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The growth respiration component in eddy CO2 flux from a Quercus ilex mediterranean forest

机译:栎栎地中海森林涡流CO2通量中的生长呼吸成分

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Ecosystem respiration, arising from soil decomposition as well as from plant maintenance and growth, has been shown to be the most important component of carbon exchange in most terrestrial ecosystems. The goal of this study was to estimate the growth component of whole-ecosystem respiration in a Mediterranean evergreen oak (Quercus ilex) forest over the course of 3 years. Ecosystem respiration (R-eco) was determined from night-time carbon dioxide flux (F-c) using eddy correlation when friction velocity (u(*)) was greater than 0.35 m s(-1)We postulated that growth respiration could be evaluated as a residual after removing modeled base R-eco from whole-ecosystem R-eco during periods when growth was most likely occurring. We observed that the model deviated from the night-time F-c-based R-eco during the period from early February to early July with the largest discrepancies occurring at the end of May, coinciding with budburst when active aboveground growth and radial growth increment are greatest. The highest growth respiration rates were observed in 2001 with daily fluxes reaching up to 4 g C m(-2). The cumulative growth respiration for the entire growth period gave total carbon losses of 170, 208, and 142 g C m(-2) for 1999, 2001, and 2002, respectively. Biochemical analysis of soluble carbohydrates, starch, cellulose, hemicellulose, proteins, lignin, and lipids for leaves and stems allowed calculation of the total construction costs of the different growth components, which yielded values of 154, 200, and 150 g C for 3 years, respectively, corresponding well to estimated growth respiration. Estimates of both leaf and stem growth showed very large interannual variation, although average growth respiration coefficients and average yield of growth processes were fairly constant over the 3 years and close to literature values. The time course of the growth respiration may be explained by the growth pattern of leaves and stems and by cambial activity. This approach has potential applications for interpreting the effects of climate variation, disturbances, and management practices on growth and ecosystem respiration.
机译:由土壤分解以及植物的维持和生长引起的生态系统呼吸已被证明是大多数陆地生态系统碳交换的最重要组成部分。这项研究的目的是估计3年间地中海常绿栎树(Quercus ilex)森林中整个生态系统呼吸的增长成分。当摩擦速度(u(*))大于0.35 ms(-1)时,利用涡旋相关性从夜间二氧化碳通量(Fc)确定了生态呼吸(R-eco)。我们假设生长呼吸可以被评估为在最有可能发生增长的时期从整个生态系统R-eco中删除建模的基础R-eco之后的残留量。我们观察到,该模型在2月初至7月初期间偏离了基于Fc的夜间R-eco,最大的差异发生在5月底,与活跃的地上生长和径向生长增量最大的芽期相吻合。 。在2001年观察到最高的呼吸速率,每日通量达到4 g C m(-2)。整个生长时期的累积生长呼吸使1999年,2001年和2002年的总碳损失分别为170、208和142 g C m(-2)。通过对叶和茎的可溶性碳水化合物,淀粉,纤维素,半纤维素,蛋白质,木质素和脂质进行生化分析,可以计算出不同生长组分的总建设成本,这在3年中产生了154、200和150 g C的值分别对应于估计的生长呼吸。叶和茎生长的估计值都显示出很大的年际变化,尽管三年中的平均生长呼吸系数和平均生长过程产量相当恒定,接近文献值。生长呼吸的时间过程可以通过叶子和茎的生长方式以及冈比亚的活动来解释。这种方法在解释气候变化,干扰和管理措施对生长和生态系统呼吸的影响方面具有潜在的应用。

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