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首页> 外文期刊>Global change biology >Effects of an experimental drought and recovery on soil emissions of carbon dioxide, methane, nitrous oxide, and nitric oxide in a moist tropical forest
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Effects of an experimental drought and recovery on soil emissions of carbon dioxide, methane, nitrous oxide, and nitric oxide in a moist tropical forest

机译:实验性干旱和恢复对湿润热带森林中二氧化碳,甲烷,一氧化二氮和一氧化氮的土壤排放的影响

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摘要

Changes in precipitation in the Amazon Basin resulting from regional deforestation, global warming, and El Nino events may affect emissions of carbon dioxide (CO sub(2)), methane (CH sub(4)), nitrous oxide (N sub(2)O), and nitric oxide (NO) from soils. Changes in soil emissions of radiatively important gases could have feedback implications for regional and global climate. Here, we report the final results of a 5-year, large-scale (1ha) throughfall exclusion experiment, followed by 1 year of recovery with natural throughfall, conducted in a mature evergreen forest near Santarem, Brazil. The exclusion manipulation lowered annual N sub(2)O emissions in four out of five treatment years (a natural drought year being the exception), and then recovered during the first year after the drought treatment stopped. Similarly, consumption of atmospheric CH sub(4) increased under drought treatment, except during a natural drought year, and it also recovered to pretreatment values during the first year that natural throughfall was permitted back on the plot. No treatment effect was detected for NO emissions during the first 3 treatment years, but NO emissions increased in the fourth year under the extremely dry conditions of the exclusion plot during a natural drought. Surprisingly, there was no treatment effect on soil CO sub(2) efflux in any year. The drought treatment provoked significant tree mortality and reduced the allocation of C to stems, but allocation of C to foliage and roots were less affected. Taken together, these results suggest that the dominant effect of throughfall exclusion on soil processes during this 6-year period was on soil aeration conditions that transiently affected CH sub(4), N sub(2)O, and NO production and consumption.
机译:区域性森林砍伐,全球变暖和厄尔尼诺事件造成的亚马逊盆地降水变化可能影响二氧化碳(CO sub(2)),甲烷(CH sub(4)),一氧化二氮(N sub(2))的排放O)和土壤中的一氧化氮(NO)。辐射性重要气体在土壤中的排放变化可能会对区域和全球气候产生反馈影响。在此,我们报告了在巴西圣塔伦附近的一个成熟的常绿森林中进行的一项为期5年的大规模(1ha)穿透降雨排除实验的最终结果,然后是通过自然穿透恢复1年的最终结果。排除操作降低了五个处理年中的四个处理年(自然干旱年除外)中的年N sub(2)O排放量,然后在干旱处理停止后的第一年恢复了。同样,在干旱处理下,大气CH sub(4)的消耗量增加了,除了在自然干旱的年份外,在第一年也恢复了预处理值,允许自然穿透重新回到样地。在前3个处理年中未检测到NO排放的处理效果,但在自然干旱期间,在禁区的极端干旱条件下,第4年NO排放增加。令人惊讶的是,任何一年都没有对土壤CO sub(2)外流的处理效果。干旱处理激起了很高的树木死亡率,并减少了碳在茎上的分配,但碳在叶子和根部的分配受到的影响较小。综上所述,这些结果表明,在这6年中,排除通流对土壤过程的主要影响是对土壤通气条件的影响,该条件暂时影响CH sub(4),N sub(2)O和NO的产生和消耗。

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