关于算子迹的若干不等式

给出了算子迹的若干不等式.应用环形图方法,证明了对正的迹类算子A_i(l≤i≤m),有|T(?)(A_1A_2…A_m)|≤(?)~(1/m)≤m~(-1)·(?)T(?)(A_i~m).从而在较广范围内,给出了 Bellman 问题的肯定回答.     

神经系统患者头发中11种微量元素分析测定

使用ICP-AES方法,对人体头发中11种微量元素测定分析,取样于神经系统患者,分析结果与标样值进行对比,并初步考察人发中微量元素对神经网络的影响.     

单叶双曲面的参数方程与腰曲线

给出了单叶双曲面新的参数方程和旋转与非旋转的单叶双曲面的腰曲线方程,进而证明了旋转单叶双曲面的腰曲线是它的腰圆,非旋转的单叶双曲面的腰曲线不是它的腰椭圓,而是一条挠曲线     

自共轭矩阵和的特征值积不等式

本文给出四元数正定自共轭矩阵的一个公式及正定自共轭矩阵和的特征值积的一些不等式和Hadamard不等式的更一般形式.     

对基本对易关系式佯谬的讨论

对量子力学的基本关系式［ｘ·ｐｘ］＝ｉｈ在取迹时两边不相等的佯谬问题进行较系统的讨论，以便更好地进行教学     

Genesis of zircon and its constraints on interpretation of U-Pb age

Zircon U-Pb dating is the most commonly used method for isotopic geochronology. However, it has been a difficult issue when relating zircon U-Pb ages to metamorphic conditions in complex metamorphic rocks. Much progress has been made in the past decade with respect to the genesis of zircon and its constraints on interpretation of U-Pb age. Three methods have been proposed to link zircon U-Pb age to metamorphic conditions: ( i ) internal structure; ( ii ) trace element feature; (iii) mineral inclusion composition. Magmatic zircon shows typical oscillatory zoning and/or sector zoning, whereas metamorphic zircon has internal structures such as no zoned, weakly zoned, cloudy zoned, sector zoned, planar zoned, and patched zoned ones. Zircons formed in different geological environments generally have characteristic internal structures. Magmatic zircons from different rock types have variable trace element abundances, with a general trend of increasing trace element abundances in zircons from ultramafic through mafic to granitic rocks. Zircons formed under different metamorphic conditions have different trace element characteristics that can be used to relate their formation to metamorphic conditions. It is an effective way to relate zircon growth to certain P-T conditions by studying the trace element partitioning between coexisting metamorphic zircon and garnet in high-grade metamorphic rocks containing both zircon and garnet. Primary mineral inclusions in zircon can also provide unambiguous constraints on its formation conditions. Therefore, interpretation of zircon U-Pb ages can be constrained by its internal structure, trace element composition, mineral inclusion and so on.     

禀经酌伟 弥纶一代－《中国现代寓言史纲》读后

《中国现代寓言史纲》是陈蒲清先生《中国古代寓言史》的续篇,是又一部填补空白 的著作。他的问世,不仅完成了他中国寓言史的宏大建构,而且,通过对我国现代寓言史的全面、深入地探究、总结,将会极大地推动我国当代的寓言研究与寓言创作向前发展。     

Application of ICP-MS trace element analysis in study of ancient Chinese ceramics

Chemical analysis plays a significant role in the study of ancient ceramics[1,2]. Most ancient Chinese kilns used clays mined from the local areas and differences in the geochemistry and mineralogy of these raw materials may be expected. The chemical composition of ceramics may also be influenced by production techniques, such as processing by washing and mixing of different sorts of raw materials. These may also vary from kiln to kiln and even change over time. Thus the raw materials and pro…     

海南岛东部地区砖红壤中微量元素含量的纵向分异研究

对海南岛东部地区发育典型的6个砖红壤剖面的微量元素的组成特征及其纵向变化规律进行研究发现,土壤母质是决定砖红壤微量元素含量的主要原因,区内花岗岩砖红壤中Cu、Sr、Zn、Pb含量明显高于砂页岩砖红壤,而砂页岩砖红壤中的As含量相对较高.砂页岩砖红壤剖面中的微量元素含量的纵向变化规律具有相似性,并显示出B层>C层>A层的特征,而花岗岩砖红壤微量元素在各层中的纵向分异规律不甚明显.区内的人类活动对海南岛东部砖红壤剖面中的部分微量元素的分布具有一定的影响,农药及老鼠药的大量使用,可致使大量的As元素进入土壤表层富集,并造成土壤中As含量超标,成为区内环境的重要隐患.