Department of Microbiology and Plant Biology, University of Oklahoma, Norman, Ok 73019, USA.
Glob Chang Biol. 2013 Nov;19(11):3553-64. doi: 10.1111/gcb.12273. Epub 2013 Jul 24.
Understanding how soil respiration (Rs) and its source components respond to climate warming is crucial to improve model prediction of climate-carbon (C) feedback. We conducted a manipulation experiment by warming and clipping in a prairie dominated by invasive winter annual Bromus japonicas in Southern Great Plains, USA. Infrared radiators were used to simulate climate warming by 3 °C and clipping was used to mimic yearly hay mowing. Heterotrophic respiration (Rh) was measured inside deep collars (70 cm deep) that excluded root growth, while total soil respiration (Rs) was measured inside surface collars (2-3 cm deep). Autotrophic respiration (Ra) was calculated by subtracting Rh from Rs. During 3 years of experiment from January 2010 to December 2012, warming had no significant effect on Rs. The neutral response of Rs to warming was due to compensatory effects of warming on Rh and Ra. Warming significantly (P < 0.05) stimulated Rh but decreased Ra. Clipping only marginally (P < 0.1) increased Ra in 2010 but had no effect on Rh. There were no significant interactive effects of warming and clipping on Rs or its components. Warming stimulated annual Rh by 22.0%, but decreased annual Ra by 29.0% across the 3 years. The decreased Ra was primarily associated with the warming-induced decline of the winter annual productivity. Across the 3 years, warming increased Rh/Rs by 29.1% but clipping did not affect Rh/Rs. Our study highlights that climate warming may have contrasting effects on Rh and Ra in association with responses of plant productivity to warming.
了解土壤呼吸(Rs)及其源组分如何响应气候变暖对于提高气候-碳(C)反馈模型的预测至关重要。我们在美国大平原南部的入侵性冬季一年生雀麦草原上进行了一项由增温和刈割组成的控制实验。我们使用红外线辐射器模拟气候变暖 3°C,并用刈割模拟每年的干草收割。非生物呼吸(Rh)是在排除根系生长的深环(70 厘米深)内测量的,而总土壤呼吸(Rs)是在表面环(2-3 厘米深)内测量的。通过从 Rs 中减去 Rh 来计算自养呼吸(Ra)。在 2010 年 1 月至 2012 年 12 月的 3 年实验期间,增温对 Rs 没有显著影响。Rs 对增温的中性响应是由于增温对 Rh 和 Ra 的补偿效应。增温显著(P < 0.05)刺激了 Rh,但降低了 Ra。刈割仅在 2010 年略微(P < 0.1)增加了 Ra,但对 Rh 没有影响。增温和刈割对 Rs 或其组成部分没有显著的交互作用。增温在 3 年内刺激了每年的 Rh 增加了 22.0%,但每年的 Ra 减少了 29.0%。Ra 的减少主要与冬季一年生生产力的增温诱导下降有关。在 3 年内,增温使 Rh/Rs 增加了 29.1%,但刈割没有影响 Rh/Rs。我们的研究强调,气候变暖可能会对 Rh 和 Ra 产生相反的影响,这与植物生产力对变暖的响应有关。