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Land-use change to bioenergy: grassland to short rotation coppice willow has an improved carbon balance

机译:土地利用方式转变为生物能源:草地到短轮伐期的柳树的碳平衡得到改善

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摘要

The effect of a transition from grassland to second-generation (2G) bioenergy on soil carbon and greenhouse gas (GHG) balance is uncertain, with limited empirical data on which to validate landscape-scale models, sustainability criteria and energy policies. Here, we quantified soil carbon, soil GHG emissions and whole ecosystem carbon balance for short rotation coppice (SRC) bioenergy willow and a paired grassland site, both planted at commercial scale. We quantified the carbon balance for a 2-year period and captured the effects of a commercial harvest in the SRC willow at the end of the first cycle. Soil fluxes of nitrous oxide (N2O) and methane (CH4) did not contribute significantly to the GHG balance of these land uses. Soil respiration was lower in SRC willow (912 ± 42 g C m−2 yr−1) than in grassland (1522 ± 39 g C m−2 yr−1). Net ecosystem exchange (NEE) reflected this with the grassland a net source of carbon with mean NEE of 119 ± 10 g C m−2 yr−1 and SRC willow a net sink, −620 ± 18 g C m−2 yr−1. When carbon removed from the ecosystem in harvested products was considered (Net Biome Productivity), SRC willow remained a net sink (221 ± 66 g C m−2 yr−1). Despite the SRC willow site being a net sink for carbon, soil carbon stocks (0–30 cm) were higher under the grassland. There was a larger NEE and increase in ecosystem respiration in the SRC willow after harvest; however, the site still remained a carbon sink. Our results indicate that once established, significant carbon savings are likely in SRC willow compared with the minimally managed grassland at this site. Although these observed impacts may be site and management dependent, they provide evidence that land-use transition to 2G bioenergy has potential to provide a significant improvement on the ecosystem service of climate regulation relative to grassland systems.
机译:从草地向第二代(2G)生物能源过渡对土壤碳和温室气体(GHG)平衡的影响尚不确定,只有有限的经验数据可用于验证景观尺度模型,可持续性标准和能源政策。在这里,我们量化了短循环小灌木林(SRC)生物能源柳树和成对的草地场的土壤碳,土壤温室气体排放量以及整个生态系统的碳平衡,二者均以商业规模种植。我们量化了两年内的碳平衡,并在第一个周期结束时捕获了SRC柳树中商业性收获的影响。一氧化二氮(N2O)和甲烷(CH4)的土壤通量对这些土地利用的温室气体平衡没有显着贡献。 SRC柳的土壤呼吸(912±42 g C m-2 yr-1)比草原(1522±39 g C m-2 yr-1)低。净生态系统交换(NEE)反映了草原是碳的净碳源,平均NEE为119±10 g C m-2 yr-1,而SRC则是净汇,-620±18 g C m-2 yr-1 。当考虑从收获产品中的生态系统中去除碳时(净生物群落生产力),SRC杨柳仍为净汇(221±66 g C m-2 yr-1)。尽管SRC柳树站点是碳的净汇,但草地下的土壤碳储量(0–30 cm)较高。收获后,SRC杨柳的NEE更大,生态系统呼吸增加;但是,该地点仍然是一个碳汇。我们的结果表明,与该地点最低限度管理的草地相比,一旦建立,SRC柳树可能会大量节省碳。尽管这些观察到的影响可能取决于场所和管理,但它们提供的证据表明,相对于草地系统,土地使用向2G生物能源的过渡有可能显着改善气候调节的生态系统服务。

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