空间电荷阻抗和纵向束团定态解

回顾了加速器的阻抗模型 ,讨论了空间电荷阻抗和管道壁阻的高频衰减特性 .从Vlasov Maxwell方程出发提出了当存在类似空间电荷阻抗时 ,在任意外场、任意分布下 ,束团定态分布的一般解法 ,并以两种重要分布为例 ,给出重离子加速器强流参数下的定态分布 .解得的定态分布可以进一步应用于稳定性分析和计算机模拟计算 .由定态分布的求解得出了对束团中的朗道阻尼和稳定性研究非常重要的纵向“色散”函数 .

Topological objects in two-gap superconductor

We discuss the non-Abelian topological objects, in particular the non-Abrikosov vortex and the magnetic knot made of the twisted non-Abrikosov vortex, in two-gap superconductor. We show that there are two types of non-Abrikosov vortex in Ginzburg-Landau theory of two-gap superconductor, the D-type which has no concentration of the condensate at the core and the N-type which has a non-trivial profile of the condensate at the core, under a wide class of realistic interaction potential. We prove that these non-Abrikosov vortices can have either integral or fractional magnetic flux, depending on the interaction potential. We show that they are described by the non-Abelian topology pi(2)(S-2) and pi(1)(S-1), in addition to the well-known Abelian topology pi(1)(S-1). Furthermore, we discuss the possibility to construct a stable magnetic knot in two-gap superconductor by twisting the non-Abrikosov vortex and connecting two periodic ends together, whose knot topology pi(3)(S-2) is described by the Chern-Simon index of the electromagnetic potential. We argue that similar topological objects may exist in multi-gap or multi-layer superconductors and multi-component Bose-Einstein condensates and superfluids, and discuss how these topological objects can be constructed in MgB2, Sr2RuO4, He-3, and liquid metallic hydrogen.

Entropy of Kaluza-Klein black hole from Kerr/CFT correspondence

We extend the recently proposed Kerr/CFT correspondence to examine the dual conformal field theory of four-dimensional Kaluza-Klein black hole in Einstein-Maxwell-Dilaton theory. For the extremal Kaluza-Klein black hole, the central charge and temperature of the dual conformal field are calculated following the approach of Guica, Hartman, Song and Strominger. Meanwhile, we show that the microscopic entropy given by the Cardy formula agrees with Bekenstein-Hawking entropy of extremal Kaluza-Klein black hole. For the non-extremal case, by studying the near-region wave equation of a neutral massless scalar field, we investigate the hidden conformal symmetry of Kaluza-Klein black hole, and find the left and right temperatures of the dual conformal field theory. Furthermore, we find that the entropy of non-extremal Kaluza-Klein black hole is reproduced by Cardy formula. (C) 2010 Elsevier B.V. All rights reserved.

Retrieval of Electron Return Time from High-order Harmonics Generated in a Mixture of He and Ne Gases

In terms of single-atom induced dipole moment by Lewenstein model, we present the macroscopic high-order harmonic generation from mixed He and Ne gases with different mixture ratios by solving three-dimensional Maxwell's equation of harmonic field. And then we show the validity of mixture formulation by Wagner et al. [Phys. Rev. A 76 (2007) 061403(R)] in macroscopic response level. Finally, using least squares fitting we retrieve the electron return time of short trajectory by formulation in Kanai et al. [Phys. Rev. Lett. 98 (2007) 153904] when the gas jet is put after the laser focus.

RETGEM的研究

提供了一种新型的微观气体探测器：RETGEM(thick GEM with electrodes made of a resistive material)，它是由标准PCB技术加工而成，厚度和孔直径在毫米量级。 本文主要分两个部分对RETGEM在常温、常压下的工作机制和性能作了初步研究：第一部分是模拟部分：MAXWELL计算电场分布和GARFIELD模拟物理过程；第二部分是对RETGEM的初步测试，表明该探测器具有400Hz的计数率，100V左右的计数率坪长， 放射源下可取得28％的能量分辨、 的有效增益和5％以下的打火率。结果表明RETGEM是一个稳定、可靠的探测器，其性能达到了设计的基本要求，为今后的工作打下了很好的基础

中能核反应中的统计发射过程及核温度参量

在过去的几年里，利用兰州重离子加速器（HIRFL）提供的束流，以及在OUVERTURE合作研究中，利用意大利国家核物理研究院南方实验室（INFN-LNS）超导回旋提供的束流，进行了多次中能区重离子核反应实验研究工作。如，最初的46.7MeV/u ~(12)C+~(58)Ni，~(115)In，~(197)Au的实验及30MeV/u ~(40)Ar+~(58)Ni，~(64)Ni~(115)In和30MeV/u Ni轰击Ni，Au，Al在MULTICS+MEDEA：4π装置上进行的实验工作。此外，本人还从事过一些理论研究工作，包括多粒子散射形式理论和相关数学物理问题研究，量子分子动力学和量子统计模型计算。本文是从事这些核物理研究工作的积累，主要侧重于实验结果的物理内容分析，而不强调实验技术，数据处理的技巧。主要的物理内容有以下几个方面：1.对于利用双同位素产额比提取同位素核温度的方法进行研究推广，使得对于实验中碰到的仅有部分能谱可以实现很好同位素分辩的情况，即使不能得到总的同位素产额，仅仅通过一段能区的同位素产额也可提取核温度。用于具体的实验研究工作中后，对于46.7MeV/u ~(12)C+~(58)Ni，~(115)In，~(197)Au核反应过程，同一体系利用这种方法得到的同位素核温度和利用粒子非稳态布居提取的核温度一致。2.围绕核反应过程中核温度的参量的提取，对于双同位素产额比与核温度的刻度关系进行了分析研究，通过计算考虑中等质量碎片（IMF）内部激发能后的内部配分函数表明，中等质量碎片的内部激发对刻度关系有重要影响。零阶近似下区域密度近似的结果和Gemini模拟计算的结果反映了相同的情况。3.研究核反应机制，多个粒子散射的形式理论的必需的，对于两体散射，其形式理论已经比较成熟，但是对于多个粒子散射问题出现的严重的困难是多体Lippmann-Schwinger方程无唯一收敛的解。作为一种探索性的研究工作，开展了多体散射理论研究工作，发展了一些具有普遍意义的数学物理方法。在本项研究工作中，通过能基础数学中的约当引理的推广，发现一个特例：对非连接图，Lippmann-Schwingwer方程存在收敛的解，因此多体散射形式理论，有可能重新建立。由于核力和多体问题是当今核物理研究的两大难点，世界各国的科学家都在努力以图攻克它们，而且多体问题还是物理学的其它许多领域的难题，因而多体散射还是引起诸多研究学科广泛兴趣的课题。通过发展一些新的数学理论和方法，我们已得到一些有意义的结果。4.将量子分子动力学这种中高能量区域所用的理论分析方法扩展至较低能区，通过对相空间中初始位置和动量抽样增加限制条件。如结合能和实验值要求一致，平均核势，核内Pauli阻塞更强一些，在演化中能量和动量守恒等等。得到一个很稳定的初始基态。均方半径保持不弥散的时间可达1600fm/c，用于研究10.6MeV/u Ne~(20)+Al~(27)的实验分析过程中。另外，量子统计模型（QSM）主要描述中心核-核碰撞，将它和碎裂模型结合，作一些改进后，可以对核-核碰撞进行统一描述。5.在中能核反应研究中发现，核反应过程中有大量的中子，轻带电粒子以及中等质量碎片发射出来，可以将这些粒子发射机制大致分为两大类。其中一类可以归结为动力学发射过程的产物。另一类则可以归于统计发射的产物。在低能核反应中，其发射能谱的斜率的负倒数，可作为复合核的核温度。而在中能重离子核反应中，其发射能谱变得很复杂，不再具有Maxwell分布。通常的三源拟合所给出的温度参数，已不能反映物理实质。提出多阶矩分析方法用于分析中能核反应中统计发射规律及受动力学过程的影响。

热核温度和激发能的实验测量

本研究利用PPAC和11组#diamond open#E-E望远镜对25MeV/u ~(40)Ar+~(108)Ag反应中的裂变碎片和轻带粒子联测量。用得到的裂变碎片角关联来确定系统的线性动量转移（LMT）。将符合测量得到的对应于不同的后角轻带电粒子能谱用MAXWELL分布来拟合其后沿。经过一些修正，由能谱得到热核的初始温度T_(ini)。在考虑反应Q值、转动能和前平衡发射之后，可以得到不同窗所对应的激发能。实验结果表明，在中心的Ar+Ag碰撞中激发能高达4.44MeV/A，温度达6MeV。在半中心碰撞中激发能达3.8MeV/A，温度达5.7MeV。在此激发能范围内，随着热核激发能升高，能级密度参数将随之增大，其趋势为A/8

大别山岩石圈有效弹性厚度初步研究

As powerful tools to study the lithosphere dynamics, the effective elastic thickness (Te) as well as the envelope of yielding stress of lithosphere have been attracted great attention of geoscientists in the past thirty years. The oceanic lithosphere, contrary to the continental lithosphere, has more fruits for its simple structures and evolution process. In continent, the lithosphere commonly is complex and variable in the rheological, thermal structures, and has a complicated history. Therefore, the application of the effective elastic thickness in continent is still a subject to learn in a long time. Te, with the definition of the thickness of an elastic plate in theory flexured by the equal benging of the real stress in the lithosphere plate (Turcotte, 1982), marks the depth of transition between elastic and fluid behaviors of rocks subjected to stress exceeding 100 MPa over the geological timescales (McNutt, 1990). There are three methods often adapted: admittance or isostatic response function, coherence and forwarding. In principle, the models of Te consist of thermal-rheological, non-linear Maxwell, non-linear work hardening and rheological layered models. There is a tentative knowledge of Te that it is affected by the following factors: crustal thickness, crust-mantle decoupling, plate bending, boundary conditions of plate (end forces and bending moments), stress state, sedimentary layer, faulting effect, variation in the mountain belts' strike, foreland basin, inheritance of tectonic evolution, convection of mantle, seismic depth and lithosphere strength. In this thesis, the author introduces the geological sketch of the Dabie collisional orogenic belt and the Hefei Basin. The Dabie Mts. is famous for the ultra-high pressure metamorphism. The crustal materials subducted down to the depth of at least 100 km and exhumed. So that the front subjects arise such as the deeply subduction of continent, and the post-collisional crust-mantle interaction. In a geological journey at June of 1999, the author found the rarely variolitic basaltic andesite in the Dabie Mts. It occurs in Susong Group, near Zhifenghe Countryside, Susong County, Anhui Province. It is just to the south of the boundary between the high-grade Susong melange and the ultra-high grade South Dabie melange. It has a noticeable knobby or pitted appearance in the surface. The size of the varioles is about 1-4 mm. In hand-specimen and under microscope, there are distinct contacts between the varioles and the matrice. The mineralogy of the varioles is primarily radiate plagioclase, with little pyroxene, hornblende and quartz. The pyroxene, hornblende and quartz are in the interstices between plagioclase. The matrix is consisted of glass, and micro-crystals of chlorite, epidote and zoisite. It is clearly subjected and extensive alteration. The andesite has an uncommon chemical composition. The SiO_2 content is about 56.8%, TiO_2 = 0.9%, MgO = 6.4%, (Fe_2O_3)_(Total) = 6.7% ～ 7.6%, 100 Mg/(Mg+Fe) = 64.1 ～ 66.2. Mg# is significantly high. The andesite has higher abundances of large-lithophile trace elements (e.g. K, Ba, Sr, LREE), e.g. La/Nd = 5.56-6.07, low abundances of high-strength-field elements (HFSE, e.g. Ta, Nb, P, Ti), particularly Ta and Nb strongly depleted. These are consistent with the characteristics of subducted-related magmas (Pearcce, 1982; Sun and McDonaugh, 1989). In the spider diagram of trace elements, from Ce to right hand, the abundances of elements decrease quickly, showing a characteristic of the continental margins (Pearce, 1982). There has a strongly enrichment of light-rare-earth elements, with a significant diffraction of REEs (the mean value of (La/Yb)_N is 32.84). No Eu anomaly, but there are anomaly high (La/Yb)_N = 28.63-36.74, (La/Y)_N = 70.33 - 82.84. The elements Y and Yb depleted greatly, Y < 20 ppm, Y_N = 2.74-2.84, Yb_N = 2.18 - 2.35. From the La-(La/Sm) diagram, the andesite is derived from partial melting. But the epsilone value of Nd is -18.7 ～ -19.2, so that the material source may be the mantle materials affected by the crustal materials. The Nd model age is 1.9 Ga indicating that the basaltic andesite was resulted from the post-collisional crust-mantle interaction between the subducted Yangze carton and the mantle of Sino-Korea carton. To obtain the Te of the lithosphere beneath the Dabie Mts. and the Hefei Basin, the author applies the coherence method in this thesis. The author makes two topography-gravity profiles (profiles 7~(th) and 9~(th)) across the Dabie Mts. and the Hefei Basin, and calculates the auto-coherence, across coherence, power spectrum, across power spectrum of the topography and gravity of the two profiles. From the relationships between the coherence and the wave-number of profiles. From the relationships between the coherence and the wave-number of profiles 7~(th) and 9~(th), it is obtained that the characteristic wavelengths respectively are 157 km and 126 km. Consequently the values of effective elastic thickness are 6.5 km and 4.8 km, respectively. However, the Te values merely are the minimum value of the lithosphere because the coherencemethod in a relative small region will generate a systemic underestimation. Why there is a so low Te value? In order to check the strength of the lithosphere beneath the Dabie Mts., the authore tries to outline the yielding-stress envelope of the lithosphere. It is suggested that the elastic layers in the crust and upper mantle are 18 km and 35 km, respectively. Since there exist a low viscosity layer about 3-5 km thickness, so it is reasonable that the decoupling between the crust and mantle occurred. So the effective thickness of the lithosphere can be estimated from the two elastic layers. Te is about 34 km. This is the maximum strength of the lithosphere. We can make an approximately estimation about the strength of the lithosphere beneath the Dabie Mts.: Te is about 20-30 km. The author believes that the following factors should be responsible for the low Te value: (1) the Dabie Mts. has elevated strongly since K_3-J_1. The north part of the Dabie Mts. elevates faster than the south part today; (2) there occur large active striking faults in this area. And in the east, the huge Tan-Lu striking fault anyway tends to decrease the lithosphere strength; (3) the lithosphere beneath the Dabie Mts. is heter-homogeneous in spatio-temporal; (4) the study area just locates in the adjacent region between the eastern China where the lithosphere thickness is significantly reduced and the normal western China. These factors will decrease the lithosphere strength.