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Soil nitrous oxide emissions following crop residue addition: a meta‐analysis
Author(s) -
Chen Huaihai,
Li Xuechao,
Hu Feng,
Shi Wei
Publication year - 2013
Publication title -
global change biology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 4.146
H-Index - 255
eISSN - 1365-2486
pISSN - 1354-1013
DOI - 10.1111/gcb.12274
Subject(s) - residue (chemistry) , crop residue , amendment , environmental science , soil water , agronomy , greenhouse gas , environmental chemistry , nitrous oxide , soil respiration , chemistry , soil science , agriculture , ecology , biochemistry , organic chemistry , political science , law , biology
Annual production of crop residues has reached nearly 4 billion metric tons globally. Retention of this large amount of residues on agricultural land can be beneficial to soil C sequestration. Such potential impacts, however, may be offset if residue retention substantially increases soil emissions of N 2 O, a potent greenhouse gas and ozone depletion substance. Residue effects on soil N 2 O emissions have gained considerable attention since early 1990s; yet, it is still a great challenge to predict the magnitude and direction of soil N 2 O emissions following residue amendment. Here, we used a meta‐analysis to assess residue impacts on soil N 2 O emissions in relation to soil and residue attributes, i.e., soil pH , soil texture, soil water content, residue C and N input, and residue C : N ratio. Residue effects were negatively associated with C : N ratios, but generally residue amendment could not reduce soil N 2 O emissions, even for C : N ratios well above ca. 30, the threshold for net N immobilization. Residue effects were also comparable to, if not greater than, those of synthetic N fertilizers. In addition, residue effects on soil N 2 O emissions were positively related to the amounts of residue C input as well as residue effects on soil CO 2 respiration. Furthermore, most significant and stimulatory effects occurred at 60–90% soil water‐filled pore space and soil pH 7.1–7.8. Stimulatory effects were also present for all soil textures except sand or clay content ≤10%. However, inhibitory effects were found for soils with >90% water‐filled pore space. Altogether, our meta‐analysis suggests that crop residues played roles beyond N supply for N 2 O production. Perhaps, by stimulating microbial respiration, crop residues enhanced oxygen depletion and therefore promoted anaerobic conditions for denitrification and N 2 O production. Our meta‐analysis highlights the necessity to connect the quantity and quality of crop residues with soil properties for predicting soil N 2 O emissions.

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