青藏高原东坡措格草原湿地生态功能区碳源/碳汇变化特征及影响因素

IF 2.5 4区 环境科学与生态学 Q3 ENVIRONMENTAL SCIENCES Environmental Research Communications Pub Date : 2024-08-15 DOI:10.1088/2515-7620/ad6b05
Bin Guo, Chao Chen, Yanmei Pang, Yu Luo
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引用次数: 0

摘要

生态系统净生产力(NEP)是指陆地生态系统中净初级生产力(NPP)减去异养呼吸消耗的光合作用碳后可用于碳循环的部分。净初级生产力的大小反映了陆地生态系统碳汇/碳源的大小,对研究气候变化和全球碳循环具有重要意义。本研究基于气象数据、植被数据和社会经济数据,采用改进的卡内基-阿姆斯-斯坦福法净增植被量模型和土壤异养呼吸统计模型,估算了青藏高原东坡措格草原湿地生态功能区(ZGW)2001-2020 年的净增植被量。此外,还分析了净生产力的时空变化,研究了自然因素和人为活动对净生产力的影响。结果表明,ZGW 总体上起到了碳汇的作用,碳汇面积约占整个 ZGW 面积的 99.3%。研究区域的年平均净排放系数为 447.9 g-m-2,以 5.0 g-m-2-a-1 的速率逐渐增加,但增加趋势并不显著。93.5%的 ZGW 的碳汇能力有所增加,5.9%的 ZGW 的碳汇能力相对稳定,0.6%的 ZGW 的碳汇能力有所下降且下降明显。气候变暖和增湿促进了 ZGW 生态系统碳汇能力的提高,降水是影响 NEP 变化的主要气候因子。自然因素是近地效应变化的决定因素,而人为活动则起次要作用。在黄河沿岸、干线公路周边和湿地核心区实施生态恢复与治理工程,继续实施有序开发草原资源的绿色协调发展政策,有利于提高 ZGW 的植被碳汇能力。
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Characteristics and influencing factors of carbon source/sink variations in the Zoige grassland wetland ecological function zone on the eastern slope of the Tibetan Plateau
Net ecosystem productivity (NEP) refers to the portion of net primary productivity (NPP) that is available for carbon cycling in terrestrial ecosystems after subtracting photosynthetic carbon consumed by heterotrophic respiration. The amount of the NEP reflects the size of carbon sinks/sources in terrestrial ecosystems, holding great significance for the research of climate change and global carbon cycle. In this study, the NEP of the Zoige grassland wetland ecological function zone (ZGW) on the eastern slope of the Tibetan Plateau from 2001 to 2020 is estimated by using the improved Carnegie-Ames-Stanford Approach model for NPP and a statistical model for soil heterotrophic respiration, based on the meteorological data, vegetation data and socioeconomic data. Additionally, the spatio-temporal variations of the NEP are analyzed, and the influences of natural factors and anthropogenic activities on the NEP are investigated. The results indicate that the ZGW overall plays a role as a carbon sink, and the carbon sink area accounts for approximately 99.3% of the whole ZGW. The annual average NEP in the study area is 447.9 g·m−2, showing a gradual increase at a rate of 5.0 g·m−2·a−1, although the increasing trend is not significant. The carbon sink capacity increased in 93.5% of the ZGW, remained relatively stable in 5.9% of the ZGW, and decreased and significantly decreased in 0.6% of the ZGW. Climate warming and humidifying promote the enhancement of carbon sink capacity in the ecosystem of the ZGW, and precipitation is the dominant climatic factor influencing NEP variations. Natural factors are the determinants of NEP variations, while anthropogenic activities play a secondary role. The implementation of ecological restoration and management projects in the areas along the Yellow River, around the main roads and the core area of wetlands, as well as the continuation of green and coordinated development policies of orderly developing grassland resources, is conducive to enhancing vegetation carbon sink capacity of the ZGW.
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Environmental Research Communications
Environmental Research Communications ENVIRONMENTAL SCIENCES-
CiteScore
3.50
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0.00%
发文量
136
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