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Emissions of methane from northern peatlands: a review of management impacts and implications for future management options

机译:北部泥炭地的甲烷排放:对管理的影响及其对未来管理选择的影响的综述

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Abstract Northern peatlands constitute a significant source of atmospheric methane (CH 4 ). However, management of undisturbed peatlands, as well as the restoration of disturbed peatlands, will alter the exchange of CH 4 with the atmosphere. The aim of this systematic review and meta-analysis was to collate and analyze published studies to improve our understanding of the factors that control CH 4 emissions and the impacts of management on the gas flux from northern (latitude 40???° to 70???°N) peatlands. The analysis includes a total of 87 studies reporting measurements of CH 4 emissions taken at 186 sites covering different countries, peatland types, and management systems. Results show that CH 4 emissions from natural northern peatlands are highly variable with a 95% CI of 7.6?¢????15.7 g C m ?¢????2 year ?¢????1 for the mean and 3.3?¢????6.3 g C m ?¢????2 year ?¢????1 for the median. The overall annual average (mean ???± SD ) is 12 ???± 21 g C m ?¢????2 year ?¢????1 with the highest emissions from fen ecosystems. Methane emissions from natural peatlands are mainly controlled by water table (WT) depth, plant community composition, and soil pH. Although mean annual air temperature is not a good predictor of CH 4 emissions by itself, the interaction between temperature, plant community cover, WT depth, and soil pH is important. According to short-term forecasts of climate change, these complex interactions will be the main determinant of CH 4 emissions from northern peatlands. Drainage significantly ( p < .05) reduces CH 4 emissions to the atmosphere, on average by 84%. Restoration of drained peatlands by rewetting or vegetation/rewetting increases CH 4 emissions on average by 46% compared to the original premanagement CH 4 fluxes. However, to fully evaluate the net effect of management practice on the greenhouse gas balance from high latitude peatlands, both net ecosystem exchange (NEE) and carbon exports need to be considered.
机译:摘要北部泥炭地是大气甲烷(CH 4)的重要来源。但是,未扰动泥炭地的管理以及受干扰泥炭地的恢复将改变CH 4与大气的交换。该系统评价和荟萃分析的目的是整理和分析已发表的研究报告,以增进我们对控制CH 4排放的因​​素以及管理对北方(纬度40°至70°)气体通量的影响的理解。 N°泥炭地。分析包括总共87项研究,报告了在不同国家,泥炭地类型和管理系统的186个站点进行的CH 4排放测量。结果显示,天然北部泥炭地的CH 4排放变化很大,CI的95%CI为7.6?1?15.7 g C m?2?2年,平均值为1,3.3。 6.3g C m≥2年,中位数为±1。总体年平均值(平均值±SD)为12±21 g C m -2年2 –1,来自芬生态系统的排放量最高。天然泥炭地的甲烷排放主要受地下水位(WT)深度,植物群落组成和土壤pH值控制。尽管年平均气温本身并不能很好地预测CH 4的排放,但温度,植物群落覆盖率,野生型深度和土壤pH值之间的相互作用很重要。根据气候变化的短期预测,这些复杂的相互作用将是决定北部泥炭地CH 4排放的主要决定因素。排水(p <.05)可将向大气中的CH 4排放量平均减少84%。与原始的管理前CH 4通量相比,通过重新湿润或植被/再湿化对排水泥炭地进行恢复平均可使CH 4排放量平均增加46%。但是,要全面评估管理实践对高纬度泥炭地温室气体平衡的净影响,既要考虑净生态系统交换(NEE),也要考虑碳出口。

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