首页|青藏高原草地生态系统碳通量研究进展

青藏高原草地生态系统碳通量研究进展

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青藏高原拥有我国面积最大的天然草地, 区域内生态系统碳通量的长期定位观测研究具有重要意义. 在总结生态系统碳通量主要研究方法基础上, 对青藏高原不同植被类型碳循环的源、汇效应、时空变化及其与影响因子关系等研究领域所取得的重要进展进行了综合评述. 现有研究表明, 不同植被类型间CO_2通量的季节变化、年际变化、交换量和碳源汇特征等存在明显差异, 光合有效辐射、温度、降水、土壤水分和叶面积指数等是影响碳通量变化的主要驱动因子. 最后, 结合当前青藏高原地区生态系统碳通量研究的现实与需要, 探讨了通量观测所面临的主要科学问题及解决途径. 未来对青藏高原碳循环关键过程的研究工作还需要多尺度、长期生态实验和CO_2通量观测数据支持, 同时以此为基础发展新的数据处理、分析和跨尺度机理模拟方法, 建立青藏高原生态系统碳循环模型.
Research Advances of Grassland Ecosystem CO_2 Flux on Qinghai-Tibetan Plateau
The Qinghai-Tibetan Plateau has the largest area of natural grassland in China. The long-term localized observation and investigation of grassland ecosystem flux on the plateau play an important role in the world. On the basis of generalizing the main methodologies of ecosystem flux, we made a general summary of research achievements, including carbon sources or sinks, spatial and seasonal variations of carbon fluxes, as well as the relationship between carbon fluxes and environmental factors. In present study, the seasonal variations of carbon fluxes and carbon sources or sinks had obvious differences in various vegetation ecosystems, and were mainly controlled by photosynthetically active radiation, temperature, precipitation, soil moisture and leaf area index. Additionally, in accordance with the realities and necessities of ecosystem flux research on Qinghai-Tibet Plateau, the existing problems and approaches were discussed in detail. It was suggested that multi-scale, long-term ecological tests and observation data support were needed in the future research, and based of which new data processing and analysis and mechanism simulation method should also be developed to build models of Qinghai-Tibetan Plateau ecosystem carbon cycle.

Qinghai-Tibet Plateaucarbon fluxeddy covariancechamber techniqueecosystem

岳广阳、赵林、赵拥华、李元寿

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中国科学院,寒区旱区环境与工程研究所,青藏高原冰冻圈观测研究站,甘肃,兰州,730000

青藏高原 碳通量 涡度相关技术 箱式法 生态系统

国家自然科学基金国家自然科学基金中国科学院基金

4070103340701022O984891001

2010

冰川冻土
中国地理学会 中国科学院寒区旱区环境与工程研究所

冰川冻土

CSTPCDCSCD北大核心
影响因子:2.546
ISSN:1000-0240
年,卷(期):2010.32(1)
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