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Spatial and Temporal Variations in Aboveground Woody Carbon Storage for Cerrado Forests and Woodlands of Mato Grosso, Brazil

机译:巴西马托格罗索林地的地上木质碳储存的空间和时间变化

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Tropical forests and savanna account for nearly 65% of the total global terrestrial net primary production (NPP); however, there are still large uncertainties in tropical forest NPP because of limited field measurements, especially in the structurally diverse Brazilian savanna (cerrado). To address this uncertainty, we measured patterns of aboveground wood C stocks (C_w) and rates of wood C storage (ΔC_w) over a 7-year period for cerrado forests and woodlands of southern Mato Grosso, Brazil, arrayed across hydrological and soil fertility gradients. We focused on ΔC_w because it is an important component of NPP, and wood is a stable, long-term, C storage reservoir. Annual rates of ΔC_w were significantly affected by estimates of P and cation (K and Ca) availability, and analysis of covariance indicated that relationships between ΔC_w and nutrient availability were independent of stand hydrology. Both upland and hyperseasonal stands exhibited a decline in ΔC_w during the 2015-16 El Ni?o event, which was exceptionally warm and dry. A limited analysis of the uncertainty associated with the field measurements ranged from 7% for wood density to 24% for tree density, while the uncertainty associated with derived quantities ranged from 10% for tree height to 41% for C_w. Overall, these results suggest that soil fertility and annual precipitation are important drivers of ΔC_w and that warming and drying associated with climate change will cause a decline in aboveground woody C storage for these, and similar, tropical forests and woodlands.
机译:热带森林和大草原占全球全球陆地净初级生产(NPP)的近65%;然而,由于现场测量有限,特别是在结构多样化的巴西大草原(Cerrado)中,热带森林NPP仍存在大的不确定性。为了解决这种不确定性,我们在巴西Mato Grosso Southern森林和林地的7年期间测量了地上木C股(C_W)和木材储存(ΔC_W)的速率,横跨水文和土壤肥力梯度排列。我们专注于ΔC_W,因为它是NPP的重要组成部分,木材是一个稳定,长期的C存储储存器。通过P和阳离子(k和CA)可用性的估计,ΔC_w的年度率显着影响,并且协方差分析表明ΔC_W和养分可用性之间的关系与实体水文无关。普满和高度暂停的立场都在2015-16 El Ni的ΔC_W中表现出ΔC_W的ΔC_W,其出现异常温暖和干燥。对与场测量相关的不确定性的有限分析范围从木质密度的7%到树密度的24%,而与衍生量相关的不确定性为树高的10%至41%的C_W。总体而言,这些结果表明,土壤肥力和年降水是ΔC_W的重要驱动因素,与气候变化相关的变暖和干燥将导致这些木质储存的下降,以及类似,热带森林和林地。

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