Maize biochars accelerate short-term soil nitrogen dynamics in a loamy sand soil

被引:283
作者
Nelissen, Victoria [1 ,2 ]
Rutting, Tobias [3 ]
Huygens, Dries [2 ,4 ]
Staelens, Jeroen [2 ,5 ]
Ruysschaert, Greet [1 ]
Boeckx, Pascal [2 ]
机构
[1] Inst Agr & Fisheries Res ILVO, Plant Sci Unit, B-9820 Merelbeke, Belgium
[2] Univ Ghent, Fac Biosci Engn, Isotope Biosci Lab ISOFYS, B-9000 Ghent, Belgium
[3] Univ Gothenburg, Dept Biol & Environm Sci, S-40530 Gothenburg, Sweden
[4] Univ Austral Chile, Fac Agr Sci, Inst Agr Engn & Soil Sci, Valdivia, Chile
[5] Univ Ghent, Fac Biosci Engn, Forest & Nat Lab, Gontrode, Belgium
基金
比利时弗兰德研究基金会;
关键词
Biochar; N-15; Tracing model; Nitrogen; Immobilization; Mineralization; Gross transformation; MICROBIAL BIOMASS; N-15; TRANSFORMATIONS; MINERALIZATION; MECHANISMS;
D O I
10.1016/j.soilbio.2012.05.019
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Biochar addition to soils has been proposed as a means to increase soil fertility and carbon sequestration. However, its effect on soil nitrogen (N) cycling and N availability is poorly understood. To gain better insight into the short-term effects of biochar on gross N transformation processes, a N-15 tracing experiment in combination with numerical data analysis was conducted. An arable loamy sand soil was used and mixed with two silage maize biochars, produced at 350 degrees C and 550 degrees C. The results showed accelerated soil N cycling following biochar addition, with increased gross N mineralization (185-221%), nitrification (10-69%) and ammonium (NH4+) consumption rates (333-508%). Moreover, transfer of N from a recalcitrant soil organic N (N-rec) pool to a more labile soil organic N (N-lab) pool was observed. In the control treatment, 8% of the NH4+ mineralized from N-lab was immobilized to the N-rec pool. In contrast, 79% and 55% of the NH4+ mineralized from N-rec were immobilized to the N-rec pool in the treatment with biochar-350 degrees C and biochar-550 degrees C, respectively. NH4+-N was adsorbed quickly to biochar at the start of the experiment, thereby buffering plant-available N. In conclusion, these types of biochar accelerated soil N transformations in the short term, thereby increasing soil N bio-availability, through a combined effect of mineralization of the recalcitrant soil organic N pool and subsequent NH4+ immobilization in a labile soil organic N pool. (C) 2012 Elsevier Ltd. All rights reserved.
引用
收藏
页码:20 / 27
页数:8
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