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.     

二苯并四氧二氮环醚及其稀土配合物合成与荧光性质研究

合成了二十员大环双氮杂冠醚：2，3，l6，l7—二苯—l，8，ll，18—四氧—5，14—二氮杂环二十烷及其7个与稀土硝酸盐(RE^3 ＝La^3 ，Sm^3 ，Eu^3 ，Gd^3 ，Tb^3 ，Dy^3 。Yb^3 )所形成的1：2(M：L)型固体配合物，并经过红外光谱、元素分析、摩尔电导及热分析等方法对配合物进行了表征．结果表明，配位是通过配体中的C—O-C进行的，而Ar—O-C未参与配位，同时含2分子配位水．对Sm(Ⅲ)，Eu(Ⅲ)，Tb(Ⅲ)，Dy(Ⅲ)的配合物进行了荧光光谱测定，所有配合物均有较强的荧光强度，其中Tb(Ⅲ)的配合物荧光强度最高，表明该新双氮杂冠醚配体三重态的能量与Tb(Ⅲ)的振动能级最为匹配．     

BP网络应用于黄河水质的预测研究

利用黄河兰州段水质指标浓度时间序列作为学习样本，选取了DO、COD、氨氮、重金属离子等l0项指标作为输出参数，运用人工神经网络BP模型中的Levenberg—Marguardt优化算法对学习样本优化建模，将优化好的网络的预测结果与实测结果进行了比较，表明BP网络可以很好地用于黄河水质指标值及水质类别的预测。     

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…     

连续事件的语义数据模型

语义抽象概念aggregation和generalization不仅对不包含时间概念的复杂情况的数据模型的建立很有用，而且还可以成功地用于连续事件的建模。建立了两种情况并存的语义数据模型：or—dering(次序)和sequencing(先后顺序)，并且可以在任何程序环境下实现。     

豫西早二叠世掌蕨Chiropteris Kurr和髻籽羊齿Nystroemia Halle有机连接标本的发现

基于河南登封早二叠世肾掌蕨Chiropteris reniformis Kawasaki和髻籽羊齿Nystroemia pectiniformis Halle有机连接的标本, 确立了肾髻籽羊齿(新组合)Nystroemia reniformis (Kawasaki) comb.nov.营养叶具长柄, 肾形, 基部心形, 全缘或具细齿; 叶脉细, 多次二歧分叉并结为多边形或菱形细网.生殖枝在苞片腋部着生.苞片与营养叶同形.胚珠器官在叶性器官腋部着生或两者分别不规则地着生于生殖枝的轴上.极多的具翼双角籽倒圆锥形, 呈两列状排列, 珠孔朝上.该植物代表了一种新的已灭绝的裸子植物.     

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.     

CHARACTERIZATION OF SOL-GEL-DERIVED ZrO2 FILM BY PHOTOTHERMAL RADIOMETRY

In modern industry,thin film on the substratc has much important role to decide the properties of product, especially for electrical, optical and wear-resistant etc, production. There are some technical methods to prepare thin film,including plasma spray,physical vapor deposition (PVD),chemical vapor deposition (CVD) and sol-gel,etc. Among of them,sol-gel method has been developed a popular tech nique for preparing thin films.