Nutrient cycling and greenhouse gas emissions from soil amended with biochar-manure mixtures

被引:29
作者
Romero, Carlos M. [1 ,2 ]
Li, Chunli [1 ,2 ]
Owens, Jen [1 ]
Ribeiro, Gabriel O. [3 ]
Mcallister, Tim A. [1 ]
Okine, Erasmus [2 ]
Hao, Xiying [1 ]
机构
[1] Agr & Agrifood Canada, Lethbridge Res & Dev Ctr, Lethbridge, AB T1J 4B1, Canada
[2] Univ Lethbridge, Fac Arts & Sci, Dept Biol Sci, Lethbridge, AB T1K 3M4, Canada
[3] Univ Saskatchewan, Dept Anim & Poultry Sci, Saskatoon, SK S7N 5A8, Canada
关键词
animal husbandry; black carbon; carbon dioxide; methane; Orthic Black Chernozem; soil fertility; DISSOLVED ORGANIC-MATTER; NITROUS-OXIDE; ENZYME-ACTIVITIES; METHANE EMISSIONS; CALCAREOUS SOIL; LAND-USE; CARBON; MANAGEMENT; IMPACT; WATER;
D O I
10.1016/S1002-0160(20)60071-6
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Integrating biochar into cattle diets has recently emerged as a potential management practice for improving on-farm productivity. Yet, information concerning the cycling of biochar-manure mixtures is scarce. A 70-d incubation experiment was conducted within two surface (0-15 cm) Mollisols with contrasting textures, i.e., sandy clay loam (Raymond) and clayey (Lethbridge), to evaluate the effects of biochar (3 Mg ha(-1)) on cumulative greenhouse gas (GHG) emissions and related fertility attributes in the presence or absence of cattle manure (120 Mg ha(-1)). Five treatments were included: i) non-amended soil (control, CK), ii) soil amended with pinewood biochar (B), iii) soil amended with beef cattle manure (M) (manure from cattle on a control diet), iv) soil amended with biochar-manure (BM) (manure from cattle on a control diet, with pinewood biochar added at 20 g kg(-1) of diet dry matter), and v) soil amended with B and M at the aforementioned rates (B+M). A total of 40 soil columns were prepared and incubated at 21 degrees C and 60%-80% water-holding capacity. On average, total CO2 fluxes increased by 2.2- and 3.8-fold under manure treatments (i.e., M, BM, and B+M), within Raymond and Lethbridge soils, respectively, relative to CK and B. Similarly, total CH4 fluxes were the highest (P < 0.05) in Raymond soil under B+M and BM relative to CK and B, and in Lethbridge soil under M and BM relative to CK and B. In Lethbridge soil, application of BM increased cumulative N2O emissions by 1.8-fold relative to CK. After 70-d incubation, amendment with BM increased (P < 0.05) PO4-P and NO3-N + NH4-N availability in Raymond and Lethbridge soils compared with B. A similar pattern was observed for water-extractable organic carbon in both soils, with BM augmenting (P < 0.05) the occurrence of labile carbon over CK and B. It can be concluded that biochar, manure, and/or biochar-manure have contrasting short-term effects on the biogeochemistry of Mollisols. At relatively low application rates, biochar does not necessarily counterbalance manure-derived inputs. Although BM did not mitigate the flux of GHGs over M, biochar-manure has the potential to recycle soil nutrients in semiarid drylands.
引用
收藏
页码:289 / 302
页数:14
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