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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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The effects of fluff deposit on benthic biota,NH4 + fluxes and nitrification was studied in thelaboratory using waterlogged and reflooded intertidal sediments fromMarennes-Oléron Bay, France. The fluff deposit was enriched inNH4 + compared to underlying sediments, and promotedchanges of the sediment pH, Eh, C:N ratio, C:chla ratio and the NH4 + efflux tooverlying water. Statistical analysis showed that pore waterNH4 + concentrations were strongly influenced byinteractions between fluff, drying, depth and bioturbation. The fluff depositresulted in anoxia in the top sediments and moved the nitrification zone tosurface layers in fluff. However, the NH4 + enrichment influff did not significantly change actual nitrification rates (range 0–1mmol m−2 d−1) or potentialnitrification rates (range 3–11 mmolNO3 − m−2d−1).
机译:在实验室中,使用法国Marennes-Oléron湾的涝渍和潮洪潮间带沉积物研究了绒毛沉积物对底栖生物,NH4 + 通量和硝化作用的影响。与下层沉积物相比,绒毛沉积物富含NH4 + ,并促进了沉积物pH,Eh ,C:N比,C:chla比和NH4 +的变化。 外溢到上层水。统计分析表明,孔隙水NH4 + 的浓度受绒毛,干燥,深度和生物扰动之间相互作用的强烈影响。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,NH4 + 富集涌入并未显着改变实际硝化速率(范围为0–1mmol m-2 d-1 )或潜在的硝化速率(范围为3-11) mmolNO3 - m-2 d-1 )。

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