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首页> 外文期刊>Oecologia >Effects of an increase in summer precipitation on leaf, soil, and ecosystem fluxes of CO2 and H2O in a sotol grassland in Big Bend National Park, Texas
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Effects of an increase in summer precipitation on leaf, soil, and ecosystem fluxes of CO2 and H2O in a sotol grassland in Big Bend National Park, Texas

机译:夏季降水增加对得克萨斯州大弯国家公园Sotol草地的叶片,土壤和生态系统通量的CO2和H2O的影响

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Global climate models predict that in the next century precipitation in desert regions of the USA will increase, which is anticipated to affect biosphere/ atmosphere exchanges of both CO2 and H2O. In a sotol grassland ecosystem in the Chihuahuan Desert at Big Bend National Park, we measured the response of leaf-level fluxes of CO2 and H2O 1 day before and up to 7 days after three supplemental precipitation pulses in the summer (June, July, and August 2004). In addition, the responses of leaf, soil, and ecosystem fluxes of CO2 and H2O to these precipitation pulses were also evaluated in September, 1 month after the final seasonal supplemental watering event. We found that plant carbon fixation responded positively to supplemental precipitation throughout the summer. Both shrubs and grasses in watered plots had increased rates of photosynthesis following pulses in June and July. In September, only grasses in watered plots had higher rates of photosynthesis than plants in the control plots. Soil respiration decreased in supplementally watered plots at the end of the summer. Due to these increased rates of photosynthesis in grasses and decreased rates of daytime soil respiration, watered ecosystems were a sink for carbon in September, assimilating on average 31 mmol CO2 m(-2) s(-1) ground area day(-1). As a result of a 25% increase in summer precipitation, watered plots fixed eightfold more CO2 during a 24-h period than control plots. In June and July, there were greater rates of transpiration for both grasses and shrubs in the watered plots. In September, similar rates of transpiration and soil water evaporation led to no observed treatment differences in ecosystem evapotranspiration, even though grasses transpired significantly more than shrubs. In summary, greater amounts of summer precipitation may lead to short-term increased carbon uptake by this sotol grassland ecosystem.
机译:全球气候模型预测,到下个世纪,美国沙漠地区的降水将增加,预计将影响到CO2和H2O的生物圈/大气交换。在大弯国家公园奇瓦瓦沙漠的独生草草地生态系统中,我们测量了夏季三个补充降水脉冲前1天和之后7天(6月,7月和5月)的CO2和H2O叶片水平通量的响应。 2004年8月)。此外,还在最后的季节性补充浇水事件后的1个月的9月(9月)评估了叶片,土壤和生态系统通量的CO2和H2O对这些降水脉冲的响应。我们发现,整个夏季,植物固碳对补充降水的反应都是积极的。在六月和七月的脉冲之后,浇水区的灌木和草丛的光合作用速率均增加。在9月,只有浇水区的草具有比对照区植物高的光合作用速率。夏季结束时,补充灌溉的地块土壤呼吸减少。由于这些草丛中光合作用的增加和白天土壤呼吸的减少,因此,9月浇水的生态系统是碳汇,平均每天吸收31 mmol CO2 m(-2)s(-1)。 。由于夏季降水增加了25%,浇水区在24小时内固定的二氧化碳比对照区多了八倍。 6月和7月,浇水区的草和灌木的蒸腾速率更高。 9月,蒸腾速率和土壤水分蒸发速率相似,尽管草的蒸发量比灌木的蒸发量多,但在生态系统的蒸散量方面没有观察到处理差异。总而言之,夏季大量降水可能会导致该单一草地生态系统的短期碳吸收增加。

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