Strongly acidic soils(pH < 5.0) are detrimental to tea(Camellia sinensis) production and quality.Little information exists on the ability of surface amendments to ameliorate subsoil acidity in the tea garden soils.A 120-d glasshouse column leaching experiment was conducted using commonly available soil ameliorants.Alkaline slag(AS) and organic residues,pig manure(PM) and rapeseed cake(RC) differing in ash alkalinity and C/N ratio were incorporated alone and in combination into the surface(0—15 cm) of soil columns(10 cm internal diameter × 50 cm long) packed with soil from the acidic soil layer(15-30 cm) of an Ultisol(initial pH =4.4).During the 120-d experiment,the soil columns were watered(about 127 mm over 9 applications) according to the long-term mean annual rainfall(1143 mm) and the leachates were collected and analyzed.At the end of the experiment,soil columns were partitioned into various depths and the chemical properties of soil were measured.The PM with a higher C/N ratio increased subsoil pH,whereas the RC with a lower C/N ratio decreased subsoil pH.However,combined amendments had a greater ability to reduce subsoil acidity than either of the amendments alone.The increases in pH of the subsoil were mainly ascribed to decreased base cation concentrations and the decomposition of organic anions present in dissolved organic carbon(DOC) and immobilization of nitrate that had been leached down from the amended layer.A significant(P < 0.05) correlation between alkalinity production(reduced exchangeable acidity — N-cycle alkalinity) and alkalinity balance(net alkalinity production — N-cycle alkalinity) was observed at the end of the experiment.Additionally,combined amendments significantly increased(P < 0.05) subsoil cation concentrations and decreased subsoil Al saturation(P < 0.05).Combined applications of AS with organic amendments to surface soils are effective in reducing subsoil acidity in high-rainfall areas.Further investigations under field conditions and over longer timeframes are needed to fully understand their practical effectiveness in ameliorating acidity of deeper soil layers under naturally occurring leaching regimes. Strongly acidic soils (pH <5.0) are detrimental to tea (Camellia sinensis) production and quality. Little information exists on the ability of surface amendments to ameliorate subsoil acidity in the tea garden soils. A 120-d glasshouse column leaching experiment was conducted using all available soil ameliorants. Alkaline slag (AS) and organic residues, pig manure (PM) and rapeseed cake (RC) differing in ash alkalinity and C / N ratio were incorporated alone and in combination into the surface (0-15 cm) of The columns were watered (about 10 cm internal diameter × 50 cm long) packed with soil from the acidic soil layer (15-30 cm) of an Ultisol (initial pH = 4.4) 127 mm over 9 applications) according to the long-term mean annual rainfall (1143 mm) and the leachates were collected and analyzed. At the end of the experiment, soil columns were partitioned into various depths and the chemical properties of soil were measured. The PM with a higher C / N ratio increased subsoil pH, compared the RC with a lower C / N ratio decreased subsoil pH. Even, combined amendments had a greater ability to reduce subsoil acidity than either of the amendments alone. these increases in pH of the subsoil were mainly ascribed to decreased base cation concentrations and the decomposition of organic anions present in dissolved organic carbon (DOC) and immobilization of nitrate that had been leached down from the amended layer. A significant (P <0.05) correlation between alkalinity production (reduced exchangeable acidity - N-cycle alkalinity ), and alkalinity balance (net alkalinity production - N-cycle alkalinity) was observed at the end of the experiment. Additionally, combined amendments significantly increased (P <0.05) subsoil cation concentrations and decreased subsoil Al saturation of AS with organic amendments to surface soils are effective in reducing subsoil acidity in high-rainfall areas. Future investigations under field condi tions and over longer timeframes are needed to fully understand their practical effectiveness in ameliorating acidity of deeper soil layers under naturally occurring leaching regimes.