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31.
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33.
Two processes are generally explained as causes of temporal changes in the stoichiometric silicon/nitrogen (Si/N) ratios of
sinking particles and of nutrient consumption in the surface water during the spring diatom bloom: (1) physiological changes
of diatom under the stress of photosynthesis of diatom and (2) differences of regeneration between silicon and nitrogen. We
investigated which process plays an important role in these changes using a one-dimensional ecosystem model that explicitly
represents diatom and the other non-silicious phytoplankton. The model was applied to station A7 (41°30′ N, 145°30′ E) in
the western North Pacific, where diatom regularly blooms in spring. Model simulations show that the Si/N ratios of the flux
exported by the sinking particles at 100 m depth and of nutrient consumptions in the upper 100 m surface water have their
maxima at the end of the spring diatom bloom, the values and timings of which are significantly different from each other.
Analyses of the model results show that the differences of regeneration between silicon and nitrogen mainly cause the temporal
changes of the Si/N ratios. On the other hand, the physiological changes of diatoms under stress can hardly cause these temporal
changes, because the effect of the change in the diatom's uptake ratio of silicon to nitrogen is cancelled by that in its
sinking rate. 相似文献
34.
Several large deployments of neutrally buoyant floats took place within the Antarctic Intermediate (AAIW), North Atlantic Deep Water (NADW), and the Antarctic Bottom Water (AABW) of the South Atlantic in the 1990s and a number of hydrographic sections were occupied as well. Here we use the spatially and temporally averaged velocities measured by these floats, combined with the hydrographic section data and various estimates of regional current transports from moored current meter arrays, to determine the circulation of the three major subthermocline water masses in a zonal strip across the South Atlantic between the latitudes of 19°S and 30°S. We concentrate on this region because the historical literature suggests that it is where the Deep Western Boundary Current containing NADW bifurcates. In support of this notion, we find that a net of about 5 Sv. of the 15–20 Sv that crosses 19°S does continue zonally eastward at least as far as the Mid-Atlantic Ridge. Once across the ridge it takes a circuit to the north along the ridge flanks before returning to the south in the eastern half of the Angola Basin. The data suggest that the NADW then continues on into the Indian Ocean. This scheme is discussed in the context of distributions of dissolved oxygen, silicate and salinity. In spite of the many float-years of data that were collected in the region a surprising result is that their impact on the computed solutions is quite modest. Although the focus is on the NADW we also discuss the circulation for the AAIW and AABW layers. 相似文献
35.
With the development of high-resolution multibeam echosounder systems (MBES) for surveying shallow-water areas a new tool is available to monitor rapid changes in seabed morphology as, e.g., caused by the dumping of dredge spoil in coastal waters. In this study, four data sets of repeated bathymetric surveys with a MBES were processed and analyzed. The data were collected in a 1.94-km2 dumping site in the outer Weser Estuary (German Bight). Between June and December 1998, 2.6 million m3 of dredged sediment were deposited there. The bathymetric maps generated in the course of this study reveal features such as subaqueous dunes, scour holes, and mounds of dumped dredge spoil. The mean water depth decreased by about 1 m during the dumping period. Furthermore, difference grids showing changes in sediment volume allowed a calculation of the sediment budget for the monitored area. After a time period of only 5 months, 0.5 million m3 of the originally dumped 2.6 million m3 of dredge spoil had already been removed from the dumping site. 相似文献
36.
晚中生代─新生代南海周缘地块运动与南海演化 总被引:1,自引:0,他引:1
报道了由华南几个盆地的古地磁数据综合而得的反映该区白垩纪以来古纬度变化曲线,结合Schmidtke等(1990)发表的加里曼丹150Ma以来的古地磁数据,表明华南与加里曼丹在40Ma前具有大致相同的古纬度变化史,差异仅出现在距今30Ma前后和10Ma以来。若此趋势可靠,则可作出下列推断:(1)南海的扩张只能发生在距今30Ma附近或10Ma以后华南与加里曼丹反向运动时期;距今30Ma的扩张已被广为接受;(2)华南与加里曼丹之向可能存在的古南海只能在91Ma之前存在;(3)南海演化可能存在两期扩张。南海的拟合可通过沿3500m等深线的先道时针旋转、后北向平移两个步骤完成。这与Hayashida等(1991)提出的日本海张开与扩张模式很相似,提示东亚边缘海的形成和演化可能具有同样的机制。华南距今50Ma以来的古纬度变化与Tapponnier(1982)的传播挤出构造模式所预期的基本吻合,表明距今50Ma以来华南古纬度变化的运动学机制可用Tapponnier模式作解释。 相似文献
37.
东海黑潮及琉球群岛以东海流研究进展 总被引:4,自引:0,他引:4
东海是西太平洋的一个边缘海,它西部有广阔的大陆架,东面以九州岛、琉球群岛(由奄美诸岛、冲绳诸岛、先岛诸岛组成)和台湾岛连线为界,具有较深的海槽。黑潮是一支高温、高盐、高流速的西边界流,它起源于菲律宾以东海域、流经台湾东岸进入东海,沿东海大陆架外缘向东北向流动,穿越吐噶喇海峡返回太平洋。通常的把自台湾东北端起至吐噶喇海峡一段称为东海黑潮。此外,在琉球群岛以东海域也常年存在一支稳定的西边界流,称为琉球海流。
对于东海黑潮和琉球海流的硏究,主要起步于20世纪80年代,通过进行中日联合调查研究、中日副热带环流调查研究等,取得了许多重要成果,苏纪兰(1994)、袁耀初(2000,Yuan,2006)、管秉贤(2002)等人都做过评述。本文基于以上研究评述,主要叙述200年以来对东海黑潮及琉球海流的硏究新进展。 相似文献
38.
随着工业的高速发展和人口的急剧増加及环境污染的加剧,淡水资源危机已引起世界各国的普遍关注。据统计,城市用水中工业用水通常占80%左右,而工业用水中有80%是工业冷却用水,所以开发利用海水代替淡水直接作冷却用水是节约淡水的重要途径。海水直流冷却系统具有深海取水温度低且恒定、冷却效果好和系统管理简单等优点,但必须具备以下条件:(1)管道系统防除生物附着污损;(2)管道系统的防结垢;(3)金属腐蚀与防护。多年来有关方面虽然相应地采取了许多措施,但由于主设备通常需常年连续运行,因而往往出现在某段时间、某些部位上效果降低与失效。现行的对海水环境中生物附着腐蚀检测主要采取取样离位分析方法,其结果与实际状态有差异,且生过程中许多重要部位,如海上平台、浮码头、船舶、海滨电厂、化工厂的海水冷却系统和海水管路的管道内、及死角区都很难取样,必要时只有定期停机检查(侯保荣1998; Efird,1976;吉井彻,1967),造成很大的经济损失。
防止海水环境中的金属设施遭受海水腐蚀和海洋生物污损的方法很多,通常采用阴极保护、防污涂料、电解海水或电解重金属等方法,但这些方法的缺点是:(1)阴极保护能防止金属腐蚀而不能防止海洋生物附着;(2)防污涂料涂刷一次,只能用3-5年,对许多一次性埋入水中的管件无法进行二次补涂,防污涂料所释放出的毒物将长期污染环境;(3)利用电解海水或电解重金属所产生的次氯酸钠或重金属离子来进行防污,即电解防污效果明显,但对金属防腐的作用不大(侯保荣,1999;陈光章,1994;马土德,1996)。总结前人的经验,经过多年的研究,我们利用电化学方法研制出既能防止金属海水腐蚀又能防生物附着的双防与检测新技术系统装置,已通过实海实验,取得了良好的效果。 相似文献
39.
中国"数字海洋"发展的基本构想 总被引:16,自引:4,他引:16
为迎接海洋21世纪,中国从国家发展的战略的高度出发,将发展“数字海洋”列入“十五”和2015年海洋科学发展计划。其目标是广泛收集海洋立体监测信息,全面完成海洋信息化工程和空间数据基础设施建设基本实现海洋信息共享和“数字海洋”基础工程建设。 相似文献
40.
Size-Fractionated Primary Production Estimated by a Two-Phytoplankton Community Model Applicable to Ocean Color Remote Sensing 总被引:3,自引:0,他引:3
In order to estimate primary production from ocean color satellite data using the Vertical Generalized Production Model (VGPM; Behrenfeld and Falkowski, 1997), we propose a two-phytoplankton community model. This model is based on the two assumptions that changes in chlorophyll concentration result from changes of large-sized phytoplankton abundance, and chlorophyll specific productivity of phytoplankton tends to be inversely proportional to phytoplankton size. Based on the analysis of primary production data, P
opt
B
, which was one parameter in the VGPM, was modeled as a function of sea surface temperature and sea surface chlorophyll concentration. The two-phytoplankton community model incorporated into the VGPM gave good estimates in a relatively high productive area. Size-fractionated primary production was estimated by the two-phytoplankton community model, and P
opt
B
of small-sized phytoplankton was 4.5 times that of large-sized phytoplankton. This result fell into the ranges observed during field studies. 相似文献