Center for Permafrost, Department of Geosciences and Natural Resource Management, University of Copenhagen, 1350 Copenhagen K, Denmark.
Center for Permafrost, Department of Geosciences and Natural Resource Management, University of Copenhagen, 1350 Copenhagen K, Denmark.
Sci Total Environ. 2021 Nov 15;795:148847. doi: 10.1016/j.scitotenv.2021.148847. Epub 2021 Jul 3.
The frequency and severity of fire is increasing in Arctic tundra regions with climate change. Here we investigated effects of experimental low-intensity fire and shrub cutting, in combination with warming, on soil biogeochemical cycles and post-fire greenhouse gas (GHG) emissions in a dry heath tundra, West Greenland. We performed in vitro incubation experiments based on soil samples collected for up to two years after the fire. We observed tendency for increased soil nitrate (14-fold) and significant increases in soil ammonium and phosphate (four-fold and five-fold, respectively) two years after the fire, but no effects of shrub cutting on these compounds. Thus, changes appear to be largely due to fire effects rather than indirect effects by vegetation destruction. Two years after fire, nitrous oxide (NO) and carbon dioxide (CO) production was significantly increased (three-fold and 32% higher, respectively), in burned than unburned soils, while methane (CH) uptake remained unchanged. This stimulated NO and CO production by the fire, however, was only apparent under conditions when soil was at maximum water holding capacity, suggesting that fire effects can be masked under dry conditions in this tundra ecosystem. There were positive effects by modest 2.5 °C warming on CO production in control but not in burned soils, suggesting that fire may decrease the temperature response in soil respiration. Methane uptake was neither altered by the modest warming in shrub-cut nor in burned soils after two years, suggesting that the removal of vegetation may play a key role in controlling future temperature response of CH oxidation. Altogether, our results show that post-fire tundra soils have the potential to enhance soil GHG emissions (e.g. NO and CO) especially during episodes with wet soil conditions. On the other hand, the lack of warming responses in post-fire soil respiration may weaken this positive feedback to climate change.
随着气候变化,北极苔原地区的火灾频率和严重程度正在增加。在这里,我们研究了低强度实验火灾和灌木砍伐,以及与变暖相结合,对格陵兰西部干燥石楠苔原土壤生物地球化学循环和火灾后温室气体(GHG)排放的影响。我们基于火灾后最多两年内采集的土壤样本进行了体外孵育实验。我们观察到火灾后两年土壤硝酸盐(增加 14 倍)和土壤铵和磷酸盐(分别增加 4 倍和 5 倍)有增加的趋势,但灌木砍伐对这些化合物没有影响。因此,这些变化似乎主要是由于火灾的影响,而不是由于植被破坏的间接影响。火灾后两年,与未燃烧土壤相比,燃烧土壤中的氧化亚氮(NO)和二氧化碳(CO)的产生显著增加(分别增加了 3 倍和 32%),而甲烷(CH)的吸收保持不变。火灾导致的这种硝化和 CO 产生的刺激作用仅在土壤持水能力达到最大值的情况下才明显,这表明在这种苔原生态系统中,火灾的影响可能会在干燥条件下被掩盖。适度 2.5°C 的变暖对对照土壤中的 CO 产生有积极影响,但对燃烧土壤没有影响,这表明火灾可能会降低土壤呼吸对温度的响应。灌木砍伐或燃烧后两年,适度变暖对 CH 氧化的土壤吸收没有影响,这表明植被的去除可能在控制未来 CH 氧化的温度响应方面发挥关键作用。总的来说,我们的结果表明,火灾后的苔原土壤具有增强土壤 GHG 排放(例如 NO 和 CO)的潜力,尤其是在土壤湿润条件下。另一方面,火灾后土壤呼吸对变暖没有响应,这可能会削弱这种对气候变化的正反馈。