Limitations of a calculated N mineralization potential in studies of the N mineralization process

Soil is often incubated under controlled conditions to assess its capacity to mineralize nitrogen and to define the N mineralization potential (N_o) by fitting a negative exponential curve to N mineralization data. The specificity of N_o for a given soil and its relevance in N mineralization studies was examined as part of an overall study of the N mineralization process. Soil mixed with an equal amount of sand was aerobically incubated at 35 °C and leached at specific time intervals. Upon leaching, ammonium and nitrate were measured in the extract.It was found that N mineralization data did not always follow first-order kinetics making it difficult to calculate N_o. The computed N_o value was influenced by the shape of the curve, the duration of the incubation experiment and was reciprocally related to the N mineralization constant (k_exp). N_o did not always give an adequate indication of the amount of N mineralized and was not soil specific as the time of sampling largely affected its size. The usefulness of N_o in the simulation of the N mineralization process with a k_exp value valid for all soils was limited and a k_exp value specific for each soil was required. A value combining the soil specific N_o and k_exp values and reflecting the amount of N mineralized over one year was proposed as a suitable alternative to the use of N_o in comparative studies of the N mineralization process. It was concluded that a calculated N_o could not be used in studies comparing the N mineralization of different soils. In addition, the simulation of the N mineralization required the use of the soil specific k_exp and could not be carried out with a k_exp valid for all soils.