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PHOTODEGRADATION OF DISSOLVED ORGANIC CARBON IN HUMIC COASTAL LAGOONS(RJ,BRAZIL)

机译:腐殖沿线泻湖溶解有机碳的光降解(RJ,巴西)

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Dissolved organic carbon(DOC)accounts for most of the carbon in lakes and represents a dynamic link between the geosphere,the hydrosphere and the biosphere(Graneli et al.,1998).Heterotrophic bacteria are the major consumers of DOC,reintroducing it into the food web through the microbial loop(Azam et al.,1983).DOC is composed mainly by humic substances in the majority of aquatic ecosystems(Thomas,1997).Due to their biologically refractory nature,these substances acumulate in aquatic ecosystems,unless other processes remove them from the water.Sunlight oxidize DOC directly to CO_2 or break it down into smaller molecules,generally labile bacterial substrates(Moran & Zepp,1997).This process of photodegradation enhances the removal of refractory DOC(i.e.humic substances)from aquatic ecosystems through 1)direct mineralization(photo-oxidation)and 2)increase in the bacterial consumption and consequent respiration(Graneli et al.,1998).Thus,any attempt to understand the interaction of light,DOC and bacteria in humic aquatic ecosystems,assumes a great importance for the understanding of the carbon cycle and ecological functioning of these ecosystems.
机译:溶解有机碳(DOC)占湖泊中大部分碳的账户,代表了地球圈,水液和生物圈之间的动态联系(Graneli等,1998)。Herterotrophic细菌是Doc的主要消费者,将其重新引入食物纤维网通过微生物环(Azam等,1983).doc主要由大多数水生生态系统(托马斯,1997)中的腐殖质。它们在其生物难治性的本质上,这些物质致致水生态系统,除非其他方法将它们从水中移除。灯光将DOC直接氧化至CO_2或将其分解为较小的分子,通常是不稳定的细菌基材(MORAN&Zepp,1997)。光电降解过程增强了从水生去除难熔官僚(Ihumic物质)的过程通过1)生态系统通过1)直接矿化(光氧化)和2)细菌消耗和随后的呼吸(Graneli等,1998).thus,任何理解光的相互作用,Doc和腐殖液水生生态系统的细菌非常重视了解这些生态系统的碳循环和生态功能。

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