22 resultados para Trafalgar, Batalla de, 1805
Resumo:
采用中温水热法合成了立方钙钛矿单相 KZn F3 及 KZn F3 ∶ Eu,通过 SEM观察了产物形态 ;XPS测定结果表明 ,产物含氧量不高 ;荧光光谱及 ESR谱表明 ,KZn F3 ∶ Eu体系中 Eu2 +与 Eu3 +共存 ,进一步讨论了不等价取代中的电荷补偿途径
Resumo:
Photoluminescence characteristics and the energy transfer between Ce3+ and Eu2+ in BaLiF3 host lattice have been investigated. A series of concentrations of Ce3+ ion with a fixed Eu2+ concentration in doubly doped BaLiF3:Ce3+,Eu2+ have been studied. According to the defects forming after Eu2+ and Ce3+ entering the host lattice, cerium ions occupy the positions of nearest neighbors of the europium ions. The energy transfer probability and critical distance are calculated. (C) 1999 Elsevier Science Ltd. All rights reserved.
Resumo:
合成了三茚基稀土配合物(η~5-C_9H_7)_3Ln·OC_4H_8(Ln=Nd、Gd、Er),经元素分析、红外光谱、水解产物核磁共振谱及质谱表征,并测得了(η~5-C_9H_7)_3Nd·OC_4H_8(1)及(η~5-C_9H_7)_3Gd·OC_4H_8(2)的晶体结构。(1)、(2)均属六方晶系,P6_3空间群,Z=2。(1)的晶体学参数为a=b=1.1843(3)nm,c=1.0304(4)nm,V=1.25165(87)nm~3,D_c=1.49g·cm~(-3),最后一致性因子R=0.049;(2)的晶体学参数a=b=1.1805(2)nm,c=1.0236(2)nm,V=1.23536(56)nm~3,D_c=1.54 g·cm~(-3),R=0.023。平均Nd-C=0.2812nm,Gd-C=0.2795nm;Nd-O=0.2557(21)nm,Gd—O=0.2459(13)nm。配合物中四氢呋喃的四个碳原子处于完全无序状态。
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Ecological and physiological features of the planktonic copepod Calanus sinicus in the southern Yellow Sea in summer were studied to reveal its life history strategy. From the coastal shallow waters to the central part of the southern Yellow Sea, a shift of the stage composition occurs from being dominated by the egg-nauplius stage to being dominated by the fifth copepodite (CV) stage. Most CVs reside in the Yellow Sea Cold Water Mass (YSCWM), where both temperature and food abundance are low. CVs in the YSCWM have longer body lengths, heavier body weights and higher carbon contents than those outside the YSCWM. Onboard incubations show that the development of CVs in the YSCWM is suspended. Energy conservation, development suspension and lack of diel vertical migration (DVM) behavior suggest a diapause status for the CVs in the YSCWM, although vertical distribution patterns indicate the CV individuals are not fully synchronous in physiology and development. This adaptive oversummering strategy would help C. sinicus to live through the warm and food-limited summer in the central part of the southern Yellow Sea; both low temperature and low food supply are necessary for CV to maintain the resting state in the YSCWM. Calanus sinicus exhibits different life history strategies in different regions of the southern Yellow Sea in summer.
Resumo:
通过对多年生植物黄帚橐吾(Ligularia virgaurea)在四个不同海拔梯度下的克隆生长行为进行研究,结果表明:(1)资源水平(土壤养分)、干扰和群落性质影响间隔物(spacer)长度的变化.在第一和第四海拔梯度中(土壤养分较丰富)间隔物长度较短,而在第二和第三海拔梯度中(土壤养分较贫乏)间隔物长度较长,说明其能对资源水平和生境优劣作出反应.(2)分枝强度(branching intensity)随资源水平的增加而上升.(3)在高海拔、寒冷和资源较丰富的生境中,其生物量的投资偏向于地下部分生物量,说明黄帚橐吾的资源分配方式受到环境资源条件和群落性质的影响.
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本文简要介绍了一个数控自动编程专家系统的自然语言接口的实现.该自然语言接口是以我们研制的数控自动编程专家系统为背景,运行在 SUN3/4 工作站的 UNIX 下和 IBM/AT 机的 DOS 下,用 C语言编程.该自然语言接口由词法分析、句法分析、语义语用分析、目标生成和图形仿真五个模块及相应的知识库构成.该接口能够接受数控编程系统所需的对工件的英语自然语言描述并处理一些比较简单的英语语言现象.
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分配模型认为疏水性有机物在土壤上的吸附过程是一种分配的过程[1,2],平衡分配系数与土壤有机碳的含量存在线性相关关系.Weber和Huang[3,4]提出土壤吸附有机污染物的三端员模式.认为无机矿物表面和无定形有机质对有机污染物的吸附以相分配为主,而凝聚态有机质对有机污染物吸附则表现为非线性的.Pignatello和Xing[5,6]指出双模式吸附模型可将土壤有机质分为溶解相和孔隙填充相两个部分;认为有机污染物在溶解相上的吸附是一个分配过程,而在孔隙填充相中的吸附则服从兰格缪尔吸附等温模型,表现为非线性.可以肯定土壤有机质是引起疏水性有机物非线性吸附过程的主要组分.因此,本研究利用现代分析方法表征土壤有机质的化学组成和结构;定量研究多环芳技烃化合物菲和萘在吸附剂上的等温吸附过程;探讨疏水性有机污染物的非线性等温吸附与吸附剂中有机质化学组成和结构之间的关系.