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Stem respiration and carbon dioxide efflux of young Populus deltoides trees in relation to temperature and xylem carbon dioxide concentration

机译:杨树幼树的茎呼吸和二氧化碳外流与温度和木质部二氧化碳浓度的关系

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Oxidative respiration is strongly temperature driven. However, in woody stems, efflux of CO2 to the atmosphere (E-A), commonly used to estimate the rate of respiration (R-S), and stem temperature (T-st) have often been poorly correlated, which we hypothesized was due to transport of respired CO2 in xylem sap, especially under high rates of sap flow (f(s)). To test this, we measured E-A, T-st, f(s) and xylem sap CO2 concentrations ([CO2*]) in 3-year-old Populus deltoides trees under different weather conditions (sunny and rainy days) in autumn. We also calculated R-S by mass balance as the sum of both outward and internal CO2 fluxes and hypothesized that R-S would correlate better with T-st than E-A. We found that E-A sometimes correlated well with T-st, but not on sunny mornings and afternoons or on rainy days. When the temperature effect on E-A was accounted for, a clear positive relationship between E-A and xylem [CO2*] was found. [CO2*] varied diurnally and increased substantially at night and during periods of rain. Changes in [CO2*] were related to changes in f(s) but not T-st. We conclude that changes in both respiration and internal CO2 transport altered E-A. The dominant component flux of R-S was E-A. However, on a 24-h basis, the internal transport flux represented 9-18% and 3-7% of R-S on sunny and rainy days, respectively, indicating that the contribution of stem respiration to forest C balance may be larger than previously estimated based on E (A) measurements. Unexpectedly, the relationship between R-S and T-st was sometimes weak in two of the three trees. We conclude that in addition to temperature, other factors such as water deficits or substrate availability exert control on the rate of stem respiration so that simple temperature functions are not sufficient to predict stem respiration.
机译:氧化呼吸强烈地受温度驱动。然而,在木本茎中,通常用于估计呼吸速率(RS)和茎温度(T-st)的二氧化碳向大气(EA)的流出通常不很相关,我们推测这是由于吸收木质部树液中的二氧化碳,特别是在树液流量高的情况下(f(s))。为了测试这一点,我们在秋季在不同天气条件下(晴天和阴雨天)对3岁的胡杨树中的E-A,T-st,f(s)和木质部汁液中的CO2浓度([CO2 *])进行了测量。我们还通过质量平衡将R-S计算为内部和外部CO2通量之和,并假设R-S与T-st的相关性比E-A更好。我们发现E-A有时与T-st相关性很好,但在阳光明媚的早晨和下午或雨天却没有。考虑到温度对E-A的影响,发现E-A与木质部[CO2 *]之间存在明显的正相关关系。 [CO2 *]昼夜变化,并在夜间和下雨期间大幅增加。 [CO2 *]的变化与f(s)的变化有关,但与T-st无关。我们得出的结论是,呼吸和内部CO2传输的变化都改变了E-A。 R-S的主要成分通量为E-A。然而,在24小时的基础上,内部运输通量分别在晴天和阴天代表RS的9-18%和3-7%,这表明茎呼吸对森林C平衡的贡献可能大于先前的估计。基于E(A)的测量结果。出乎意料的是,R-S和T-st之间的关系有时在三棵树中的两棵中很弱。我们得出的结论是,除温度外,其他因素(如水分亏缺或基质利用率)也会影响茎呼吸的速率,因此简单的温度函数不足以预测茎呼吸。

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