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81.
九龙江河口区现代沉积环境及其物质输运趋势 总被引:1,自引:0,他引:1
对九龙江河口区58个表层沉积物样品进行了激光粒度分析,并分别应用系统聚类分析和GSTA模型分析,探讨了研究区的沉积特征、沉积环境和表层沉积物输运趋势。结果表明,九龙江河口区表层沉积物由10种沉积物类型组成,与20世纪80年代相比,该海区底质沉积物在类型分布和粒径粗细上发生了一定的变化;将研究区划分为3种与沉积动力特征相对应的主要沉积环境区;表层沉积物输运趋势因受该区特殊的地形和复杂的水动力条件影响而表现为北进南出,海门岛西北海域形成逆时针方向输运趋势,而海门岛以东海域形成三向汇聚的输运趋势。 相似文献
82.
Capabilities of the bathymetric Hawk Eye LiDAR for coastal habitat mapping: A case study within a Basque estuary 总被引:1,自引:0,他引:1
Guillem Chust Maitane Grande Ibon Galparsoro Adolfo Uriarte Ángel Borja 《Estuarine, Coastal and Shelf Science》2010
The bathymetric LiDAR system is an airborne laser that detects sea bottom at high vertical and horizontal resolutions in shallow coastal waters. This study assesses the capabilities of the airborne bathymetric LiDAR sensor (Hawk Eye system) for coastal habitat mapping in the Oka estuary (within the Biosphere Reserve of Urdaibai, SE Bay of Biscay, northern Spain), where water conditions are moderately turbid. Three specific objectives were addressed: 1) to assess the data quality of the Hawk Eye LiDAR, both for terrestrial and subtidal zones, in terms of height measurement density, coverage, and vertical accuracy; 2) to compare bathymetric LiDAR with a ship-borne multibeam echosounder (MBES) for different bottom types and depth ranges; and 3) to test the discrimination potential of LiDAR height and reflectance information, together with multi-spectral imagery (three visible and near infrared bands), for the classification of 22 salt marsh and rocky shore habitats, covering supralittoral, intertidal and subtidal zones. The bathymetric LiDAR Hawk Eye data enabled the generation of a digital elevation model (DEM) of the Oka estuary, at 2 m of horizontal spatial resolution in the terrestrial zone (with a vertical accuracy of 0.15 m) and at 4 m within the subtidal, extending a water depth of 21 m. Data gaps occurred in 14.4% of the area surveyed with the LiDAR (13.69 km2). Comparison of the LiDAR system and the MBES showed no significant mean difference in depth. However, the Root Mean Square error of the former was high (0.84 m), especially concentrated upon rocky (0.55–1.77 m) rather than in sediment bottoms (0.38–0.62 m). The potential of LiDAR topographic variables and reflectance alone for discriminating 15 intertidal and submerged habitats was low (with overall classification accuracy between 52.4 and 65.4%). In particular, reflectance retrieved for this case study has been found to be not particularly useful for classification purposes. The combination of the LiDAR-based DEM and derived topographical features with the near infrared and visible bands has permitted the mapping of 22 supralittoral, intertidal and subtidal habitats of the Oka estuary, with high overall classification accuracies of between 84.5% and 92.1%, using the maximum likelihood algorithm. The airborne bathymetric Hawk Eye LiDAR, although somewhat limited by water turbidity and wave breaking, provides unique height information obscured from topographic LiDAR and acoustic systems, together with an improvement of the habitat mapping reliability in the complex and dynamic coastal fringe. 相似文献
83.
潮沟成因类型及其影响因素的探讨 总被引:14,自引:0,他引:14
潮沟是潮坪上最活跃的微地貌单元。从成因角度分出了滩面水流冲剧型、潮流辐聚侵蚀型、陆源水流侵蚀继承型和泻湖广海间潮流侵蚀型等四种潮沟类型。根据各地潮沟发育程度的明显差异,提出了影响潮沟发育的七个重要因素。 相似文献
84.
The aim of this paper is to study the REE geochemistry of the Shenzhen Bay (SZB) and Dapeng Bay(DPB) modern sediments, discuss their REE distribution patterns, reveal the REE geochemical difference between the two bays which share the same material source but are deposited in different sedimentary environments, and expound their dynamic changes.It can be concluded that the SZB and DPB sediments are essentially of continental source.Their REE distribution patterns are quite different from those of Pacific pelagic sediments, but are very similar to those of South Chi-na granites.Because of different sedimentary environments prevailing in the SZB and DPB, some REE fractionation would have taken place in the sediments of the two bays. 相似文献
85.
86.
江苏北部开敞淤泥质海岸的侵蚀过程及防护 总被引:9,自引:0,他引:9
开敞淤泥质海岸是淤泥质海岸的主要类型,其自然演变过程,主要受沿海河流泥沙供应条件的制约,一旦泥沙供应消失,海岸往往进入不可逆转的侵蚀过程。江苏北部淤泥质海岸的侵蚀过程,起自1855年黄河入海口北归利津入海以后,主要是在近岸破波对岸滩物质的冲刷和潮流的输移扩散作用下进行的。通过对淤泥质海岸动力和沉积物性质的认识和概化,对海岸侵蚀过程作出定量模拟,并对该地区海岸防护工程作出评价和讨论。 相似文献
87.
根据沙河、正定、商丘、东营四测站三天同步测量所获取的地磁日变数据,提出了三种局部地区地磁日变的拟合方法;井通过对四测站三天地磁日变曲线的分析发现了时差对日变曲线的非均衡影响以及东营日变具比较明显的海岸效应之影响。 相似文献
88.
地勘经济改革的战略思想是建设适应社会主义市场经济的新体制,将现有的地勘队伍组建为"地质找矿的野战军"和"实行企业化的地方军".分别按事业机制和企业机制运行。如何实现地勘单位(地方军)的企业化,笔者认为首先必须用现代企业制度改造和重塑现有的多种经营企业,并分析了困难和有利条件,提出了相应的对策和措施,使多种经营企业真正成为符合现代企业制度要求的经济实体。加快发展部门产业经济,才能逐步推进地勘单位的企业化。 相似文献
89.
Seasonal and diurnal variability of thermal structure in the coastal waters off Visakhapatnam has been examined in relation
to the flow field and surface winds utilizing the hourly data of temperature and currents taken at a fixed location over a
tidal cycle at monthly intervals. The coastal currents in the pre-monsoon period and strong near-surface winter cooling processes
affect the thermal structure of the coastal sea. Upwelling which is predominant during March to May with an intermittent relaxing
event helps in the development of a strong layered thermal structure while convective mixing due to winter inversions during
November to February causes weak thermal gradients in the water column. 相似文献
90.
I. Alvarez M. Gomez-Gesteira M. deCastro R. Prego 《Journal of Atmospheric & Ocean Science》2005,10(4):309-324
Thermohaline variables were simultaneously measured, July 17, 2000, at four Galician rias under favourable upwelling conditions to analyse upwelling intensity. The intensity of coastal upwelling is shown to be strongly dependent on the wind pattern. The maximum amplitudes of wind stress were observed at the western coast (0.30 Nm-2) with southward direction (favourable to upwelling) and these are shown to be related to low temperature (12°C) and high salinity (35.8) in the estuaries mouth. From Cape Finisterre to Cape Estaca de Bares the wind stress showed a lower magnitude (0.05-0.10 Nm-2) with a direction oblique to the coast. The temperature showed an increase (14°C) and the salinity a decrease (35.4) because the lower upwelling intensity at this part of the coast. The observed decrease in upwelling from south to north is not an isolated event, since the measured wind conditions are persistent during summer months, at least in the period with available QuikSCAT data (1999-2004). 相似文献