CiADS束流负载效应前馈补偿的仿真评估

在高功率超导质子直线加速器中，束流负载效应是影响超导腔幅相稳定性的一个重要因素。本工作基于谐振腔建场模型，开发了超导腔系统束流负载效应的时域仿真程序，分析了束流负载效应对超导腔幅相稳定性的影响，并在C-ADS注入器II上通过相关实验测量对仿真结果进行了验证。利用该程序，评估了CiADS超导直线加速器脉冲束流的脉冲长度，以及前馈补偿的时序抖动和束流纹波等因素对腔中电磁场幅相稳定度的影响。仿真结果表明:在当前CiADS直线加速器设计参数下，为满足超导腔中电磁场0.1%与在高功率超导质子直线加速器中，束流负载效应是影响超导腔幅相稳定性的一个重要因素。本工作基于谐振腔建场模型，开发了超导腔系统束流负载效应的时域仿真程序，分析了束流负载效应对超导腔幅相稳定性的影响，并在C-ADS注入器II上通过相关实验测量对仿真结果进行了验证。利用该程序，评估了CiADS超导直线加速器脉冲束流的脉冲长度，以及前馈补偿的时序抖动和束流纹波等因素对腔中电磁场幅相稳定度的影响。仿真结果表明:在当前CiADS直线加速器设计参数下，为满足超导腔中电磁场0.1%与$0.1^{\circ}$的幅相稳定度指标，前馈时序抖动的偏差不能超过0.79 μs，束流流强的直流偏差不能超过0.9%，并且给出了束流纹波的最大抖动幅值与纹波频率之间的关系。这些结果将为CiADS超导直线加速器相关子系统技术指标的确定提供依据。     

Li[LiCs2Cl][Ga3S6]: A Nanoporous Framework of GaS4 Tetrahedra with Excellent Nonlinear Optical Performance

A large nonlinear optical (NLO) coefficient and a wide band gap are two crucial but contradictory parameters that are difficult to achieve simultaneously in a single infrared (IR) NLO compound. A salt‐inclusion chalcogenide (SIC), Li[LiCs₂Cl][Ga₃S₆] ( 1 ), was prepared that presents a nanosized tunnel framework constructed from monotype chalcogenide tetrahedra. Highly oriented covalent GaS₄ tetrahedra in the host lead to a moderate second harmonic generation response (0.7 AgGaS₂), and ionic guests effectively broaden the band gap to the widest value (4.18 eV) among all IR NLO chalcogenides, thereby achieving a remarkable balance between NLO efficiency and band gap.     

La掺杂和空位对ZnS磁性和光学性能影响的第一性原理研究

利用密度泛函理论框架下的平面波超软赝势法,通过第一性原理对La掺杂与Zn空位(V_(Zn))及La掺杂与S空位(V_S)共存的ZnS体系的电子结构、磁性机理、形成能及吸收光谱进行了研究.结果表明, La掺杂与空位(V_(Zn)或V_S)的空间位置最近时,掺杂体系的形成能最低,体系最稳定.另外,La掺杂与Zn空位共存时,体系具有磁性,且体系的净磁矩与La原子与Zn空位的相对位置有关;La掺杂与S空位共存时,掺杂体系无磁性,但此时体系的禁带宽度最窄且吸收光谱红移最显著.     

BowtieArene: A Dual Macrocycle Exhibiting Stimuli-Responsive Fluorescence

Although highly useful in supramolecular chemistry, pillararenes lack a fluorophore in their skeleton. Here we present BowtieArene, a novel fluorescent dual macrocycle, featuring a central tetraphenylethylene-derived fluorophore and two pillar-like, pentagon-shaped cavities which are comparable to pillar[5]arene. This concisely prepared, figure-of-eight molecule exhibits vapor absorption and host–guest capabilities, as well as intriguing switchable fluorescence. The fluorochromism of BowtieArene can be triggered by multiple external stimuli including solvent, vapor, and mechanical force, with excellent reversibility and stability. Experimental and theoretical evidence indicate that the fluorochromism should be closely related to molecular packing.     

黄磷炉渣和铜渣协同制备微晶玻璃

以黄磷炉渣和铜渣为原料,添加一定比例的焦炭,熔融法制备了黄磷炉渣-铜渣微晶玻璃.借助Kissinger方程分析黄磷炉渣-铜渣基础玻璃的析晶能力,借助X射线衍射仪(XRD)进行物相分析.结果表明:随着黄磷炉渣与铜渣的质量添加比的增大,黄磷炉渣-铜渣基础玻璃的析晶峰峰温值Tp和析晶活化能E逐渐减小;当黄磷炉渣:铜渣=6:1时,黄磷炉渣-铜渣基础玻璃的析晶活化能最小,析晶能力最强;黄磷炉渣与铜渣添加比并不对黄磷炉渣-铜渣微晶玻璃晶相类型产生影响,其晶相均为钙长石Ca2 Al2 SiO7和镁黄长石Ca2 MgSiO7.     

基于Matlab GUI的微观化学反应过程可视化设计

Based on the quasi-classical trajectory (QCT) method and Matlab GUI technology, we developed a program code for visualizing the collision process of the elementary chemical reactions of the a + bc type. The general methodology of QCT, abstraction of dynamical properties of molecular collisions and the making of Graphical User Interface are introduced. The running results of an application to the reaction F + HCl→HF + Cl is also presented. The results showed that this program could vividly demonstrate the behavior and final state of the atom-diatom collision process in animated form. Students can interact with internal MATLAB code through graphical user interface, observe the reactive behavior and final results in real-time from multiple angles, which helps students to understand the complex reaction mechanism and deepen their perceptual impression of the chemical process at a microscopic atomic/molecular level.     

埋藏哈密翼龙化石的雅丹风化的光谱分析——以大海道2号水源地雅丹为例

新疆哈密地区翼龙化石具有极高的科学研究价值。哈密翼龙动物群主要埋藏在早白垩世湖相地层形成的雅丹中，富集在风暴沉积层。化石一旦暴露地表，就会发生不同程度的自然风化破碎，尤其是见水或受潮后风化更为严重。哈密大海道2号水源地附近的雅丹底部由于地下水和间歇性地表水的作用，发生了严重的盐碱析出导致的强烈风化现象，造成雅丹下部剥落侵蚀和上层雅丹重力坍塌，从下到上不同地层的风化程度差异较大，底部地层的风化最为剧烈。对大海道雅丹地层剖面取样，利用多种分析方法确定每一层的岩性和可溶盐种类，从微观上揭示雅丹风化的机理。偏光显微观察和X射线衍射（XRD）结果显示每一层都含有石英、长石、方解石和粘土矿物，矿物组成无较大差异，但粘土含量差别较大。精确的可溶盐种类鉴别方法，包括离子色谱（IC）确定出样品中可溶盐离子含量及种类，拉曼光谱（Raman）和傅里叶变换红外光谱（FTIR）鉴别出样品中的硝酸盐和硫酸盐，扫描电子显微镜能谱仪（SEM-EDS）鉴别出氯盐、硝酸盐和硫酸盐。结果显示雅丹各风化层中最底层可溶盐主要是NaCl和Na₂SO₄，第二层是NaCl和CaCl₂，第三层是NaCl，盐种类/含量的差别是此处雅丹从下到上发生不同风化现象的重要原因。结合大海道雅丹所处的气候地理环境（极干旱高盐碱地区、水源地附近），探讨水盐活动规律并关联风化表现，分析该处雅丹风化原因，内因是每层沉积岩的岩性不同，外因是水和盐（NaCl，Na₂SO₄，CaCl₂）的共同作用下，强烈的水盐活动造成了埋藏有哈密翼龙化石的雅丹严重化学风化。这一风化机理也可很好地解释哈密翼龙化石及其围岩层受潮后的强烈风化破碎现象。