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<中华人民共和国海域使用管理法>(以下简称<海域法>)颁布实施后,为了规范海域使用管理的行政行为,盐城市逐步建立海域使用管理的一系列配套制度,形成有效的约束和监督机制,使得全市海域使用管理工作有序、健康开展. 相似文献
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自1993年<国家海域使用管理暂行规定>颁布以来,我国海域物权制度经历了一个建立和不断完善的过程.<中华人民共和国海域使用管理法>和<中华人民共和国物权法>的施行,进一步确立了海域物权制度,从根本上扭转了海域使用中长期存在的"无序、无度、无偿"局面,有效地维护了国家海域所有权和海域使用权人合法权益.但是,由于认识的差异,在一些具体问题上还存在不同的观点.文章将着重对海域使用权与渔业、矿业、取水等相近权利的性质和相互之间的关系,及海域使用审批管理与其他涉海部门许可管理间的关系进行分析研究,以进一步统一认识. 相似文献
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<中华人民共和国海域使用管理法>的四项制度,既海域使用的功能控制制度、海域有偿使用制度、海域使用权属管理制度、海域审批制度,都是以海洋功能区划为科学基础和依据的.由于海洋开发明显滞后于土地的开发与管理,希望借鉴土地管理的理论和方法经验,加强海洋功能区划的研究和实施.同时建议加强海洋意识的宣传、珍惜海洋资源、健全海域登记制度. 相似文献
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为进一步落实<中华人民共和国海域使用管理法>,国家提出建立海域使用动态监视监测管理系统,以便及时掌握海域使用及其时空动态变化状况,有效使用海域资源,使其发挥最佳利用效益.介绍了海南海岸侵蚀的状况,分析了造成海岸侵蚀的原因,提出了切实落实国家海域动态监管方案和加强海岸侵蚀监控、促进海南海域使用管理的对策措施,对加强海南省海域使用管理工作有积极的意义. 相似文献
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海洋功能区划工作是国家海洋局组织开展的一项多层次、多学科的大型综合性的基础工作,也是<中华人民共和国海洋环境保护法>和<中华人民共和国海域使用管理法>规定的一项重要的基础性制度.重点讨论了海洋功能区划的概念和性质,并通过对海洋功能区划与其他规划之间关系的对比分析,提出了海洋功能区划未来的发展方向和趋势,为海洋功能区划的深入研究提供了很好的参考. 相似文献
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１９９３年，《国家海域使用管理暂行规定》的出台，拉开了我国海域使用管理法制化建设的序幕。２００１年１０月２７日，《中华人民共和国海域使用管理法》（以下简称《海域使用管理法》）的正式颁布，则成为我国海域使用管理工作正式步入法制化轨道的重要里程碑。欣喜之余，每个海洋管理工作者又不能不感觉到自己肩上的分量。《海域使用管理法》的出台，不应成为海域使用管理立法研究工作的终点，而应成为我们深化研究的新起点。继续做好海域使用管理立法研究工作，为尽早制定出和修订好相关海域使用管理配套法规做好理论准备，是海洋管理… 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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The methodology and the first results of the computations of the volumes, masses, and growth rates of the sedimentary body of the buried Black Sea basin are presented. Their temporal evolution reflects the regional paleogeodynamics, in particular, the reorientation of the vector of the relative movement of the Arabian and Eurasian lithospheric plates and the related intensification of their collision in the late Miocene-Pliocene. 相似文献
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E. L. Vinogradova 《Oceanology》2008,48(4):483-492
The spatiotemporal variability of the hydrochemical composition of the riverine runoff in nearmouth areas is presented using the example of selected rivers of the Arctic Basin. The temporal dynamics of the riverine nutrient runoff are mainly determined by the seasonal and interseasonal variations in the drainage basins. The spatial variations in the chemical composition of riverine waters in the near-mouth areas are mainly caused by the dynamics of the water flow and the river bed relief and, to a lesser degree, by biochemical processes. It is shown that the variations in the nutrient composition of the waters in near-mouth areas are comparable in magnitude to those at the river-sea geochemical barriers. 相似文献
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Izvestiya, Atmospheric and Oceanic Physics - Analysis of the temporal variations of the virtual heights of the sporadic E layer (h?ES) determined from ionograms with increased accuracy (1... 相似文献