“…Most soil reactions that follow CL addition, such as the increase in soil pH and decrease in exchangeable Al, are normally restricted to no more than a few centimetres below the liming depth, indicating that the downward movement of Ca from CL through the soil is extremely slow (Farina, Channon, & Thibaud, ). Many reports support that opinion, finding that the vertical distance that Ca moves depends mainly on the reactivity of lime, which is generally limited by its dissolution and distribution in the soil, which in turn depend on time, application rate, form (particle size) and application method, as well as on cultivation system, soil characteristics, climate conditions and the addition of acid fertilizers (Caires, Alleoni, Cambri, & Barth, ; Cifu, Xiaonan, Zhihong, Zhengyi, & Wanzhu, ; Edwards, Duncan, Harris, & Burgess, ; Elephant, Miles, & Mthimkhulu, ; Ernani, Ribeiro, & Bayer, ; Farina et al., ; Hoyt & Drought, ; Kisinyo et al., ; Liu & Hue, ; Miyazawa, Pavan, & Franchini, ; Ponette, Dufey, & Weissen, ; Sumner, ; Vázquez, Terminiello, Millán, Daverede, & Baridón, ; Vizcayno, Garcia‐Gonzalez, Fernandez‐Marcote, & Santano, ; Whitten, Wong, & Rate, ).…”