R. Stepanauskas et al., NITROGEN TRANSFORMATIONS IN WETLAND SOIL CORES MEASURED BY N-15 ISOTOPE PAIRING AND DILUTION AT 4 INFILTRATION RATES, Applied and environmental microbiology, 62(7), 1996, pp. 2345-2351
The effect of water infiltration rate (IR) on nitrogen cycling in a sa
turated wetland soil was investigated by applying a N-15 isotope dilut
ion and pairing method. Water containing [N-15]nitrate was infiltrated
through 10-cm-long cores of sieved and homogenized soil at rates of 7
2, 168, 267, and 638 mm day(-1). Then the frequencies of N-30(2), N-29
(2), (NO3-)-N-15, and (NH4+)-N-15 in the outflow water were measured,
This method allowed simultaneous determination of nitrification, coupl
ed and uncoupled denitrification, and nitrate assimilation rates. From
3% (at the highest IR) to 95% (at the lowest IR) of nitrate was remov
ed from the water, mainly by denitrification, The nitrate removal was
compensated for by the net release of ammonium and dissolved organic n
itrogen, Lower oxygen concentrations in the soil at lower IRs led to a
sharper decrease in the nitrification rate than in the ammonification
rate, and, consequently, more ammonium leaked from the soil. The decr
easing organic-carbon-to-nitrogen ratio (from 12.8 to 5.1) and the inc
reasing light A(250)/A(365) ratio (from 4.5 to 5.2) indicated an incre
asing bioavailability of the outflowing dissolved organic matter with
increasing IR, The efflux of nitrous oxide was also very sensitive to
IR and increased severalfold when a zone of low oxygen concentration a
as close to the outlet of the soil cores. N2O then constituted 8% of t
he total gaseous N lost from the soil.