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1.
梁斌 《海洋世界》2010,(6):70-72
1983年10月6日18点30分,"大庆236轮"自秦皇岛满载15449吨原油驶往黄埔港,11日6点20分,该轮正航行在广东汕头附近海面上,此时,该海域正刮着6级大风,海面上海浪滔天。"大庆236轮"的驾驶员注意到了在"大庆236"后面偏左方向,有两艘船正在驶近,其中一艘集装箱船很快就超过“大庆236”轮驶遗了,另一艘船名为“克拉巴特山”的印度尼西亚货轮9点35分驶到“大庆236”轮左舷正横0.3海里处。  相似文献   

2.
哭声。喊声。撞击声。慌乱的逃生者纷纷跳海,在惊涛骇浪中挣扎……凡是看过《泰坦尼克号》影片的人,对这一幕幕空前惨烈的历史镜头记忆犹新。然而,1999年10月17日清晨,这惊心动魄的情景在中国北部海域再现——由大连开往烟台的“盛鲁”号滚装轮离港不到3小时突然起火,不久即与装载的38辆各型汽车一同沉没,随船的160多名旅客和船员不得不弃船逃生。“盛鲁”踏上不归途呜——一声低沉的汽笛划破了寂静的夜空。10月17日清晨3时15分,大连湾码头,排水量为2380吨的“盛鲁”号滚装轮徐徐离港。“盛鲁”轮是山东烟台轮  相似文献   

3.
漂流卡与原油膜漂移速度的实验研究   总被引:3,自引:0,他引:3  
为了给“胶州湾及附近海域溢油扩散范围的数值预报”提供原油膜和风、流速度间的关系,我们在水槽中利用漂流卡和原油进行了模拟实验。实验中,测量了不同风、流、浪情况下漂流卡和原油膜的漂移速度,并获得了某些经验公式  相似文献   

4.
1997年1月2日,俄罗斯的“纳霍德卡”号油轮(载重13139吨,船龄26年)在日本的岛根县隐歧岛海域沉没,从船上流出的大约5000升的C号重燃料油大面积地污染了日本海沿岸。“纳霍德卡”号油轮的溢油漂浮在福井县三国町附近的海面上,为了防止海洋环境的恶化,当地的人们用长柄勺将重油从海面舀出,那无可奈何的情景令人感触极深,总也不能从脑海中抹去。 1997年7月2日,一艘巴拿马籍油轮(载重147000吨,船龄1年)在日本横浜市本牧码头海域触礁,流出原油1556公升。日本国出动104艘作业船,采用吸油垫除掉漂浮在海面上的油膜,用中和剂对油污进行了处理。出事海域附近的渔船也通力合作参加清除油污的行动,投入的船只最多时3000余艘,大约用了10天才把漂浮的油污清除,而那些沉入海  相似文献   

5.
海洋纵横     
中国温州海关查获全国最大海上走私香烟案中国温州海关近日在浙江温州海域南部查获的两艘台湾走私船,7名走私嫌疑人和“555”、卡地亚、希尔顿等走私香烟押靠岸。温州海关针对当前依然严峻的海上走私势头,多次在温州海域南部设卡拦载,经反复搜索追缉,先后查获台湾走私船“吉丰”轮和“新发”轮,香烟走私1700余箱,案值折合人民币1600多万元,是今年以来查获的全国最大的海上走私  相似文献   

6.
《海洋世界》2007,(3):4-5
2007年3月,“南海一号”整体打捞工程将正式启动。“南海一号”为南宋早期商船,1987年8月在阳江海域意外发现,随之被命名为“南海一号”。该船是迄今为止世界上发现的海上沉船中年代最早、船体最大、保存最完整的远洋贸易商船。以前的探摸显示“南海一号”长约23.8米,宽约9.6米。船舱内保存文物总数估计超过5万件。考古学界普遍认为这艘船与海上丝绸之路有关,价值非凡。[第一段]  相似文献   

7.
《海洋世界》2009,(1):18-22
2008年12月26目,中国人民解放军海军舰艇编队开赴索马里海域执行护航任务。这是新中国的舰队第一次渡海“远征”,也是自15世纪初郑和下西洋之后600年来中国海军的首次远洋作战行动。中国海军护航舰艇编队由中国人民解放军海军南海舰队“武汉”号、“海口”号导弹驱逐舰和“微山湖”号综合补给舰组成。编队主要任务是:保护中国航经亚丁湾、索马里海域船舶、人员安全,  相似文献   

8.
近年来,国际油轮漏油事件频繁,少则漏油数百吨,多则数十万吨,使海洋遭到了严重的石油污染,海洋生态平衡破坏严重。威尔斯海岸是英国唯一的自然生态保护区,但今年初发生的油轮漏油事件可能将毁了这一海区的海洋生态。超级油轮“海皇”号搁浅后7万余吨浓黑原油滚滚流入海中,污染了大片海域,造成严重污染,引起英国朝  相似文献   

9.
继“鹰”号油轮之后,有号称世界上最安全的“渡鸟”号巨型双壳安全型油轮已进入航线营运。 “鹰”号和“渡鸟”号均为美孚石油公司的两艘双壳安全型巨型油轮,后者可满载原油220万桶。  相似文献   

10.
38年前,大连人建造了中国第一艘万吨轮“跃进”号,却在“处女航”中冤沉东海,惊愕全国,震惊世界!大连造船人忍住悲咽,勒紧裤带,又造出了“红旗”号,继承“跃进”号的未成使命,成为“第一艘驶出国门的国产万吨轮”。这一对“姐妹船”在中国造船、航运和外贸历史上记载着深沉浓重的一笔,大连人和中国人民都不会忘记。  相似文献   

11.
The analysis of the structure of the cryolithozone, facies, and thicknesses of the Quaternary sediments and the results of the physicochemical mathematical modeling of the modern shelf of the western part of the Laptev Sea support the influence of the Late Pleistocene glaciations on the heat conditions and the distribution of the permafrost in the area. A ~200-m thick glacier formed under aerial conditions from atmospheric precipitation represented the metamorphosed snow cover. According to the modeling, the long-living (from 60?50 to 10?4 ky) glacier reduced the thickness of the permafrost rocks in the reviewed shelf area for 280–360 m. The Holocene marine transgression additionally decreased the thickness from 50–140 m on the inner shelf to 220–350 m on the outer shelf. The modern submarine cryolithozone 450-0 m thick is wide-spread in the studied region from the coast to the shelf boundary (isobaths of 130–140 m), where it pinches out at a distance of ~380 km from the coast at a depth of ~250 m above the sea level.  相似文献   

12.
We analyze the components of the carbon system of the Sevastopol bay waters and the balance of main sediment-forming substances using the data of field investigations in 1998–2008. The interannual variations of total inorganic carbon and the equilibrium partial pressure of carbon dioxide in the bay water are noted. An increase in the flux of carbon dioxide into the bay and in the content of organic carbon in bottom sediments is revealed, and an explanation of this phenomenon is given. The priority accumulation of organic carbon in the sediments of the bay is established. We assess the interannual variation in the relative abundances of organic and inorganic carbon as an index of the carbon cycle stability.  相似文献   

13.
We generalize and analyze the state of investigations of the influence of river waters on the hydrologic structure of the Black Sea. Specific features of the water, regime and hydrography of rivers flowing into the sea, data on the discharge of rivers, and intrayear and interyear variability of the discharge are presented. We discuss and analyze works studying the transformation of river waters, routes of desalinized sea waters, and their influence on the thermohaline structure and dynamic regime of the sea. Translated by Peter V. Malyshev and Dmitry V. Malyshev  相似文献   

14.
We analyze the results of numerical calculations performed according to the three-dimensional interdisciplinary model of an ecological system of the Black-Sea shelf zone near the estuary of the Danube. The complete system of equations of hydrothermodynamics is solved together with transport equations of the advection-diffusion-reaction type used to describe the transformation of a substance (nitrogen) between the components of the characteristic vectors of the ecosystem: plankton, detritus, and biogenic elements (nitrates). We describe the distinctive features of the circumcontinental distribution of components obtained as a result of numerical experiments and present arguments for the conclusion that the ecosystem of the Danube estuary water area plays the role of a buffer zone between the press of the Danubian biogenic pollutions and the neighbouring areas of the shelf zone and open sea. Translated by Peter V. Malyshev and Dmitry V. Malyshev  相似文献   

15.
Ten years of semistationary studies of the interaction of the ice cover and the coastal relief of the Kandalakhsa Gulf in the White Sea allowed us to reveal the peculiarities of these processes in the warm and cold years and the mechanisms of the origination of ice forms, including ice tents, which govern the character of the tidal flats. Three dynamic fast ice zones are distinguished by their geomorphological location, morphology, and ice dynamics. The dependence of the mechanisms and volumes of the enrichment of the fast ice in the sediments on the coastal zone??s relief was established. At the coast of the Kindo Peninsula (Velikaya Salma Strait), the ice mostly contains fine-sandy sediments. Coarser sediments, including boulders, are occasional and frozen into the ice at the contact of the fast ice and the bottom. At the expense of the ice??s spreading by 4?C6 times in the warm years and 2?C4 times in the cold years, several thousand tons of sediments mostly from the tidal flat??s surface (100?C700 m3 from 1 km of coast in the wide tidal flats and <50 m3 on the steep coasts) are delivered to the water area.  相似文献   

16.
We use many-year archival observations of hydrologic and hydrobiologic state of the Sea of Azov for the identification of the structure of a model of its ecosystem. The ecosystem model, supplemented with expert estimates of bioresource consumption (fish reserve), contamination level, and possible ecologic fines for violation of the sea natural state, is formalized by the method of system dynamics. Hereat, the major part of influence functions is found in terms of observational data with application of self-organization algorithms. We also present the results of simulated experiments with the model of the ecosystem, which enable us to analyse scenarios of its behaviour under the influence of various external factors (wind, river discharge, water exchange with the Black Sea, etc.). Translated by Peter V. Malyshev and Dmitry V. Malyshev  相似文献   

17.
A relationship between paths of the Kuroshio and Kuroshio Extension (KE) is investigated, using the satellite-derived altimetry dataset of 1993–2008. When the Kuroshio takes the nearshore nonlarge meander path or typical large meander path and resultantly goes through the deeper channel (about 2500 m) of the Izu-Ogasawara Ridge, the KE path adopts a relatively stable state with the two quasi-stationary meanders. On the other hand, when the Kuroshio takes the offshore nonlarge meander path and then passes over the shallower part of the Ridge (about 1000 m), the KE path tends to be convoluted, i.e., an unstable state.  相似文献   

18.
The stages of the development of the basin of the Bransfield Strait   总被引:1,自引:0,他引:1  
The study of the sedimentary body of the Bransfield Strait has made it possible to identify several sedimentary complexes, to construct the first electronic charts for the acoustic basement, and to establish four stages of the evolution of its floor, which updates the previous knowledge about the formation of the strait. At the first stage, there was an increase in tension stresses that were accompanied by the local splits of the continental crust at the periphery of the Antarctic Peninsula. At the second stage, a graben-like structure filled with the Lower stratigraphic complex was formed northward of the Antarctic Peninsula. At the third stage, the continuing processes of extension led to intensive explosive activity of the growing volcanic structures and filling of the graben with sediments of the Middle seismostratigraphic complex. The fourth stage, which has continued until recently, is characterized by quasi-linear localization of the major centers of volcanic activity in the band closer to the South-Shetland Islands and the formation of the Upper seismostratigraphic sedimentary complex. The evolution of the floor of the Bransfield Strait reflects the process of penetration of the American-Antarctic ridge to the continental lithosphere of the Antarctic Peninsula for the last million years.  相似文献   

19.
The first data on the temporal evolution of the slope of the buried depression of the Black Sea are obtained. The sharp change in the rate of the decrease in the slope steepness that occurred in the Late Miocene-Pliocene time reflects a reorientation of the vector of mutual movement and a related intensification of the collision between the Arabian and Eurasian lithospheric plates.  相似文献   

20.
Three mathematical models are considered: a two-dimensional model for calculating the concentration fields of the ecosystem components on the shelf of the Republic of Guinea, a pointwise model for the annual variation of the components, and a two predators-prey model. These models are used to study the effect of hydrodynamic conditions on the state of the shelf ecosystem and for research into the causes which distort the balance between marketable and unmarketable fish.Translated by Mikhail M. Trufanov.  相似文献   

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