新能源汽车技术专业“1+X”课证融合思考

在《国家职业教育改革实施方案》当中,明确提出了开启"1+X"的证书制度,其主要目的是要利用把学历教育和技能培训进行有效融合,培养出符合时代需求的高素质技术技能人才。以新能源车技术专业作为实例,对"1+X"制度进行积极地探索,找到培养高品质应用型技术人才的新方式,从新能源汽车技术专业的课程内容、考核方式、师资力量等各方面进行探索,为"1+X"课证融合的有效开展寻找高效途径,从而提高人才的质量。     

基于精准供给教学团队建设的路径与成效--以广东生态工程职业学院林业技术专业群为例

教学团队的建设是职业教育的关键,高质量的师资力量能够明确人才培养目标、保证教学质量、推动专业建设、实现人才的精准供给。文中以广东生态工程职业学院林业技术专业群为例,基于精准供给的视角,总结了教学团队建设的路径:一是构建合理的团队结构;二是建立团队带头人管理机制;三是建立"传帮带"培养模式;四是推进校企合作机制;五是构建技能学习型团队;六是强化信息化教学。实践证明,加强教学团队的建设,对促进专业的发展、实现人才精准供给具有积极的作用。     

引汉济渭工程岭北TBM无扩大洞室刀盘边块更换技术

本文以陕西省引汉济渭工程岭北TBM施工段为依托,为解决TBM在狭小空间内较大部件更换维修困难难题,开展大直径TBM刀盘边块在狭小空间内更换技术研究。通过大量研究,创新性提出新刀盘边块更换方法——基坑法,即通过专用设备配合TBM固有性能,在无扩大洞室工况下完成刀盘边块更换。经岭北TBM刀盘边块更换实例证明,此方法操作简单、适用性高,尤其在狭小空间内更具有优越性,且能节省大量维修时间,有效提高施工工效,可为同类TBM施工提供有益借鉴。     

Influence of initial heeling angle on ship roll motion response北大核心CSCD

[目的]系统地研究初始横倾角对随机横浪下船舶横摇运动响应的影响。[方法]以路径积分法为基础,通过数值求解控制横摇运动微分方程概率属性的Fokker-Planck方程,得到横摇运动响应的概率分布。[结果]结果显示,初始横倾角对船舶横摇运动响应谱的影响有限,但对横摇角概率分布以及横摇运动响应极值分布的影响十分明显,且会造成船舶安全性的显著恶化。[结论]路径积分法可作为研究随机海浪下船舶横摇运动特性的有效数值方法。     

不同水文组合对长江口南港流场的影响

长江口南港河段流场受径流、潮流、地形及风浪的影响,相当复杂。现场资料耗资巨大,且水文条件差别较大,模型进行了12种不同水文组合的试验,以弥补现场资料的不足。根据试验结果对南港河段水位、流量、流速的变化规律进行了研究,同时分析了南港的流场特征。     

苏通长江大桥4号主墩钢吊箱设计

苏通长江公路大桥4号主墩钢吊箱是目前世界桥梁建筑中采用规模最大的施工设施。阐述了4号主墩钢吊箱设计理念,确定分析了首节吊箱的起吊、吊箱整体下沉定位、浇筑水下砼封底、吊箱内抽水及承台砼浇筑等主要工况,并采用了信息化施工等先进技术。使用及现场实例结果说明钢吊箱的结构设计是十分成功的。     

信息系统综合集成技术

综合集成作为我军实现新军事变革的重要方法，越来越受到各方面的广泛重视，首先概要介绍了综合集成的理念和实现的三个层次，着重分析介绍了信息系统综合集成中相关软件技术的发展和应用。     

川江上游船型比选思路探讨

本文在分析川江上游运输船舶现状的基础上,提出船型比选的原则,并阐述了对现有船型比选的思路和方法,最后介绍了采用VB开发的计算机比选程序。     

Organic carbon budget for the Gulf of Bothnia

We calculated input of organic carbon to the unproductive, brackish water basin of the Gulf of Bothnia from rivers, point sources and the atmosphere. We also calculated the net exchange of organic carbon between the Gulf of Bothnia and the adjacent marine system, the Baltic Proper. We compared the input with sinks for organic carbon; permanent incorporation in sediments and mineralization and subsequent evasion of CO₂ to the atmosphere. The major fluxes were riverine input (1500 Gg C year^− 1), exchange with the Baltic Proper (depending on which of several possible DOC concentration differences between the basins that was used in the calculation, the flux varied between an outflow of 466 and an input of 950 Gg C year^− 1), sediment burial (1100 Gg C year^− 1) and evasion to the atmosphere (3610 Gg C year^− 1). The largest single net flux was the emission of CO₂ to the atmosphere, mainly caused by bacterial mineralization of organic carbon. Input and output did not match in our budget which we ascribe uncertainties in the calculation of the exchange of organic carbon between the Gulf of Bothnia and the Baltic Proper, and the fact that CO₂ emission, which in our calculation represented 1 year (2002) may have been overestimated in comparison with long-term means. We conclude that net heterotrophy of the Gulf of Bothnia was due to input of organic carbon from both the catchment and from the Baltic Proper and that the future degree of net heterotrophy will be sensible to both catchment export of organic carbon and to the ongoing eutrophication of the Baltic Proper.     

Distribution of suspended sediment in the coastal sea off the Ganges–Brahmaputra River mouth: observation from TM data

Remote sensing technique was applied to estimate suspended sediment concentration (SSC) and to understand transportation, distribution and deposition of suspended sediment in the estuary and throughout the coastal sea, off the Ganges–Brahmaputra River mouth. During low river discharge period, zone of turbidity maximum is inferred in the estuary near the shore. SSC map shows that maximum SSC reaches 1050 mg/l in this period. Magnitude of SSC is mainly owing to resuspension of the bottom surface sediments induced by tidal currents flowing over shallow water depths. The influence of depth on resuspension is farther revealed from the distribution and magnitude of SSC along the head of Swatch of No Ground (SNG) submarine canyon. During high river discharge period, huge river outflow pushed the salt wedge and flashes away the suspended sediments in the coastal sea off the river mouth. Zone of turbidity maximum is inferred in the coastal water approximately within 5–10 m depth of water, where the maximum SSC reaches 1700 mg/l. In this period, huge fluvial input of the suspended sediments including the resuspended bottom sediments and the particles remaining in suspension for longer period of time since their initial entry control mainly the magnitude of SSC. In the estuary near the shore, seasonal variation in the magnitude of SSC is not evident. In the coastal sea (>5 m water depth), seasonal influence in the magnitude of SSC could be concluded from the discrepancy between SSC values of two different seasons. Transportation and deposition of suspended sediments also experiences seasonal variations. At present, suspended sediments are being accumulated on the shallow shelf (between 5 and 10 m water depth) in low discharge period and on the mid-shelf (between 10 and 75 m water depth) during high discharge period. An empirical (exponential) relationship was found between gradual settle down of suspended sediments in the coastal sea and its lateral distance from the turbidity maximum.