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Greenhouse gas fluxes under drought and nitrogen addition in a Southern California grassland

机译:在南加州草原的干旱和氮气添加下温室气体助气

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Climate and regional air quality models predict that Southern California will experience longer and more severe droughts, and possibly wetter, more intense storms and changing nitrogen (N) deposition. We investigated how the three major soil greenhouse gas (GHG) fluxes respond to 4-6 years of exposure to a full-factorial experiment of reduced and augmented precipitation crossed with increased N in a semi-arid grassland in Irvine, CA, USA. The mean emission fluxes across all treatments were 249.8 mg CO2 m(-2) h(-1), -16.41 mu g CH4 m(-2) h(-1), and 2.24 mu g N2O m(-2) h(-1). Added N plots released 3.5 times more N2O than ambient N plots, and N treatment and soil moisture interacted, such that volumetric soil moisture in added N plots correlated positively with N2O release. Soil moisture, which was higher in the added water plots, correlated positively with respiration. CH4 consumption increased with soil moisture in the drought treatment, an opposite trend to that observed in most other studies.
机译:气候和区域空气质量模型预测,南加州将经历更长,更严重的干旱,并且可能更潮湿,更强烈的风暴和改变氮气(n)沉积。我们调查了三大土壤温室气体(GHG)助势如何应对4-6多年的暴露于美国欧文,加利福尼亚州伊尔文伊尔文中的半干旱草原上的减少和增强降水的全部因子试验。所有处理中的平均发射通量为249.8mg CO 2 M(-2)H(-1),-16.41μgch 4 m(-2)h(-1)和2.24μgn2Om(-2)h( -1)。添加了N个图释放了3.5倍的N2O,而不是环境N图,N个处理和土壤水分相互作用,使得添加的n块释放的容量土壤水分与N2O释放相关。在添加的水图中较高的土壤水分,随着呼吸呈正相关。 CH4消费随着干旱治疗的土壤水分而增加,在大多数其他研究中观察到的相反趋势。

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