Initial Nitrification Activity (INA) was measured in 68 New Zealand grassland soil sampies (0–75 mm) using a 17‐h laboratory perfusion technique to provide a measure of the nitrifying activity. Considerable variation (< 0.02–5.70 μg N oxidised/g soil/h)was found between soils, yellow‐brown loams having higher INA values than other soil groups. Variation of pH, % total N, % organic C, and C:N ratio explained only 12–44% of the variation of INA. Four characteristic patterns of nitrification were found when soils were perfused for 300 h. Significant populations of ammonium oxidisers(1.6 × 10 4 –2.2 × 10 6 /g soil) and nitrite oxiders (5.4 × 10 4 ‐1.9 × 10 7 /g soil) were found in the top 75 mm of 13 soils, even those oflow INA. Field measurements of nitrification activity in 2 soils of low and medium INA values supported the predicted difference in INA. The mean rate of nitrification under field conditions was 0.68 × 10 ‐2 μg N oxidised/g soil/h in the soil of low INA (Wharekohe silt loam) and 5.3 × 10 ‐2 μg N oxidised/g soil/h the soil of medium INA (Kiripaka silt loam). This difference resulted in an average NH 4 ‐ N: NO 3 ‐ N ratio of 16:1 in the former and 1:1 in the latter soil.
No takes yet. Share an insight, caveat, or question.
Steele et al. (1980) studied this question.