双辊铸轧高速钢薄带的晶粒细化

主要介绍了W9Mo3Cr4V高速钢在双辊铸轧过程中的晶粒细化。薄带钢在铸轧过程中的冷却时间仅为0．2—0．3s，冷却速度很快，冷却速度已达到100—1000℃／s，因此，在快速凝固的过程中，液体金属获得了较大的过冷度，晶核的临界半径随过冷度的增加而减小，晶粒必然细化。另外，过冷度增大，晶核形核功减小,形核几率增大，也使晶粒细化。     

双辊铸轧高速钢薄带的晶粒细化

主要介绍了W9Mo3Cr4V高速钢在双辊铸轧过程中的晶粒细化.薄带钢在铸轧过程中的冷却时间仅为0.2-0.3 s,冷却速度很快,冷却速度已达到100-1000℃/s,因此,在快速凝固的过程中,液体金属获得了较大的过冷度,晶核的临界半径随过冷度的增加而减小,晶粒必然细化.另外,过冷度增大,晶核形核功减小,形核几率增大,也使晶粒细化.     

双辊铸轧高速钢薄带的晶粒细化

主要介绍了W9Mo3Cr4V高速钢在双辊铸轧过程中的晶粒细化.薄带钢在铸轧过程中的冷却时间仅为0.2-0.3 s,冷却速度很快,冷却速度已达到100-1000℃/s,因此,在快速凝固的过程中,液体金属获得了较大的过冷度,晶核的临界半径随过冷度的增加而减小,晶粒必然细化.另外,过冷度增大,晶核形核功减小,形核几率增大,也使晶粒细化.     

Al-5Ti-0.2C细化剂对7085铝合金形核及过冷度的影响

在7085铝合金凝固过程中添加不同质量分数的Al-5Ti-0.2C细化剂,对比其铸锭凝固组织,并用DSC测定其凝固过程熔体过冷度,探讨Al-5Ti-0.2C细化剂对铝熔体形核与过冷度的影响。研究结果表明:Al-5Ti-0.2C细化剂能够明显细化晶粒,当细化剂质量分数为0.5%时细化效果最好;细化剂质量分数的差异对DSC曲线中的熔化曲线影响较小,而凝固曲线有明显差异;在凝固过程中增大细化剂质量分数,铝熔体形核过冷度与最大过冷度都呈递减趋势,当细化剂质量分数超过0.5%时,过冷度不再有明显递减趋势;Ti C颗粒是铝熔体异质形核的核心,凝固过程中Ti C颗粒的发生团聚,从而增大形核基底颗粒粒度,减小润湿角与临界形核能,最终减小熔体中形核所需过冷度。     

深过冷金属熔体中单晶形成的临界条件

将形核率和晶体生长速度对过冷金属结晶晶粒数的影响用过冷度统一起来，建立了过冷金属结晶晶粒数随金属热力学过冷度变化的理论关系。结果表明：过冷金属的结晶晶粒数随金属热力学过冷度的增大而减小，过冷度增大到一临界值后，过冷金属的结晶晶粒数减小到１；所得到的在过冷金属熔体中形成单晶的理论判据与有关实验结果完全吻合。     

基于均匀形核的金属液滴凝固过程

研究了均匀形核的金属液滴凝固过程,应用渐近分析法求得金属液滴内晶核生长数学模型的渐近解,分析了表面张力、界面动力学参数、初始晶核尺寸和过冷度对晶核界面生长速度、晶核半径以及液滴凝固时间的影响。在一定的过冷条件下,表面张力和界面动力学参数显著减缓了晶核界面生长速度。在凝固开始的很短时间内晶核界面生长速度迅速上升,当速度上升到最大值后,随着晶核半径的增大,界面生长速度逐渐减慢,表面张力和界面动力学参数对晶核生长速度的作用也逐渐减小。过冷度越大,液滴凝固时间越短。经过在开始的瞬变凝固阶段之后,温度场从设定的初始分布迅速地调整为由过冷度、表面张力、界面动力学参数等所确定的特定温度分布。     

基于均匀形核的金属液滴凝固过程

研究了均匀形核的金属液滴凝固过程,应用渐近分析法求得金属液滴内晶核生长数学模型的渐近解,分析了表面张力、界面动力学参数、初始晶核尺寸和过冷度对晶核界面生长速度、晶核半径以及液滴凝固时间的影响.在一定的过冷条件下,表面张力和界面动力学参数显著减缓了晶核界面生长速度.在凝固开始的很短时间内晶核界面生长速度迅速上升,当速度上升到最大值后,随着晶核半径的增大,界面生长速度逐渐减慢,表面张力和界面动力学参数对晶核生长速度的作用也逐渐减小.过冷度越大,液滴凝固时间越短.经过在开始的瞬变凝固阶段之后,温度场从设定的初始分布迅速地调整为由过冷度、表面张力、界面动力学参数等所确定的特定温度分布.     

低钛铝合金晶粒细化的凝固计算

基于单个晶粒生长所形成的成分过冷为邻近的形核颗粒提供形核所需成分过冷的假设，提出晶粒细化的相关晶粒尺寸(RGS)判据。0．03％TiB2细化不同含钛量的铝合金的试验数据拟和出的形核过冷度与试验测量结果较一致。分析发现成分过冷区初期其形成的速率正比于抑制生长因子Q，成分过冷参数P可作为柱状晶向等轴晶转变的判据。对于使用强形核颗粒合金的晶粒尺寸可用直接使用抑制生长因子Q来衡量，而弱形核颗粒使用RGS可能更准确一些。     

深过冷Fe-30%Co合金的组织演化

采用熔融玻璃净化与循环过热相结合的方法，使原子分数Fe-30%Co合金获得了高达457K的大过冷度.系统考察了合金凝固组织随过冷度的演化规律.发现合金的凝固组织随过冷度的增大存在两次细化和一次粗化过程, 即在小过冷度范围内粗大树枝晶向粒状晶的转变和中等过冷度下局域定向枝晶的细化，而在大过冷度范围内随着亚稳枝晶核数目的增加,存在一个明显晶粒粗化的过程.     

微观组织参数及工艺条件对430不锈钢凝固显微结构的影响

在多元合金CAFE模型的基础上,分析了微观组织参数(形核密度、高斯分解参数、Gibbs-Thomson系数等)与430不锈钢凝固过程中晶粒形貌的复杂关系,以及过热度与冷却强度等工艺参数对凝固组织的影响.研究发现,晶粒尺寸和柱状晶向等轴晶转变不仅与体最大形核过冷度有关,也受体形核密度的影响.高斯分解参数和Gibbs-Thomson系数增大时,一次枝晶间距减小,等轴晶范围增大;但当它们增加至一定范围后,其对显微结构的影响逐渐变得不明显.过热度或冷却强度增大时,等轴晶范围减小,但一次枝晶间距的变化不明显.     

Markedness and its Interpretation in Language Use

Language markedness is a common phenomenon in languages, and is reflected from hearing, vision and sense, i.e. the variation in the three aspects such as phonology, morphology and semantics. This paper focuses on the interpretation of markedness in language use following the three perspectives, i.e. pragmatic interpretation, psychological interpretation and cognitive interpretation, with an aim to define the function of markedness.     

Lower Paleozoic oil relationships within Williston Basin, Canada

The Williston Basin is a significant petroleum province, containing oil production zones that include the Middle Cambrian to Lower Ordovician, Upper Ordovician, Middle Devonian, Upper Devonian and Mississippian and within the Jurassic and Cretaceous. The oils of the Williston Basin exhibit a wide range of geochemical characteristics defined as "oil families", although the geochemical signature of the Cambrian Deadwood Formation and Lower Ordovician Winnipeg reservoired oils does not match any "oil family". Despite their close stratigraphic proximity, it is evident that the oils of the Lower Palaeozoic within the Williston Basin are distinct. This suggests the presence of a new "oil family" within the Williston Basin. Diagnostic geochemical signatures occur in the gasoline range chromatograms, within saturate fraction gas chromatograms and biomarker fingerprints. However, some of the established criteria and cross-plots that are currently used to segregate oils into distinct genetic families within the basin do not always meet with success, particularly when applied to the Lower Palaeozoic oils of the Deadwood and Winnipeg Formation.     

An Analysis of Catherine＇s Character——Wuthering Heights

Wuthering Heights, Emily Bronte＇s only novel, was published in December of 1847 under the pseudonym Ellis Bell. The book did not gain immediate success, but it is now thought one of the finest novels in the English language. Catherine is the key character of this masterpiece, because everybody and everything center on her though she had a short life. We can understand this masterpiece better if we know Catherine well.     

Features of Women's language

Language is a means of verbal communication. People use language to communicate with each other. In the society, no two speakers are exactly alike in the way of speaking. Some differences are due to age, gender, statue and personality. Above all, gender is one of the obvious reasons. The writer of this paper tries to describe the features of women＇s language from these perspectives： pronunciation, intonation, diction, subjects, grammar and discourse. From the discussion of the features of women＇s language, more attention should be paid to language use in social context. What＇s more, the linguistic phenomena in a speaking community can be understood more thoroughly.     

Characterization of Ordovician carbonate reservoirs, southeastern Saskatchewan, Canada

The discovery of the prolific Ordovician Red River reservoirs in 1995 in southeastern Saskatchewan was the catalyst for extensive exploration activity which resulted in the discovery of more than 15 new Red River pools. The best yields of Red River production to date have been from dolomite reservoirs. Understanding the processes of dolomitization is, therefore, crucial for the prediction of the connectivity, spatial distribution and heterogeneity of dolomite reservoirs.The Red River reservoirs in the Midale area consist of 3～4 thin dolomitized zones, with a total thickness of about 20 m, which occur at the top of the Yeoman Formation. Two types of replacement dolomite were recognized in the Red River reservoir: dolomitized burrow infills and dolomitized host matrix. The spatial distribution of dolomite suggests that burrowing organisms played an important role in facilitating the fluid flow in the backfilled sediments. This resulted in penecontemporaneous dolomitization of burrow infills by normal seawater. The dolomite in the host matrix is interpreted as having occurred at shallow burial by evaporitic seawater during precipitation of Lake Almar anhydrite that immediately overlies the Yeoman Formation. However, the low δ18O values of dolomited burrow infills (-5.9‰～ -7.8‰, PDB) and matrix dolomites (-6.6‰～ -8.1‰, avg. -7.4‰ PDB) compared to the estimated values for the late Ordovician marine dolomite could be attributed to modification and alteration of dolomite at higher temperatures during deeper burial, which could also be responsible for its 87Sr/86Sr ratios (0.7084～0.7088) that are higher than suggested for the late Ordovician seawaters (0.7078～0.7080). The trace amounts of saddle dolomite cement in the Red River carbonates are probably related to "cannibalization" of earlier replacement dolomite during the chemical compaction.     

Design and analysis of generic LBS application developing platform

Location based services is promising due to its novel working style and contents.A software platform is proposed to provide application programs of typical location based services and support new applications developing efficiently. The analysis shows that this scheme is easy implemented, low cost and adapt to all kinds of mobile nework system.     

橡胶颗粒沥青混合料低温抗裂性试验研究

以AC-13级配为基础,将橡胶颗粒代替部分集料掺入混合料中,以低温弯曲试验为评价方法对不同橡胶颗粒掺量下沥青混合料的低温抗裂性进行研究,并引入应变能密度值对混合料的低温抗裂性进行综合评价.试验结果表明:橡胶颗粒沥青混合料试件的破坏微应变均超过2 300,满足冬寒区的技术指标;无论是否掺加橡胶颗粒,随着温度的下降,沥青混合料破坏时的最大弯拉强度增大,弯拉应变降低,劲度模量增大;弯曲应变能密度在胶粒掺量为1%左右时具有较大的弯曲应变能密度值,此时橡胶颗粒沥青混合料具有较好的低温抗裂性.     

低渗透非均质砂岩油藏启动压力梯度研究

理论推导与室内实验相结合,建立了低渗透非均质砂岩油藏启动压力梯度确定方法。首先借助油藏流场与电场相似的原理,推导了非均质砂岩油藏启动压力梯度计算公式。其次基于稳定流实验方法,建立了非均质砂岩油藏启动压力梯度测试方法。结果表明:低渗透非均质砂岩油藏的启动压力梯度确定遵循两个等效原则。平面非均质油藏的启动压力梯度等于各级渗透率段的启动压力梯度关于长度的加权平均;纵向非均质油藏的启动压力梯度等于各渗透率层的启动压力梯度关于渗透率与渗流面积乘积的加权平均。研究成果可用于有效指导低渗透非均质砂岩油藏的合理井距确定,促进该类油藏的高效开发。     

On Tragic Consciousness In The Works By Ernest Hemingway

As an American modern novelist who were famous in the literary world, Hemingway was not a person who always followed the trend but a sharp observer. At the same time, he was a tragedy maestro, he paid great attention on existence, fate and end-result. The dramatis personae's tragedy of his works was an extreme limit by all means tragedy on the meaning of fearless challenge that failed. The beauty of tragedy was not produced on the destruction of life, but now this kind of value was in the impact activity. They performed for the reader about the tragedy on challenging for the limit and the death.     

Quantitative trait loci （QTLs） for quality traits related to protein and starch in wheat

Quality traits in wheat （Triticum aestirum L.） were studied by quantitative trait locus （QTL） analysis in a recombinant inbred line （RIL） population, a set of 131 lines derived from Chuan 35050 × Shannong 483 cross （ChSh）. Grains from RILs were assayed for 21 quality traits related to protein and starch. A total of 35 putative QTLs for 19 traits with a single QTL explaining 7.99-40.52% of phenotypic variations were detected on 10 chromosomes, 1D, 2A, 2D, 3B, 3D, 5A, 6A, 6B, 6D, and 7B. The additive effects of 30 QTLs were positive, contributed by Chuan 35050, the remaining 5 QTLs were negative with the additive effect contributed by Shannong 483. For protein traits, 15 QTLs were obtained and most of them were located on chromosomes 1 D, 3B and 6D, while 20 QTLs for starch traits were detected and most of them were located on chromosomes 3D, 6B and 7B. Only 7 QTLs for protein and starch traits were co-located in three regions on chromosomes 1D, 2A and 2D. These protein and starch trait QTLs showed a distinct distribution pattern in certain regions and chromosomes. Twenty-two QTLs were clustered in 6 regions of 5 chromosomes. Two QTL clusters for protein traits were located on chromosomes 1D and 3B, respectively, three clusters for starch traits on chromosomes 3D, 6B and 7B, and one cluster including protein and starch traits on chromosome 1D.