Degradation kinetics of biochar from pyrolysis and hydrothermal carbonization in temperate soils

Background and Aims Estimates of biochar residence times in soils range over three orders of magnitude. We present the first direct comparison between the biodegradation of a char from hydrothermal carbonization (htcBC) and pyrolysis (pyrBC) with high temporal resolution. Methods Mineralization of t...

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Published inPlant and soil Vol. 372; no. 1/2; pp. 375 - 387
Main Authors Bai, Mo, Wilske, Burkhard, Buegger, Franz, Esperschütz, Jürgen, Kammann, Claudia Irene, Eckhardt, Christian, Koestler, Martin, Kraft, Philipp, Bach, Martin, Frede, Hans-Georg, Breuer, Lutz
Format Journal Article
LanguageEnglish
Published Dordrecht Springer 01.11.2013
Springer Netherlands
Springer Nature B.V
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Summary:Background and Aims Estimates of biochar residence times in soils range over three orders of magnitude. We present the first direct comparison between the biodegradation of a char from hydrothermal carbonization (htcBC) and pyrolysis (pyrBC) with high temporal resolution. Methods Mineralization of the biochars and their shared Miscanthus feedstock in three soils was determined directly by the ¹³CO₂ efflux using a novel method incorporating wavelength scanned cavity ring-down spectroscopy. Biochar half-life (t ½ ) was estimated with three empirical models. Results (1) The htcBC was readily biodegradable, whereas pyrBC was more recalcitrant. (2) Cumulative degradation of both biochars increased with soil organic carbon and nitrogen content. (3) The corrected Akaike information criterion (AIC C ) showed an overall preference for the double exponential model (DEM) reflecting a labile and a recalcitrant C-pool, over the first-order degradation model (FODM) and a logarithmic model. (4) The DEM resulted in t ½ ranging from 19.7-44.5, 0.7-2.1 and 0.8-1.3 years for pyrBC, pyrBC and feedstock, respectively. Conclusion The degradation was rather similar between feedstock and htcBC but one order of magnitude slower for pyrBC. The AIC C preferred FODM in two cases, where the DEM parameters indicated no distinction between a labile and recalcitrant carbon pool.
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ISSN:0032-079X
1573-5036
DOI:10.1007/s11104-013-1745-6