25Cr2MoVA 钢快速离子渗氮的X射线衍射分析

分析了２５Ｃｒ２ＭｏＶＡ钢经常规离子渗氮和快速离子渗氮后氮化表层的物相组成;研究了快速离子渗氮后时效温度与物相的关系。     

25Cr2MoVA钢快快速离子渗氮的X射线衍射分析

分析了２５Ｃｒ２ＭｏＶＡ钢经常规离子渗氮和快速离子渗氮后氮化表层的物相组成;研究了快速离子渗氮后时效温度与物相的关系。     

高碳低合金钢真空离子渗氮及其特性研究

利用自行研制的直流脉冲离子渗氮设备对高碳低合金钢GCr15在温度为460～550℃进行了真空离子渗氮处理1～5h,采用显微硬度计、XRD、SEM、耐腐蚀性检测仪等表征手段研究了离子渗氮对其性能的影响．实验结果表明：通过离子渗氮处理得到的表面硬度均在700HV0.3以上;渗氮层主要形成γ-Fe4N相及少量的ε-Fe2N／Fe3N相氮化物,氮化物的含量随渗氮温度的升高、渗氮时间的增加而增大;经真空离子渗氮处理其耐腐蚀性得到大大提高．     

热循环离子渗氮的快渗机制

根据热循环离子渗氮（ＩＮＴＣ）过程渗层生长动力学特性和表面相组分的变化规律,分析了辉光放电等离子体对热循环渗氮的增强作用,提出了循环变温过程相的脱溶和离子轰击形成的表面γ’相导致内扩散速度加快的机制,指出ＩＮＴＣ的深层快渗效果系集离子渗氮与热循环渗氮二者之长所致．     

TD3合金离子渗氮耐磨性能研究

采用离子渗氮技术对TD3合金表面进行离子渗氮处理,采用金相显微镜、XRD,对渗氮层的组织形貌、物相结构进行观察分析;用显微硬度仪(维氏)测量渗氮层硬度,再用摩擦磨损试验机(往复式)进行常温干摩擦实验,对其耐磨性、磨痕形貌进行分析。结果表明:渗氮层深度可达80μm,渗氮层显微硬度最高可达1 190 HV,较基材硬度提高2.3倍以上,渗氮层含TiN、Ti_2N。渗氮试样磨痕深度与宽度减小,耐磨性能比基材也有显著提高。     

等离子体渗氮用微脉冲电源的研制

研制开发了一种等离子体渗氮用高频微脉冲电源，其工作频率在100kHz以上，能很好地抑制弧光放电和空心阴极效应，能更有效地实现小孔径内表面等特殊条件下的离子渗氮处理。     

离子渗氮提高硬质膜层与普通结构钢基体结合力的研究

选用４０Ｃｒ作基体材料，ＴｉＮ作膜层材料，在离子镀膜进行离子渗氮预处理，性能测试与结构分析证实渗氮层的可以缓解膜性质的差异，提高膜基结合力。     

常压等离子体渗氮层摩擦学性能的试验研究

利用介质阻挡放电，形成非平衡等离子体，在自制的设备上进行常压等离子体渗氮研究，采用优化工艺对42CrMo材料进行离子渗氮处理，对处理后的试样硬度、断面金相组织进行了分析，对渗层的摩擦学性能进行了研究，并辉光离子渗氮工艺比较，试验结果表明：这种工艺完全达到了辉光渗氮处理的要求，并且组织致密，有利于提高其耐磨性，该渗氮工艺具有渗速快、渗层深、白亮层厚，渗氮效率高等优点。     

激光熔覆-离子渗氮复合改性层的组织和耐磨耐蚀性研究

为解决常规渗氮技术渗氮速度慢渗层浅、截面硬度梯度大、脆性高和耐磨耐蚀性偏低的问题,在N80钢表面制备Cr-Ni-Ti-La激光熔覆-离子渗氮复合改性层.采用光学显微镜、X射线衍射仪、硬度计、摩擦磨损试验机及电化学工作站对激光熔覆-离子渗氮复合改性试样和未熔覆直接渗氮试样的组织和耐磨耐蚀性进行对比研究.结果表明:渗氮前后...     

离子渗氮自动控制系统的设计

给出了基于单片机的等离子体渗氮工艺自动控制系统的设计方案,该系统由PIC单自机、AI智能仪表及脉冲电源等组成,对该系统组成部分的功能和监控程序设计作了详细地说明,该系统实现了对等离子体渗氮工艺的自动控制,为现行离子渗氮的设备发行和该工艺的技术进步将起到重要的作用。     

钛对35CrMo钢离子氮化层的影响

利用在离子氮化炉阴极上挂海绵钛的方法研究了钛对离子氮化层时影响。结果表明：钛能提高氮化层硬度、增加氮化层深度，并对氮化层的相组成有影响。     

40Cr基体与TiN膜层界面微观结构研究

在40Cr基体上镀TiN,存在膜基结合不牢的问题,作者前期工作已证实在镀TiN膜前先进行离子渗氮予处理,可以提高膜基结合力,本文从微观的方面对这一机理进行研究,膜层与膜基界面的透射电镜观察结果表明,40Cr基体经离子渗氮后再镀TiN,膜层晶粒细小、均匀、膜基结合紧密。     

奥氏体不锈钢的氮、铬离子淹没离子轰击处理

将铬离子源引入常规离子氮化炉,在铬、氮离子淹没条件下轰击不锈钢,采用金相显微镜、磨损试验机和电化学工作站等分析了不同工艺条件下渗层的显微组织、耐磨性和耐蚀性.结果表明:与未经处理的不锈钢相比,经氮、铬离子淹没离子轰击处理的不锈钢的耐磨性提高2-5倍;处理后不锈钢的耐蚀性虽有所下降,但与常规的离子氮化试样相比仍明显改善.     

显示渗层组织的彩色金相法

通过彩色金相的方法显示了离子渗氮层及固体渗硼组织。结果表明彩金相不仅可使不同深度的渗层组织清晰显现,还能够使渗层各区珠各相组合显示出来,简单讨论了各相着色原理。     

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).     

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.     

前混合磨料射流系统性能和结构的改进

针对前混合磨料射流系统存在的磨料涌出而导致对系统管件 ,尤其是喷嘴产生磨损的问题 ,对原有的射流系统进行了分析 .在分析结果的基础上 ,提出了 3种改进型系统 .对改进型系统进行了定性的理论分析 ,用试验手段得到高压管路的波速值 ,并用试验检验的方法得出了 3种改进型系统性能优劣的比较 ,认为改进 型系统较好的解决了磨料涌出并磨损管路元件的问题 .图 6 ,表 2 ,参 6     

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.     

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。     

微生物作用下混凝土裂缝修复效果试验研究

微生物矿化作用可以有效愈合混凝土裂缝,达到修复混凝土裂缝的目的.本文以带裂缝混凝土为研究对象,设置0.2、0.3、0.6 mm三个裂缝宽度和20、30 mm两个裂缝深度,以巴氏芽孢杆菌为菌株,通过裂缝观测、超声波测试、立方体抗压强度测试及裂缝内部微生物沉积物质的微观形貌分析,研究微生物对不同深度及宽度混凝土裂缝的修复效果.研究结果表明:巴氏芽孢杆菌可有效修复混凝土表面裂缝;氧气的供给是微生物在裂缝内部矿化的重要环境条件,随着裂缝深度的增加,巴氏芽孢杆菌的修复效果减弱;随着裂缝宽度的增大,微生物在裂缝内部的矿化效果减弱.