首页 | 本学科首页   官方微博 | 高级检索  
     

华西雨屏区亮叶桦凋落叶分解对模拟氮沉降的响应
引用本文:涂利华,胡红玲,胡庭兴,张健,雒守华,戴洪忠. 华西雨屏区亮叶桦凋落叶分解对模拟氮沉降的响应[J]. 植物生态学报, 2012, 36(2): 99-108. DOI: 10.3724/SP.J.1258.2012.00099
作者姓名:涂利华  胡红玲  胡庭兴  张健  雒守华  戴洪忠
作者单位:四川农业大学林学院, 四川雅安 625014
长江上游林业生态工程四川省重点实验室, 成都 611130
基金项目:“国家十一五”科技支撑计划项目(2006-BAC01A11-03);“国家十二五”科技支撑计划项目(2011BAC09B05);四川农业大学“211”工程建设科技支撑计划项目共同资助
摘    要:从2008年1月至2009年2月, 对华西雨屏区亮叶桦(Betula luminifera)人工林进行了模拟氮(N)沉降试验, N沉降水平分别为对照(CK, 0 g N·m-2·a-1)、低N (5 g N·m-2·a-1)、中N (15 g N·m-2·a-1)和高N (30 g N·m-2·a-1)。利用凋落袋法对亮叶桦凋落叶进行原位分解试验, 并在每月下旬定量地对各处理施N (NH4NO3)。结果表明, 虽然华西雨屏区大气N沉降量较高, 但模拟N沉降试验表明: 在N沉降继续增加的情况下, 凋落叶分解这一碳(C)循环和养分循环过程仍会受到显著影响。在1年的分解试验中, 模拟N沉降显著抑制了亮叶桦凋落叶的分解, N沉降处理使得凋落叶质量损失95%的时间在2.65年的基础上增加了1.14-1.96年。N沉降抑制凋落叶分解的原因在于无机N的富集对木质素和纤维素的分解造成阻碍。N沉降处理也导致C、N、磷、钾和镁元素在凋落物中的残留量增加, 但N沉降加速了钙元素的释放。凋落物基质化学特性在很大程度上决定了凋落物分解对N沉降的响应方向, 以及凋落物分解过程中各元素的动态变化。

关 键 词:亮叶桦  凋落叶分解  氮沉降  养分动态  华西雨屏区  
收稿时间:2011-11-23
修稿时间:2012-01-12

Response of Betula luminifera leaf litter decomposition to simulated nitrogen deposition in the Rainy Area of West China
TU Li-Hua , HU Hong-Ling , HU Ting-Xing , ZHANG Jian , LUO Shou-Hua , DAI Hong-Zhong. Response of Betula luminifera leaf litter decomposition to simulated nitrogen deposition in the Rainy Area of West China[J]. Acta Phytoecologica Sinica, 2012, 36(2): 99-108. DOI: 10.3724/SP.J.1258.2012.00099
Authors:TU Li-Hua    HU Hong-Ling    HU Ting-Xing    ZHANG Jian    LUO Shou-Hua    DAI Hong-Zhong
Affiliation:College of Forestry, Sichuan Agricultural University, Ya’an, Sichuan, 625014, China
Sichuan Provincial Key Laboratory of Forestry Ecological Engineering in Upper Reaches of Yangtze River, Chengdu 611130, China
Abstract:Aims Our objective was to determine the effect of simulated increased nitrogen (N) deposition on decomposition of Betula luminifera leaf litter, under a high wet-nitrogen deposition background.
Methods From January 2008 to February 2009, a field experiment of simulated N deposition was conducted in a B. luminifera plantation in the Rainy Area of West China. The levels of nitrogen deposition were control (CK), low, medium and high N (0, 5, 15 and 30 g N·m–2·a–1, respectively). A field experiment using the litterbag method was conducted on the decomposition of leaf litter of B. luminifera. In the end of each month, NH4NO3 was added into N-treated plots.
Important findings Despite the high background N deposition, there were significant effects of simulated increased N deposition on B.luminifera leaf litter. N treatments significantly slowed the decomposition of B. luminifera leaf litter through inhibiting the decay of lignin and cellulose. The time of 95% mass loss (T95%) of B. luminifera leaf litter was increased by 1.14–1.96 a from 2.65 a (T95% of CK) caused by simulated N deposition. Simulated N deposition significantly increased the remaining amount of carbon, N, phosphorus, potassium, and magnesium after one year of decomposition. However, calcium release rate was stimulated by simulated N deposition in all three N treatments. The initial chemical characteristics of litter determined the response direction of litter decomposition to simulated N deposition, as well as the nutrient release pattern during litter decomposition.
Keywords:Betula luminifera  leaf litter decomposition  nitrogen deposition  nutrient dynamics  Rainy Area of West China
本文献已被 CNKI 万方数据 等数据库收录!
点击此处可从《植物生态学报》浏览原始摘要信息
点击此处可从《植物生态学报》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号