posted on 2023-05-19, 05:44authored byPulito, AP, Goncalves, JLDM, Smethurst, PJ, Arthur, JC, Alvares, CA, Rocha, JHT, Hubner, A, de Morales, LF, Miranda, AC, Kamogawa, MY, Gava, JL, Chaves, R, Silva, CR
<em>Eucalyptus</em> plantations have seldom responded to N fertilization in tropical and subtropical regions of Brazil. This implies that rates of N mineralization have been adequate to supply tree needs. However, subsequent crop rotations with low N fertilization may result in declining concentrations of organic and potentially mineralizable N (N<sub>0</sub>), and consequent loss of wood productivity. This study investigated (a)<em> in situ </em>N mineralization and N<sub>0</sub> in soils of eucalypt plantations in São Paulo state, Brazil; (b) tree growth responses to N fertilizer applied 6-18 months after planting; and (c) the relationships between N<sub>0, </sub>other soil attributes and tree growth. We established eleven N fertilizer trials (maximum 240 kg ha<sup>−1</sup> of N) in <em>E. grandis</em> and <em>E. grandis</em> x <em>urophylla</em> plantations. The soil types at most sites were Oxisols and Quartzipsamments, with a range of organic matter (18 to 55 g kg<sup>−1</sup>) and clay contents (8% to 67%) in the 0-20 cm layer. Concentrations of N<sub>0</sub> were measured using anaerobic incubation on soil samples collected every three months (different seasons). The samples collected in spring and summer had N<sub>0</sub> 140-400 kg ha<sup>−1 </sup>(10%–19% total soil N), which were best correlated with soil texture and organic matter content. Rates of<em> in situ</em> net N mineralization (0-20 cm) ranged from 100 to 200 kg ha<sup>−1</sup> year<sup>−1</sup> and were not correlated with clay, total N, or N<sub>0</sub>. These high N mineralization rates resulted in a low response to N fertilizer application during the early ages of stand growth, which were highest on sandy soils. At the end of the crop rotation, the response to N fertilizer was negligible and non-significant at all sites.