Because of measurement difficulties, only a few studies on natural N-1
5 abundance (delta(15)N) of inorganic N in forest soil have been pursu
ed despite its importance for interpretations of plant delta(15)N sign
atures. To investigate stable N isotope ratios in inorganic N, the del
ta(15)N values and concentrations of total N, NH4+-N, and NO3--N of fo
rest mineral soils in four profiles were measured along a slope (altit
ude of 765-870 m) in a coniferous (Japanese red cedar, Cryptomeria jap
onica D. Don) forest in Japan. Generally, the delta(15)N values of tot
al N, NH4+-N, and NO3--N increased with increasing soil depth. The val
ues of delta(15)N ranged from 1.0 to 6.8 parts per thousand, 2.5 to 15
.6 parts per thousand, and -14.8 to 5.6 parts per thousand for total N
, NH4+-N, and NO3--N, respectively. Additionally, the delta(15)N value
s were different between NH4+-N and NO3--N for each soil depth. Thus,
it was concluded that the assumptions about inorganic N used in interp
retation of plant delta(15)N values were valid. Moreover, on upper slo
pe sites where soil inorganic N was predominantly NH4+-N, the order of
delta(15)N was generally total N > NH4+-N > NO3--N for each depth, wh
ereas the order of delta(15)N was NH4+-N > total N > NO3--N on lower s
lope sites where NH4+-N was less dominant as soil inorganic N and rela
tively high net nitrification rates were measured. Our results suggest
ed that nitrification plays an important role in regulating delta(15)N
in forest-soil N.