Offsetting global warming-induced elevated greenhouse gas emissions from an arable soil by biochar application

© 2017 John Wiley & Sons Ltd.

Bibliographische Detailangaben
Veröffentlicht in:Global change biology. - 1999. - 24(2018), 1 vom: 17. Jan., Seite e318-e334
1. Verfasser: Bamminger, Chris (VerfasserIn)
Weitere Verfasser: Poll, Christian, Marhan, Sven
Format: Online-Aufsatz
Sprache:English
Veröffentlicht: 2018
Zugriff auf das übergeordnete Werk:Global change biology
Schlagworte:Journal Article Research Support, Non-U.S. Gov't agroecosystem biochar carbon dioxide carbon sequestration methane nitrous oxide soil warming temperature sensitivity mehr... Greenhouse Gases Soil Carbon Dioxide 142M471B3J Charcoal 16291-96-6 Carbon 7440-44-0 Nitrous Oxide K50XQU1029 Methane OP0UW79H66
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520 |a Global warming will likely enhance greenhouse gas (GHG) emissions from soils. Due to its slow decomposability, biochar is widely recognized as effective in long-term soil carbon (C) sequestration and in mitigation of soil GHG emissions. In a long-term soil warming experiment (+2.5 °C, since July 2008) we studied the effect of applying high-temperature Miscanthus biochar (0, 30 t/ha, since August 2013) on GHG emissions and their global warming potential (GWP) during 2 years in a temperate agroecosystem. Crop growth, physical and chemical soil properties, temperature sensitivity of soil respiration (Rs ), and metabolic quotient (qCO2 ) were investigated to yield further information about single effects of soil warming and biochar as well as on their interactions. Soil warming increased total CO2 emissions by 28% over 2 years. The effect of warming on soil respiration did not level off as has often been observed in less intensively managed ecosystems. However, the temperature sensitivity of soil respiration was not affected by warming. Overall, biochar had no effect on most of the measured parameters, suggesting its high degradation stability and its low influence on microbial C cycling even under elevated soil temperatures. In contrast, biochar × warming interactions led to higher total N2 O emissions, possibly due to accelerated N-cycling at elevated soil temperature and to biochar-induced changes in soil properties and environmental conditions. Methane uptake was not affected by soil warming or biochar. The incorporation of biochar-C into soil was estimated to offset warming-induced elevated GHG emissions for 25 years. Our results highlight the suitability of biochar for C sequestration in cultivated temperate agricultural soil under a future elevated temperature. However, the increased N2 O emissions under warming limit the GHG mitigation potential of biochar 
650 4 |a Journal Article 
650 4 |a Research Support, Non-U.S. Gov't 
650 4 |a agroecosystem 
650 4 |a biochar 
650 4 |a carbon dioxide 
650 4 |a carbon sequestration 
650 4 |a methane 
650 4 |a nitrous oxide 
650 4 |a soil warming 
650 4 |a temperature sensitivity 
650 7 |a Greenhouse Gases  |2 NLM 
650 7 |a Soil  |2 NLM 
650 7 |a biochar  |2 NLM 
650 7 |a Carbon Dioxide  |2 NLM 
650 7 |a 142M471B3J  |2 NLM 
650 7 |a Charcoal  |2 NLM 
650 7 |a 16291-96-6  |2 NLM 
650 7 |a Carbon  |2 NLM 
650 7 |a 7440-44-0  |2 NLM 
650 7 |a Nitrous Oxide  |2 NLM 
650 7 |a K50XQU1029  |2 NLM 
650 7 |a Methane  |2 NLM 
650 7 |a OP0UW79H66  |2 NLM 
700 1 |a Poll, Christian  |e verfasserin  |4 aut 
700 1 |a Marhan, Sven  |e verfasserin  |4 aut 
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