
%0 Journal Article
%A Robertson, FA 
%A Myers, RJK 
%A Saffigna, PG 
%T Carbon and nitrogen mineralization in cultivated and grassland soils in subtropical Queensland
%J Soil Research
%D 1993/10/01
%V 31
%N 5
%P 611-619
%K Microbial Biomass;Respiration;Immobilization;C and N Ratios;
%R https://doi.org/10.1071/SR9930611
%U https://www.publish.csiro.au/paper/SR9930611 
%X Availability of N in the clay soils of the brigalow region of Queensland declines rapidly under sown pasture, but under continuous cultivation and cropping, it remains high enough to supply the needs of cereal crops for at least 20 years. The aim of this work was to determine whether the low availability of N under pasture was due to low microbial activity or to rapid re-immobilization of mineralized N. Microbial biomass C and N (0-28 cm) were 420 and 68 µg g-1 respectively in pasture soil but only 214 and 41 µg g-1 respectively in cultivated soil. Pasture soils respired more CO2 (Cresp) and mineralized less N (Nmin) than cultivated soils (219 and 93 µg C g-1 and 3.1 and 5.9 µg N g-1 respectively) during 10-day incubations over 2 years. Increased Crop under pasture was due to an increase in the amount rather than the specific activity of the microbial biomass. The smaller Nmin in grassland soils was due to more rapid immobilization rather than reduced gross mineralization of N, as the ratio Cresp : Nmin was larger and the ratio Nmin :biomass N was smaller in the grassland than in the cultivated soil. On prolonged incubation. with progressive loss of CO2 through respiration, Nmin increased and N immobilization decreased in the grassland soils. Prolonged incubation of the cultivated soils reduced Nmin because of C limitation. The above patterns of C and N mineralization in the grassland and cultivated soils helped to explain the differences in N availability in the two systems. 
