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Comparative analyses of wetland plant biomass accumulation and litter decomposition subject to in situ warming and nitrogen addition

机译:湿地原生态加氮条件下湿地植物生物量积累与凋落物分解的比较分析

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摘要

The effects of climate warming on boreal wetland plant structure and carbon (C) sequestration on local scale may be overestimated. An in situ passive warming experiment manipulated by open-top chambers and artificial nitrogen (N) addition was deployed in a lacustrine wetland of Xingkai Lake for 3 consecutive years. The annual changes and allocations of the aboveground biomass of Glyceria spiculosa, and decomposition dynamics of the total litter and cotton strips as standard references were observed. Results showed that the aboveground biomass was significantly affected by warming and increased from 99.43 +/- 10.59 g m(-2) (ambient) to 112.02 +/- 8.08 g m(-2) (ca.+1 degrees C) and 117.21 +/- 9.92 g m(-2) (ca. +2 degrees C). N addition had a more positive effect on the annual aboveground biomass accumulations than warming, for the relative importance weights of N addition were 2.60 and 1.49 times greater than warming in 2011 and 2013 respectively. Their main effects on the allocations had significant interannual variations, and their interaction effects were dependent on organ and year. The decomposition constant (k-value) of the litter and cotton strips were 0.747 yr(-1) and 2.057 yr(-1), respectively. Compared to warming and N addition, the internal quality characterized by Lignocellulose index and soil organisms reflected by litterbag size played overwhelming role in decomposition dynamics, with 2 orders greater of relative importance weights in 2011 and 2012. Our results highlight the importance of interannual variation for differentiating the contributions of external and internal factors to boreal wetland plant biomass accumulation and decomposition. Given the asymmetric responses of accumulation and decomposition, the C storage in the litter would increase in long term. (c) 2019 Elsevier B.V. All rights reserved.
机译:气候变暖对北方湿地植物结构的影响以及当地碳(C)的固存可能被高估了。在开凯湖的湖泊湿地上连续3年进行了由开顶室和人工氮(N)操纵的原地被动增温实验。观察到蒲甘地上生物量的年度变化和分配,以及总凋落物和棉条的分解动力学作为标准参考。结果表明,地上生物量受变暖的影响很大,从99.43 +/- 10.59 gm(-2)(环境)增加到112.02 +/- 8.08 gm(-2)(约+1摄氏度)和117.21 + / -9.92 gm(-2)(约+2摄氏度)。氮的添加对年度地上生物量积累的影响大于变暖,因为添加的相对重要性权重分别是2011年和2013年变暖的2.60和1.49倍。它们对分配的主要影响有明显的年际变化,它们的相互作用影响取决于器官和年份。凋落物和棉条的分解常数(k值)分别为0.747 yr(-1)和2.057 yr(-1)。与变暖和氮添加相比,以木质纤维素指数和小袋大小反映的土壤生物为代表的内部质量在分解动力学中起着压倒性的作用,在2011年和2012年,相对重要性权重增加了2个数量级。区分外部和内部因素对北方湿地植物生物量积累和分解的贡献。考虑到积累和分解的不对称响应,垃圾中的碳储存量将长期增加。 (c)2019 Elsevier B.V.保留所有权利。

著录项

  • 来源
    《The Science of the Total Environment》 |2019年第15期|769-778|共10页
  • 作者单位

    Northeast Normal Univ Sch Environm Minist Educ State Environm Protect Key Lab Wetland Conservat Changchun 130117 Jilin Peoples R China|Northeast Normal Univ Sch Environm Minist Educ Jilin Prov Key Lab Ecol Restorat & Ecosyst Manage Changchun 130117 Jilin Peoples R China|Northeast Normal Univ Sch Environm Minist Educ Key Lab Vegetat Ecol Changchun 130117 Jilin Peoples R China|Chinese Acad Sci Northeast Inst Geog & Agroecol Key Lab Wetland Ecol & Environm Changchun 130102 Jilin Peoples R China|Chinese Acad Sci Northeast Inst Geog & Agroecol Jilin Prov Joint Key Lab Changbai Mt Wetland & Ec Changchun 130102 Jilin Peoples R China;

    Chinese Acad Sci Northeast Inst Geog & Agroecol Key Lab Wetland Ecol & Environm Changchun 130102 Jilin Peoples R China|Chinese Acad Sci Northeast Inst Geog & Agroecol Jilin Prov Joint Key Lab Changbai Mt Wetland & Ec Changchun 130102 Jilin Peoples R China|Henan Acad Sci Inst Geog Sci Zhengzhou 450052 Henan Peoples R China;

    Chinese Acad Sci Northeast Inst Geog & Agroecol Key Lab Wetland Ecol & Environm Changchun 130102 Jilin Peoples R China|Chinese Acad Sci Northeast Inst Geog & Agroecol Jilin Prov Joint Key Lab Changbai Mt Wetland & Ec Changchun 130102 Jilin Peoples R China;

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

    Global warming; Plant responses; Glyceria spiculosa; Wetland carbon balance; Xingkai Lake;

    机译:全球暖化;植物反应;香茅;湿地碳平衡;兴凯湖;

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