原子核质量的高精度测量；Precise mass measurement of nuclides

原子核的质量直接反映了核内强相互作用、电磁相互作用和弱相互作用的结果.文章简要阐述了原子核质量测量的意义、现状和主要方法,介绍了基于兰州重离子冷却储存环的原子核质量测量实验,比较了首次得到的63Ge,65As,67Se和71Kr核质量测量值与理论计算结果,探讨了65As质量对天体物理快质子俘获过程的影响,文章最后给出了今后的研究内容.中国科学院近代物理研究所在轻质量丰中子区,系统测量了从Ne到Ca核素的质量,研究了N=20和28幻数随中子数和质子数变化的演化;在丰质子区,精确测量了快质子俘获路径上关键核素的质量,为解释X射线暴等爆发性天体过程提供重要的质量数据;在中重丰中子区,系统地测量丰中子核质量,通过天体网络计算模拟超新星爆发中的快中子俘获过程.

Production of new superheavy Z=108-114 nuclei with U-238, Pu-244, and Cm-248,Cm-250 targets

Within the framework of the dinuclear system (DNS) model, production cross sections of new superheavy nuclei with charged numbers Z=108-114 are analyzed systematically. Possible combinations based on the actinide nuclides U-238, Pu-244, and Cm-248,Cm-250 with the optimal excitation energies and evaporation channels are pointed out to synthesize new isotopes that lie between the nuclides produced in the cold fusion reactions and the Ca-48-induced fusion reactions experimentally, which are feasible to be constructed experimentally. It is found that the production cross sections of superheavy nuclei decrease drastically with the charged numbers of compound nuclei. Larger mass asymmetries of the entrance channels enhance the cross sections in 2n-5n channels.

DIRECT MASS MEASUREMENTS OF EXOTIC NUCLEI IN STORAGE RINGS

Mass measurements of exotic nuclei is a fast, developing field which is essential for basic nuclear physics and a wide range of applications. The method of storage ring mass spectrometry has many advantages: (1) a large amount of nuclides can be simultaneously measured; (2) very short-lived (T-1/2 greater than or similar to 50 mu s) and very rare species (yields down to single ions) can be accessed; (3) nuclides in several atomic charge states can be investigated, (4) half-life measurements can be performed with time-resolved mass spectrometry. In this contribution we concentrate on some recent achievements and future perspectives of the storage ring mass spectrometry.

Discovery of Highly Excited Long-Lived Isomers in Neutron-Rich Hafnium and Tantalum Isotopes through Direct Mass Measurements

A study of cooled Au-197 projectile-fragmentation products has been performed with a storage ring. This has enabled metastable nuclear excitations with energies up to 3 MeV, and half-lives extending to minutes or longer, to be identified in the neutron-rich nuclides Hf-183,Hf-184,Hf-186 and Ta-186,Ta-187. The results support the prediction of a strongly favored isomer region near neutron number 116.

Penning trap mass measurements on nobelium isotopes

The Penning trap mass spectrometer SHIPTRAP at GSI Darmstadt allows accurate mass measurements of radionuclides, produced in fusion-evaporation reactions and separated by the velocity filter SHIP from the primary beam. Recently, the masses of the three nobelium isotopes No252-254 were determined. These are the first direct mass measurements of transuranium elements, which provide new anchor points in this region. The heavy nuclides were produced in cold-fusion reactions by irradiating a PbS target with a Ca-48 beam, resulting in production rates of the nuclei of interest of about one atom per second. In combination with data from decay spectroscopy our results are used to perform a new atomic-mass evaluation in this region.

A high performance Time-of-Flight detector applied to isochronous mass measurement at CSRe

A high performance Time-of-Flight detector has been designed and constructed for isochronous mass spectrometry at the experimental Cooler Storage Ring (CSRe) The detector has been successfully used in an experiment to measure the masses of the N approximate to Z approximate to 33 nuclides near the proton drip-line Of particular interest is the mass of As-65 A maximum detection efficiency of 70% and a time resolution of 118 +/- 8 Ps (FWHM) have been achieved in the experiment The dependence of detection efficiency and signal average pulse height (APH) on atomic number Z has been studied The potential of APH for Z identification has been discussed (C) 2010 Elsevier B V All rights reserved

143Pm高自旋态和重丰中子新核素的合成及衰变性质研究

本论文从内容上可以分为两大部分：第一部分：对近球形核~(143)Pm高自旋态进行的在束γ研究。这一部分是本文的重点。利用能量为82和90 MeV的~(19)F束流，通过融合蒸发反应~(128)Te (~(19)F,4nγ) ~(143)Pm布局~(143)Pm的高自旋态。利用联合在束装置(JIBGE)的10套带BGO反康的HPGe探测器进行了标准在束γ谱学测量，包括γ射线的激发函数、γ单谱、γ-γ-t符合谱以及DCO测量。在已有工作的基础上，建立了~(143)Pm激发能高达10.5 MeV，自旋约为(61/2)h的高自旋态能级结构。观测到了28条新的跃迁能级和48条新的γ射线。对两个已知的同质异能态寿命进行了提取，并在8 MeV激发能附近进行了高自旋态同质异能态的搜索。以~(142)Nd，~(144)Sm为核实，用零级弱耦合模型对~(143)Pm的晕态能级结构进行了定量的解释。计算表明，直到激发能Ex = 6.77 MeV，自旋宇称J~π = (37/2~+)的晕态能级都可以用弱耦合模型进行很好的解释。但是，对于更高激发能的能级，组态情况要复杂的多，有出现N = 82中子闭壳打破的可能。同时，利用大基壳模型OXBASH程序对其能级结构进行了计算和讨论，其结果支持弱耦合模型的假设。第二部分：利用中能重离子的多核子转移反应，(~(186)W-2p + 2n)，(~(238)U-2p + 2n)对丰中子核~(186)Hf和~(238)Th进行了合成和鉴别。测量它们的半衰期分别为(2.6 ± 1.2) min和 (9.4 ± 2.0) min，与用质子一中子准粒子随机相近似方法的预言值是相符的。同时，对β延发裂变先驱核~(230)Ac进行了实验研究。观测到了它的两个裂变事件，得到~(230)Acβ延发裂变几率为(1.19 ± 0.85) * 10~(-8)。从而使~(230)Ac成为世界上第一种被确认了的基态β延发裂变先驱核。

大气散落核素复合示踪在土壤侵蚀科学中的应用

介绍了大气散落核素 7Be、2 1 0 Pbex、1 37Cs复合在土壤侵蚀和泥沙来源领域中的研究进展 ;阐述了核素比率应用的原理、特点及其能更为敏感地反映土壤侵蚀速率和过程等优点 ;说明多元素复合示踪在推断土壤不同侵蚀过程及估算土壤侵蚀速率方面的作用 ;论述了建立两核素相关深度曲线确定泥沙起源深度的应用原理和特点及其应用范围 ,并对各种方法进行了简单的评价。

中国北方风成堆积的风化作用与环境变迁—U-Th、~(10)Be及元素地球化学的研究

The surface of the Earth is continuously undergoing changes as a result of weathering-erosion, plate tectonics and volcanic processes. Continental weathering-erosion with its complex rock-water interactions is the central process of global biochemical cycling of elements, and affects the long-term ocean atmosphere budget of carbon dioxide both through the consumption of carbonic acid during silicate weathering and through changes in the weathering and burial rates of organic carbon. Rates of the weathering-erosion depend on a variety of factors, in particular rock properties and chemical composition, climate (especially rainfall), structure, and elevation. They are quite variable on a regional scale. Thus, environmental changes in a region could be indicated by the history of weathering-erosion in the region. Recent attention has focused on increased silicate weathering of tectonically uplifted areas in the India-Asia collision zone as a possible cause for falling atmospheric CO_2 levels in the Cenozoic era. The wind blown dust deposits in the Loess Plateau is derived from the arid and semiarid regions in northwestern China, in turn, where the deposits have been derived from the Qinghai-Xizang Plateau and the high mountains around. Therefore, geochemistry of the wind blown loess-paleosol and red clay sequences may provide insight both to paleoenvironmental changes on the Loess Plateau, and to the uplift and weathering-erosion histories of the Qinghai-Xizang Plateau. In this paper, uranium-thorium series nuclides and cosmogenic ~(10)Be have been employed as tracers of weathering intensities and histories of the dust sediments in the Loess Plateau. Major elements, such as Na, Al, Fe etc., are also used to estimate degree of chemical alteration of the dust sediments and to rebuild the history of weathering on the Loess Plateau. First of all, using a low-level HPGe γ-ray detector, we measured U and Th series nuclides in 170 loess and paleosol samples from five sites in the Loess Plateau, going back 2.6 Ma. The results show that ~(238)U activities are disequilibrium with its daughter nuclide ~(230)Th in young loess-paleosol sequence, indicating that weathering was happened both in dust deposition site and in dust source regions. Using concentrations of ~(238)U and ~(232)Th in the samples, we estimated the amounts of ~(238)U leached out of from paleosols due to weathering. Further, based on analyses of ~(230)Th in paleosols deposited in the past ca. 140 ka, we determined when the paleosols weathered in the source regions. We conclude that most of the weathering in the dust-source regions may have occurred during the interglacials before dust deposition.