Measurement of total reaction cross section for neutron-rich nucleus Li-11 on Si-28 target at medium energy

The neutron-rich nucleus Li-11 is separated by the radioactive ion beam line RIBLL at HIRFL from the breakup of 50MeV/u C-13 on Be target. The total reaction cross sections for Li-11 at energies range from 25 to 45MeV/u on Si target have been measured by using the transmission method. The experimental data at high and low energies can be fitted well by Glauber model using two Gauss density distribution. The matter radius of Li-11 was also deduced.

Li同位素的结构和性质

锂同位素的结构性质，特别是滴线核 ~(11)Li的异常特性，目前微观机制并不很清楚。本文系统地研究了锂同位素基态和低位态的性质，包括基态结合能、能谱、电磁矩和电磁跃迁性质、及β衰变性质，发现~6Li核基态的四极矩敏感地依赖于相互作用力中的张量力分量，~6Li、~7Li和~8Li核的第一激发态电磁跃迁几率增大，呈现集体性，可能是由集团结构所致，对远离核~9Li的某些态需要考虑sd-shell组态侵入的影响。在~(6-9)Li核性质系统研究的基础上，发现滴线核~(11)Li核的结构性质仍可在壳模型框架内得到解释，平均场效应是引起其奇异性质的微观起因，对于~(10)Li核的性质仍需进一步探讨。对锂同位素引进平均场的同位旋依赖项尚需近一步研究。在3

Quasi-Elastic Scattering of C-16 from C-12 at 47.5 MeV/Nucleon

Differential cross sections for the quasi-elastic scattering of C-16 at 47.5 MeV/nucleon from C-12 target are measured. Coupled-channels calculations are carried out and the optical potential parameters are obtained by fitting the experimental angular distribution.

Production cross section of neutron cluster from the reaction of light neutron rich nuclei

Within the Boltzmann-Langevin equation, the neutron cluster production cross sections in the reactions induced by Be-14, He-8, He-6, Li-11, B-17, Be-11, C-19 on C-12 at 35MeV/u were studied. The experimental data for (4)n production cross section from Be-14+C-12 at 35MeV/u can be reproduced. It is found that the production cross section of neutron cluster is large in the reaction that the projectile has more halo nucleons. And the projectiles with big mass number are easy to produce the neutron cluster, when they have the same number of halo nucleons. The neutron cluster is probably mainly from the halo nucleons of projectile.

Close correlation between the reaction mechanism and inner structure of loosely halo-nuclei

It was based on the comparisons of the variance properties of fragment multiplicities FM's and nuclear stoppings R's for the neutron-halo colliding system with those of FZ's and R's for the proton-halo colliding system with the increases of beam energy in more detail, the closely correlations between the reaction mechanism and the inner structures of halo-nuclei is found. From above comparisons it is found that the variance properties of fragment multiplicities and nuclear stopping with the increases of beam energy are quite different for the neutron-halo and proton-halo colliding systems, such as the effects of loosely bound neutron-halo structure on the fragment multiplicities and nuclear stopping are obviously larger than those for the proton-halo colliding system. This is due to that the structures of halo-neutron nucleus Li-11 is more loosely than that of the proton-halo nucleus Al-23 in this paper. In this case, the fragment multiplicity and nuclear stopping of halo nuclei may be used as a possible probe for studying the reaction mechanism and the correlation between the reaction mechanism and the inner structure of halo-nuclei.

Elastic Scattering of He-6 + p at 82.3 MeV/nucleon

Differential cross sections for the elastic scattering of halo nucleus He-6 on proton target were measured at 82.3 MeV/u. The experimental results are well reproduced by optical model calculations using global potential KD02 with a reduction of the depth of real volume part by a factor of 0.7. A systematic analysis shows that this behavior might be related to the weakly bound property of unstable nuclei.

岩浆－热液过渡阶段体系中不相容元素地球化学行为及其机制－以新疆阿尔泰3号伟晶岩脉研究为例

伟晶岩形成和演化中岩浆-热液过渡阶段物理化学性质、过铝质富挥发分岩浆体系岩浆液相不混溶、流体相出溶事件的相对时间尺度以及在岩浆-热液过渡阶段体系中稀土和其它微量元素地球化学行为(稀土“四重效应”机制和微量元素分异及控制因素等)是目前过铝质岩浆体系研究的焦点问题。对上述问题的研究和探讨，将有助于了解伟晶岩形成和演化的全过程，有助于了解挥发分(H_20、F、B、P)对过铝质岩浆体系物理性质以及对REE和其它微量元素地球化学行为影响，这对于理解过铝质岩浆体系成岩、成矿作用过程具有重大的理论和实际意义。本论文选择著名的新疆阿尔泰3号伟晶岩脉为研究对象，由于它具有完美的分带特征，使我们有可能通过各结构带矿物学、地球化学的研究揭示伟晶岩成因和演化过程以及讨论岩浆-热液过渡阶段体系中的稀土和微量元素地球化学行为。由于LCT型伟晶岩具有明显的分带性、矿物颗粒大小不均匀性等特点，因此利用全岩样品研究伟晶岩往往因取样没有代表性而被大多数岩石学家和地球化学家所否定。考虑到这点，本文系统采集阿尔泰3号伟晶岩脉各结构带磷灰石、电气石、碱性长石、石英矿物，部分结构带的石榴石、绿柱石、锂辉石矿物以及伟晶岩冷凝边和蚀变围岩的全岩样品，通过各结构带磷灰石矿物化学组成和~(87)Sr／~(86)Sr比值测定，电气石矿物的化学组成和硼同位素组成分析，碱性长石中磷含量的电子探针分析和碱性长石-石英矿物对的氧同位素体系研究以及蚀变围岩和冷凝边的化学组成分析，本文较为详尽系统地探讨以上所有的问题。通过本次多年的研究，我们获得了以下几点新的认识：f1) 富挥发分过铝质岩浆体系的样品存在稀土“四重效应”和Y-Ho、Zr-Hf、Nb-Ta、Sr-Eu元素对的显著分异，表明在过铝质岩浆演化过程中含氟流体相起着重要的作用；目前，稀土“四重效应”机制被认为是含水流体相与过铝质岩浆熔体相互作用的结果(Irber 1999；Bau 1997)，而不是独居石、磷钇矿、石榴石矿物等矿物的早期结晶引起的残余熔体稀土含量的异常变化。由于阿尔泰3号伟晶岩脉各带磷灰石以及与其共生的石榴石、绿柱石、碱性长石、锂辉石矿物均存存明显的稀土“四重效应”以及相同电价、相似离子半径的不相容元素间存在显著的分异，并结合最近赵振华等(1999)和Sba and Chappell(1999)报道S型花岗岩全岩和单矿物(磷灰石、独居石、长石、黄玉等)均存在稀土“四重效应”这一现象，本文研究提出，稀土“四重效应”是富挥发分过铝质岩浆体系的一个基本特征，其机制既不可能由含稀土的副矿物早期结晶引起残余熔体相中REE含量变化的结果，也不能定性地归因于流体相与熔体相相互作用过程中稀土元素在流体／熔体之间分异的结果，而很可能与伟晶岩岩浆形成之前某些过程密切相关，S型花岗岩岩浆在液相线以上存在硅酸盐熔体与高盐熔体(或卤水相)的不混溶液相分离有可能是过铝质岩浆体系产生稀土“四重效应”的主要原因。(2) 由于Sr~(2+)与Eu~(2+)具有相同的电价、相似的离子半径，根据经典的地球化学原理，它们具有相似的地球化学行为，在各种地质过程中其它们具有紧密的一致性。阿尔泰3号伟晶岩磷灰石中Sr／Eu比值具有二歧变化现象，其中I、Il、III和IV带磷灰石具有低的Sr／Eu比值(16:0～111.2)，而V、VI、VII带、核部带和IV带中的一个磷灰石则显示较大的Sr／Eu比值(主要在246．6～514:9范围，其中IV带的一个磷灰石该比值在10000以上)。对世界范围内的过铝质花岗岩统计表明，过铝质岩浆岩的全岩样品中的Sr／Eu也呈现二歧变化，由此本文提出Sr／Eu比值是指示过铝质岩浆体系中岩浆流体相出溶的有效地球化学参数，大于300的Sr／Eu比值是Eu~(2+)强烈分配进入流体相的地球化学标志。(3) 阿尔泰3号伟晶岩I、II、III带电气石矿物的硼同位素组成(δ~(11)B)分布在-41.11‰～-30.90‰之间，V、VI、VII带电气石矿物硼同位素组成(δ~(11)B)在-15.23‰～-9.20‰范围，IV带电气石硼同位素分布于-39.19～13.10‰范围，如此大的硼同位素分馏无法根据实验研究获得的熔体／流体相间的分馏系数进行合理解释。我们的研究表明岩浆成因电气石的B同位素组成与电气石化学组成具相关性，随电气石Y位上AI、Li阳离子数的增大，δ~(11)B值显示明显增大的趋势。阿尔泰3号伟晶岩最初形成的结构带中电气石的B同位素组成是目前所发现的最低值之一(-41.1l～39.01‰)，指示形成伟晶岩脉的初始岩浆可能由含非海相蒸发岩的泥质岩经变质深熔作用形成，或是伟晶岩岩浆在上侵定位过程中同化了含非海相蒸发岩地层的结果。本次研究利用电气石-白云母和电气石-四硼酸盐矿物间的同位索分馏以及熔体相-流体相间的同位索分馏，合理解释了阿尔泰3号伟晶岩脉电气石B同位素分馏过程，并首次获得伟晶岩形成、演化过程中B同位素组成演化的全程图谱。(4)伟晶岩岩浆形成和演化过程是否存在由过磷引起的液相不混溶现象未见确凿的岩石学和实验地球化学证据。阿尔泰3号伟晶岩脉糖粒状钠长石带(II带)明显由两种不同组构的岩性组成，而且该带是3号脉主要的Be矿化带，也是P、REE最重要的沉淀场所。阿尔泰3号伟晶岩脉梳状结构带和I带的碱性长石具较高P含量(平均值分别为0.42 wt％和0.22 wt％)，随着岩浆的演化进行，从III带到核部带，碱性长石中P含量逐渐增大(平均值由0.21 wt％增至0.50 wt％)，而II带碱性长石中异常低的P含量(平均值为0.08、wt％)是该带大量磷灰石矿物饱和结晶，导致残余熔体相中P极度亏损所造成的，而不是晚期出溶的岩浆热液交代形成的。根据Watson (1978)、Ryerson and Hess(1980)在液相线以上温度下实验研究获得的微量元素在不混溶的基性和酸性液相中分配特征，以及Webster et a1．(1997）对德国Ehrenfriedersdorf矿区伟晶岩石英中熔体包裹体的研究成果，我们推断在富磷岩浆体系中，在其演化的早期将出现由磷引起的液相不混溶作用，它对伟晶岩成岩和Be的成矿具有重大的影响。

中能区丰中子核~(11)Li的反应总截面的测量(英文)

利用HIRFL提供的50MeV/u的~(13)C束流轰击Be靶,通过RIBLL选择出放射性核素~(11)Li.实验采用透射法测量了25—45MeV/u的~(11)Li在~(28)Si靶上的反应总截面.采用双参数Gauss密度分布形式,利用Glauber模型很好地拟合了高能和中能区的~(11)Li实验数据,并从密度分布中提取了核的物质均方根半径.

晕核~(11)Be和~(11)Li的能谱

基于自相似结构壳模型,并考虑到单粒子轨道的均方根半径的振动,提出了尺度共振模型。在尺度共振模型中,考虑了晕中子轨道的尺度共振和核实表面的尺度共振。用尺度共振模型成功地计算了~(11)Be和~(11)Li的激发谱。

太行花属（Taihangia Yu et Li）种质资源的研究

本文报道了太行花属（Taihangia Yu et Li）的种群分布、生物学特性和离体培养的初步结果。 太行花种群由于环境和生物等方面的原因仅在太行山区有狭小分布。来源于不同地区种群的太行花其形态特征具有丰富的表型，在引种条件下更为显著。而酯酶同工酶和过氧化物酶同工酶分析进一步证实了其遗传的稳定性和同源性。 实验表明，太行花在北纬39°58'，最低温度-11℃的北京北京植物园，露地越冬正常。温度提高至40℃时生长发育受抑制而迟滞，以25℃最为适宜，增殖率最高。太行花对土壤的适应范围较广，在泥炭培养土上移殖的幼苗成活率达97.20%，主根须根发达，叶生长良好。不同强度光照处理12000Lux效果最好。 太行花生育期为230多天，生长积温为3763℃左右。物候期受环境条件和当年气候的影响，不同种群和个体之间有一定的差异。花的性别、花期和开花量等与纬度、海拔主要与温湿度相关。 太行花的茎尖、花芽、花梗、萼片、花瓣和叶子等外植体均能在MS附加不同种类和浓度植物激素的培养基中分化，其分化途径和分化效果因附加成分、外植体类别而异。在含有0.1mg/L IAA和0.5mg/L 6-BA的培养基中，不但能启动花芽正常生长、开花、形成合子胚，而且也能诱导花芽、花梗、茎尖产生花芽和营养芽。在芽的继代培养中，细胞分裂素能大量诱导芽的分化，最好的配比是0.5mg/L 6-BA、0.1mg/L ZJ;只含生长素时可以诱导生根或脱分化，其中生根最好的是0.5mg/L IAA;2.4-D单独使用时，能较好地使花芽、叶等脱分化，其最佳浓度为1.0mg/L。

Distribution and morphology of two endemic gomphonemoid species, Gohphonema kaznakowi Mereschkowsky and G-yangtzensis Li nov sp in China

The morphology of Gomphonema kaznakowi Mereschkowsky was investigated using light microscopy. This species has two morphologically distinct areas near the headpole; an unornamented and an ornamented area. The two areas are distinguished from each other by the combination of size and striae number. A new species, Gomphonema yangtzensis Li nov. sp. is identified based on an ornamented area near the headpole. G. kaznakowi is reported from the upper and middle part of the Yangtze River, and was also found in the upper section of the Yellow River. G. yangtzensis was found in the upper area of the Yellow River and the middle of the Yangtze River. Their limited distribution may be due to certain environmental conditions or a different dispersal rate. Both species are illustrated.

Luminescence study of (11(2)over-bar0) GaN film grown by metalorganic chemical-vapor deposition

Investigations on photoluminescence properties of (11 (2) over bar0) GaN grown on (1 (1) over bar 02) Al2O3 substrate by metalorganic chemical-vapor deposition are reported. Several emission lines not reported before are observed at low temperature. The sharp peak at 3.359 eV is attributed to the exciton bound to the neutral acceptor. Another peak at 3.310 eV represents a free-to-bound, probably a free electron-to-acceptor, transition. The 3.241 and 3.170 eV lines are interpreted as phonon replica lines of the 3.310 eV line. The phonon energy is 70 meV, consistent with the energy of transverse optical E-1 phonon. The optical properties of the lines are analyzed. (C) 2003 American Institute of Physics.

Multi-electron processes in 4.15-11.08 keV/u(13)C(6+) on argon collisions

The relative partial cross sections for C-13(6+)-Ar collisions at 4.15-11.08 keV/u incident energy are measured. The cross-section ratios sigma(2E)/sigma(SC), sigma(3E)/sigma(SC), sigma(4E)/sigma(SC) and sigma(5E)/sigma(SC) are approximately the constants of 0.51 +/- 0.05, 0.20 +/- 0.03, 0.06 +/- 0.03 and 0.02 +/- 0.01 in this region. The significance of the multi-electron process in highly charged ions (HCIs) with argon collisions is demonstrated (sigma(ME)/sigma(SC) as high as 0.79 +/- 0.06). In multi-electron processes, it is shown that transfer ionization is dominant while pure electron capture is weak and negligible. For all reaction channels, the cross-sections are independent of the incident energy in the present energy region, which is in agreement with the static characteristic of classic models, i.e. the molecular Coulomb over-the-barrier model (MCBM), the extended classical over-the-barrier (ECBM) and the semiempirical scaling laws (SL). The result is compared with these classical models and with our previous work of C-13(6+)-Ne collisions