Critical comparison of the impact of biochar and wood ash on soil organic matter cycling and grassland productivity

被引:47
|
作者
Reed, Eleanor Y. [1 ,2 ]
Chadwick, David R. [1 ]
Hill, Paul W. [1 ]
Jones, Davey L. [1 ]
机构
[1] Bangor Univ, Sch Environm Nat Resources & Geog, Bangor LL57 2UW, Gwynedd, Wales
[2] Wardell Armstrong LLP, 11 Waterloo Sq, Newcastle Upon Tyne NE1 4DP, Tyne & Wear, England
来源
关键词
Black carbon; Charcoal; Life cycle assessment; Nutrient cycling; PLFA; MICROBIAL COMMUNITIES; PLANT-GROWTH; CARBON; CROP; EMISSIONS; BIOMASS; MINERALIZATION; TEMPERATURE; MECHANISMS; DYNAMICS;
D O I
10.1016/j.soilbio.2017.03.012
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Wood represents the single most important source of renewable energy worldwide and depending on the mechanism of energy production can lead to the production of by-products with vastly different properties (i.e. wood ash (WA) from incineration and biochar (BC) from pyrolysis). These are typically applied to land, however, a critical comparison of their impact on soil quality and carbon (C) cycling is lacking. To address this, we generated biochar (450 degrees C) and wood ash (870 degrees C) from the same mixed hardwood feedstock and added it to an agricultural grassland at comparable rates under both laboratory and field conditions (10 t ha(-1) and 571 kg ha(-1) for BC and WA, respectively). We hypothesized that alkaline, nutrient-rich wood ash would stimulate microbial activity, resulting in the loss of soil organic matter (SOM), while biochar which is recalcitrant to microbial attack would promote the stabilization of native SOM. The effects on the soil microbial community and soil C and N cycling were determined over 1 year. Overall, biochar promoted soil quality by enhancing nutrient availability (P and K), moisture retention and increasing soil C content. However, it was also associated with an increase in below-ground CO2 loss. As plant productivity was unaffected and laboratory incubations of biochar with C-14-labelled SOM showed no indication of priming, we deduce that this CO2 originates from the biochar itself. This is supported by the lack of effect of biochar on soil N cycling, microbial biomass and community structure. Wood ash had almost no effect on either soil quality or vegetation quality (yield and foliar nutrient content) under field conditions but did induce negative SOM priming under both laboratory and field conditions. We conclude that when applied at field-relevant rates, neither amendment had a detrimental effect on native SOM cycling. While wood ash promotes the retention of native SOM, biochar may be a better strategy for enhancing SOM levels because of its intrinsic recalcitrant character, however, this needs to be offset against the reduced amount of energy derived from pyrolysis in comparison to incineration. (C) 2017 Elsevier Ltd. All rights reserved.
引用
收藏
页码:134 / 142
页数:9
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