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巴西季节性干旱热带森林净生态系统 CO2 交换的季节变化。

Seasonal variation in net ecosystem CO exchange of a Brazilian seasonally dry tropical forest.

机构信息

Climate Sciences Post-graduate Program, Federal University of Rio Grande do Norte, Av. Senador Salgado Filho, 3000, Zip Code 59078-970, Lagoa Nova, Natal, Brazil.

Meteorology Post-graduate Program, Federal University of Campina Grande, Rua Aprígio Veloso, 882, Zip Code 58429-900, Universitário, Campina Grande, Brazil.

出版信息

Sci Rep. 2020 Jun 11;10(1):9454. doi: 10.1038/s41598-020-66415-w.

Abstract

Forest ecosystems sequester large amounts of atmospheric CO, and the contribution from seasonally dry tropical forests is not negligible. Thus, the objective of this study was to quantify and evaluate the seasonal and annual patterns of CO exchanges in the Caatinga biome, as well as to evaluate the ecosystem condition as carbon sink or source during years. In addition, we analyzed the climatic factors that control the seasonal variability of gross primary production (GPP), ecosystem respiration (R) and net ecosystem CO exchange (NEE). Results showed that the dynamics of the components of the CO fluxes varied depending on the magnitude and distribution of rainfall and, as a consequence, on the variability of the vegetation state. Annual cumulative NEE was significantly higher (p < 0.01) in 2014 (-169.0 g C m) when compared to 2015 (-145.0 g C m) and annual NEP/GPP ratio was 0.41 in 2014 and 0.43 in 2015. Global radiation, air and soil temperature were the main factors associated with the diurnal variability of carbon fluxes. Even during the dry season, the NEE was at equilibrium and the Caatinga acted as an atmospheric carbon sink during the years 2014 and 2015.

摘要

森林生态系统大量地固定大气中的 CO,而季节性干旱热带森林的贡献不容忽视。因此,本研究的目的是量化和评估卡廷加生物群落 CO 交换的季节性和年度模式,并评估生态系统作为碳汇或碳源的状况。此外,我们分析了控制总初级生产力(GPP)、生态系统呼吸(R)和净生态系统 CO 交换(NEE)季节性变化的气候因素。结果表明,CO 通量组成部分的动态变化取决于降雨量的大小和分布,从而影响植被状态的变化。与 2015 年(-145.0 g C m)相比,2014 年(-169.0 g C m)的年累积 NEE 显著更高(p < 0.01),2014 年的年 NEP/GPP 比为 0.41,2015 年为 0.43。总辐射、空气和土壤温度是与碳通量日变化相关的主要因素。即使在旱季,NEE 也处于平衡状态,卡廷加在 2014 年和 2015 年期间充当大气碳汇。

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