M. V. Galdos, J. R. Soares, K. S. Lourenço, P. Harris, M. Zeri, G. Cunha-Zeri, V. P. Vargas, I. A. M. Degaspari, H. Cantarella
{"title":"甘蔗种植过程中土壤氧化亚氮排放的多试验评价","authors":"M. V. Galdos, J. R. Soares, K. S. Lourenço, P. Harris, M. Zeri, G. Cunha-Zeri, V. P. Vargas, I. A. M. Degaspari, H. Cantarella","doi":"10.1007/s10705-023-10321-w","DOIUrl":null,"url":null,"abstract":"Abstract Soil nitrous oxide (N 2 O) fluxes comprise a significant part of the greenhouse gas emissions of agricultural products but are spatially and temporally variable, due to complex interactions between climate, soil and management variables. This study aimed to identify the main factors that affect N 2 O emissions under sugarcane, using a multi-site database from field experiments. Greenhouse gas fluxes, soil, climate, and management data were obtained from 13 field trials spanning the 2011–2017 period. We conducted exploratory, descriptive and inferential data analyses in experiments with varying fertiliser and stillage (vinasse) type and rate, and crop residue rates. The most relevant period of high N 2 O fluxes was the first 46 days after fertiliser application. The results indicate a strong positive correlation of cumulative N 2 O with nitrogen (N) fertiliser rate, soil fungi community (18S rRNA gene), soil ammonium (NH 4 + ) and nitrate (NO 3 − ); and a moderate negative correlation with amoA genes of ammonia-oxidising archaea (AOA) and soil organic matter content. The regression analysis revealed that easily routinely measured climate and management-related variables explained over 50% of the variation in cumulative N 2 O emissions, and that additional soil chemical and physical parameters improved the regression fit with an R 2 = 0.65. Cross-wavelet analysis indicated significant correlations of N 2 O fluxes with rainfall and air temperature up to 64 days, associated with temporal lags of 2 to 4 days in some experiments, and presenting a good environmental control over fluxes in general. The nitrogen fertiliser mean emission factors ranged from 0.03 to 1.17% of N applied, with urea and ammonium nitrate plus vinasse producing high emissions, while ammonium sulphate, ammonium nitrate without vinasse, calcium nitrate, and mitigation alternatives (nitrification inhibitors and timing of vinasse application) producing low N 2 O-EFs. Measurements from multiple sites spanning several cropping seasons were useful for exploring the influence of environmental and management-related variables on soil N 2 O emissions in sugarcane production, providing support for global warming mitigation strategies, nitrogen management policies, and increased agricultural input efficiency.","PeriodicalId":19336,"journal":{"name":"Nutrient Cycling in Agroecosystems","volume":"67 4","pages":"0"},"PeriodicalIF":2.4000,"publicationDate":"2023-10-21","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Multi-experiment assessment of soil nitrous oxide emissions in sugarcane\",\"authors\":\"M. V. Galdos, J. R. Soares, K. S. Lourenço, P. Harris, M. Zeri, G. Cunha-Zeri, V. P. Vargas, I. A. M. Degaspari, H. Cantarella\",\"doi\":\"10.1007/s10705-023-10321-w\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Abstract Soil nitrous oxide (N 2 O) fluxes comprise a significant part of the greenhouse gas emissions of agricultural products but are spatially and temporally variable, due to complex interactions between climate, soil and management variables. This study aimed to identify the main factors that affect N 2 O emissions under sugarcane, using a multi-site database from field experiments. Greenhouse gas fluxes, soil, climate, and management data were obtained from 13 field trials spanning the 2011–2017 period. We conducted exploratory, descriptive and inferential data analyses in experiments with varying fertiliser and stillage (vinasse) type and rate, and crop residue rates. The most relevant period of high N 2 O fluxes was the first 46 days after fertiliser application. The results indicate a strong positive correlation of cumulative N 2 O with nitrogen (N) fertiliser rate, soil fungi community (18S rRNA gene), soil ammonium (NH 4 + ) and nitrate (NO 3 − ); and a moderate negative correlation with amoA genes of ammonia-oxidising archaea (AOA) and soil organic matter content. The regression analysis revealed that easily routinely measured climate and management-related variables explained over 50% of the variation in cumulative N 2 O emissions, and that additional soil chemical and physical parameters improved the regression fit with an R 2 = 0.65. Cross-wavelet analysis indicated significant correlations of N 2 O fluxes with rainfall and air temperature up to 64 days, associated with temporal lags of 2 to 4 days in some experiments, and presenting a good environmental control over fluxes in general. The nitrogen fertiliser mean emission factors ranged from 0.03 to 1.17% of N applied, with urea and ammonium nitrate plus vinasse producing high emissions, while ammonium sulphate, ammonium nitrate without vinasse, calcium nitrate, and mitigation alternatives (nitrification inhibitors and timing of vinasse application) producing low N 2 O-EFs. 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Multi-experiment assessment of soil nitrous oxide emissions in sugarcane
Abstract Soil nitrous oxide (N 2 O) fluxes comprise a significant part of the greenhouse gas emissions of agricultural products but are spatially and temporally variable, due to complex interactions between climate, soil and management variables. This study aimed to identify the main factors that affect N 2 O emissions under sugarcane, using a multi-site database from field experiments. Greenhouse gas fluxes, soil, climate, and management data were obtained from 13 field trials spanning the 2011–2017 period. We conducted exploratory, descriptive and inferential data analyses in experiments with varying fertiliser and stillage (vinasse) type and rate, and crop residue rates. The most relevant period of high N 2 O fluxes was the first 46 days after fertiliser application. The results indicate a strong positive correlation of cumulative N 2 O with nitrogen (N) fertiliser rate, soil fungi community (18S rRNA gene), soil ammonium (NH 4 + ) and nitrate (NO 3 − ); and a moderate negative correlation with amoA genes of ammonia-oxidising archaea (AOA) and soil organic matter content. The regression analysis revealed that easily routinely measured climate and management-related variables explained over 50% of the variation in cumulative N 2 O emissions, and that additional soil chemical and physical parameters improved the regression fit with an R 2 = 0.65. Cross-wavelet analysis indicated significant correlations of N 2 O fluxes with rainfall and air temperature up to 64 days, associated with temporal lags of 2 to 4 days in some experiments, and presenting a good environmental control over fluxes in general. The nitrogen fertiliser mean emission factors ranged from 0.03 to 1.17% of N applied, with urea and ammonium nitrate plus vinasse producing high emissions, while ammonium sulphate, ammonium nitrate without vinasse, calcium nitrate, and mitigation alternatives (nitrification inhibitors and timing of vinasse application) producing low N 2 O-EFs. Measurements from multiple sites spanning several cropping seasons were useful for exploring the influence of environmental and management-related variables on soil N 2 O emissions in sugarcane production, providing support for global warming mitigation strategies, nitrogen management policies, and increased agricultural input efficiency.
期刊介绍:
Nutrient Cycling in Agroecosystems considers manuscripts dealing with all aspects of carbon and nutrient cycling as well as management and examining their effect in ecological, agronomic, environmental and economic terms. Target agroecosystems include field crop, organic agriculture, urban or peri-urban agriculture, horticulture, bioenergy, agroforestry, livestock, pasture, and fallow systems as well as their system components such as plants and the fertility, chemistry, physics or faunal and micro-biology of soils. The scale of observation is the cycles in the soil-plant-animal system on or relevant to a field or watershed level as well as inputs from or losses to the anthroposphere, atmosphere and hydrosphere. Studies should thus consider the wider system in the examination of cycling and fluxes in agroecosystems or their components. These may include typically multi-year field observations, farm gate budgets, watershed studies, life cycle assessments, enterprise and economic analyses, or regional and global modeling. Management objectives may not only include the maximization of food, fiber and fuel production, but also its environmental and economic impact. The results must allow mechanistic conclusions of broad applicability and distinguish itself from empirical results or case studies of merely local or regional importance. If unsure whether a study fits into this scope, please contact the editor with a brief inquiry before manuscript submission.