Soil properties and the ability of the urease inhibitor N-(n-BUTYL) thiophosphoric triamide (nBTPT) to reduce ammonia volatilization from surface-applied urea

尿素氨挥发 挥发 尿素酶 化学 尿素 土壤水分 环境化学 修正案 肥料 动物科学 有机质 土壤pH值 土壤科学 环境科学 生物化学 有机化学 政治学 法学 生物
作者
Chris Watson,Helen R. Miller,Polska Akademia Nauk Poland,David C. Kilpatrick,M. Allen,Michelle D. Garrett,C. B. Christianson
出处
期刊:Soil Biology & Biochemistry [Elsevier BV]
卷期号:26 (9): 1165-1171 被引量:158
标识
DOI:10.1016/0038-0717(94)90139-2
摘要

A laboratory study was made to evaluate the ability of the urease inhibitor N-(n-butyl) thiophosphoric triamide (nBTPT) to reduce NH3 volatilization from surface-applied urea. Urea was amended with 0.0, 0.01, 0.058 or 0.28% nBTPT (w/w) and was applied, at a rate equivalent to 100kgN ha−1, to the surface of 16 grassland soils, selected to show a wide range of different chemical and physical characteristics. Daily NH3 loss was measured for 9 days, after fertilizer application, using ventilated enclosures at 13°C. The influence of soil properties on the effectiveness of nBTPT as a urea amendment was investigated using a modelling approach followed by stepwise multiple regression analysis. NH3 volatilization from unamended urea ranged from 5.8 to 38.9% of the N applied and was greatest from a soil with a high pH and low titratable acidity. The % inhibition of NH3 loss by nBTPT was highly dependent on soil type, being effective on some soils even at the 0.01% nBTPT level. The % inhibition at the 0.28% level ranged from 99.4 to 54.4%. Modelling the relationship between total NH3 loss and inhibitor concentration showed that the % nBTPT required to achieve a given % decrease in NH3 volatilization was constant for all soils. For example, 0.092% nBTPT was predicted to lower total NH3 loss by 90% from any given soil. The response to increasing inhibitor concentration in lowering NH3 volatilization was greatest in a soil with low organic matter content and high pH. Stepwise multiple regression analysis showed that 4 soil properties (titratable acidity, pH-H2O, urease activity and cation-exchange capacity) contributed significantly to explaining 90.6% of the variation in total NH3 loss. In all soils the % urea remaining at the end of the incubation was 2.6, 4.6, 10.9 and 25.5% for 0.00, 0.01, 0.058 and 0.28% nBTPT, respectively. The persistence of urea treated with nBTPT was particularly marked in soils with a high pH and could have physiological implications for plants. It is particularly interesting that nBTPT was most effective in soils which showed high NH3 volatilization from unamended urea.
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