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Production, respiration, and overall carbon balance in an old-growth Pseudotsuga-tsuga forest ecosystem

机译:古老的假tsu--森林生态系统中的生产,呼吸和总体碳平衡

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Ground-based measurements of stores, growth, mortality, litterfall, respiration, and decomposition were conducted in an old-growth forest at Wind River Experimental Forest, Washington, USA. These measurements were used to estimate gross primary production (GPP) and net primary production (NPP); autotrophic respiration (R-a) and heterotrophic (R-h) respiration; and net ecosystem production (NEP). Monte Carlo methods were used to calculate uncertainty (expressed as +/- 2 standard deviations of 200-400 calculations). Live carbon (C) stores were 39,800 g C m(-2) (34,800-44,800 g C m(-2)). The store of C in detritus and mineral soil was 22,092 g C m(-2) (20,600-23,600 g C m(-2)), and the total C stores were 61,899 g C m(-2) (56,600-67,700 g C m(-2)). Total NPP was 597 g C m(-2) y(-1) (453 to 741 g C m(-2) y(-1)). R-a was 1309 g C m(-2) y(-1) (845-1773 g C m(-2) y(-1)), indicating a GPP of 1906 g C m(-2) y(-1) (1444-2368 g C m(-2) y(-1)). R-h, including the respiration of heart rots in tree boles, was 577 g C m(-2) y(-1) (479-675 g C m(-2) y(-1)). Long-term NEP was estimated to be +20 g C m(-2) y(-1) (-116 to +156 g C m(-2) y(-1)), indicating this stand might be a small sink. These estimates contrast with the larger sink estimated at the same site using eddy-flux methods. Several hypotheses to explain this discrepancy were explored, including (a) undetected biomass increases, (b) underestimates of NPP, (c) unmeasured losses, and (d) a temporal mismatch between the two sets of measurements. The last hypothesis appears the most likely.
机译:在美国华盛顿的风河实验林的一个老树森林中进行了地面存储,生长,死亡率,凋落物,呼吸和分解的测量。这些测量被用来估计初级总产值(GPP)和净初级产值(NPP)。自养呼吸(R-a)和异养呼吸(R-h);和净生态系统产量(NEP)。蒙特卡罗方法用于计算不确定性(表示为200-400计算的+/- 2标准偏差)。活性碳(C)储存量为39,800 g C m(-2)(34,800-44,800 g C m(-2))。碎屑和矿物土壤中的C储量为22,092 g C m(-2)(20,600-23,600 g C m(-2)),总C储量为61,899 g C m(-2)(56,600-67,700 g C m(-2))。总NPP为597 g C m(-2)y(-1)(453至741 g C m(-2)y(-1))。 Ra为1309 g C m(-2)y(-1)(845-1773 g C m(-2)y(-1)),表明GPP为1906 g C m(-2)y(-1) (1444-2368 g C m(-2)y(-1))。 R-h包括树干中心腐的呼吸作用为577 g C m(-2)y(-1)(479-675 g C m(-2)y(-1))。长期NEP估计为+20 g C m(-2)y(-1)(-116至+156 g C m(-2)y(-1)),这表明该林地可能是一个小水池。这些估计值与使用涡流方法在同一位置估计的较大汇形成对比。探索了几种假设来解释这种差异,包括(a)未检测到的生物量增加,(b)对NPP的低估,(c)未测量的损失,以及(d)两组测量之间的时间不匹配。最后一个假设最有可能出现。

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