TiO2纳米晶的低温制备及其抗紫外线性能

采用溶胶-凝胶法,在低温条件下制备纳米TiO2,用X射线衍射（XRD）对其结构和粒径进行表征,并测试分析了纳米TiO2溶胶对紫外-可见光的透射和吸收特性．结果表明,制得的纳米TiO2为锐钛矿型纳米晶,粒子尺寸小于10nm.纳米TiO2溶胶在波长250-350nm的紫外光区透射率极小,在220-340nm区域出现强吸收峰．将制得的纳米TiO2制成整理剂用于织物的整理．经过处理的棉织物对紫外线的阻隔率明显提高,紫外线防护指数（UPF值）从未处理时的6．72增加到50以上,表现出优异的抗紫外线性能．     

纳米ZnO/TiO2复合颗粒制备及紫外屏蔽性能研究

以Ti(SO4)2和Zn(AC)2为原料,在制备金红石型纳米TiO2粉体的基础上,用溶胶凝胶法制得纳米ZnO／TiO2复合粉体．实验结合纳米TiO2和纳米ZnO的优点制得一种广谱防晒剂．TEM显示该复合颗粒为核一壳式结构;XRD分析该复合颗粒内核为金红石型TiO2,表面包覆一层六方晶系ZnO且该复合颗粒中存在强的化学键．UV-Vis测试表明该复合颗粒在整个紫外区的吸收能力达到85％,在UVA(320-400nm)区吸收性能比纯的TiO2强得多．     

纳米流体强化CO2鼓泡吸收实验

利用两步法制备了多种乙醇基质纳米流体,建立了一套纳米流体强化气体吸收实验装置,分别测试了CO2在体积分数为0．01％-0．10％的Al2O3-C2H50H、MgO-C2H50H、SiO2-C2H5OH、TiO2（5nm）．C2H50H、TiO2（25nm）．C2H50H、Ti02（60nm）-C2H50H纳米流体中的吸收浓度曲线,得到了纳米流体的体积分数、纳米粒子的种类和粒径等因素对C02吸收过程的影响．实验结果表明,纳米流体的吸收强化效果随着纳米粒子体积分数的增加而增加,并且随着纳米流体中纳米粒子粒径的增加而减少．此外,还对纳米流体强化CO2吸收过程的机理进行了分析．     

Pt/TiO2的制备、表征及其光催化性能研究

以钛酸异丙酯为前驱体，反微乳法和溶胶-凝胶法相结合制备了TiO2纳米粉末，光还原法在TiO2表面沉积责金属Pt。用XRD、XPS对材料进行了表征。结果表明：TiO2为锐钛矿晶型，平均粒径约17 nm，沉积在TiO2表面的Pt主要以单质形式存在。少量以氧化态Pt^2＋存在。光催化结果表明Pt／TiO2的光催化活性比纳米TiO2大大提高，用荧光光谱讨论了Pt／TiO2光催化活性提高的机理。     

氮和硫共掺杂的纳米二氧化钛的制备及表征

以钛酸丁酯（TPOT）为原料，通过溶胶-凝胶法制得掺有氮和硫两种非金属元素的纳米二氧化钛（TiO2），并利用紫外-可见光谱（UV—vis）、红外光谱（IR）、X射线光电子能谱（XPS）等方法对其进行了表征。结果表明，该方法的确可以使N和S元素共掺杂到纳米TiO2中，并且使得纳米TiO2的吸收范围拓展到可见光区域，从400nm拓展到580nm．     

Ti02纳米晶的低温制备及其抗紫外线性能

采用溶胶一凝胶法,在低温条件下制备纳米TiO2.用x射线衍射(xRD)对其结构和粒径进行表征,并测试分析了纳米TiO2溶胶对紫外一可见光的透射和吸收特性.结果表明,制得的纳米TiO2为锐钛矿型纳米晶,粒子尺寸小于10nm纳米TiO2溶胶在波长250-350nm的紫外光区透射率极小.在220-340 nm区域出现强吸收峰.将制得的纳米TiO2制成整理剂用于织物的整理.经过处理的棉织物对紫外线的阻隔率明显提高,紫外线防护指数(UPF值)从来处理时的6.72增加到50以上,表现出优异的抗紫外线性能.     

转晶对纳米锐钛TiO2光催化活性的影响

加热处理纳米锐钛TiO2使其发生转晶，因而得到一种利用可见光激发的光催化剂，并对此催化剂用x射线衍射，红外吸收，紫外可见吸收等方法进行了表征．用该方法得到的TiO2为催化剂，进行可见光催化降解酸性红B的研究．结果表明，随着加热温度的升高，TiO2转晶比例逐渐增大，温度升到1000℃，全部锐钛型转变成金红石型TiO2，但TiO2在500℃下加热30min催化活性最高，酸性红B的光降解效果明显优于单独使用纳米锐钛型、纳米金红石型TiO2和按照转晶的比率混合的锐钛型和金红石型TiO2．这种显著提高的光催化作用归因于加热所形成的特殊锐钛-金红石界面耦合状态，导致光生电子从金红石相转移到锐钛相，避免了电子-空穴对的复合．     

La2O3／A1203／TiO2纳米复合粉体的制备及其耐温性能的研究

以TiCl4La2O3、A1片为原料，采用液相共沉淀法制备了La2O3／Al2O3／TiO2纳米复合粉体，采用DSC—TG、XRD、TEM技术对该纳米复合粉体进行了表征．结果表明：纳米TiO2粉体经La2O3掺杂和Al2O3复合后，其耐温性能得到显著提高，该复合粉体经900℃煅烧后，粒径在32nm左右，锐铁矿含量约为77．2％(mool％)     

纳米TiO2膜的制备及表征

通过溶胶-凝胶工艺制备了表面均匀的纳米TiO2光催化薄膜．用UV—Vis、AFM、XRD和XPS等对薄膜的表面形貌、结构和组成等进行了表征．结果表明，TiO2膜的表面均匀，颗粒大小约50nm，晶型为锐钛矿型．     

两步法仿生合成TiO2纳米线及其表征

以钛酸正四丁酯及L-半胱氨酸为钛源和模板剂,醇热法仿生合成纳米TiO2前体,冉将前体与氢氧化钠溶液水热反应制备出TiO2纳米线．通过SEM、XRD、FTIR以及比表面积及孔径分析仪对前体及纳米线进行表征,结果表明：TiO2纳米线为无定型的钛酸盐结构,直径在20～40nm,长度达数微米,其比表面积为312．58m2／g;煅烧后TiO2纳米线由无定型转变成锐钛矿型结构,FT—IR图谱分析表明纳米线含有Ti—O键．     

Markedness and its Interpretation in Language Use

Language markedness is a common phenomenon in languages, and is reflected from hearing, vision and sense, i.e. the variation in the three aspects such as phonology, morphology and semantics. This paper focuses on the interpretation of markedness in language use following the three perspectives, i.e. pragmatic interpretation, psychological interpretation and cognitive interpretation, with an aim to define the function of markedness.     

Lower Paleozoic oil relationships within Williston Basin, Canada

The Williston Basin is a significant petroleum province, containing oil production zones that include the Middle Cambrian to Lower Ordovician, Upper Ordovician, Middle Devonian, Upper Devonian and Mississippian and within the Jurassic and Cretaceous. The oils of the Williston Basin exhibit a wide range of geochemical characteristics defined as "oil families", although the geochemical signature of the Cambrian Deadwood Formation and Lower Ordovician Winnipeg reservoired oils does not match any "oil family". Despite their close stratigraphic proximity, it is evident that the oils of the Lower Palaeozoic within the Williston Basin are distinct. This suggests the presence of a new "oil family" within the Williston Basin. Diagnostic geochemical signatures occur in the gasoline range chromatograms, within saturate fraction gas chromatograms and biomarker fingerprints. However, some of the established criteria and cross-plots that are currently used to segregate oils into distinct genetic families within the basin do not always meet with success, particularly when applied to the Lower Palaeozoic oils of the Deadwood and Winnipeg Formation.     

An Analysis of Catherine＇s Character——Wuthering Heights

Wuthering Heights, Emily Bronte＇s only novel, was published in December of 1847 under the pseudonym Ellis Bell. The book did not gain immediate success, but it is now thought one of the finest novels in the English language. Catherine is the key character of this masterpiece, because everybody and everything center on her though she had a short life. We can understand this masterpiece better if we know Catherine well.     

Features of Women's language

Language is a means of verbal communication. People use language to communicate with each other. In the society, no two speakers are exactly alike in the way of speaking. Some differences are due to age, gender, statue and personality. Above all, gender is one of the obvious reasons. The writer of this paper tries to describe the features of women＇s language from these perspectives： pronunciation, intonation, diction, subjects, grammar and discourse. From the discussion of the features of women＇s language, more attention should be paid to language use in social context. What＇s more, the linguistic phenomena in a speaking community can be understood more thoroughly.     

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.     

Design and analysis of generic LBS application developing platform

Location based services is promising due to its novel working style and contents.A software platform is proposed to provide application programs of typical location based services and support new applications developing efficiently. The analysis shows that this scheme is easy implemented, low cost and adapt to all kinds of mobile nework system.     

橡胶颗粒沥青混合料低温抗裂性试验研究

以AC-13级配为基础,将橡胶颗粒代替部分集料掺入混合料中,以低温弯曲试验为评价方法对不同橡胶颗粒掺量下沥青混合料的低温抗裂性进行研究,并引入应变能密度值对混合料的低温抗裂性进行综合评价.试验结果表明:橡胶颗粒沥青混合料试件的破坏微应变均超过2 300,满足冬寒区的技术指标;无论是否掺加橡胶颗粒,随着温度的下降,沥青混合料破坏时的最大弯拉强度增大,弯拉应变降低,劲度模量增大;弯曲应变能密度在胶粒掺量为1%左右时具有较大的弯曲应变能密度值,此时橡胶颗粒沥青混合料具有较好的低温抗裂性.     

低渗透非均质砂岩油藏启动压力梯度研究

理论推导与室内实验相结合,建立了低渗透非均质砂岩油藏启动压力梯度确定方法。首先借助油藏流场与电场相似的原理,推导了非均质砂岩油藏启动压力梯度计算公式。其次基于稳定流实验方法,建立了非均质砂岩油藏启动压力梯度测试方法。结果表明:低渗透非均质砂岩油藏的启动压力梯度确定遵循两个等效原则。平面非均质油藏的启动压力梯度等于各级渗透率段的启动压力梯度关于长度的加权平均;纵向非均质油藏的启动压力梯度等于各渗透率层的启动压力梯度关于渗透率与渗流面积乘积的加权平均。研究成果可用于有效指导低渗透非均质砂岩油藏的合理井距确定,促进该类油藏的高效开发。     

On Tragic Consciousness In The Works By Ernest Hemingway

As an American modern novelist who were famous in the literary world, Hemingway was not a person who always followed the trend but a sharp observer. At the same time, he was a tragedy maestro, he paid great attention on existence, fate and end-result. The dramatis personae's tragedy of his works was an extreme limit by all means tragedy on the meaning of fearless challenge that failed. The beauty of tragedy was not produced on the destruction of life, but now this kind of value was in the impact activity. They performed for the reader about the tragedy on challenging for the limit and the death.     

Quantitative trait loci （QTLs） for quality traits related to protein and starch in wheat

Quality traits in wheat （Triticum aestirum L.） were studied by quantitative trait locus （QTL） analysis in a recombinant inbred line （RIL） population, a set of 131 lines derived from Chuan 35050 × Shannong 483 cross （ChSh）. Grains from RILs were assayed for 21 quality traits related to protein and starch. A total of 35 putative QTLs for 19 traits with a single QTL explaining 7.99-40.52% of phenotypic variations were detected on 10 chromosomes, 1D, 2A, 2D, 3B, 3D, 5A, 6A, 6B, 6D, and 7B. The additive effects of 30 QTLs were positive, contributed by Chuan 35050, the remaining 5 QTLs were negative with the additive effect contributed by Shannong 483. For protein traits, 15 QTLs were obtained and most of them were located on chromosomes 1 D, 3B and 6D, while 20 QTLs for starch traits were detected and most of them were located on chromosomes 3D, 6B and 7B. Only 7 QTLs for protein and starch traits were co-located in three regions on chromosomes 1D, 2A and 2D. These protein and starch trait QTLs showed a distinct distribution pattern in certain regions and chromosomes. Twenty-two QTLs were clustered in 6 regions of 5 chromosomes. Two QTL clusters for protein traits were located on chromosomes 1D and 3B, respectively, three clusters for starch traits on chromosomes 3D, 6B and 7B, and one cluster including protein and starch traits on chromosome 1D.