Os efeitos da calagem e da gessagem são amplamente conhecidos na literatura, mas a sua magnitude em relação aos efeitos no perfil do solo é dependente do tempo após a aplicação desses insumos. Dessa maneira, o objetivo deste trabalho foi avaliar em longo prazo a aplicação conjunta de gesso e calcário nos atributos químicos de um solo em rotação de culturas, no sistema de plantio direto. O experimento foi conduzido em uma propriedade rural no município de Jaguariaíva, PR, em um Latossolo Vermelho-Amarelo distrófico típico, de textura areia franca, durante os anos de 2002 a 2008. O experimento foi conduzido em blocos ao acaso sob esquema fatorial com 10 tratamentos, sendo cinco doses de gesso agrícola (0; 1,5; 3,0; 6,0; e 12,0 Mg ha-1) e duas doses de calcário (0 e 3,42 Mg ha-1), com três repetições. Foram avaliadas no decorrer dos 72 meses as espécies aveia-preta-comum (2004, 2006 e 2007), milho (2005/2006), trigo (2003) e soja (2003/2004, 2004/2005, 2006/2007 e 2007/2008). Realizaram-se amostragem e análise de solo nos anos de 2005 e 2008 até 100 cm de profundidade e de tecido foliar da soja, na safra de 2007/2008. A aplicação de calcário corrigiu o pH, aumentou a concentração de Ca e Mg e diminuiu o Al, nas camadas superficiais do solo. O gesso proporcionou incremento no pH e nas concentrações de Ca e S em profundidade, lixiviou Mg e não lixiviou o K. A calagem elevou a produtividade do milho, da soja (uma das quatro safras avaliadas) e da aveia- preta. O gesso favoreceu a produtividade do milho e do trigo e a da soja, somente quando houve deficiência hídrica. Quando, no entanto, não houve deficiência hídrica, altas doses de gesso prejudicaram a produtividade de grãos de soja por indução de deficiência de Mg.

The use of nitrification inhibitors (NIs; dicyandiamide - DCD) is an alternative to reduce oxidation of ammonium (NH4+-N) to nitrate (NO3–-N) in the soil, reducing NO3–-N losses from fertilization practices. Based on the hypothesis that DCD reduces conversion of NH4+-N to NO3–-N in tropical soils and inhibits ammonia oxidizing microorganisms (AOM) abundance, soils from the Piracicaba region, São Paulo, with different textures (sand, loam and clay) were incubated with ammonium sulphate (AS) and DCD. Contents of NH4+-N, NO3–-N, soil pH, and AOM abundance were quantified periodically. Ammonium sulphate increased AOM abundance in all soils, but AS+DCD presented AOM abundances similar to the control. During 90 days of incubation, the effectiveness of DCD in reducing NO3–-N production was 1.8, 86.4, and 145.6 mg kg–1, while the effectiveness of DCD in reducing AOM abundance was 1.2, 3.0 and 2.3 × 10–3 g soil–1 for sandy, loamy, and clayey soils, respectively. DCD effectiveness was greater in loamy and clayey soils due to the naturally low nitrification in sandy soils. Application of AS treated with DCD showed potential not only to reduce NO3–-N production in loamy and clayey soils, but also to decrease the soil nitrification rate. Overall, DCD was effective in reducing AOM abundance and conversion of NH4+-N to NO3–-N in loamy and clay soils evaluated here. The increase in clay content directly influences DCD effectiveness in reducing conversion of NH4+-N to NO3–-N.

Anthropic action, such as the soil use and management systems, promote changes in the soil structure. These changes might hamper the development of plants in soil management practices that involve its mobilization, and the negative effects might be increased due to intensive use. The aim of this study was to evaluate the physico-hydrical properties of a Haplohumox in integrated production systems under different soil managements. The soil superficial (0.0-0.10 m) and sub-superficial (0.10-0.20 m) layers were evaluated in the different systems: conventional tillage (CT), minimum tillage (MT), no-tillage (NT) and chiseled no-tillage (CNT), taking into consideration the annual ryegrass cropped for different uses [cover crop (C), grazing (G) and silage (S)] during the winter. Soil bulk density (Db), total porosity (TP), macro (Ma) and microporosity (Mi), water retention curves (SWRC) and water retention due to pore size (r) were determined. The annual ryegrass used as C produced lower Db and Mi and higher TP and Ma in CT, MT and CNT systems. No difference was verified between G and S in any of the management systems or soil layers. The superficial layer SWRC presented similar behavior regarding CT, MT and CNT. Under NT, C resulted in higher water retention. However, G and S provided higher water retention due to the pore size in this system

Extensive research has been performed into the effectiveness of nitrification inhibitors (NIs) in preventing N losses; however, tropical agriculture has been underrepresented in recent meta-analyses. Here, we apply a meta-analytic approach using data from 50 articles to identify the impact of NIs (DMPP, DCD, and DCD + NBPT) on crop yield, N₂O emissions, soil NH₄⁺ and NO₃⁻ concentrations, and NH₃ volatilization in subtropical and tropical regions of Brazil. In addition, the survey includes information about location; climate zone; cultivated crops; soil pH; soil organic carbon; soil texture; experimental method; soil management; irrigation; fertilizer source, rate, and type; and NI type and rate. Overall, the data set showed that NIs increased crop yield and soil NH₄⁺ concentrations by 3 and 60%, respectively, whereas N₂O emissions and soil NO₃⁻ concentrations were reduced by 62 and 31%, respectively. Ammonia volatilization was not changed by NI application. However, the combination of a NI with a urease inhibitor decreased such losses by 39%. The effectiveness of the NIs was highest in irrigated fields, fine-textured soils, and mineral N sources. Moreover, NI performance in Brazil was found to be similar in tropical and subtropical climates, and was also comparable to values previously reported in meta-analyses, including those conducted in temperate climates. Therefore, NI application is indicated to be an efficient strategy to delay nitrification and mitigate N₂O emissions in tropical agroecosystems.