The amount of nitrous oxide (N2O) continues to increase in the atmosphere.
Agricultural use of nitrogen fertilizers in the tropics is thought to be an
important source of atmospheric N2O. High frequency, highly precise measur
ements of the N2O flux were made with an automated system deployed in N fer
tilized and unfertilized agricultural plots of papaya and corn in Costa Ric
a for an entire corn crop growth to harvest cycle. N2O fluxes were as high
as 64 ng N-N2O cm(-2) h(-1) from fertilized versus 12 ng N-N2O cm(-2) h(-1)
from unfertilized corn and 28 ng N-N2O cm(-2) h(-1) from fertilized versus
4.6 ng N-N2O cm(-2) h(-1) from unfertilized papaya. Fertilized corn releas
ed more N2O than fertilized papaya over the 125 days of the crop cycle, 1.8
3 kg N ha(-1) versus 1.37 kg N ha(-1). This represents a loss as N2O of 1.1
and 0.9% of the total N applied as ammonium nitrate to the corn and papaya
, respectively. As has often been observed, N2O fluxes were highly variable
. The fastest rates of emission were associated with fertilization and high
soil moisture. A diurnal cycle in the fluxes was not evident probably due
to the minimal day/night temperature fluctuations. Each chamber was measure
d between 509 and 523 times over the course of the experiment. This allows
us to evaluate the effect on constructed mean fluxes of lowered sampling fr
equencies. Sampling each collar about once a day throughout the crop cycle
(25% of the data set) could result in a calculated mean flux from any indiv
idual chamber that can vary by as much as 20% even though the calculated me
an would probably be within 10% of the mean of the complete data set. The u
ncertainty increases very rapidly at lower sampling frequencies. For exampl
e, if only 10% of the data set were used which would be the equivalent of s
ampling every other day, a very high sampling frequency in terms of manual
measurements, the calculated mean flux could vary by as much as 40% or more
at any given site.