HIRFL新B1���束器冷却系统设计

在利用 MAFIA程序计算得到的新 B1���束器腔体表面电流分布的基础上 ,提出了新 B1���束器的冷却方案 ,并计算了水流及水管表面的电流分布 ,得到了冷却所需要的流量。最后估计了由于工作温度的升高所引起的并联阻抗的减小及频率的漂移。

HIRFL新B1���束器耦合环的设计与计算

通过将聚束器腔体等效为 RLC并联回路 ,求得了功率馈入耦合环与腔体的互感及自感的公式 ,根据对腔体的计算结果求出了在聚束器的工作频段内达到阻抗匹配所要求的互感变化范围 ,并在该互感变化范围内设计了可移动的耦合电感环 ,计算了它的自感及整个腔体的剩余电感。

三维电磁场数值模拟在腔体设计中的应用——新B1���束器的腔体设计

为了提高HIRFL的束流指标，特别是束流强度，以满足放射性次级束流线（RIBLL）及大科学工程兰州重离子冷却储存环（CSR）对束流的更高要求，目前 HIRFL 正在进行很多方面的改造，其中之一便是建造一台新聚束器B1���改善注入器 SFC 与主加速器SSC之间的给向匹配。为了克服非线性效应，新B1���计工作在多模式下，频率范围为 22MHz～54MHz，最高电压达110kV。由于较宽的工作频率范围、较高的电压及有限的空间位置，新B1���束器的腔体设计存在许多困难。本论文的主要工作便是设计新B1���束器的腔体。主要工作可分为三部分：1．腔体设计：在这部分，我们利用三维电磁场模拟程序－MAFIA，辅之以传输线近似法，设计出了满足物理要求的腔体方案，给出了模拟计算所得到了的腔体主要参数，并就这些参数的可信度进行了评估。2．耦合环设计：在这部分，我们利用 MAFIA 模拟得到的结果，从腔体的等效集总电路出发，推导出了耦合环参数与腔体特性参数之间的关系，并设计出了满足物理要求的耦合方案。3．冷却系统设计：这部分的主要工作为从对流、传导换热理论出发，结合新B1���实际，建立了自己的传热模型，设计了新B1���体的冷却系统，计算了腔体的最高工作温度，并讨论了工作温度的升高对腔体性能的影响。另外，在论文的最后一章还介绍了其它一些工作，主要包括SFC中 Dee 电压分布计算、原B2腔体的实验研究以及原B1���体的传输线近似法模拟。

A MASS-SPECTROMETRIC STUDY OF ORGANIC PHOSPHORUS-COMPOUNDS .5. EI SPECTRA OF 1, 3, 2-OXAZAPHOSPHOLIDINE 2-SULFIDES DERIVATES

The mass spectral behaviour of 15 new type of organic phosphorus compounds with a considerable insecticidal activity, 1, 3,2-oxazaphospholidine 2-sulfides derivatives, under 70 eV electron impact has been studied by means of high and low resolution mass spectrometry as well as by B/E linked scan and MIKES/CID analysis. Discussion is focused into the isomerization between oxygen and sulphur in molecules and some rearrangement reactions.

Element enrichment and U-series isotopic characteristics of the hydrothermal sulfides at Jade site in the Okinawa Trough

The geochemical and U-series isotopic characteristics of hydrothermal sulfide samples from the Jade site (127A degrees 04.5'E, 27A degrees 15'N, water depth 1300-1450 m) at Jade site in the Okinawa Trough were analyzed. In the hydrothermal sulfide samples bearing sulfate (samples HOK1 and HOK2), the LREEs are relatively enriched. All the hydrothermal sulfide samples except HOK1 belong to Zn-rich hydrothermal sulfide. In comparison with Zn-rich hydrothermal sulfides from other fields, the contents of Zn, Pb, Ag, Cd, Au and Hg are higher, the contents of Fe, Al, Cr, Co, Ni, Sr, Te, Cs, Ti and U lower, and the Pb-210 radioactivity ratios and Pb-210/Pb ratios very low. In the hydrothermal sulfide mainly composed of sphalerite, the correlations between rare elements Hf and U, and Hf and Mn as well as that between dispersive elements Ga and Zn, are strongly positive; also the contents of Au and Ag are related to Fe-sulfide, because the low temperature promotes enrichment of Au and Ag. Meanwhile, the positive correlations between Fe and Bi and between Zn and Cd are not affected by the change of mineral assemblage. Based on the Pb-210/Pb ratios of hydrothermal sulfide samples (3.99x10(-5)-5.42x10(-5)), their U isotopic composition (U-238 content 1.15-2.53 ppm, U-238 activity 1.07-1.87 dpm/g, U-234 activity 1.15-2.09 dpm/g and U-234/U-238 ratio 1.07-1.14) and their Th-232 and Th-230 contents are at base level, and the chronological age of hydrothermal sulfide at Jade site in the Okinawa Trough is between 200 and 2000 yr.

Helium, neon and argon isotope compositions of fluid inclusions in massive sulfides from the Jade hydrothermal field, the Oldnawa Trough

Helium, neon and argon isotope compositions of fluid inclusions have been measured in massive sulfide samples from the Jade hydrothermal field in the central Okinawa Trough. Fluid-inclusion He-3/He-4 ratios are between 6.2 and 10.1 times the air value (Ra), and with a mean of 7.8Ra, which are consistent with the mid-ocean ridge basalt values [He-3/He-4 approximate to (6Rasimilar to 11Ra)]. Values for Ne-20/Ne-22 are from 10.7 to 11.3, which are significantly higher than the atmospheric ratio (9.8). And the fluid-inclusion Ar-40/Ar-36 ratios range from 287 to 334, which are close to the atmosperic values (295.5). These results indicate that the noble gases of trapped hydrothermal fluids in massive sulfides are a mixture of mantle- and seawater-derived components, and the helium of fluid inclusions is mainly from mantle, the nelium and argon isotope compositions are mainly from seawater.

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.