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Feedback responses of soil greenhouse gas emissions to climate change are modulated by soil characteristics in dryland ecosystems

机译:旱地生态系统中土壤特性调节土壤温室气体排放对气候变化的反馈响应

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Understanding feedback responses of greenhouse gas (GHG) emissions to future climate projections is critical for the effective development of mitigation and adaptation strategies. It is proposed that effects of elevated carbon dioxide (CO2) and temperature can have differential effects on GHG fluxes but the magnitude and direction of such impact is not fully known, especially in dryland ecosystems, which are typically water and nutrient limited. We examined individual and interactive impacts of elevated CO2 (400 ppm vs. 600 ppm) and elevated temperature (ambient vs. +3 degrees C increase) treatments on GHG fluxes, in three Australian dryland soils. Firstly, we quantified the individual and interactive effects of elevated CO2 and temperature on CO2, methane (CH4) and nitrous oxide (N2O) fluxes and the corresponding soil net global warming potential (GWP). Secondly, biotic and abiotic drivers of GHG emissions were identified by exploring the relationship between CO2, CH4 and N2O fluxes with the abundance of bacteria, methanotrophs and N2O-reducing bacteria as well as soil abiotic characteristics. Our results show that soil CO2 emissions and CH4 uptake respond mainly to elevated temperature in all dryland soils tested, with interactive treatment effects showing a less than additive trend on soil net GWP. Nitrous oxide emissions responded less to climate change treatments, and these were site-specific. Soil site characteristics were the main determinant of all GHG emissions; however, the abundance of total bacteria and N2O-reducing bacteria significantly explained CO2 and N2O fluxes, respectively. This study shows that dryland soils respond to climate change with an offset under interactive climate treatments. Our findings suggest that future studies on GHG feedback responses should explicitly consider both biotic and abiotic soil characteristics in order to provide a better mechanistic understanding for the development of future mitigation strategies. (C) 2016 Elsevier Ltd. All rights reserved.
机译:了解温室气体(GHG)排放对未来气候预测的反馈响应对于有效制定缓解和适应策略至关重要。有人提出,升高的二氧化碳(CO2)和温度的影响可能会对温室气体通量产生不同的影响,但这种影响的程度和方向尚不完全清楚,尤其是在干旱和干旱的生态系统中,这通常受到水和养分的限制。我们研究了三种澳大利亚旱地土壤中CO2浓度升高(400 ppm vs. 600 ppm)和温度升高(环境温度升高+3摄氏度)对温室气体通量的个体和互动影响。首先,我们量化了升高的CO2和温度对CO2,甲烷(CH4)和一氧化二氮(N2O)通量以及相应的土壤净全球变暖潜势(GWP)的个体和交互作用。其次,通过探索CO2,CH4和N2O通量与细菌,甲烷营养菌和减少N2O的细菌的丰度以及土壤非生物特性之间的关系,确定了温室气体排放的生物和非生物驱动因素。我们的结果表明,在所有测试的旱地土壤中,CO2排放量和CH4的吸收量主要对温度升高做出响应,交互处理效果显示出对土壤净GWP的累加趋势较小。一氧化二氮排放对气候变化处理的响应较小,而且这些针对特定地点。土壤场地特征是所有温室气体排放的主要决定因素;然而,总细菌和减少N2O的细菌的丰度分别显着解释了CO2和N2O的通量。这项研究表明,在交互气候处理下,旱地土壤对气候变化的响应有所抵消。我们的发现表明,有关温室气体反馈响应的未来研究应明确考虑生物和非生物土壤的特征,以便为未来缓解策略的发展提供更好的机械理解。 (C)2016 Elsevier Ltd.保留所有权利。

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