辽宁沿海经济带空间演变与城市化响应机制研究     

王亚丰 《地域研究与开发》2011,30(3)

城市是区域发展的核心,城市化是区域发展过程中的一种重要运动形式.近百年来,辽宁沿海地区逐渐完成带状空间格局演变,但由于各种原因,这一地区内部城市化进程不均衡,城市等级体系不完善,城市化滞后工业化,城市基础设施不健全.通过实际考察分析,从城市化响应视角探究辽宁沿海经济带的经济复兴和区域发展,提出中心城市化辐射带动、城市体系重构、区域空间结构优化、城市生态空间构建4种适合辽宁沿海经济带内城市化发展的响应机制.  相似文献   

辽宁沿海经济带产业结构分析   总被引：1，自引：0，他引：1  

关伟  蔚振杰 《地域研究与开发》2011,30(4)

辽宁沿海经济带开发开放上升为国家战略之后不仅使其成为全省经济总量扩张承载的重要区域,而且还肩负着辽宁转变经济发展方式、加大产业结构调整的重要使命。在应用三轴图法研究辽宁沿海经济带产业结构的变化及其轨迹的基础上,利用SSM模型及其计算公式对辽宁沿海经济带产业结构进行比较分析,认为营口、丹东、锦州等城市的第一产业竞争力较强,其第二产业的发展水平都较高,尤以大连、营口两市为突出,锦州、营口两市的第三产业发展速度较快。依据分析结果并结合辽宁十二五经济社会发展战略,提出辽宁沿海经济带加快转变经济发展方式、加大产业结构调整的对策建议。  相似文献   

The research of sea-land breeze (SLB) on the west coast of Bohai Bay based on field observation     

Wei Gu  LaiYin Zhu  WeiJia Cui  Ning Li  JianOu Cong  YingJun Xu  ShuQing Huang  HaiYang Yu  LanTao Li 《寒旱区科学》2011,3(3):0264-0273

Four automatic meteorological stations were set up in a line from beach to inland perpendicular to the west coast of Bohai Bay. Wind direction and velocity at altitudes of 2 m, 4 m and 12 m were surveyed with 10 minute intervals. On "Sea-Land Breeze" (SLB) days, the transition from sea breeze to land breeze was very evident in the study area. Direction of sea breeze was basically perpendicular to the coast and mainly from the ENE and E. Duration of sea breeze varied by the stations’ distance to the coastline, and the near-coast wind velocity was larger than that of the inland and decreases as it reaches inland. There was increased development of SLB on sunny days than on overcast days. The term "Climatic Coastal Zone" can be defined for the area influenced by SLB, which reaches more than 74 km inland on a typical SLB day but less than 10 km on a non-typical SLB day.  相似文献   

滨海断裂带珠江口段的重磁资料解释   总被引：1，自引：0，他引：1  

任镇寰  孙崇赤  黄剑涛  廖桂金  刘天佑  乔计花  魏伟  刘大为 《海洋地质与第四纪地质》2008,28(3)

通过重磁资料系统处理、研究、解释,确认滨海断裂带珠江口段的存在,且是一条规模巨大特征明显的断裂带,深度在30 km以上,呈NEE向展布,是由滨岸断裂带和滨海断裂带界限的高重力地质块体带,重力、航磁梯度带或灰度带图像反映清楚。在浅部,它与NW和NE向断裂互有切割,不过,NW向断裂切割滨海断裂带和NE向断裂带的频度更高,图像更清晰。在10 km以深,NE、NW向断裂基本上消失,阻截在滨海断裂带内,某些资料认为,NE向莲花山断裂带往西南入海(本区)转为NEE走向,从重磁资料分析,这些NEE走向断裂其实是滨海断裂带的一部分。莲花山断裂带进入本区后,仍以NE45°左右方向,经深圳、香港,至万山群岛被滨海断裂带截断,图像清楚,不存在NE向转NEE向现象。滨海断裂带是一条活动性较强的断裂带,在珠江口段,强势不改,它与NW、NE向断裂交汇并相互切割,具备5级以上地震构造条件,尤其是与形成时代新、活动性较强的NW向断裂交切部位(如镇海湾、广海湾、崖门、澳门、担杆列岛地区)。但是,NW向断裂在本区较浅,不如粤闽、粤桂交界地区深(≥30 km),所以本研究区(段)地震强度应低于后者。  相似文献   

RECENT TRENDS OF TEMPERATURE AND PRECIPITATION DISTURBED BY LARGE-SCALE RECLAMATION IN THE SANGJIANG PLAIN OF CHINA   总被引：2，自引：0，他引：2  

YANMin-hua DENGWei CHENPan-qint 《中国地理科学(英文版)》2003,13(4):317-321

The regional observed temperature and precipitation changes and their abrupt jumps disturbed by large-scale reclamation in the Sanjiang Plain, Northeast China were studied. Mean annual temperature of the region was tending to go up and has increased by 1.2-2.2℃ over the past 50 years. A warming jump of mean annual temperature of the region occurred in the 1980s, which had an increase amplitude of 0.9℃. Linear tendency rates of annual precipitation were negative in most of the region. The maximum of annual precipitation decrease was 155.8mm over the past 50 years. An abrupt decrease of regional annual precipitation happened in the middle of the 1960s,which had a decrease of 102.1 mm. Based on the fact of climatic change of the Sanjiang plain over the past 50 years,it is held that the region had larger warming amplitude than that change of the Sanjiang Plain over the past 50 years,it is held that the region had larger warning amplitude than that of the surrounding areas in the recent years, which resulted from the large-scale reclamation of various kinds of wetlands.  相似文献   

A two‐dimensional analytical solution for groundwater flow in a leaky confined aquifer system near open tidal water     

Zhonghua Tang  Jiu J. Jiao 《水文研究》2001,15(4):573-585

Groundwater in coastal areas is commonly disturbed by tidal fluctuations. A two‐dimensional analytical solution is derived to describe the groundwater fluctuation in a leaky confined aquifer system near open tidal water under the assumption that the groundwater head in the confined aquifer fluctuates in response to sea tide whereas that of the overlying unconfined aquifer remains constant. The analytical solution presented here is an extension of the solution by Sun for two‐dimensional groundwater flow in a confined aquifer and the solution by Jiao and Tang for one‐dimensional groundwater flow in a leaky confined aquifer. The analytical solution is compared with a two‐dimensional finite difference solution. On the basis of the analytical solution, the groundwater head distribution in a leaky confined aquifer in response to tidal boundaries is examined and the influence of leakage on groundwater fluctuation is discussed. Copyright © 2001 John Wiley & Sons, Ltd.  相似文献   

Surface current patterns in front of the Venice Lagoon     

Miroslav Gačić  Vedrana Kovačević  Simone Cosoli  Andrea Mazzoldi  Jeffrey D. Paduan  Isaac Mancero-Mosquera  Sadegh Yari 《Estuarine, Coastal and Shelf Science》2009

Surface patterns of the low-frequency current in a 20 × 30 km region in front of the Venice Lagoon were analysed from a 13-month-long HF radar data set. Surface circulation was related to prevalent wind regimes in the area and to the tidal flow through the lagoon inlet. Three different categories of wind-forcing were defined: bora (NE wind), sirocco (SE wind), and finally the category containing all other wind directions and calms (winds lower than 3 m/sec). Mean flow and vorticity spatial distributions were discussed for different wind conditions. The coastal area about 5 km wide is characterized by a flow field with maximum vorticity. Outside the coastal boundary layer the interior flow is part of the Adriatic basin-wide cyclonic circulation. Two counter-rotating vortices of the dimension of about 4–5 km were evidenced in the average flow field in front of the lagoon inlet (Malamocco inlet) in all situations except for the bora. The vortex-pair is probably associated with the tidal flow through the inlet. The bora wind induces a strong southward coastal jet detached from the coast by about 5 km homogenizing the flow and eliminating the dipole. The average coastal flow pattern in calm wind conditions was also analysed as a function of the strong inflow/outflow (currents in the inlet > 0.7 m s⁻¹) from the lagoon inlet. In both cases the vorticity pattern is similar, with the negative vorticity to the left of the inlet and positive to the right looking seaward.  相似文献   

RIVERINE SEDIMENTS AND CHINESE COASTLINE CHANGES     

李从先  张桂甲 《中国地理科学(英文版)》1997,7(3):201-207

I.TI~IC~~RIWiRIrmssoITheupliftingoftheQiughal--Xoing(Tibet)PIateaugeneratedlargeandsediment--ladenrivers,thusthenorthernindianOceanandthewesternPacificOceanreceivedlargevolumeofriverinesedimentswhichconstituteabbothalfofthetotalbinesedimentsintheworld.ChineseoutlinecrossesbobtectonicupliftbeltsandtectonicdepressionbeltS.RiverssuchastheHuanghe(Yellow)myerandChangjiang(Yangtze)caver,etc.~nglargevolumeofSedimentsadnlyrunintOtheseaatthetectonicdepreSSionbelts,andriverssuchastheZhujiang(…  相似文献   

Sustainable development and coastal management of tidal flat in Jiangsu Province, China     

Huang Qiaohua  Chen Fang  Zhu Dakui 《中国地理科学(英文版)》1997,8(1):33-43

With huge area, favorable light, heat and water conditions, rich biological diversity, and a unique ecological system of submarine sand ridges, Jiangsu tidal flat has great significance to its economic development. Based on the geomorphological characteristics, Jiangsu tidal flat is dynamically divided into stable, erosional and accumulative types. In light of resources distribution, evolution rules of Jiangsu tidal flat, existing problems in coastal management, exploitation and utilization, the sustainable development theory is applied to guide the comprehensive exploitation and utilization of tidal flat. Taking different regions with different local conditions in consideration, and in order to make economic development coordinate with local resources and environments, four regional sustainable development models, i.e. (A) Abandoned Huanghe (Yellow) River delta section for salt and aquatic products industries, (B) Sheyang section for reed, aquaculture and rare animal protection, (C) Dafeng and Dongtai section for agricultural comprehensive exploitation, (D) Nantong section for aquaculture and agriculture, are suggested. Meanwhile, the paper takes the guiding ideology of sustainable development to be reflected in modern integrated coastal management and legislation. Supported by Natural Sciences Foundation of Fujian (D 97006) and State Pilot Laboratory of Coast & Island Exploitation, Nanjing University.  相似文献   

RESEARCH ON SYSTEM OF FLOOD DISASTER CONTROL AND REDUCTION SUPPORTED BY GIS IN MEDIUM AND SMALL BASINS   总被引：2，自引：0，他引：2  

XUYon－peng  DUJin－kang 《中国地理科学(英文版)》2002,12(1):30-34

Southeast China coastal areas belong to subtropical monsoon climatic zone,thus easily affected by floods resulted from typhoons and rainstorm.Since the areas of river basins are small,rivers flood regulation capacities are low,and therefore flood hazard is grave.In the paper,taking the Yongjiang basin in southeast China as an example,the approaches and methods of geographic information system(GIS) applied to flood disaster control and reduction research on small basin are explred.On GIS help the rainfall-runoff calculation model and the river dchannel flood routing model are developed.And the evaluating flood submerged are and the damage assessment models are built supported by digit elevation models.Lastly the decision support system on GIS supported for flood control in research basin has been set up.This greatly improves flood-proofing decision-making capacities in river basin,and provides valuable information and a mode for flood prevention and reduction in the medium and small basin .Meanwhile,the research indicates that technologies of GIS provide a powerful tool for flood disaster control.  相似文献