高级检索+

淹水条件下兴凯湖湿地3种典型植物枯落物分解及碳、氮释放动态

Litter decomposition and carbon-nitrogen release dynamics of three typical plants in the Khanka Lake wetland under flooded conditions

  • 摘要: 本研究以我国东北兴凯湖地区典型湿地植物芦苇(Phragmites australis (Cav.) Trin. ex Steud)、小叶章(Deyeuxia angustifolia (Kom.) Y. L. Chang)和狭叶甜茅(Glyceria spiculosa (F. Schmidt) Roshev.)枯落物为研究对象,通过室内模拟实验,探究淹水条件下单一和混合枯落物的分解速率及碳、氮元素释放特征。结果显示:(1)经过240 d的分解,芦苇、小叶章和狭叶甜茅的干质量损失率分别为15.13%、20.3%和21.1%,芦苇分解速率最慢;狭叶甜茅与小叶章混合枯落物质量损失率达23.83%,显著高于混合枯落物狭叶甜茅与芦苇(22.20%)及芦苇与小叶章(19.10%),总体表现为混合枯落物分解速率较快;混合效应分析结果表明,狭叶甜茅的混合枯落物在分解过程中主要表现为协同作用,而芦苇与小叶章混合枯落物存在阶段性拮抗效应。(2)枯落物分解速率与其初始C∶N值(r=−0.178)、C∶P值(r=−0.181)呈显著负相关,枯落物自身生态化学计量是调控其分解速率的关键因素。(3)分解过程中,所有枯落物发生了碳元素净释放(碳相对归还指数CRRI>0),而仅小叶章枯落物发生了氮元素净释放(NRRI>0),芦苇及其与狭叶甜茅混合枯落物则发生了氮元素净累积(氮相对归还指数NRRI<0)。(4)枯落物分解过程的碳元素损失以CO2排放为主(占总碳损失量的81.7%~88.1%),其次为溶解性有机碳(7.1%~11.3%)和CH4排放(1.5%~8.3%)。研究结果表明,淹水条件下,湿地枯落物分解速率和养分释放动态主要受其初始化学性质调控,混合枯落物分解存在非加和效应,其分解模式不能通过单一植物的分解进行预测。

     

    Abstract: This study examined how flooding affects decomposition and carbon and nitrogen release from single-species and mixed-species litter of three dominant wetland plants (Phragmites australis (Cav.) Trin. ex Steud, Deyeuxia angustifolia (Kom.) Y. L. Chang, and Glyceria spiculosa (F. Schmidt) Roshev.) in Khanka Lake, Northeast China. Based on a laboratory simulation experiment, results showed that after 240 d of decomposition, the mass loss rates of P. australis, D. angustifolia, and G. spiculosa were 15.13%, 20.3%, and 21.1%, respectively, with P. australis exhibiting the slowest decomposition rate. Mixed litter generally decomposed more rapidly than single-species litter. The mixture of G. spiculosa and D. angustifolia showed the highest mass loss rate (23.83%), exceeding that of G. spiculosa mixed with P. australis (22.20%) and P. australis mixed with D. angustifolia (19.10%). Mixing effect analysis indicated that mixtures containing G. spiculosa primarily produced synergistic effects during decomposition, whereas P. australisD. angustifolia mixed litter showed stage-specific antagonistic effects. Litter decomposition was significantly and negatively correlated with initial litter C : N ratio (r=−0.178) and C : P ratio (r=−0.181), indicating that initial stoichiometric composition was a key regulator of litter breakdown under flooded conditions. All litter types showed net carbon release during decomposition, as indicated by carbon relative return index values above zero (CRRI>0). In contrast, net nitrogen release occurred only in D. angustifolia litter (nitrogen relative return index, NRRI>0), whereas P. australis litter and its mixture with G. spiculosa exhibited net nitrogen accumulation (NRRI<0). Carbon loss occurred primarily through CO2 emissions (81.7%–88.1%), followed by dissolved organic carbon (7.1%–11.3%) and CH4 emissions (1.5%–8.3%). These findings show that litter decomposition and nutrient release in flooded wetlands are strongly controlled by initial litter chemistry, but that mixed-species litter can generate non-additive effects that can not be inferred from single-species decomposition patterns alone.

     

/

返回文章
返回