2-维磁流体议程组整体经典解

利用分析技巧得到磁流体力学方程组新的对称形式.在此基础上,在初始密度趋于真空状态假设下,利用处理双曲方程组的方法证明了经典解的局部存在性,进而得到了经典解的整体存在性.     

地理信息系统在环境监测中的应用

地理信息系（Geographic Information System简称GIS）是一项以计算机为基础的新兴技术，是管理和研究空间数据的技术系统。在太原市环境保护局综合信息管理系统中，我们采用MapObjects建立太原市环境监测地理信息系统，主要介绍了太原市环境地理信息系统的功能及其实现过程中的几个关键技术。     

计算同杆双回输电线路潜供电流与恢复电压的二次模方法

提出了利用二次模变换计算同杆双回输电线路潜供电流与恢复电压稳态值的方法.该方法首先利用变换矩阵T进行相模变换,将相量转化为模量,在此基础上再利用变换矩阵H进行第二次模变换,将一次模量转化为二次模量,然后在二次模域中建立计算潜供电流与恢复电压的数学模型.该模型与一次模方程相比,方程和未知数的个数减少了一半, 使得计算量减少,且易于编程实现.对某实际线路进行了计算,其结果与EMTP计算结果一致,表明此方法为进行潜供电流和恢复电压稳态计算提供了另一种途径和选择.     

SPN结构线性层的设计

SPN结构是一种流行的分组密码总体结构；差分和线性分析是攻击分组密码的最强有力的方法．章介绍了SPN结构研究的最新进展，着重论述如何用矩阵方法设计抗差分和线性分析的线性层．     

一种还原糖自动检测系统

根据生化反应的基本原理,利用MCS-51单片机开发设计了一种还原糖自动检测系统.介绍了该系统的硬件和软件设计模式,其特点是结构简单、操作方便,是还原糖检测的一种新方法.     

Initial organic geochemical investigation on Late Neoproterozoic-Early Cambrian sediments in the Yangtze region, China

Totally 19 samples of typical Upper Proterozoic-Lower Cambrian sedimentary rocks were collected and analyzed for an organic geochemical investigation. Almost all these rocks have high TOCs, super-maturities and similar biomarker distribution. As an exception, however, the Sinian Nantuo Tillite shows much lower TOCs and little phytane and pristane in comparison with those in other strata, which implies a very faint photosynthetic process, and a restricted euphotic zone and quite limited sunlight within the sedimentary water column during the Sinian glaciation age in the western Yangtze region providing an evidence for palaeo-oceanic environment of the Neoproterozoic Snowball Earth age.     

从果子狸谈起——从SARS的流行省思人与自然的关系

果子狸是SARS病毒的宿主之一 ,野生动物是人类SARS的毒源。人工驯养野生动物 ,让人造的化学成分进入了大自然本来的生物过程 ,其产生的危害给世人带来了生态性的灾难。人类要善待自然 ,慎用科技 ,让人的自然体在大自然中正常生息才能达致人与自然的和谐。     

Combustion energies and standard molar enthalpies of formation for the complexes of the first-row transitional metal chlorides withL-α-histidine

Seven novel solid complexes of the first-row transitional metal with L-α-histidine were synthesized, and their compositions were determined. The constant-volume combustion energies of the complexes were measured by a precision rotation bomb calorimeter. The standard molar enthalpies of combustion and the standard molar enthalpies of formation were calculated. The results indicated that the plots of the standard enthalpies of formation against the atomic number of the metal show a regularity of zigzag.     

Design and application of 60mer oligonucleotide microarray in SARS coronavirus detection

In April 2003, a novel coronavirus[1,2] which was associated with cases of Severe Acute Respiratory Syn-drome (SARS) was first isolated and sequenced in Canada. The genome of SARS coronavirus (SARS-CoV) is 29727[3] nucleotides in length and has 11 known open reading frames (ORFs). Although the genome organiza-tion of this virus is similar to that of other coronaviruses, phylogenetic analyses and sequence alignment show that SARS-CoV is not closely related to any of the previously ch…     

Temperature variations on the Tibetan Plateau over the last two millennia

The paleoclimate data recovered from ice cores,tree rings and lake sediments indicate regional features of cfimatic change on the Tibeta n Plateau (TP) during the last 2000 years. The composite temperature reconstructions in-dicate that several main climatic episodes, such as the “LittleIce Age“ between 1400 and 1900, the “Medieval Warm Pe-riod“ in 1150-1400, a less warm period in 800-1100, and an earlier cold period between the 3rd and 5th centuries,occurred in the TP. In addition, temperature varied from region to region. The period from AD 800 to 1100, which waswarm in northeastern TP, was contemporaneous with cool-ing in the western and southern TP. The southern TP ex-perienced warming between 1150 and 1400. For western TP,the δ^18O records of the Guliya ice core indicate that the pe-Hod 1250-1500 witnessed a clear warming. Large-scaletrends in the temperature history from northeastern TP aremore similar to those in eastern China than are the trendsfrom the Guliya ice cap far to the west and southern TP. The most prominent similarities between the temperature varia-tions of the TP and eastern China are such cold phases as 1100-1150, 1500-1550, 1650-1700 and 1800-1850, andthe latter three cold events match with three widespreadg lacial advances which occurred on the TP during the Little Ice A2e.