高校毕业生工作状况跟踪调查分析研究 --以江西医学院本科毕业生为例

通过邮寄问卷(用人单位问卷、毕业生问卷)，开展针对江西医学院本科毕业生临床工作状况的跟踪调查．以期了解该校毕业生在岗工作状况及用人单位、毕业生对教育、教学、管理工作的评价和建议，以进一步推动高等医学院校教学改革．促进教育、教学质量的全面提高。     

含一阶导数的奇异二阶两点边值问题的可解性

应用Leray—Schauder不动点定理考察了含一阶导数的奇异二阶两点边值问题的可解性。结论的主要条件都是局部的，即只要非线性项的主部在其定义域的某个有界子集上的“高度”是适当的，该问题必然存在解或者正解。     

渗调修复黄瓜陈种子基因组DNA损伤的RAPD研究

用Vc，CaCl2，PEG及其组合对自然老化的黄瓜种子进行渗调处理，利用随机扩增多态性DNA(RAPD)技术对处理前后的种子基因组DNA多态性进行比较分析．结果表明：渗调作用可以修复黄瓜陈种子的DNA损伤．修复效果与种子贮藏时间有关，贮藏半年的种子渗调处理前后RAPD产物差异不明显，贮藏1～2a的陈种子修复的效果好，表现为分子量高的DNA重新合成，RAPD扩增条带增多，亮度增加；贮藏3a的陈种子修复效果不理想。     

商场火灾危险性的评价方法

构造了针对商场类建筑的火灾危险性进行评价的模式·通过实地考察得到商场建筑设计和消防管理方面的具体资料后与《建筑设计防火规范》相对照 ,进行定性的评价 ,在此基础上利用模糊综合评判法 ,对其火灾危险性进行客观的评价·根据具体的结果判断其防火等级 ,得出商场的火灾危险性评价结果 ,针对以上结果提出改进措施·以某商业城为例进行了实际计算 ,结果合理、可行·     

强夯—塑料板排水法在粉土和粉质粘土地基加固中的试验研究

针对黄河中下游粉土、粉质粘土成层地基,通过插设塑料排水板和不插排水板条件下强夯对比试验研究,证实了插设塑料排水板可以有效的降低强夯时超静孔隙水压力峰值,加快其消散,缩短强夯施工工期;提高强夯夯沉,减少振动对土体的扰动,缩短触变恢复时间,因而人工塑料排水板在强夯处理此类地基中是十分有效的。     

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.