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Effects of elevated atmospheric CO2, prolonged summer drought and temperature increase on N2O and CH4 fluxes in a temperate heathland

机译:大气CO2升高,夏季干旱延长和温度升高对温带荒地N2O和CH4通量的影响

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In temperate regions, climate change is predicted to increase annual mean temperature and intensify the duration and frequency of summer droughts, which together with elevated atmospheric carbon dioxide (CO2) concentrations, may affect the exchange of nitrous oxide (N2O) and methane (CH4) between terrestrial ecosystems and the atmosphere. We report results from the CLIMAITE experiment, where the effects of these three climate change parameters were investigated solely and in all combinations in a temperate heathland. Field measurements of N2O and CH4 fluxes took place 1-2 years after the climate change manipulations were initiated. The soil was generally a net sink for atmospheric CH4. Elevated temperature (T) increased the CH4 uptake by on average 10 mu g C m(-2) h(-1), corresponding to a rise in the uptake rate of about 20%. However, during winter elevated CO2 (CO2) reduced the CH4 uptake, which outweighed the positive effect of warming when analyzed across the study period. Emissions of N2O were generally low (< 10 mu g N m(-2) h(-1)). As single experimental factors, elevated CO2, temperature and summer drought (D) had no major effect on the N2O fluxes, but the combination of CO2 and warming (TCO2) stimulated N2O emission, whereas the N2O emission ceased when CO2 was combined with drought (DCO2). We suggest that these N2O responses are related to increased rhizodeposition under elevated CO2 combined with increased and reduced nitrogen turnover rates caused by warming and drought, respectively. The N2O flux in the multifactor treatment TDCO2 was not different from the ambient control treatment. Overall, our study suggests that in the future, CH4 uptake may increase slightly, while N2O emission will remain unchanged in temperate ecosystems on well-aerated soils. However, we propose that continued exposure to altered climate could potentially change the greenhouse gas flux pattern in the investigated heathland
机译:在温带地区,预计气候变化将使年平均温度升高,并加剧夏季干旱的持续时间和频率,这与大气中二氧化碳(CO2)浓度升高一起可能影响一氧化二氮(N2O)和甲烷(CH4)的交换在陆地生态系统和大气之间。我们报告了CLIMAITE实验的结果,在该实验中,仅对了这三个气候变化参数的影响进行了研究,并在温带荒地中对所有这些变化进行了研究。 N2O和CH4通量的现场测量是在气候变化操纵开始后的1-2年进行的。土壤通常是大气中CH4的净汇。升高的温度(T)使CH4的吸收平均增加10μg C m(-2)h(-1),这对应于约20%的吸收率上升。但是,在冬季,较高的CO2(CO2)减少了CH4的吸收,而在整个研究期间进行分析时,其重要性超过了变暖的积极作用。 N2O的排放通常较低(<10μg N m(-2)h(-1))。作为单个实验因素,升高的CO2,温度和夏季干旱(D)对N2O通量没有重大影响,但是CO2和变暖(TCO2)的结合会刺激N2O的排放,而当CO2与干旱结合时N2O的排放会停止( DCO2)。我们建议,这些N2O响应与在升高的CO2下根状沉积的增加以及分别由变暖和干旱引起的氮周转率的增加和减少有关。多因素处理TDCO2中的N2O通量与环境控制处理无差异。总体而言,我们的研究表明,将来在富氧土壤上的温带生态系统中,CH4的吸收可能会略有增加,而N2O的排放量将保持不变。但是,我们建议,持续暴露于气候变化可能会改变调查的欧石南丛生的温室气体通量模式

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