The aim of the study was to determine the levels of soil mineral elements in groundwater and the volume of that water draining from fields under different fertilization systems. In 2011, drainage systems were installed to collect groundwater from selected plots of long-term fertilization experiments located at the Experimental Station of the Faculty of Agriculture and Biology of Warsaw University of Life Sciences SGGW in Skierniewice. The study involved limed (CaNPK) and unlimed (NPK) plots of two fertilization experiments, one with mineral and the other with mineral-organic fertilization. During the study, the volume of the drainage water was measured and samples of the water were analyzed for Ca, Mg, K, Na, Zn, Fe, Mn, Cu and Al. The levels of mineral elements in the water flowing out of the soil profile were found to vary significantly and were dependent on the volume of the outflow, the system of fertilization and soil acidification. The load of elements in the outflow water can be put in the following relative order: Ca>Mg>K>Na>Al>Zn>Fe>Mn>Cu. Application of manure in the dose of fertilizers increased the leaching of magnesium and potassium, as well as zinc, iron and manganese. However, organic fertilization did not increase the leaching of calcium from the soil, and reduced the activity and mobility of aluminium in the soil. Depending on the fertilization system and soil acidification status, the amounts of elements washed out with 1 m 3 of water flowing out of ha a sandy soil were: 186434 g Ca, 12.633 g Mg, 13.280 g K, 9.323.4 g Na, 29.5251 mg Al, 53184 mg Zn, 24.5319 mg Fe, and 2076.5 mg Mn.