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Biometric and eddy-covariance based estimates of carbon fluxes in an age-sequence of temperate pine forests

机译:基于生物统计和涡度协方差的温带松林年龄序列中碳通量的估算

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摘要

We present four years (2005-2008) of biometric (B) and eddy-covariance (EC) measurements of carbon (C) fluxes to constrain estimates of gross primary production (GPP), net primary production (NPP), ecosystem respiration (RE) and net ecosystem production (NEP) in an age-sequence (6-, 19-, 34-, and 69-years-old in 2008) of pine forests in southern Ontario, Canada. The contribution of individual NPP and respiration component fluxes varied considerably across the age-sequence, introducing different levels of uncertainty. Biometric and EC-based estimates both suggested that annual NPP, GPP, RE, and NEP were greatest at the 19-year-old site. Four-year mean values of NEP(B) and NEP(EC) were similar at the 6-year-old seedling (77 and 66 g C m(-2) y(-1)) and the 69-year-old mature site (135 and 124 g C m(-2) y(-1)), but differed considerably at the 19-year-old (439 and 736 g C m(-2) y(-1)) and the 34-year-old sites (170 and 392 g C m(-2) y(-1)). Both methods suggested similar patterns for inter-annual variability in GPP and NEP. Multi-year convergence of NEP(B) and NEP(EC) was not observed over the study period. Ecosystem C use efficiency was correlated to both forest NEP(EC) and NPP(B) suggesting that high productive forests (e.g. middle-age stands) were more efficient in sequestering C compared to low productive forests (e.g. seedling and mature stands). Similarly, negative and positive relationships of forest productivity with the total belowground C flux (TBCF) to GPP ratio and with the ratio of autotrophic to heterotrophic respiration (RA:RH), respectively, determined inter-annual and inter-site differences in C allocation. Integrating NEP across the age-sequence resulted in a total net C sequestration of 137 and 229 t C ha(-1) over the initial 70 years as estimated by the biometric and EC method, respectively. Total ecosystem C sequestered in biomass at the 69-year-old site suggested an accumulation of 160 t Char. These three estimates resulted in a mean C sequestration of 175 +/- 48 t C ha(-1). This study demonstrates that comparing estimates from independent methods is imperative to constrain C budgets and C dynamics in forest ecosystems
机译:我们提出了四年(2005-2008年)的碳(C)通量的生物特征(B)和涡旋协方差(EC)测量,以限制对总初级生产(GPP),净初级生产(NPP),生态系统呼吸(RE)的估计)和加拿大安大略省南部松树林的年龄序列(2008年分别为6岁,19岁,34岁和69岁)的净生态系统产量(NEP)。各个NPP和呼吸成分通量的贡献在整个年龄序列中差异很大,从而带来了不同程度的不确定性。基于生物识别和基于EC的估计都表明,在19岁的站点上,年度NPP,GPP,RE和NEP最高。在6岁的幼苗(77和66 g C m(-2)y(-1)和69岁的幼苗上,NEP(B)和NEP(EC)的四年平均值相似网站(135和124 g C m(-2)y(-1)),但在19岁年龄段(439和736 g C m(-2)y(-1))和34-岁的网站(170和392 g C m(-2)y(-1))。两种方法都为GPP和NEP中的年际可变性提出了相似的模式。在研究期间未观察到NEP(B)和NEP(EC)的多年收敛。生态系统C的利用效率与森林NEP(EC)和NPP(B)均相关,这表明高生产力森林(例如中年林分)比低生产力森林(例如苗木和成熟林分)更有效地封存C.同样,森林生产力与地下总碳通量(TBCF)与GPP比率以及自养与异养呼吸的比率(RA:RH)的负向和正向关系分别确定了碳分配的年际差异和站点间差异。通过生物测定法和EC方法分别估算,在整个年龄序列中对NEP进行积分后,在最初的70年中,总净C螯合量分别为137 t和229 t C ha(-1)。在这个拥有69年历史的地点隔离的生物量中,总生态系统C的蓄积量为160 t Char。这三个估计值导致平均C螯合为175 +/- 48 t C ha(-1)。这项研究表明,比较来自独立方法的估计值对于约束森林生态系统中的碳预算和碳动态是必不可少的。

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