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Allocation of forest biomass across broad precipitation gradients in China’s forests

机译:中国森林广泛降水梯度的森林生物量分配

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Forests act as major sinks for atmospheric CO2. An understanding of the relationship between forest biomass allocation and precipitation gradients is needed to estimate the impacts of changes in precipitation on carbon stores. Biomass patterns depend on tree size or age, making it unclear whether biomass allocation is limited by tree age at regional scales. Using a dataset of ten typical forest types spanning a large age scale, we evaluated forest biomass allocation–precipitation correlations with the aim of testing whether biomass allocation patterns vary systematically in response to altered precipitation. With increasing mean annual precipitation, a significant quadratic increase occurred in ≤30?yr and 60?yr groups in stem biomass, 60?yr group in branch biomass, and 60?yr groups in leaf biomass; and a significant cubic increase occurred in 30–60?yr and all age forest groups in stem biomass, ≤30?yr, 30–60?yr and all age forest groups in branch biomass, ≤30?yr and all age forest groups in leaf biomass, and in each group in root biomass, indicating that organ biomass is strongly limited by precipitation. Thus, forest biomass responds predictably to changes in mean annual precipitation. The results suggest that forest organ biomass–precipitation relationships hold across independent datasets that encompass a broad climatic range and forest age.
机译:森林充当大气二氧化碳的主要水槽。需要了解森林生物量分配和降水梯度之间的关系,以估算碳储存降水变化的影响。生物质图案依赖于树尺寸或年龄,缺乏生物量分配是否受区域尺度的树龄的限制。利用跨越大年龄级别的十种典型森林类型的数据集,我们评估了森林生物量分配 - 降水相关性,目的是测试生物质分配模式是否有效地变化,响应于改变的降水。随着平均年降水量的增加,在茎生物质中的≤30℃和> 60·YR基团中发生显着的二次增加,> 60?YR组在枝生物质中,>叶片生物质中的60〜YR组;在30-60岁的情况下发生重大的立方体增加,茎生物质的所有年龄森林群体,≤30?Yr,30-60?Yr和枝生物质的所有年龄森林群,≤30?Yr和所有年龄森林群体叶生物质,以及根生物质中的每组中,表明器官生物量受到沉淀的强烈限制。因此,森林生物量可预测地响应平均年降水量的变化。结果表明,森林器官生物量 - 降水关系持有独立的数据集,包括广泛的气候范围和森林时代。

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