Tw. Speir et al., AEROBIC EMISSIONS OF N2O AND N-2 FROM SOIL CORES - FACTORS INFLUENCING PRODUCTION FROM N-13 LABELED NO3- AND NH4+, Soil biology & biochemistry, 27(10), 1995, pp. 1299-1306
Gas-stripping procedures, with air as the stripping and carrying gas,
were used to investigate the effects of amendments on production in so
il cores of N2O and N-2 arising from N-13-labelled NO3- (denitrificati
on) or NH4+ (nitrification). These cores had been used previously to i
nvestigate ambient gas emission rates; the rates after amendment were
compared with these ''natural'' emission results. Using (NO3-)-N-13, t
he results of amendment with H2O, glucose, NO3- or glucose + NO3-, sev
eral hours before the experiment, were usually explicable in terms of
effects on microbial numbers and soil O-2 status. However, results obt
ained immediately after amendments were made, before de novo enzyme sy
nthesis or change of O-2 status would have occurred, were generally di
fficult to interpret. Amendments which included NO3- gave spuriously l
ow N2O and N-2 emission rates, probably due to isotopic dilution. The
immediate effect of amendments may vary from time to time and depend u
pon soil conditions at the time of sampling. Only glucose consistently
stimulated gas emissions, presumably because it enhanced activity of
the existing denitrifying population. Using (NH4+)-N-13, amendment wit
h H2O increased production of N-2, but not N2O, and amendment with glu
cose reduced emissions of both gases. The advantages and disadvantages
of this N-13 method for investigating the influence on N2O and N-2 pr
oduction of various soil amendments, and the relationships of these re
sults with those of more conventional studies, are discussed.