跨洋流动、地方适应与中国联结——毛里求斯华人社团与社会探析

基于田野调查与文献研究,从华人社团组织与社会发展的角度,可见毛里求斯华人的跨洋流动、文化适应与地方化进程,而华人社团的历史变迁,见证了毛里求斯华人跨洋寻求发展的历程。毛里求斯华人社团活动与社会关系的交织重叠,乃华人社会与文化延续的内在动力,同时也为当地华人提供了更为广泛的公共空间。随着中国的崛起,加之毛里求斯作为中非之间人、物流动"中转站"的特殊地理区位,更使两国之间的经济、文化交流在全球时代日趋频繁,并对毛里求斯的华人社团乃至地方社会产生了更进一步的影响。     

古代中朝海上交往与船文化交流

本文以古代中朝海上交通为主线,论及华夏文明在朝鲜半岛的传播以及中国古代造船技术对朝鲜的影响.频繁的海上贸易导致黄海两侧中朝港口的繁荣.     

东海大桥Ⅶ标主桥斜拉桥的施工控制

东海大桥Ⅶ标主桥颗珠山大桥,是一座双塔双索面结合梁斜拉桥,通过对施工的精心控制及对各种因素的详细分析,大桥的线形和索力符合设计要求,合拢精度达到了±1 mm的水平。     

西部地区高速公路发展规划生态环境影响评价——指标体系构建及评价方法探讨

在探讨战略环境评价意义的基础上，按照战略环境评价指标体系构建的一般步骤，针对高速公路规划自然生态环境的影响因素，建立了公路交通发展的战略性生态环境评价的可选指标集，并根据指标的特点给出了一种基于GIS技术的评价方法。这种构建指标体系的方法简单易行，评价要素明确，层次分明，构建的可选指标集可为西部地区高速公路发展规划生态环境评价提供参考。     

西江水运主通道通航枢纽建设关键技术研究

文章主要介绍西部项目西江水运主通道通航枢纽建设研究的背景、内容、成果及关键技术,为其他航运枢纽建设提供了设计、决策的依据,其研究成果具有广阔的应用和参考价值。     

Inorganic carbon fluxes through the boundaries of the Greenland Sea Basin based on in situ observations and water transport estimates

A carbon budget for the exchange of total dissolved inorganic carbon C_T between the Greenland Sea and the surrounding seas has been constructed for winter and summer situations. An extensive data set of C_T collected over the years 1994–1997 within the European Sub-polar Ocean Programmes (ESOP1 and ESOP2) are used for the budget calculation. Based on these data, mean values of C_T in eight different boxes representing the inflow and outflow of water through the boundaries of the Greenland Sea Basin are estimated. The obtained values are then combined with simulated water transports taken from the ESOP2 version of the Miami Isopycnic Coordinate Ocean Model (MICOM). The fluxes of inorganic carbon are presented for three layers; a surface mixed layer, an intermediate layer and a deep layer, and the imbalance in the fluxes are attributed to air–sea exchange, biological fixation of inorganic carbon, and sedimentation. The main influx of carbon is found in the surface and the deep layers in the Fram Strait, and in the surface waters of direct Atlantic origin, whereas the main outflux is found in the surface layer over the Jan Mayen Fracture Zone and the Knipovich Ridge, transporting carbon into the Atlantic Ocean via the Denmark Strait and towards the Arctic Ocean via the Norwegian Sea, respectively. The flux calculation indicates that there is a net transport of carbon out of the Greenland Sea during wintertime. In the absence of biological activity, this imbalance is attributed to air sea exchange, and requires an oceanic uptake of CO₂ of 0.024±0.006 Gt C yr⁻¹. The flux calculations from the summer period are complicated by biological fixation of inorganic carbon, and show that data on organic carbon is required in order to estimate the air–sea exchange in the area.     

海浪统计资料对船舶波浪弯矩设计值的影响

对船舶,特别是超规范船舶,进行结构的直接计算设计时,首先要知道波浪弯矩设计值。 要确切地做到这一点,设计人员应合理地选择船舶航行海域的海浪长期统计资料,然后根据船 舶的装载工况和实际可能达到的航速,借用线性理论或非线性理论进行波浪弯矩的长期预报 来确定设计值。本文就一艘大型集装箱船舶,按五个典型海域的海浪统计资料,对波浪弯矩及 波浪合成弯矩作了长期预报计算,并与 ＩＡＣＳ的统一纵强度要求ＵＲ—Ｓ１１的结果作了比较和 分析,给出了对船舶结构直接计算设计有指导意义的几点结论。     

Exchange rate and transport cost sensitivities of bilateral freight flows between the US and China

This paper explores the long-run impacts of gross domestic product, exchange rate, and transport costs on bilateral air and ocean freight flows between the US and China. The study employs a cointegration framework by using export and import data over the period of 2003:Q1-2014:Q2. Results show that gross domestic product is the key determinant of bilateral freight flows, indicating that real income of a trading partner is a driving force of the bilateral freight flows between the US and China. In examining the sensitivities of the bilateral trade flows, air freight flows are found to be more responsive to a real income change than ocean freight flows. The bilateral exchange rate is a significant factor affecting the freight flows from China to the US, suggesting that a US dollar appreciation against the Chinese yuan increases the inflows of Chinese commodities to the US. The impacts of the bilateral exchange rate and transport cost are found to vary at industry and commodity levels. These findings support the importance of employing disaggregate data in the bilateral freight flow analysis.     

Norwegian North Sea action programme: Analysis of measures to reduce nutrient inputs

According to the terms of the Ministerial Declaration on the Protection of the North Sea, input of the nutrients phosphorus (P) and nitrogen (N) to the coast from the Norwegian‐Swedish border to Lindesnes should be reduced by about 50% between 1985 and 1995. The State Pollution Control Authority (SFT) has analyzed how Norway can achieve this reduction in the most cost‐effective way and at the same time achieve the greatest possible improvement in water quality along the Norwegian coast and in its watercourses.

Two alternative sets of measures were analyzed, both of which would meet the requirements of the Declaration. The lowest‐cost alternative would have average annual costs of about NKr 930 million (U.S.S150 million), and investments of about NKr 4000 million (U.S. $643 million). However, this set of measures would not take account of local water quality, and measures would therefore not always be introduced where the need is most pressing. SFT proposed that an alternative set of measures be implemented, almost all of which would also help to achieve local goals for water quality. This alternative will have annual costs of about NKr 980 million (U.S.$158 million), and investments of about NKr 4100 million (U.S.$659 million).     

On the application of hydraulic theory to the deep-water flow through the Irbe Strait

A flow-dependent critical-point method for investigating topographically controlled flow in natural channels is applied to the bottom current through the Irbe Strait connecting the Baltic proper and the Gulf of Riga. This approach is based on the functional formalism due to Gill [Gill, A.E., 1977. The hydraulics of rotating-channel flow. J. Fluid Mech., 80, 641–671.], and here is used for the stratified flow structure observed during the IRBEX-95 field campaign. A critical section of the realizable flow regime was found to be located slightly downstream of the most pronounced horizontal constriction of the channel. The predicted baroclinic volume flux 7200 m³ s⁻¹ overestimates the observed mean bottom-water transport by around 30%, a discrepancy which most likely can be explained by the lack of sea level conditions and friction in the model.