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Partitioning of Microbially Respired CO2 Between Indigenous and Exogenous Carbon Sources During Biochar Degradation Using Radiocarbon and Stable Carbon Isotopes

Published online by Cambridge University Press:  05 November 2018

Niels C Munksgaard*
Affiliation:
College of Science and Engineering and Centre for Tropical Environmental and Sustainability Science, James Cook University, Smithfield, QLD4878, Australia Research Institute for the Environment and Livelihoods, Charles Darwin University, Casuarina, NT0810, Australia
Anna V McBeath
Affiliation:
College of Science and Engineering and Centre for Tropical Environmental and Sustainability Science, James Cook University, Smithfield, QLD4878, Australia Department of Agriculture and Fisheries, Queensland Government, South Johnstone, QLD4859, Australia
Philippa L Ascough
Affiliation:
NERC Radiocarbon Facility, Scottish Universities Environmental Research Centre (SUERC), Scottish Enterprise Technology Park, Rankine Avenue, East KilbrideG75 0QF, UK
Vladimir A Levchenko
Affiliation:
Australian Nuclear Science and Technology Organisation (ANSTO), KirraweeDC, NSW2232, Australia
Alan Williams
Affiliation:
Australian Nuclear Science and Technology Organisation (ANSTO), KirraweeDC, NSW2232, Australia
Michael I Bird
Affiliation:
College of Science and Engineering and Centre for Tropical Environmental and Sustainability Science, James Cook University, Smithfield, QLD4878, Australia ARC Centre for Excellence for Australian Biodiversity and Heritage, James Cook University, Smithfield, QLD4878, Australia
*
*Corresponding author. Email: niels.munksgaard@jcu.edu.au.

Abstract

Pyrolized carbon in biochar can sequester atmospheric CO2 into soil to reduce impacts of anthropogenic CO2 emissions. When estimating the stability of biochar, degradation of biochar carbon, mobility of degradation products, and ingress of carbon from other sources must all be considered. In a previous study we tracked degradation in biochars produced from radiocarbon-free wood and subjected to different physico-chemical treatments over three years in a rainforest soil. Following completion of the field trial, we report here a series of in-vitro incubations of the degraded biochars to determine CO2 efflux rates, 14C concentration and δ13C values in CO2 to quantify the contributions of biochar carbon and other sources of carbon to the CO2 efflux. The 14C concentration in CO2 showed that microbial degradation led to respiration of CO2 sourced from indigenous biochar carbon (≈0.5–1.4 μmoles CO2/g biochar C/day) along with a component of carbon closely associated with the biochars but derived from the local environment. Correlations between 14C concentration, δ13C values and Ca abundance indicated that Ca2+ availability was an important determinant of the loss of biochar carbon.

Type
Research Article
Copyright
© 2018 by the Arizona Board of Regents on behalf of the University of Arizona 

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