1000 resultados para 28-267


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研究了高电荷态离子129Xe28+轰击金属Au和Mo表面产生的特征X射线谱。实验结果表明,在入射离子的电荷态和能量相同的条件下,对于核电荷数较小、原子质量较轻的靶原子,只有其内壳层的电子才能被激发而产生X射线,而核电荷数较大、原子质量较重的靶原子只有其较外壳层的电子能被激发而产生X射线。特征X射线的产额随入射离子动能的增加而增加。

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测量了27,28P和相应同中子异位素在28Si靶上的中能反应截面.测得N=12和13同中子异位素的反应截面在Z=15处突然增大.对Z≤14同中子异位素和28P的实验数据结果可以用改进的光学极限近似的Glauber理论很好地描述.28P的反应截面能够用扩大核芯以改进的Glauber理论来解释.但是,用改进光学极限和少体近似的Glauber理论却低估了27P的实验数据.理论分析表明,扩大的核芯加质子晕可能是响应27P+28Si反应截面增强的机制.

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实验测量了20—40MeV u的轻丰中子核6He在Si靶上的反应总截面,并且结合6He的高能实验数据,采用双参数HO密度分布形式用Glauber模型计算得到较好的拟合.与Warner的实验数据比较,反应总截面数据系统性好,并与能量有明显的依赖关系.

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用同位旋相关的Boltzmann Langevin方程研究了在入射能量为2 8 7MeV/u下 ,不同弹核 14O ,16 O和 18O轰击不同靶核 7Be和 9Be的反应 ,计算了生成碎片的产生截面 ,发现用丰中子 (缺中子 )炮弹或丰中子 (缺中子 )靶进行反应 ,所得到的产物均有丰中子 (缺中子 )的碎片出现 .同位素分布宽度和峰位与入射体系密切相关 ,产生碎片的电荷数越接近入射弹核的电荷数 ,则同位素分布的宽度越大 ,峰位偏离β稳定线值越远 ,其同位旋效应越明显 .

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描述了 5 0 .4MeV/u的12 N和 42 .3MeV/u的13 N次级放射性束在2 8Si靶上引起的核反应总截面σr 实验研究 ,结果发现12 N的反应总截面σr 比其相邻同位素核13 N有着异常的增大 .这可能是核形变及核子对效应造成的 ,试验中的测量误差也不可忽视 .利用微观Glauber模型计算了12 N在2 8Si靶上的核反应总截面 ,并与实验结果做了比较 ,发现理论计算与实验结果拟合较好

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利用ΔE E望远镜系统测量了 1 56 3MeV2 8Si+ 12 C反应 (近对称系统 )中出射的Z =4— 1 4的产物元素的能谱和角分布 ,并由此给出了这些产物的胁变截面图 .从理论上计算了Z =4— 1 1产物的实验室系最可几动能分布E1(θ)和各元素的质心系的总动能分布Et(Z) ,指出了这些产物主要来自系统的两体反应过程 .还给出了该反应系统的全熔合截面值为 (980± 68)mb ,并指出从低能数据外推到此能量下的全熔合截面值与实验值之差主要归因于两体过程 .

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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.

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An experiment to study exotic two-proton emission from excited levels of the odd-Z nucleus P-28 was performed at the National Laboratory of Heavy Ion Research-Radioactive Ion Beam Line (HIRFL-RIBLL) facility. The projectile P-28 at the energy of 46.5 MeV/u was bombarding a Au-197 target to populate the excited states via Coulomb excitation. Complete-kinematics measurements were realized by the array of silicon strip detectors and the CsI + PIN telescope. Two-proton events were selected and the relativistic-kinematics reconstruction was carried out. The spectrum of relative momentum and opening angle between two protons was deduced from Monte Carlo simulations. Experimental results show that two-proton emission from P-28 excited states less than 17.0 MeV is mainly two-body sequential emission or three-body simultaneous decay in phase space. The present simulations cannot distinguish these two decay modes. No obvious diproton emission was found.

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A series of experiments have been performed by complete kinematics measurements to study two-proton (2p) correlated emission from the excited states of Ne-17,Ne-18 and S-28,S-29 via the Coulomb excitation by bombarding on Au-197 target. 2p and residua coincident events were picked Out under strict conditions. Visible p-p correlations were observed. It is shown that 2p can be emitted from the high-lying excited states. 2p halo may lead to 2p emission with large spectroscopy factor for the states close to or beyond the threshold.

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ΔE-E望远镜探测器是用于重离子校反应测量的一种装置,它可以测量产物的电荷数和能量。在单路ΔE-E的基础上,我们研制了一路ΔE气体探测器和十路E金硅石垒探测器构成的多路ΔE-E望远镜探测系统。电离室窗直径为8cm,阴极到栅极距离为6cm,栅极到阳极距离为2cm,充入50的Ar(90%) + CH_4 (10%)气体,测得对~(241)Am的5.41Mev/α其能量分辩为13%。所用的十块金硅石垒探测器能量为1%左右。此系统可以同时测量22 °范围内的10个角度点,这对角分布测量将十分有利。该探测器系统对~(16)O + ~(12)C反应体的Z分辩约为6%,它可以清楚的分开C到Mg的各种元素。利用上述多路ΔE-E探测系统,我们测量了E_(16O) = 50Mev-90Mev的16_O束流轰击~RC、~(24)Mg、~(28)Si和~(32)S等四个体系校反应产物的角分布、能谱和激发函数。在测量激发函数时,我们选取能量步长为ΔE_(Lab) = 1Mev,以便观察振荡结构在角分布测量时,对于三个能量点,我们测量了5.1 °- 39 °范围内的13个角度点。由于时间限制,本毕业论文仅给出~(16)O + ~(28)Si反应的全熔合激发函数和角分布。并且运用G-M模型和Wiecki公式对全熔合截石进行了理论计算。从激发函曲线看,实验结果的平均趋势与G-M模型的理论结果符合的相当好,同时还发现了该体系全熔合截石随能量有规律的起伏,这种起伏具有公认的振荡结构和某些特征,因此这些起伏极有可能就是振荡结构

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长白落叶松是东北地区主要的用材树种,其种子雨和种子库研究鲜见报道。在辽东山区用收集器收集的种子分析了长白落叶松种子雨组成、质量和扩散距离,每隔2个月调查1次种子库数量,并结合靛蓝染色法测定每次种子的活力来分析土壤种子库动态。结果表明,辽东山区的长白落叶松种子雨从8月中旬开始,9月末到10月初达到高峰期,11月初结束。在起始期,种子雨以干瘪的不完整种子为主,而从高峰期开始,种子雨以完整种子为主。整个长白落叶松种子雨中不完整种子约占种子雨总量的45%,这些不完整种子由被动物取食、空粒和病虫害危害种子组成。完整种子的平均生活力为56.4%,即有活力的种子仅占整个种子雨的30%。种子雨集中在母树周围,在林缘1次扩散距离一般不超过1.5倍树高。种子雨到达地面之后,主要分布在枯枝落叶层,土壤0~5cm层有少量分布,土壤5 cm以下没有种子分布;土壤种子库的种子主要在翌年雪融化后开始萌发、被取食、搬运以及腐烂,其中腐烂种子数占45.4%,动物取食为30.0%。种子库的种子数量和活力在冬季没有明显变化,而在翌年,种子数量和活力明显减少,4、6月和8月份种子数量分别为(506.3±35.56)粒m-2,(267.1±17.47)粒m-2和(143.6±9.83)粒m-2,对应的活力分别为47.8%±4.68%,19.4%±3.39%和0%,这表明长白落叶松种子不能在地面形成连续的种子库。