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首页> 外文期刊>Agricultural and Forest Meteorology >Component-specific dynamics of riverine mangrove CO2 efflux in the Florida coastal Everglades
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Component-specific dynamics of riverine mangrove CO2 efflux in the Florida coastal Everglades

机译:佛罗里达沿海大沼泽地河流红树林CO2外排的特定组分动力学

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Carbon cycling in mangrove forests represents a significant portion of the coastal wetland carbon (C) budget across the latitudes of the tropics and subtropics. Previous research suggests fluctuations in tidal inundation, temperature and salinity can influence forest metabolism and C cycling. Carbon dioxide (CO2) from respiration that occurs from below the canopy is contributed from different components. In this study, we investigated variation in CO2 flux among different below-canopy components (soil, leaf litter, course woody debris, soil including pneumatophores, prop roots, and surface water) in a riverine mangrove forest of Shark River Slough estuary, Everglades National Park (Florida, USA). The range in CO2 flux from different components exceeded that measured among sites along the oligohaline-saline gradient. Black mangrove (Avicennia germinans) pneumatophores contributed the largest average CO2 flux. Over a narrow range of estuarine salinity (25-35 practical salinity units (PSU)), increased salinity resulted in lower CO2 flux to the atmosphere. Tidal inundation reduced soil CO2 flux overall but increased the partial pressure of CO2 (pCO(2)) observed in the overlying surface water upon flooding. Higher pCO(2) in surface water is then subject to tidally driven export, largely as HCO3. Integration and scaling of CO2 flux rates to forest scale allowed for improved understanding of the relative contribution of different below-canopy components to mangrove forest ecosystem respiration (ER). Summing component CO2 fluxes suggests a more significant contribution of below-canopy respiration to ER than previously considered. An understanding of below-canopy CO2 component fluxes and their contributions to ER can help to elucidate how C cycling will change with discrete disturbance events (e.g., hurricanes) and long-term change, including sea-level rise, and potential impact mangrove forests. As such, key controls on below-canopy ER must be taken into consideration when developing and modeling mangrove forest C budgets. (C) 2015 Elsevier B.V. All rights reserved.
机译:红树林中的碳循环占整个热带和亚热带纬度沿海湿地碳(C)预算的很大一部分。先前的研究表明,潮汐淹没,温度和盐度的波动会影响森林的新陈代谢和碳循环。冠层下方的呼吸产生的二氧化碳(CO2)来自不同的成分。在这项研究中,我们调查了大沼泽地国家级鲨鱼河泥沼河口红树林森林中不同冠层以下成分(土壤,树叶凋落物,过程木屑,土壤(包括气管,支柱和地面水))之间的CO2通量变化。公园(美国佛罗里达州)。来自不同成分的CO2通量范围超出了沿盐卤盐碱梯度站点测得的范围。黑美洲红树(Avicennia Germinans)的肺部隐喻贡献了最大的平均CO2通量。在狭窄的河口盐度范围内(25-35个实际盐度单位(PSU)),盐度的增加导致二氧化碳向大气的通量降低。潮汐淹没总体上降低了土壤CO2通量,但增加了洪水后上层地表水中观测到的CO2分压(pCO(2))。然后,地表水中较高的pCO(2)受潮汐驱动,主要是HCO3。 CO2通量率与森林规模的积分和换算可以更好地了解不同冠层以下成分对红树林森林生态系统呼吸作用的相对贡献。汇总CO2通量表明,冠层下呼吸对ER的贡献比以前考虑的要大。对冠层下CO2组分通量及其对ER的贡献的理解有助于阐明C循环如何随着离散的扰动事件(例如飓风)和长期变化(包括海平面上升以及对红树林的潜在影响)而变化。因此,在制定和建模红树林C预算时,必须考虑对冠层下ER的关键控制。 (C)2015 Elsevier B.V.保留所有权利。

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