Abstract

The achievement of carbon neutrality till 2050 will require the deployment of negative carbon emission technologies like the production and soil incorporation of biochar, produced from pyrolyzed plant-based residues. The carbon sequestration potential of biochar (BC) from hazelnut (Corylus avellana L.) shells (HNS) and sunflower (Helianthus annuus L.) husks (SFH) was evaluated when the biomass was carbonized in a fixed bed reactor, in a rotary kiln and in a screw reactor. In all tested reactors, higher temperatures (>500 °C) and longer retention times increased the C concentration and stability of the biochar, with negligible effects of the reactor type and feedstock. A national case study was developed for Austria concerning the potential use of SFH- and HNS-BC in combination with compost for reaching the “4 per mille” objective. An annual soil organic carbon increase of 2.5 Mt C would be needed, requiring amendment rates of 2.2 Mt C a−1 for all annual crop areas and 0.3 Mt C a−1 for all vineyards and orchards. If compost only were used, the annual cost would be about 200 EUR ha−1 but short-term re-mineralization would have to be considered. If the more recalcitrant biochar were used only, about 2.3 t BC ha−1 would be needed at a cost of 1400–1870 EUR ha−1. The study shows in principle the feasibility of applying compost–biochar mixtures for achieving the “4 per mille” objective but in practice, supplemental soil management strategies for sequestering C will be required.

Highlights

  • Many different approaches to abate climate change and its consequences are under investigation.The deployment of negative emission technologies (NETs) is considered indispensable to reach the 2 ◦ C goal [1]

  • This study focused on two residues that are either burnt or left to rot: sunflower husks and hazelnut shells

  • Rising pyrolysis temperatures decreased the yield of biochar and increased its C content in different types of reactors

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Summary

Introduction

The deployment of negative emission technologies (NETs) is considered indispensable to reach the 2 ◦ C goal [1]. Sequestering C in soil in order to drastically delay and mitigate its release to the atmosphere reduces carbon dioxide emissions and can lead to increased soil organic carbon (SOC) and contribute to enhanced soil fertility and crop production [2]. 21st Conference of the Parties (COP21) suggests an annual increase in SOC stocks of 0.4% of the current stocks in the top 30–40 cm soil of all land covers around the world. Minasny et al [3] emphasized that soils with low initial SOC under 30 t C/ha in the topsoil could even sequester annual rates of up to 1%

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