中国航运企业发展现状及对策研究

从中国航运企业所面临机遇、存在的问题两方面出发,即从国际航运市场、政府及企业自身因素分析中国航运企业所处的环境,提出如何提高中国航运企业国际竞争力的策略。     

国际航运物流虚拟联盟伙伴选择研究

提出了国际航运物流虚拟联盟的概念,介绍了国际航运物流虚拟联盟合作伙伴的选择程序。根据合作伙伴选择评价的原则和我国航运物流企业的现状,初步构建了国际航运物流虚拟联盟合作伙伴的选择评价指标体系,然后采用调查问卷的形式,对选择评价指标体系进行了修正。以鼎盛航运物流公司为例,采用层次分析法(AHP)对国际航运物流虚拟联盟进行了实证分析,结果合理、实用。     

航运电子市场价格监控机制研究

通过对航运电子市场价格监控系统构成要素、基本功能的阐述,分析了航运电子市场价格监控系统的建立原则,提出了航运电子市场价格监控的事前四级监管机制、事中价格实时监测与预警机制、事后应急处理机制。     

建立上海国际航运中心的研究

在上海建立国际航运中心，是尽快把上海建成国际经济、贸易、金融中心的重要组成部分，两者相辅组成。该文对建立国际航运中心的必要性与可能性，基本功能与特征，存在问题，发展目标与建设步骤，从理论上与实际上进行了分析，在此基础上，提出了符合国际经济发展方向、并且有可操作性的结论与建议。     

香港回归与上海经济和航运业的发展

随着１９９７年香港的回归和９０年代上海经济持续稳定的发展，中国未来半出现丙个国际中心城市－香港和上海。如何认识这两个国际中心城市之间的关系对中国经济的发展是至关重要的。本文从经济和航运两方面对这一问题进行了深入的分析。     

加快上海枢纽港建设,促进城市经济的发展

本文从枢纽港、航运中心和城市经济金融贸易中心之间的相互关系，说明上海经济金融贸易中心的建立，必须以发达的航运业为基础，而枢纽港建设是航运发展、航运中心建立的关键。上海枢纽港的建设，有利于增强与亚太地区其它中心港、枢纽港的竞争能力，从而更好地参与世界集装箱运输大循环，有利于加快上海经济金融贸易中心的建立，促进上海经济的快速发展。同时文章从上海及周边腹地经济的发展状况等方面阐述了上海建设国际枢纽港的可能性，最后指出了拓宽融资渠道，加快上海枢纽港建设的途径。     

张力式平台运动响应的理论计算与模型试验

本文对一座51700t作业水深为256m的张力式平台模型在规则波及不规则波中进行了试验,并利用二维及三维计算程序计算了该平台的波频运动响应,计算与实验结果颇为一致。文中还讨论了运动响应的非线性问题,最后对在生存海况下估算张力式平台纵荡及横荡的方法提出了看法。     

Carbonate chemistry dynamics and carbon dioxide fluxes across the atmosphere–ice–water interfaces in the Arctic Ocean: Pacific sector of the Arctic

Climatic changes in the Northern Hemisphere have led to remarkable environmental changes in the Arctic Ocean, which is surrounded by permafrost. These changes include significant shrinking of sea-ice cover in summer, increased time between sea-ice break-up and freeze-up, and Arctic surface water freshening and warming associated with melting sea-ice, thawing permafrost, and increased runoff. These changes are commonly attributed to the greenhouse effect resulting from increased atmospheric carbon dioxide (CO₂) concentration and other non-CO₂ radiatively active gases (methane, nitrous oxide). The greenhouse effect should be most pronounced in the Arctic where the largest air CO₂ concentrations and winter–summer variations in the world for a clean background environment were detected. However, the air–land–shelf interaction in the Arctic has a substantial impact on the composition of the overlying atmosphere; as the permafrost thaws, a significant amount of old terrestrial carbon becomes available for biogeochemical cycling and oxidation to CO₂. The Arctic Ocean's role in determining regional CO₂ balance has been ignored, because of its small size (only  4% of the world ocean area) and because its continuous sea-ice cover is considered to impede gaseous exchange with the atmosphere so efficiently that no global climate models include CO₂ exchange over sea-ice. In this paper we show that: (1) the Arctic shelf seas (the Laptev and East-Siberian seas) may become a strong source of atmospheric CO₂ because of oxidation of bio-available eroded terrestrial carbon and river transport; (2) the Chukchi Sea shelf exhibits the strong uptake of atmospheric CO₂; (3) the sea-ice melt ponds and open brine channels form an important spring/summer air CO₂ sink that also must be included in any Arctic regional CO₂ budget. Both the direction and amount of CO₂ transfer between air and sea during open water season may be different from transfer during freezing and thawing, or during winter when CO₂ accumulates beneath Arctic sea-ice; (4) direct measurements beneath the sea ice gave two initial results. First, a drastic pCO₂ decrease from 410 μatm to 288 μatm, which was recorded in February–March beneath the fast ice near Barrow using the SAMI-CO₂ sensor, may reflect increased photosynthetic activity beneath sea-ice just after polar sunrise. Second, new measurements made in summer 2005 beneath the sea ice in the Central Basin show relatively high values of pCO₂ ranging between 425 μatm and 475 μatm, values, which are larger than the mean atmospheric value in the Arctic in summertime. The sources of those high values are supposed to be: high rates of bacterial respiration, import of the Upper Halocline Water (UHW) from the Chukchi Sea (CS) where values of pCO₂ range between 400 and 600 μatm, a contribution from the Lena river plume, or any combination of these sources.     

航运服务业集聚模式的生成机理及要素研究——推进上海国际航运中心建设的思考

为了研究航运服务业集聚的生成模式和生成要素,本文在对服务业集聚理论研究的基础上,根据市场和政府对航运服务业集聚的作用,将其生成模式划分为自然生成模式、政府主导型生成模式和混合推动型生成模式,并分别结合伦敦、新加坡和上海三个城市的航运服务业集聚模式的生成要素进行了系统研究。