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High sulfide production induced by algae decomposition and its potential stimulation to phosphorus mobility in sediment

机译:藻类分解引起的高硫化物产生及其对沉积物中磷迁移率的潜在刺激

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This study is devoted to addressing the effects of algae blooms on sulfur cycle and the consequent phosphorus mobility in the sediments of freshwater lake ecosystems. A mesocosm experiment was conducted to investigate these effects through monitoring the dynamics of sulfur (S), iron (Fe) and phosphorus (P) in water and sediments, and their diffusion fluxes at the sediment-water interface (SWI). In addition, the abundance of sulfate-reducing bacteria (SRB) in the water column was also detected. The addition of the algae lead to an increase of SRB, a drastic decline of sulfate and a significant increase of total dissolved sulfide (Sigma S2-, the peak value of near 3.0 mmol/L on day 6) in thewater column. These results suggest the sulfate reduction was dramatically promoted during algae decomposition. Indeed the Sigma S2- was 2 to 3 times of SO42- initial concentration, and higher Sigma S2- was produced with higher algal biomass. Moreover, the diffusive flux of Sigma S2- at the SWI was negative, indicating that diffusion of Sigma S2- from water column toward sediment was occurring. These results indicated that algae decomposition might also be another important source of Sigma S2- (termed "algae-derived Sigma S2-") in addition to sulfate reduction. The increase of Fe(II) in surface sediment pore-water was slightly delayed compared to the Sigma S2- generation in the water column, which illustrated that Fe oxyhydroxides in sediments were transformed into Fe(II) through chemical reduction of Sigma S2-. Concomitantly, the vertical distribution of PO43- in high amounts algae group suggested that desorption and release of iron oxides-bound PO43- occurred in sediments. Collectively, algae bloom can boost the lake eutrophication not only through direct release of nutrients but also through the high production of Sigma S2- and indirect promotion of phosphorus mobility in sediment. (c) 2018 Published by Elsevier B.V.
机译:这项研究致力于解决藻类大量繁殖对硫循环的影响以及随之而来的磷在淡水湖生态系统沉积物中的迁移率。通过监测水和沉积物中硫(S),铁(Fe)和磷(P)的动力学及其在沉积物-水界面(SWI)的扩散通量,进行了介观试验以研究这些影响。另外,还检测到水柱中有大量的硫酸盐还原细菌(SRB)。藻类的添加导致水柱中SRB的增加,硫酸盐的急剧下降以及总溶解硫化物(Sigma S2-,第6天的峰值接近3.0 mmol / L)的显着增加。这些结果表明,在藻类分解过程中,硫酸盐还原作用得到了显着促进。实际上,Sigma S2-是SO42-初始浓度的2至3倍,并且更高的Sigma S2-产生的藻类生物量更高。此外,西格玛S2-在SWI处的扩散通量为负,表明西格玛S2-从水柱向沉积物扩散。这些结果表明,除硫酸盐还原外,藻类分解还可能是Sigma S2-的另一个重要来源(称为“藻类衍生的Sigma S2-”)。与水柱中Sigma S2-生成相比,地表沉积物孔隙水中Fe(II)的增加略有延迟,这表明沉积物中的Fe羟基氧化物通过Sigma S2-的化学还原转化为Fe(II)。同时,高藻类群中PO43-的垂直分布表明,沉积物中发生了铁氧化物结合的PO43-的解吸和释放。总的来说,藻类繁殖不仅可以通过直接释放养分,而且可以通过大量生产Sigma S2-和间接促进沉积物中磷的迁移来促进湖泊富营养化。 (c)2018年由Elsevier B.V.

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