Waterlogging refers to a condition where soil pores become saturated, reducing aeration and restricting root growth. It is a major problem in canal command areas and poorly drained regions.

Reasons for waterlogging:

Excessive canal irrigation: Continuous use without drainage raises water table.

Seepage losses: From unlined canals and field channels.

Poor natural drainage: Clayey soils and flat topography restrict percolation.

High rainfall: Inadequate runoff disposal causes accumulation.

Over-irrigation with tubewells: Indiscriminate pumping raises soil moisture beyond capacity.

Obstruction of natural flow: Roads, embankments, and bunds impede water movement.

Management strategies:

Surface drainage: Construction of open drains, ditches, and field channels for quick removal of excess water.

Subsurface drainage: Installation of tile or pipe drains at depth to lower water table.

Bio-drainage: Planting trees like Eucalyptus and Poplar with high water consumption.

Irrigation scheduling: Adopting need-based, controlled irrigation reduces excess application.

Canal lining: Prevents seepage and reduces recharge to groundwater.

Rainwater harvesting and recycling: Captures excess water for later use.

Conjunctive water use: Balances groundwater withdrawal with surface water application.

By integrating engineering, biological, and management approaches, waterlogging can be mitigated sustainably.