Comparison of two kinetics models for estimating N mineralization affected by different quality of organic matter in Typic Hapludults

Abstract

N availability in the soil is determined by the rate of mineralization. N mineralization can be estimated using several models. Aim of research is to compare of two kinetics models for estimating N mineralization affected by different inputs of organic matter and soil fertility in Typic Hapludults. Research used completely randomized design with two factors. The first factor was land use : (1). Soil from land cultivated by cassava crops for less than 10 years, and (2). Soil from land cultivated by cassava crops for more than 30 years. The second factor was type of organic matter: (1). Groundnut biomass, (2). Maize biomass, (3). Groundnut-maize biomass, with ratio of 1:1, (4). Groundnut -maize biomass, with ratio of 2:1, (5). Groundnut -maize biomass, with ratio of 1:2, and (6). Without organic matter. The result shows that based on the value of R 2 , first-order kinetics equation is more suitable to decribe N mineralization than double-pool kinetics equation because R-square value higher than double-pool kinetics and is positively correlated with N mineralization parameters (N0, k and N0.k).

Nitrogen release kinetics of organic nutrient sources in two benchmark soils of Indo-Gangetic plains

“…The rate of N mineralization in soil is controlled by a number of soil and environmental factors in a complex manner (Benbi and Richter, 2002). The important factors that dictate N mineralization kinetics include organic matter content, microbial biomass, soil texture, temperature and mois-ture (Fritschi et al, 2005;Wijanarko and Purwanto, 2016). Despite the complex controls on this process, and the involvement of a vast array of microbes from different taxonomic groups, the rate of mineralization is largely dependent on the quantity and quality (composition) of organic matter and the influence of environmental factors on biological activity (Gómez-Muñoz et al, 2015).…”