塔里木-中朝板块北缘的志留纪岛弧公婆泉群火山岩地质地球化学及构造意义

公婆泉群位于北山中部，可分为：北、南两带。南带为弧后盆地玄武岩-安山岩组合，北带为岛弧火山岩组合，西段窑洞努如为火山角砾岩和熔火山角砾岩组合，中段公婆泉一带为玄武岩-安山岩-流纹岩-粗面岩组合，东段东七一山地区为玄武岩-安山岩-流纹岩组合。岩石组合，地球化学综合分析认为，公婆泉群是中-晚志留世哈萨克斯坦板块俯冲与塔里木-中朝板块的产物。岛弧西段窑洞努如位于近大陆或者在水下陆壳。公婆泉位于近海沟陆壳，而东七一山则远离海沟，是在洋壳的基础上发育的。说明塔里木-中朝板块是一个统一的板块，同时在早古生代存在哈萨克斯坦板块向塔里木-中朝板块的俯冲。     

渐近非扩张映象具误差的迭代收敛问题

研究了Banach空间中渐近非扩张型映象不动点的迭代逼近问题，所得结果改进了相关文献的最新成果．     

碳纤维表面特性对反硝化菌固着化的影响

通过对比反硝化菌在不同基体碳纤维表面的固着化及碳纤维表面含氧官能团对菌种的固着化实验,研究了碳纤维(基体、比表面积、循环利用性等)特性,尤其表面含氧官能团对反硝化菌固着化的影响。实验结果表明,反硝化菌在PAN基碳纤维上的平均挂膜厚度明显高于沥青基和粘胶基碳纤维。碳纤维表面适量的含氧官能团有助于较多、较牢固地固着反硝化菌。对三种PAN基碳纤维的XPS谱图分析表明碳纤维表面含氧官能团—O—CO对反硝化菌的固着化影响较大,当碳纤维表面含氧官能团—O—CO中碳原子占表面碳原子总量的3%左右时反硝化菌固着化效果较佳。经过比较表明PAN基碳纤维是一种生物相容性好、固着化程度高、再生能力强、耐微生物分解及化学腐蚀的优异的新型反硝化菌固着化载体。     

掺杂Fe3+的纳米TiO2光催化降解氮氧化物研究

利用Fe(NO3)3*9H2O,采用浸渍的方法,制备了掺Fe3+的纳米TiO2.讨论了此种纳米TiO2对氮氧化物的光催化效率,并分析了Fe3+在催化过程中的作用.试验结果表明:Fe3+明显提高了纳米TiO2的光催化性能;在室内自然光作用下对较高质量浓度的氮氧化物均具有较高的光催化效率.通过对TEM照片和XRD谱的分析,从能级理论解释了Fe3+提高催化活性的原因.     

蚂蚁算法在公交查询最短路径求法中的应用

公交乘客出行路径选择是公交乘客信息系统的关键技术 ,提出以换乘次数最少为首要目标、出行距离最短为第二目标的算法 ,本算法是基于广度优先搜索并结合蚂蚁算法提出公交路线最短路径选择的新算法     

Optimal Dispatching of Large—scale Water Supply System

This paper deals with the use of optimal control techniques in large-scale water distribution networks. According to the network characteristics and actual state of the water supply system in China, the implicit model, which may be solved by utilizing the hierarchical optimization method,is established. In special, based on the analyses of the water supply system containing variable-speed pumps, a software tool has been developed successfully. The application of this model to the city of Shenyang (China) is compared to experiential strategy. The results of this study show that the developed model is a very promising optimization method to control the large-scale water sup-ply systems.     

双语制对语言本身及社会生活的影响:以壮族地区为例

以壮族地区双语制为主要考察对象,提供新的材料,并从新的角度进行探讨。结论要点是:一是壮族地区双语现象的量化分析结果;二是双语制给壮语语音、词汇、语法系统带来了明显的影响;三是双语制给汉语有关方言的语音、词汇、语法系统也带来了明显的影响;四是双语制需要有与之相适应的语文政策。     

The age of formation of the mirabilite and sand wedges in the Hexi Corridor and their paleoclimatic interpretation

The Hexi Corridor is located at the transition zone of the Asian summer monsoon and westerly airflow, and lies in an important position in terms of its ecological fragility and climatic sensitivity. During a recent field expedition to this region, we found a sedimentary mirabilite layer in a number of localities including Suwushan, Yanchi, Baitujing, Yanchi Gaotai, Huahai, Yumen, Halanuo扙r, and Dunhuang (Fig. 1), which have the potential to provide important information about environmenta…     

Triassic U-Pb age for zircon from granites in the Tonghua area and its response to the Dabie-Sulu ultrahigh-pressure collisional orogenesis

Single-grain zircon U-Pb dating was carried out to constrain the emplacement timing of granitic plutons at Chaxinzi, Xiaoweishahe and Longtou in the Tonghua area, south of Jilin Province. The results show that these plutons formed in the Triassic with ages of 203—217 Ma. Geological and geochemical characteristics indicate that the plutons are composed of quartz diorite and granite. The former was derived from partial melting of mafic lower crust, whereas the latter originated from thickened crust with garnet as the residue in the source. It appears that protoliths of these two types of granitits are different although they have the same emplacement age. Considering that these plutons are petrologically different from the coeval granites in the Xingmeng (Xing‘an-Mongolian) to Jihei (Jilin-Heilongjiang) orogenic belt in the north, it is suggested that their formation was related to the Dabie-Sulu ultrahigh-pressure collisional orogenesis since their ages are only 10—20 Ma younger than timing of the ultrahigh-pressure metamorphism, but comparable to that of the first rapid exhumation of the ultra-high-pressure metamorphic rocks and the emplacement of the post-collisional granites.     

Loess-soil sequences in southern Anhui Province： Magnetostratigraphy and paleoclimatic significance

Two parallel loess-soil sequences from Xuancheng and Fanchang in southern Anhui Provinces are dated using geomagnetic and luminescence methods.The Brunhes/Matuyama(B/M) reversal boundary is recognized within the lower part of the so-calles Vermiculated Red Soil (VRS) in the Xuancheng section while the entire Fanchang sequence is of Brunhes age.This indicated that the most recent VRS in southern China,a stratigraphic marker and an indication of extremely warm-humid conditions,was formed during the middle Pleistocene,chronologically correlative with the S4 and S5 soil units in northern China.Microscopic and sedimentologic in vestigations reveal that eolian deposition started in this region at about 0.85 MaBp,roughly synchronous with the well-known Mid-Pleistocene climate change of global significance.The strengthening of both summer and winter monsoon circulations and the consequent river hydrological changes at that time would have provided favorable conditions for sustained eolian deposition in the middle-lower reaches of the Yangtze River since 0.85 MaBP.