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文章从马克思地租理论的角度,阐述海域资源绝对地租、级差地租及其价格表现形式,探讨江苏省省管海域--江苏省"两沙"海域资源有偿使用的科学实施. 相似文献
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近年来,随着国家资源管理体制改革的加快,海域资源市场化配置程度不断提高,海域招拍挂即将成为海域使用权出让的主要方式。对海域基准价格进行研究,可以科学确定海域使用权的价格,为海域资源市场化配置提供科学支撑。本文建立了海域定级和海域基准价格评估方法,并利用建立的方法评估了厦门市货运港口用海、客运港口用海、游乐场用海和游艇泊位用海的海域基准价格。结果显示,厦门市各级各类海域基准价格差异很大,各地区各类用海的海域基准价格在11.04～89.32万元/公顷之间。从区域看,同一区域不同用海类型的海域基准价格相差很大,厦门岛周边海域基准价格普遍较高,与陆域的经济发展水平相对一致;从用途看,同级别海域游艇泊位用海年均海域基准价格最高,货运港口用海最低。 相似文献
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随着国家全面推进海域资源市场化配置,海域招拍挂将成为海域使用权出让的重要形式,海域使用权价格评估是其基础性工作。文章设计建设填海造地用海一级市场海域使用权价格评估案例,利用不同评估方法对海域使用权价格进行评估,最后基于评估过程和结果对各评估方法的适用性进行分析。结果显示:假设开发法理论成熟,能很好地体现海域使用权价格的内涵,可作为海域使用权价格评估工作中最优选择的方法;成本法无法体现海域自然属性和其他影响因素对海域使用权价格的影响,且待评估海域往往为裸海,尚未有实际成本发生,因此并不适用于海域一级市场评估;成本法不适用的根源在于其忽略海域增值收益,亟须在原有计算公式的基础上增加海域增值收益。 相似文献
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海域资源作为我国资源的重要组成部分,其科学的开发利用与合理计价对于我国经济发展有着至关重要的作用。自十八大提出"五位一体"和谐社会总构想以来,对于海域资源的价值又有了更深层次的理解,对其科学的计价方式也有了新的要求。海域基准价格作为海域使用与交易过程中的指导价格,在市场运行与开发过程中处于指导地位,科学地评估海域基准价格具有至关重要的意义。海域基准价格动态计量方法是考虑了时间因素、经济因素、社会因素等相关因素的价格计量方法,是一种较以往进步的、科学的计量方法。正确分析海域动态基准价格的界定与构成是正确计量海域动态基准价格的基础。 相似文献
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通过开展海域资源现状调查,摸清海域资源禀赋基本情况,进行海域资源资产核算,建立实物账户和价值账户,是海域分等定级和价格评估的基础,是健全自然资源资产产权制度、保障海域使用金应收尽收、实现海域国有资源性资产保值增值、履行国家海域资源资产所有者职责的必要条件。文章针对我国现有海域资源调查核算不能满足海域有偿使用管理需要的具体问题,提出3点建议,包括:开展海域空间资源调查,建立资源实物账户;开展资源价值评估,建立海域资源价值账户;构建海域资源资产-价值核算体系。 相似文献
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随着国家资源管理体制改革的加快,海域资源的市场化配置程度不断提高,而海域使用权价格评估是其基础工作。在诸多评估方法中,假设开发法把在开发和未开发海域假设为已完工状态而进行评估,非常适宜于当前海域市场化出让前的状态,已经成为目前海域使用权评估领域最常用的评估方法。文章选取A市游艇码头项目用海为例,利用假设开发法详细测算了该宗海域价格,并通过对测算过程和测算结果进行分析,探讨假设开发法在海域价格评估领域的应用及局限,对进一步完善海域使用权价格评估工作具有积极意义。 相似文献
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随着我国海域有偿使用制度的推行,海域资源从无偿使用逐步走上有偿使用的轨道,海域资源配置逐渐向市场机制过渡,海域价格评估方法的探讨成为当前海域研究的热点.文章在海域价格形成机制的基础上,从本质上分析得出我国海域价格的构成,对于进一步探讨海域价格的评估方法具有十分重要的意义. 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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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
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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