A laboratory study was conducted to compare methods of labelling the soil N
H4+ pool with N-15 as a prerequisite to the measurement of gross N minerali
sation. Composite soil (0-12 cm) was collected from 12 sites differing in l
and use and soil texture. Three methods were used to apply N-15 to the soil
: (i) addition of a (NH3)-N-15-air gas mixture to the headspace above the s
oil (gas jar), (ii) injection of a (NH3)-N-15-air gas mixture into re-packe
d soil cores (gas injector) and (iii) addition of a ((NH4)-N-15)(2)SO4 solu
tion pipetted onto the soil surface (solution), N-15 isotopic dilution was
determined between 24 and 72 h after N-15 application. Of the applied N-15
52 to 93% was recovered as inorganic N 24 h after application. Less N-15 wa
s recovered in the clay loam compared to the sandy loam and silty clay loam
for all methods. Recovery from the gas injector was lower than from the ga
s jar or solution treatments in the sandy loam and silty clay loam. No diff
erence in the recovery of applied N-15 between methods was observed in the
clay loam. N-15 isotopic dilution was less in the gas jar compared to the g
as injector and solution treatments. This resulted in significantly lower e
stimates of gross N mineralisation rates and NH4+ consumption for the gas j
ar treatment. The non-uniform distribution of N-15 through the soil probabl
y caused these differences as a consequence of (NH3)-N-15 dissolving quickl
y in the surface of the soil. In seven of the 12 soils, gross rates of N mi
neralisation were not significantly different when N-15 was applied as solu
tion or by gas injection. In the remaining five soils, estimates of gross N
mineralisation rates were greater in the solution treatment. Ammonium cons
umption was significantly different between the solution and gas injector t
reatments in three soils, Where there were differences in values for gross
N mineralisation and NH4+ consumption rates between methods, the effects we
re not associated with a particular soil texture or land use. Greater nitri
fication of (NH4+)-N-15 to (NO3-)-N-15 and shorter pseudo-residence rimes o
f the NH4+ pool were observed in the solution treatment compared to gas inj
ector, This suggests a difference in the distribution of N-15 within soil m
icrosites, with the N-15 applied in the solution treatment being more acces
sible for microbial consumption. Nevertheless, application of N-15 as an NH
4+ solution, or injection of (NH3)-N-15 gas into soil, resulted in estimate
s of a similar magnitude for gross N mineralisation rates and identified th
e same differences between soil type and land use. (C) 1999 Elsevier Scienc
e Ltd, All rights reserved.