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季节和偶发性水分对植物和微生物土壤呼吸贡献的控制作用。

Seasonal and episodic moisture controls on plant and microbial contributions to soil respiration.

机构信息

Department of Geography, University of California, Santa Barbara, CA 93106-4060, USA.

出版信息

Oecologia. 2011 Sep;167(1):265-78. doi: 10.1007/s00442-011-1975-3. Epub 2011 Apr 13.

Abstract

Moisture inputs drive soil respiration (SR) dynamics in semi-arid and arid ecosystems. However, determining the contributions of root and microbial respiration to SR, and their separate temporal responses to periodic drought and water pulses, remains poorly understood. This study was conducted in a pine forest ecosystem with a Mediterranean-type climate that receives seasonally varying precipitation inputs from both rainfall (in the winter) and fog-drip (primarily in the summer). We used automated SR measurements, radiocarbon SR source partitioning, and a water addition experiment to understand how SR, and its separate root and microbial sources, respond to seasonal and episodic changes in moisture. Seasonal changes in SR were driven by surface soil water content and large changes in root respiration contributions. Superimposed on these seasonal patterns were episodic pulses of precipitation that determined the short-term SR patterns. Warm season precipitation pulses derived from fog-drip, and rainfall following extended dry periods, stimulated the largest SR responses. Microbial respiration dominated these SR responses, increasing within hours, whereas root respiration responded more slowly over days. We conclude that root and microbial respiration sources respond differently in timing and magnitude to both seasonal and episodic moisture inputs. These findings have important implications for the mechanistic representation of SR in models and the response of dry ecosystems to changes in precipitation patterns.

摘要

水分输入驱动半干旱和干旱生态系统土壤呼吸(SR)动态。然而,确定根系和微生物呼吸对 SR 的贡献,以及它们对周期性干旱和水分脉冲的单独时间响应,仍然知之甚少。本研究在具有地中海型气候的松林生态系统中进行,该系统季节性地接收来自降雨(冬季)和雾滴(主要在夏季)的降水输入。我们使用自动 SR 测量、放射性碳 SR 源分区和水分添加实验来了解 SR 及其单独的根和微生物源如何响应水分的季节性和偶发性变化。SR 的季节性变化受表层土壤含水量和根系呼吸贡献的较大变化驱动。在这些季节性模式之上,降水的偶发性脉冲决定了短期 SR 模式。来自雾滴的暖季降水脉冲和长时间干燥期后的降雨刺激了最大的 SR 响应。微生物呼吸主导了这些 SR 响应,在数小时内增加,而根系呼吸则在数天内缓慢响应。我们得出结论,根系和微生物呼吸源对季节性和偶发性水分输入的时间和幅度的响应不同。这些发现对模型中 SR 的机制表示以及干旱生态系统对降水模式变化的响应具有重要意义。

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