在阿拉斯加的沿海多边形原中,热石岩景观表现出大量的氧化排放
Josh Hashemi1,2,3, David A Lipson1, Kyle A Arndt4
1Biology Department, San Diego State University, San Diego, CA USA.
概括
北极热地景观是氧化 (N2O) 排放的重要来源. 这些无植被,退化的原特征以与其他排放热点相比的速度释放N2O,影响温室气体预算.
科学领域:
- 环境科学 环境科学
- 地质科学是地球科学.
- 气候科学 气候科学
背景情况:
- 全球二氧化 (N2O) 度正在上升,北极地区成为其中的主要贡献者.
- 热岩石过程降解了原,形成了无植被,排水良好的土壤,释放N2O.
研究的目的:
- 量化阿拉斯加北坡的热岩特征的N2O排放量.
- 确定控制这些景观中N2O排放变化的因素.
主要方法:
- 来自无植物高中心多边形的N2O流量的室内测量.
- 同位素分析 (15N丰富) 以推断微生物过程的贡献 (脱化,化).
主要成果:
- 在生长季节测量高N2O排放量 (中位数为104.7μg N2O-N m-2 h-1) 的无植物多边形.
- 排放量明显高于北极原湿地,类似于其他没有植被的热点.
- 同位素数据表明,在荒的土壤中,微生物过程起着主导作用.
结论:
- 热石岩特征,尽管占地面积小 (约1.5%),但是N2O的显著来源.
- 生长季节的排放 (16 mg N2O-N ha-1 h-1) 可能会显著影响景观层面的温室气体预算.
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