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Abstract The effect of soil pH on rates of ammonification and nitrification was studied. Soil samples which ranged in pH from 4.7 to 6.6 from an established lime and N fertility experiment were used. Soil pH values in the lime plots have been relatively constant for several years. Soil pH did not affect rates of ammonification appreciably; however it had a significant effect on nitrification rates. Length of the delay period ( t ′) was increased and rate of NO 3 ‐ accumulation (Km) decreased with a decrease in soil pH. Previous field N treatments increased the length of t ′ at low pH and decreased t ′ and Km at high pH. Nitrification rates and production of NO 3 ‐ were similar for soil pH values of 5.3, 6.0, 6.3, and 6.6 with a different pattern at pH 4.7.
Dancer et al. (Mon,) studied this question.