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为了促进江苏海洋空间资源科学合理地开发利用,使江苏沿海开发步入科学发展道路,根据江苏沿海海洋空间资源的优势及其开发中面临的诸多挑战,从江苏沿海独特的港航空间资源、岛屿空间资源以及滩涂和沙洲空间资源等条件着手,提出江苏沿海空间资源一系列的开发路径,为江苏沿海新一轮开发提出更有力的科学依据和发展思路. 相似文献
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黄莉新 《海洋与海岸带开发》2009,(12):16-16
沿海地区是江苏发展的潜力和希望所在。党中央、国务院对江苏沿海地区发展高度重视,胡锦涛总书记、温家宝总理作出重要指示、寄予殷切期望。2009年6月,国务院常务会议讨论并通过了《江苏沿海地区发展规划》。这标志着江苏沿海开发已经正式上升到国家层面，成为连接南北、带动中西部地区发展的国家战略。这是江苏人民的多年期盼， 相似文献
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江苏近海紫菜养殖区的空间扩张模式研究 总被引：1，自引：0，他引：1
为精准实施海域使用现状的动态监测与有效管理,开展了江苏近海紫菜养殖区空间扩张模式研究。选取1990年、2000年、2013年和2018年四个时相的Landsat遥感影像为数据源,采用面向对象分类方法提取江苏近海紫菜养殖区的空间分布信息,分别计算1990年、2000年、2013年和2018年江苏近海紫菜区养殖面积并分析其变化趋势,揭示江苏近海紫菜养殖区空间分布特征,并剖析江苏近海紫菜养殖区的空间扩张模式。研究结果表明:(1) 1990年、2000年、2013年和2018年,江苏近海紫菜养殖区分布面积分别为804.69 hm~2、6 097.95 hm~2、29 453.29 hm~2、42 316.98 hm~2,呈现逐年增加的变化趋势。(2)江苏近海紫菜养殖区主要分布在连云港海域以及盐城-南通交界海域。(3)基于2018年紫菜养殖区空间分布格局,在江苏近海的部分港口航运区和特殊利用区存在紫菜养殖的不合理用海行为。(4)连云港海域紫菜养殖扩张模式以密度增大的填充型为主,盐城-南通交界海域以密度增大的外延型为主。该研究可为相关海洋管理部门提供江苏近海紫菜养殖区空间分布和扩张模式的基础数据,也可为控制江苏近海紫菜养殖规模,优化海洋产业布局提供决策支持。 相似文献
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成长春 《海洋与海岸带开发》2012,(9):120-128
为了完成“坚持陆海统筹构建江苏海洋经济优势研究”的课题研究任务,课题组成员调查走访了江苏省及沿海3市与海洋经济有关的部门,获取了第一手的数据和信息,既为江苏海洋经济在“十一五”期间取得的快速发展而高兴,又为江苏海洋经济与兄弟省市存在的明显落差而着急。陆海兼备、滨江临海是江苏典型的地缘优势,也是江苏经济继续保持强劲发展的潜力和希望所在。放大地缘优势,统筹陆海,联动江海,是实现江苏经济社会又好又快发展的必由选择。 相似文献
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通过对不同海区浒苔及其与紫菜之间的比较,分析评价了江苏海区定生浒苔和漂浮浒苔的营养特性。通过主成分分析可以将江苏浒苔与其他浒苔和紫菜明显区分开,说明江苏浒苔的营养具有区域一致性。江苏浒苔具有高蛋白、低膳食纤维的特点,浒苔中钙、镁含量高于紫菜,磷含量低于紫菜。江苏浒苔的必需氨基酸含量组成适合人体需要,是良好的蛋白质来源。第一限制氨基酸为甲硫氨酸,呈味氨基酸含量达到氨基酸总量的33.6%—42.9%,具有较好的呈味特性。江苏浒苔的铅、铬离子含量较高,食用风险不容忽视。 相似文献
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为了完成"坚持陆海统筹构建江苏海洋经济优势研究"的课题研究任务,课题组成员调查走访了江苏省及沿海3市与海洋经济有关的部门,获取了第一手的数据和信息,既为江苏海洋经济在"十一五"期间取得的快速发展而高兴,又为江苏海洋经济与兄弟省市存在的明显落差而着急。陆海兼备、滨江临海是江苏典型的地缘优势,也是江苏经济继续保持强劲发展的潜力和希望所在。放大地缘优势,统筹陆海,联动江海,是实现江苏经济社会又好又快发展的必由选择。 相似文献
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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
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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
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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
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V. A. Ivanov S. P. Lyubartseva N. Mikhailova N. B. Shapiro 《Physical Oceanography》2001,11(6):509-524
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
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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
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Relationship between the path of the Kuroshio in the south of Japan and the path of the Kuroshio Extension in the east 总被引：2，自引：0，他引：2
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
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I. E. Timchenko A. A. Primalenny V. D. Yarin E. F. Vasechkina E. M. Igumnova 《Physical Oceanography》2001,11(4):367-378
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
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I. G. Ostrovskaya 《Physical Oceanography》1992,3(5):397-403
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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Al. A. Shreider 《Oceanology》2007,47(1):91-103
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
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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