M型(Ca_xSr_(1-x)Fe_(12)O_(19))与W型(Ca_xSr_(1-x)Fe_(18)O_(27))六角铁氧体的研究

Ca离子在M型(Ca_xSr_(1-x)Fe_(12)O_(19))和W型(Ca_xSr_(1-x)Fe_(18)O_(27))六角铁氧体中的最大固溶量X_m≈0.5,在固溶量范围内,Ca~(2 )离子代换Sr~(2 )离子对本征磁性能如居里温度θ_f,比饱和磁化强度σ_s,以及磁晶各向异性场H_A没有明显的影响,因此有可能在不使这两种类型的钙锶铁氧体的磁性能变坏的情况下降低成本。     

BaMnZnCoTi-W型铁氧体微波吸收特性的研究

对用Ｃｏ２＋,Ｔｉ４＋置换Ｆｅ３＋的ＢａＭｎＺｎ－Ｗ型平面六角晶系微波铁氧体吸收材料的制备和吸收性能进行分析研究,发现涂层厚度为１．０６ｍｍ在７－１２ＧＨｚ频率范围内有三个吸收峰,峰值最高达３４ｄＢ以上;同时比较了在相同工艺条件下,随着Ｃｏ２＋,Ｔｉ４＋含量的增加,材料的吸收频率特性和涂层厚度的关系。     

BaMnZnCoTi-W型铁氧体微波吸收特性的研究

对用Ｃｏ２＋,Ｔｉ４＋置换Ｆｅ３＋的ＢａＭｎＺｎ－Ｗ型平面六角晶系微波铁氧体吸收材料的制备和吸收性能进行分析研究,发现涂层厚度为１．０６ｍｍ在７－１２ＧＨｚ频率范围内有三个吸收峰,峰值最高达３４ｄＢ以上;同时比较了在相同工艺条件下,随着Ｃｏ２＋,Ｔｉ４＋含量的增加,材料的吸收频率特性和涂层厚度的关系。     

用Sol-gel法制备掺杂的锶铁氧体的结构研究

采用溶胶-凝胶法（Sol-gel法）制备镧钴掺杂的纳米锶铁氧体（Sr1-xLaxFe12-yCoyO19）,使用X射线衍射仪、振动样品磁强计、阻抗自动测量仪（LCR电桥）对掺杂的锶铁氧体进行表征,对其结构、相变进行研究。实验结果表明,温度高于850℃时样品为稳定的M相结构,在掺杂的样品中发现了磁导率减落现象,证实了Co^2＋离子进入到六角晶体的晶位中。     

新型NTC热敏电阻材料：Mn基铁氧化的研究

研究了Ｍｎ基铁氧体的阻温特性，讨论了过铁含量，Ｔｉ＾４＋离子及工艺对Ｍｎ基铁氧体电阻率ρ和材料参数Ｂ的影响，通过改变铁离子氧化状态，掺杂及淬火工艺，改善Ｍｎ基铁离子氧化状态，掺杂及淬火工艺，改变Ｍｎ基铁氧体的整体的整体电阻率ρ和材料参数Ｂ。     

短切碳纤维-铁氧体填充的复合材料吸波性能

使用溶胶凝胶法制备了一种M型掺杂六角铁氧体，研究了该铁氧体、短切碳纤维以及玻璃纤维制成的单层和双层复合材料的微波吸收性能．结果表明：铁氧体和短切碳纤维混合填充的复合材料反射率在-10．0dB以下的有效带宽为3．5GHz；而以玻璃纤维复合材料作为面层的双层结构吸波材料在9．8～18．0GHz范围，有效带宽达到8．2GHz．     

磁记录用的BaFe_（12－2x）CoxTixO_（19）微粉的晶化特性研究

采用玻璃晶化法制备适合磁记录用的Ｃｏ－Ｔｉ替代型钡铁氧体ＢａＦｅ_（１２－２ｘ）Ｃｏ_ｘＴｉ_ＸＯ_（１９）（ｘ＝０，０．５，０．６，０．７，０．８，０．８５，０．９）微粉。动态（变温）Ｘ射线衍射和ＤＴＡ曲线分析表明，在非晶薄片基体的晶化过程中，随热处理温度的升高，首先晶化出ＢａＢ_２Ｏ_４和Ｂａ_２Ｂ_２Ｏ_７相，随后出现钡铁氧体相；温度到达８５０℃后，非磁性相消失，仅剩有磁性的钡铁氧体相．晶化过程为先成核而后长大。有关晶化条件对钡铁氧体微粉粒子尺寸及分布的影响、对形貌的影响也作了详细的探讨。     

甚高频片式电感用低温烧结平面六角软磁铁氧体的电磁性能

采用BPb玻璃为助烧剂，870℃烧结Y型平面六角结构软磁铁氧体，分析其烧结工艺、显微结构及起始磁导率和介电常数的频率特性。研究发现，含Co、Zn、Cu的Y型铁氧体材料(Ba2Me2Fe12O22，Me=Co、Zn、Cu)在甚高频段具有良好的磁性能，采用BPb玻璃为助烧剂可有效地实现此种材料的低温烧结，并大大改善其介电性能。     

用铁砂研制铁氧体电波吸收材料

以铁砂为原料制备一种尖晶石型铁氧体电波吸收材料,在７－１２ＧＨｚ范围,发现有两个吸收峰,吸收量在９－１３ｄｂ;将铁氧体吸收体和铁砂吸收体组成复合电波吸收材料,亦有两个吸收峰,一峰向低频区偏移,吸收量增至１４．５ｄｂ;以复合吸收体为基础材料,在其中添加六角铁氧体和稀土元素,可改变吸收峰位置,提高吸收量,最大可达２７ｄｂ。     

六角结构磁铅石铁氧体吸波机制的设计与研究

利用离子复合取代和控制物相平衡转化的方法，制成六角结构磁铅石多元铁氧体吸波材料，用于航空、航天隐身技术与抗电磁辐射技术。文中探讨了吸波机理以及测定了吸收体晶结构，并说明吸收频率与厚度等诸参数关系。文中采用宏面与微观相结合的分析方法，其结果与设计相符。     

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.     

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.     

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.     

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。     

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.