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CO2 fluxes of a boreal black spruce chronosequence in eastern North America

机译:北美东部北方黑云杉年代序列的CO2通量

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摘要

Forest harvest and subsequent stand development can have major effects on the carbon cycle of boreal stands. Carbon dioxide (CO2) fluxes of a three-point black spruce harvest chronosequence located in the boreal forest of eastern North America were measured over a one-year period at the ecosystem scale with the eddy covariance technique and CO2 efflux from soils was measured with a portable infrared gas analyzer. The three sites (pre-harvest, recently harvested, and juvenile) were 105-, 8- and 33-years old, respectively. On an annual basis, the pre-harvest site (EOBS) was a weak carbon sink (6 +/- 4 g C m(-2) yr(-1)), the recently harvested site (HBS00) a source (-87 +/- 3 g C m(-2) yr(-1)) and the juvenile site (HBS75) a moderate to strong sink (143 +/- 35 g C m(-2) yr(-1)). Annual gross ecosystem production (GEP) at the pre-harvest site was only 28% greater than at the recently harvested site (646 +/- 6 versus 504 +/- 5 g C m(-2) yr(-1)), while GEP at the juvenile site (1107 +/- 32 g C m(-2) yr(-1)) was more than double that at the recently harvested site, suggesting significant physiological constraints to photosynthesis at the pre-harvest site. Annual ecosystem respiration (R-e) followed the same pattern, but intersite differences were somewhat less (640 +/- 8 to 591 +/- 6 to 964 +/- 50 g C m(-2) yr(-1)). Annual soil respiration (R-s) decreased following harvest from 593 to 500 g C m(-2) yr(-1) and increased with further stand development to 644 g C m(-2) yr(-1), although the changes were less than for GEP and R-e. Q(10) and R-10 of R-s for the snow-free period varied between sites, were lowest for the recently harvested site, and appeared to be related to GEP via substrate supply. The annual ratio of R-s to R-e was lower for the juvenile site (67%) than for the pre-harvest and recently harvested sites (93 and 85%, respectively). These results quantify how some of the major physiological processes that influence the carbon cycle of boreal black spruce stands evolve following harvest and should be useful for better incorporating stand-age effects into regional and global scale models. (C) 2011 Elsevier B.V. All rights reserved.
机译:森林采伐和随后的林分发展会对北方林分的碳循环产生重大影响。使用涡度协方差技术,在生态系统规模下,在一年的时间内测量了位于北美东部寒带森林中的三点黑云杉采伐时间序列的二氧化碳(CO2)通量,并利用碳纳米管测量了土壤中的二氧化碳排放量。便携式红外气体分析仪。这三个地点(收获前,最近收获的地点和少年地点)分别是105岁,8岁和33岁。每年,收割前的土地(EOBS)是弱碳汇(6 +/- 4 g C m(-2)yr(-1)),最近收获的土地(HBS00)是碳源(-87 +/- 3 g C m(-2)yr(-1)和少年部位(HBS75)中等至强沉(143 +/- 35 g C m(-2)yr(-1))。收获前地点的年生态系统总产量(GEP)仅比最近收获的地点高28%(646 +/- 6与504 +/- 5 g C m(-2)yr(-1)),而少年点的GEP(1107 +/- 32 g C m(-2)yr(-1))是最近收获地点的两倍以上,这表明收获前地点的光合作用受到明显的生理限制。年度生态系统呼吸(R-e)遵循相同的模式,但站点间差异略小(640 +/- 8至591 +/- 6至964 +/- 50 g C m(-2)yr(-1))。收获后的年度土壤呼吸(Rs)从593降至500 g C m(-2)yr(-1),并随着林分的进一步发展而增加至644 g C m(-2)yr(-1),尽管变化是小于GEP和Re。在无雪期,R-s的Q(10)和R-10在站点之间变化,对于最近收获的站点最低,并且似乎通过底物供应与GEP有关。幼年地点的R-s与R-e的年比率(67%)低于收获前和最近收获地点的比率(分别为93%和85%)。这些结果量化了影响北方黑云杉林分碳循环的一些主要生理过程在收获后如何演变,并应有助于更好地将年龄效应纳入区域和全球规模模型中。 (C)2011 Elsevier B.V.保留所有权利。

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