乙炔在NO中燃烧反应机理探讨

利用公式ΔH=-0.1196n λ计算了乙炔在NO中燃烧反应的火焰温度,计算值为3587K,与实际温度3368K非常接近.根据火焰温度,提出了乙炔在NO中燃烧反应的机理.该机理为:(1)NO+hν→N·+O·,(2)N·+NO→N2+O·,(3)C2H2→2C+H2,(4)H2+O·→H2O+hν,(5)C+O·→CO+hν,(6)CO+O·→CO2+hν.     

醇燃烧反应机理探讨

利用公式ΔH =- 0 .1196n/λ计算了甲醇和乙醇燃烧反应的理论火焰温度 ,提出了醇燃烧反应的机理 .该机理为 :(1)O2 +ν→ 2O· ;(2 )CmH2m + 1OH→CmH2m +H2 O ;(3)CmH2m →mC +mH2 ;(4 )H2 +O·→H2 O +hν ;(5 )C +O·→CO +hν;(6 ) 2CO +O2 → 2CO2 .     

H2在N2O内燃烧反应机理探讨

本文利用公式ΔH=-0.1196n λ计算了H2在N2O内燃烧反应的火焰温度,计算值为3197K,与实际温度2923K较为接近.根据火焰温度,提出了H2在N2O内燃烧反应的机理,该机理为:(1)2N2O→N2 2NO;(2)NO hv→N· O;(3)N· NO→N2 O·;(4)H2 O·→H2O hv.     

H2在F2内燃烧反应机理探讨

利用公式△H=-0.119 6n/λ计算了H_2在F_2内燃烧反应的理论火焰温度.当反应物温度为400 K时,其理论火焰温度为4 354 K,与实际温度3 962 K较为接近,根据火焰温度,提出了H_2在F_2内燃烧反应的机理,该机理为:(1)F_2+hv→2F·,(2)H_2+2F·→2HF+2hv,     

乙醚与丙酮燃烧反应机理

利用公式△H=-0．1196n／A计算了乙醚和丙酮分别在氧气和空气中燃烧反应的温度,并推测了乙醚和丙酮燃烧反应的机理．乙醚在氧气中燃烧反应的火焰温度理论值为3272K,与测定温度3134K接近,误差为4．40％．丙酮在空气中燃烧反应的火焰温度理论值为1292K,与测定温度173K接近,误差为1．49％．根据乙醚和丙酮燃烧反应的火焰温度,推测乙醚和丙酮燃烧反应机理为：（1）O2＋hv→2O·;（2）（C2H5）2O→4C＋4H2＋H2O（乙醚）,CH3COCH3→3C＋2H2＋H2O（丙酮）;（3）H2＋O·→H2O＋hv;（4）C＋O·→CO＋hv;（5）2CO＋O2→2CO2．     

煤气燃烧反应的火焰温度

计算了水煤气和焦炉气燃烧反应的火焰温度,进一步明确氢气和烃燃烧反应的机理.氢燃烧反应的机理为:(1)O2 hv→2O·,(2)H2 O·→H2O hv;烃燃烧反应的机理为:(1)O2 hv→2O·,(2)CpH2q→pC qH2,(3)H2 O·→H2O hv,(4)C O·→CO hv,(5)2CO O2→2CO2.     

S、H2S及CS2在氧气中燃烧反应机理

利用公式△H=-0.1196n/λ计算了S、H2S及CS2在氧气中燃烧反应的火焰温度,并推测了三种物质燃烧反应的机理.S在氧气中燃烧反应的火焰温度计算值为2086 K,与测定值2093K接近,误差为-0.30％.H2S在氧气中燃烧反应的火焰温度计算值为2238K,测定温度2383K,误差为-6.1％.CS2在氧气中燃烧反应的火焰温度计算值为2502K,测定温度2468K,误差为0.14％.根据燃烧反应的火焰温度,推测S、H2S及CS2在氧气中燃烧反应机理.S燃烧反应机理为：（1）O2＋ hv→2O·,（2）S ＋O·→SO＋hv,（3）2SO＋O2→2SO2,（4）SO2＋O·→SO3 ＋hv.H2S燃烧反应机理为：（1）O2＋ hv→2O·,（2） H2S→H2 ＋S,（3）H2 ＋O·→H2O＋hv,（4）S＋O·→SO＋hv,（5） 2SO＋ O2→2SO2,（6）SO2 ＋O·→SO3＋ hv.CS2燃烧反应机理为：（1）O2＋hv→2O·,（2） CS2→C ＋2S,（3）C＋O·→CO＋ hv,（4）CO＋O·→CO＋hv,（5）S＋O·→SO＋ hv,（6）2SO＋ O2→2SO2,（7）SO2＋O·→SO3＋ hv.     

高氯酸铕与L-谷氨酸配合物单晶体的标准生成焓及热化学研究

合成了稀土高氯酸铕-谷氨酸配合物晶体.经热重、差热、化学分析及对比有关文献,知其组成是[Eu2(Glu)2(H2O)8](ClO4)4·H2O,单晶结构,纯度是95.06%.选用Eu(NO3)3·6H2O、L-Glu、NaClO4·H2O、NaNO3和H2O作辅助物,使用具有恒温环境的反应热量计,以2mol·L-1HCl作溶剂,分别测定了[2Eu(NO3)3·6H2O+2Glu+6NaClO4·H2O]和{[Eu2(Glu)2(H2O)8](ClO4)4·H2O+6NaNO3+9H2O}在25℃时的溶解焓.设计-热化学循环求得化学反应的反应焓△rH =36.873kJ·mol-1,计算得配合物[Eu2(Glu)2(H2O)8](ClO4)4·H2O(s)在298.15K时的标准生成焓△1 H ,298.15K=-6584.853kJ·mol-1.     

反应条件对Pd/Ce-Ti催化剂CO低温氧化性能的影响

对溶胶-凝胶法制备的CeO2 TiO2复合氧化物载体负载Pd催化剂进行了表观动力学研究,在pCO==1×10-3～4×10-3MPa,CO和O2的反应级数分别为-1.0和1.0级.在温度范5×10-4～3×10-3MPa,pO2/pCO接近化学计量比的条件下,CO氧化反应的平均表观活化能为67.2kJ·mol-1.考察了气围303～343K,pO2体组成对CO低温氧化反应的影响和催化剂的稳定性.x(O2)/x(CO)=0.5时,CO氧化反应的起燃温度为345K,提高x(O2)/x(CO),可以降低起燃温度,在较低的CO浓度(0.5%)和较高的x(O2)/x(CO)(6.3)下,催化剂在室温下就有氧化活性,起燃温度仅为308K.在φ(CO)=1.0%的空气中,空速39000mL·h-1·g-1的条件下,CO反应在室温(293～303K)就可以实现完全转化,其反应稳定性与反应温度相关,313K下催化剂寿命可达15.5h.     

NH_3·(H_2O)体系中氢键的理论计算

用量子化学密度泛函理论方法研究了NH3·(H2 O)体系中氢键特征 ,计算了不同基组条件下NH3·(H2 O)体系中氢键的键长 ,同时在Gaussian 3 (G3 )水平上计算了NH3·(H2 O)体系中氢键的键能和成键特征 ,得到NH3·(H2 O)体系中生成氢键有两种构象 .     

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