@Article{ZeriYanCunGibBer:2020:ChTeVa,
author = "Zeri, Marcelo and Yang, Wendy H. and Cunha Zeri, Gisleine da Silva
and Gibson, Christy D. and Bernacchi, Carl J.",
affiliation = "{Centro Nacional de Monitoramento e Alertas de Desastres Naturais
(CEMADEN)} and {University of Illinois at Urbana-Champaign} and
{Instituto Nacional de Pesquisas Espaciais (INPE)} and {University
of Illinois at Urbana-Champaign} and {University of Illinois at
Urbana-Champaign}",
title = "Nitrous oxide fluxes over establishing biofuel crops:
characterization of temporal variability using the cross-wavelet
analysis",
journal = "Global Change Biology Bioenergy",
year = "2020",
volume = "12",
number = "9",
pages = "756--770",
month = "Sept.",
keywords = "agriculture, biofuels, nitrous oxide fluxes, wavelet analysis.",
abstract = "Emissions of nitrous oxide (N2O) over croplands are a major source
of greenhouse gases to the atmosphere. The precise accounting of
sources of N2O is essential to national and global budgets, as
well as the understanding of the spatial and temporal
relationships with environmental variables such as rainfall, air
and soil temperature, and soil moisture. The objective of this
work was to investigate the temporal correlations of N2O fluxes
with soil and air temperatures, as well as soil moisture. N2O
fluxes were measured over four biofuel crops in Central Illinois
during their establishment phase. Measurements were carried out
from 2009 to 2011 using a trace gas analyzer (TGA) with tunable
laser technology. Measurements of concentrations of N2O and
CO(2)were taken at the center of four plots of maize/soybean
rotation, miscanthus (Miscanthus x giganteus), switchgrass
(Panicum virgatum) and a mixture of native prairie plants.
Cumulative fluxes indicate an average emission of nitrogen via N2O
fluxes on the order of 1.5 kg N ha(-1) year(-1), in agreement with
chamber measurements previously reported for the site. N2O fluxes
were associated with peaks in soil and air temperature, and soil
moisture, particularly during spring and winter thaws.
Cross-wavelet analysis was used to investigate the correlation
between N2O fluxes and those variables. Results indicate that N2O
fluxes and meteorological variables have significant covariance in
time scales ranging from 4 to 32 days. In addition, temporal
delays of 1-8 days were found in those relationships.
Cross-wavelet patterns were similar when relating N2O fluxes with
soil temperature, air temperature and soil moisture. The temporal
patterns of fluxes and environmental variables reported here
support the modeling of emissions and highlight the importance of
considering the timing of fluxes in relation to trends in
meteorological variables.",
doi = "10.1111/gcbb.12728",
url = "http://dx.doi.org/10.1111/gcbb.12728",
issn = "1757-1693",
language = "en",
targetfile = "zeri_nitrous.pdf",
urlaccessdate = "15 maio 2024"
}