Abstract
Ammonium sulphate applied continuously for six years steadily decreased the soil pH, the lowest pH occurring in the 0–15cm depth. At 80 kg N/ha, organic matter was significantly decreased while NO3‐N increased, with the reverse occurring at the 120 kg/ha N treatment. Extractable Ca decreased sharply, particularly in the surface soil with increasing N application. Topsoil (0–15cm) cation exchange capacity (CEC) was unaffected by N treatments, whereas in the lower soil depths CEC was significantly lower at the 80 and 120 kg/ha N treatments. Nitrogen treatments steadily decreased %BS in all soil depths.
Soil extractable Fe and Mn increased with increasing rates of N, while Cu and Zn were unaffected. Surface soil pH (0–15cm) established a significantly positive relationship with pH, P, Ca, and %BS in lower soil depths and a negative relationship with Mg and CEC. The use of nitrogeneous fertilizers in tropical soils should be preceded by an efficient soil testing programme.
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