Nitrification inhibitor DMPP mitigated N2O emissions and decreased N2 losses in a low-nitrate vegetable soil after application of manure
- 1College of Eco-environment Engineering, Guizhou Minzu University, Guiyang 550025, China
- 2College of Resources and Environmental Sciences, China Agricultural University, Beijing 100193, China
- 3Environment and Plant Protection Institute, Chinese Academy of Tropical Agricultural Sciences, Haikou 571101, China
In China, amounts of organic manure as basal fertilizer application along with flooding irrigation usually resulted in large N2O emissions from intensively protected vegetable soils. However, little attention paid on the N2O emission bursts after application of manure, in a newly established vegetable soil with a low-nitrate content. The nitrification inhibitor, 3,4-dimethylpyrazole phosphate (DMPP), can be used to reduce N2O emissions from agricultural soils, little is known about how DMPP affect N2 emissions and gaseous nitrogen (N2O+N2) losses. Here, we conducted a microcosm experiment in a robotized incubation system under an aerobic (O2/He) condition. Dried chicken manure was applied with and without DMPP to a protected vegetable soil. Two drying-rewetting events occurred during the 19 days monitoring period, and the relevant soil properties (e.g., NO2-, WFPS, DOC, DON, SMBC) were analyzed. Our results showed DMPP addition strongly retarded soil nitrification process that kept a higher NH4+ concentration than that of only manure application. A significant decline of NO2- and NO3- concentration was found in a manure-treated soil with DMPP addition. Clearly, DMPP addition significantly reduced N2O emissions from the protected vegetable soil by 77.0% and remarkably decreased N2 emissions and overall N2O+N2 losses (compared with manure alone) by 51.9% and 54.0%, respectively. Pearson analysis showed that soil N2O fluxes were significantly related to soil WFPS, NH4+, SMBC (P<0.01) and SMBN (P<0.05), whereas N2 fluxes were significantly correlated with soil WFPS, SMBC (P<0.01), NO2-, NH4+ and SMBN (P<0.05) during the whole incubation. The fluxes of N2O+N2 were positively correlated with WFPS, NO2-, SMBC and SMBN, whereas negatively correlated with NH4+ (P<0.05). Moreover, the ratio of N2O to N2O+N2 (N2O/(N2O+N2)) was positively correlated with NO3- (P<0.05), and negatively correlated with DOC, DON and SMBC (P<0.01). An aggregated boosted tree (ABT) analysis further indicated that the relative influence of WFPS, SMBC and NH4+ on N2O fluxes were 19.4%, 14.9% and 12.8%, respectively. Moreover, the relative influence of WFPS on N2 fluxes was the largest (47.4%), followed by SMBC and SMBN (14.3% and 9.66%, respectively). In addition, the relative influence of WFPS, SMBN and SMBC on N2O+N2 losses were 32.6%, 17.0% and 12.6%, respectively, and the relative influence of SMBC, DOC and NO2- on N2O/(N2O+N2) were 22.5%, 20.2% and 11.1%, respectively. In conclusion, our data show that DMPP combined with manure can significantly reduce N2O and N2 emissions in a low-nitrate newly established vegetable soil, and their emissions were strongly affected by WFPS.
How to cite: Liu, Y., Yin, J., and Cao, W.: Nitrification inhibitor DMPP mitigated N2O emissions and decreased N2 losses in a low-nitrate vegetable soil after application of manure , EGU General Assembly 2021, online, 19–30 Apr 2021, EGU21-10794, https://doi.org/10.5194/egusphere-egu21-10794, 2021.