Sources of Enrichment of Dissolved Free and Combined Amino Acids in the Sea Surface Microlayer

海表微层中溶解的游离氨基酸和结合氨基酸的富集来源

• 批准号: 0117208
• 负责人: Cindy Lee
• 金额: $ 30.02万
• 依托单位: SUNY at Stony Brook
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2001
• 资助国家: 美国
• 起止时间: 2001-10-01 至 2005-09-30
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0117208&HistoricalAwards=false
• 关键词: Sources; Enrichment; Dissolved; Free; Combined; Sources; Enrichment; Dissolved; Free; Combined

ABSTRACTOCE-0117208In this study, researchers at the State University of New York at Stony Brook will attempt to identify and describe the various processes that lead to the enrichment of dissolved organic matter in the sea-surface microlayer. The sea-surface microlayer plays a major role in the exchange of matter and energy in the ocean-atmosphere system. Organic matter enriches the surface microlayer and influences its chemical, biological, and physical characteristics. Different constituents concentrate in the microlayer non-uniformly; consequently, the ratios of many dissolved elements and organic compounds therein differ from those in bulk water. These studies will focus on the transfer of dissolved free and combined amino acids between particulate and dissolved pools under the unique conditions of the interfacial laminar layer. A number of factors will be considered: increased physical stress on the biological community at the sea surface (e.g., by UV-radiation, evaporation, entrapment in spray), which causes leaching of organic matter from the resulting dead or injured organisms; dissolved organic matter decomposition by metabolically active neuston (hydrolysis, oxidation, and uptake); adsorption of dissolved matter onto particles which in the microlayer; and bubble scavenging from bulk water to the surface microlayer of proteinaceous matter that is dissolved or weakly associated with particles.

Abstractoce-0117208在这项研究中，纽约州立大学Stony Brook大学的研究人员将试图识别和描述导致Sea-Torface Microlayer中溶解有机物富集的各种过程。海面微层层在海洋 - 大气系统中的物质和能量交换中起着重要作用。 有机物丰富了表面的微层，并影响其化学，生物学和物理特征。 不同的成分不均匀地集中在微层中；因此，其中许多溶解元件和有机化合物的比率与大量水的比率不同。 这些研究将集中于在界面层状层的独特条件下，溶解的游离和合并氨基酸在颗粒和溶解的池之间的转移。 将考虑许多因素：增加海面生物群落的身体压力增加（例如，通过紫外线辐射，蒸发，喷雾中的夹带），从而导致从最终的死亡或受伤的生物体中浸出有机物； 溶解有机物分解，代谢活跃的Neuston（水解，氧化和摄取）；溶解的物质吸附到微层中的颗粒上；气泡从散装水清除到蛋白质物质的表面微层，这些物质溶解或与颗粒薄弱相关。