莠去津在填充土柱中的运移

用土柱实验模拟莠去津在土壤中的运移、实验结果表明相当浓度的莠去津被淋溶到土柱的底部，说明莠去津对地下水存在很大威胁、应用CXTFIT的平衡与非平衡模型模拟莠去津在土柱中的运移，模拟结果表明CXTFIT的非平衡模型能很好地模拟莠去津的穿透曲线．由CXTFIT率定得到的莠去津在土柱实验中的吸附和降解参数和从批次实验得到的吸附和降解参数有较好的一致性．     

曝气生物流化床处理炼油厂含硫和高氨氮污水的研究

炼油厂含硫污水因含高浓度的油、COD、硫化物及挥发酚而难于生化降解，催化剂生产中排放的污水因含高浓度的氨氮、盐类、悬浮物质以及低浓度的有机物而成为水处理的难题．本文采用一种曝气生物流化床（ABFT）工艺，对含硫污水和催化剂高氨氮污水的混合污水进行了现场连续试验，结果表明：在混合污水COD为2090mg／L、氨氮为600mg／L、挥发酚为27mg／L和硫化物为154mg／L的情况下，ABFT系统出水COD为95mg／L、氨氮为4．0mg／L、挥发酚为0．30mg／L和硫化物为0．0067mg／L，出水达到了国家污水排放标准一级标准．在处理工艺中，动态氧化和混凝沉淀作为预处理，ABFT反应器采用了合成高分子载体固定化微生物技术，该载体具有大孔网状以及优良的机械强度和化学性能，高效微生物B350通过化学键固定在载体上．克氏定氮法表明，ABFT中生物负载量为32mg／L．试验结果显示：在处理高氨氮污水方面，ABFT工艺比SBR工艺具有更强的优势，同时，ABFT系统具有较高的处理效率和耐冲击负荷能力．     

变更图的边添加

证明了:对任何整数t≥6和d≥2,从一条长为d的简单路通过添加t条边后得到的图的最小直径上界为[d-2/t 1] 2,如果d∈J'(t,k)={2k(t 1) 1,2k(t 1) 2,2k(t 1)-t 1}∪{2k(t 1)-t h:h=6,7,…,t};其他情形为[d-2/t 1] 1.这个证明改进了已知结果,而且[d-2/t 1] 1是最好的上界.     

The fate of injectant coal in blast furnaces: The origin of extractable materials of high molecular mass in blast furnace carryover dusts

The aim of the work was to investigate the fate of injectant coal in blast furnaces and the origin of extractable materials in blast furnace carryover dusts. Two sets of samples including injectant coal and the corresponding carryover dusts from a full sized blast furnace and a pilot scale rig have been examined. The samples were extracted using 1-methyl-2-pyrrolidinone (NMP) solvent and the extracts studied by size exclusion chromatography (SEC). The blast furnace carryover dust extracts contained high molecular weight carbonaceous material, of apparent mass corresponding to 10⁷?10⁸ u, by polystyrene calibration. In contrast, the feed coke and char prepared in a wire mesh reactor under high temperature conditions did not give any extractable material. Meanwhile, controlled combustion experiments in a high-pressure wire mesh reactor suggest that the extent of combustion of injectant coal in the blast furnace tuyeres and raceways is limited by time of exposure and very low oxygen concentration. It is thus likely that the extractable, soot-like material in the blast furnace dust originated in tars is released by the injectant coal. Our results suggest that the unburned tars were thermally altered during the upward path within the furnace, giving rise to the formation of heavy molecular weight (soot-like) materials.     

Land vehicle positioning using GPS and dead reckoning

To ensure reliable land vehicle positioning, the Global Positioning System (GPS) is one of the best techniques commonly used in present-day positioning systems. However, GPS signals are not available if line of sight with the satellites is lost. In this respect, the addition of the Dead Reckoning (DR) method to complement the GPS unit would enhance the reliability of land vehicle positioning system. For implementing the DR method, the magnetic sensor and accelerometer are used for obtaining heading and velocity or distance information. Calibration of two sensors' dynamic model and DR algorithm are also introduced in this paper. The test result utilizing the GPS and DR methods is analyzed in this paper. It utilize spositioning information from GPS receiver when GPSsignal is available, otherwise DR is started to compensate GPS outage with the GPS output as the original point. The results showed that the error in east and north produced by the DR algorithm for a short time interval can be limitedwithin an acceptable range.     

In-vehicle GPS/DR navigation system development and test results in Singapore

This paper introduces the in-car navigation system prototype development and test results under the context of Singapore. In the system, integrated GPS/DR is used for continuous vehicle positioning. A digital road network map database is built for the whole Singapore. The database is designed to support map matching, route determination, and route guidance functions. The prototype system demonstrates GPS positioning of the vehicle in real-time, tracking the vehicle onto a digital map with fix updates every one or two seconds.With the map matched vehicle location on the map, voice and/or text guidance is provide to the driver. The vehicle position can also be transferred to control centre through communication data link for the purpose of fleet management.     

Temperature variations on the Tibetan Plateau over the last two millennia

The paleoclimate data recovered from ice cores,tree rings and lake sediments indicate regional features of cfimatic change on the Tibeta n Plateau (TP) during the last 2000 years. The composite temperature reconstructions in-dicate that several main climatic episodes, such as the “LittleIce Age“ between 1400 and 1900, the “Medieval Warm Pe-riod“ in 1150-1400, a less warm period in 800-1100, and an earlier cold period between the 3rd and 5th centuries,occurred in the TP. In addition, temperature varied from region to region. The period from AD 800 to 1100, which waswarm in northeastern TP, was contemporaneous with cool-ing in the western and southern TP. The southern TP ex-perienced warming between 1150 and 1400. For western TP,the δ^18O records of the Guliya ice core indicate that the pe-Hod 1250-1500 witnessed a clear warming. Large-scaletrends in the temperature history from northeastern TP aremore similar to those in eastern China than are the trendsfrom the Guliya ice cap far to the west and southern TP. The most prominent similarities between the temperature varia-tions of the TP and eastern China are such cold phases as 1100-1150, 1500-1550, 1650-1700 and 1800-1850, andthe latter three cold events match with three widespreadg lacial advances which occurred on the TP during the Little Ice A2e.     

A carbon- and oxygen-isotope record of recent environ- mental change from Qinghai Lake, NE Tibetan Plateau

An understanding of natural climatic variability is essential for evaluating anthropogenic impacts on recent and future climate[1—3]. Due to the lack of lengthy instrumental records, such an understanding must be gained from natural archives of climate change. Palaeolimnological indicators of past lake levels may provide a sensitive record of changes in effective precipitation in closed basins. This approach is particularly relevant on the Tibetan Plateau, where instrumental records are very…     

Ni2MnGa铁磁形状记忆材料

铁磁形状记忆合金 (FSMA)是在一定温度范围马氏体相稳定同时又具铁磁性的一类特殊的形状记忆合金。Ni2MnGa铁磁形状记忆合金近年来成为呈现磁场驱动大应变的新型驱动材料 ,这些应变来自磁场诱发马氏体孪晶的重排 ,而不是磁场对奥氏体至马氏体相变的作用。孪晶变体的重排在宏观上呈现为正或切应变 ,一非化学计量比Ni2 MnGa单晶于室温加 0 .4T磁场能产生6 %的应变 ,Ni Mn Ga单晶在高至 15 0Hz的交变磁场仍可得到 2 .5 %的应变。本文阐述了与这种磁控形状记忆效应相关的孪晶界迁动的磁学和晶体学理论。马氏体相的大磁晶各向异性能使磁化沿c轴方向有利 ,穿过孪晶界c轴刚好转动 90度 ,同时 ,这个孪晶界也构成了约 90度的畴界。在各向异性的情况下 ,孪晶界的迁动仅有相邻孪晶变体的Zeeman能差驱动 ,μ0 ΔMis·Hi。磁场和外应力对应变的影响通过对一简单的自由能表达式取极小值来表示 ,自由能表达式包括Zeeman能、磁晶各向异性能和外应力以及在某些情况下需考虑的内部弹性能 ,模型的所有参数可通过应力 应变曲线和磁化曲线测量得到。铁磁形状记忆合金的磁场诱发应变可类比传统热弹性形状记忆效应 ,与更为人们所熟知的磁致伸缩现象不同。     

五台山滹沱群SHRIMP锆石U-Pb年龄: 华北克拉通早元古代拼合新证据

采自五台山台怀镇南8 km处滹沱群变质火山-沉积岩层中的长英质凝灰岩样品含有两组锆石, 所记录的SHRIMP锆石方法²⁰⁷Pb/²⁰⁶Pb年龄分别为2180±5 Ma和2087±9 Ma. 在误差范围内, 较老的一组年龄与五台山大洼梁花岗岩年龄相当, 表明它们来自相似的地壳岩浆源; 而较年轻的一组锆石年龄与相邻地区阜平杂岩湾子表壳岩中变沉积岩和变火山岩及南营花岗片麻岩年龄相当, 因而被解释为滹沱群火山作用年龄. 这两组年龄的存在表明: (1) 滹沱群形成于早元古代而非太古宙; (2) 早元古代火山-沉积作用在五台和阜平地区同时间发生. 这样, 早元古代沉积作用在该区是广泛的, 它们代表了华北克拉通东部陆块西侧大陆边缘相沉积. 滹沱群火山作用年龄的确定也表明该群所经历的变质-变形事件发生在2087±9 Ma 之后, 这进一步佐证我们最近根据其他方面研究结果所得出的吕梁造山事件(约1.8 Ga)是该区主要构造事件的结论: 该事件导致华北克拉通东部陆块和西部陆块的最终拼合, 并成为全球早-中元古代超级大陆组成部分之一.