Characterization of colloids before, during, and after a phytoplanktonic bloom in Lake Geneva (Switzerland/France)

V. Chanudet, J. Loizeau, J. Druart, Régis Kottelat, D. Vignati, J. Dominik
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Abstract

Colloids play an important role in trace metal cycling in lakes(Morel & Gschwend 1987) due to their high sorptioncapacity and long residence times. Indeed, because of Brow-nian motion, colloids do not settle individually, even in stillwater; however, they can aggregate into larger particles andstart to settle entraining bound or embedded compounds.Aggregation, and ultimately colloid removal rates, canstrongly be enhanced during a phytoplankton bloom, particu-larly through the production of sticking exopolymers (Pas-sow 2002) released by phytoplankton (Jackson & Burd1998). Sticking exopolymers are also known to promote dia-tom aggregation in both marine (Alldregde & Jackson1995 and other references in this special issue) and freshwa-ter systems (Hoffman et al. 2001).In an international project aiming to assess trace metalremoval in Lake Geneva during a phytoplanktonic bloom,colloids were extensively studied during 3field campaignsbefore, during, and after the 2006 spring bloom. Changes insize, concentration, composition, and aggregation rate of col-loids with time will be extensively presented elsewhere (V.Chanudet, unpubl.). Here we present specifically the resultsof the second campaign (bloom), in which phytoplankton wasexpected to most influence the colloidal particle size distri-bution and play a significant role in the aggregation process.To verify this assumption, we carried out experiments on col-loid aggregation using a single particle counter (SPC), aunique tool allowing measurements of colloids in the sizerange 0.1–2µm at natural concentrations. We were able todemonstrate that during an early phase of bloom in lakes,small centric diatoms settle individually rather than as aggre-gates, possibly because of a low concentration of exopoly-mers.
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日内瓦湖浮游植物爆发前、期间和之后胶体的特征(瑞士/法国)
胶体由于其高吸附能力和长停留时间,在湖泊中痕量金属循环中起着重要作用(Morel & Gschwend 1987)。事实上,由于布朗运动,胶体不会单独沉降,即使在静水中也是如此;然而,它们可以聚集成更大的颗粒,并开始沉淀夹带或嵌入的化合物。在浮游植物繁殖期间,聚集和最终的胶体去除率可以大大提高,特别是通过浮游植物释放的粘性外聚合物(pass -sow 2002)的产生(Jackson & Burd1998)。众所周知,黏附的外聚合物也会促进海洋系统(Alldregde & Jackson1995以及本期特刊中的其他参考文献)和淡水系统(Hoffman et al. 2001)中的硅藻聚集。在一个旨在评估日内瓦湖浮游植物水华期间微量金属去除情况的国际项目中,在2006年春季水华之前、期间和之后的3次实地活动中,对胶体进行了广泛的研究。胶体的大小、浓度、组成和聚集速率随时间的变化将在其他地方广泛介绍(v.c anudet, unpubl.)。在这里,我们特别提出了第二个运动(开花)的结果,其中浮游植物被认为对胶体粒度分布的影响最大,并在聚集过程中发挥重要作用。为了验证这一假设,我们使用单颗粒计数器(SPC)进行了胶体聚集实验,SPC是一种独特的工具,可以测量自然浓度下0.1-2 μ m大小的胶体。我们能够证明,在湖泊水华的早期阶段,小的中心硅藻单独定居,而不是聚集在一起,可能是因为低浓度的外聚体。
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