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前期土壤湿度和季节性降水影响半干旱草原冠层尺度碳和水分交换对降雨脉冲的响应。

Antecedent moisture and seasonal precipitation influence the response of canopy-scale carbon and water exchange to rainfall pulses in a semi-arid grassland.

作者信息

Potts D L, Huxman T E, Cable J M, English N B, Ignace D D, Eilts J A, Mason M J, Weltzin J F, Williams D G

机构信息

University of Arizona, Department of Ecology and Evolutionary Biology, Tucson, AZ, USA.

出版信息

New Phytol. 2006;170(4):849-60. doi: 10.1111/j.1469-8137.2006.01732.x.

Abstract

The influences of prior monsoon-season drought (PMSD) and the seasonal timing of episodic rainfall ('pulses') on carbon and water exchange in water-limited ecosystems are poorly quantified. *In the present study, we estimated net ecosystem exchange of CO(2) (NEE) and evapotranspiration (ET) before, and for 15 d following, experimental irrigation in a semi-arid grassland during June and August 2003. Rainout shelters near Tucson, Arizona, USA, were positioned on contrasting soils (clay and sand) and planted with native (Heteropogon contortus) or non-native invasive (Eragrostis lehmanniana) C4 bunchgrasses. Plots received increased ('wet') or decreased ('dry') monsoon-season (July-September) rainfall during 2002 and 2003. Following a June 2003 39-mm pulse, species treatments had similar NEE and ET dynamics including 15-d integrated NEE (NEE(pulse)). Contrary to predictions, PMSD increased net C uptake during June in plots of both species. Greater flux rates after an August 2003 39-mm pulse reflected biotic activity associated with the North American Monsoon. Furthermore, August NEE(pulse) and ecosystem pulse-use efficiency (PUE(e) = NEE(pulse)/ET(pulse)) was greatest in Heteropogon plots. PMSD and rainfall seasonal timing may interact with bunchgrass invasions to alter NEE and ET dynamics with consequences for PUE(e) in water-limited ecosystems.

摘要

季风季节前干旱(PMSD)和间歇性降雨(“脉冲”)的季节时间对水分受限生态系统中碳和水分交换的影响,目前量化程度很低。在本研究中,我们估算了2003年6月和8月美国亚利桑那州图森市附近雨棚下种植于对比土壤(黏土和沙土)上的本地(扭黄茅)或非本地入侵(画眉草)C4丛生禾本科植物在实验灌溉前及灌溉后15天的生态系统净CO₂交换量(NEE)和蒸散量(ET)。这些地块在2002年和2003年接受了增加(“湿润”)或减少(“干旱”)的季风季节(7 - 9月)降雨。在2003年6月一场39毫米的降雨脉冲后,物种处理组具有相似的NEE和ET动态,包括15天累计NEE(NEE(pulse))。与预测相反,PMSD增加了两个物种地块6月的净碳吸收量。2003年8月一场39毫米降雨脉冲后的通量率更高反映了与北美季风相关的生物活性。此外,8月的NEE(pulse)和生态系统脉冲利用效率(PUE(e) = NEE(pulse)/ET(pulse))在扭黄茅地块中最高。PMSD和降雨季节时间可能与丛生禾本科植物入侵相互作用,改变NEE和ET动态,从而影响水分受限生态系统中的PUE(e)。

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