国土空间规划下海岸带的功能定位及空间响应——以上海海岸带为例

海岸带规划作为国土空间规划体系中的唯一涉海规划,不仅要对海岸带地区进行陆海统筹综合管控,而且要对海岸带地区的发展进行战略功能引导,以适应海洋强国建设的蓝色发展要求。文章分析新一轮国土空间规划对海岸带规划的新要求,提出海岸带规划进行功能定位和空间响应的规划策略和方法;结合上海海岸带发展实际,从多维战略对接、区域功能耦合、未来发展趋势应对3个方面谋划海岸带功能定位,提出海岸带“三心二市”的功能内涵;在此基础上提出海岸带空间响应策略,主要包括对接国土空间分层逻辑、海洋功能区划和岸线区段功能耦合、开放式分圈层分区划分、落实核心功能诉求。     

基于陆海统筹的海岸带空间功能分区——以宁波市为例

海岸带空间功能分区是优化海岸带开发与保护的基础性工作,在国土空间规划体系中具有重要作用。当前我国海陆功能分区在分区层级、分区方法等方面并不一致,导致海岸带保护与开发利用失衡。本文在梳理国内外海岸带空间功能分区研究的基础上,从陆海统筹角度出发,构建海岸带空间功能分区体系,并以宁波市为例进行验证,在优先划定生态保护区基础上,对海陆空间进行适宜性评价,根据评价结果确定功能分区。结果表明：（1）宁波市海岸带功能区中生态保护区面积占比约为60%,海陆一体发展区占比约为22.3%,海洋发展区占比约为12.5%,陆地发展区占比约为5.2%;(2)宁波市开发利用功能区空间分布与以临港产业、海洋服务业和海洋渔业为基础的海洋经济发展导向相符。海岸带空间功能分区要以生态保护为底线,以优化空间布局为导向,为优化海岸带开发与保护提供有力支撑。     

市县级海洋国土空间规划技术体系探索与编制实践——以广西壮族自治区北海市为例

为推动海陆一体国土空间规划体系的形成,本文以自然资源部"两空间内部一红线"海洋空间开发与保护格局总体要求为指导,以基于生态系统管理、陆海统筹为基本原则,从格局目标确定、格局分区探索、陆海统筹对策等几个方面进行了深入研究,形成了较为完善的市县级海洋国土空间规划技术体系,并以广西北海市海洋国土空间规划编制为例进行了应用示范。研究结果表明:该技术体系实现了北海市海洋空间资源的合理配置,形成了生态优先的空间发展格局和综合管控体系,可为市县级海洋国土空间规划的编制提供重要参考。     

基于陆海统筹的我国海岸带空间规划指标体系研究

2018年自然资源部提出建立国土空间规划体系,之后涵盖海陆两个国土区域的统一的规划研究愈加被重视。海岸带作为陆地与海洋的交汇地带,具有鲜明性和独特性,为实现海岸带地区的协调及可持续发展,对海岸带地区进行空间规划显得颇为重要。本文在梳理国内外海岸带空间规划及其指标体系研究现状的基础上,分析了我国海岸带空间规划存在的问题,进而采用频度分析法构建了基于陆海统筹的包含3个一级指标和30个二级指标的我国海岸带空间规划指标体系,以期为新时期海岸带空间规划乃至国土空间规划编制工作提供借鉴。     

基于陆海统筹的海岸带"三生空间"分区体系研究

随着经济社会的快速发展,海岸带区域生产、生活等活动逐渐增多,开发程度不断提高,给海岸带区域的各种资源和环境造成极大压力。党的“十八大”以来,将优化国土空间开发格局作为生态文明建设的首要举措,对国土空间开发利用保护提出新要求。在此基础上,文章从海陆统筹的角度按照《国民经济行业分类》和《海洋及相关产业分类》,根据系统性、复合性、兼顾性、前瞻性4个原则,提出了一套包括3个大类、9个二级类、33个三级类的海岸带空间分类体系,并且与土地利用现状分类及海域使用分类进行了较好的衔接,以期为有关规划提供参考借鉴。     

韩国《海洋空间规划与管理法》概况及对我国的启示

海洋空间规划作为重要的海洋空间管理工具,其重要性日益凸显。韩国为科学管理有限的海洋空间资源,合理协调用海空间矛盾,有效保护海洋生态环境,于2018年4月17日颁布《韩国海洋空间规划与管理法》。该法从早期海岸带空间管理扩大到全部管辖海域,从海洋空间资源的无序开发到海域整体性开发,统筹兼顾、突出海域核心价值,推动海洋的可持续利用。文章在梳理韩国海洋空间规划发展沿革的基础上,全面解析了《韩国海洋空间规划与管理法》的内容,包括其空间规划的分类、内容、范围、期限、原则、区域划分等,分析了中韩两国海洋空间规划在多方面的异同,在此基础上得出其对完善中国海洋空间规划制度的启示。     

基于生态系统的挪威海海洋环境综合管理计划

为推动我国国土空间规划新视角下的海洋空间规划实践,提升我国海洋综合管理水平,文章概述基于生态系统的挪威海海洋环境综合管理计划的主要内容,并重点分析挪威海的海洋环境空间管理措施。研究结果表明:挪威海海洋环境综合管理计划是基于生态系统的海洋空间规划,建立在良好的海洋环境状况和海洋生物多样性与其栖息地的保护基础之上,以可持续利用海洋资源来实现海洋产业的价值创造与生态系统服务供给;该管理计划制定一系列海洋环境保护措施和人类活动空间管理措施,以实现挪威海海洋环境的有效保护和海洋经济产业的有效管理;挪威海海洋空间规划的发展可为我国国土空间规划涉海内容的编制、海洋资源的可持续利用与海洋产业的快速健康发展提供重要参考。     

基于多维影响机制的海岸带退缩线分级分类评估及管控研究——以东营市为例

海岸带退缩线是海岸带国土空间规划工作的重要部分,平衡沿海城市资源利用与生态保护需求,保障沿海地区健康可持续化发展的安全底线。目前我国海岸带退缩线缺乏系统的评估和管控体系,文章通过梳理社会经济价值、空间发展潜力、景观风貌风险、海洋灾害风险、生态环境价值5个影响维度与海岸带各类要素的关联机制,建立了陆海统筹的滨海地区海岸带退缩线重要程度的评估体系,总结我国海岸带退缩线分级分类差异化管控策略,并以东营市为例,进一步探讨了该评估体系在退缩线划定和管控层面的应用,以期为海岸带国土空间规划的管控提供参考。     

浙江省近岸海域环境功能区管理现状、问题及对策研究

浙江省近岸海域环境功能区划在保护海域生态环境和调整海域资源开发利用等方面发挥着重要作用,已成为近岸海域环境监管的重要依据。然而在当前进一步优化国土空间规划和海洋经济高质量发展的新形势下,区划内容已明显滞后。文章梳理历年浙江省近岸海域环境功能区划编制、调整和监测的工作经验,研究管理过程中存在的主要问题,并在此基础上提出坚持生态优先底线约束原则、有序衔接浙江省国土空间规划、科学合理制订分类分区管控措施、有机融合涉海专项规划保护目标、基于陆海统筹合理认定管理边界等对策措施,以期为浙江省近岸海域环境功能区管理提供参考。     

柬埔寨海洋空间用途管控研究

用途管控是海洋空间规划的核心内容,也是海洋空间规划实施的重要工具。文章构建了以人类活动为基础的《柬埔寨海洋空间规划（2018-2023年）》功能区用途管控清单。首先,综合分析柬埔寨海洋与海岸带发展战略、资源环境条件、开发利用现状、用海需求和未来发展趋势,确定柬埔寨现有及潜在用海活动总清单;其次,根据各海洋功能区主导功能、兼容功能及管理要求确定主导性、兼容性和禁止性用海活动;再次,结合用海活动目的、对资源消耗和环境影响程度设置准入条件,形成各功能区的用途管控清单,以实现对柬埔寨海洋空间用途的有效管控。     

Model of the post-Cenozoic evolution of the cryolithozone of the shelf of the western part of the Laptev Sea

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.     

Investigation of the mechanism of the long-term evolution of the carbon cycle in the ecosystem of the Sevastopol bay

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.     

Contemporary state of the investigation of the influence of the discharge of rivers on the hydrologic structure of the Black Sea

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     

Modelling of the ecosystem of the Black-Sea shelf zone near the estuary of the Danube

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     

Dynamics of the ice cover and peculiarities of the ice transportation of the sediments at the tidal flats of the Kandalaksha Gulf of the White Sea

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.     

Relationship between the path of the Kuroshio in the south of Japan and the path of the Kuroshio Extension in the east

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.     

Variability of the nutrient runoff of the rivers of the Arctic Basin

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.     

Parameters of the sediments of the deep-water basin of the Black Sea

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.     

Modelling of the ecosystem on the shelf of the Republic of Guinea

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.     

Evolution of the slope of the buried depression of the Black Sea

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.