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Patterns of NPP, GPP, respiration, and NEP during boreal forest succession.

机译:北方森林演替过程中NPP,GPP,呼吸和NEP的模式。

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We combined year-round eddy covariance with biometry and biomass harvests along a chronosequence of boreal forest stands that were 1, 6, 15, 23, 40, ~74, and ~154 years old to understand how ecosystem production and carbon stocks change during recovery from stand-replacing crown fire. Live biomass (Clive) was low in the 1- and 6-year-old stands, and increased following a logistic pattern to high levels in the 74- and 154-year-old stands. Carbon stocks in the forest floor (Cforest floor) and coarse woody debris (CCWD) were comparatively high in the 1-year-old stand, reduced in the 6- through 40-year-old stands, and highest in the 74- and 154-year-old stands. Total net primary production (TNPP) was reduced in the 1- and 6-year-old stands, highest in the 23- through 74-year-old stands and somewhat reduced in the 154-year-old stand. The NPP decline at the 154-year-old stand was related to increased autotrophic respiration rather than decreased gross primary production (GPP). Net ecosystem production (NEP), calculated by integrated eddy covariance, indicated the 1- and 6-year-old stands were losing carbon, the 15-year-old stand was gaining a small amount of carbon, the 23- and 74-year-old stands were gaining considerable carbon, and the 40- and 154-year-old stands were gaining modest amounts of carbon. The recovery from fire was rapid; a linear fit through the NEP observations at the 6- and 15-year-old stands indicated the transition from carbon source to sink occurred within 11-12 years. The NEP decline at the 154-year-old stand appears related to increased losses from Clive by tree mortality and possibly from Cforest floor by decomposition. Our findings support the idea that NPP, carbon production efficiency (NPP/GPP), NEP, and carbon storage efficiency (NEP/TNPP) all decrease in old boreal stands.Digital Object Identifier http://dx.doi.org/10.1111/j.1365-2486.2010.02274.x
机译:我们将沿常年,分别为1、6、15、23、40,〜74和〜154年的北方林分的时间序列的全年涡度协方差与生物特征和生物量收获相结合,以了解恢复过程中生态系统产量和碳储量如何变化从替换架子的冠火。 1岁和6岁林分中的活生物量(C live )低,并且在74岁和154岁林分中遵循逻辑模式增加到高水平。在1年生林分中,林地(C forest floor )和粗木屑(C CWD )的碳储量相对较高,而6-到40岁的看台,最高的是74岁和154年的看台。 1年和6年展位的总净初级生产力(TNPP)下降,在23至74年展位中最高,而在154年展位中有所下降。拥有154年历史的树苗的NPP下降与自养呼吸增加有关,而不是与初级生产总值(GPP)下降有关。通过综合涡度协方差计算得出的净生态系统产量(NEP)表示1和6年龄的林分正在减少碳,15年历史的林分正在获得少量的碳,而23年和74年古老的林分获得了可观的碳,而拥有40年和154年历史的林分获得了适度的碳。从火中恢复很快;通过NEP观测值对6岁和15岁展位的线性拟合表明,碳源向碳汇的过渡发生在11-12年内。拥有154年历史的林分的NEP下降似乎与树木死亡导致的C live 损失增加以及分解造成的C 森林地面损失增加有关。我们的发现支持这样的观点,即在旧的寒带林中NPP,碳生产效率(NPP / GPP),NEP和碳存储效率(NEP / TNPP)都会降低。数字对象标识符http://dx.doi.org/10.1111/ j.1365-2486.2010.02274.x

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