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在考虑岸滩的冲淤变化特性、不同岸段冲淤速率差异以及岸外滩涂资源存量差异的基础上,扩展定义了适用于淤泥质海岸的围填海强度与潜力定量评价模型,并以2007-2013年江苏南通海岸老坝港-东灶港淤积岸段、东灶港-蒿枝港侵蚀岸段和蒿枝港-连兴港稳定岸段的围填海造地工程为对象,进行了围填海开发状况定量评价分析及开发潜力预测。结果表明:在以5级为上限的强度评价体系下,2013年老坝港-东灶港、蒿枝港-连兴港岸段的围填海开发强度为3级,围填海压力中等,对岸段的后续开发有一定影响;东灶港-蒿枝港岸段的围填海强度等级为4级,围填海压力较强,应注重围填海域集约利用。由于岸外资源存量的差异以及围填海开发速率的差异,三段海岸未来的可供开发年数预测分别为8年、1年和11年。该评价方法可为定量评估淤泥质海岸围填海开发强度、实现围填海开发潜力科学预测提供参考。 相似文献
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围填海是缓解沿海地区土地资源紧缺的重要途径。进入21世纪以来,我国掀起了新一轮大规模的围填海热潮,随后关于围填海造成的负面影响受到越来越多的关注。近岸围填海作为最常见的一种围填海工程,其环境影响评价的理论体系和技术方法至今尚不系统。本研究从单一环境影响和综合环境影响两方面对近岸围填海环境影响评价的最新研究方法与成果进行归纳总结,在单一环境影响评价方面重点研究了水动力与沉积环境影响评价以及污染物运移影响评价,在综合环境影响评价研究方面重点研究了综合效益评价、适宜性评价、承载力评价、脆弱性评价等方法,以期为海洋管理部门的围填海开发与管理提供参考。 相似文献
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围填海是区域社会经济发展到一定阶段向海洋谋求发展空间的一种基本手段。珠江三角洲是我国社会经济发展的热点区域之一,探索其近岸河口区域围填海时空过程并对其未来趋势进行分析对海岸带综合开发具有重要的意义。本研究以多源陆地资源卫星Landsat为数据源,通过影像数据处理分析探讨了珠江口围填海历史变迁过程,并对其围填海生命周期进行了估计。结果表明,珠江口围填海主要发生在改革开放后,其中1978—1988年围填海面积为18 572hm2,1988—1996年间围填海面积为25 528hm2,1996—2005年间围填海面积为13 911hm2,2005—2015年间围填海面积6 723hm2。截至2015年,珠江口共围填海面积64 753hm2,空间上主要集中分布于西部岸段。基于历史围填海时空演变过程,通过围填海生命周期图进一步对珠江口未来的围填海工程实施潜力进行形式预判。结果显示,珠海岸段和深圳前海岸段是珠江口今后实施围填海热点区域,其他区域围填海速度会相对减缓,但随着珠江口海岛逐渐与陆地海岸带相接,该区域围填海过程也将会终止。围填海生命周期分析可为海岸带实施围填海工程规划提供相关决策依据。 相似文献
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利用1985—2018年6个时间段的Landsat TM、ETM、OLI遥感影像,使用面向对象的遥感提取方法,通过选取空间利用结构、开发利用程度、景观指数及质心转移分析了沧州市围填海空间格局变化特征。结果表明:33年间研究区内围填海活动剧烈,1985—2018年,沧州近岸海域新增围填海面积137.05 km2,围填用海规模随时间变化不断扩大。1985—2003年,围填海空间利用结构和类型经历了从以围填养殖用海为主到各类型围填用海兼备的演化过程。研究区内围填海强度逐渐上升,2018年围填海开发强度指数达到274.55。港口用海逐渐成为沧州近海海域围填海的主要类型,围海养殖用海次之。1985—2018年,沧州市围填海景观的聚集度指数与蔓延度指数均较高,平均聚集度指数高达99.4004,围填海景观分布具有较强的规律性。沧州市围填海质心不断向东南方向移动,说明沧州市围填海开发的重点区域逐步迁移至沧州南部海域。在当前围填海现状下,应注重后续围填海开发活动的合理规划和集约利用。 相似文献
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21世纪以来伴随着我国城市化、工业化和人口向沿海地区集聚趋势的进步加快,沿海地区土地资源不足导致的用地矛盾促使围填海项目不断增加。通过围填海向海洋要发展、生产和生活空间,已成为缓解沿海地区发展土地资源的"瓶颈"、推动沿海地区经济社会发展重要途径之一。开展海域使用动态监视监测是加强围填海项目用海监管的重要手段。文章从监测目的、监测准备、监测方法及流程、监测成果编制等方面对围填海项目海域使用动态监视监测进行了全面论述,以期为相关技术规程的制定和海域动态监视监测业务的规范提供参考。 相似文献
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基于椒江河口大、小潮期间水位、流速、盐度和悬沙浓度观测数据,研究了椒江河口主潮汐通道的水动力、盐度和悬沙浓度的时空变化特征,解释了高浊度强潮作用下的层化物理机制。椒江河口大潮期悬沙浓度和盐度均大于小潮期,主潮汐通道区域落潮期悬沙浓度大于涨潮期;盐度随潮变化,盐水锋面出现在S2测站,锋面附近出现最大浑浊带;自陆向海,悬沙浓度递减,盐度递增;随水深增加,悬沙浓度与盐度递增。Richardson数与混合参数显示,盐度和悬沙引起的层化现象,是随着潮汐的变化而变化,涨潮时的层化均强于落潮,小潮时的层化持续时间最长,区域更广。混合参数随潮周期变化,大潮期高于临界值1.0,小潮期低于临界值1.0。小潮期水体层化强于大潮期;潮汐应变项是影响势能差异变化率的重要因素;落潮期间层化向混合状态转化,涨潮相反。 相似文献
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Dong Lixian 《海洋学报(英文版)》1998,17(4):469-482
ThisstudywassupportedbytheNationalNaturalScienceFoundationofChinaundercontractNo.49276274,theZhejiangProvinceNaturalScienceFoundationundercontractNo.490013,theChina-Australiabilateralscienceandtechnologyprogram,theAustralianInstituteofMarineScience,theModellingLaboratoryoftheMarineScienceintheSecondInstituteofOceanographyoftheStateOceanicAdministration.INTRODUCTIONTheJiaojiangEstuaryis1ocatedintheeasterncoastofChina,2OokmfromthesouthoftheChangjiangRiver(YangtzeRiver),linkedin… 相似文献
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A Model for Environmental Impact Assessment of Land Reclamation 总被引:2,自引:0,他引:2
Land reclamation is a complex marine environmental engineering and has a huge impact on social, economic, and physical environment. Reclamation environmental impact assessment (REIA) is also a complicated project, including the assessment of social economic background, ocean engineering, coastal geomorphology, sediment transportation, marine hydrodynamics and marine ecosystem and so on. Nowadays, a large number of land reclaimed projects have been carried out or in the process of construction along the coastal zone, thus, it is necessary to build up a framework on REIA to evaluate and quantify the environmental changes, to contribute to reclamation program, to reduce marine environmental disasters, and to sustain development of coastal zone. This article focuses on the research of REIA framework theory and puts forward a REIA model on land reclaimed evaluation, at the same time, applies this assessment system in Shenzhen City, which is a highly developed coastal city with an expectation of land reclamation. By use of the Remote Sensing (RS) and Geographic Information System (GIS) techniques, along with the topographic map and in situ survey in reclamation area, it concludes that the area of 2680 hectares in total has been reclaimed in Shenzhen city by the end of the year 2000. Thus, reclamation is usually applied to meet the needs for infrastructure, such as harbors, industries and highways in Shenzhen City. However, some serious negative impacts have been created to the coastal environment shown clearly in the following aspects. Firstly, it caused the dramatic changes of tidal flat and channels along the western coast, made this area more unstable, which is threatening the function of the harbor in this area. Secondly, Tidal prism has decreased rapidly. During the 20 years of reclamation, the tidal prism has been reduced by 20%~30% along the western coast in the Lingdingyang Estuary, and 15.6% in the Shenzhen Bay. As a result, the velocity of the tidal current has also declined, and the direction of the tidal current has changed, which is harmful to the dilution and diffusion process of the contaminants. Thirdly, it has threatened the eco-environment finally. More than 147 hectares of mangrove area along the coast of Shenzhen Bay, accounting for 48.8% of the total mangrove reserve area in this region, has been reclaimed only during the short period from 1988 to 2000. Thus, the biodiversity is decreasing, and more and more plants and animals are disappearing. Based on the above analyses of the environmental impacts, strategies and suggestions for the future reclamation in this area have been put forward in order to support the sustainable development of the coastal zone. 相似文献
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Extensive data were obtained of the water and fine sediment dynamics during spring tides in the extremely turbid Jiaojiang River estuary at spring tides. These data enabled the calibration of a two-dimensional (2-D) width-integrated model. Four processes dominated the mud dynamics. These were, firstly, the formation at slack tide of soft mud deposits with an erosion constant much smaller than that of the underlying compacted sediment, secondly the sediment-induced buoyancy effects, thirdly the collapse of the turbulence by the sediment suspension in the fluid mud range and fourthly the inflow of sediment at the mouth of the estuary. These findings demonstrate the necessity to have detailed field data to enable quantitative, as opposed to qualitative, modelling of mud dynamics in turbid estuaries. The estuary is infilling with sediment from the East China Sea and not from riverine inflow, this sediment presumably originates from the Yangtze River located 200 km further north. 相似文献
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3-D fluid-mud dynamics in the Jiaojiang Estuary, China 总被引:3,自引:0,他引:3
A 3-D model has been developed for the muddy Jiaojiang Estuary and adjoining coastal waters, and verified against field observations. To simulate fluid-mud formation, the model uses a fine resolution grid near the bottom and involves coupling processes between hydrodynamics and fluid mud such as the sediment-induced buoyancy, increasing turbulent kinetic energy sink and kinematic viscosity, mixing by internal waves riding on the lutocline, and non-Newtonian properties of fluid mud. The effective hydrodynamic drag was reduced in the presence of fluid mud. It is shown that the estuary is infilled by tidal pumping and that longitudinal and transversal gradients of suspended sediment concentration, salinity, and currents control the formation of mud banks. Thus a 3-D model is necessary to estimate the fate of mud, although the model results are very sensitive to details of the parameterization of the hydrodynamics-mud feedback processes. 相似文献
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夏季闽江口和椒江口浮游动物群落结构的比较 总被引:1,自引:1,他引:1
根据2008年9月在闽江口水域和2010年8月在椒江口水域的调查资料,对两个河口浮游动物的种类组成、生态类群、优势种和生态适应差异进行分析比较,探讨夏季闽江口海域和椒江口海域浮游动物群落结构的区别及其组成受水团变化的影响。研究结果表明:夏季,椒江口受上升流的影响出现13个暖温带种,导致椒江口(44)水域浮游动物种类数要大于闽江口(36);闽江口海域夏季主要受到台湾暖流的影响,6个优势种全部为亚热带种,椒江口有7个优势种,包括4个亚热带种和3个暖温带种;从适温性上看,闽江口和椒江口均主要以亚热带种为主,椒江口由于上升流的原因出现较多数量的暖温带种,从适盐性上看,椒江口主要以近海种为主,闽江口主要以外海种为主,这是闽江口和椒江口浮游动物生态类群的主要差异;闽江口浮游动物群落结构主要受到台湾暖流和沿岸流的影响,而椒江口主要受到浙江近海上升流和沿岸流的影响,通过对两个河口群落结构的比较和生态适应差异的分析,表明水团是各自浮游动物群落结构的形成过程中的一个重要因素。 相似文献
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本文利用多年水文泥沙和水深地形资料,分析了椒江河口河床宽深比长周期变化特征,并尝试探讨了河床宽深比对水沙条件的响应。结果表明,径流和潮动力对河床形态影响程度沿程此消彼长,江口沙上游河段受径流作用较明显,栅浦下游河段受潮动力影响较显著,这应是弯曲和顺直河段河床横断面形态调整差异的影响因素;河床宽深比与径流平均输沙率正相关,径流产沙量减少,河床形态趋向窄深;顺直河段宽深比与平均流量负相关,径流来水减少,河床趋于宽浅;河床宽深比与平均潮差负相关,应是人为作用改变了潮动力对河口河床形态调整的影响。 相似文献