淬火分配处理对高碳钢组织、力学性能和磨损性能的影响

The present work employed the X-ray diffraction, scanning electron microscopy, electron backscattered diffraction, and electron probe microanalysis techniques to identify the microstructural evolution and mechanical and abrasive behavior of high carbon steel during quenching-partitioning treatment with an aim to enhance the toughness and wear resistance of high carbon steel. Results showed that, with the increase in partitioning temperature from 250 to 400°C, the amount of retained austenite (RA) decreased resulting from the carbide precipitation effect after longer partitioning times. Moreover, the stability of RA generally increased because of the enhanced degree of carbon enrichment in RA. Given the factors affecting the toughness of high carbon steel, the stability of RA associated with size, carbon content, and morphology plays a significant role in determining the toughness of high carbon steel. The analysis of the wear resistance of samples with different mechanical properties shows that hardness is the primary factor affecting the wear resistance of high carbon steel, and the toughness is the secondary one.     

Microstructure and properties of high emissivity coatings

A new coating on lining in industrial furnace for energy saving has been developed. Properties and microstructure of the coatings were revealed by emissivity instrument,X-ray diffraction (XRD),transmission electron microscope (TEM) and scanning electron microscope (SEM),respectively. The result indicates that the emissivity of coatings is higher than 0.90 and the thickness of coatings is about 200 μm. ZrO₂,Cr₂O₃ and SiC in the coating benefit practical applications of coatings at high temperature with durable high emissivity and the continuous structure between the coatings and the substrate makes the coatings high cohesion and excellent adhesion for both specimens with and without sintering at high temperature. Result from laboratory experiment shows that the heating speed of specimen with coating is higher than that of controlled specimen and the temperature increases 30℃ during the heating. The average temperature drop of specimen with coatings has a 13.5% improvement in the cooling speed. The application of coatings on the checker brick in a blast furnace of 1750m3 indicates that the coating causes the blast temperature to an average increase of 28℃,reduces the fluctuation of blast temperature before the blowing-in and leads to a fuel saving of 10% approximately.     

The Microstructure of Graphite Spherulites in Cast Iron

The microstructure of graphite spherulites (G.S.) in Ce addition ductile cast iron was carried out using transmission electron microscopy (TEM) techniques. The structral characterization of the graphites is as following: there are platelets growing along the periphery as well as fan-like structure formed from platelet aggregates in the diameter section of spherulite, in which most of the platelets are with sizes ranging from several to tens nm in radial; the [001] direction of the platelets would have a tend to parallel to radial of the G. S. and meanwhile, they also a small misorientation deviated from the radial among the platelets each other. It shows that the anisotropy of graphites has been restrained by adding Ce element in cast iron and the structural characterization of the G. S. is consistent with the Double' s model of the conical helixes formed in helical growing and branching.     

Intergrowth texture in Au-Ag-Te minerals from Sandaowanzi gold deposit, Heilongjiang Province: Implications for ore-forming environment

Sandaowanzi gold deposit,Heilongjiang Province,is the only single telluride type gold deposit so far documented in the world,in which 90% of gold is hosted in gold-silver telluride minerals.Optical microscope observation,scanning electron microscope,electron probe and X-ray diffraction analysis identified abundant intergrowth textures in the Au-Ag-Te minerals,typified by sylvanite-hosting hessite crystals and hessite-hosting petzite crystals.The intergrown minerals and their chemistry are consistent,and the hosted minerals are mostly worm-like or as oriented stripes,evenly distributed in the hosting minerals,with clear and smooth interfaces.These suggest an exsolution origin for the intergrowth texture.With reference to the phase-transformation temperature derived from synthesis experiments of tellurides,the exsolution texture of Au-Ag-Te minerals implies that the veined tellurides formed at 150-220℃.The early stage disseminated tellurides formed at log f(Te 2) from 13.6 to 7.8,log f(S 2) from 11.7 to 7.6,whereas the late stage veined tellurides formed at log f(Te 2) ranging from 11.2 to 9.7 and log f(S 2) from 16.8 to 12.2.     

Preparation and bioactivity of sol-gel macroporous bioactive glass

Bioactive glass is well known for its ability of bone regeneration, and sol-gel bioactive glass has many advantages compared with melt-derived bioactive glass. 3-D scaffold prepared by the sol-gel method is a promising substrate material for bone tissue engineering and large-scale bone repair. Porous sol-gel glass in the CaO-SiO₂-P₂0₅ system with macropores larger than 100 μm was prepared by the addition of stearic acid as a pore former. The diameter of the pore created by the pore former varied from 100 to 300 μm. The formation of a hydroxyapatite layer on the glass was analyzed by studying the surface of the porous glass by scanning electron microscopy, energy dispersive spectroscopy, X-ray diffraction, and Raman spectra after they had been immersed in simulated body fluid (SBF) for some time, and the porous glass shows good bioactivity.     

Microstructure, crystallography and nucleation mechanism of NANOBAIN steel

The microstructure of bainite ferrite in NANOBAIN steel transformed at different temperatures was investigated by scanning electron microscopy, transmission electron microscopy, electron back-scattered diffraction, and vickers hardness tester in detail. It is found that the average width of bainitic ferrite (BF) plates can be refined to be thinner with the reduction of temperature (473–573 K), and the bainitic ferrite plates can reach up to 20–74 nm at 473 K. Crystallographic analysis reveals that the bainitic ferrite laths are close to the Nishiyama-Wasserman orientation relationship with their parent austenite. Temperature shows a significant effect on the variant selection, and a decrease in temperature generally weakens the variant selection. Thermodynamic analyses indicates that the Lacher, Fowler and Guggenheim (LFG) model is more suitable than the Kaufman, Radcliffe and Cohen (KRC) model dealing with NANOBAIN steel at a low temperature range. The free energy change ΔGγ→BF is about ?1500 J·mol?1 at 473 K, which indicates that nucleation in NANOBAIN steel is the shear mechanism. Finally, the formation of carbon poor regions is thermodynamically possible, and the existence of carbon poor regions can greatly increase the possibility of the shear mechanism.     

Exsolution microstructures in ultrahigh-pressure rocks: Progress, controversies and challenges

Exsolution microstructures in minerals of rocks from orogenic belts played an important role in recognition of ultrahigh-pressure （UHP） metamorphism in their host rocks by defining the subduction depth and improving our understanding of the dynamics during the subduction and exhumation of UHP rocks. However, it is a challenging scientific topic to distinguish the ＇exsolution microstructures＇ from the ＇non-exsolution microstructures＇ and decipher their geological implications. This paper describes the subtle differences between the ＇exsolution microstructures＇ and the ＇non-exsolution microstructures＇ and summarizes the progress in studies of exolution microstructures from UHP rocks and mantle rocks of ultra-deep origin. We emphasize distinguishing the ＇exsolution microstructures＇ from the ＇non-exsolution microstructures＇ based on their geometric topotaxy and chemistry. In order to decipher correctly the exsolution microstructures, it is crucial to understand the changes of chemistry and habits of host minerals with pressure and temperature, Therefore, it is important to combine observations of exsolution microstructure in natural rocks with experimental results at high pressure and temperature and results of micro-scale analyses. Such studies will improve our understanding of the UHP metamorphism and cast new lights on solid geoscience issues such as deep subduction of continental crusts and crust-mantle interactions.     

Characterization of 17-4PH stainless steel powders produced by supersonic gas atomization

17-4PH stainless steel powders were prepared using a supersonic nozzle in a close-coupled gas atomization system. The characteristics of powder particles were carried out by means of a laser particle size analyzer, scanning electron microscopy (SEM), and the X-ray diffraction (XRD) technique. The results show that the mass median particle diameter is about 19.15 μm. Three main types of surface microstructures are observed in the powders:well-developed dendrite, cellular, and cellular dendrite structure. The XRD measurements show that, as the particle size decreases, the amount of fcc phase gradually decreases and that of bcc phase increases. The cooling rate is inversely related to the particle size, i.e., it decreases with an increase in particle size.     

Petrographic and geochemical characterization of seep carbonate from Alaminos Canyon,Gulf of Mexico

Seep carbonates were collected from the Alaminos Canyon lease area, Gulf of Mexico. The carbonates are present as slabs and blocks. Bivalve shell and foraminifer are the dominant bioclasts in carbonate. Pores are common and usually filled with acicular aragonite crystals. XRD investigation shows that aragonite is the dominate mineral （98%）. Peloids, clotted microfabirc and botryoidal aragonite are developed in carbonate and suggest a genesis linked with bacterial degradation of the hydrocarbons. The δ^13C value of bioclasts in carbonate is from -4.9‰ to -0.6‰, indicating that the carbon source is mainly from sea water as well as the small portion incorporation of the seep hydrocarbon. The microcrystalline and sparite aragonite shows the δ^13C value from -31.3‰ to -23.4‰, suggesting that their carbon is derived mainly from microbial degradation of crude oil. ^14C analyses give the radiocarbon age of about 10 ka. Rare earth elements （REE） analyses of the 5% HNO3-treated solution of the carbonates show that the total REE content of the carbonates is low, that is from 0.752 to 12.725 μg·g^-1. The shale-normalized REE patterns show significantly negative Ce anomalies. This suggests that cold seep carbonate is most likely formed in a relatively aerobic environment.     

On the measurement of slip length for liquid flow over super-hydrophobic surface

To design a surface with large slip or larger drag reduction is a pop issue in the fields of liquid transporting and body swimming. In this context, it is a crucial problem to measure the slip length for these surfaces. Here we propose a novel method by using rheometer for this objective. This method is implemented by designing the distribution of the super-hydrophobic area on the sample. Using this method, a slip length of 40 μm for 70 wt% glycerin flow over a super-hydrophobic surface with stripe structure （the period, width and height of ridges are 150 μm, 40 μm and 65 μm, respectively） is measured. The result shows that the slip length measured using this method is in good agreement with former results measured by other methods. This method is fit for measuring the slip length of super-hydrophobic surface whose structure ranges from microto nano-scale.     

Quartz and clinoenstatite exsolutions in clinopyroxene of garnet-pyroxenolite from the North Dabie Mountains, eastern China

The exsolution lamellae of quartz and clinoen-statite are idenfied in diopside of garnet-pyroxenolite from the North Dabie Mountain by transmission electron microscopy, which is interpreted that the lamellae are originally exsolved from a former ultra-high-pressure clinopyroxene due to decreasing of pressure. Study of petrography shows that there is compositional zoning hi the diopside itself. It is implied that the garnet-pyroxenolite had undergone intensive high-temperature granulite fades and high-amphibolitic fades retrogressive metamorphism, while the peridotite (the garnet-pyroxenolite's host rock) emplaced the crust     

电子探针中的Map图在矿物出溶体中的应用--以石榴石橄榄岩中橄榄石的矿物出溶体为例

以中国苏鲁石榴石橄榄岩和瑞士Arami石榴石橄榄岩的橄榄石中针状出溶体的研究为例,运用电子探针中的Map分析技术,很好地解决了图像与成分的对应性问题,使得测试结果真实、可信.为矿物出溶体的研究提供了新的思路.     

Discovery of ultrahighpressure magnesite-bearing garnet lherzolite (>3.8 GPa) in the Altyn Tagh,Northwest China

Magnesite-bearing garnet lherzolite from the Altyn Tagh, associated with garnet pyroxenite, and garnet-bearing felsic gneiss, crops out as lenses in Proterozoic gneiss about 100 km east of the Jianggelasayi River. The garnet lherzolite, together with the eclogite in western Jianggelasayi, composes a high-pressure to ultrahigh- pressure metamorphic belt in the southern margin of the Altyn Tagh. Parageneses of minerals from magnesite-bearing garnet lherzolite indicate that the rock evolved a multi-stage metamorphism. The peak-stage metamorphism produces an assemblage of Grt+Ol+Opx+Cpx±Mgs, in which Al₂O₃ content of Opx is very low (0.30 — 0.66wt%). The calculated P-T condition of the peak stage is 3.8—5.1GPa and 880—970℃, some exsolution rods of clinopyroxene and rutile occur in the Grt and magnesite is rimed by dolomite and orthopyroxene, all implying that the peak stage was a UHP metamorphic process. Together with regional geological studies, isotopic dating and the discovery of coesite inclusions in zircon separates from felsic gneiss from the northern margin of the Qaidam Basin, the presence of a very long UHP metamorphic belt in northwest China is suggested.     

太行山东麓煤田含煤地层中铵伊利石矿物特征

 通过X射线衍射分析(XRD)、傅里叶红外光谱分析(IR)和X射线光电子能谱分析(XPS)等测试手段,发现太行山东麓煤田部分煤层及其夹矸中含有铵伊利石,并对样品中的铵伊利石进行了详细的矿物学研究。分析结果表明:X射线衍射谱图上,铵伊利石的d₍₀₀₁₎值高于普通伊利石的d₍₀₀₁₎值(1.006nm),(002)衍射峰强度与(003)衍射峰强度相当,而普通伊利石的(002)衍射峰强度为24.4%,约为(003)衍射峰强度的1/3;对铵伊利石晶格常数进行了计算,太行山东麓煤田含煤地层中的铵伊利石空间群属于C2/m,晶胞参数a介于0.52133～0.52774nm之间,b介于0.89814~0.91693nm之间,c介于1.02538~1.05285nm之间,β介于101.127°~101.699°之间,z为2,体积介于0.47611~0.49224nm³之间,密度介于2545~2697e^-/nm³之间;研究区铵伊利石类型为1M多型;红外光谱曲线中,铵伊利石中的NH₄⁺ 变形振动峰范围为1427.58~1431.95 cm^-1;铵伊利石的NH₄⁺ 的N 1s XPS结合能为402.4eV。     

用激光衍射法测量细丝直径简

文中对激光衍射测径法测量细丝直径提出了具体的实现方案,并与普通物理实验中的其他测量细丝直径方法一螺旋测微器法进行结果比对：用激光衍射法测量细丝的直径精度更高,前者为0.000 1 mm,后者为0.001 mm;在单缝衍射实验中,用衍射法测量细丝直径比测量狭缝的宽度对彰显“衍射法测量微小量”更直观.     

GaAs(001)衬底上经双缓冲层生长的Hg_(1-x)Cd_xTe-HgTe超晶格结构

用 X-射线衍射测定了分子束外延 ( MBE)法生长的 Hg1-x Cdx Te- Hg Te超晶格样品在 ( 0 0 1 )附近的扫描徊摆曲线 ,并用动力学理论模拟计算出衍射曲线 ,实验曲线与理论计算基本上相符合 .由实验衍射曲线计算出的超晶格周期长度 ,阱 Hg Te层厚度及垒 Hg1-x Cdx Te层厚度与模拟计算的相一致 .用透射电子显微镜 ( TEM)对同一样品的横截面进行了分析 ,对 Cd Te/Zn Te/Ga As异质结界面失配位错的组态特征进行了研究 .证明用 Cd Te/Zn Te作为双缓冲层比单一的 Cd Te有较好的效果 .截面 TEM高分辨率明场象显示 Hg1-x Cdx Te- Hg Te超晶格的生长较为成功 ,界面较为平整 .由截面 TEM高分辨率明场象观测的周期长度与 X-射线衍射测定的结果相接近     

Influence of crystal materials on the synchrotron X-ray fluorescence analysis: A study of crystal and amorphous clinopyroxene

Synchrotron X-ray fluorescence analyses of crystal and amorphous clinopyroxene were compared. The results showed that using the synchrotron X-ray as a source of energy, the diffraction X-ray of crystal materials will seriously affect the X-ray fluorescence analysis. In order to avoid the influence of diffraction, the best way to solve it is to use the monochromatic source, or to have a collimating slit between sample and Si (Li) detector.     

Isothermal Kinetics of the Pentlandite Exsolution from mss/Pyrrhotite Using Model-Free Method

Introduction Pyrrhotite(Fe,Ni)1?xS and pentlandite(Fe,Ni)9S8areimportant constituents of primary nickel sulfide oredeposits.Pentlandite is invariably associated with pyr-rhotite.At high temperatures(above610℃)(Fe,Ni)1?xS has the NiAs structure and is kno…     

La0.7Sr0.3MnO3外延膜厚度引起的电阻率变化

不同厚度的La0.7Sr0.3MnO3(LSMO)外延薄膜被沉积到立方相的LaA lO3(001)单晶衬底上,XRD测试结果显示,LSMO外延膜的结构是单相的,具有与衬底相同的晶格取向;随着膜厚的增加,LSMO外延膜的晶格经历应变到驰豫的变化.电阻测量显示,应变驰豫的薄膜(较厚的薄膜)有较大的电阻率,这与该膜中缺陷浓度增加有关.此外,也对生长在不同单晶衬底上的LSMO外延膜(厚度相同)的结构和电阻进行了对比研究.