Cited by 664Soil Carbon and Nitrogen DynamicsFire effects on ecosystemsThermochemical Biomass Conversion Processes

Biochar stability in soil: decomposition during eight years and transformation as assessed by compound-specific 14C analysis

Kuzyakov, Yakov, Bogomolova, Irina, Glaser, Bruno·2014·Soil Biology and Biochemistry

Abstract

Stability and transformation products of incomplete combustion of vegetation or fossil fuel, frequently called pyrogenic or black carbon and of biochar in soil, remains unknown mainly because of their high recalcitrance compared to other natural substances. Therefore, direct estimations of biochar decomposition and transformations are difficult because 1) changes are too small for any relevant experimental period and 2) due to methodological constraints (ambiguity of the origin of investigated compounds). We used 14C-labeled biochar to trace its decomposition to CO2 during 8.5 years and transformation of its chemical compounds: neutral lipids, glycolipids, phospholipids, polysaccharides and benzenepolycarboxylic acids (BPCA).14C-labeled biochar was produced by charring 14C-labeled Lolium residues. We incubated the 14C-labeled biochar in a Haplic Luvisol and in loess for 8.5 years under controlled conditions. In total only about 6% of initially added biochar were mineralized to CO2 during the 8.5 years. This is probably the slowest decomposition obtained experimentally for any natural organic compound. The biochar decomposition rates estimated by 14CO2 efflux between the 5th and 8th years were of 7 × 10−4 % per day. This corresponds to less than 0.3% per year under optimal conditions and is about 2.5 times slower as reported from the previous shorter study (3.5 years).After 3.5 years of incubation, we analyzed 14C in dissolved organic matter, microbial biomass, and sequentially extracted neutral lipids, glycolipids, phospholipids, polysaccharides and BPCA. Biochar-derived C (14C) in microbial biomass ranged between 0.3 and 0.95% of the 14C input. Biochar-derived C in all lipid fractions was less than 1%. Over 3.5 years, glycolipids and phospholipids were decomposed 1.6 times faster (23% of their initial content per year) compared to neutral lipids (15% year−1). Polysaccharides contributed ca. 17% of the 14C activity in biochar. The highest portion of 14C in the initial biochar (87%) was in BPCA decreasing only 7% over 3.5 years. Condensed aromatic moieties were the most stable fraction compared to all other biochar compounds and the high portion of BPCA in biochar explains its very high stability and its contribution to long-term C sequestration in soil.Our new approach for analysis of biochar stability combines 14C-labeled biochar with 14C determination in chemical fractions allowed tracing of transformation products not only in released CO2 and in microbial biomass, but also evaluation of decomposition of various biochar compounds with different chemical properties.

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Crossref · 10.1016/j.soilbio.2013.12.021

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Authors
Kuzyakov, Y., Bogomolova, I., & Glaser, B.
Affiliations
  • University of Göttingen (DE)
  • Martin Luther University Halle-Wittenberg (DE)
Corresponding author
Kuzyakov, Yakov
Venue
Soil Biology and Biochemistry
Publisher
Elsevier BV
Published
2014-03
Volume
70
Pages
229-236
ISSN
0038-0717 (ISSN-L)
OpenAlex
W2088901483
Cited by
664
References
3
Citations by year
2026: 57 · 2025: 70 · 2024: 66 · 2023: 72 · 2022: 70 · 2021: 53 · 2020: 54 · 2019: 46 · 2018: 51 · 2017: 40 · 2016: 39 · 2015: 29 · 2014: 15 · 2013: 1
FWCI
58.02
Type
journal article
Language
en
Open access
closed
Locations
  • Soil Biology and Biochemistry (publishedVersion)
  • GRO (submittedVersion)
Funders
German Academic Exchange Service (DAAD)
Topics
  • Life Sciences › Agricultural and Biological Sciences › Soil Science › Soil Carbon and Nitrogen Dynamics
  • Physical Sciences › Environmental Science › Global and Planetary Change › Fire effects on ecosystems
  • Physical Sciences › Engineering › Biomedical Engineering › Thermochemical Biomass Conversion Processes
Keywords
biochar stability, pyrogenic carbon, black carbon, dissolved organic matter, microbial biomass, neutral lipids, glycolipids, phospholipids, polysaccharides, benzene polycarboxylic acids, Haplic Luvisol, loess, soil carbon

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