4.8 Article

Interactive Priming of Biochar and Labile Organic Matter Mineralization in a Smectite-Rich Soil

Journal

ENVIRONMENTAL SCIENCE & TECHNOLOGY
Volume 45, Issue 22, Pages 9611-9618

Publisher

AMER CHEMICAL SOC
DOI: 10.1021/es202186j

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Biochar is considered as an attractive tool for long-term carbon (C) storage in soil. However, there is limited knowledge about the effect of labile organic matter (LOM) on biochar-C mineralization in soil or the vice versa. An incubation experiment (20 degrees C) was conducted for 120 days to quantify the interactive priming effects of biochar-C and LOM-C mineralization in a smectitic clayey soil. Sugar cane residue (source of LOM) at a rate of 0, 1, 2, and 4% (w/w) in combination with two wood biochars (450 and 550 degrees C) at a rate of 2% (w/w) were applied to the soil. The use of biochars (similar to-36 parts per thousand) and LOM (-12.7 parts per thousand) or soil (-14.3 parts per thousand) with isotopically distinct delta C-13 values allowed the quantification of C mineralized from biochar and LOM/soil. A small fraction (0.4-1.1%) of the applied biochar-C was mineralized, and the mineralization of biochar-C increased significantly with increasing application rates of LOM, especially during the early stages of incubation. Concurrently, biochar application reduced the mineralization of LOM-C, and the magnitude of this effect increased with increasing rate of LOM addition. Over time, the interactive priming of biochar-C and LOM-C mineralization was stabilized. Biochar application possesses a considerable merit for long-term soil C-sequestration, and it has a stabilizing effect on LOM in soil.

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