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1.
通过对海岸自然条件、海岸利用现状和项目用海需求等三项专题分析研究,确定海岸基本功能、明确海岸开发利用方向和管理保护措施,达到建立以海岸基本功能管制为核心的管理机制,进一步落实海洋功能区划,规范海岸开发秩序,调控海岸开发的规模和强度。在尽量满足海洋经济发展需要的同时,最大限度地提高海洋资源的利用价值,减少海岸资源浪费,保护海洋生态环境和海岸资源,推动广东省沿海地区社会、经济和环境的和谐发展。  相似文献   

2.
文章基于"多规合一"的视角,从概念内涵、规划体系、区别联系等方面,对比分析了海洋功能区划与土地利用总体规划的差异性和关联性。重点分析两者在功能定位、时间定位、层级体系、分类体系、评价制度等方面的差异,研究海洋功能区划需完善之处,并提出完善海洋功能区划期限及目标的设置、明确不同层级的细化标准和要求、增加海洋保护、生态环境整治修复类等功能区类型、加强海洋功能区划实施情况评估制度的建设等对策和建议,为实现海洋功能区划在"多规合一"进程中与土地利用规划等其他规划统筹衔接提供研究基础。  相似文献   

3.
海洋功能区划实施评估是监督海洋功能区划实施成效,提升海洋管理水平的重要工具。基于一致性理念,以规划蓝图为依据,从海域用途符合性、环境质量标准符合性、开发利用影响三方面集成构建海域利用现状和海洋功能区划的协调性判别方法即海洋功能区划协调性指数,并以温州市为实例进行验证。研究表明:基于一致性理念与海洋功能区划蓝图构建的评估方法可以有效测度海洋功能区划实施成效。海洋功能区划修订具有显著适应性,能够高效契合区域海洋经济与海洋生态文明建设需求。该方法对未来国土空间规划海洋部分的有效实施和修订具有重要参考价值。  相似文献   

4.
海洋功能区划制度是我国海洋综合行政管理的一项制度和法律,对我国海洋保护、使用和管理起到了十分重要的作用,对我国海洋的可持续发展具有重大的历史意义,对世界海洋管理理论也是一重大贡献.但是,海洋功能区划的体系和理论还不完善.文章对海洋功能区划的理论、实践和思想的矛盾做了初步探讨,对管理范围、海洋功能、海域区划、社会需求、社会发展和应用等方面的矛盾做了分析,对海洋功能区划的变革做了初步讨论.  相似文献   

5.
《海洋开发与管理》2011,28(2):46-49
记者:2010年河北省海洋经济发展势头良好.首先请您从宏观角度介绍一下2010年河北省海洋局在布局规划、行政服务方面保障海洋经济发展的主要工作成果. 王保民:2010年,河北省委、省政府进一步加快滑海开放战略的实施,海洋经济的发展进入新阶段,海洋工作服务经济建设取得新进展.一是科学谋划海洋产业布局,加快完善海洋规划体系."海洋功能区划"和"海岸保护与利用规划"是强化海域管理、统筹产业发展、实施资源配置、协调和促进海洋经济健康发展的重要依据,是管理工作的重中之重.  相似文献   

6.
天津海洋功能区划是国家海洋局和天津市科委于1989年7月相继下达的“渤海区海洋功能区划”的一部分。根据“渤海区功能区划大纲”和“渤海区功能区划简明技术规定”的要求,区划工作自1989年8月开始,历时5个月,于1989年12月底全部结束。天津海洋功能区划工作由天津市海岸带综合调查领导小组领导,由市海岸办组织天津海岸带开发咨询服务公司、海洋情报所等8个有关部门共同承担。为加强对区划工作  相似文献   

7.
为提高我国海洋空间规划和海域使用管理水平,文章以国土空间为视角,分析海洋功能区划融入"多规合一"的必要性、可行性和路径。研究结果表明:"多规合一"是基于对国土空间的统一分区和用途管制,对现有规划体系的有机融合、升级和重构;海洋功能区划是我国法律确定的海洋管理基本制度,在实现用海有度、有序和有规,保护海洋生态环境,促进海洋经济发展以及保障养殖用海空间等方面发挥重要作用;海洋功能区划的实施具有法律依据,其"综合分区+目标管控+用途管制"的核心理念与"多规合一"一致,分区分类方式有利于现有规划体系的衔接,在保护性、前瞻性和陆海统筹等方面的不足亟须在"多规合一"的过程中改进;"多规合一"可参考海洋功能区划实施的经验和教训,制定"一个规划"和"一套标准"。  相似文献   

8.
根据国务院总理温家宝关于“国家海洋局要把工作重点放在规划、立法和管理上”的重要批示,国家组织力量先后进行了《全国海洋功能区划》和《全国海洋经济发展规划纲要》的制定工作。2002年8月22日,国务院批准了《全国海洋功能区划》。同年9月4日,经国务院同意,由国家海洋局发布了《全国海洋功能区划》。2003年5月9日,国务院批准了由国家发展和改革委员会、国土资源部和国家海洋局组织制定的《全国海洋经济发展规划纲要》。《全国海洋功能区划》和《全国海洋经济发展规划纲要》的颁布,是我国海洋事业发展里程碑的两件大事,具有重大的现实意义…  相似文献   

9.
海洋功能区划控制体系研究   总被引:2,自引:0,他引:2  
王江涛  刘百桥 《海洋通报》2011,30(4):371-376
合理利用海域、改善海洋环境质量和降低海洋开发利用活动负外部性,都需要通过加强海洋开发利用活动的控制来实现,而海洋功能区划是控制和管理开发利用活动的重要手段和工具。从文本控制、图则控制、指标控制、海域使用全过程控制四个方面构建了海洋功能区划控制体系,其中文本控制由目标、原则和文本条款组成;图则控制由图则边界、用海类型和管理要求组成;指标控制由规模控制、结构控制、利用方式控制、海域使用强度和效率控制、环境控制指标构成;海域使用全过程控制由建设期、运行期和结束后构成。通过构建海洋功能区划控制体系,有助于区划目标  相似文献   

10.
随着辽宁沿海经济带新型城镇化、工业化、农业现代化以及城市智慧化的不断发展,城乡规划、土地利用总体规划、林业保护规划、海洋功能区划等专项规划对同一区域土地安排的矛盾和冲突越来越明显,影响了经济社会的协调、稳定发展。为此,文章研究了城乡规划、土地利用总体规划、林业保护规划、海洋功能区划等多规冲突测度的技术方法,探讨了"1+X"的多规融合路径,并以大连庄河为例进行实证分析。为辽宁沿海经济带乃至全国沿海地区实现土地资源区域统筹协调利用提供技术依据和借鉴。  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.
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   

17.
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   

18.
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.
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   

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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