茁霉多糖发酵工艺条件研究

以出芽短梗霉为生产菌株，蔗糖为碳源进行发酵生产茁霉多糖．通过摇瓶实验，确定了该菌株的发酵条件，并对发酵条件进行了优化，在此条件下，获得了较高的多糖产量．实验表明，摇瓶转速和发酵初始pH值是多糖发酵的重要影响因素，它们与多糖的合成密切相关．     

冻干法制备乳酸菌发酵剂工艺条件研究

对乳酸菌冻干发酵剂的制备工艺进行了初步探索，通过对乳酸菌液体摇瓶培养中的参数和超滤浓缩特性参数测定，确定了发酵剂冻干制备的工艺参数．由于乳酸菌冻干发酵剂有着广泛应用，因此，本工艺在实际上有一定的参考价值。     

松嫩平原西南部--半湿润地区/半干旱地区再议

本文仅就松嫩平原西南部，对以往的区划方案中把其归为半湿润地区有不同认识，并分别从区划原则、区划方法、区划指标上论述其应归属于半干旱地区的合理性。进一步提出了该区的土地利用发展方向。     

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。     

点、边带约束成本的最短路问题及其算法

提出了点和边都带有成本约束的最短路问题，证明了该问题是NP－完全的，建立了这类问题的数学规划模型，并采用拉格朗日松弛算法对模型进行求解，给出了次梯度优化求解算法的一般步骤，考虑到算法在实际求解过程中收敛速度较慢的问题，进一步对拉格朗日松弛算法进行了2个方面的改进，一方面确定适当的迭代步长，另一方面选择较好的迭代方向，算法实例表明，改进后的拉格朗日松弛算法迭代步数显著较少，证明算法是有效的。     

Lightning activity on the central Tibetan Plateau and its response to convective available potential energy

Lightning flash activities on the central Tibetan Plateau have been studied by using the satellite-based Lightning Imaging Sensor(LIS)database from January 1998 to July 2002.The lightning activity shows a clear diurnal variation on the central Plateau.The peak lightning activity appears at about 17:00 which is 3 h earlier than that in Jingxhou,Hubei in the same latitude belt nearby,indicating that the lightning activity is a sensitive indicator of solar heating on the Plateau.The lightning discharge is weaker on the Plateau than Jingzhou.Hubei and other low-altitude continental regions because of the lower convective available potential energy(CAPE)on the Plateau.The CAPE on the Plateau is 12 times lower than that in Jingzhou,Hubei,and 20 times lower than that in the sea-level region,such as Guangzhou and Florida.However,the sensitivity of lightning activity to CAPE changes on the Plateau is up to 30 times more sensitive than other prominent low-altitude regions.     

C－isotope composition and significance of the Sinian on the Tarim plate

102 samples of limestones,mudrocks shales and tillites from the Sinian in Kuluketage have been analyzed ,Four formations in the Sinian belong to glacial deposits in which the differences in δ^13C are distinct (-14.7‰- 4.2‰),Distinctly negative δ^13C excursions for three times support the viwe of three glacial deposits in this area suggested by previous authors,except for the durations of them ,δ^13C values are generally positive in the Beiyixi Formation of lower part of the Lower Sinian ,representing probably the rock records of a continental rift related to break-up of the Rodinian supercontinent,There are three times of distinct excursions of δ^13C curve in all strata,The first one is from positive values at the bottom to about -5‰ at the top of the Beiyixi Formation ,The second one,from 0‰-3‰ in the Arletonggou Formation of upper part of the Lower Sinian to -3.4‰---14.4‰ in the Teruiaiken Formation.The third one,from positive values in the Zhamoketi Formation of lower part of the Upper Sinian to negative values in glacial varves at the top of the Hankeerqiaoke Formation.     

A new Euprox from the Late Miocene of Yuanmou,Yunnan Province,China,with interpretation of its paleoenvironment

The Yuanmou Basin of Yunnan Province is a hotspot for the research of early homind evolution and its environmental background.During the implementation of the Program“Research of the Origin and Evolution of Early Man and Its Environmental Baqckground” from 1998 to 2001,a huge quantity of hominoid and mammal fossils were collected.The present report systematically describes an Euprox robustus sp.nov.identified during the recent laboratory work on the collected material.Euprox is a group of earliest cervids with true antlers.The new species is the third one of the genus discovered in China.Judged by its morphologic characteristics,the new species feed on juicy and tender leaves of dicotyledon.It implies that the vegetation of its epoch in the Yuanmou Basin is a kind of southern subtropical evergreen forest and the climate is humid and temperate with evident seasonality.The latter is mostly influenced by the monsoon and secondly by the latitude.     

Inorganic chemical composition and source signature of PM2.5 in Beijing during ACE-Asia period

Aerosol samples for PM2.5 were collected in Beijing for 38 consecutive days from March to April 2001 using an IMPROVE Sampler. Concentrations of 20 elements in PM2.5 were determined using a PIXE method. Results show that the average mineral dust concentration of PM2.5 was 14.6 Ilg/m3 during the observation period. On the sand-dust event days of March 21 and April 10, dust PM2.5 mass concentrations were 62.4 and 54.1 μg/m^3, respectively.These demonstrate that fine particle pollution by dust event in Beijing was very severe. The enrichment factors of S and Cu reached minimums on the dusty days and were high on the non-dusty days. It is considered that enrichment factors of elements in PM2.5, which are associated with human activities, can probably provide an effective method to distinguish local sources from external sources of dust. Factor analysis on the chemical composition in PM2.5 shows that sources of crustal matters, anthropogenic emission, and oil combustion contributed to PM2.5 levels in air in the springtime of 2001 in Beijing.     

Progress in the study of tectophysicochemistry

Tectophysicochemistry is a research area that deals with the interrelations between physical and chemical changes of crustal materials caused by tectonism. A given tectonic force may be resolved into two parts: homogeneous stress and differential stress. Homogeneous stress refers to isotopic pressure, which is superimposed on the original pressure and affects the equilibrium of various chemical reactions. It is also a factor that influences petrogenesis,metallogenesis and metamorphism. Differential stress is commonly produced when external forces act on a given solid body. It may cause deformation of crustal materials and generate various kinds of structural features. Tectophysicochemistry pays special attention to pressure, temperature and other physicochemical conditions produced or induced by tectonism and studies the influences of additional tectonic parameters on various chemical equilibria, so it gradually develops into an independent area of science.