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树木和森林中的甲烷产生和排放。

Methane production and emissions in trees and forests.

机构信息

Environmental Studies and Sciences Program, Skidmore College, 815 N Broadway, Saratoga Springs, NY, 12866, USA.

School of Forestry and Environmental Studies, Yale University, 195 Prospect St., New Haven, CT, 06511, USA.

出版信息

New Phytol. 2019 Apr;222(1):35-51. doi: 10.1111/nph.15624. Epub 2019 Jan 11.

DOI:10.1111/nph.15624
PMID:30521089
Abstract

Contents Summary 35 I. Introduction 36 II. Tree CH fluxes 36 III. Tree emissions of soil-produced CH 40 IV. Tree-produced CH 42 V. Trees in forest CH budgets 44 VI. Conclusions 46 Acknowledgements 48 Author contributions 48 References 48 SUMMARY: Forest ecosystem methane (CH ) research has focused on soils, but trees are also important sources and sinks in forest CH budgets. Living and dead trees transport and emit CH produced in soils; living trees and dead wood emit CH produced inside trees by microorganisms; and trees produce CH through an abiotic photochemical process. Here, we review the state of the science on the production, consumption, transport, and emission of CH by living and dead trees, and the spatial and temporal dynamics of these processes across hydrologic gradients inclusive of wetland and upland ecosystems. Emerging research demonstrates that tree CH emissions can significantly increase the source strength of wetland forests, and modestly decrease the sink strength of upland forests. Scaling from stem or leaf measurements to trees or forests is limited by knowledge of the mechanisms by which trees transport soil-produced CH , microbial processes produce and oxidize CH inside trees, a lack of mechanistic models, the diffuse nature of forest CH fluxes, complex overlap between sources and sinks, and extreme variation across individuals. Understanding the complex processes that regulate CH source-sink dynamics in trees and forests requires cross-disciplinary research and new conceptual models that transcend the traditional binary classification of wetland vs upland forest.

摘要

内容概述 35 I. 引言 36 II. 树木 CH 通量 36 III. 土壤产生的 CH 排放 40 IV. 树木产生的 CH 42 V. 森林 CH 预算中的树木 44 VI. 结论 46 致谢 48 作者贡献 48 参考文献 48 摘要:森林生态系统甲烷(CH )研究主要集中在土壤上,但树木也是森林 CH 预算中的重要源和汇。活体和死树运输和排放土壤中产生的 CH;活体树木和枯木通过微生物排放树木内部产生的 CH;树木通过非生物光化学过程产生 CH。在这里,我们综述了活体和死树产生、消耗、运输和排放 CH 的科学现状,以及这些过程在包括湿地和旱地生态系统在内的水文梯度上的时空动态。新兴研究表明,树木 CH 排放可以显著增加湿地森林的源强度,并适度降低旱地森林的汇强度。从茎或叶测量到树木或森林的尺度受到树木运输土壤产生的 CH 的机制、树木内部微生物过程产生和氧化 CH 的知识限制、缺乏机制模型、森林 CH 通量的弥散性质、源和汇之间复杂的重叠以及个体之间的极端变化。要了解调节树木和森林 CH 源汇动态的复杂过程,需要跨学科研究和新的概念模型,超越湿地与旱地森林的传统二元分类。

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