改革高职学院实训模式 提高实训效果——借鉴香港职前与在职训练的成功经验

香港职业训练局是香港政府设立的专业职业教育培训和就业推广的法定机构。本文介绍了香港职业训练局的法定职能、下属的教育与训练机构、职前和在职训练的特色和成功经验,提出了改进高职学院实训模式、提高实训效果的几点建议。     

进行物理校本研究提高教学有效性

新课程倡导探究性教学,而探究性教学的核心要素是问题,什么问题能够引发学生的探究,促进深度思考,建立起科学的概念,是我们学校教师值得研究的问题.在校本研究中,掌握学生的前概念,有利于我们进行教学设计,帮助学生建立科学概念.探究性教学基于学生的好奇心源于科学家的科学探究,国内外的研究表明探究性教学有助于转变学生的前概念.     

基于Agent油田前磁信息数字化信息管理系统的研究

为了实现在石油工业地质研究中用先进的网络系统管理前磁信息数据,使用面向Agent的软件工程方法——Gaia方法详细分析了油田前磁信息数字化信息管理系统,建立了该系统的分析模型和设计模型,将Gaia和OAA的系统分析与设计方法应用在基于Multi Agent前磁信息处理系统中.本文应用Gaia的分析方法建立了系统的角色模型,在此基础上构建了基于Multi Agent前磁信息数据处理整体框架体系,该体系也可基于异构平台的数据环境.     

When and how did plate tectonics begin？ Theoretical and empirical considerations

Plate tectonics is the horizontal motion of Earth’s thermal boundary layer (lithosphere) over the convecting mantle (asthenosphere) and is mostly driven by lithosphere sinking in subduction zones. Plate tectonics is an outstanding example of a self organizing, far from equilibrium complex system (SOFFECS), driven by the negative buoyancy of the thermal boundary layer and controlled by dissipation in the bending lithosphere and viscous mantle. Plate tectonics is an unusual way for a silicate planet to lose heat, as it exists on only one of the large five silicate bodies in the inner solar system. It is not known when this mode of tectonic activity and heat loss began on Earth. All silicate planets probably experienced a short-lived magma ocean stage. After this solidified, stagnant lid behavior is the common mode of planetary heat loss, with interior heat being lost by delamination and “hot spot” volcanism and shallow intrusions. Decompression melting in the hotter early Earth generated a different lithosphere than today, with thicker oceanic crust and thinner mantle lithosphere; such lithosphere would take much longer than at present to become negatively buoyant, suggesting that plate tectonics on the early Earth occurred sporadically if at all. Plate tectonics became sustainable (the modern style) when Earth cooled sufficiently that decompression melting beneath spreading ridges made thin oceanic crust, allowing oceanic lithosphere to become negatively buoyant after a few tens of millions of years. Ultimately the question of when plate tectonics began must be answered by informa- tion retrieved from the geologic record. Criteria for the operation of plate tectonics includes ophiolites, blueschist and ultra-high pressure metamorphic belts, eclogites, passive margins, transform faults, paleomagnetic demonstration of different motions of different cratons, and the presence of diagnostic geochemical and isotopic indicators in igneous rocks. This record must be interpreted individually; I interpret the record to indicate a progression of tectonic styles from active Archean tectonics and magmatism to something similar to plate tectonics at ~1.9 Ga to sustained, modern style plate tectonics with deep subduction——and powerful slab pull——beginning in Neoproterozoic time.     

浅议徐志摩对拉斐尔前派诗歌的接受

徐志摩是中国卓有影响的新月派诗人.他曾留学英美等西方国家,受西方文化影响很大,尤其是英美浪漫主义和唯美主义对他的影响最大.拉斐尔前派诗歌直接影响了徐志摩的创作思想和诗歌形式.     

Effects of historical land cover changes on climate

In order to explore the influence of anthropogenic land use on the climate system during the last mil- lennium, a set of experiments is performed with an Earth system model of intermediate complexity—— the McGill Paleoclimate Model (MPM-2). The present paper mainly focuses on biogeophysical effects of historical land cover changes. A dynamic scenario of deforestation is described based on changes in cropland fraction (RF99). The model simulates a decrease in global mean annual temperature in the range of 0.09-0.16℃, especially 0.14-0.22℃ in Northern Hemisphere during the last 300 years. The responses of climate system to GHGs concentration changes are also calculated for comparisons. Now, afforestation is becoming an important choice for the enhancement of terrestrial carbon sequestration and adjustment of regional climate. The results indicate that biogeophysical effects of land cover changes cannot be neglected in the assessments of climate change.     

混合地震反演技术及其在东海南部陆架盆地中的应用

介绍了一种在无井或少井情况下的叠前叠后混合地震反演方法。该方法充分利用了叠前反演分辨率高和叠后反演效率高、抗噪能力强的优点。首先应用遗传算法理论在所选控制点的角道集数据上进行叠前波形反演,求取控制点的虚拟纵波速度曲线;然后利用纵波速度曲线和已知地质信息来建立初始模型,进行叠后约束反演。我国东海南部陆架盆地勘探程度低、探井数量少,适合于混合地震反演技术的应用。利用该地区的实际资料进行了混合地震反演,并对影响混合地震反演效果的关键因素（层速度、角道集数据、迭代次数、已知地质信息）进行了分析。结果表明,为了获取虚拟纵波速度,需要准确的速度谱和角道集数据;为了增强叠前反演的实用性,需要选择恰当的控制点;充分利用已知地质信息,可以减小叠后反演结果的多解性。     

论翻译中译者的现身

劳伦斯.韦努蒂的《译者的隐身》一书从解构主义的观点入手,对十七世纪至今流行的一种通畅翻译、透明的译文的归化翻译策略提出了质疑。本文主要从译者的前见、译者的文化身份、译者的性别和译者的意识形态四个方面入手对译者在翻译中的现身进行分析。     

认不出自己的脸盲症

海德·赛勒患有面孔遗忘症,也就是大众所熟知的"脸盲症"。她说道:"我记不住人脸,对我而言,任何人的脸都只是一张面孔,没有特别之处。我无法像处理车的外观和宠物的样子一般,区分人脸的信息。这不是视力问题,而是认知问题。很多情况下,这种病症可以算是隐性的。因为大脑很容易找到许多其他因素来辨认一个人:头发的颜色、走路的姿态或是某件衣     

《兵部行〈市办药料星赴督师军前〉稿》辑注

《兵部行<市办药料星赴督师军前>稿》是一份珍贵的药材史料,它不仅对研究明代药材及其相关社会经济问题有重要意义,同时还为研究明代战争中药料的使用情况及相关后勤保障提供了一些线索,其中药料是否被用作武器打击对手尤其值得探究.