Carbon Dioxide and Methane Distribution in Peat Deposits of an Oligotrophic Forest Bog and Their Emission in Western Siberia

IF 0.7 4区 环境科学与生态学 Q4 ECOLOGY
L. I. Inisheva, M. A. Sergeeva, A. V. Golovchenko, B. V. Babikov
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引用次数: 0

Abstract

Swamps and wetlands in forested areas, as well as nonforest swamps, are collectively involved in the global carbon cycle. They play an important role in depositing greenhouse gases. This article analyzes the long-term dynamics of concentration of greenhouse gases (CO2 and CH4) in a peat deposit and their emission in a natural and reclaimed oligotrophic bog in the southern taiga zone of Western Siberia. It is shown that a significant role in the dynamics of CO2 and CH4 concentration in peat deposits is played by weather conditions in each month of the warm period, as well as by the botanical composition, the activity of biochemical processes, and the structure and physical and mechanical properties of peat deposits. We have also identified the intradeposit spatial and temporal dynamics of indices of greenhouse gas concentrations. It has been proven that there are multicomponent dependences of CO2 and CH4 concentrations on parameters of external and intradeposit conditions. Parameters of concentrations in the peat deposit of the oligotrophic bog from the swampy catchment basin of the Klyuch River have been determined as follows: extreme concentrations of CO2 were 0.002–3.64 mmol/dm3 and extreme concentrations of CH4 were 0.003–2.03 mmol/dm3; normalized CO2 fluxes varied from /–22.2/ to 157.8 mg C/(m2 h), the extreme values of normalized CH4 fluxes were /–3.0/–5.3 mg C/(m2 h), CO2 fluxes for the warm period were 20–110 g C/(m2 year), and CH4 fluxes for the warm period were 0.8–3.7 C/(m2 year). A slight increase in the activity of normalized CO2 fluxes has been recorded at the forest reclamation site compared to a natural swamp, while the concentrations of greenhouse gases in the peat deposit have proven to be comparable in both cases. It is shown that the absence of an operating drainage system leads to rebogging. The vast areas of swamps on the West Siberian Plain and the aggressive pattern of bogging implies moderate and selective forest reclamation for its taiga zone.

Abstract Image

西伯利亚西部低营养森林沼泽泥炭沉积物中二氧化碳和甲烷的分布及其排放量
摘要森林地区的沼泽和湿地以及非森林沼泽共同参与了全球碳循环。它们在沉积温室气体方面发挥着重要作用。本文分析了西西伯利亚南部泰加带泥炭沉积物中温室气体(CO2 和 CH4)浓度的长期动态及其在天然和开垦的寡营养沼泽中的排放情况。研究表明,温暖期每个月的天气条件、植物组成、生化过程的活性以及泥炭沉积物的结构、物理和机械特性对泥炭沉积物中二氧化碳和甲烷浓度的动态变化起着重要作用。我们还确定了沉积物内部温室气体浓度指数的时空动态。事实证明,二氧化碳和甲烷浓度与外部和沉积物内部条件参数存在多组分依赖关系。克柳奇河沼泽流域低营养沼泽泥炭沉积物的浓度参数确定如下:二氧化碳极端浓度为 0.002-3.64 mmol/dm3,甲烷极端浓度为 0.003-2.03 mmol/dm3;正常浓度为 0.002-3.64 mmol/dm3,甲烷极端浓度为 0.003-2.03 mmol/dm3。03 mmol/dm3 ;归一化 CO2 通量在 /-22.2/ 至 157.8 mg C/(m2 h) 之间变化,归一化 CH4 通量的极值为 /-3.0/-5.3 mg C/(m2 h),温暖时期的 CO2 通量为 20-110 g C/(m2 year),温暖时期的 CH4 通量为 0.8-3.7 C/(m2 year)。与天然沼泽地相比,森林开垦地的二氧化碳通量的正常化活动略有增加,而泥炭沉积物中的温室气体浓度在两种情况下都相当。结果表明,没有运行的排水系统会导致沼气回流。西西伯利亚平原上大片的沼泽地以及沼泽化的严重程度意味着在泰加地带进行适度的、有选择性的森林开垦。
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来源期刊
Contemporary Problems of Ecology
Contemporary Problems of Ecology 环境科学-生态学
CiteScore
1.40
自引率
12.50%
发文量
54
审稿时长
6-12 weeks
期刊介绍: Contemporary Problems of Ecology is a multidisciplinary periodical that publishes original works on the following subjects: theoretical and methodical issues of ecology, regional aspects of ecology, regional ecological disasters, structure and functioning of ecosystems, anthropogenic transformation of ecosystems. All basic aspects of modern ecology, including the most complicated interactions between living organisms and their environment, are presented. Some of the journal issues are dedicated to global changes in biological diversity at various levels of organization (populations, species, ecosystems) principles and methods of nature conservation.
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