长期体外反搏对颈动脉硬化及斑块形成的干预

目的：体外反搏能改善血管内皮细胞功能，长期体外反搏是否对动脉硬化及斑块形成产生影响呢？方法：采用彩色超声波检测颈动脉血管壁状态及损伤的程度，观察两组患者，体外反搏治疗组165例，反搏治疗时间1—9年（治疗组）未体外反搏治疗组68例（未治疗组）。结果：反搏组血管壁异常15．2％，斑块形成占11．5％，但反搏治疗2年以上，大于100次，斑块形成占4．2％。未反搏组血管异常为63.2％其中斑块形成占51.5％。体外反搏不仅可以改善各脏器血供；同时长期体外反搏，可以干预动脉硬化和斑块形成     

工程机械维修探讨

本文在系统分析工程机械维修现状的基础上，总结了目前工程机械维修中存在的主要问题，结合国内外研究现状，对维修的对策进行了探讨。并分别针对工程机械维修企业和施工企业提出了一些建议性的维修对策。     

硫代磷酸三(4-马来亚酰氨基苯)酯的合成

以对乙酰氨基苯酚和三氯硫磷为原料,经过酯化反应、水解反应得到硫代磷酸三(4-氨基苯)酯(TPTA),再以TPTA和马来酸酐为原料,经过酰胺化反应得到硫代磷酸三(4-马来亚酰氨基苯)酯(TPTM),总产率达到76.5%.以红外光谱、质谱及核磁共振谱对各产物的结构进行了表征,结果表明该法成功合成了目标产物.对TPTM紫外光谱进行了初步的研究,发现在204.5nm、280.0nm两处有吸收峰.     

互联网时代的“数字化校园”建设与高校管理工作的思考

随着互联网的飞速发展,教育界掀起了一股数字化校园建设热潮,众多的学校纷纷投入到其中,架构在网络环境上的＂数字化校园＂成为学校信息化建设的重点。搞好校园网络建设,构建现代化的教育环境,成为教育现代化的重要内容,也是形成现代教育办学体系的重要组成部分。我们的数字化校园建设是要以网络技术、多媒体技术等现代化信息技术为手段、以提高教育教学工作效率为目的,实现资源的有效整合和优化,从根本上转变教育教学和管理模式与方法。因此,我们要从根本上转变思想,建立与完善现代化管理意识的校园网络;同时,加强师资队伍建设,培养一支素养高、勇于创新、善于运用现代化技术的教师队伍。     

Discussion of the Hospital Union Management System Innovation in the New Era

医院工会作为工作人员利益的代表,在医院对工作人员开展的管理工作中发挥着极其重要的作用,而随着目前人力资源管理工作不断地趋于复杂,工会工作也产生了诸多新的工作任务.推动工会管理工作制度的有效创新,以使工会工作能够达到对时代要求的有效满足,已成为当前时期医院工作所不可避免的一项任务.文章通过分析新时期时代对于我国医院工会管理工作提出的新要求,探讨了医院积极对工会管理制度进行创新改革的几点措施.     

Preface

In the past decades, the ability of observing and manipulating quantum phenomena has been tremendously improved. It has advanced the thriving of quantum technologies with atomic, optical and solid-state systems.     

《陕西理工学院学报》（自然科学版）作者群现状分析

对2006年-2009年<陕西理工学院学报>(自然科学版)出版的16期学报载文的署名作者信息进行统计分析.结果显示,<陕西理工学院学报>(自然科学版)载文的论文合著率和合著度较高,且总体上呈逐年上升趋势;作者群的性别、职称结构符合我国科技人员的分布规律;作者群以正处于科研能力发展期和研究精力旺盛期的校内外中青年科研工作者为主,<学报>的作者队伍会持续壮大;稿源分布于23个省、自治区和直辖市,<学报>社会影响力和传播广度有了较大程度的提升,已经拥有一支年轻化、有活力、相对稳定的作者群队伍.这对<学报>进一步提高学术水平、更好地实现社会功能、提高社会效益起到基础保障作用.     

对我国美声唱法民族化发展问题的思考

美声唱法民族化的发展,应当更好地借鉴我国传统民族声乐的咬字训练方法、语言处理方法、表演方法,以进一步提高美声唱法的咬字技巧、突出其民族风格、增强其表演的艺术感染力。     

Sedimentation processes and sedimentary characteristics of tidal bores along the north bank of the Qiantang Estuary

A tidal bore is a unique Earth surface process, characterized by its highly destructive energy, predictable periodicities and magni-tudes, and the production of characteristic sedimentary features. Tidal bores and associated rapid flood flows are highly turbulent flows of the upper-flow regime with a velocity over several meters per second. Reynolds (Re) and Froude (Fr) numbers, respectively, are larger than 104 and 1.0, making them significantly different from regular tidal flows but analogous to turbidity currents. Until now, understanding of tidal-bore depositional processes and products has been limited because of the difficulty and hazards involved with gauging tidal bores directly. The Qiantang bore is known as the largest breaking bore in the world. Field surveys were carried out in May 2010, along the north bank of the Qiantang Estuary to observe the occurrence of peak bores, including regular observations of current, water level and turbidity at the main channel. Several short cores were sampled on the intertidal flats to study the characteristic sedimentary features of tidal bores. Hydrodynamic and sedimentological studies show that the processes of sediment resuspension, transport and deposition are controlled primarily by the tidal bores, and the subsequent abruptly accelerated and decelerated flood flows, which only account for one tenth of each semidiurnal tidal cycle in the estuary. Tidal-bore deposits are generally poorly sorted because of rapid sedimentation after highly mixed suspension by intense turbulence. This behavior is characteristic of the absence of tractive-current depositional components in a C-M diagram. It also goes along with well-developed massive bedding, graded bedding, basal erosion structures, convolute bedding and dewatering structures. Together, these sedimentary features can constitute fingerprinting of turbidites, widely distributed in the deep-water environment. However, a tidal bore is triggered by intensely deformed tidal waves propagating into a shallow-water environment, which returns to regular tidal flows rapidly after the passage of the bore head. The tidal-bore deposits are usually bounded by the intertidal-flat deposits with typical tidal beddings at the top and on both flanks. The difference between tidal-bore deposits (TBD) and tidal sandy/muddy deposits (TSD/TMD) is evident not only in sedimentary structures, but also in the grain-size composition. They can be clearly distinguished in grain-size bivariate plots, typically the plot of mean grain size vs. standard deviation (or sorting). Some trend variations generally exist in mean grain size with TBD>TSD>TMD, sorting with TMD>TBD>TSD (larger value indicating poorer sorting), and both skewness and kurtosis with TSD>TBD>TMD. These findings will undoubtedly shed new light on our understanding of tidal-bore sedimentology, ancient tidal-bore sedimentary facies and environments, and related oil-and-gas field prospecting.