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首页> 外文期刊>Journal of Geophysical Research. Biogeosciences >Distribution characteristics of transparent exopolymer particles in the Pearl River estuary, China
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Distribution characteristics of transparent exopolymer particles in the Pearl River estuary, China

机译:珠江口透明外聚合物颗粒的分布特征

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摘要

Distribution of Transparent Exopolymer Particles (TEP) in the Pearl River estuary, China, was investigated during two cruises in August 2009 and January 2010. TEP_(color) concentrations were 521.5-1727.4 μg Xeq.L~(-1) (μg Gum Xanthan equivalent liter-1) in August 2009 and 88.7-1586.9 μg Xeq.L~(-1) in January 2010, respectively. The size of TEP generally increased in the seaward along the longitudinal section with the dominant size of 2-40 μm during the cruises. Experimental work suggested that both concentration and size of TEP increased with Ca~(2+) concentration (from 0.8 mmol L~(-1) to 10 mmol L~(-1)). In the field study, Ca~(2+) concentration had a positive correlation with TEP_(color) concentration in the surface layer with salinity <16. Decrease of TEP concentration seaward from intermediary salinity was partly due to dilution of seawater as well as enhanced aggregation and sedimentation of TEP via increasing divalent cation concentration. TEP concentration and turbidity maximum coexisted at the tip of salt wedge in the bottom layer during the wet season, and positive correlation between TEP and turbidity was observed in the winter. Relationships between TEP and turbidity suggested the important contribution of TEP aggregation to flocculation and sedimentation of particles in estuaries. Different pattern of TEP during two cruises can be attributed to physical process (i.e., mixing type) in estuaries. These findings indicated that formation and distribution of TEP were largely influenced by interaction between physical and biogeochemical processes in the Pearl River estuary. A conceptual model for TEP formation and distribution in the Pearl River estuary was developed.
机译:在2009年8月和2010年1月的两次航行中,对中国珠江河口的透明外聚合物颗粒(TEP)的分布进行了研究。TEP_(color)浓度为521.5-1727.4μgXeq.L〜(-1)(μg胶黄原胶)当量升当量)(2009年8月)和88.7-1586.9μgXeq.L〜(-1)。在航行期间,TEP的大小通常沿纵向向海增加,主要大小为2-40μm。实验工作表明,TEP的浓度和大小均随Ca〜(2+)浓度的增加而增加(从0.8 mmol L〜(-1)增加到10 mmol L〜(-1))。在田间研究中,盐度<16时,Ca〜(2+)浓度与表层TEP_(色)浓度呈正相关。中间盐度使TEP浓度向海减少的部分原因是海水稀释以及通过增加二价阳离子浓度增强了TEP的聚集和沉降。在潮湿季节,TEP浓度和浊度最大值在底层的盐楔尖端共存,并且在冬季观察到TEP与浊度呈正相关。 TEP与浊度之间的关系表明,TEP聚集对河口颗粒的絮凝和沉降具有重要作用。两次巡航期间TEP的不同模式可归因于河口的物理过程(即混合类型)。这些发现表明,TEP的形成和分布在很大程度上受到珠江口物理和生物地球化学过程之间相互作用的影响。建立了珠江口TEP形成和分布的概念模型。

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