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Carbon sequestration potential of tropical pasture compared with afforestation in Panama

机译:与巴拿马的造林相比,热带牧场的固碳潜力

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Tropical forest ecosystems play an important role in regulating the global climate, yet deforestation and land-use change mean that the tropical carbon sink is increasingly influenced by agroecosystems and pastures. Despite this, it is not yet fully understood how carbon cycling in the tropics responds to land-use change, particularly for pasture and afforestation. Thus, the objectives of our study were: (1) to elucidate the environmental controls and the impact of management on gross primary production (GPP), total ecosystem respiration (TER) and net ecosystem CO2 exchange (NEE); (2) to estimate the carbon sequestration potential of tropical pasture compared with afforestation; and (3) to compare eddy covariance-derived carbon budgets with biomass and soil inventory data. We performed comparative measurements of NEE in a tropical C-4 pasture and an adjacent afforestation with native tree species in Sardinilla (Panama) from 2007 to 2009. Pronounced seasonal variation in GPP, TER and NEE were closely related to radiation, soil moisture, and C-3 vs. C-4 plant physiology. The shallow rooting depth of grasses compared with trees resulted in a higher sensitivity of the pasture ecosystem to water limitation and seasonal drought. During 2008, substantial amounts of carbon were sequestered by the afforestation (-442 gCm(-2), negative values denote ecosystem carbon uptake), which was in agreement with biometric observations (-450 gCm(-2)). In contrast, the pasture ecosystem was a strong carbon source in 2008 and 2009 (261 gCm(-2)), associated with seasonal drought and overgrazing. In addition, soil carbon isotope data indicated rapid carbon turnover after conversion from C-4 pasture to C-3 afforestation. Our results clearly show the potential for considerable carbon sequestration of tropical afforestation and highlight the risk of carbon losses from pasture ecosystems in a seasonal tropical climate.
机译:热带森林生态系统在调节全球气候中起着重要作用,但是森林砍伐和土地利用的变化意味着热带碳汇越来越受到农业生态系统和牧场的影响。尽管如此,人们尚未完全了解热带地区的碳循环如何响应土地利用变化,特别是对牧场和造林而言。因此,我们的研究目标是:(1)阐明环境控制和管理对初级生产总值(GPP),总生态系统呼吸(TER)和净生态系统CO2交换(NEE)的影响; (2)估算与绿化相比热带牧场的固碳潜力; (3)将涡度协方差衍生的碳预算与生物量和土壤清单数据进行比较。我们从2007年至2009年在热带C-4牧场和附近撒丁岛(巴拿马)的原生树种造林中进行了NEE的比较测量。GPP,TER和NEE中明显的季节性变化与辐射,土壤湿度和土壤湿度密切相关。 C-3对C-4植物生理学。与树木相比,草的浅生根深度导致牧场生态系统对水分限制和季节性干旱的敏感性更高。 2008年期间,植树造林封存了大量碳(-442 gCm(-2),负值表示生态系统碳吸收),这与生物特征观测结果一致(-450 gCm(-2))。相反,牧场生态系统在2008年和2009年是重要的碳源(261 gCm(-2)),与季节性干旱和过度放牧有关。此外,土壤碳同位素数据表明,从C-4牧场转换为C-3造林后,碳的周转速度很快。我们的结果清楚地表明了热带造林中大量固碳的潜力,并强调了在季节性热带气候下牧场生态系统碳损失的风险。

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