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Geochemical processes controlling dissolved selenium in the Changjiang (Yangtze) Estuary and its adjacent waters

机译:控制长江口及其邻近海域溶解硒的地球化学过程

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摘要

Dissolved selenium in the Changjiang (Yangtze) Estuary and its adjacent waters was determined by hy-dride generation atomic fluorescence spectrometry to elucidate the source, behavior in estuary, adsorp-tion-desorption process and biological role. In surface water, Se(IV ) concentration ranged 0.05-1.14 nmol/L and Se(VI) concentration varied 0.01-1.20 nmol/L, with the means of 0.76 and 0.49 nmol/L, respectively. In bottom water, Se(IV) content varied 0.03-0.27 nmol/L and Se(VI) content ranged 0.04-0.85 nmol/L, with the averages of 0.10 and 0.40 nmol/L, respectively. High level of Se(IV ) was observed near the shore with a significant decrease towards the open sea, suggesting the continental input from the adjacent rivers. Large value of Se( VI) was found in bottom water, reflecting the release from suspended sediment. Besides, high value appeared in the same latitude of the Changjiang Estuary and Hangzhou Bay illustrated the effect of lat-eral mixing and the long-distance transport of selenium. Se(VI), more soluble, occupied higher percentage in aqueous environment. The presence of Se(IV ) resulted from the degradation of residue and the reduction of Se(VI) under anaerobic condition. The positive relationship to suspended particulate material (SPM) and negative correlation to depth indicated that Se(IV ) tended to be released from the high density particulate matter. Instead, Se(VI) content did not significantly relate to SPM since it generally formed inner-sphere complex to iron hydroxide. Se(IV ) content negatively varied to salinity and largely depended on the fresh-water dilution and physical mixing. While, Se( VI) level deviated from the dilution line due to the in situ bio-geochemical process such as removal via phytoplankton uptake and inputs via organic matter regeneration. As the essential element, Se(IV) was confirmed more bioavailable to phytoplankton growth than Se(VI), and moreover, seemed to be more related to phosphorus than to nitrogen.
机译:通过氢化物发生原子荧光光谱法测定了长江口及其附近水域中的溶解硒,以阐明其来源,在河口的行为,吸附-解吸过程和生物学作用。在地表水中,Se(IV)的浓度范围为0.05-1.14 nmol / L,Se(VI)的浓度范围为0.01-1.20 nmol / L,平均值分别为0.76和0.49 nmol / L。在底部水中,Se(IV)的含量变化为0.03-0.27 nmol / L,Se(VI)的含量变化为0.04-0.85 nmol / L,平均值分别为0.10和0.40 nmol / L。在海岸附近观测到高水平的Se(IV),向公海的方向显着减少,这表明来自相邻河流的大陆输入。在地下水中发现了较大的Se(VI)值,这反映了悬浮沉积物中的释放。此外,长江口的同一纬度也出现了高价值,杭州湾则说明了横向混合和硒的长距离迁移的影响。 Se(VI)较易溶解,在水性环境中占较高的百分比。 Se(IV)的存在是由于在厌氧条件下残留物的降解和Se(VI)的减少。与悬浮颗粒物(SPM)的正相关和与深度的负相关表明,Se(IV)倾向于从高密度颗粒物质中释放出来。相反,Se(VI)的含量与SPM无关,因为它通常与氢氧化铁形成内球络合物。硒(IV)含量随盐度的变化而变化,主要取决于淡水稀释和物理混合。同时,由于原位生物地球化学过程(例如通过浮游植物吸收去除和通过有机物再生输入),Se(VI)水平偏离了稀释线。作为必需元素,已证实Se(IV)比Se(VI)对浮游植物的生物利用度更高,而且似乎与磷比与氮更相关。

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  • 来源
    《海洋学报(英文版)》 |2014年第10期|19-29|共11页
  • 作者单位

    Institute of 0ceanology, Chinese Academy of Sciences, Qingdao 266071, China;

    Institute of 0ceanology, Chinese Academy of Sciences, Qingdao 266071, China;

    Institute of 0ceanology, Chinese Academy of Sciences, Qingdao 266071, China;

    Institute of 0ceanology, Chinese Academy of Sciences, Qingdao 266071, China;

    Institute of 0ceanology, Chinese Academy of Sciences, Qingdao 266071, China;

  • 收录信息 中国科学引文数据库(CSCD);
  • 原文格式 PDF
  • 正文语种 eng
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