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[模拟湿地水位变化对小叶章凋落物分解及氮动态的影响]

[Effects of simulated wetland water change on the decomposition and nitrogen dynamics of Calamagrostis angustifolia litter].

作者信息

Sun Zhi-gao, Liu Jing-shuang, Yu Jun-bao, Qin Sheng-jin

机构信息

Yantai Institute of Coastal Zone Research for Sustainable Development, Chinese Academy of Sciences, Yantai 264003, China.

出版信息

Huan Jing Ke Xue. 2008 Aug;29(8):2081-93.

Abstract

From May 2005 to September 2006, the potential effects of wetland water change on the decomposition and nitrogen (N) dynamics of the typical meadow Calamagrostis angustifolia (TMC) and marsh meadow C. angustifolia (MMC) litters were studied by litterbag technique in the typical depressional wetland in the Sanjiang Plain. In this study, the natural water gradient in the depressional wetland was applied to simulate the changes of wetland water conditions, and six decomposition sub-zones were laid in turn in the six communities, Carex pseudocuraica (PF), Carex lasiocarpa (MG), Carex meyeriana (WL), Marsh meadow C. angustifolia (XII), Typical meadow C. angustfolia (XI), and Island forest (DZL), along the water gradient. The results show that water condition has significant effects on the decomposition of litters. If the hydrous environment is formed in C. angustfolia wetland due to the change of precipitation pattern in the future, the litter weightless rates of TMC and MMC will increase 4.33%-16.76% and 24.84%-53.97%, the decomposition rates will increase 10.51%-32.73% and 77.85%-93.92%, and the 95% decomposition time will decrease 0.72-1.85 a and 3.67-4.05 a, respectively. The changes of N contents and N accumulation indices of TMC and MMC litters are relatively consistent, but the change patterns indifferent sub-zones are different. In general, the N in litters in DZL, XI, WL, MG and PF sub-zones show the alternant change characteristics of release and accumulation, but the release process is predominated. In contrast with that, the N in litters in XII sub-zone show release at all times. The C/N ratios have important regulation functions to the changes of N in litters in decomposition process. The estimation results show that the N standing crops of TMC and MMC litters are 12.75 g x m(-2) and 8.29 g x m(-2), and the N annual returning amounts are larger than 1.95 g x (m2 x a)(-1) and 2.25 g x (m2 x a)(-1), respectively. The studies of affecting factors indicate that temperature has promotion effects on the relative decomposition rates of litters, while water condition has restraint effects on them. Further analysis shows that the relative decomposition rates, to some extent, depend on the substrate quality of litters if the nutrient status of decomposition environment does not change greatly. In reverse, if the nutrient status of decomposition environment changes greatly, the relative decomposition rates, to some extent, depend on the supply status of nutrient in decomposition environment.

摘要

2005年5月至2006年9月,运用凋落物袋技术,在三江平原典型洼地湿地研究了湿地水分变化对典型草甸小叶章(TMC)和沼泽草甸小叶章(MMC)凋落物分解及氮(N)动态的潜在影响。本研究利用洼地湿地的自然水分梯度来模拟湿地水分条件的变化,沿着水分梯度在漂筏苔草(PF)、毛果苔草(MG)、狭叶甜茅(WL)、沼泽草甸小叶章(XII)、典型草甸小叶章(XI)和岛状林(DZL)6个群落依次设置6个分解亚区。结果表明,水分条件对凋落物分解有显著影响。若未来降水格局变化导致小叶章湿地形成淹水环境,TMC和MMC凋落物失重率将分别增加4.33% - 16.76%和24.84% - 53.97%,分解速率将分别增加10.51% - 32.73%和77.85% - 93.92%,95%分解时间将分别缩短0.72 - 1.85年和3.67 - 4.05年。TMC和MMC凋落物N含量及N积累指数变化趋势较一致,但不同亚区变化模式不同。总体而言,DZL、XI、WL、MG和PF亚区凋落物N呈现释放与积累交替变化特征,但以释放过程为主;相比之下,XII亚区凋落物N一直处于释放状态。C/N比在分解过程中对凋落物N变化具有重要调节作用。估算结果表明,TMC和MMC凋落物N现存量分别为12.75 g·m⁻²和8.29 g·m⁻²,N年归还量分别大于1.95 g·(m²·a)⁻¹和2.25 g·(m²·a)⁻¹。影响因素研究表明,温度对凋落物相对分解速率有促进作用,水分条件对其有抑制作用。进一步分析表明,若分解环境养分状况变化不大,相对分解速率在一定程度上取决于凋落物底物质量;反之,若分解环境养分状况变化较大,相对分解速率在一定程度上取决于分解环境养分供应状况。

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