4.7 Article

Short term soil priming effects and the mineralisation of biochar following its incorporation to soils of different pH

Journal

SOIL BIOLOGY & BIOCHEMISTRY
Volume 43, Issue 11, Pages 2304-2314

Publisher

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.soilbio.2011.07.020

Keywords

Biochar; Biochar decomposition; CO2 evolution; Priming effect; Pyrolysis temperatures; Ryegrass; Soil microbial biomass; Soil organic carbon

Categories

Funding

  1. Biotechnology and Biological Sciences Research Council of the UK
  2. Chinese Scholarship Council
  3. BBSRC [BBS/E/C/00004959] Funding Source: UKRI

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The aim of this work was to determine the magnitude of the priming effect, i.e. short-term changes in the rate (negative or positive) of mineralisation of native soil organic carbon (C), following addition of biochars. The biochars were made from Miscanthus giganteus, a C4 plant, naturally enriched with C-13. The biochars were produced at 350 degrees C (biochar350) and 700 degrees C (biochar700) and applied with and without ryegrass as a substrate to a clay-loam soil at pH 3.7 and 7.6. A secondary aim was to determine the effect of ryegrass addition on the mineralisation of the two biochars. After 87 days, biochar350 addition caused priming effects equivalent to 250 and 319 mu g CO2-C g(-1) soil, in the low and high pH soil, respectively. The largest priming effects occurred at the start of the incubations. The size of the priming effect was decreased at higher biochar pyrolysis temperatures, which may be a way of controlling priming effects following biochar incorporation to soil, if desired. The priming effect was probably induced by the water soluble components of the biochar. At 87 days of incubation, 0.14% and 0.18% of biochar700 and 0.61% and 0.84% of biochar350 were mineralized in the low and high pH soil, respectively. Ryegrass addition gave an increased biochar350 mineralisation of 33% and 40%, and increased biochar700 at 137% and 70%, in the low and high pH soils, respectively. Certainly, on the basis of our results, if biochar is used to sequester carbon a priming effect may occur, increasing CO2-C evolved from soil and decreasing soil organic C. However, this will be more than compensated for by the increased soil C caused by biochar incorporation. A similar conclusion holds for accelerated mineralisation of biochar due to incorporation of fresh labile substrates. We consider that our results are the first to unequivocally demonstrate the initiation, progress and termination of a true positive priming effect by biochar on native soil organic C. (C) 2011 Elsevier Ltd. All rights reserved.

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