In three dairy grasslands on peat, minerals were added to manipulate the soil Ca:Mg ratio with or without effect on pH. The responses of soil properties and grass N yield were measured. CaCO 3 application led to higher soil Ca:Mg ratio and pH KCl compared to the untreated control, decreased N total and C total , and increased P availability. Grass N yield increased in the first year by only 6% of the reduction in soil N total , but not in the second year. A higher pH increased SOM decomposition, especially in soils with high P availability. MgCO 3 reduced the Ca: Mg ratio, had little influence on soil parameters and no effect on grass N yield. In contrast, CaSO 4 and MgSO 4 did not influence pH KCl but reduced grass N yield in most cases. Results suggest stabilisation of organic matter by Ca binding in treatments with added Ca. We conclude that grass N yield was not linked with changes in Ca:Mg ratio but with soil pH. The pH effects on SOM decomposition depended on P availability and Ca binding. Hence, to avoid potentially large soil losses of C and N, the current agricultural advice on pH management in peat grasslands should be better adapted to local edaphic characteristics.