Effects of N Fertilization on the Distribution of Organic and Inorganic N in Soils

G.A. Breitenbeck, E.P. Millhollon, and D.H. Boquet


 
ABSTRACT

The distribution of soil nitrogen (N) in profiles of plots receiving annual plant applications of 0, 45 or 68 kg anhydrous ammonia N ha-1 prior to planting cotton in experiments established in 1955 was studied by determining the amounts of N in various organic and inorganic fractions of soil cores collected May 1988 in 15 cm increments to a depth of 150 cm. The data obtained indicated that N cycling in Norwood soil cropped to cotton is highly efficient, and that fertilization led to a greater portion of total soil N in the profile residing as organic N near the soil surface. The amounts of total N in the surface 45 cm were 34-68% greater in fertilized plots than in unfertilized plots, whereas the amounts of organic and clay-fixed N at depths between 60 and 105 cm were greater in unfertilized plots. These findings suggest that mineralization of organic N was the principal source of plant-available N in unfertilized plots, and that clay-fixed N in surface and subsoils is involved in N nutrition of cotton. Regression analyses relating seedcotton yield to the distribution of soil N showed that a model including the rate of N applied and the amounts of organic N and mineral N from the surface 15 cm only provided the greatest predictive value (r2=0.97). Although these experiments indicate that nitrate concentrations and indices of N availability are less effective than measures of organic or total N in predicting the`response of cotton to fertilizer N, additional experiments on a Commerce silt loam showed that substantial amounts of residual nitrate are available when excessive amounts of fertilizer N are applied the preceding season.



Reprinted from Proceedings: 1989 Beltwide Cotton Research Conferences pp. 485 - 488
©National Cotton Council, Memphis TN

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Document last modified Sunday, Dec 6 1998