globalchange  > 气候变化与战略
CSCD记录号: CSCD:5647295
论文题名:
不同形态氮输入对湿地生态系统碳循环影响的研究进展
其他题名: Effects of Nitrogen Forms on the Stability of Soil Organic Carbon in Wetlands: A Review
作者: 陶宝先; 陈永金
刊名: 生态环境学报
ISSN: 1674-5906
出版年: 2016
卷: 25, 期:1, 页码:2362-2372
语种: 中文
中文关键词: 氮素形态 ; 湿地 ; 土壤 ; 碳循环
英文关键词: nitrogen forms ; wetlands ; soil ; carbon cycling
WOS学科分类: ENVIRONMENTAL SCIENCES
WOS研究方向: Environmental Sciences & Ecology
中文摘要: 人类活动导致湿地生态系统氮负荷明显增加,引起生态系统碳循环过程发生诸多变化。外源氮输入对湿地生态系统土壤碳库稳定性的影响已成为当今国际研究的前沿问题之一。文章综述了不同形态氮素对湿地植物固碳潜势、土壤自养与异养呼吸速率的影响、土壤甲烷排放及不同形态氮与全球变暖对土壤有机碳及其组分矿化速率的交互作用的研究进展。研究表明,(1)植物对不同形态氮素的选择性吸收,会影响植物叶片的光合速率,改变植物的固碳潜势,影响植物根系的自养呼吸速率;同时,会影响凋落物归还量,改变植物对土壤的有机碳输入;此外,还可能影响凋落物的质量(如C/N),改变凋落物的分解速率,影响土壤异养呼吸速率。(2)各种形态氮输入对土壤pH产生不同的影响,改变土壤微生物及酶活性,影响有机碳的分解及土壤异养呼吸速率。(3)土壤有机碳组分对各种形态氮素的不同响应,也会改变土壤有机碳的矿化速率。(4)植物对不同形态氮素的选择性吸收,及各种形态氮输入对土壤pH产生的不同影响,会影响土壤中可利用C、N源的供应,改变土壤的酸碱环境及氧化还原电位,影响土壤CH_4排放。(5)大气氮沉降与全球变暖同时影响土壤碳循环过程,但不同形态氮素与全球变暖对湿地土壤碳循环过程的交互作用研究仍较少见。迄今为止,氮沉降对湿地土壤碳库稳定性的影响效应仍存在很大的不确定性,仅有少量研究区分氮素形态对土壤碳库稳定性的影响,而关于湿地生态系统的研究鲜有报道。今后应着重区分不同形态氮素对湿地土壤碳库稳定性的影响机理研究,以便深入了解氮沉降与湿地土壤碳库稳定性之间的关系。
英文摘要: The processes of carbon cycling in wetlands have been affected by increasing nitrogen (N) input derived from anthropogenic activities, and concern is growing over the effects of nitrogen input on carbon stability. So far, the overwhelming studies concentrated on the relationships between the amount of N addition and the stability of soil organic carbon (SOC). However, much less information is known how various N forms affect the stability of SOC in wetlands. We reviewed the effects of N forms on the fixation of CO_2, soil autotrophic and heterotrophic respiration, soil methane emission, and the temperature sensitivity of SOC decomposition. Firstly, the results indicated that the selective utilization of N forms for plant species may change the photosynthetic rate, fixation of CO_2, and thus autotrophic respiration rate. Moreover, the return of plant litter and its quality, such as C/N ratio, may be varied under the input of different N forms, these can affect litter decomposition and soil heterotrophic respiration rate. Secondly, the input of various N forms may produce different effects on soil pH and the activities of soil microorganisms and enzymes, which may change soil heterotrophic respiration rate. Thirdly, the decomposition of SOC fractions may have varied responses to various forms of N input, but we have known little about this. Fourthly, the effect of various nitrogen forms on plant biomass, soil ph and redox may affect the input of available C and N from plant to soil and thus microbial activity, changing methane emission. Fifthly, atmospheric N deposition and global warming simultaneous affect soil carbon cycling. However, there is still no answer about the combined effect of N forms and temperature on SOC decomposition, although this issue is very important. So far, many uncertainties still exist in the relationship between N input and SOC stability, and there is litter studies distinguishing the effect of N forms SOC stability in wetlands. Therefore, much more attention should concentrate on distinguishing the effects and mechanisms of N forms on SOC stability, so as to further know the relationship between N deposition and SOC stability.
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/151250
Appears in Collections:气候变化与战略

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作者单位: 聊城大学环境与规划学院, 聊城, 山东 252059, 中国

Recommended Citation:
陶宝先,陈永金. 不同形态氮输入对湿地生态系统碳循环影响的研究进展[J]. 生态环境学报,2016-01-01,25(1):2362-2372
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