“…However, organic acid anions from the soluble fraction of plant residues improve the chemical conditions of acidic soils in the relatively short term (Tang et al, 1999;Naramabuye and Haynes, 2006), while the decomposition of plant residues causes soil acidification in the long term (Caires et al, 2005(Caires et al, , 2008b. Since at least a fraction of the Ca-fulvate complex is very stable and release of Ca 2+ occurs very slowly while the complex is transported downwards into the soil profile (van der Watt et al, 1991), it is possible that the complex Ca-fulvate encourages the transport of Ca 2+ into the subsoil and contributes to alleviating the effects of acidity in deeper layers under no-till systems.…”