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Temporal changes and spatial variation of soil oxygen consumption, nitrification and denitrification rates in a tidal salt marsh of the Lagoon of Venice, Italy

机译:意大利威尼斯泻湖潮汐盐沼中土壤耗氧量,硝化和反硝化速率的时空变化

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摘要

The aim of the present study was to investigate seasonal and spatial patterns of soil oxygen consumption, nitrification, denitrification and fluxes of dissolved inorganic nitrogen (DIN) in a tidal salt marsh of the Lagoon of Venice, Italy. In the salt marsh, intact soil cores including overlying water were collected monthly at high tide from April to October in salt marsh creeks and in areas covered by the dominant vegetation, Limonium serotinum. In May, cores were also collected in areas with vegetation dominated by Juncus maritimus and Halimione portulucoides. In laboratory incubations at in situ temperature in the dark, flux rates of oxygen and DIN were monitored in the overlying water of the intact cores. ~(15)N-nitrate was added to the overlying water and nitrification and denitrification were measured using isotope-dilution and -pairing techniques. The results show that highest soil oxygen consumption coincided with the highest water temperature in June and July. The highest denitrification rates were recorded in spring and autumn coinciding with the highest nitrate concentrations. Soil oxygen consumption and nitrification rates differed between sampling sites, but denitrification rates were similar among the different vegetation types. The highest rates were recorded in areas covered with L. serotinum. Burrowing soil macrofauna enhanced oxygen consumption, nitrification and denitrification in April and May. The data presented in this study indicate high temporal as well as spatial variations in the flux of oxygen and DIN, and nitrogen transformations in the tidal salt marshes of the Venice lagoon during the growth season. The results identify the salt marshes of the Venice lagoon as being metabolically very active ecosystems with a high capacity to process nitrogen.
机译:本研究的目的是调查意大利威尼斯泻湖潮汐盐沼中土壤耗氧量,硝化作用,反硝化作用和溶解性无机氮通量的季节性和空间格局。在盐沼中,从4月到10月,在涨潮时每月在盐沼小河以及优势植被Serotinum覆盖的地区收集完整的土壤核心,包括上覆水。 5月,还在以海马草(Juncus maritimus)和哈密欧内(halimione portulucoides)为主的植被区域收集了岩心。在黑暗中原位温度下的实验室温育中,在完整芯的上层水中监测氧气和DIN的通量速率。将〜(15)N硝酸盐添加到上层水中,并使用同位素稀释和配对技术测量硝化和反硝化作用。结果表明,最高的土壤耗氧量与6月和7月的最高水温相吻合。春季和秋季记录的最高反硝化率与最高硝酸盐浓度一致。不同采样点的土壤耗氧量和硝化率不同,但不同植被类型的反硝化率相似。最高感染率出现在丝状乳杆菌覆盖的区域。在4月和5月,挖土大型动物会增加耗氧量,硝化作用和反硝化作用。在这项研究中提供的数据表明,在生长季节中,威尼斯泻湖的潮汐盐沼中的氧气和DIN的通量以及氮的转化在时间和空间上都存在很大的变化。结果表明,威尼斯泻湖的盐沼是代谢活跃的生态系统,具有很高的处理氮的能力。

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