Understanding the Relations between Soil Biochemical Properties and N2O Emissions in a Long-Term Integrated Crop–Livestock System

Author:

de Carvalho Arminda Moreira1ORCID,Ramos Maria Lucrécia Gerosa2ORCID,Dos Santos Divina Cléia Resende2ORCID,de Oliveira Alexsandra Duarte1ORCID,de Carvalho Mendes Ieda1ORCID,Silva Stefany Braz2ORCID,de Sousa Thais Rodrigues2ORCID,Dantas Raíssa de Araujo1ORCID,Silva Antonio Marcos Miranda3ORCID,Marchão Robélio Leandro1ORCID

Affiliation:

1. Embrapa Cerrados, BR-020, Km 18, Planaltina 73310-970, Brazil

2. Faculty of Agronomy and Veterinary Medicine, University of Brasilia, Campus Darcy Ribeiro, Brasilia 70910-970, Brazil

3. Department of Soil Science, University of São Paulo-ESALQ, Av. Pádua Dias, 11, Piracicaba 13418-900, Brazil

Abstract

Edaphoclimatic conditions influence nitrous oxide (N2O) emissions from agricultural systems where soil biochemical properties play a key role. This study addressed cumulative N2O emissions and their relations with soil biochemical properties in a long-term experiment (26 years) with integrated crop–livestock farming systems fertilized with two P and K rates. The farming systems consisted of continuous crops fertilized with half of the recommended P and K rates (CCF1), continuous crops at the recommended P and K rates (CCF2), an integrated crop–livestock system with half of the recommended P and K rates (ICLF1), and an integrated crop–livestock at the recommended P and K rates (ICLF2). The ICLF2 may have promoted the greatest entry of carbon into the soil and positively influenced the soil’s biochemical properties. Total carbon (TC) was highest in ICLF2 in both growing seasons. The particulate and mineral-associated fractions in 2016 and 2017, respectively, and the microbial biomass fraction in the two growing seasons were also very high. Acid phosphatase and arylsulfatase in ICLF1 and ICLF2 were highest in 2016. The soil properties correlated with cumulative N2O emissions were TC, total nitrogen (TN), particulate nitrogen (PN), available nitrogen (AN), mineral-associated organic carbon (MAC), and microbial biomass carbon (MBC). The results indicated that ICLF2 induces an accumulation of more stable organic matter (OM) fractions that are unavailable to the microbiota in the short term and result in lower N2O emissions.

Funder

National Council for Scientific and Technological Development

Conselho Nacional de Desenvolvimento Científico e Tecnológico

CNPq for scholarship

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior

Publisher

MDPI AG

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3. Global soil nitrous oxide emissions since the preindustrial era estimated by an ensemble of terrestrial biosphere models: Magnitude, attribution, and uncertainty;Tian;Glob. Chang. Biol.,2019

4. Stocker, T.F., Qin, D., Plattner, G.-K., Tignor, M., Allen, S.K., Boschung, J., Nauels, A., Xia, Y., Bex, V., and Midgley, P.M. (2014). Climate Change 2013: The Physical Science Basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change, Cambridge University Press. Available online: https://www.ipcc.ch/site/assets/uploads/2018/02/WG1AR5_Chapter06_FINAL.pdf.

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