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NITRIFICATION IN STREAM SEDIMENT BIOFILMS THE ROLE OF AMMONIUM CONCENTRATION AND DOC QUALITY

机译:沉积物生物膜中的硝化作用-铵浓度和DOC质量的作用

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Nitrification was shown to be important in the nitrogen cycle of intact streambed sediment from the Mediterranean stream La Solana, Spain. We employed sediment biofilm reactors (SBR) with a continuous throughflow of water and solutes and used the one-dimensional advection-dispersion and transformation model to simulate SBR output ammonium and nitrate concentrations. An average input nitrogen flux of l.7pg NH4.-Nmin-1' saturated ammonium retention in streambed sediments. Nitrification rates ranged between 4 and 20 ng Nmin-1 g-1 dry mass sediment and its efficiency amounted 85. In order to better understand the coupled effect of both nitrogen and carbon cycles in stream sediments. we performed simultaneous and successive glucose,ammonium additions. In this experiments, nitrification efficiency decreased to 31-45. We `present first evidence, that pulses of highly available carbon can shift the microbial biofilm community from predominantly chemoautotrophy to predominantly heterotrophy in the La Solana streambed. Under these conditions. heterotrophic bacteria can potentially compete for ammonium with nitnfiers.
机译:研究表明,硝化作用在来自西班牙拉索拉纳河的完整河床沉积物的氮循环中很重要。我们使用具有连续水和溶质通流的沉积物生物膜反应器(SBR),并使用一维对流扩散和转化模型来模拟SBR输出的铵和硝酸盐浓度。流化沉积物中平均输入氮通量为1.7pg NH4-Nmin-1'饱和铵保留量。硝化速率介于4至20 ng Nmin-1 g-1干物质沉积物之间,其效率总计为85。为了更好地了解氮和碳循环在河流沉积物中的耦合作用。我们同时和连续进行葡萄糖,铵的添加。在此实验中,硝化效率降至31-45。我们提供了第一个证据,即高可用碳的脉冲可以使流经的La Solana的微生物生物膜群落从主要的化学自养作用转变为主要的异养作用。在这些条件下。异养细菌可能会与硝化细菌竞争铵离子。

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