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The effect of biomass harvesting on greenhouse gas emissions from a rewetted temperate fen

机译:生物质收获对重新洗温水芬的温室气体排放的影响

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The growing demand for bioenergy increases pressure on peatlands. The novel strategy of wet peatlands agriculture (paludiculture) may permit the production of bioenergy from biomass while avoiding large greenhouse gas emissions as occur during conventional crop cultivation on drained peat soils. Herein, we present the first greenhouse gas balances of a simulated paludiculture to assess its suitability as a biomass source from a climatic perspective. In a rewetted peatland, we performed closed-chamber measurements of carbon dioxide, methane, and nitrous oxide exchange in stands of the potential crops Phragmites australis , Typha latifolia , and Carex acutiformis for two consecutive years. To simulate harvest, the biomass of half of the measurement spots was removed once per year. Carbon dioxide exchange was close to neutral in all tested stands. The effect of biomass harvest on the carbon dioxide exchange differed between the 2?years. During the first and second year, methane emissions were 13–63?g?msup?2/sup?asup?1/sup and 2–5?g?msup?2/sup?asup?1/sup, respectively. Nitrous oxide emissions lay below our detection limit. Net greenhouse gas balances in the study plots were close to being climate neutral during both years except for the Carex stand, which was a source of greenhouse gases in the first year (in COsub2/sub-equivalents: 18 t?hasup?1/sup?asup?1/sup). Fifteen years after rewetting the net greenhouse gas balance of the study site was similar to those of pristine fens. In addition, we did not find a significant short-term effect of biomass harvest on net greenhouse gas balances. In our ecosystem, ~17 t?hasup?1/sup?asup?1/sup of COsub2/sub-equivalent emissions are saved by rewetting compared to a drained state. Applying this figure to the fen area in northern Germany, emission savings of 2.8–8.5 Mt?asup?1/sup COsub2/sub-equivalents could possibly be achieved by rewetting; this excludes additional savings by fossil fuel replacement.
机译:对生物能源的需求不断增长增加了泥炭地的压力。湿泥炭地农业(洋化工)的新型战略可能允许从生物量产生生物能源,同时避免在排水泥炭土壤中常规作物培养中发生的大型温室气体排放。在此,我们介绍了模拟营业术的第一个温室气体余量,以评估其从气候角度来评估其作为生物质来源的适用性。在再浸润的泥炭块中,我们连续两年进行潜在作物澳大利亚,Typha Latifolia和Carex Acuriformis的潜在作物,甲烷和氧化二氮氧化物交换的闭合室测量。为了模拟收获,每年将一半的测量点的生物质删除一次。二氧化碳交换在所有测试台中接近中性。生物质收获对二氧化碳交换的影响差异为2?年。在第一年和第二年期间,甲烷排放为13-63?g?m Δ2?a 1 和2-5?g?m ?2 ?分别?1 。氧化亚氧化物排放量低于我们的检测极限。研究情节中的净温室气体余额在两年内是气候中性,除了Carex立场,这是第一年的温室气体来源(在CO 2 - 等价值:18 t ?ha ?1 ?a ?1 )。重新润湿后十五年后,研究现场的净温室气体平衡与原始葫芦相似。此外,我们在净温室气体余额上没有找到生物质收获的显着短期效果。在我们的生态系统中,〜17 t?ha ?1 ?a 2 2 - 与排水相比,通过重新摩擦来节省等等的排放量状态。将这个数字应用于德国北部的汾地区,排放节省为2.8-8.5吨?a 1 co <​​sub> 2 -equivalents可以通过重新润湿来实现;这不包括化石燃料更换的额外节省。

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