Linked from

The 17 pages that link to Waterlogging, each with the reason it gives.

• IrrigationRelated: Poor drainage can leave irrigated fields saturated and impair crop growth.

• Soil compactionRelated: Slow drainage through compacted soil can prolong waterlogging after rainfall.

• Water tableRelated: A rising water table can bring saturation into the root zone.

• TundraRelated: Impermeable frozen subsoil traps meltwater near the tundra surface.

• SalinizationRelated: A shallow water table can bring dissolved salts upward as water evaporates.

• Drought stressCompared with: It is an opposite soil-water extreme, though both conditions can impair plant function.

• PneumatophoreRelated: Waterlogging creates the low-oxygen conditions to which pneumatophores are adapted.

• Soil aerationCompared with: Waterlogging is a common cause of inadequate soil aeration.

• Soil waterCompared with: Excess soil water can impair roots by displacing air from pore spaces.

• Oasis agricultureRelated: Over-irrigation or poor drainage can waterlog oasis fields.

• MoorlandRelated: Persistent waterlogging slows plant decay and helps peat accumulate on wet moors.

• HetaoRelated: Heavy irrigation can raise water tables and damage Hetao farmland.

• Ipomoea aquaticaRelated: Unlike many crops, water spinach tolerates saturated soils and can grow in shallow water.

• North Jiangsu Main Irrigation CanalRelated: Drainage through the canal helps address waterlogged farmland in low-lying areas.

• Raised fieldRelated: Elevated plots can keep roots above saturated ground.

• Sirhind CanalRelated: Poor drainage in irrigated areas can raise water tables and waterlog fields.

• Soil salinity controlRelated: Leaching without sufficient drainage can raise water tables and suffocate crop roots.