2008
DOI: 10.1071/sr07088
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Long-term acidification of a Brazilian Acrisol as affected by no till cropping systems and nitrogen fertiliser

Abstract: Cropping systems and N fertilisation affect soil acidification mainly due to the removal of alkaline plant material from the field and nitrate leaching. The study evaluated the acidification of a subtropical soil under no till cropping systems with different C and N addition rates for 19 years. The contributions of leguminous and non-leguminous crops (fallow/maize, black oat/maize, black oat + vetch/maize, black oat + vetch/maize + cowpea, lablab + maize, pigeon pea + maize, and digitaria) and mineral N fertil… Show more

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Cited by 40 publications
(26 citation statements)
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“…The soil management systems did not affect the pH or exchangeable Al content. The increased soil acidity, also demonstrated by the low base and high Al saturation, was mainly due to the extraction of bases by harvest removal of grains during this long period (26 years) without liming, while nitrate leaching may also have contributed slightly to soil acidification (Vieira et al, 2008).…”
Section: Chemical Properties Of the Soil Solid Phasementioning
confidence: 99%
“…The soil management systems did not affect the pH or exchangeable Al content. The increased soil acidity, also demonstrated by the low base and high Al saturation, was mainly due to the extraction of bases by harvest removal of grains during this long period (26 years) without liming, while nitrate leaching may also have contributed slightly to soil acidification (Vieira et al, 2008).…”
Section: Chemical Properties Of the Soil Solid Phasementioning
confidence: 99%
“…The long-term effusion of nitrogen fertilizer affects its surrounding environment, including the river. In many studies, overuse of nitrogen fertilizer is a cause of soil acidifi cation [27][28][29][30].…”
Section: Long-term Spatial and Longitudinal Analysismentioning
confidence: 99%
“…Thus, N volatilization is favored by high urease activity in the surface layer of no-tilled soils (Barreto & Westerman, 1989) and the presence of straw on the soil surface, which limits contact between the soil and the fertilizer (Menguel, 1996). However, high soil moisture, organic matter content and CEC levels in the surface layer of NT soils are important factors increasing the buffer capacity of soil pH variation (Vieira et al, 2008) with possible effects decreasing NH 3 volatilization (Ferguson et al, 1984).…”
Section: Introductionmentioning
confidence: 99%