攀枝花地区昔格达土中钒的含量及分布

对母质为昔格达组粘土的攀枝花土壤样品数据进行了分析研究。结果表明，该区土壤中的钒普遍具有一定的地带性分布规律及剖面分布特征。一般来说，矿区土壤中的钒含量明显高于非矿区，表明该区土壤主要受采矿污染的影响；水田土壤中钒含量明显高于旱地，表明水是钒元素迁移的重要介质（载体）。钒含量在土壤剖面上的空间分布呈底层富集型，反映了成土因素的综合影响。     

准噶尔盆地南缘西部地区原油地球化学特征及油源对比

对准噶尔盆地南缘南西部地区各钻井的原油、地面油气苗、以及油砂样品进行分析化验，从其物理性质、轻烃特征、碳同位素以及生物标志物等地球化学特征进行了详尽的分析，进而通过原油及油砂、烃源岩在物理性质、轻烃特征、碳同位素以及生物标志物和成熟度等方面进行了系统的对比分析。认为准噶尔盆地南缘西部地区第三系—白垩系原油更可能是侏罗系煤系烃源岩生成的油与二叠系湖相烃源岩生成的油通过断裂或各种裂隙向上运移混合的结果。     

监控量测技术在通渝隧道出口段中的应用

重庆通渝隧道是“八小时重庆”工程的控制性工程，地质条件复杂，集涌水、岩爆、瓦斯、有害气体、塑性变形、高应力于一身，是典型的复杂条件下的长大公路隧道。在施工过程中，严格进行了新奥法监控量测指导施工，通过开挖面地质素描、拱顶下沉、水平收敛、锚杆轴向力、喷层应力、格栅拱架压力、围岩内变形、二衬应力等多项涉及围岩稳定性及支护合理与否的参数的跟踪量测，并及时将量测数据的散点、回归图等处理信息反馈给施工，以了解隧道开挖后围岩的稳定情况及采取相应的支护措施，实践证明效果可靠，隧道出口段掘进已突破l500m大关。     

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。     

Dependence of mutual information of big protein sequence

The mutual information function is used to describe the auto-correlation of amino acids in protein. We find two interesting phenomenon: (1) for any given big protein, the mutual information function l(k) is almost a const, where k is the length of gap. (2) for any two sequence similar proteins, the mutual information are nearly the same. As a consequent, we may use mutual information of protein as a character for sequences comparison. Foundation item: Supported by the National Natural Science Foundation of China (30170214) Biography: Shi Feng ( 1966-), male, Ph. D, Associate professor, research direction: bioinformatics.     

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.