尖晶石中He离子辐照缺陷的演化及其对重金属原子的俘获效应研究

本项工作利用多种分析手段（FTIR、TDS、RBS/C、AFM、SEM），对100keV He离子不同剂量（0.5，2.0，8.0×1016cm-2）注入的尖晶石中缺陷的形成及其对重金属原子的俘获效应进行了研究。在FTIR谱上观察到了Al-O键的共振吸收峰随剂量增加向小波数方向移动和随退火温度升高向大波数方向回复；随退火温度增加这三组样品的晶格损伤均经历先增大后减小的过程，但随剂量不同晶格损伤开始增加的温度不同；注入剂量为2.0×1016 cm-2样品在退火过程中其表面发生了形变，随剂量增加样品表面发现起皮现象。上述差异被认为是样品中不同缺陷的形成所引起的。随后，尝试了利用He离子注入形成的空位型缺陷俘获重金属原子的方法在尖晶石中合成金属纳米颗粒。吸收光谱上SPR吸收峰的出现，证实了金属纳米颗粒的形成

在线He-喷嘴β-反冲飞行时间质谱仪的研制

本论文阐明了He-喷嘴反冲传输系统设计及其机制，并将它用于β-反冲飞行时间测量中构成-名在线He-喷嘴β-反冲飞行时间质谱仪装置。该装置对于探索高温难熔金属元素，鉴别其质量具有潜在的能力，预计在对远离β稳定线核素的探索及其质量数的鉴别中发挥作用。通过离线实验测定了0.189μg ~(252)Cf源的自发型裂变碎片的传输特征，得到了各种情况下装置运行的最佳参数，同时利用该装置在线测定了0.135 + 0.189 μg ~(252)Cf的裂变碎片的飞行时间谱。质量数为100左右的核素很好地分开，并给出了实验结果及其讨论。最后在附录中提出了提高谱仪性能的改进建议

Li蒸气电荷交换负He离子源的设计与调试

本论文分别从离子源的历史发展，负He离子的产生机理，设计思想及调试运行等方面描述了锂蒸气电荷交换负He离子源。该离子源可以引出1μA以上的He~-离子流，可连续稳定运行十二小时以上。本文研究了其性能，获得了束流强度随蒸气温度、引出电压的变化规律，并对蒸气靶靶厚、电荷交换截面、转化率进行了简单的估算。当引出电压为18KV，蒸气温度500 ℃时，靶厚为8.5 * 10~(13)cm~(-2)，交换截面为1.0 * 10~(-16)cm~2， 转化率为0.86%。最大负He离子流强为1.37℃A.该源配置在2 * 2MeV串列静电加速器上，可在核物理实验和离子束分析提供良好的He负离子流和负H离子流。本文还提出了一些改进完善意见和设想

He喷嘴带传输及X-γ符合测量装置

本文介绍了He喷嘴带传输及X-γ符合测量装置对重缺中子远离核作活性分离鉴别的基本原理和技术路线，以及该装置首次在本所在线完成的实验结果。通过对110 MeV ~(16)O+~(185)Re实验主要反应产物的测量，指定出~(195)Bi，~(196)Bi，~(192)Tl的半衰期分别为3.11 ± 0.30，4.39 ± 0.53和10.8 ± 1.8 Min，与文献报道一致，并根据母子体衰变平衡拐点Tm初步分析了~(195)Pb；在110 MeV ~(16)O+~(142)Nd实验中，首次测量了~(153)Er的EC/β~+衰变，得到其下列四条新γ线：188.6，352.3，400.0，451.6 KeV(±0.3KeV)，并指定其寿命值T_(1/2) = 35.3 ± 1.6 Sec，与文献报道的根据α衰变测得的半衰期36 ± 2 Sec一致

HE PHASE TRANSFER OF CO(II) CATALYZED BY 2,2 '-BIPYRIDINE AT THE WATER/NITROBENZENE INTERFACE

The chemical reactions coupled with the phase transfer of Co(Ⅱ) catalyzed by 2,2′ -bipyridine across the water/nitrobenzene interface have been observed by using cyclic voltammetry (CV). Coupled chemical reactions both in the organic phase or in the aqueus phase influence the CV behavior of successive complex phase transfer obviously and an irreversible phenomenon similar to that existed at the metal electrode/electrolyte solution interface was observed. For different complexes, the phase transfer mechanism...

He, Ne and Ar isotope compositions of fluid inclusions in hydrothermal sulfides from the TAG hydrothermal field, Mid-Atlantic Ridge

Helium, rieon and argon isotope compositions of fluid inclusions have been measured in hydrothermal sulfide samples from the TAG hydrothermal field at the Mid-Atlantic Ridge. Fluid-inclusion He-3/He-4 ratios are 2.2-13.3 times the air value (Ra), and with a mean of 7.2 Ra. Comparison with the local vent fluids (He-3/He-4=7.5-8.2 Ra) and mid-ocean ridge basalt values (He-3/He-4=6-11 Ra) shows that the variation range of He-3/He-4 ratios from sulfide-hosted fluid inclusions is significantly large. Values for Ne-20/Ne-22 are from 10.2 to 11.4, which are significantly higher than the atmospheric ratio (9.8). And fluid-inclusion Ar-40/Ar-36 ratios range from 287 to 359, which are close to the atmospheric values (295.5). These results indicate that the noble gases of fluid inclusions in hydrothermal sulfides are a mixture of mantle- and seawater-derived noble gases; the partial mantle-derived components of trapped hydrothermal fluids may be from the lower mantle; the helium of fluid inclusions is mainly from upper mantle; and the Ne and Ar components are mainly from seawater.

He, Ne and Ar isotopic composition of Fe-Mn crusts from the western and central Pacific Ocean and implications for their genesis

The noble gas nuclide abundances and isotopic ratios of the upmost layer of Fe-Mn crusts from the western and central Pacific Ocean have been determined. The results indicate that the He and Ar nuclide abundances and isotopic ratios can be classified into two types: low He-3/He-4 type and high He-3/He-4 type. The low He-3/He-4 type is characterized by high He-4 abundances of 191x10(-9) cm(3.)STP(.)g(-1) on average, with variable He-4, Ne-20 and Ar-40 abundances in the range (42.8-421)x10(-9) cm(3.)STP(.)g(-1), (5.40-141)x10(-9)cm(3.)STP(.)g(-1), and (773-10976)x10(-9) cm(3.)STP(.)g(-1), respectively. The high He-3/He-4 samples are characterized by low He-4 abundances of 11.7x10(-9) cm(3.)STP(.)g(-1) on average, with He-4, Ne-20 and Ar-40 abundances in the range of (7.57-17.4)x10(-9) cm(3.)STP(.)g(-1), (110.4-25.5)x10(-9) cm(3.)STP(.)g(-1) and (5354-9050)x10(-9) cm(3.)STP(.)g(-1), respectively. The low He-3/He-4 samples have He-3/He-4 ratios (with RIRA ratios of 2.04-2.92) which are lower than those of MORB (R/R-A=8 +/- 1) and Ar-40/Ar-36 ratios (447-543) which are higher than those of air (295.5). The high He-3/He-4 samples have He-3/He-4 ratios (with R/R-A ratios of 10.4-12.0) slightly higher than those of MORB (R/R-A=8 +/- 1) and Ar-40/Ar-36 ratios (293-299) very similar to those of air (295.5). The Ne isotopic ratios (Ne-20/Ne-22 and Ne-21/Ne-22 ratios of 10.3-10.9 and 0.02774-0.03039, respectively) and the Ar-38/Ar-36 ratios (0.1886-0.1963) have narrow ranges which are very similar to those of air (the Ne-20/Ne-22, Ne-21/Ne-22, Ar-38/Ar-36 ratios of 9.80, 0.029 and 0.187, respectively), and cannot be differentiated into different groups. The noble gas nuclide abundances and isotopic ratios, together with their regional variability, suggest that the noble gases in the Fe-Mn crusts originate primarily from the lower mantle. The low He-3/He-4 type and high He-3/He-4 type samples have noble gas characteristics similar to those of HIMU (High U/Pb Mantle)- and EM (Enriched Mantle)-type mantle material, respectively. The low He-3/He-4 type samples with HIMU-type noble gas isotopic ratios occur in the Magellan Seamounts, Marcus-Wake Seamounts, Marshall Island Chain and the Mid-Pacific Seamounts whereas the high He-3/He-4 type samples with EM-type noble gas isotopic ratios occur in the Line Island Chain. This difference in noble gas characteristics of these crust types implies that the Magellan Seamounts, Marcus-Wake Seamounts, Marshall Island Chain, and the Mid-Pacific Seamounts originated from HIMU-type lower mantle material whereas the Line Island Chain originated from EM-type lower mantle material. This finding is consistent with variations in the Pb-isotope and trace element signatures in the seamount lavas. Differences in the mantle surce may therefore be responsible for variations in the noble gas abundances and isotopic ratios in the Fe-Mn crusts. Mantle degassing appears to be the principal factor controlling noble gas isotopic abundances in Fe-Mn crusts. Decay of radioactive isotopes has a negligible influence on the nuclide abundances and isotopic ratios of noble gases in these crusts on the timescale of their formation.

湖南芙蓉锡矿田流体包裹体的He同位素组成及成矿流体来源示踪

芙蓉锡矿田位于湖南省骑田岭花岗岩体的南部，是一个新近发现的超大型锡矿田．与以往所研究的与S型花岗岩有关的锡矿床明显不同，这个矿田在时空上都与骑田岭A型花岗岩密切相关．该矿田矿石硫化物流体包裹体的^3He／^4He测定值为0．14～2．95Ra，低于地幔的^3He／^4He值（6～7Ra），且高于地壳的^3He／^4He值（0．01～0．05Ra）．这表明芙蓉锡矿田成矿流体中的He具壳幔两端元混合的特点．该区一致的硫、锶及其他证据也都表明，深部地幔物质确实参与了该区锡的成矿．骑田岭岩体属造山期后张性环境下形成的A型花岗岩类．芙蓉锡矿田就产在骑田岭岩体的内外接触带或岩体中，其主成矿期与骑田岭岩体的形成时间相当吻合，且两者均具壳幔两端元混合成因的特征，所以其形成地球动力学背景可能均与中生代华南岩石圈的拉张、伸展作用密切相关．