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首页> 外文期刊>Rangeland Ecology & Management >Carbon and Water Fluxes in an Exotic Buffelgrass Savanna
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Carbon and Water Fluxes in an Exotic Buffelgrass Savanna

机译:稀有野牛草中的碳和水通量

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Buffelgrass savanna is becoming widespread in aridland ecosystems around the world following invasion or deliberate land conversion for cattle forage. There is still a gap of information regarding functional and ecohydrological aspects such as carbon, water, and greenhouse gas exchanges in these highly productive novel ecosystems where buffelgrass is an exotic species. We measured net ecosystem CO2 exchange (NEE), ecosystem respiration (Rego), gross primary production (GPP), and evapotranspiration (ET) with eddy covariance techniques over a buffelgrass savanna established for cattle grazing, approximately 30 yr ago within the Sonoran Desert. The savanna was a net carbon sink (NEE 230 g C/m(2)/yr) during both a year with above average and one with below-average precipitation (NEE 84 g C/m(2)/yr). Water loss through evapotranspiration (ET) was similar to total annual rainfall input. Up to 62% of the annual fixed carbon and 75% of ET occurred during the summer monsoon season, when 72 86% of annual rainfall occurred and buffelgrass was active. ET from summer months explained 73% of variation in NEE, with an average ET of 50 mm H2O/month needed to turn the ecosystem into a net carbon sink during this season. Other seasons in the year, when buffelgrass was dormant, contributed with up to 48% of annual fixed carbon but with higher water use efficiency (-NEE/ET). We discuss the importance of the seasonal variability in R-eco, GPP, and ET processes and the phenology of native plant species for the net carbon uptake through the year for this managed novel ecosystem. (C) 2016 The Society for Range Management. Published by Elsevier Inc. All rights reserved
机译:在入侵或故意将土地改作牧草之后,Buffelgrass稀树草原在世界各地的干旱生态系统中变得越来越普遍。在这些水牛草是外来物种的高产新型生态系统中,关于功能和生态水文方面(如碳,水和温室气体交换)的信息仍然不足。我们在大约30年以前在Sonoran沙漠内为牛放牧的水牛草稀树草原上使用涡度协方差技术测量了生态系统的净二氧化碳交换(NEE),生态系统呼吸(Rego),初级生产总值(GPP)和蒸散(ET)。稀树草原是一年的净碳汇(NEE 230 g C / m(2)/ yr),均高于平均水平,而降水量低于平均水平(NEE 84 g C / m(2)/ yr)。蒸发蒸腾(ET)引起的水分流失与每年的降雨总量相似。在夏季风季,每年多达62%的固定碳和75%的ET发生,而当年有72 86%的降雨发生并且水牛草活跃。夏季的ET解释了NEE变化的73%,该季节将生态系统转化为净碳汇所需的平均ET为50 mm H2O /月。水牛草处于休眠状态的其他季节,贡献了每年固定碳的48%,但用水效率更高(-NEE / ET)。我们讨论了在这种管理型新生态系统中,R-eco,GPP和ET过程中季节性变化的重要性以及本地植物物种物候对于全年净碳吸收的重要性。 (C)2016年范围管理学会。由Elsevier Inc.出版。保留所有权利。

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