Biochar-mediated changes in soil quality and plant growth in a three year field trial

被引:702
作者
Jones, D. L. [1 ]
Rousk, J. [1 ,2 ]
Edwards-Jones, G. [1 ]
DeLuca, T. H. [1 ]
Murphy, D. V. [3 ]
机构
[1] Bangor Univ, Environm Ctr Wales, Bangor LL57 2UW, Gwynedd, Wales
[2] Lund Univ, Dept Biol, Microbial Ecol, S-22362 Lund, Sweden
[3] Univ Western Australia, Fac Nat & Agr Sci, UWA Inst Agr, Sch Earth & Environm,Soil Biol Grp, Crawley, WA 6009, Australia
基金
瑞典研究理事会;
关键词
Black carbon; Black nitrogen; Carbon sequestration; Charcoal; Soil organic matter; Climate change mitigation; LEUCINE INCORPORATION; AMMONIA VOLATILIZATION; MICROBIAL ACTIVITY; PROTEIN-SYNTHESIS; BACTERIAL-GROWTH; ORGANIC-C; CARBON; TURNOVER; NITROGEN; FUNGAL;
D O I
10.1016/j.soilbio.2011.10.012
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
While many laboratory studies have focused on the short term effects of biochar addition to soil), there have been comparatively few tracing its longer term effects in the field. This study investigated the multiyear impact of biochar on crop performance and soil quality with specific emphasis on carbon (C) and nitrogen (N) cycling over a 3 y period. Biochar was added to an agricultural field at 0, 25 and 50 t ha(-1) and planted with maize (year 1) and grass (years 2 and 3). Biochar addition affected plant performance in the grass crop with significant increases in foliar N (year 2) and above-ground biomass (year 3). Below-ground, biochar increased soil respiration, fungal and bacterial growth rate and turnover in year 2. This change coincided with a shift toward a bacterial dominated decomposer community, suggesting a decrease in the potential for microbially mediated C sequestration. Biochar did not affect dissolved organic C (DOC) and N (DON), NO3- or NH4+ pool sizes. Similarly, biochar addition had limited effects on the turnover of C-14-labelled SOC (plant litter), DOC (sugars and organic acids) and DON (amino acids) and no long term effect on N mineralization, NH3 volatilization, denitrification and NH4+ sorption. After 3 years in the field, the alkalinity associated with the biochar had been fully neutralized and biochar lost most of its cations (K, Na, Ca) but had built up an associated microbial community. We conclude that biochar addition to soil causes small and potentially transient changes in a temperate agroecosystem functioning. Importantly, many of the short-term effects of biochar on plant growth and soil behavior reported from laboratory studies were not observed in the field emphasizing the need for long term field trials to help inform agronomic management decisions involving biochar. (C) 2011 Elsevier Ltd. All rights reserved.
引用
收藏
页码:113 / 124
页数:12
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