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首页> 外文期刊>International Journal of Biometeorology >Incorporating diffuse photosynthetically active radiation in a single-leaf model of canopy photosynthesis for a 56-year-old Douglas-fir forest
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Incorporating diffuse photosynthetically active radiation in a single-leaf model of canopy photosynthesis for a 56-year-old Douglas-fir forest

机译:在56岁的道格拉斯冷杉林冠层光合作用的单叶模型中纳入漫射光合作用的辐射

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A simple top-down model of canopy photosynthesis (P) was developed and tested in this study. The model (referred to as the Qe-MM model) is P = αQ e P max/(αQ e + P max), α and P max are quantum-use efficiency and potential P, respectively. Q e is given by Q d 0 + kQ b 0, where Q d 0 and Q b 0 are the diffuse and direct photosynthetically active radiation (PAR) incident on the canopy, respectively. Q e can be considered to be the effective incident PAR contributing to P and k is a measure of the contribution of Q b 0 to Q e. When k = 1, the Qe-MM model becomes the regular Michaelis-Menten type model of P (referred to as the MM model). A major objective of this study was to determine how well the Qe-MM model could estimate P of a 56-year-old coastal Douglas-fir stand. To this end, we parameterized the Qe-MM model using five and half years of eddy-covariance measurements of CO2 flux above the Douglas-fir stand. The Qe-MM model, with the incorporation of a function of air temperature, accounted for 74% of the variance in over 34,000 half-hourly P measurements. P estimated using the Qe-MM model had no systematic errors with respect to Q d 0. Although the Qe-MM model has only one more parameter than the MM model, it accounted for 30% more variance in P than the latter when total incident PAR exceeded 900 μmol m−2 s−1. On average, k was found to be 0.22. We show that this small value of k reflects the significant effect of the scattering of the solar beam and the fraction of light-limited sunlit leaves. We also show that the success of the Qe-MM model was due to the fact that a large fraction of the sunlit leaves were light-limited as a result of their orientation to the solar beam. Keywords Canopy photosynthesis - Eddy covariance - Light-use efficiency - Photosynthetically active radiation - Single-leaf photosynthesis model
机译:在这项研究中开发并测试了一个简单的自上而下的冠层光合作用(P)模型。该模型(称为Q e -MM模型)为P =αQ e P max /(αQ e + P max ),α和P max 分别是量子利用效率和电势P。 Q e 由Q d 0 + kQ b 0 给出,其中Q d 0 和Q b 0 是入射在冠层上的散射光和直接光合有效辐射(PAR),分别。 Q e 可以被认为是对P起作用的有效事件PAR,而k是对Q b 0 对Q < sub> e 。当k = 1时,Q e -MM模型成为P的常规Michaelis-Menten类型模型(称为MM模型)。这项研究的主要目的是确定Q e -MM模型可以很好地估计56岁沿海道格拉斯冷杉林分的P。为此,我们使用了道格拉斯冷杉台架上方CO 2 通量的涡流-协方差测量的五年半,对Q e -MM模型进行了参数化。 Q e -MM模型结合了气温函数,在超过34,000个半小时P测量值中占74%的方差。使用Q e -MM模型估计的P相对于Q d 0 没有系统误差。尽管Q e -MM模型仅比MM模型多一个参数,但是当总入射PAR超过900μmolm −2 <时,它比P模型要多30%。 / sup> s -1 。平均而言,k为0.22。我们表明,k的这个小值反映了太阳光束的散射和有限的阳光照射叶片的分数的重大影响。我们还表明,Q e -MM模型的成功是由于以下事实:大部分阳光照射的叶子由于它们朝向太阳束而受到光的限制。关键词冠层光合作用-涡动协方差-光利用效率-光合有效辐射-单叶光合作用模型

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