Modelling the silica pump in the Permanently Open Ocean Zone of the Southern Ocean

A coupled 1D physical–biogeochemical model has been built to simulate the cycles of silicon and of nitrogen in the Indian sector of the Permanently Open Ocean Zone of the Southern Ocean. Based on a simplified trophic network, that includes two size classes of phytoplankton and of zooplankton, and a microbial loop, it has been calibrated by reference to surface physical, chemical and biological data sets collected at the KERFIX time-series station (50°40′S–68°25′E). The model correctly reproduces the high nutrient low chlorophyll features typical of the studied area. In a region where the spring–summer mixed layer depth is usually deeper than 60 m, the maximum of chlorophyll never exceeds 1.5 mg m⁻³, and the annual primary production is only 68 g C m⁻² year⁻¹. In the surface layer nitrate is never exhausted (range 27–23.5 mmoles m⁻³) while silicic acid shows strong seasonal variations (range 5–20 mmoles m⁻³). On an annual basis 71% of the primary production sustained by nanophytoplankton is grazed by microzooplankton. Compared to North Atlantic, siliceous microphytoplankton is mainly prevented from blooming because of an unfavourable spring–summer light-mixing regime. Silicic acid limitation (high half saturation constant for Si uptake: 8 mmoles m⁻³) also plays a major role on diatom growth. Mesozooplankton grazing pressure excerpts its influence especially in late spring. The model illustrates the efficiency of the silica pump in the Southern Ocean: up to 63% of the biogenic silica that has been synthetized in the photic layer is exported towards the deep ocean, while only 11% of the particulate organic nitrogen escapes recycling in the surface layer.     

Phytoplanktonic nutrient utilisation and nutrient signature in the Southern Ocean

The separation in Southern Ocean provinces of silicate excess at nitrate exhaustion and of nitrate excess at silicate exhaustion was already introduced by Kamykowski and Zentara (Kamykowski, D., Zentara, S.J., 1985. Nitrate and silicic acid in the world ocean: patterns and processes. Mar. Ecol. Prog. Ser. 26, 47–59; and Kamykowski, D., Zentara, S.J., 1989. Circumpolar plant nutrient covariation in the Southern Ocean: patterns and processes. Mar. Ecol. Prog. Ser. 58, 101–111) and our investigations of the silicate to nitrate uptake ratios confirm the earlier distinction. Oligotrophic antarctic waters mainly exhibit proportionally higher silicate removal what induces a potential for nitrate excess. The nitrogen uptake regime of such areas is characterised by low absolute as well as specific nitrate uptake rates throughout. Maximal values did not exceed 0.15 μM d⁻¹ and 0.005 h⁻¹, respectively. Corresponding f-ratios ranged from 0.39 to 0.86. This scenario contrasts strikingly to the more fertile ice edge areas. They showed a drastic but short vernal increase in nitrate uptake. Absolute uptake rates reached a maximum value of 2.18 μM d⁻¹ whereas the maximal specific uptake rate was 0.063 h⁻¹. In addition to an optimal physical environment for bloom development, accumulation of ammonium stimulated nitrate uptake in a direct or indirect way. Since ammonium build-up in surface waters traces enhanced remineralisation, release of other essential compounds during degradation of organic matter might have been the main trigger. This peak nitrate utilisation during early spring led to the observed potential for silicate excess. With increasing seasonal maturity the nitrate uptake became inhibited by the presence of enhanced ammonium availability (up to 8% of the inorganic nitrogen pool), however, and after a short period of intensive nitrate consumption the uptake rates drop to very low levels, which are comparable to the ones observed in the area of nitrate excess at silicate exhaustion.     

Size-fractionated phytoplankton biomass and species composition in the Indian sector of the Southern Ocean during austral summer

During the late austral summer of 1994, Antarctic waters were characterized by low phytoplankton biomass. Along the 62°E meridian transect, between 49°S and 67°S, chlorophyll (Chl.) a concentration in the upper 150 m was on average 0.2 mg m⁻³. However, in the Seasonal Ice Zone (SIZ) chlorophyll a concentrations were higher, with a characteristic deep chlorophyll maximum. The highest value (0.6 mg Chl. a m⁻³) was measured at the Antarctic Divergence, 64°S, corresponding to the depth of the temperature minimum (100 m). This deep biomass maximum decreased from South to North, disappeared in the Permanently Open Ocean Zone (POOZ) and reappeared with less vigour in the vicinity of the Polar Front Zone (PFZ). In the SIZ, the upper mixed layer was shallow, biomass was higher and the >10 μm fraction was predominant. In this zone the >10 μm, 2–10 μm and <2 μm size fractions represented on the average 46%, 25.1% and 28.9% of the total integrated Chl. a stock in the upper 100 m, respectively. The phytoplankton assemblage was diverse, mainly composed of large diatoms and dinoflagellate cells which contributed 42.7% and 33.1% of the autotrophic carbon biomass, respectively. Moving northwards, in parallel with the decrease in biomass, the biomass of autotrophic pico- and nanoflagellates (mainly Cryptophytes) increased steadily. In the POOZ, the picoplanktonic size fraction contributed 47.4% of the total integrated Chl. a stock. A phytoplankton community structure with low biomass and picoplankton-dominated assemblage in the POOZ contrasted with the relatively rich, diverse and diatom-dominated assemblage in the SIZ. These differences reflect the spatial and temporal variations prevailing in the Southern Ocean pelagic ecosystem.     

水下船舶判定海面海况技术研究

通过对水下船舶的海浪观测谱分析,提出水下船舶适用的测海况模型,并对该模型进行实验验证,为该类装置的技术改进提供理论和实验支持。     

风帆助航技术实船应用的若干思考

首先分析了风帆助航装置应用在远洋船舶上的技术要求,通过对海洋风能资源特点、风帆的选择及其控制、船舶稳性校核、风帆助航装置的操纵和维护管理等问题的分析,风帆助航技术在远洋船舶上的应用被证明是可行的,它将成为船舶节能减排的重要措施,其推广应用对我国航运业的可持续发展将有着积极的意义。     

Impact of container chassis management practices in the United States on terminal operational efficiency: An operations and mitigation policy analysis

Existing policies designed to mitigate the environmental and social impacts of truck queuing at maritime terminals often focus on congestion problems outside of the terminal gate, targeting a reduction in the waiting and turn time of trucks as the measure of success. This paper evaluates the impact that intra-terminal truck and equipment movements have on the terminal’s overall performance and the implications that these movements have on the effectiveness of current mitigation policies. Through a simulation of terminal processes occurring at Southern California ports it is shown that measures driving reductions in truck turn times impose greater operational loads on terminal equipment, essentially transferring savings in truck turn time rather than eliminating it in terms of the overall system. Consequently, the paper finds that total truck and cargo handling equipment movement and operational time constitutes a more accurate measure of the effectiveness of policies seeking to mitigate the impacts of truck operations at marine terminals.     

Reconstruction of the Aceh Region following the 2004 Indian Ocean tsunami disaster: A transportation perspective

Aceh, located in the northernmost area of Sumatra Island, is one of the regions that suffered the most damage from the Indian Ocean tsunami in 2004. The process of reconstruction after a large-scale disaster is considered an opportunity to create a safer society, especially for developing countries, however the accumulation of knowledge about how to improve reconstruction is insufficient. The affected areas have diverse social and economic characteristics and unprecedented restoration efforts have been made. The Indian Ocean tsunami disaster, therefore, provides numerous research opportunities, and many surveys and other researches have been conducted to better understand what happened and how the reconstruction process could be improved. However, the majority of such research has focused on housing reconstruction, rebuilding livelihoods and community rehabilitation and there has been only limited research on transportation-related issues. Thus, there is significance in evaluating the reconstruction of Aceh from a transportation perspective, a dimension that has yet to be examined systematically. As a first step in the effort to evaluate various aspects of the reconstruction of Aceh from a transportation perspective, this research aims to present three transportation-related issues within the reconstruction process—1) the road network in the Banda Aceh coastal area, 2) mobility in relocation sites, and 3) reconstruction of the Banda Aceh–Meulaboh road—and to conduct a preliminary analysis of these issues by adding the viewpoint of disaster management and reconstruction, the authors' area of specialization. For conducting a preliminary analysis, existing information such as research papers, articles and reports and data collected through interviews and field reconnaissance conducted by the authors were utilized as much as possible, and such “qualitative data” was analyzed by applying the “interpretive approach”, considered an appropriate analytical framework for qualitative data.     

基于工程简化的Topside管廊结构疲劳寿命分析

对“船形”海洋工程结构的疲劳评估方法进行了详细讨论,并结合有限元法,采用工程简化实用的疲劳评估方法,对某海洋工程Topside管廊结构的疲劳损伤和疲劳寿命进行计算分析,验证了该结构抗疲劳设计的合理性。此疲劳分析过程简单方便,可为类似工程结构的疲劳寿命分析提供参考。     

Annual cycle of distribution of three ice-associated copepods along the coast near Dumont d'Urville, Terre Adélie (Antarctica)

In polar regions sea ice is a site of enhanced primary production during winter and provides important habitat for small grazers, such as copepods. We sampled zooplankton from the sea ice and water column throughout 2005, near Dumont d'Urville station (Terre Adélie, Antarctica). Three species of ice-associated copepods were found: two calanoid copepods Paralabidocera antarctica and Stephos longipes and the harpacticoid copepod Drescheriella glacialis. P. antarctica was the most abundant of the three and was closely associated with the sea ice during most of the year. This species had a one year life cycle with a probable over-wintering period in the sea ice as nauplii and a short copepodite phase in spring. Reproduction and spawning occurred in early summer. A comparison with two other populations (near Syowa and Davis stations) along the east coast of Antarctica showed that there was a temporal shift in the life cycles of the three populations, which was linked to variability in sea ice conditions. D. glacialis was the second most abundant copepod and was more common during the winter than during summer, indicating its preference for the sea ice habitat. In autumn, the presence of D. glacialis in the deeper part of the water column suggested that this species colonised the sea ice from the benthos. S. longipes was found only in the water column near Dumont d'Urville and was not very abundant. In Terre Adélie particular environmental conditions, such as the absence of a permanent sea ice zone throughout the year, a longer time of open water, strong katabatic winds and the presence of polynyas, have influenced both the abundance and distribution of the three common ice-associated copepods.     

马尔代夫群岛与印度洋的海贝贸易

从史前时期开始,马尔代夫群岛出产的海贝就是印度洋地区不少沿岸国家的传统货币,甚至经由缅甸、暹罗和孟加拉等地辗转输入中国,成为我国云南、四川等西南边疆地区的流通货币。本文根据中外相关文献的记载,对马尔代夫群岛海贝的名称、产地、捕捞、加工、运输、互市、贸易航线、马尔代夫帆船和水手、土著王室的垄断、穆斯林商人等问题逐一进行考察。本文认为,历史上马尔代夫群岛的海贝贸易曾经相当繁盛,孟加拉湾与波斯湾分别是印度洋东部航线与西部航线的海贝集散中心,印度的穆斯林商贾则在其中扮演了相当重要的角色。海贝在印度洋沿岸国家的贸易与流动,就像是一张无形的网络,将古代中国的西南腹地整合进了以孟加拉湾为中心的印度洋货币体系,进而说明古代云南和四川等地曾一度是印度洋海洋文明圈的一个不可分割的组成部分。