1) tidal flat
潮滩
1.
Seasonal accumulation and bioavailabilities of phosphorous in the tidal flat surface sediments from the Yangtze estuary;
河口潮滩沉积物磷的季节性累积和生物有效性
2.
Heavy metal accumulation features and significance in tidal flat surface sediments of Guanhe Estuary;
灌河口潮滩重金属累积特征及污染评价
3.
Distribution of biogenic silica in tidal flat sediments of Yangtze Estuary and its influence factors;
长江口潮滩沉积物生物硅的分布及其影响因素
2) Intertidal flat
潮滩
1.
In 1998-1999, contents of inorganic nitrogen (NH4N, NO3N and NO2N) in water and sediment of intertidal flats of Shanghai coast were investigated at three stations (CY, DH and LY).
对长江口南翼上海滨岸带三个站点潮滩上覆水、沉积物和间隙水中的三态无机氮的含量分布的年度季节性监测研究表明:潮滩上覆水中溶解无机氮以NO3 N为主;表层沉积物中可交换态无机氮以NH4 N为主,约占70%~85%;沉积物间隙水中主要无机氮为NH4 N和NO3 N。
2.
It is indicated that the adsorption of sediments on NH~+_4-N shows linear Changes in the possible range of NH~+_4-N in overlying waters and porewaters from the intertidal flat of the Changjiang Estuary.
沉积物对NH4+-N的吸附是氮素生物地球化学循环的关键过程之一,它在河口潮滩生态系统内氮素循环过程中起着非常重要的作用。
3.
The development of intertidal flat in river mouths depends on favorable conditions such as riverborn sediment supply, estuarine hydrodynamics and morphology of seabed.
该文阐述河口潮滩的发育依赖于河流泥沙来源、河口动力和海底地形诸方面的有利条件。
3) tidal flats
潮滩
1.
Nitrogen profiles in core sediment and interstitial water of tidal flats in Changjiang(Yangtze)River Estuary;
长江口滨岸潮滩柱样沉积物与孔隙水中氮的垂直分布特征
2.
In this paper, a total of 56 relatively nonpoint source pollution sediment s amples were collected from the tidal flats of the Jiuduansha shoal and the Chong ming island of the Yangtze river estuary.
采集长江口无明显点源污染的崇明东滩和九段沙潮滩56个沉积物样品,测定沉积物原样和粘粒中Cu,Zn,Pb,Cr,Cd和Ni的含量以及沉积物的主要性状(粒径分布、游离铁、活性铁、总铁、游离锰、总锰、有机碳和磁化率等),以相关分析和偏相关分析研究沉积物中重金属含量与沉积物主要性质之间的关系。
5) Feiyantan tidal flat
飞雁滩潮滩
6) high tidal flat
高潮滩
1.
The features of NH_4~+-N concentration changes within a tidal cycle at the sediment-water interface in the edge of of high tidal flat;
高潮滩盐沼前缘沉积物—水界面NH_4~+-N浓度的潮周期变化
2.
According to the assessment by pollution load index method,in Chongming Wetland which was mainly with silty soil,both medium and high tidal flats were moderately polluted with heavy metals, while low-tidal flat had not been polluted.
对取自崇明东滩的高潮滩、中潮滩和低潮滩的沉积物柱样进行了磁学、粒度、重金属含量等指标的分析、比较与综合研究。
补充资料:潮滩
潮滩 tidal bank 沿海岸分布,由小于0.06毫米粉沙和粘土组成的长数十千米的平缓地带。属于一种海岸堆积地貌类型。主要受潮流影响。按地貌特性和出露部位分为:①潮上带。指平均大潮高潮线以上至特大潮汛或风暴潮作用上界之间的地带。常出露水面,蒸发作用强,地表呈龟裂现象,有暴风浪和流水痕迹,生长着稀疏的耐盐植物。该带常被围垦。②潮间带。指平均大潮低潮线至平均大潮高潮线之间的地带。此带周期性地受海水的淹没和出露,侵蚀、淤积变化复杂,滩面上有水流冲刷成的潮沟和浪蚀的坑洼。此带是发展海水养殖业的重要场所。③潮下带。指平均大潮低潮线以下的潮滩及其向海的延伸部分。此带水动力作用较强,沉积物粗。中国沿海地区每年接受来自黄河、长江、珠江等输出的泥沙达20多亿吨,潮滩广为发育。它分为两类:在河口三角洲基础上形成的潮滩,如江苏北部和渤海西部海岸;沿岸水流搬移泥沙在隐蔽海湾堆积成的潮滩,如杭州湾以南至闽江口以北海岸。 |
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