1) inner Lingdingyang
内伶仃洋
2) Lingding Bay
伶仃洋
1.
Distribution of Alkylphenols in Surface Water and Sediments from Lingding Bay;
伶仃洋水和沉积物中烷基酚的分布特征
2.
By means of GIS and remote sensing technique, the changes and evolvements characteristics of foreshore and deep channels of Lingding bay in Pearl River Estuary are analyzed.
借助GIS和遥感技术 ,计算分析了 2 0a来珠江口伶仃洋滩槽演变特点 ,阐明了其变化原因和后果 ,并以此提醒人们要从可持续发展的高度规范岸区开发行为 ,以利于珠江三角洲的长期稳定发
3) Lingdingyang Estuary
伶仃洋
1.
The receptor model which was developed by study of aerosol source and acid rain formation was applied to the research of heavy metal pollution of sediments in Lingdingyang Estuary.
首次将该模型移植到水环境的沉积物重金属污染研究中，经验证处理后，解析了伶仃洋沉积物中重金属的地理区域源，并定量计算了这些区域源对特征污染元素的贡献率。
2.
Through investigation of the water environment condition and collection of water quality data,emphatically discussed is the impact of hydrological factors and pollutant quantity upon the temporal and spatial variation of water quality in the Lingdingyang estuary.
通过调查及收集伶仃洋水域环境现状资料，着重分析水文因素和排污量对伶仃洋水质时空变化的影响。
3.
Based on measured data and the model of longitudinal material fluxes, thepaper analyzes the vertical profiles of Eulerian, Stokes and Lagrange residual currents inwet season in the Lingdingyang Estuary of the Zhujiang River Mouth.
根据实测资料，运用物质纵向输移模式探讨了丰水期伶仃洋河口湾余流的垂向结构。
4) Lingding Sea
伶仃洋
1.
A Stagger Compntation for Water Quadity with One-Dinensional Model for Pearl River Delta and Three-Dimensional Model for the Lingding Sea;
珠江三角洲河网与伶仃洋一、三维水质模型联解研究
2.
Formation mechanism and distribution characteristics of the fluid mud in the seaward channel of the Lingding Sea;
伶仃洋出海航道浮泥形成机制与分布特征
3.
Coupling solution of 1-D hydrodynamic model for the river network of Pearl River Delta and 3-D hydraulic model for Lingding Sea;
珠江三角州河网与伶仃洋一、三维水动力学模型联解研究
5) Lingdingyang
伶仃洋
1.
Pollution of heavy metals in the Lingdingyang of Pearl river Estuary and its assessment of potential ecological risk;
珠江口伶仃洋海底表层沉积物重金属污染及潜在生态危害评价
2.
Reactive Silicate in the Water Body of Lingdingyang;
伶仃洋水域水体中的活性硅酸盐
3.
It will be very useful for sustainable development of regional exploitation and construction if understanding the characteristics of sea bottom deposit in Lingdingyang Bay.
在前人工作的基础上,利用2003—2005年广州海洋地质调查局1∶10万《珠江三角洲近岸海洋地质环境与地质灾害调查》项目的实测资料,综合分析了伶仃洋海底的沉积特征,认为伶仃洋表层沉积物类型有:砂、黏土质砂、砂-粉砂-黏土、砂质黏土、黏土质粉砂、粉砂质黏土等6种类型。
6) Lingdingyang Bay
伶仃洋
1.
Analysis of influencing factor on shoal and though development of Lingdingyang Bay at Zhujiang Estuary;
珠江口伶仃洋滩槽发育演变影响因素的分析
2.
Longitudinal transport mechanism of water and sediment in west channel of Lingdingyang Bay during flood season;
伶仃洋西槽洪季水沙纵向输移机制研究
3.
Synchronous and quasi-synchronous information acquired in a larg area in a moment by remote sensing technique has notonly overcome the limitations of data obtained by observations uesd to be done before, but also provided accurate and reliable data forthe planning and improvement of Lingdingyang Bay and four eastern outlets.
利用遥感技术来观察伶仃洋，可以在瞬间获得大面积的地表或地表浅层信息，其时间上的同步或准同步性克服了以前由直接观测点或线推证到面的局限性，为伶仃洋和珠江三角洲东四口门规划治理研究和局部工程治理监测提供了准确可靠的数据资料。
补充资料：伶仃洋
| 伶仃洋 位于中国广东省珠江口外，为一喇叭形河口湾。又称零丁洋、珠江口。其范围北起虎门，口宽约4千米，南达香港、澳门，宽约65千米，水域面积约2100平方千米。东由深圳市赤湾，经内伶仃岛，西到珠海市淇澳岛一线以北为内伶仃洋，水域面积1041平方千米。浅滩发育。珠江经虎门、蕉门、洪奇沥、横门，年均排泄泥沙3000多万吨，滩涂每年向江内延伸100米左右，航道面临着缩窄变浅的危险。 |
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条