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Changes in size distribution of fresh water nanoscale colloidal matter and associated elements on mixing with seawater

机译:与海水混合时淡水纳米胶体及相关元素的尺寸分布变化

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Changes in size distribution and elemental composition of 0.5-50 nm fresh water colloids during estuarine mixing have been studied by in-laboratory mixing of natural creek water and synthetic seawater, followed by size fractionation with Asymmetrical Flow Field-Flow Fractionation, and online elemental quantification by High-Resolution ICPMS. At least two types of colloids were present in the studied size region; 0.5-3 nm fluorescent dissolved organic matter (FDOM), and >3 nm colloids that were rich in Fe and colored dissolved organic matter (CDOM). Most trace elements were associated in different proportions to these two populations of colloids. Following mixing with synthetic seawater, the >3 nm. Fe-rich colloids and CDOM were extensively removed from the studied size region by salt induced aggregation. The degree of removal with increasing salinity was greatest below 2.5 parts per thousand. salinity, continued to a lesser degree between 2.5%. and 15 parts per thousand. salinity, above which only very small additional removal could be distinguished. At 25 parts per thousand. salinity, the Fe concentration in the 0.5-50 size region had been reduced down to 15% of its original value in freshwater, while the amount of CDOM had been reduced to 55%. On the contrary, the concentration of the 0.5-3 run FDOM was unchanged by the increased concentration of sea salt. Therefore, colloidally associated Al, P, Co, Cu, Zn, Ce, Lu and Ph were removed from the 0.5-50 nm size region according to their relative distributions between the FDOM and the Fe-rich colloids. Consequently, at 25 parts per thousand. salinity, the 0.5-50 nm concentrations of Al, Mn, P and Pb, (mainly associated with the Fe-rich colloids) had been reduced down to 13-26% of their values in freshwater, while the concentrations of Co and Cu (with higher preferences for FDOM) were less reduced, down to 46% and 57%, respectively. Changes in the elemental composition of the remaining colloidal matter were observed, the most pronounced were increased contents of P, A] and Pb in Fe-rich colloidal matter of medium size (similar to 3-15 nm) and increased Pb content in Fe-rich colloidal matter of larger size (similar to 5-50 nm). (c) 2007 Elsevier Ltd. All rights reserved.
机译:河口混合过程中,通过在实验室内混合天然小溪水和合成海水,然后通过不对称流场-流分馏进行大小分级分离和在线元素定量研究了0.5-50 nm淡水胶体的粒度分布和元素组成的变化。由高分辨率ICPMS提供。在研究的大小区域中至少存在两种​​类型的胶体。 0.5-3 nm的荧光溶解有机物(FDOM)和> 3 nm的胶体,其中富含Fe和有色溶解有机物(CDOM)。大多数痕量元素以不同比例与这两个胶体种群相关。与合成海水混合后,> 3 nm。通过盐诱导的聚集将富铁胶体和CDOM从研究的大小区域中广泛去除。盐度增加时,去除程度最大,低于千分之2.5。盐度在2.5%之间持续较小程度。和千分之十五。盐度,在此之上只能分辨出很小的额外去除量。千分之二十五。在盐度下,0.5-50尺寸区域中的铁浓度已降低至淡水原始值的15%,而CDOM的含量已降至55%。相反,随着海盐浓度的增加,0.5-3游程FDOM的浓度保持不变。因此,根据FDOM和富铁胶体之间的相对分布,从0.5-50 nm尺寸区域中去除了与胶体相关的Al,P,Co,Cu,Zn,Ce,Lu和Ph。因此,千分之二十五。在盐度方面,淡水中Al,Mn,P和Pb的0.5-50 nm浓度(主要与富铁胶体有关)已降低至其值的13-26%,而Co和Cu(对FDOM具有较高偏好的用户减少的幅度较小,分别降至46%和57%。观察到剩余胶体物质元素组成的变化,最明显的是中等尺寸(约3-15 nm)的富铁胶体中P,A]和Pb的含量增加,而Fe-较大尺寸(类似于5-50 nm)的富胶体物质。 (c)2007 Elsevier Ltd.保留所有权利。

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