Pyrolysis temperature of biochar affects ecoenzymatic stoichiometry and microbial nutrient-use efficiency in a bamboo forest soil
•Microbial nutrient-use efficiencies were compared among biochars in a forest soil.•Ecoenzymatic stoichiometry reveals a nutrient limitation for microbes under biochar.•Biochar prepared at 500 °C and 700 °C increased microbial C-use efficiency.•Biochar prepared at 350 °C and 500 °C increased microbi...
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Published in | Geoderma Vol. 363; p. 114162 |
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Main Authors | , , , , , , , , , , , , |
Format | Journal Article |
Language | English |
Published |
Elsevier B.V
01.04.2020
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Subjects | |
Online Access | Get full text |
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Summary: | •Microbial nutrient-use efficiencies were compared among biochars in a forest soil.•Ecoenzymatic stoichiometry reveals a nutrient limitation for microbes under biochar.•Biochar prepared at 500 °C and 700 °C increased microbial C-use efficiency.•Biochar prepared at 350 °C and 500 °C increased microbial N-use efficiency.•Effect of biochar on microbial metabolic activity was pyrolysis temperature dependent.
A microcosm study was performed to investigate changes in soil enzyme activities and microbial C- and N-use efficiencies (CUE and NUE) with amendment of biochars prepared at three pyrolysis temperatures (350, 500 and 700 °C) in an acid bamboo (Phyllostachys praecox) forest soil. The results showed that, compared to the non-amended control, biochars produced at 500 and 700 °C significantly (P < 0.05) increased soil pH, total N, and dissolved N (DN) concentrations, whereas significantly decreased dissolved organic C (DOC) and exchangeable acidity concentrations after three months. The microbial biomass C (MBC) and N (MBN) and the ratio of fungi: bacteria (F:B) were only significantly increased under 350 °C biochar. The ratios of both soil C:N and DOC:DN to MBC:MBN were reduced under 500 and 700 °C biochars, suggesting a lower C:N imbalance between resources and microorganism. The ratio of C- to N-acquiring enzyme activities increased gradually under biochars with increasing temperature. Moreover, microbial CUE increased whereas NUE declined under biochars at 500 and 700 °C, and the threshold elemental ratio (TER) revealed that the microbial nutrient metabolisms were limited by N in soils amended with residue, but were limited by C under biochars at 500 and 700 °C. Structural equation modeling indicated that the C:N imbalance had a great impact on microbial CUE, while changes in F:B ratio and soil pH were closely associated with NUE. This study suggests that changes in microbial nutrient-use efficiency and ecoenzymatic stoichiometry reveals a clear C-limitation, but a N-availability under short-term amendment of biochar produced at a high pyrolysis temperature. |
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Bibliography: | ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 23 |
ISSN: | 0016-7061 1872-6259 |
DOI: | 10.1016/j.geoderma.2019.114162 |