金属间化合物SmFe11-xMnxTi的结构和磁性

研究了Mn部分替代SmFe11-xMnxTi中的Fe对化合物结构和磁性的影响,利用真空电弧熔炼和真空热处理制备了SmFe11-xMnxTi（x=2．0,3．0,4．0,5．0,6．0）化合物样品,室温粉末样品的X射线衍射扣热磁曲线测量表明：2．0≤x≤6．0成分范围内的SmFe11-xMnxTi化合物具有ThMn12型结构,且具有良好的单相性．随着Mn替代量的增加,单胞体积增大,所有上述成分范围的化合物都存在自发磁化现象,SmFe11-xMnxTi化合物的居里温度随Mn替代量的提高迅速下降,化合物在4．4K温度下的饱和磁矩和过渡金属次晶格磁矩随Mn替代量的增加而单调减小。     

金属间化合物ErFe12-xMnx的结构和磁性

研究了Mn对金属间化合物ErFe12-xMnx的结构和磁性的影响。2．0≤x≤5．0成分范围内的ErFe12-xMnx化合物具有单相ThMn12型结构。晶格常数α和c及单胞体积V随Mn成分的增加而增大。ErFe10Mn2和ErFe9Mn3化合物的热磁曲线上出现了自旋重取向转变,ErFe8Mn4化合物的热磁曲线上出现了补偿点。随着Mn成分增加,居里温度TC单调降低,过渡金属次晶格磁矩μT单调减小。     

DyFe11-xMnxTi赝三元化合物的结构和磁性

研究了Mn部分替代DyFe11Ti中的Fe对化合物结构和磁性的影响.利用真空电弧熔炼和真空热处理制备了DyFe11-xMnxTi(1.0≤x≤5.0)化合物样品.X-射线衍射和热磁曲线测量表明:用Mn部分取代DyFe11 Ti中的Fe仍保持ThMn12型结构,且具有较好的单相性;晶格常数a和单胞体积V随Mn含量的增加而增大;在DyFe7Mn4Ti化合物的热磁曲线上观察到了补偿点;随着Mn含量的增加,化合物在4.4 K温度下的饱和磁化强度逐渐减小,在某一成分点为零.而后随Mn含量的继续增加而增大.     

TbFe10.5-xMnxMo1.5化合物的结构和磁性

用X射线和磁性测量研究了Mn替代Fe对TbFe10.5-xMnxMo1.5型金属间化合物的结构和磁性的影响。X射线衍射表明：TbFe10.5-xMnxMo1.5(x=1．5，2．0，3．0，4．0，5．0)化合物均为TnMn12型四方结构，晶格常数和单胞体积均随Mn含量增加而增大。磁性测量表明：TbFe10.5-xMnxMo1.5（x=1．5，2．0，3．0，4．0，5．0)化合物的居里温度和过渡金属次晶格磁矩随Mn含量的增加而逐渐降低；x=3．0化合物的热磁曲线上出现一个非零磁矩的类似补偿点；在4．5K温度下，化合物的饱和磁矩随Mn含量的增加而缓慢减小；x=3．0时达到最小值，然后又随Mn含量的增加而迅速增大。     

ErFe_(11-x)Cr_xTi化合物结构和居里温度研究

通过X射线衍射和磁测量手段研究ErFe11-xCrxTi(x=0,0.5,1.0,1.5,2.0,2.5,3.0)化合物的晶体结构与居里温度.结果表明:ErFe11-xCrxTi化合物均为ThMn12型结构.Cr对Fe的替代导致单胞体积和晶格参数c的单调减小以及晶格参数a的复杂变化,这可能与Cr的择优占位有关;同时,随着Cr替代量x的增加,ErFe11-xCrxTi化合物的居里温度单调下降,这可能是Cr的替代引起3d次晶格中铁磁交换作用削弱和Cr择优占位共同作用的结果.     

金属间化合物RFe8Mn4的结构和磁性

通过X射线衍射和磁测量研究了金属间化合物RFe8Mn4（R＝Y,Gd,Ho和Er)的结构和磁性。所有这些化合物都具有单相ThMn12型结构,其晶格常数a,c和单胞体积V随原子序数增加而减小。HoFe8Mn4和ErFe8Mn4化合物的热磁曲线上出现了补偿点,补偿点温度分别为95K和70K左右。本文还给出了这些化合物的居里温度和饱和磁化强度。     

Tb3Fe（29-x）Crx（2.5≤x≤6.0）化合物的结构和室温特性

采用真空电弧熔炼法制备了Tb3Fe29-xCrx(2.5≤x≤6.0)系列化合物,采用X射线衍射和磁性测量等方法研究该系列化合物的结构和磁特性.实验结果表明,Cr含量在2.5≤x≤6.0时化合物保持Nd3(Fe,Ti)29型单斜结构,属于A2/m空间群.Tb3Fe29-xCrx系列化合物晶胞体积V随Cr含量增加而增加.随着Cr含量的增加,化合物的居里温度TC单调减小,低温自发磁化强度M0和饱和磁化强度Ms降低,各向异性场Ba先增加后降低,在x=3.5处出现极大值.     

Mn_5Ge_(3-x)Cu_x系列化合物的结构和二级相变特性

采用流动氩气电弧熔炼和高温退火法,制备了Mn5Ge3-xCux(x=0.0-0.2)化合物,并用粉末X-射线衍射研究了该系列化合物的晶体结构.结果表明:这些化合物都具有Mn5Si3型六角结构,空间群为P63/mcm;Cu对Ge的替代不改变化合物的晶体结构;晶格常数a和晶胞体积V随着Cu含量的增加而增加,而晶格常数c略微减小.用Lakeshore 7407型振动样品磁强计对每个化合物在低场(0.05T)下进行热磁测量,确定了居里温度和磁相变.结果表明,随着Cu含量的增加,化合物的居里温度几乎不变,其磁相变属于铁磁-顺磁二级相变.     

Mn掺杂的TiO2粉体的结构和磁性

采用溶胶-凝胶法制备了过渡金属Mn掺杂的TiO2基稀磁半导体粉末.XRD结果表明,所有样品均为锐铁矿结构,不存在任何杂相,且随掺杂浓度的增大,品格常数单调减小,表明Mn替代Ti进入晶格形成稀磁半导体结构.采用VSM检测样品磁性,x=0.06,0.08的样品显示为室温顺磁性,x=0.12的样品在刚加外磁场时,饱和磁化强度随磁场强度的变化类似铁磁材料的情形,但与铁磁材料不同的是随着H的增加,M并没有趋于饱和,而是像顺磁材料那样M随H的增加而线性增加.     

Nd3Fe29—xTix（x=1.3—2.0）化合物的成相范围及其温度特性

用热磁测量和X－光衍射谱研究了Nd3Fe29-xTix化合物的成相范围及其温度特性，研究发现，x=1.3-2.0范围内的所有化合物都成单相，其晶体结构具有A2／m空间群的单斜结构，随着Ti含量的增加，晶格参数a,b,c几乎不变，而晶胞体积V略微增加，每个样品都出现了自旋重取向现象，但自旋重取向温度Tsr和居里温度Tc几乎不随Ti的含量而改变。     

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.