Waterlogging refers to soil saturation from high water tables, preventing air and oxygen flow needed by crops. It is caused by over-irrigation, inadequate drainage, flooding, and high water tables during monsoons. Waterlogging can be permanent, periodic, or temporary, and often leads to soil salinization in irrigated areas due to prevented leaching of salts. Major waterlogged areas in Bangladesh include wetlands, floodplains, coastal areas, and areas with artificial irrigation. Waterlogging hampers soil microbial activity, reduces nutrient availability, increases soil pH, and favors weed growth. Reducing measures include dams, embankments, and bridges/culverts to restrict water flow.