首页> 外文学位 >Elevated atmospheric carbon dioxide and precipitation alter ecosystem carbon fluxes over northern mixed-grass prairie at the prairie heating and carbon dioxide enrichment (PHACE) experiment in Cheyenne, Wyoming, United States .
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Elevated atmospheric carbon dioxide and precipitation alter ecosystem carbon fluxes over northern mixed-grass prairie at the prairie heating and carbon dioxide enrichment (PHACE) experiment in Cheyenne, Wyoming, United States .

机译:在美国怀俄明州夏安的草原加热和二氧化碳富集(PHACE)实验中,大气二氧化碳和降水的升高改变了北部混合草草原的生态系统碳通量。

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摘要

Understanding net carbon (C) balance under future global change scenarios requires a comprehensive understanding of photosynthetic (GPP) and ecosystem respiration (Re) responses to atmospheric CO2 concentration and soil moisture availability. We measured midday net ecosystem exchange of CO2 (NEE), GPP and Re prior to and following early and late growing season simulated precipitation 'pulse' events (May 31st and August 4th) and diurnally on five additional dates over the growing season under ambient and elevated atmospheric [CO2] in a northern mixed-grass prairie of Wyoming, USA. We also measured soil CO2 concentration on 10 days over the growing season and modeled soil respiration using a flux gradient approach. Elevated atmospheric [CO2] differentially stimulated GPP and Re both within and between pulse events and across the growing season. Elevated [CO2] increased the magnitude and duration of GPP and Re responses to moisture inputs, supporting the hypothesis that atmospheric [CO2] interacts with individual precipitation events to alter CO2 exchange patterns, and demonstrates that this interaction varies seasonally. Over both the pulses and growing season, the greatest effects on CO2 exchange patterns were due to soil moisture, and elevated [CO2] had the greatest effect on respiration fluxes, Re an Rs. Estimates of cumulative C uptake and loss both following individual precipitation events and over the growing season suggest that elevated [CO2] did not enhance C uptake in the 2006-growing season.
机译:要了解未来全球变化情景下的净碳(C)平衡,需要全面了解光合作用(GPP)和生态系统呼吸(Re)对大气CO2浓度和土壤水分有效性的响应。在生长季节的早期和晚期模拟降水“脉冲”事件之前和之后(5月31日和8月4日),以及在环境和气候条件下,在生长季节的另外五个日期,我们测量了中午之前和之后的二氧化碳(NEE),GPP和Re的中午净生态系统交换。美国怀俄明州北部混合草草原的大气[CO2]升高。我们还测量了生长期10天的土壤CO2浓度,并使用通量梯度法对土壤呼吸进行了建模。在脉冲事件之内和之间以及整个生长季节,升高的大气[CO2]差异刺激了GPP和Re。升高的[CO2]增加了GPP和Re对水分输入的响应的幅度和持续时间,支持了以下假设:大气[CO2]与各个降水事件相互作用以改变CO2交换模式,并证明这种相互作用随季节变化。在脉搏和生长季节中,对CO2交换模式的最大影响是由于土壤水分,而升高的[CO2]对呼吸通量Re a Rs的影响最大。在个别降水事件之后以及整个生长季节,对累积的C吸收和损失的估计表明,升高的[CO2]不会增加2006年生长季节的C吸收。

著录项

  • 作者

    Bachman, Sarah.;

  • 作者单位

    University of Wyoming.$bBotany.;

  • 授予单位 University of Wyoming.$bBotany.;
  • 学科 Biology Ecology.
  • 学位 M.S.
  • 年度 2007
  • 页码 103 p.
  • 总页数 103
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 生态学(生物生态学);
  • 关键词

  • 入库时间 2022-08-17 11:39:51

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