射流悬浮床气固两相流动的数值模拟

从多相流多流体模型、气相湍流k-ε模型与颗粒湍流k_p模型出发,对底部向上射流悬浮床内气固两相流动进行数值模拟,得到了不同入口气速下各截面的颗粒相速度场、颗粒相脉动速度场的分布,结果与实验定性一致。计算结果与实验值对比的结果表明,数值模拟对进一步的研究有指导意义。数值结果与实测值间存在的差异则有待于进行直接三维流动模拟、进一步考察更为合理的边界条件及应用更先进的模型来解决。     

百色盆地百49块百岗组三段高分辨率层序地层学分析

以高分辨率层序地层学理论为指导，通过地表露头、岩芯、测井资料的综合研究，并结合地震剖面资料，分析了百色盆地塘寨油田百49块古近系百岗组三段不同级别的层序界面和湖泛面特征及识别标志，划分出1个长期、3个中期、14个短期基准面旋回层序。在此基础上，详细讨论了各级次基准面旋回层序的垂向序列、岩性岩相组合、结构类型及更加样式等特征，并探讨了高分辨率层序地层学的研究成果在区块油气开发工程中的应用前景。     

平面锥形光波导模斑转换器的研究

基于三维有限差分束传输法（FD－BPM）对平面光波导器件中的关键元件之一－平面锥形模斑转换器作了深入的研究，对线性和数种非线性侧面边界的模斑转换器进行了数值仿真和对比，分析了平面锥形模斑转换器侧面边界函数对耦合损耗的影响，以及模斑转换器中模场分布随传输距离的变化，确定了不同长度的平面锥形模斑转换器的最佳侧面边界，指出长度在200－1000μm范围内具有余弦边界的平面锥形模斑转换器性能最佳，并且发现，光纤中的出射光进入模斑转换器以后，光波模式会逐渐发生变化，并最终转化为单模。     

发展循环经济的科技策略的探讨

自工业革命以来 ,人类创造了大量的物质财富 ,但也付出了沉重的代价 ,环境污染和地球生态系统的破坏 ,已经严重影响并会制约经济的发展。当前的经济已经从工业经济向循环经济演进 ,如何在保持经济发展的同时不破坏环境 ,作者提出了发展循环经济的科技策略 ,即重构、调整、及合作 ,对当前经济发展具有一定的指导作用。     

边水驱油藏调剖技术

针对边水驱油藏的地质及开发特点 ,提出了边水调剖技术 ,同时对调剖井点的选择、调剖剂的筛选、调剖剂用量的确定、调剖施工工艺等配套技术进行了研究。通过向优选的调剖井注入调剖剂 ,可以控制边水的侵入方向和推进速度 ,从而增大波及系数 ,提高最终采收率。 2 0 0 0年 5月到 1 1月 ,对高 1 0 4 5区块 8口井进行了边水调剖试验 ,共注入调剖剂 1 851 6m3。调剖后 ,内部井的含水率下降、产量回升 ,明显提高了区块的采收率。数值模拟预测结果表明 ,调剖增油超过 70 0 0t,投入产出比大于 1∶2。     

民族生态审美场论

与相应的审美氛围、审美风范双向对生并走向整生的民族审美活动循环圈 ,构成民族生态审美场。民族生态审美场是民族生态审美学的整体对象 ,它的逻辑结构统观化整生化展开 ,构成当代民族生态审美学的理论体系     

N-terminal of L protein of vesicular stomatitis virus contains a new signal sequence

The L protein (241kD) of vesicular stomatitis virus (VSV) is the most important snbnnit of the replication complex. The existence of specific localization signal in the L protein was investigated by making recombinant constructs expressing truncated mutants of the L protein fused to green fluorescent protein (GFP) in transient transfection assays. The chimeric genes encoding varied N-terminal of L and GFP gene were put under the control of T7 promoter or CMV promoter. The fusion proteins were transiently expressed in BHK-21, COS-7, CHO or Hep G2 cells. When more than 120 residues were deleted or only 96 residues were kept on the N-terminal, the fusion proteins were shown to be distributed throughout the cells, cytoplasm and nucleus under the confocal microscope. However, other chimeric proteins with 120 or more amino acids were dotted and distributed in the perinuclear regions. And the fusion protein with 96—120 aa has the similar distribution. A thirteen-residue peptide QGYSFLHEVDKEA (108—120) was identified as localization signal, whose function would be absolutely distributed with the deficiency of D or V. Our results show that there is an independent localizing signal in N-terminal domain of L protein of VSV and this functional signal is conserved in different cell lines.     

New geological evidence of crustal thickening in the Gangdese block prior to the Indo-Asian collision

Recent mapping in the Gangdese block has revealed many leucogranites that are similar to those in the High Himalaya. These leucogranites formed at ～140 Ma as indicated by monazite Th-Pb ion-microprobe dating and cooled at ～130 Ma as indicated by muscovite ^40Ar/^39Ar dating. In conjunction with previous structural and paleogeographic studies, the new data indicate that the Gangdese block underwent crustal thickening and associated exhumation during ～140—130 Ma. In this regard, the southern margin of Eurasia continent was comparable to the modern South American Altiplano-Puna plateau, the prime example of active ocean-continent subduction and associated thickened crust. Specifically, the early stages of crustal thickening and uplifting of the Gangdese block may result from subduction of the Neo-Tethyan Ocean. If the Tibetan Plateau would form by accretion of a series of blocks with thickened crust, an elevated topographic plateau similar to the Altiplano-Puna plateau had formed before collision between the Indian and Eurasian plates. Then the Tibetan Plateau would have quickly thickened, uplifted, and begun to extend soon after onset of the collision. Thus, the deformational mechanism of the Tibetan Plateau is not distributed shortening, but rather concentrating deformation within regions of thin crust between the accreted blocks.     

Contributions of different land cover types in Otindag Sandy Land and Bashang area of Hebei Province to the material source of sand stormy weather in Beijing

Different land cover types in Otindag Sandy Land and Bashang area of Hebei Province are linked to a material source of sand stormy weather in Beijing based on results of field vegetation and soil survey and laboratory works. Results of grain size analysis show that dust release potential in per unit area of moving sandy land is small,while lowland meadow and meadow steppe in stony hills have high potential of releasing dusts in per unit area during sand stormy weather occurrence. Further considering the effects of vegetation, it is inferred that the moving sandy land served as a material source of past dust storm and the possibility of dust release in per unit area is low in current time.Typical steppe in stony hills is undergoing desertification and its dust release possibility in per unit area is high. Farmland has strong potential of release dusts when they are ploughed in spring, but a large amount of therophytes grow and thus prevent dusts from release when cultivation was terminated.Potentials of dust release in per unit area in fixed sand dunes,stony mountain meadow steppe and low land meadow are lowdue to high cover of perennials. Sand dune reactivation and desiccation of lakes and lowlands under estimated future climatic change will make them serve as a future material source of sand stormy weather.     

兰州北山生物结皮中陆生藻种类组成与群落结构

通过对沙井驿、刘家堡、九州台、白塔山、小牛圈沟等样点采集的生物结皮样的培养和鉴定 ,研究了兰州市北山生物结皮中陆生藻种类组成及其群落结构 .结果发现 ,该地陆生藻共计 5 3种 ,其中蓝藻 34种 ,绿藻 7种 ,硅藻10种 ,裸藻 2种 .蓝藻中以丝状种类占优势 (6 5 % ) ,绿藻中仍以球状种类居多 (5 7% ) ,但也有不少丝状个体(43% ) .黄土结皮以非洲席藻为第一优势种 ,石崖表具鞘微鞘藻占绝对优势 ,人工草丛中小球藻最丰富 ;种类数在砾质黄土中最多 (2 3) ,黄粘土中最少 (16 ) .