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Fluff deposition on intertidal sediments: effects on benthic biota, ammonium fluxes and nitrification rates

机译:潮间带沉积物上的绒毛沉积:对底栖生物群,铵通量和硝化速率的影响

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摘要

The effects of fluff deposit on benthic biota, NH4+ fluxes and nitrification was studied in the laboratory using waterlogged and reflooded intertidal sediments from Marennes-Oleron Bay, France. The fluff deposit was enriched in NH4+ compared to underlying sediments, and promoted changes of the sediment pH, E-h, C:N ratio, C:chl a ratio and the NH4+ efflux to overlying water. Statistical analysis showed that pore water NH4+ concentrations were strongly influenced by interactions between fluff, drying, depth and bioturbation. The fluff deposit resulted in anoxia in the top sediments and moved the nitrification zone to surface layers in fluff. However, the NH4+ enrichment in fluff did not significantly change actual nitrification rates (range 0-1 mmol m(-2) d(-1)) or potential nitrification rates (range 3-11 mmol NO3- m(-2) d(-1)).
机译:在实验室中,使用法国Marennes-Oleron湾的涝渍和再潮汐潮汐沉积物研究了绒毛沉积物对底栖生物,NH4 +通量和硝化的影响。与下面的沉积物相比,绒毛沉积物富含NH4 +,并促进了沉积物pH,E-h,C:N比,C:chl a比和NH4 +向上覆水的流出的变化。统计分析表明,毛孔,干燥,深度和生物扰动之间的相互作用对孔隙水中NH4 +的浓度影响很大。绒毛沉积物在顶部沉积物中导致缺氧,并使硝化区移动到绒毛的表层。但是,绒毛中的NH4 +富集不会显着改变实际硝化速率(0-1 mmol m(-2)d(-1))或潜在的硝化速率(3-11 mmol NO3- m(-2)d( -1))。

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