阿利特-硫铝酸钡钙水泥熟料烧成与性能研究

采用正交试验的方法研究了阿利特-硫铝酸钡钙水泥的烧成制度。结果表明：对该熟料力学性能影响最大的因素是冷却方式，其次是烧成温度，影响程度最小的是保温时间。该水泥的最佳烧成制度为：烧成温度为1380℃，保温时间为60min，冷却方式为自然冷却；同时，在最佳烧成条件下制备的阿利特-硫铝酸钡钙水泥的1d，3d，28d抗压强度分别达到24．7MPa，52．5MPa，102．5MPa，展现出良好的力学性能。同时利用XRD和SEM—EDS对熟料矿物组成及结构进行了分析。     

利用工业原料合成阿利特-硫铝酸钡钙水泥及其性能研究

应用前期研究获得的熟料最佳组成,利用工业原料合成阿利特-硫铝酸钡钙水泥熟料,研究了原料中不同MgO含量对熟料f-CaO及水泥后期力学性能的影响,研究结果表明:利用工业原料能够合成阿利特-硫铝酸钡钙水泥;随着原料中MgO含量的增加,熟料f-CaO含量增加,水泥后期力学性能降低;中等MgO含量的阿利特-硫铝酸钡钙水泥1d、3d和28d龄期标准砂浆抗压强度分别达到13.5、34.9和61.1MPa.借助于XRD和SEM-EDS等分析测试手段,对该水泥熟料的组成、结构及性能进行了研究.     

C3S-C2.75B1.25A3S--C2S-C3A-B2O3体系熟料组成与性能的研究

设计了C3S-C2．7581．25A3S-C2S-C3A-B2O3体系组成的水泥熟料,实验以分析纯化学试剂为原料,在1350℃煅烧并保温1h。结果表明,在该熟料体系中阿利特、硫铝酸钡钙、贝利特和铝酸三钙等矿物的最佳组成分别为50％、10％、25％和15％,B2O3的适宜掺量为2％。在最佳组成和制备工艺条件下,所制的阿利特-硫铝酸钡钙水泥的1d、3d和28d抗压强度分别达到21．3MPa、48．1MPa和80．8MPa,展现良好的早期力学性能。同时还研究了氟化钙对该体系水泥熟料的影响,并利用SEN-EDS、XRD等测试手段对熟料的组成、结构及性能进行了分析研究。     

C_3S-C_(2.75)B_(1.25)A_3-C_2S-C_3A-B_2O_3体系熟料组成与性能的研究

设计了C_3S-C_(2.75)B_(1.25)A_3-C_2S-C_3A-B_2O_3体系组成的水泥熟料 ,实验以分析纯化学试剂为原料 ,在 135 0℃煅烧并保温 1h。结果表明 ,在该熟料体系中阿利特、硫铝酸钡钙、贝利特和铝酸三钙等矿物的最佳组成分别为 5 0 %、10 %、2 5 %和 15 % ,B2 O3 的适宜掺量为 2 %。在最佳组成和制备工艺条件下 ,所制的阿利特 -硫铝酸钡钙水泥的 1d、3d和 2 8d抗压强度分别达到 2 1.3MPa、4 8.1MPa和 80 .8MPa ,展现良好的早期力学性能。同时还研究了氟化钙对该体系水泥熟料的影响 ,并利用SEM -EDS、XRD等测试手段对熟料的组成、结构及性能进行了分析研究。     

CaF2对阿利特-硫铝酸钡钙水泥合成及性能的影响

用化学纯试剂为原料,研究了CaF2对阿利特-硫铝酸钡钙水泥熟料矿物形成过程及水泥性能的影响。实验设计将具有早强性能的硫铝酸钡钙矿物引入到硅酸盐水泥熟料矿物体系中,并取代其中的C3A矿相。实验表明:适量的CaF2能改善熟料的易烧性,促进f-CaO的吸收和熟料矿物的形成。CaF2质量掺量为0.5%~1%时,有利于提高水泥的早期力学性能。CaF2质量掺量超过1.5%时,生成氟铝酸盐C11A7.CaF2,且不利于C3S和硫铝酸钡钙矿物形成。XRD和SEM-EDS分析表明,在该矿物体系中,含有阿利特、贝利特和少量硫铝酸钡钙矿物。这说明硫铝酸钡钙矿物能够和硅酸盐水泥熟料矿物复合并共存。     

矿渣掺量对阿利特-硫铝酸钡钙水泥性能的影响

研究矿渣掺量对阿利特-硫铝酸钡钙水泥性能的影响,当质量分数掺量为10%时,阿利特-硫铝酸钡钙水泥3d、28d的强度分别达到44.5MPa和77.6MPa.采用XRD、SEM等方法研究阿利特-硫铝酸钡钙水泥水化产物的组成、结构和形貌,并对该水泥的水化机理进行探讨.结果表明:当矿渣掺量质量分数为10%时,促进了该水泥的水化,有利于水泥强度的提高.     

铁相组分对硫铝酸钡钙水泥的影响

以纯化学试剂配料,经 X 射线衍射仪（XRD）、扫描电子显微镜（SEM）和强度测试,研究铁相 C6A2F、C4AF、C6AF2和 C2F 对硫铝酸钡钙水泥熟料的煅烧及性能的影响。结果表明：各生料配比试件在 1 350oС 时,熟料矿物形成较好;随铁相中Al 与 Fe 的摩尔比的减小,熟料外观颜色呈浅绿色→ 深绿色→ 黑绿色变化;熟料矿物主要生成菱形十二面体的硫铝酸钡钙和卵粒状的硅酸二钙;铁相能够促进 Ba2 +取代 Ca2 +;主要水化产物为水化硫铝酸钡钙、BaSO4和水化铝酸钙。铁相组分为 C4AF时,其 1 d 和 3 d 抗压强度分别为 73. 2 MPa 和 97. 9 MPa。     

阿利特-硫铝酸钡钙水泥熟料矿相体系的组成结构与性能

研究了以阿利特-硫铝酸钡钙为主导矿物的熟料矿相体系C3S—C2．75B1．25A3S^-—C2S—C2F,探讨了该体系的组成与匹配关系。研究结果表明,阿利特、硫铝酸钡钙这两种高低温型矿物可以在1380℃煅烧条件下共存于同一熟料中。从该矿相体系的力学性能分析可知,熟料的最佳质量分数：C2.7581．25A3S^-为55％,GS为15％,C2F为5％,C2S为25％。在该组成条件下,熟料的1d和3d抗压强度均在40MPa以上,展现了良好的快硬早强性能。影响熟料1d、3d强度的主要因素是C3S和C2.75B1.25A3S^-矿物的含量,影响28d强度的主要因素是C3S和C2F含量。同时,利用SEM—EDS和XRD分析了熟料的组成与结构。     

硫铝酸钡钙矿物水化过程的研究

硫铝酸钡钙是一种性能优良的水泥新矿物，以该矿物为基础生产了性能优良的含钡硫铝酸盐水泥。本实验采用不同量的Ba^2 取代C4A3S中的Ca^2 ，合成了一系列新型硫铝酸钡钙物。利用XRD、IR、SEM等测试手段，研究了在外掺一定量石膏条件下的水化过程，确定了系统的水化产物主要为AFt、BaSO4和AH3凝胶，得出了含钡硫铝酸盐水泥早强快硬的原因。     

不同钡矿物对制备无水硫铝酸钡钙矿物的影响

目的研究不同钡矿物对制备无水硫铝酸钡钙矿物的影响,为工业生产含钡硫铝酸盐水泥提供理论依据.方法分别采用毒重石和重晶石为含钡原材料,在1 400℃保温180 min的烧成制度下烧成硫铝酸钡钙矿物(2Ca O·Ba O·Ca SO4),使用X射线粉末衍射法对烧成熟料进行测试,并使用TOPAS软件进行定量分析.结果在全谱拟合过程中,使用毒重石制备无水硫铝酸钡钙矿物的Rw p的值为7.71%,使用重晶石制备无水硫铝酸钡钙矿物的Rw p值为12.64%,使用毒重石烧成的熟料中无明显杂质相,使用重晶石烧成的熟料中出现了11.22%的铝酸钡.结论使用毒重石制备的无水硫铝酸钡钙矿物比使用重晶石制备的矿物更为纯净.     

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