 30 wt% fine particles of Fe3O4 or -Fe were dispersed in the matrix of amorphous carbon at 800 or 900 K, respectively. At 1000 K, -Fe was partly transformed to Fe3C, and the agglomeration of -Fe was not so significant. At this temperature the carbon was graphitized, which resulted in a lowering of the surface area of the composite. It is suggested that the graphitization proceeds through the mechanism involving the formation and subsequent decomposition of Fe3C. Thus, the use of Fe-PVA complexes achieves a high yield of carbon and a high dispersion of a large amount of iron species throughout the carbon matrix.  相似文献   

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