含非热电子的自引力尘埃系统中尘埃离声波的色散

基于等离子体动理论,研究了非热电子修正的尘埃离声波(DIAW)的色散关系,分析了自引力尘埃系统中非热电子对尘埃离声波色散的影响。结果表明,非热电子和尘埃自引力对尘埃离声波色散关系具有修正效应,分析易知,离声波的相速度随着非热指数的增大而减小,而群速度随非热指数增大而增大。此外,当电子非热指数ke→∞时,该修正的尘埃离声波的色散关系回到麦氏分布的情况。研究结果可以为天体物理和实验尘埃等离子体中观测到的现象提供理论参考。     

极区中层电子数密度不均匀特征尺度与尘埃声波波长的估计

基于火箭探测数据的结果及相关理论,给出了极区中层尘埃等离子体电子数密度不均匀特征尺度与尘埃声波波长的量级,对两个量级的比较得出,电子数密度不均匀特征尺度远远大于尘埃声波波长,为采用局域均匀假设建立极区中层尘埃等离子体纵波色散关系奠定了基础．     

热尘埃等离子体中尘埃声波的调制不稳定性

通过约化摄动法,得到了描述具有2种离子温度且尘埃微粒电荷可变的热尘埃等离子体中尘埃声波的非线性薛定谔方程,并研究了热尘埃等离子体中低温离子未受扰动的数密度、低温离子温度、高温离子未受扰动的数密度、高温离子温度、尘埃微粒的温度对尘埃声波调制不稳定性的影响.结果表明,具有2种离子温度且尘埃微粒电荷可变的热尘埃等离子体中尘埃声波是调制稳定的,低温离子未受扰动的数密度是影响尘埃声波调制不稳定性的主要因素.具有2种离子温度且尘埃微粒电荷可变的热尘埃等离子体中仅存在暗孤子.     

双温非热尘埃等离子体中的孤波

使用约化摄动方法得到了高阶横向扰动下的含有双温非热离子的无磁化尘埃等离子体中的MKP方程.经数值模拟分析可知,在该尘埃等离子体中,孤波的振幅和宽度均会随系统参数变化.     

非线性尘埃声波在含有2种不同温度离子的尘埃等离子体中的稳定性问题

在无磁场的尘埃等离子体中 ,由冷的尘埃颗粒和热的电子和离子组成的尘埃等离子体 ,对于有限的小振幅的非线性波的运动可以用KdV方程描述 .对由 2种不同温度离子的尘埃等离子体中的弱二维尘埃声波 ,得到了它所满足的KP方程 .并且发现 ,在横向扰动下 ,弱的非线性孤立波在尘埃等离子体中是稳定的 .在这个系统中既存在压缩孤立波又存在稀疏孤立波     

低β尘埃等离子体中的非线性尘埃-动力学阿尔芬波

研究低β尘埃等离子体中的尘埃－动力学阿尔芬孤立波，采用Ｓａｇｄｅｅｖ势方法，在小振幅极限下，对局域尘埃－动力学阿尔芬波进行了解析和数值研究，结果表明：在等离子体中可以形成密度坑及密度隆起结构，并且随着尘埃含量的增加，密度坑得以加深，而密度隆起幅度增大。     

射频放电尘埃等离子体系统中的斑图现象

在射频放电的尘埃等离子体系统中观察到各种尘埃斑图. 按照尘埃由小到大的生长过程, 将斑图分为两个阶段: 小颗粒阶段(或尘埃云阶段)和大颗粒阶段(或尘埃晶体阶段). 具体研究了气压变化时, 不同斑图之间的演化关系. 小颗粒阶段主要介绍空洞、尘埃声波和强湍流模式. 大颗粒阶段研究了粒子自组织形成的尘埃晶格和尘埃团簇. 通过计算径向分布函数来表征尘埃晶格的静态结构. 还研究了在二维平面上不同粒子数目形成的尘埃团簇, 以及气压变化时尘埃团簇有规律的演化过程. 利用二维径向约束势下的分子动力学模拟验证了二维尘埃团簇的壳层排布规律.     

包含双温非热离子的热尘埃等离子体中的三维尘埃声孤波

研究了高阶横向扰动下含有双温非热离子的无磁化的热尘埃等离子体,使用约化摄动方法得到了(3+1)维Kadomtsev-Petviashvili(KP)方程.讨论了尘埃流体温度σ与快离子数λ(α)对尘埃声孤波性质的影响.研究结果表明,这些因素均可显著影响和改变孤波结构.系统中不仅会出现稀疏形孤波,也会出现压缩形孤波.另外,孤波的振幅随快离子数λ(α)的增大而减小,但孤波的宽度却随之增大.     

含有非热力学平衡离子和尘埃颗粒电荷变化的热尘埃等离子体中的尘埃声波

使用约化摄动法得到了描述含有尘埃颗粒电荷变化、非热力学平衡离子和玻尔兹曼分布的电子的热尘埃等离子体中尘埃声波修正的KdV(mKdV)方程.并对孤立波受尘埃流体、离子和电子的温度,非热力学平衡快离子参数,尘埃电荷变化以及尘埃颗粒、离子和电子数密度的影响进行了数值模似.     

包含双温非热离子的尘埃等离子体中的三维尘埃声孤波

考虑高阶横向扰动的因素,使用约化摄动方法得到描述含有双温非热离子的无磁化尘埃等离子体中的尘埃声波的(3+1)维KP方程.详细讨论一些尘埃等离子体系统参数如电子与非热高温离子数密度v与μh、快离子数λ(α)、低温非热离子与电子的温度比1β、非热双温离子温度比2β对尘埃声孤波性质的影响.研究结果表明:这些因素均可显著影响和改变孤波结构.在考虑双温非热离子后,稀疏形孤波与压缩形孤波的临界条件也发生极大变化.     

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.     

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     

Exciton Seebeck in Molecular Systems

Various applications relevant to the exciton dynamics,such as the organic solar cell,the large-area organic light-emitting diodes and the thermoelectricity,are operating under temperature gradient.The potential abnormal behavior of the exicton dynamics driven by the temperature difference may affect the efficiency and performance of the corresponding devices.In the above situations,the exciton dynamics under temperature difference is mixed with