Grain-size spectra maps of beaches in W. Peloponnese, Greece     

N. Kontopoulos 《Mathematical Geology》1984,16(2):207-211

Grain-size spectra maps of sands from beaches of the western Peloponnese are related to statistical parameters and can be used to infer characteristics of the sedimentation process involved which were unresolved by previous statistical analysis. On the basis of similarities in spectral patterns, the studied beaches fall into four groups: A, B, C, and D. The periodicity observed on the sinuous pattern of the spectra map of groups A and B is interpreted as indicating edge-wave activity. Regarding group D, the gradual W—E increase of particle size along the coast suggests a W—E increase of wave energy, which is also reflected by the inclined trend of the spectra map. Lack of periodicity on the contour pattern of group C probably reflects intensive sample-to-sample sorting variation.  相似文献   

Preliminary hydrodynamic results of a field experiment on a barred beach, Truc Vert beach on October 2001     

N. Sénéchal  H. Dupuis  P. Bonneton 《Ocean Dynamics》2004,54(3-4):408-414

A field experiment conducted on a sandy barred beach, situated on the southern part of the French Atlantic coastline, allowed us to investigate the impact of the intertidal bar on the wave-energy dissipation on the beach face in presence of a high-energy long-incoming swell (significant wave height of about 1.7 to 3.0 m in 56 m water depth and significant wave period about 12 s). Data were collected along three parallel cross-shore transects deployed along an intertidal ridge and runnel system. Wave heights in the inner surf zone are depth-limited, consistent with previous works, and the wave-energy dissipation in the inner surf zone appears to be relatively independent of the offshore energy level. On the other hand, the presence of the bar seems to scatter the data. In models of surf-zone hydrodynamics, wave-energy dissipation is often parameterized in terms of , the ratio of the sea-swell significant wave height to the local mean water depth. The observed values of are not constant along a cross-shore transect, and increase onshore. Furthermore, the observed values observed onshore the intertidal bar are higher than those observed outside the influence of the intertidal bar, and this cannot be fully explained by the different local beach slope.Responsible Editor: Iris Grabemann  相似文献   

中国海岸带分布规律及其海部要素变化检测   总被引：2，自引：1，他引：1  

冯伍法  潘时祥  张朝阳  张俊华 《测绘科学技术学报》2006,23(5):370-373,377

在海岸带图测绘完成后,海部要素的变化是导致海岸带图使用价值降低的重要因素.根据我国海岸的组成物质将其归纳为淤泥质海岸、沙砾质海岸、基岩海岸、红树海岸和珊瑚海岸,并归纳总结了每一种海岸的空间分布规律.分析了影响海岸线、干出滩以及近海水深等海部要素变化的主要因素,海岸要素变化的因素和变化规律,进而提出了海部要素实质性变化的检测统计方法,对提高海岸带图测绘效率、缩短成图周期、确定更新周期和制定更新方案都具有重要的意义.  相似文献   

遥感技术在沿海滩涂提取中的应用     

吴定定 《测绘与空间地理信息》2012,35(11):83-84,88

基于遥感技术,利用TM多光谱影像和SPOT全色影像,在遥感影像处理软件ERDAS 8.7中进行几何配准、IHS融合,采用监督分类的方法,对福州市长乐地区的沿海滩涂进行自动提取,并结合地理信息系统软件Arc-GIS DeskTop 8.3制作滩涂提取专题图。结果表明,遥感技术用于沿海滩涂监测,具有科学性和直观性,是传统方法无法比拟的,能更好地为滩涂管理相关部门的规划和管理提供实时、准确的依据。  相似文献   

基于无人机航空摄影技术的厦门滩涂养殖调查     

王镇 《福建地理》2012,(3):38-43

近年来随着实时化测绘的需求增加,无人机航空摄影发展迅速.无人机航摄具有运行成本低、执行任务灵活性高等优点,是遥感数据获取的重要手段.本研究论述了利用无人机对厦门市翔安区滩涂进行航空摄影制作1∶2 000正射影像的方法,其成果用于滩涂养殖信息调查.  相似文献   

李官海滩旅游规划的客源市场分析与容量测算   总被引：3，自引：0，他引：3  

荀怡  王欣  杜瑜 《地域研究与开发》2004,23(3):94-97

文章在通过对辽宁省大连市李官海滩的客源市场进行实地调查的基础上,结合引力模型,还考虑到影响李官海滩旅游市场开发的的因素,运用比例缩小法和类比法分析李官海滩旅游规划的客源市场结构,并根据李官现有的旅游环境和设施接待能力,综合分析李官海滩旅游开发的客源容量。对比分析李官客源地的居民生活水平,以距离衰减规律为依据,预测出客源市场规模,并将客源市场进行分级分类。  相似文献   

辽河盆地西部凹陷古近系沙四上亚段沉积相及演化     

王夏斌  姜在兴  胡光义  范廷恩  王俊辉  卢欢 《吉林大学学报(地球科学版)》2019,49(5):1222-1234

薄互层砂体研究是湖盆沉积学的研究难点。本文针对辽河西部凹陷沙四上亚段（Es^4上）薄互层砂体,以层序地层学、沉积学、测井地质学等理论为指导,综合岩心、测录井和地震等多种资料,对西部凹陷的薄互层砂体进行精细描述和深入剖析。结果表明,研究区主要发育辫状河三角洲和湖泊沉积相,其中,滩坝砂体是湖泊相的主力砂体。通过考虑不同沉积背景下滩坝在岩相组合、发育位置和成因机理的差异性,将滩坝划分成侧缘改造型滩坝、前缘改造型滩坝、基岩改造型滩坝、淹没改造型滩坝和风暴改造型滩坝5种沉积模式;对薄层滩坝砂体的控制因素进行分析,认为其受到"风场-物源-盆地"三端元的控制。  相似文献   

Short-Term Morphological and Shoreline Changes at Trinkat Island,Andaman and Nicobar,India, After the 2004 Tsunami     

P. Yunus Ali 《Marine Geodesy》2013,36(1):26-39

The tsunami waves generated during the Sumatra-Andaman earthquake of 26 December 2004 devastated the coastal area along Trinkat Island, causing sudden changes to the morphology of the landforms. This study uses a series of satellite images to record the short-term morphological response and shoreline changes as well as the recovery of coastal land after its destruction. Results indicate that the island experienced substantial erosion and a significant reduction in land area. Shoreline erosion is more prevalent than accretion at an average linear regression rate of ～?9 m per year between 2004 and 2013. The major morphological changes at Trinkat Island were observed in coastal inlets, beaches, and bay head-lands. Straight beaches had almost recovered eight years after the tsunami; however, erosion is continually observed in other areas. Our study will help understanding the response and recovery of shorelines in Indian Ocean regions after the 2004 tsunami.  相似文献   

海阳市典型砂质海岸侵蚀机制与防护对策研究     

王勇智  田梓文  李霞  孙惠凤 《海洋科学》2021,45(12):18-30

海阳市砂质海岸资源丰富,延绵近120 km,尤以万米沙滩浴场著称,但近年岸滩侵蚀严重影响其社会经济发展.本研究基于海阳市羊角畔两侧长约20 km典型砂质海岸连续3 a的海岸线蚀和典型剖面蚀淤调查,定量化研究海滩侵蚀及其变化,辅以一维数值模型,研究人类活动影响下的泥沙运动特征和海滩侵蚀机制.研究结果表明,调查区42.5％和5.90％的砂质海岸分别处于侵蚀和强侵蚀状态,羊角畔东侧海岸侵蚀强度高于西侧,海阳港至海阳核电厂之间海滩侵蚀强度最高,海滩侵蚀强度与人类活动扰动程度密切相关.海岸工程、临海养殖和人为采砂导致海阳市部分砂质海岸侵蚀严重的主要原因,导致羊角畔两侧海岸侵蚀机制也不同.基于各岸段侵蚀机制特征有针对性地提出退养还滩、凸堤拆除和沙滩喂养等对策,以减缓海阳砂质海岸侵蚀威胁.  相似文献   

琼东北海湾海滩地形年度变化特征对比分析          下载免费PDF全文

吴多誉  张航飞  张东强  符广卷 《海岸工程》2021,40(1):29-36

利用2016—2017年琼东北海湾海滩断面高程数据,对比分析了琼东北海湾-海口湾、铺前湾和木兰湾年度地形变化特征。结果表明,海口湾、铺前湾和木兰湾海滩断面地形均具有季节性变化特征,整体上夏缓冬陡,表现为前滨遭受侵蚀作用,而后滨则发生堆积作用。冬季,琼州海峡的海平面较高且风浪作用更强,这是导致冬季的海滩地形变化幅度较夏季更为明显的原因之一。同时,岸外人工岛的建设、河流输沙量的急剧减少和人类活动等,也是海滩地形变化的重要影响因素。研究结果可为琼东北海湾岸线资源开发利用与地质环境保护提供一定的科学依据。  相似文献