Njoroge Brian, Li Yuelin, Wei Shimin, Meng Ze, Liu Shizhong, Zhang Qianmei, Tang Xuli, Zhang Deqiang, Liu Juxiu, Chu Guowei
Core Botanical Gardens, Chinese Academy of Sciences, Guangzhou, China.
Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou, China.
Front Plant Sci. 2021 Oct 18;12:715340. doi: 10.3389/fpls.2021.715340. eCollection 2021.
Compared with other forest systems, research interest in the potential for a stronger ecosystem carbon sequestration of evergreen forests throughout subtropical China has greatly increased. The eddy covariance technique is widely employed to determine accurate forest-atmosphere carbon dioxide (CO) flux, which is subsequently used to determine forest ecosystem carbon exchange characteristics. The Dinghushan Biosphere Reserve, a subtropical monsoon evergreen broad-leaved forest, is a suitable study area due to its warm and humid climate (compared with other regions within the same latitude), consequently playing a role in the carbon cycle in the region. For this study, we hypothesized that the forest land in this region generally acts as a carbon sink, and that its carbon sequestration capacity increases over time despite the influence of climatic factors. Here, we compared net CO flux data derived from the eddy covariance technique over an 8-year study window. Additionally, we ascertained the effects of various environmental factors on net CO flux, while also using the Michaelis-Menten model and a physiologically based process model to track and report on ecosystem carbon exchange characteristics. We observed seasonal trends in daily ecosystem flux, indicative of sensitivity to climatic factors, such as air temperature, precipitation, and sunlight. The carbon sequestration capacity of the region exhibited seasonal variability, increasing from October to March (-264 g C m year, i.e., 48.4%) while weakening from April to September (-150 g C m year, i.e., 40.4%) on average. The net ecosystem exchange (NEE) rate varied from -518 to -211 g C m year; ecosystem respiration (Re) varied from 1,142 to 899 g C m year; and gross primary production (GPP) varied from 1,552 to 1,254 g C m year. This study found that even though the Dinghushan Biosphere Reserve generally acts as a carbon sink, its carbon sequestration capacity did not increase significantly throughout the study period. The techniques (models) used in this study are suitable for application in other ecosystems globally, which can aid in their management and conservation. Finally, the Dinghushan Biosphere Reserve is both an exemplary and a model forest system useful in exploring CO absorption and sequestration from the atmosphere.
与其他森林系统相比,中国亚热带地区常绿森林更强的生态系统碳固存潜力引发的研究兴趣大幅增加。涡度相关技术被广泛用于测定准确的森林 - 大气二氧化碳(CO₂)通量,随后用于确定森林生态系统碳交换特征。鼎湖山生物圈保护区是亚热带季风常绿阔叶林,因其温暖湿润的气候(与同纬度其他地区相比),成为一个合适的研究区域,在该地区的碳循环中发挥着作用。在本研究中,我们假设该地区的林地总体上作为碳汇,并且尽管受气候因素影响,其碳固存能力会随时间增加。在此,我们比较了在8年研究期内通过涡度相关技术得出的净CO₂通量数据。此外,我们确定了各种环境因素对净CO₂通量的影响,同时还使用米氏模型和基于生理过程的模型来追踪和报告生态系统碳交换特征。我们观察到每日生态系统通量的季节性趋势,表明其对气候因素如气温、降水和阳光敏感。该地区的碳固存能力呈现季节性变化,10月至次年3月增加(-264 g C m⁻² year⁻¹,即48.4%),而4月至9月平均减弱(-150 g C m⁻² year⁻¹,即40.4%)。净生态系统交换(NEE)速率在-518至-211 g C m⁻² year⁻¹之间变化;生态系统呼吸(Re)在1,142至899 g C m⁻² year⁻¹之间变化;总初级生产力(GPP)在1,552至1,254 g C m⁻² year⁻¹之间变化。本研究发现,尽管鼎湖山生物圈保护区总体上作为碳汇,但其碳固存能力在整个研究期间并未显著增加。本研究中使用的技术(模型)适用于全球其他生态系统,有助于其管理和保护。最后,鼎湖山生物圈保护区是探索从大气中吸收和固存CO₂的典范和典型森林系统。