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Short-term effect of oxic to anoxic transition on benthic microbial activity and solute fluxes in organic-rich phytotreatment ponds

机译:有氧-无氧过渡对富有机处理池中底栖微生物活性和溶质通量的短期影响

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Manipulative experiments to test the short-term effect of oxygen depletion events on microbial activity and benthic fluxes in organic-rich sediments were carried out in March and June 2004. Oxic–anoxic transitions were induced by prolonged dark incubation of sealed sediment cores collected in phytotreatment ponds. Benthic fluxes of oxygen (O2), carbon dioxide (CO2), inorganic nutrients, and free sulfides were measured before (oxic) and after (anoxic) the transition occurred. A multifactorial design was employed for monitoring esoenzymatic activity, heterotrophic bacterial production, total prokaryotic abundance, actively respiring bacterial cells, and the biochemical composition of sedimentary organic matter. The oxic to anoxic transition resulted in a significant increase of esoenzymatic activity and bacterial production in March, due to the profound modification of the benthic community and the release of labile organic compounds which followed the onset of anoxia. In parallel, net efflux rates of dissolved inorganic carbon (DIC) and ammonium (NH4 +) sharply decreased, soluble reactive phosphorus (SRP) influx reversed, and sulfide was buffered within the oxidized sediments. From March to June, ponds evolved toward oxygen deficit and reducing conditions in the upper sediment horizon, losing benthic fauna and biogeochemical buffering capacity. Thus, the oxic to anoxic transition had a much smaller effect on microbial activity and net flux exchange, while S2− was consistently delivered from the sediment to the water column. Overall data from this study suggest that the short-term response of benthic microbial activity and solute fluxes to anoxic events may have a significant impact on sediment biogeochemistry (e.g., at the oxic–anoxic interface), and that this impact may vary greatly depending on the sediment features, mainly its organic content and redox condition. Keywords Oxic–anoxic transition - Microbial activity - Solute fluxes - Organic-rich sediments - Biogeochemical buffers - Eutrophication Guest editors: J. H. Andersen & D. J. Conley Eutrophication in Coastal Ecosystems: Selected papers from the Second International Symposium on Research and Management of Eutrophication in Coastal Ecosystems, 20–23 June 2006, Nyborg, Denmark
机译:在2004年3月和2004年6月进行了操纵实​​验,以测试耗氧事件对富含有机物的沉积物的微生物活性和底流的短期影响。通过长时间暗藏在植物处理中的密封沉积物核,可引起氧-氧过渡。池塘。在发生过渡之前(有氧)和之后(缺氧)测量了氧气(O 2 ),二氧化碳(CO 2 ),无机养分和游离硫化物的底通量。采用多因素设计来监测酶活性,异养细菌的产生,原核生物的总丰度,主动呼吸细菌的细胞以及沉积有机物的生化组成。由于底栖动物群落的深刻改变和缺氧发生后不稳定有机化合物的释放,从有氧到无氧的转变在三月导致了酶活性和细菌产量的显着增加。同时,溶解的无机碳(DIC)和铵(NH 4 + )的净流出速率急剧下降,可溶性反应性磷(SRP)流入逆转,硫化物被缓冲在氧化的沉积物中。从3月到6月,池塘向着缺氧状态发展,并在沉积物上层水平降低了条件,失去了底栖动物区系和生物地球化学缓冲能力。因此,从有氧到无氧的转变对微生物活性和净通量交换的影响要小得多,而S 2-始终如一地从沉积物中输送到水柱。这项研究的总体数据表明,底栖微生物活性和溶质通量对缺氧事件的短期响应可能会对沉积物的生物地球化学产生重大影响(例如,在有氧-缺氧界面),并且这种影响可能会因沉积物的特征,主要是其有机物含量和氧化还原条件。关键词氧-氧过渡-微生物活性-溶质通量-富含有机物的沉积物-生物地球化学缓冲液-富营养化客座编辑:JH Andersen&DJ Conley沿海生态系统富营养化:选自第二届国际沿海生态系统富营养化研究与管理研讨会,2006年6月20日至23日,丹麦尼堡

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