Soil nitrous oxide emissions following crop residue addition: a meta-analysis

被引:402
作者
Chen, Huaihai [1 ]
Li, Xuechao [1 ,2 ,3 ]
Hu, Feng [2 ]
Shi, Wei [1 ]
机构
[1] N Carolina State Univ, Dept Soil Sci, Raleigh, NC 27695 USA
[2] Nanjing Agr Univ, Lab Soil Ecol, Coll Resources & Environm Sci, Nanjing 210095, Jiangsu, Peoples R China
[3] Wujiang Environm Protect Bur, Suzhou 215200, Jiangsu, Peoples R China
关键词
arable soil; C:N ratio; crop residue; meta-analysis; nitrous oxide; soil CO2 respiration; soil pH; soil texture; water-filled pore space; N2O EMISSIONS; PLANT RESIDUES; NITRIC-OXIDE; DENITRIFICATION; WATER; NITRATE; NITRIFICATION; TEXTURE; DECOMPOSITION; MANAGEMENT;
D O I
10.1111/gcb.12274
中图分类号
X176 [生物多样性保护];
学科分类号
090705 ;
摘要
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 N2O, a potent greenhouse gas and ozone depletion substance. Residue effects on soil N2O emissions have gained considerable attention since early 1990s; yet, it is still a great challenge to predict the magnitude and direction of soil N2O emissions following residue amendment. Here, we used a meta-analysis to assess residue impacts on soil N2O 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 N2O 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 N2O emissions were positively related to the amounts of residue C input as well as residue effects on soil CO2 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 N2O production. Perhaps, by stimulating microbial respiration, crop residues enhanced oxygen depletion and therefore promoted anaerobic conditions for denitrification and N2O production. Our meta-analysis highlights the necessity to connect the quantity and quality of crop residues with soil properties for predicting soil N2O emissions.
引用
收藏
页码:2956 / 2964
页数:9
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