To assess the extent to which moist color value of forest mineral soil
s supports their differentiation according to concentrations of minera
lizable and total N, 239 samples of 0-30-cm mineral-soil layers were e
xamined for the relationship between nitrogen measures and selected ca
tegorical climatic and soil variables. The best regression models, usi
ng soil color value (SCV), climate, soil moisture and soil texture as
categorical variables, explained nearly 70% of the variation in both m
ineralizable and total N, with climate accounting for most of the vari
ation. The results provided support for the present usage of SCV in es
timating mineralizable and total N in forest soils but suggested impro
vements for the development of a more effective estimation procedure.