TA1/Q235钢复合板累积叠轧焊界面特性

对TA1/Q235钢复合板累积叠轧焊进行了研究.研究结果表明:采用累积叠轧焊方法能够制备出结合性能较好的钛/碳钢复合板,其结合强度随着累积变形量与首道次变形量的增加而提高,叠轧过程中经磨床打磨与喷丸处理获得洁净、新鲜并具有一定加工硬化程度的结合界面,会促进复合板结合强度的提高.800℃以下热轧后,Q235钢的组织呈明显的条带状;而850℃以上热轧后,Q235钢条带状变形组织逐渐转化为等轴状,界面附近的Q235钢脱碳,出现明显的排列整齐且粗大的铁素体晶粒带.钛侧的组织主要有等轴α组织和魏氏α组织.综合考虑轧制温度对钛与Q235钢组织与界面结合性能的影响,累积叠轧温度应控制在800～850℃之间.     

TA2-Q235B爆炸复合板钢侧组织特征

借助光学显微镜、电子背散射衍射和扫描电子显微镜等测试技术和手段,系统地研究热处理温度对TA2--Q235B爆炸复合板钢侧组织转变的影响,并分析了其形成机理.结果表明:在热处理过程中,钢侧界面组织发生脱碳,形成完全由铁素体组织组成的脱碳层,这些铁素体没有织构特征;当热处理温度在850℃及以下时,钢侧界面组织在靠近波头漩涡的地方发生异常长大,形成粗大的铁素体;当热处理温度在900℃及以上时,钢侧界面组织在钛钢复合界面上发生异常长大,产生柱状的铁素体组织.这些组织的形成受到碳元素的扩散和钢侧基体组织相变的共同作用.热处理过程中,界面产生的TiC在界面上分布不均,随温度升高,在界面局部富集,从而加速了碳元素向界面的扩散.     

25Cr5MoA钢/微合金钢/Q235钢的复合轧制

将25Cr5MoA钢/微合金钢/Q235钢板复合板坯加热到轧制温度950～1100℃,经保温后轧制1道次,压下量为50%～65%,制成25Cr5MoA钢/微合金钢/Q235钢热轧复合板试样.利用剪切实验方法测定了复合板材的界面结合强度,通过光学显微镜观察结合界面的组织.结果表明:当轧制温度为1000～1100℃时,25Cr5MoA钢/微合金钢/Q235钢能有效复合;压下量对25Cr5MoA钢/Q235钢复合板界面结合强度有一定的影响,当压下量达到一定程度后,随着压下量的增加,复合板的结合强度逐渐降低;轧制温度对25Cr5MoA钢/微合金钢/Q235钢复合板界面结合强度影响很大,在道次压下量一定的情况下,随着轧制温度的升高,复合板的结合强度逐渐升高.在1100℃的轧制温度和50%压下量的轧制条件下结合强度达到最大值.     

Q235钢CSP轧制时动态再结晶行为研究

利用Gleeble-1500热模拟实验机研究Q235钢连铸坯CSP轧制时在高温变形过程中的动态再结晶行为.结果表明,在高变形温度和低应变速率条件下Q235钢易发生动态再结晶;在回归相应的数学模型后,建立了Q235钢的热变形方程式.对Q235钢连铸坯热变形后的组织进行分析,发现奥氏体发生动态回复后转变的铁素体组织中也有动态再结晶晶粒.     

25Cr5MoA/Q235钢复合板的结合性能

将25Cr5MoA/Q235钢板复合板坯加热到800～1 100 ℃,经保温后轧制1道次,压下量为50%～70%,制成25Cr5MoA/Q235钢热轧复合板试样. 用材料力学性能试验机测试复合板试样复合界面的剪切强度,用光学显微镜和扫描电镜观察界面的组织. 结果表明:当轧制温度在900～1 000 ℃时,有利于25Cr5MoA/Q235钢的复合;道次压下量对25Cr5MoA/Q235钢复合板界面结合强度影响非常大,道次压下量大,有利于形成更多洁净、活化的新生表面,并且可以细化晶粒,提高复合板的结合强度;金属组织中晶粒的梯度变化,有利于提高双金属复合材料的结合强度.     

变形温度对细晶高强IF钢应力-应变曲线及显微组织的影响

以细晶高强IF钢为研究对象,在东北大学轧制技术及连轧自动化国家重点实验室MMS-300热力模拟实验机上,测定了在变形速率为10 s-1,真应变为0.5,变形温度分别为750、800、850、900、950、1 000 ℃时的应力应变曲线.通过实验发现,钢的应力应变曲线为动态回复型,不随温度而变化;流变应力随着变形温度的增加而下降;通过显微组织观察发现,随变形温度的降低,晶粒变细.     

Q690低碳微合金钢热变形微观组织演变及加工图

利用Gleeble-3800数字控制热/力模拟试验机研究了Q690低碳微合金钢在变形温度850～1150℃,应变速率0.01～30s-1条件下的高温单道次压缩变形行为.建立了基于动态材料模型(DMM)的加工图,结合OM观察变形体微观组织确定了该钢种的高温热变形机制.结果表明:应变量0.7及以下的加工图中包含2个峰区(1 000～1 120℃,0.01～0.37s-1和1 100～1 150℃,3.16～30s-1)和3个加工失稳区(850～900℃,0.01～0.32s-1和850～900℃,10～30s-1以及1 000～1 085℃,1～30s-1).应变量超过0.8的加工图包含2个峰区(1 025～1 100℃,0.01～0.38s-1和1 100～1 150℃,3～30s-1),失稳区为低温(850～900℃,0.01～30s-1)以及应变速率1s-1以上的中低温度(850～1 100℃)范围,在这两个峰区峰值点附近的热变形显微组织为均匀的完全动态再结晶组织,因此,这两个区域均适合Q690钢的热加工变形.     

中温压力容器钢12CrMo的高温塑性研究

通过热模拟试验对中温压力容器钢12CrMo连铸坯的高温塑性进行研究.在不同的变形温度下采用10-3 s-1的应变速率对试样进行拉伸变形,测量拉伸断口的面缩率,并对拉伸断口的显微组织和析出物进行分析.结果表明, 当变形温度高于900 ℃时,试样在拉伸过程中发生动态再结晶,其面缩率大于85%,表现出优良的高温塑性;当变形温度为850 ℃时,有大量细小的AlN在12CrMo钢中弥散析出,其尺寸约为10 nm;当变形温度降至800 ℃时,大量的先共析铁素体沿奥氏体晶界析出,形成网状结构,试样面缩率降至36%,12CrMo钢的高温塑性显著下降.     

40CrNiMo钢的热变形组织变化

利用G leeble 1500热/力学模拟实验机,对40CrN iMo钢进行双道次热模拟单向压缩试验。变形温度分别为710℃、760℃、950℃,变形速率为0.5~30 s-1,变形量为0.05~0.4,道次间停留时间为1~100 s。分析了钢热变形组织特征,结果表明钢在950℃温度变形过程中发生奥氏体动态再结晶,在760℃温度变形过程中,应变奥氏体诱发铁素体析出,而在710℃温度变形过程中,应变奥氏体加速了铁素体析出。     

Q345钢低温形变微纳米级铁素体制备实验研究

为了充分激发钢材自主控制晶粒的潜力,以Q345为研究对象,采用Gleeble-3500热模拟试验机进行低温大塑性平面变形实验,研究了低温大变形下制备微纳米级晶粒的工艺条件.实验中变形温度为500～700℃,应变速率为0.01～1 s-1,并借助数值模拟技术确定出了单道次平面压缩实验最大可产生4.0以上的塑性应变.根据实验金相分析结果,得出了Q345钢低温大变形下铁素体晶粒细化以动态再结晶为主和晶粒尺寸与Z因子的关系,且获得的铁素体晶粒尺寸小于1μrn.实验结果表明,Q345钢低温大塑性形变制备微纳米级铁素体组织是可行的.     

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.     

An Index mechanism for multi-scale view in spatial databases

There are numerous geometric objects stored in the spatial databases. An importance function in a spatial database is that users can browse the geometric objects as a map efficiently. Thus the spatial database should display the geometric objects users concern about swiftly onto the display window. This process includes two operations:retrieve data from database and then draw them onto screen. Accordingly, to improve the efficiency, we should try to reduce time of both retrieving object and displaying them. The former can be achieved with the aid of spatial index such as R-tree, the latter require to simplify the objects. Simplification means that objects are shown with sufficient but not with unnecessary detail which depend on the scale of browse. So the major problem is how to retrieve data at different detail level efficiently. This paper introduces the implementation of a multi-scale index in the spatial database SISP (Spatial Information Shared Platform) which is generalized from R-tree. The difference between the generalization and the R-tree lies on two facets: One is that every node and geometric object in the generalization is assigned with a importance value which denote the importance of them, and every vertex in the objects are assigned with a importance value,too. The importance value can be use to decide which data should be retrieve from disk in a query. The other difference is that geometric objects in the generalization are divided into one or more sub-blocks, and vertexes are total ordered by their importance value. With the help of the generalized R-tree, one can easily retrieve data at different detail levels.Some experiments are performed on real-life data to evaluate the performance of solutions that separately use normal spatial index and multi-scale spatial index. The results show that the solution using multi-scale index in SISP is satisfying.     

A computer generator for randomly layered structures

AcomputergeneratorforrandomlylayeredstructuresYUJia shun1,2,HEZhen hua2(1.TheInstituteofGeologicalandNuclearSciences,NewZealand;2.StateKeyLaboratoryofOilandGasReservoirGeologyandExploitation,ChengduUniversityofTechnology,China)Abstract:Analgorithmisintrod…     

海南岛地体及其毗邻陆缘晚中生代—新生代古地磁研究和构造演化

本文叙述了对海南岛及其毗邻大陆边缘白垩纪到第四纪地层岩石进行古地磁研究的全部工作过程。通过分析岩石中剩余磁矢量的磁偏角及磁倾角的变化,提出海南岛白垩纪以来经历的构造演化模式如下:早期伴随顺时针旋转而向南迁移,后期伴随逆时针转动并向北运移。联系该地区及邻区的地质、地球物理资料,对海南岛上述的构造地体运动提出以下认识:北部湾内早期有一拉张作用,主要是该作用使湾内地壳显著伸长减薄,形成北部湾盆地。从而导致了海南岛的早期构造运动,而海南岛后期的构造运动则主要是受南海海底扩张的影响。海南地体运动规律的阐明对于了解北部湾油气盆地的形成演化有重要的理论和实际意义。     

Exciton Seebeck in Molecular Systems

Various applications relevant to the exciton dynamics,such as the organic solar cell,the large-area organic light-emitting diodes and the thermoelectricity,are operating under temperature gradient.The potential abnormal behavior of the exicton dynamics driven by the temperature difference may affect the efficiency and performance of the corresponding devices.In the above situations,the exciton dynamics under temperature difference is mixed with     

Achieving Unusual States of Matter Under High Pressure

The elongation method,originally proposed by Imamura was further developed for many years in our group.As a method towards O(N)with high efficiency and high accuracy for any dimensional systems.This treatment designed for one-dimensional(ID)polymers is now available for three-dimensional(3D)systems,but geometry optimization is now possible only for 1D-systems.As an approach toward post-Hartree-Fock,it was also extended to     

《Chinese Science Bulletin》SUBJECT INDEX TO VOLUME 59(2014)

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An on-line scaling method for improving scalability of a database cluster

The explosive growth of the Internet and database applications has driven database to be more scalable and available, and able to support on-line scaling without interrupting service. To support more client's queries without downtime and degrading the response time, more nodes have to be scaled up while the database is running. This paper presents the overview of scalable and available database that satisfies the above characteristics. And we propose a novel on-line scaling method. Our method improves the existing on-line scaling method for fast response time and higher throughputs. Our proposed method reduces unnecessary network use, i.e. , we decrease the number of data copy by reusing the backup data. Also, our on-line scaling operation can be processed parallel by selecting adequate nodes as new node. Our performance study shows that our method results in significant reduction in data copy time.     

An improved R-tree based on childnode''s probability

R-Tree is a good structure for spatial searching. But in this indexing structure,either the sequence of nodes in the same level or sequence of traveling these nodes when queries are made is random. Since the possibility that the object appears in different MBR which have the same parents node is different, if we make the subnode who has the most possibility be traveled first, the time cost will be decreased in most of the cases. In some case, the possibility of a point belong to a rectangle will shows direct proportion with the size of the rectangle. But this conclusion is based on an assumption that the objects are symmetrically distributing in the area and this assumption is not always coming into existence. Now we found a more direct parameter to scale the possibility and made a little change on the structure of R-tree, to increase the possibility of founding the satisfying answer in the front sub trees. We names this structure probability based arranged R-tree (PBAR-tree).     

Integrating GIS Web services based on mediating architecture

The geographic information service is enabled by the advancements in general Web service technology and the focused efforts of the OGC in defining XML-based Web GIS service. Based on these models, this paper addresses the issue of services chaining,the process of combining or pipelining results from several interoperable GIS Web Services to create a customized solution. This paper presents a mediated chaining architecture in which a specific service takes responsibility for performing the process that describes a service chain. We designed the Spatial Information Process Language (SIPL) for dynamic modeling and describing the service chain, also a prototype of the Spatial Information Process Execution Engine (SIPEE) is implemented for executing processes written in SIPL. Discussion of measures to improve the functionality and performance of such system will be included.