“…These reports have documented large water capacity of heavy-textured alluvial soils, particularly in the Wisła delta, while susceptibility for drought (after drainage) of coarse-textured soils in the valleys of central and southern Poland. Fine-textured topsoil horizons of alluvial soils have high exchange cation capacity and ability to adsorb macronutrients, as well as support stabilisation of organic matter (Banach-Szott et al, 2018;Brogowski and Okołowicz, 2008;Brogowski and Kwasowski, 2014;Dąbkowska-Naskręt, 1990;Długosz et al, 2018;Kabała et al, 2002;Kalembasa and Becher, 2010;Kobierski and Banach-Szott, 2022;Malinowski, 2008;Malinowski et al, 2004;Niedźwiedzki et al, 2011;Orzechowski et al, 2005;Woźniak, 1998). Strzemski et al (1973) have concluded that the thickness of the fine-textured topsoil (above the sandy subsoil), along with the depth of mean groundwater table, decide about the productivity of arable alluvial soils in Poland.…”