RESIDUE FRACTIONATION AND DECOMPOSITION - THE SIGNIFICANCE OF THE ACTIVE FRACTION

This paper describes an incubation experiment with homogeneously C-14 labeled maize-straw and its insoluble fraction. The role of the solubl e fraction in the decomposition process was assessed, using three inde pendently measured characteristics: (1) fractionation of the maize-str aw, resulting in kinetically different fractions; (2) microbial biomas s C and its C-14 activity determined by a fumigation extraction method , and (3) the C-14 activity of the released CO2-C. The fumigation extr action method was proved to be useful from 9 days after the applicatio n of the maize-straw onwards. The fractionation method yielded a solub le (48%), a (hemi)cellulosic (47%), and a lignin fraction (1%). Nine d ays after addition of either the complete residue or its insoluble fra ction, the microbial biomass C increased from 53 to 337 and 217 mg C k g(-1) dry soil, respectively. Similar values were maintained up to day 40. The large increase in microbial activity was accompanied by a N-i mmobilization of 65 and 29 mg N kg(-1) dry soil for the maize-straw tr eatment and its insoluble fraction, respectively, resulting in biomass C/N values of 5.5 and 5.6. A genuine priming effect (10 and 7% of the total CO2-C production) on the mineralization fo native soil organic C was caused by an increase in decomposition of the native C rather th an by an increase in turnover of the microbial biomass in the soil ame nded with maize straw. The soluble fraction caused a 'priming effect' on the decomposition of the less decomposable cell-wall fraction. Calc ulations by nonlinear regression confirmed this observation.