The determination of potential ammonification in soil by arginine method
Author(s) -
Mirjana Kresović,
V. Ličina
Publication year - 2002
Publication title -
journal of agricultural sciences belgrade
Language(s) - English
Resource type - Journals
eISSN - 2406-0968
pISSN - 1450-8109
DOI - 10.2298/jas0202129k
Subject(s) - vertisol , arginine , chemistry , nitrogen , nitrogen cycle , soil ph , fertilizer , cycling , environmental chemistry , soil type , zoology , agronomy , soil science , biochemistry , soil water , amino acid , environmental science , biology , organic chemistry , forestry , geography
In this paper investigations were carried out on two soil types (vertisol and brown forest soil) with different doses of applied N-fertilizer: diameter, N60 N90; N120 and N250. The potential ammonification in soil was obtained by arginine method. The following properties of soil were determined: pH value organic C, available NH4-N and mobile-Al. The pH value in vertisol was 3.75-4.07; mobile-Al was 0.67-4.90 mg/100g; % organic C 1.38-1.46 and the content of available nitrogen was 4.4-11.2 ppm. The amount of released NH4-N by arginine ammonification in this soil type was very low [(-0.12)-0.27mg/g-1h-1]. Correlation coefficients between released NH4-N from arginine and soil pH were (-0.96*), mobile Al - (-0.99**), applied fertilizer doses - (-0.95*). In brown forest soil the amount of released NH4-N by arginine ammonification was greater than in vertisol, ranging from 3.16 to 7.11mg/g-1h-1. Correlation coefficients between soil properties and released NH4-N from arginine were not statistically significant
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