
TY  - JOUR
A1  - Guinto, D. F. 
A1  - Xu, Z. H. 
A1  - Saffigna, P. G. 
A1  - House, A. P. N. 
A1  - Perera, M. C. S. 
T1  - Soil nitrogen mineralisation and organic matter composition revealed by <emph type="7">13</emph>C NMR spectroscopy under repeated prescribed burning in eucalypt forests of south-east Queensland
JF  - Soil Research
JO  - Soil Res.
Y1  - 1998
VL  - 37
IS  - 1
SP  - 123
EP  - 136
KW  - fuel reduction burning, soil C pools, soil N availability.
UR  - https://doi.org/10.1071/S97034 
N2  - The effects of burning on in situ extractable nitrogen (NH+4-N+NO-3-N) and net Nmineralisation following scheduled fuel reduction burns in repeatedly burnt dry and wet sclerophyll forest sites in south-east Queensland were assessed. In addition, soil organic matter composition in the wet sclerophyll site was assessed by 13C NMR spectroscopy. The results showed that at the dry sclerophyll site, extractable N and net N mineralisation for 1 year were largely unaffected by burning, while at the wet sclerophyll site, these parameters decreased. 13C NMR analysis of soil samples from the wet sclerophyll site revealed that there was a significant reduction in the proportion of O-alkyl (alkoxy/carbohydrate) C with increasing burning frequency. Statistically significant effects on the other chemical shift regions were not detected. The ratio of alkyl C to O-alkyl C, a proposed index of organic matter decomposition, increased with increasing burning frequency. A high ratio of alkyl C to O-alkyl C suggests low amounts of carbohydrates relative to waxes and cutins, which could in turn lead to slower mineralisation. The findings are in accord with this hypothesis. There were significant linear relationships between cumulative N mineralisation for 1 year and the proportions of alkyl C and O-alkyl C, and the ratio of alkyl C/O-alkyl C. Thus, in addition to reductions in substrate quantity (low organic C and total N for burnt soils), there was also an alteration of substrate quality as revealed by 13C NMR spectroscopy which is reflected in low N mineralisation. 
ER  -

