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Transforming Meadows Into Free Surface Water Wetlands: Impact Of Increased Nitrate And Carbon Loading On Greenhouse Gas Production

机译:将草地转变为地表水湿地:硝酸盐和碳含量增加对温室气体生产的影响

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In a laboratory study we investigated 1) the potential production of nitrous oxide (N_2O), methane (CH_4) and carbon dioxide (CO_2) and 2) the effect of nitrate (NO_3~-) and anaerobic N_2O development on CH_4 production in sediment from a recently recreated free surface water wetland (FSWW) and in soil from an adjacent meadow. We designed an experiment where production of greenhouse gases was registered at the time of maximum net development of N_2O. We made additions of biodegradable carbon (glucose) and/or NO_3~- to sediment and soil slurries and incubated them at four temperatures (4,13, 20, 28 ℃). Gas production from both substrates was positively correlated with temperature. We also found that the sediment produced more N_2O than the soil. N_2O production in sediment was NO3 limited, whereas in soil carbon availability was lower and only combined additions of NO~-_3 and glucose supported increased N_2O development. CH_4 production was generally low and did not differ between soil and sediment. Nor did glucose addition increase CH_4 rates. The results suggest that neither soil nor sediment environment did support development of methanogenic populations. There were no clear effects of NO_3~- on CH_4 production. However, the highest records of CH_4 were found in incubations with low N_2O production, which indicates that N_2O might be toxic to methanogens. In summary, our study showed that transforming meadows into FSWWs implies a risk of increased N_2O emissions. This does not seem to be valid for CH_4. However, since N_2O is almost always produced wherever NO_3~- is denitrified, increased N_2O production in wetlands leads to reduced rates in downstream environments. Hence, we conclude that when balancing NO_3~- retention and global warming aspects, we find no reason to discourage future creation or restoration of wetlands.
机译:在实验室研究中,我们调查了1)一氧化二氮(N_2O),甲烷(CH_4)和二氧化碳(CO_2)的潜在生产,以及2)硝酸盐(NO_3〜-)和厌氧N_2O的形成对沉积物中CH_4产生的影响最近重建的自由地表水湿地(FSWW)以及邻近草地的土壤中。我们设计了一个实验,其中在N_2O达到最大净发展时记录了温室气体的产生。我们在沉积物和土壤泥浆中添加了可生物降解的碳(葡萄糖)和/或NO_3〜-,并在四个温度(4、13、20、28℃)下对其进行了培养。两种基材的产气量与温度呈正相关。我们还发现,沉积物产生的N_2O比土壤多。沉积物中N_2O的产生受到NO3的限制,而土壤中碳的有效性较低,只有NO〜-_3和葡萄糖的联合添加才支持N_2O的增加。 CH_4的产量通常较低,土壤和沉积物之间没有差异。葡萄糖添加也没有增加CH_4率。结果表明,土壤和沉积物环境都不支持产甲烷种群的发展。 NO_3〜-对CH_4的产生没有明显影响。然而,在低N_2O产生的培养中发现了最高的CH_4记录,这表明N_2O可能对产甲烷菌有毒。总而言之,我们的研究表明,将草地转变为FSWW意味着增加N_2O排放的风险。这似乎对CH_4无效。但是,由于N_2O几乎总是在NO_3〜-被反硝化的地方产生,因此湿地中N_2O产量的增加导致下游环境中氮素的减少。因此,我们得出的结论是,在平衡NO_3〜-保留量和全球变暖方面,我们没有理由阻止未来湿地的建立或恢复。

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