The low capacity of acid sandy soils to bind P is one reason for the leaching and runoff of P from these soils. Various soil amendments have been used to reduce P leaching. This study was conducted to show the effect of CaCO 3 , dolomite, gypsum, and CaCl 2 on P retention by the Ap horizon of a Spodosol. Phosphorus sorption was studied in a batch experiment at an initial P concentration range of 0 to 10 mg L ؊1 . The amendment rate used was 0.05 mmol of either Ca or Ca ؉ Mg (and also 0.1 mmol in the case of CaCO 3 and gypsum) per g of soil. The influence on P retention of time after soil amendment (1 h to 1 week) was assessed. P adsorption was described by Langmuir and Freundlich equations. All amendments, except for CaCl 2 , increased soil pH and P retention by soil. CaCO 3 was more effective then dolomite, the carbonates (CaCO 3 and dolomite) were more effective in their interaction with the soil, and gypsum increased P retention by itself, its effect was weakened upon interaction with soil. Sorption of P in soil amended with gypsum was faster than sorption in soil amended with CaCO 3 . The effect of the amendments under study was mainly to provide Ca ions, which must be accompanied by an increase in pH to increase P retention. (Soil Science 2003;Volume 168:699-706)