European farmland has been abandoned at an unprecedented rate over the last few decades, resulting in an increase of the area of fallows and a decrease in plant diversity in meadows. This work was aimed at determining whether differences in the persistence and plant diversity of the two ecosystem types, similar in plant biomass and geographical location, resulted in changes in soil physicochemical properties. Soil physicochemical properties and floristic composition were studied in six fallows at the initial stage of secondary succession and six fresh meadows with high plant diversity. Fallow soils had several-fold higher content of available phosphorus, potassium and nitrates. Meadow soils had a slightly higher C:N ratio and water-holding capacity (WHC), what suggest more humus in meadow soil. The main differences in soil properties between meadows and fallows were after-effects of agricultural management, most probably previous fertilization. The difference in the C:N ratio and WHC can be attributed to ecosystem ages. Abandoned farmlands had relatively good nutrient supply but low species diversity. Meadows, though depleted in available nutrients, showed high floristic richness. The legumes, which were more abundant in meadows, might have supplemented this ecosystem with the limiting N.