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1.
海域使用权在《中华人民共和国物权法》（以下简称《物权法》）中被列入用益物权,与土地使用权具有同等的法律权利。长期以来,由于对海域使用权法律地位和作用的认识不足,不仅导致了在《海域使用权证书》确定范围上的建（构）筑物领不到房屋产权权属证书,也导致了这部分建（构）筑物的建设工程管理缺位,存在着很大的安全隐患和无序无度建设及建设配套费流失等现象。 相似文献
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一、概说 2007年3月颁布的<物权法>第46条规定:"矿藏、水流、海域属于国家所有."这一规定,是在2001年颁布的<海域使用管理法>首次宣布海域归国家所有的基础上,对海域之国家专属所有权的重申.而<物权法>在其关于用益物权一般规定一章(第十章)中,单条规定"依法取得的海域使用权受法律保护."(第122条),同时,单条还规定"依法取得的探矿权、采矿权、取水权和使用水域、滩涂从事养殖、捕捞的权利受法律保护."(第123条). 相似文献
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《中华人民共和国物权法》规定海域使用权为用益物权,为完善海域使用权物权制度奠定了法律基础。推进海域使用权抵押贷款,是从制度上落实海域使用权物权属性的一个重要方面。 相似文献
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2006年10月13日,国家海洋局印发了《海域使用权管理规定》和《海域使用权登记办法》,这两个规定是《中华人民共和国海域使用管理法》(以下简称《海域法》)的重要配套制度,进一步完善和明确了海域使用权的设定、变更和登记等重要制度。但由于各种原因,海域使用权收回制度仍未在这两个规范性文件中得到具体的规定。海域使用权收回制度建设,将是今后落实《海域法》、加强海域使用管理、维护海域使用权人的合法权益的重要任务之一。本文拟对建立我国海域使用权收回制度中的几个主要法律问题进行初步探讨,希望对这项工作有所裨益。 相似文献
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“失海”渔民的权益缺失与法律救济 总被引：1，自引：0，他引：1
"失海"渔民作为新弱势群体,其基本权利渔业权存在制度上的缺失,并与海域使用权在权利设置上存在冲突,进而造成了救济的困难,因此从立法上国家应完善渔业权制度,制定渔民特别权益保护法,从程序上加强"失海"渔民权益的法律救济。 相似文献
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《中华人民共和国海域使用管理法》和《物权法》确立了海域使用权的物权性质，因此海域使用权具有一般物权的效力。同时海域使用权作为一种新型的用益物权．其效力又有特殊之处。从物权角度来说．海域使用权的效力基础是海域使用权的用益物权性质．而其效力内容包括海域使用权的优先效力、排他效力和妨害排除效力。通过对海域使用权效力的理解和分析，海域使用法律制度可以从突出海域使用权的物权性、建立海域区分使用制度和加强海域使用权宏观保护等三方面加以完善。 相似文献
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一、关于海域使用权登记制度１．海域使用权登记制度是由海域使用权的性质决定的海域使用权具有物权的性质。我国“民法通则”，“土地管理法”，“矿产资源法”，“水法”等，承认国有土地和资源所有权与使用权的分离，规定了组织和个人可依法取得国有土地使用权、或采矿权、或取水权等。法学专家将对国有自然资源的使用权归为用益物权。改革开放以来，我国海域使用的种类和规模不断扩大，对海域空间资源使用权的取得越来越迫切。如港池、养殖、围海、油气开发、海上娱乐场等海域使用权，是从海域国家所有权中分离出来的一种排他性权利。海… 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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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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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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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
19.
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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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