4.5 Article

Black carbon decomposition under varying water regimes

Journal

ORGANIC GEOCHEMISTRY
Volume 40, Issue 8, Pages 846-853

Publisher

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.orggeochem.2009.05.004

Keywords

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Funding

  1. Vietnam Education Foundation (VEF)
  2. Wu Fellowship (Cornell University)
  3. Department of Crop and Soil Sciences at Cornell University
  4. Rubber Research Institute of Vietnam (RRIV)

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The stability of biomass-derived black carbon (BC) or biochar as a slow cycling pool in the global C cycle is an important property and is likely governed by environmental conditions. This study investigated the effects of water regimes (saturated, unsaturated and alternating saturated-unsaturated conditions) and differences in BC materials, produced by carbonizing corn residues and oak wood at two temperatures (350 degrees C and 600 degrees C) on BC degradation at 30 degrees C over I year in a full factorial experiment. Effects of water regime on C loss and potential cation exchange capacity (CECp at pH 7) significantly depended on biomass type. Corn BC was both mineralized (16% C loss for the first year) and was oxidized [1000 mmole(+)kg(-1) C] significantly faster under unsaturated conditions than under other water regimes, whereas oak BC mineralized most rapidly (12%) under alternating Saturated-unsaturated conditions with similar oxidation, irrespective of water regime. Over I year of saturated incubation, the O/C ratio values did not significantly (P > 0.05) increase even though BC was mineralized by 9% and CECp increased by 170 mmole(+) kg(-1) C, in contrast to unsaturated and alternating saturated-unsaturated conditions. While mineralization and oxidation significantly decreased at higher charring temperature for corn, no difference was observed for oak (P > 0.05). Unsaturated and alternating conditions increased carboxylic and OH functional groups, while they decreased aliphatic groups. The pH increased by about one unit for corn BC, but decreased by 0.2 units for oak BC, indicating strong mineral dissolution of corn BC. Carbon loss strongly correlated with changes in O/C values of both corn BC and oak BC, indicating that oxidation of BC was most likely the major mechanism controlling its stability. However, under saturated conditions, additional mechanisms may govern BC degradation and require further investigation. (C) 2009 Elsevier Ltd. All rights reserved,

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