On the Relationship Between Methane Production in Anaerobic Incubations of Peat Material and In Situ Methane Emissions

IF 3.7 3区 环境科学与生态学 Q2 ENVIRONMENTAL SCIENCES
Alexandra B. Cory, Rachel M. Wilson, Olivia C. Ogles, Patrick M. Crill, Zhen Li, Kuang-Yu Chang, Samantha H. Bosman, Virginia I. Rich, Jeffrey P. Chanton, EMERGE Project Coordinators, Moira Hough, Sky Dominguez, Nicole Irwin-Raab, Gareth Trubl, Robert M. Jones, Darya Anderson, Isogenie Field Team
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Abstract

Anaerobic incubations of peat have been widely used to explore soil processes, but this in vitro technique raises many questions as to how well it reproduces in situ conditions. To investigate this, we conducted 60–100 days (+25 days pre-incubation) anaerobic, temperature-controlled incubation experiments across a temperature range of 1–26°C on samples from bog and fen habitats, at two different depths (9–19and 25–35 cm). We observed exponential increases in CO2 and methane production with temperature in all conditions. We then compared field-based measurements of methane emission with modeled expectations by extrapolating incubation-determined methane production rates based on (a) soil temperature profiles, (b) the observed incubation temperature-methane production relationship, and (c) seasonal thaw depth from each site. The resulting incubation-extrapolated methane production agreed with measured emission rates within a factor of two at both sites and corresponded to 182 ± 54% and 59 ± 14% of the measured average yearly fluxes from the field for the bog and fen, respectively. The underestimation of fen methane fluxes may be due to the lack of living plant root-derived dissolved organic carbon inputs in incubations, a key process in fens. Conversely, the overestimation in bogs could be attributed to methane oxidation in the field, which is absent in anaerobic incubation conditions. Nonetheless incubations predicted greenhouse gas emissions from a northern peatland within a factor of two.

泥炭的厌氧培养已被广泛用于探索土壤过程,但这种体外技术在多大程度上再现了原地条件,却引发了许多问题。为了研究这个问题,我们对来自沼泽和沼泽栖息地的两种不同深度(9-19 厘米和 25-35 厘米)的样本进行了 60-100 天(培养前 25 天)的厌氧温控培养实验,温度范围在 1-26°C 之间。我们观察到,在所有条件下,二氧化碳和甲烷的产生量都随温度呈指数增长。然后,我们将甲烷排放的实地测量结果与模型预期结果进行了比较,方法是根据(a)土壤温度剖面、(b)观察到的孵化温度与甲烷产生量的关系以及(c)每个地点的季节性解冻深度来推断孵化确定的甲烷产生率。由此得出的孵育外推甲烷产量与两个地点的测量排放率相差不超过 2 倍,分别相当于沼泽和沼泽地实地测量年平均通量的 182 ± 54% 和 59 ± 14%。低估沼泽甲烷通量的原因可能是在孵化过程中缺乏源于植物根系的溶解有机碳输入,而这是沼泽的一个关键过程。相反,沼泽中甲烷通量被高估的原因可能是甲烷在田间被氧化,而在厌氧培养条件下不存在甲烷氧化。尽管如此,孵育对北方泥炭地温室气体排放量的预测仍在 2 倍以内。
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来源期刊
Journal of Geophysical Research: Biogeosciences
Journal of Geophysical Research: Biogeosciences Earth and Planetary Sciences-Paleontology
CiteScore
6.60
自引率
5.40%
发文量
242
期刊介绍: JGR-Biogeosciences focuses on biogeosciences of the Earth system in the past, present, and future and the extension of this research to planetary studies. The emerging field of biogeosciences spans the intellectual interface between biology and the geosciences and attempts to understand the functions of the Earth system across multiple spatial and temporal scales. Studies in biogeosciences may use multiple lines of evidence drawn from diverse fields to gain a holistic understanding of terrestrial, freshwater, and marine ecosystems and extreme environments. Specific topics within the scope of the section include process-based theoretical, experimental, and field studies of biogeochemistry, biogeophysics, atmosphere-, land-, and ocean-ecosystem interactions, biomineralization, life in extreme environments, astrobiology, microbial processes, geomicrobiology, and evolutionary geobiology
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