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1.
区域是人类经济活动所占据的空间范围,它具有明显的要素禀赋、经济活动、范围大小等特征。区域空间结构是指各种经济活动在区域内的空间分布状态及空间组合形式。在区域经济发展中,要始终考虑如何实现要素的空间优化配置和经济活动在空间上的合理组合,从而克服空间距离对经济活 相似文献
2.
沿海县域经济发展比较研究 总被引：1，自引：0，他引：1
县域经济是国民经济的基本单元,随着我国城市经济集聚、人口膨胀,县区成为实现经济、人口转移的重要空间,县域经济的发展成为社会经济增长的新领域.县域经济的发展差别主要体现为竞争力的差别,即县域进行资源配置来获得竞争优势的能力,这可以通过各沿海县域产业结构的相似性系数来体现. 相似文献
3.
谭晓岚 《海洋与海岸带开发》2012,(1):144-147
产业转型升级是否成功的影响因素和矛盾很多,在推动日照经济产业升级的同时,照顾到各相关方的利益,使产业升级可能导致的负面影响最小化,是产业升级中必须要解决好的问题。日照经济转型升级成功与否,日照地方政府和日照地方经济体是两股起到决定性的作用力量,只有两者全面有效结合,双方互动,日照经济的转型升级才可能有效地实现。日照地方政府要利用山东半岛蓝色战略经济区建设的有利时机,从不同途径争取到资源和政策,为地方企业提供激发其加快产业转型升级的动力,是工作的关键。 相似文献
4.
低碳城市(Low-carbon City),指以低碳经济为发展模式及方向、市民以低碳生活为理念和行为特征、政府公务管理层以低碳社会为建设标本和蓝图的城市。低碳城市是一个综合体系,主要包括低碳经济、低碳建筑、低碳交通、低碳生活、低碳环境、低碳社会等。目前,占地球面积2%的城市制造了一半以上的温室气体,汽车尾气已经成为许多城市碳排放量的主要来源之一。因此,"低碳城市"的理念应该融入到生产、生活各领域,如在城市各个建筑采用太阳能照明、太阳能热水系统、地源热泵、水源热泵、以及垃圾填埋场的填埋气体回收利用等技术;市民也践行节约能源、环保的低碳生活。气候组织的报告认为,在以"低排放、高能效、高效率"为特征的"低碳城市"中,低碳经济不会放慢经济增长,反而会促进经济的新一轮高增长,并增加就业机会,改善生活水平。现在就让我们来看一下究竟有哪些城市已经离"低碳"更近一步? 相似文献
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6.
我国海洋管理中的协调机制探析 总被引：2，自引：0，他引：2
由于海洋管理客体的特殊性,以及海洋管理中各涉海主体矛盾的不断增多,协调问题日益受到重视,建立协调机制也就成为迫切的需求.海洋管理协调机制主要处理的关系有:各涉海行业间的关系、涉海的中央与地方政府间的关系、海洋综合管理部门与各涉海行业间的关系以及海洋管理部门与企业、公众的关系.从政府的角度看,健全组织机构和促进制度化建设,是建立健全海洋管理协调机制的前提和基础. 相似文献
7.
文章以中国沿海11个省、市、自治区包含的47个国家级经济技术开发区及其所在的36个城市有关数据资料为基础,从空间经济效益、空间经济增长力、空间财政回馈度、空间经济外向度等多个方面,就经济技术开发区对我国沿海城市空间效益的影响作用进行了综合评估分析;并运用系统聚类方法和纳尔逊分类法将经济技术开发区对沿海城市空间效益的影响贡献及作用模式分为高水平高效益型、空间经济外向度主导高水平型、空间财政回馈主导高水平型、相对均衡型和极度不均衡型5种类型,并指出了各类型所对应的城市组群。 相似文献
8.
海岛经济体脆弱性是指在海岛经济体发展过程中,资源、社会、经济和生态环境等方面呈现出不同程度的可持续发展能力的损坏。从时间序列的视角对海岛经济体脆弱性动态演变过程及发生机理进行研究是针对性提出海岛脆弱性治理的重要途径。作者以舟山市为例,从资源-生态环境-经济-社会综合研究视角,采用综合指数法对1996—2016年舟山市脆弱性动态演变特征进行分析。研究表明:1996—2016年,舟山市资源脆弱性、经济脆弱性、社会脆弱性总体呈下降趋势,生态环境脆弱性"先升后降再升",呈周期性变化;由各子系统对综合脆弱性的影响程度来看,综合脆弱性由生态环境脆弱性和社会脆弱性主导向各子系统均衡影响转变;舟山市脆弱性发展演变过程是自然资源条件、经济发展方式、政府宏观调控相互影响、相互制约的结果,并依据其驱动机制提出相应的应对措施。 相似文献
9.
文章以大连为例,探讨了全域城市化过程中游憩系统的概念模型,尝试构建了大连核心城区游憩系统空间结构模型：即市区开敞空间 （日游憩中心）—城市边缘游憩中心—城市近郊游憩中心—城市远郊游憩中心—多个中心的互补和融合,最终形成无疆界游憩空间系统。文章对于城市游憩规划具有参考指导意义,并对未来城市化的游憩系统的建立提出了发展规划思路。 相似文献
10.
随着人均GDP的增长,滨海温泉旅游逐渐被大众接受并喜爱。滨海温泉旅游以温泉养生为主题,是一种新兴的休闲度假旅游方式。目前,我国对滨海温泉旅游地的空间结构研究较少,但滨海温泉旅游地的空间演化、发展趋势对于蓬勃发展的海洋旅游和温泉旅游意义重大。鉴于此,文章尝试运用人文地理学中的文化扩散理论解释滨海温泉旅游地空间结构的形成和演化,并选取营口鲅鱼圈为例进行说明。从温泉小镇内部、温泉小镇之间、温泉与滨海其他旅游形式、温泉旅游地与周边旅游地4个方面探讨鲅鱼圈温泉旅游地空间演化形式,在此基础上,尝试总结滨海温泉旅游地空间结构演化机制。 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.
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
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.
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
17.
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
18.
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
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.
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