C and N turnover in structurally intact soils of different texture

The turnover of native and applied C and N in undisturbed soil samples of different texture but similar mineralogical composition, origin and cropping history was evaluated at −10 kPa water potential. Cores of structurally intact soil with 108, 224 and 337 g clay kg(−1) were horizontially sliced and (15)N-labelled sheep faeces was placed between the two halves of the intact core. The cores together with unamended treatments were incubated in the dark at 20 °C and the evolution of CO(2-)C determined continuously for 177 d. Inorganic and microbial biomass N and (15)N were determined periodically. Net nitrification was less in soil amended with faeces compared with unamended soil. When adjusted for the NO(3-)N present in soil before faeces was applied, net nitrification became negative indicating that NO(3-)N had been immobilized or denitrified. The soil most rich in clay nitrified least N and (15)N. The amounts of N retained in the microbial biomass in unamended soils increased with clay content. A maximum of 13% of the faeces (15)N was recovered in the microbial biomass in the amended soils. CO(2-)C evolution increased with clay content in amended and unamended soils. CO(2-)C evolution from the most sandy soil was reduced due to a low content of potentially mineralizable native soil C whereas the rate constant of C mineralization rate peaked in this soil. When the pool of potentially mineralizable native soil C was assumed proportional to volumetric water content, the three soils contained similar proportions of potentially mineralizable native soil C but the rate constant of C mineralization remained highest in the soil with least clay. Thus although a similar availability of water in the three soils was ensured by their identical matric potential, the actual volume of water seemed to determine the proportion of total C that was potentially mineralizable. The proportion of mineralizable C in the faeces was similar in the three soils (70% of total C), again with a higher rate constant of C mineralization in the soil with least clay. It is hypothesized that the pool of potentially mineralizable C and C rate constants fluctuate with the soil water content.