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首页> 外文期刊>Journal of Environmental Quality >Denitrification potential and organic matter as affected by vegetation community, wetland age, and plant introduction in created wetlands
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Denitrification potential and organic matter as affected by vegetation community, wetland age, and plant introduction in created wetlands

机译:受植被群落,湿地年龄和人工湿地植物引进影响的反硝化潜能和有机质

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摘要

Denitrification potential (DP) and organic matter (OM) in soils were compared in three different vegetation communities-emergent macrophyte, open water, and forested edge-in two 10-yr-old created riverine wetlands. Organic matter, cold water-extractable organic matter (CWEOM), anaerobic mineralizable carbon (AnMC), and DP varied significantly (P<0.05) among vegetation communities. The surface (0 to 9 cm) soils in the emergent macrophyte community (EMC) showed highest DP (0.07+/-0.01 mg N h-1 kg-1), OM (84.90+/-5.60 g kg-1), CWEOM (1.12+/-0.20 g kg-1), and AnMC (1.50+/-0.10 mg C h-1 kg-1). In the deeper layer (9 to 18 cm), DP and CWEOM (0.04+/-0.01 mg N h-1 kg-1 and 1.13+/-0.20 g kg-1, respectively) were significantly higher in the open water community (OWC) than in the emergent macrophyte and forested edge communities. Plant introduction did not affect DP or OM content and characteristics. After 10 yr of wetland development, mean DP increased 25-fold in the surface layer (from 0.002 to 0.053 mg N h-1 kg-1); OM content more than doubled to 90.80+/-19.22 g kg-1, and CWEOM and HWEOM increased 2.5 and 2.7 times respectively from 1993 (prewetland conditions) to 2004. Humic acids were the most abundant form of OM in 2004 and 1993 samples. Significant (P<0.05) positive relationships between DP and OM, CWEOM, and AnMC were found in the surface layer; in the 9- to 18-cm layer, significant positive relationships were found between DP and CWEOM and AnMC.
机译:在两个10岁的河流湿地中,比较了三种不同的植被群落(新兴的大型植物,开放水域和森林边缘)中土壤的反硝化潜能(DP)和有机质(OM)。植被群落中有机质,冷水可提取有机质(CWEOM),厌氧可矿化碳(AnMC)和DP差异显着(P <0.05)。新兴大型植物群落(EMC)的表层土壤(0至9 cm)表现出最高DP(0.07 +/- 0.01 mg N h-1 kg-1),OM(84.90 +/- 5.60 g kg-1),CWEOM (1.12 +/- 0.20 g kg-1)和AnMC(1.50 +/- 0.10 mg C h-1 kg-1)。在更深的层(9至18 cm)中,开放水域的DP和CWEOM(分别为0.04 +/- 0.01 mg N h-1 kg-1和1.13 +/- 0.20 g kg-1)显着更高( OWC)比出现的大型植物和森林边缘群落中的数量高。引入植物不会影响DP或OM的含量和特性。湿地发展10年后,平均DP在表层增加了25倍(从0.002到0.053 mg N h-1 kg-1)。 OM含量增加了一倍以上,达到90.80 +/- 19.22 g kg-1,CWEOM和HWEOM从1993年(前湿地条件)到2004年分别增加了2.5倍和2.7倍。腐殖酸是2004年和1993年样品中OM含量最高的形式。在表面层中发现DP与OM,CWEOM和AnMC之间存在显着(P <0.05)的正相关关系。在9至18厘米的层中,DP与CWEOM和AnMC之间发现了显着的正相关。

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