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Fire frequency drives decadal changes in soil carbon and nitrogen and ecosystem productivity

机译:火频率驱动土壤碳,氮和生态系统生产力的年代际变化

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Fire frequency is changing globally and is projected to affect the global carbon cycle and climate(1-3). However, uncertainty about how ecosystems respond to decadal changes in fire frequency makes it difficult to predict the effects of altered fire regimes on the carbon cycle; for instance, we do not fully understand the long-term effects of fire on soil carbon and nutrient storage, or whether fire-driven nutrient losses limit plant productivity(4,5). Here we analyse data from 48 sites in savanna grasslands, broadleaf forests and needleleaf forests spanning up to 65 years, during which time the frequency of fires was altered at each site. We find that frequently burned plots experienced a decline in surface soil carbon and nitrogen that was non-saturating through time, having 36 per cent (+/- 13 per cent) less carbon and 38 per cent (+/- 16 per cent) less nitrogen after 64 years than plots that were protected from fire. Fire-driven carbon and nitrogen losses were substantial in savanna grasslands and broadleaf forests, but not in temperate and boreal needleleaf forests. We also observe comparable soil carbon and nitrogen losses in an independent field dataset and in dynamic model simulations of global vegetation. The model study predicts that the long-term losses of soil nitrogen that result from more frequent burning may in turn decrease the carbon that is sequestered by net primary productivity by about 20 per cent of the total carbon that is emitted from burning biomass over the same period. Furthermore, we estimate that the effects of changes in fire frequency on ecosystem carbon storage may be 30 per cent too low if they do not include multidecadal changes in soil carbon, especially in drier savanna grasslands. Future changes in fire frequency may shift ecosystem carbon storage by changing soil carbon pools and nitrogen limitations on plant growth, altering the carbon sink capacity of frequently burning savanna grasslands and broadleaf forests.
机译:火灾频率在全球范围内正在发生变化,预计会影响全球碳循环和气候(1-3)。但是,由于不确定的生态系统如何响应着火频率的年代际变化,因此很难预测火势变化对碳循环的影响。例如,我们不完全了解火灾对土壤碳和养分储存的长期影响,或者火灾导致的养分流失是否会限制植物的生产力(4,5)。在这里,我们分析了长达65年的稀树草原,阔叶林和针叶林的48个站点的数据,在此期间,每个站点的火灾发生频率都发生了变化。我们发现,经常燃烧的地块的表层土壤碳和氮随着时间的推移不饱和,减少了36%(+/- 13%),而碳减少了38%(+/- 16%)。 64年后的氮比受火保护的地块高。以火为动力的碳和氮的损失在热带草原和阔叶林中相当可观,而在温带和北方针叶林中则不然。我们还在独立的田间数据集和全球植被的动态模型模拟中观察到可比的土壤碳和氮损失。该模型研究预测,由于频繁燃烧而造成的长期土壤氮损失可能反过来将净初级生产力所隔离的碳减少了在同一时间燃烧生物质所排放的总碳的约20%。期。此外,我们估计,如果不包括土壤碳的多年代变化,尤其是在较干旱的热带稀树草原上,火灾频率的变化对生态系统碳存储的影响可能太低了30%。未来火灾频率的变化可能会通过改变土壤碳库和氮对植物生长的限制,改变经常燃烧的稀树草原和阔叶林的碳汇能力,从而改变生态系统的碳储量。

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  • 来源
    《Nature》 |2018年第7687期|194-198|共5页
  • 作者单位

    Stanford Univ, Dept Earth Syst Sci, Stanford, CA 94305 USA;

    Stanford Univ, Dept Earth Syst Sci, Stanford, CA 94305 USA|Lund Univ, Dept Phys Geog & Ecosyst Sci, Lund, Sweden;

    Univ Minnesota, Dept Ecol Evolut & Behav, St Paul, MN 55108 USA;

    Univ Minnesota, Dept Forest Resources, St Paul, MN 55108 USA|Western Sydney Univ, Hawkesbury Inst Environm, Sydney, NSW, Australia;

    Lund Univ, Ctr Environm & Climate Res, CEC, Lund, Sweden;

    Yale Univ, Dept Ecol & Evolutionary Biol, New Haven, CT 06520 USA;

    Univ Wisconsin, Coll Nat Resources, Stevens Point, WI 54481 USA;

    Kansas State Univ, Div Biol, Ackert Hall, Manhattan, KS 66506 USA;

    Univ Utah, Dept Biol, Salt Lake City, UT 84112 USA;

    Univ Calif Irvine, Dept Earth Syst Sci, Irvine, CA 92697 USA;

    Stanford Univ, Dept Earth Syst Sci, Stanford, CA 94305 USA|Stanford Univ, Woods Inst Environm, Stanford, CA 94305 USA|Stanford Univ, Precourt Inst Energy, Stanford, CA 94305 USA;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);美国《化学文摘》(CA);
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  • 正文语种 eng
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  • 入库时间 2022-08-18 02:51:26

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