2：2型过氧钨酸盐的制备,结构和性质研究

在H_2O_2溶液中.通过活性粉状白钨酸的解聚制备了二个O_2~(2-):W为2:2型的新的过氧钨酸盐:K_2W_2O_s(O_2)_2·4H_2O(1)和(E_(t4)N~-)_2W_2O_5(O_2)_2·2H_2O(2).用IR、UV和XRD对二个过氧化物进行了表征,并推断了过氧钨酸阴离子的可能结构.     

过氧四钨酸钾的制备和性质表征

本文采用白钨酸解聚法,在室温下制备了一种新的过氧钨酸钾,通过元素分析和差热分析确定其化学组成是 K_4H_2W_4(O_2)_8O_7·8H_2O,通过 IR、UV 和 XRD 对其一些性质进行了表征.     

含钒的6—钨(钼)碲(vl)酸铵的合成与性质

某些6—钼碲酸盐用作催化剂应用于工业上后,对碲的杂多化合物的研究引起人们的关注。大量杂多酸催化化学的研究表明,钒原子取代钨(钼)后所形成的混和杂多化合物往往具有更高的催化活性和选择性。我们在系统研究碲的杂多化合物过程中,合成出几种文献上未见报道的含钒6—钨(钼)碲(Vl)酸铵:(NH_4)_7TeW_5VO_(24)·5H_2O,(NH_4)_8TeW_4V_2O_(24)、H_2O,(NH_4)_9TeW_3V_3O_(24)·H_2O 和(NH_4)_7TeMo_5VO_(24)·8H_2O 并研究了它们的一些性质。(NH_4)_7TeW_5VO_(24)·5H_2O 的合成方法是向60℃ 0.2mol钨酸铵溶液中加入溶于20ml 水中的0.4克 H_6TeO_6溶液、以醋酸调 PH 至3.5,回流3小时。然后加入溶于     

三元体系Na_2SO_4-(NH_4)_2SO_4-H_2O中的Na_2SO_4·10H_2O-(NH_4)_2SO_4和Na_2SO_4·10H_2O-(NH_4)_2SO_4·Na_2SO_4·4H_2O多温截面图

本文对Na_2SO_4-(NH_4)_2SO_4-H_2O三元体系中的Na_2SO_4·10H_2O_-(NH_4)_2SO_4(Ⅰ)和Na_2SO_4·10H_2O-(NH_4)_2SO_4·Na_2SO_4·4H_2O(Ⅱ)两个多温截面进行了研究.在(Ⅰ)中有三个四相转熔点:P_1,38wt%(NH_4)_2SO_4,58.8℃;P_2,10.9 wt%(NH_4)_2SO_4,26℃;P_3,39.1 wt%(NH_4)_2SO_4,-16℃.在(Ⅱ)中有两个四相转熔点:P_1,100 wt%(NH_4)_2SO_4·Na_2SO_4·4H_2O,59℃;P_2,23.62 wt%(NH_4)_2SO_4·Na_2SO_4·4H_2O,26.1℃,转熔反应热为180 J/g。     

电解酸化法制备偏钨酸氢铵

近年来,偏钨酸铵(NH_4)_6[H_2(W_3O_(10)_4]·nH_2O 的研究,特别是工业上的制备方法更引起人们的关注。本文用离子交换树脂作隔膜的电解酸化法制备酸式偏钨酸铵,此法操作简单,安全、成本低廉、产率达90%以上。同时,由于电解法不需加入其他试剂,可避免引入杂质,有利于产品的纯化。产物为无色透明的削角八面体晶形。不同 pH 值制得的偏钨酸铵通过组成分析,紫外光谱、红外光谱,热分析及水溶性等都是一致的,并与文献所得产品相同。     

草酸镨草酸钕及其混合物的热分解

將差热分析法与热失重法配合,分别測定了草酸镨与草酸钕的热分解現象。 pr_2(C_2O_4)_3·10H_2O■Pr_2(C_2O_4)_3·2H_2O■Pr_2(C_2O_4)_3·1/2H_2O■Pr_2(C_2O_4)_3■Pr_2O_3·CO_2■Pr_6O_11。 Nd_2(C_2O_4)_3·10H_2O■Nd_2(C_2O_4)_3·4H_2O■Nd_2(C_2O_4)_3·H_2O■Nd_2(C_2O_4)_3■Nd_2O_3·CO_2■Nd_2O_3。草酸镨与草酸钕的混合物,热分解曲綫仍具有分別代表镨与钕草酸盐的分解峯。但在镨钕混合物的草酸盐差热曲綫上,却不再有分別代表镨与钕的草酸盐分解峯。从而說明镨钕混合物的草酸盐,不同于镨钕草酸盐的混合物,而前者是属于复杂的多核络合物。因此,草酸盐热分解法不能适用于镨钕的分离。     

稀土元素杂多钨锑酸铵的合成与性质研究

首次报道了(NH_4)_(15)[Ln(NH_4Sb_9W_(21)O_(86)]·xH_2O(Ln~(3+)=La~(3+)、Ce~(3+)、Pr~(3+))和(NH_4)_(14)[Ln_2O(NH_4Sb_9W_(21)O_(86)]·XH_2O(Ln~(3+)=Gd~(3+)、Dy~(3+)、Yb~(3+))的合成方法,对这六种配合物进行了元素分析,确定了其组成,进行了IR、UV、TG等光谱性质研究.其结果表明配体结构在形成配合物的过程中基本上未发生变化.配合物IR光谱中γ(as)(w-od)和γas(w-ob)的向高频移动.     

稀土磺基水杨酸络合物与抑菌效应

在无水乙醇介质中合成了3价(钅兰)、铈、镨、钕的磺基水杨酸络合物和4价铈的磺基水杨酸络合物。经元素分析、红外光谱、可见紫外光谱和热分析得知,Ce(Ⅲ)L·nH_2O 络合物,是一种含磺基水杨酸根、硝酸根的三结晶水的络合物,其组成是:Ce(Ⅲ)(C_7H_5O_6S)_2·NO_3·3H_2O,在60℃下脱水,312℃开始分解。Ce(Ⅳ)L’·nH_2O 络合物是一种含磺基水杨酸根、硝酸根和铵离子的六结晶水的络合物,其组成可能是:NH_4[Ce(Ⅳ)_2(C_7H_3O_6S)_2(C_7H_4O_6S)·NO_3]·6H_2O在62℃下脱水,在301℃开始分解。用平皿洞穴法研究了 La、Ce、Pr、Nd 等(钅兰)系元素的3价络合物对真菌的抑茵效应,它们的抑菌圈宽度超过22～35mm,均属于强的抑菌效应。     

杂多酸的研究 Ⅱ.在非水溶剂中用电导滴定法测定12-钨磷酸的碱度

钨磷酸的碱度研究是解决它的结构的重要方面。多年来,对钨磷酸碱度的看法,一直是在争论之中。Rosenheim(1917)首先提出为七元酸(H_7[P(W_2O_7)6]·nH_2O);后来Keggin(1934)用X射线法研究了晶体结构,认为是三元酸(H_3[P(W_3O_(10)_4]·xH_2O)。这二种相对立的看法,Jander根据电导滴定结果,作了统一的解释;他认为Keggin的工作并不排斥Rosenheim的七元论,因为杂多酸中的水分子由于受多个W_3O_4基团的影响,在溶液中可以解离成酸:     

Al2o3—H3po4体系中生成物及热变化的研究

本文拟以Al_2O_3和85％的H_3PO_4为原料,采用H_3PO_4/Al_2O_3=6.8的投料比,在300℃以下温度范围内对磷酸铝系列化合物的生成进行了比较系统地考察。得出了AlH_3(PO_4)_2·3H_2O、AlH_3(PO_4)_2H_2O、Al(H_2PO_4)_3和AlH_2P_3O_(10)的生成量与温度的关系,研究了Al(H_2PO_4)_3和AlH_2P_3O_(10)·2H_2O的热变化过程。     

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.     

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.     

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.     

A computer generator for randomly layered structures

AcomputergeneratorforrandomlylayeredstructuresYUJia shun1,2,HEZhen hua2(1.TheInstituteofGeologicalandNuclearSciences,NewZealand;2.StateKeyLaboratoryofOilandGasReservoirGeologyandExploitation,ChengduUniversityofTechnology,China)Abstract:Analgorithmisintrod…     

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.     

海南岛地体及其毗邻陆缘晚中生代—新生代古地磁研究和构造演化

本文叙述了对海南岛及其毗邻大陆边缘白垩纪到第四纪地层岩石进行古地磁研究的全部工作过程。通过分析岩石中剩余磁矢量的磁偏角及磁倾角的变化,提出海南岛白垩纪以来经历的构造演化模式如下:早期伴随顺时针旋转而向南迁移,后期伴随逆时针转动并向北运移。联系该地区及邻区的地质、地球物理资料,对海南岛上述的构造地体运动提出以下认识:北部湾内早期有一拉张作用,主要是该作用使湾内地壳显著伸长减薄,形成北部湾盆地。从而导致了海南岛的早期构造运动,而海南岛后期的构造运动则主要是受南海海底扩张的影响。海南地体运动规律的阐明对于了解北部湾油气盆地的形成演化有重要的理论和实际意义。     

An Index mechanism for multi-scale view in spatial databases

There are numerous geometric objects stored in the spatial databases. An importance function in a spatial database is that users can browse the geometric objects as a map efficiently. Thus the spatial database should display the geometric objects users concern about swiftly onto the display window. This process includes two operations:retrieve data from database and then draw them onto screen. Accordingly, to improve the efficiency, we should try to reduce time of both retrieving object and displaying them. The former can be achieved with the aid of spatial index such as R-tree, the latter require to simplify the objects. Simplification means that objects are shown with sufficient but not with unnecessary detail which depend on the scale of browse. So the major problem is how to retrieve data at different detail level efficiently. This paper introduces the implementation of a multi-scale index in the spatial database SISP (Spatial Information Shared Platform) which is generalized from R-tree. The difference between the generalization and the R-tree lies on two facets: One is that every node and geometric object in the generalization is assigned with a importance value which denote the importance of them, and every vertex in the objects are assigned with a importance value,too. The importance value can be use to decide which data should be retrieve from disk in a query. The other difference is that geometric objects in the generalization are divided into one or more sub-blocks, and vertexes are total ordered by their importance value. With the help of the generalized R-tree, one can easily retrieve data at different detail levels.Some experiments are performed on real-life data to evaluate the performance of solutions that separately use normal spatial index and multi-scale spatial index. The results show that the solution using multi-scale index in SISP is satisfying.     

《Chinese Science Bulletin》SUBJECT INDEX TO VOLUME 59(2014)

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Achieving Unusual States of Matter Under High Pressure

The elongation method,originally proposed by Imamura was further developed for many years in our group.As a method towards O(N)with high efficiency and high accuracy for any dimensional systems.This treatment designed for one-dimensional(ID)polymers is now available for three-dimensional(3D)systems,but geometry optimization is now possible only for 1D-systems.As an approach toward post-Hartree-Fock,it was also extended to