Effects of Ca:Mg ratio and pH on soil chemical, physical and microbiological properties and grass N yield in drained peat soil

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. CaCO3 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. MgCO3 reduced the Ca:Mg ratio, had little influence on soil parameters and no effect on grass N yield. In contrast, CaSO4 and MgSO4 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.

Automated summary

This study manipulated the soil Ca:Mg ratio by adding minerals in three dairy grasslands on peat. The study found that CaCO3 application increased soil Ca:Mg ratio and pH, decreased N-total and C-total, and increased P availability. MgCO3 had little influence on soil parameters and grass N yield. CaSO4 and MgSO4 reduced grass N yield in most cases. Results suggest that Ca binding can stabilize organic matter, and grass N yield is influenced by soil pH.