Tropical forest CH4 budget: the importance of local hotspots

Hella van Asperen,Thorsten Warneke,Alessandro De Araújo,Bruce Forsberg, Sávio Ferreira, João Alves-Oliveira,Leonardo Ramos de Oliveira, Thiago de Lima Xavier,Marta Sá, Paulo Teixeira, Elaine Pires, Veber Moura,Shujiro Komiya,Santiago Botia, Sam Jones,Jost Lavrič,Susan Trumbore,Justus Notholt

crossref(2022)

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摘要
<p>Methane (CH<sub>4</sub>) is one of the most important anthropogenic greenhouse gases. Despite its importance, natural sources of methane, such as tropical wetlands and termites, are still not well understood and a large source of uncertainty in the tropical CH<sub>4</sub> budget. The Amazon rainforest is a key region for the (global) CH<sub>4</sub> budget but, due to its remote location, local CH<sub>4</sub> concentration and flux measurements are still rare.</p><p>Fieldsite ZF2 (60 km NW of Manaus, Brazil) is located in pristine tropical rain forest. At this fieldsite, a Spectronus FTIR-analyzer (measuring CO<sub>2</sub>, CO, CH<sub>4</sub>, N<sub>2</sub>O & &#948;<sup>13</sup>CO<sub>2</sub>) was installed at the foot of the K34 tower, set up to measure different heights above and below the canopy continuously. In addition, by use of a Los Gatos portable analyzer (measuring CO<sub>2</sub> & CH<sub>4</sub>), additional semi-continuous concentration measurements were performed at the valley tower (studying the nighttime build up of valley CH<sub>4</sub>), above the igarap&#233;&#160; (capturing the CH<sub>4</sub> ebullition bubbles leaving the water surface), and on the plateau (studying the spatial horizontal heterogeneity of CH<sub>4</sub> concentrations within the canopy). Furthermore, the portable analyzer was used for soil, water, termite mound, and termites flux measurements.</p><p>By combining tower and flux chamber measurements, the role and magnitude of different ecosystem sources could be assessed. We observed that, while soils in the valley are a small source of CH<sub>4</sub> (0.1 to 0.2 nmol CH<sub>4</sub> m<sup>-2</sup> s<sup>-1</sup>), overall the soils of this ecosystem are expected to be a net CH<sub>4</sub> sink (-0.3 to -0.5 nmol m<sup>-2</sup> s<sup>-1 </sup>). Estimated total ecosystem CH<sub>4</sub> flux, based on nighttime concentration analyses of the tower data, indicate that the ecosystem is a net CH<sub>4</sub> source (~1 to 2 nmol CH<sub>4</sub> m<sup>-2</sup> s<sup>-1</sup>). We propose that the net CH<sub>4</sub> emission of the ecosystem is driven by local emitting hotspots, such as the valley stream and standing water, termites and termite mounds (~1 nmol CH<sub>4</sub> m<sup>-2</sup> s<sup>-1</sup>), anoxic soil spots and decaying dead wood.</p><p>&#160;</p>
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