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Reductions in soil surface albedo as a function of biochar application rate

Implications for global radiative forcing

Bibliographic Data

ID15544334
AuthorsFrank Verheijen (0000-0001-6741-4249, University of Aveiro, corresponding author), Frank G A Verheijen, Simon Jeffery (0000-0003-1014-9100, Wageningen University & Research), Marijn van der Velde (0000-0002-9103-7081, International Institute for Applied Systems Analysis), Vít Penížek (0000-0001-6131-7608, Czech University of Life Sciences Prague), Martin Béland (0000-0002-2504-9578, University of California, Berkeley), Ana Catarina Bastos (0000-0003-1185-2172, University of Aveiro), Jan Jacob Keizer (0000-0003-4833-0415, University of Aveiro)
Year2013
Volume8
Issue4
Pages044008-044008
Publication date2013-10-16
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueEnvironmental Research Letters (JOURNAL)
Journal identifiersISSN: 1748-9326 • E-ISSN: 1748-9326
PublisherIOP Publishing (PUBLISHER • GB)
DOI10.1088/1748-9326/8/4/044008
OpenAlexW1999739813
LanguageEN
Citations received3
References cited24

Biochar can be defined as pyrolysed (charred) biomass produced for application to soils with the aim of mitigating global climate change while improving soil functions. Sustainable biochar application to soils has been estimated to reduce global greenhouse gas emissions by 71-130 Pg CO2-Ce over 100 years, indicating an important potential to mitigate climate change. However, these estimates ignored changes in soil surface reflection by the application of dark-coloured biochar. Through a laboratory experiment we show a strong tendency for soil surface albedo to decrease as a power decay function with increasing biochar application rate, depending on soil moisture content, biochar application method and land use. Surface application of biochar resulted in strong reductions in soil surface albedo even at relatively low application rates. As a first assessment of the implications for climate change mitigation of these biochar-albedo relationships, we applied a first order global energy balance model to compare negative radiative forcings (from avoided CO2 emissions) with positive radiative forcings (from reduced soil surface albedos). For a global-scale biochar application equivalent to 120 t/ha, we obtained reductions in negative radiative forcings of 5 and 11% for croplands and 11 and 23% for grasslands, when incorporating biochar into the topsoil or applying it to the soil surface, respectively. For a lower global biochar application rate (equivalent to 10 t/ha), these reductions amounted to 13 and 44% for croplands and 28 and 94% for grasslands. Thus, our findings revealed the importance of including changes in soil surface albedo in studies assessing the net climate change mitigation potential of biochar, and we discuss the urgent need for field studies and more detailed spatiotemporal modelling

Albedo (alchemy · Atmospheric sciences · Biochar · Climate change · Greenhouse gas · Pyrolysis · Radiative forcing · Soil water · Topsoil · Atmospheric and Environmental Gas Dynamics · Atmospheric chemistry and aerosols · Chemistry · Climate Change and Geoengineering · Environmental Science · Ecology · Geology · Soil Science

  • Biogeochemical potential of biomass pyrolysis systems for limiting global warming to 1.5 °C

    Open Access•Constanze Werner, Hanns-Peter Schmidt et al.•Environmental Research Letters•2018

  • Mapping of soil organic carbon stocks for spatially explicit assessments of climate change mitigation potential

    Open Access•Tor‐gunnar Vågen, Tor-Gunnar Vagen et al.•Environmental Research Letters•2013

  • Mimicking biochar-albedo feedback in complex Mediterranean agricultural landscapes

    Open Access•E Bozzi, Lorenzo Genesio et al.•Environmental Research Letters•2015

  • Surface albedo following biochar application in durum wheat

    Open Access•Lorenzo Genesio, F Miglietta et al.•Environmental Research Letters•2012

Unique citing works3
Citations per year0,23
Citation span2013 - 2018 (6)
Citation velocityhistorical
Highly citedNo
Citation typesNeutral: 3

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