核磁共振法研究DTPA-BIN稀土配合物的溶液结构

用核磁共振方法研究了抗磁稀土配合物 Ln( DTPA-BIN) ( Ln=La,Y,Lu,Sc)的水溶液结构 . 1 H和1 3 C NMR谱的谱形特征表明 ,每一种配合物在水溶液中存在着两种以上不对称的异构体 ,异构体之间的差别较小 .并由 Y3+ 与 Gd3+ 离子半径的相似性推测出 Gd( DTPA-BIN)的溶液结构 ,即 DTPA-BIN分子提供 8个配位点 :3个骨架氮、 3个乙羧基氧及 2个酰胺氧 ,1个水分子占据另一个配位点 ,从而与 Gd3+ 形成了九配位结构 .溶液结构随中心金属离子半径不同而呈规律性变化

Effects of vegetation control on ecosystem water use efficiency within and among four grassland ecosystems in China

Through 2-3-year (2003-2005) continuous eddy covariance measurements of carbon dioxide and water vapor fluxes, we examined the seasonal, inter-annual, and inter-ecosystem variations in the ecosystem-level water use efficiency (WUE, defined as the ratio of gross primary production, GPP, to evapotranspiration, ET) at four Chinese grassland ecosystems in the Qinghai-Tibet Plateau and North China. Representing the most prevalent grassland types in China, the four ecosystems are an alpine swamp meadow ecosystem, an alpine shrub-meadow ecosystem, an alpine meadow-steppe ecosystem, and a temperate steppe ecosystem, which illustrate a water availability gradient and thus provide us an opportunity to quantify environmental and biological controls on ecosystem WUE at different spatiotemporal scales. Seasonally, WUE tracked closely with GPP at the four ecosystems, being low at the beginning and the end of the growing seasons and high during the active periods of plant growth. Such consistent correspondence between WUE and GPP suggested that photosynthetic processes were the dominant regulator of the seasonal variations in WUE. Further investigation indicated that the regulations were mainly due to the effect of leaf area index (LAI) on carbon assimilation and on the ratio of transpiration to ET (T/ET). Besides, except for the swamp meadow, LAI also controlled the year-to-year and site-to-site variations in WUE in the same way, resulting in the years or sites with high productivity being accompanied by high WUE. The general good correlation between LAI and ecosystem WUE indicates that it may be possible to predict grassland ecosystem WUE simply with LAI. Our results also imply that climate change-induced shifts in vegetation structure, and consequently LAI may have a significant impact on the relationship between ecosystem carbon and water cycles in grasslands.

空值环境下关系数据库的更新 Ⅰ：扩展关系模型及基本运算

本文从空值语义及更新操作的关系出发，提出了一种新的扩展关系模型，用以组织更新操作下的含有空值的关系数据库中的信息．同时，定义了这种模型下的基本关系代数运算．为实现空值环境下关系数据库的数据更新奠定了基础。

自治式潜水器下水回收系统

本文介绍了作者研制的一个工作水深为1000米的自治式潜水器下水回收系统.该系统在没有专用母船的条件下,下水回收4级海况下作业的自治式潜水器.

赣中周潭群石榴石、斜长石和黑云母微区化学成分特征及其地球动力学意义

周潭群变质岩中石榴石、斜长石和黑云母微区化学成分变化明显,石榴石变斑晶具典型的生长环带,由晶体中心向两侧边缘XMg 、XFe值以光滑曲线递增,XCu 、XMn值以光滑曲线递减,反映其增温过程;晶体最边缘的化学成分反映变质峰期的温度条件。通过石榴石变斑晶生长环带剖面分析,应用Grt-Bi 温度计和GASP 压力计,确定本区变质作用p T 轨迹为顺时针形式,发生于大陆碰撞造山带环境。

太湖五里湖表层沉积物中不同形态磷的分布特征

利用连续提取法(SEDEX) 详细调查了太湖五里湖表层沉积物中不同形态磷的组成和分布特征。结果显示:其中磷的含量较高,受人为污染输入的影响较大,并且已经有了一定的释放。总磷的变化范围为2105～4105 mg/ g ,平均约为2180 mg/ g。总磷主要由无机磷组成(70 %～90 %) ,大多数无机磷为CDB 溶液提取的铁结合态磷(75 %～85 %) 。CDB 溶液的n ( Fe) / n ( P) 都较小(210～513) ,说明CDB 溶液提取的铁主要是以无定形态存在的,并且铁与磷酸盐之间的吸附可能已经达到了平衡状态。除底部个别样品以外,多数样品n (Corg) / n (Norg) 较小(818～1016) ,所有样品的n (Corg) / n ( Porg) 都较大(135～320) ,表明沉积物在早期成岩作用过程中,湖泊内源自生有机质降解时有机磷优先释放。无机磷,特别是铁结合态磷,在氧化还原条件变化的情况下,能够通过沉积物—水体界面被再次释放到水体中去,这可能对湖泊的水体质量和营养状况有一定的影响。