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Waterlogging and Soil Salinization: Drainage Engineering Solutions in Command Areas

 ​Intensive surface irrigation without adequate drainage often causes the water table to rise near the ground surface, resulting in waterlogging. When capillary action draws this shallow, saline groundwater upward, it evaporates and leaves harmful salt crusts that destroy agricultural productivity. Subsurface drainage design relies on steady-state and transient groundwater flow equations, such as Hooghoudt’s Equation, to determine the optimal spacing (S) between parallel tile drains:

S^2 = (4 * K * (h_2^2 - h_1^2)) / q

​Where K is hydraulic conductivity, h values represent water table heights above the drain level, and q is the drainage flux.

​Large tracts of fertile land in canal-irrigated zones across Punjab, Haryana, and parts of western Uttar Pradesh have suffered from secondary soil salinization due to impeded natural drainage.

​Contemporary agricultural water management in India deploys subsurface horizontal drainage systems using corrugated PVC perforated pipes wrapped in geotextile filters. Combined with the conjunctive use of saline drainage water and fresh canal water, these engineered drainage networks successfully lower the water table, leach accumulated salts from the root zone, and restore degraded soils back to high productivity

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