Subsurface Drainage & Spacing the Buried Drains

Subsurface drainage uses buried perforated pipes (tile drains) laid below the root zone to carry away excess water. It lowers a high water table so the root zone stays aerated, and in saline areas it flushes salts down and out of the soil. It is the standard way to reclaim waterlogged and saline fields and keep them productive.

This tool uses the Hooghoudt steady-state equation, which balances the water flowing into the drains against the drainage coefficient. The spacing depends on soil permeability (K), the drainage coefficient (the mm/day you need to remove), the allowable head of water above the drains midway between them, and the depth to the impermeable barrier below the drains.

The drainage coefficient is the depth of water, in mm per day, that the system must remove to keep the water table low enough for the crop. Humid regions and sensitive crops need a higher coefficient; arid leaching needs a value matched to the salt load. A larger coefficient drains faster but forces closer, more expensive spacing.

Hydraulic conductivity K is how fast water moves through the soil, in metres per day. Sands and well-structured loams have a high K and water reaches the drains easily, allowing wide spacing. Clays have a low K, so water moves slowly and the drains must be placed closer together to remove the same amount of water.

The Hooghoudt equation accounts for water flowing both above and below the drain level toward the drains. A deeper impermeable layer leaves a thicker layer of conducting soil beneath the drains, which carries more flow and lets you use wider spacing. A shallow barrier restricts that flow and pulls the spacing in.

It is how high the water table is allowed to rise midway between two drains, measured above the drain level, during the design drainage. A smaller allowable head keeps the root zone drier but demands closer drains; the crop's tolerance to a high water table sets this value.

Yes. Closer spacing means more drain pipe, more trenching and more outlets per hectare, so the cost rises sharply. The design balances faster, more reliable drainage against installation cost — the tool reports the drain length per hectare so you can see the material implication of a given spacing.

Drain depth is usually 0.9–1.8 m, deep enough to keep the water table below the root zone midway between drains but above the impermeable barrier. Deeper drains can be spaced wider for the same protection, but trenching cost and outlet levels limit how deep you can practically go.

Yes. Subsurface drains are the engine of salt reclamation: applied leaching water dissolves salts in the root zone and the drains carry that saline water away. Without working drainage, leaching just raises the water table and salts come back. Check the Soil Salinity (EC) tool to see how much leaching your field needs.

The Hooghoudt result is an excellent planning estimate, but a final design should use field-measured K, observed barrier depth and local crop and drainage-coefficient standards. Treat the spacing here as a starting point to size the system and compare options, then confirm with a drainage engineer for installation.