细菌脱驱动在干旱的加利福尼亚南部干旱地区增加N2O排放
Alexander H Krichels1,2,3, G Darrel Jenerette2,4, Hannah Shulman5,6
1Environmental Sciences, University of California, Riverside, CA, USA.
沙漠土壤,即使经过极度干旱,也可以在湿时立即排放氧化 (N2O). 细菌脱剂耐受恶劣的条件,并在降雨后迅速产生这种强大的温室气体.
科学领域:
- 环境科学 环境科学
- 微生物学 微生物学
- 土壤科学 土壤科学
背景情况:
- 土壤是大气氧化 (N2O) 的主要来源,这是一个强大的温室气体.
- 脱化,主要的N2O生产过程,通常需要无氧条件,这在干燥的土壤中很少见.
研究的目的:
- 调查是否可以在极端干旱中生存,并在湿沙漠土壤后立即产生N2O.
- 了解重新灌干旱土壤快速排放N2O背后的微生物机制.
主要方法:
- 在加利福尼亚沙漠生态系统中利用同位素和分子方法.
- 测量N2O排放和分析微生物基因表达 (酸盐降低转录).
- 评估了抑制微生物活动对N2O排放的影响.
主要成果:
- 脱剂在15分钟内使干燥的土壤湿后产生了N2O.
- 在干燥的土壤中检测到降低酸盐的转录,表明休眠的微生物种群.
- 抑制微生物活动减少了59%的N2O排放.
结论:
- 细菌脱剂可以承受极端的干旱 (几个月没有雨,高温,低含水量).
- 这些有弹性的脱剂是导致沙漠土壤湿后立即排放的大多数N2O的原因.
- 这些发现挑战了干旱土壤在干旱时期对N2O生产不活跃的假设.
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