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Long-term phosphorus addition enhances the biodegradability of dissolved organic carbon in a nitrogen-limited temperate freshwater wetland

机译:长期添加磷提高了氮限制的温带淡水湿地中溶解有机碳的生物降解能力

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摘要

Phosphorus (P) enrichment is expected to strongly influence dissolved organic carbon (DOC) biodegradation. However, the relationship between P availability and DOC biodegradation is largely unknown in nitrogen (N)-limited ecosystems. Here, we investigated the changes in the ratio of DOC to dissolved total nitrogen (DTN), specific UVabsorbance at 254 nm (SUVA_(254)), and DOC biodegradation in surface water and soil pore water (0-15 cm depth) following eight years of multi-level P addition (0,1.2,4.8, and 9.6 g P m~(-2) year~(-1)) in an N-limited freshwater marsh in Northeast China. We found that P addition caused an increase in DOC biodegradation in surface water and soil pore water, irrespective of the P addition levels. Compared with the control treatment the P addition rates of 12,4.8, and 9.6 g P m~(-2) year~(-1) increased DOC biodegradation by 20.7%, 15.2%, and 14.5% in surface waters, and 11.3%, 9.4%, and 12.0% in soil pore waters, respectively. The DOC biodegradation was separately negatively correlated with the DOCDTN ratio and SUVA254, indicating that the positive effect of P addition on DOC biodegradation was caused by the elevated N concentration and the reduced DOC aromaticity. Our findings suggest that P enrichment enhances the biodegradability of DOC through increased N availability and altered DOC chemical composition, which would accelerate DOC loss from the waters and alter ecosystem C balance in N-limited temperate wetlands.
机译:磷(P)的富集预计会强烈影响溶解有机碳(DOC)的生物降解。但是,在氮(N)受限的生态系统中,磷的有效性与DOC生物降解之间的关系在很大程度上是未知的。在这里,我们研究了以下八种条件下DOC与溶解的总氮(DTN)的比率,254 nm处的特定紫外线吸收率(SUVA_(254))以及地表水和土壤孔隙水(0-15厘米深)中DOC的生物降解的变化。东北N限制的淡水沼泽中多年磷的添加量(0、1.2、4.8和9.6 g P m〜(-2)年〜(-1))。我们发现,磷的添加导致地表水和土壤孔隙水中DOC生物降解的增加,而与磷的添加量无关。与对照相比,磷的添加量分别为12,4.8和9.6 g P m〜(-2)年〜(-1),地表水中的DOC生物降解分别增加了20.7%,15.2%和14.5%,以及11.3%在土壤孔隙水中分别为9.4%和12.0%。 DOC的生物降解分别与DOCDTN比和SUVA254呈负相关,表明P添加对DOC的生物降解的积极影响是由氮浓度升高和DOC芳香度降低引起的。我们的发现表明,磷的富集通过增加氮的利用率和改变DOC的化学成分来增强DOC的生物降解性,这将加速DOC从水域的流失,并改变氮有限的温带湿地中的生态系统C平衡。

著录项

  • 来源
    《The Science of the Total Environment》 |2017年第15期|332-336|共5页
  • 作者单位

    Key Laboratory of Wetland Ecology and Environment, Northeast Institute o/Geography and Agroecology, Chinese Academy of Sciences, Changchun 130102, China,The Three Gorges Institute of Ecological Environment, Chongqing Institute of Green and Intelligent Technology, Chinese Academy of Sciences, Chongqing 400714, China;

    Key Laboratory of Wetland Ecology and Environment, Northeast Institute o/Geography and Agroecology, Chinese Academy of Sciences, Changchun 130102, China;

    The Three Gorges Institute of Ecological Environment, Chongqing Institute of Green and Intelligent Technology, Chinese Academy of Sciences, Chongqing 400714, China;

    Key Laboratory of Wetland Ecology and Environment, Northeast Institute o/Geography and Agroecology, Chinese Academy of Sciences, Changchun 130102, China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Stoichiometry; Carbon cycle; Carbon dioxide; Decomposition Eutrophication; Marsh;

    机译:化学计量;碳循环;二氧化碳;分解富营养化;沼泽;

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