57 resultados para HR-CS GF AAS


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The geometrical parameters and electronic structures of C60, (A partial derivative C60) (A = Li, Na, K, Rb, Cs) and (H partial derivative C60) (H = F, Cl, Br, I) have been calculated by the EHMO/ASED (atom superposition and electron delocalization) method. When putting a central atom into the C60 cage, the frontier and subfrontier orbitals of (A partial derivative C60) (A = Li, Na, K, Rb, Cs) and (H partial derivative C60) (H = F, Cl) relative to those of C60 undergo little change and thus, from the viewpoint of charge transfer, A (A = Li, Na, K, Rb, Cs) and H (H = F, Cl) are simply electron donors and acceptors for the C60 cage resPeCtively. Br is an electron acceptor but it does influence the frontier and subfrontier MOs for the C60 cage, and although there is no charge transfer between I and the C60 cage, the frontier and subfrontier MOs for the C60 cage are obviously influenced by I. The stabilities DELTAE(X) (DELTAE(X) = (E(X) + E(C60)) - E(x partial derivative C60)) follow the sequence I < Br < None < Cl < F < Li < Na < K < Rb < Cs while the cage radii r follow the inverse sequence. The stability order and the cage radii order have been explained by means of the (exp-6-1) potential.

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于2010-11-23批量导入

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<正>研究了CS(偶应力)和SG(二阶梯度)应变梯度复合材料中的单夹杂问题,分别得到了无限大各向同性CS和SG应变梯度介质中含有椭球形夹杂时的Eshelby张量的解析表达式,该解析解只包含一个一维积分,是目前应变梯度椭球形Eshelby张量最简单的形式。球形夹杂、长纤维夹杂的Eshleby张量都可以由它简化得到,是其一

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用47 MeV/u 12C离子轰击133Cs靶,应用放射化学分离技术和离线γ射线谱学,得到碘同位素的产生截面。丰中子碘同位素的独立产生截面指数地依赖于Qgg值,而缺中子碘同位素的独立产生截面则偏离这一直线关系。这一事实可对在深部非弹转移过程中产生丰中子碘同位素予以解释。

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使用47MeV/u12C离子轰击133Cs靶,由多核子转移反应产生Ba同位素。使用放射化学方法,从133Cs和反应产物中分离出产物Ba,再使用高纯Ge探测器测量Ba放射性同位素的γ活性,根据Ba同位素的活度和其他相关数据,确定Ba同位素的产生截面。通过分析测得的Ba同位素的厚靶平均产生截面,发现缺中子Ba同位素的独立截面不遵从规则的Qgg系统性。该结果可用重离子碰撞中的次级过程加以解释。

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通过116Cd(14N,5n),Ebeam=65MeV的核反应布居了125Cs的高自旋态.利用在束γ谱学实验方法,进行了γ γ符合测量,使已知的125Cs核能级纲图得到了扩展,并且修正了某些组态的带头激发能.

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利用融合蒸发反应 116Cd(14 N ,4n) 12 6Cs布居了 12 6Cs的高自旋态 .观测到了 10 0多条新的γ跃迁和相应的能级 ,建立了双奇核 12 6Cs由 9个转动带构成的能级纲图 .尝试性地指定了大部分能级的自旋和宇称以及各转动带的Nilsson单粒子组态 .极大地丰富了已有的实验结果 .

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利用137Cs示踪技术对干草原地区半固定沙丘表面的蚀积规律进行了初步研究。通过半固定沙丘表面不同部位137Cs剖面分布型式及其总量与背景值样点的对比分析,认为半固定沙丘表面存在微弱的风沙活动,其中沙丘中上部表现为风蚀状态,迎风坡脚与背风坡脚均为沉积部位。这一尝试性研究为风沙地貌研究提供了新思路。