Tile Drain Spacing Calculator

Calculate tile drain spacing using the Hooghoudt equation from soil hydraulic conductivity, drain depth, and drainage coefficient for farm fields.

in/hr
in
in
in/day
in
$/ft
acres
Drain Spacing
13.0 ft
155 inches between parallel drains
Lateral per Acre
3,362 ft/ac
Length of tile needed per acre
Total Lateral Length
268,962 ft
For 80 acres
Total Installation Cost
$806,886.00
$10,086.00/acre at $3.00/ft
Cost per Acre
$10,086.00
Total cost divided by field size
Effective Depth (de)
0.37 ft
Hooghoudt equivalent depth to impermeable layer
K (converted)
1.0000 ft/day
From 0.50 in/hr input
Drainage Coefficient
0.04167 ft/day
From 0.50 in/day input

Spacing vs. Cost by Drainage Coefficient

DC (in/day)Spacing (ft)Lateral/Acre (ft)Total CostRelative Density
0.2518.32,377$570,555.00
0.37515.02,912$698,784.00
0.5 *13.03,362$806,886.00
0.62511.63,759$902,126.00
0.7510.64,118$988,229.00

Hydraulic Conductivity Reference

Soil TypeK (in/hr)K (ft/day)PorosityRelative Permeability
Heavy Clay0.060.120.45
Silty Clay0.150.30.47
Clay Loam0.30.60.49
Silt Loam *0.510.5
Loam0.81.60.52
Sandy Loam1.22.40.55
Loamy Sand2.550.58
Sand5100.6
Planning notes, formulas, and examples

About the Tile Drain Spacing Calculator

Tile drain spacing is one of the most important decisions in subsurface drainage design. Closer spacing drains the field faster (higher drainage coefficient) but costs more in pipe and installation. Wider spacing reduces cost but may not provide adequate drainage during wet periods.

The Hooghoudt equation provides a theoretical basis for calculating drain spacing from soil hydraulic conductivity, drain depth, and the required drainage rate. It models steady-state flow to parallel drains in a two-layer soil system and accounts for convergence of flow near the drain pipe.

This calculator uses a simplified form of Hooghoudt's equation to estimate the required drain spacing for your soil and drainage design parameters. Use this page to compare spacing scenarios before settling on a pattern that locks in both drainage performance and total tile footage.

When This Page Helps

Correct spacing balances drainage performance and cost. Too wide wastes yield in wet years; too close wastes capital. This page helps compare those trade-offs before a spacing decision is installed across the field.

How to Use the Inputs

  1. Enter the soil hydraulic conductivity (K) in inches per hour.
  2. Enter the drain depth below the soil surface in inches.
  3. Enter the midpoint water table height above drain level at design conditions.
  4. Enter the drainage coefficient (DC) in inches per day.
  5. Read the recommended drain spacing.
Formula used
S² = (4 × K × (2 × d_e × m + m²)) / q Where: S = drain spacing (ft) K = hydraulic conductivity (ft/day) d_e = equivalent depth to impermeable layer (ft) m = midpoint water table height above drain (ft) q = drainage coefficient (ft/day)

Example Calculation

Result: Spacing ≈ 60 ft

K = 0.5 in/hr = 1.0 ft/day. Drain depth = 4 ft. m = 1 ft. DC = 0.5 in/day = 0.0417 ft/day. Assuming d_e = 6 ft: S² = 4 × 1.0 × (2 × 6 × 1 + 1) / 0.0417 = 4 × 13 / 0.0417 = 1,247. S = √1,247 ≈ 35 ft. With real field conditions, typical corn-belt spacing is 40–80 ft.

Tips & Best Practices

  • Soil K varies widely; measure it in the field with a slug test or auger-hole method.
  • Typical tile spacing: 30–50 ft in heavy clays, 60–100 ft in silt loams, 100–200 ft in sandy soils.
  • Drain depth of 3–4 ft is standard for row crops in the Midwest.
  • The impermeable layer depth significantly affects the result; core to determine it.
  • Pattern tiling (parallel laterals) is most common; random tiling addresses isolated wet spots.
  • Narrower spacing pays back in yield on poorly drained soils; model the economics.

Measuring Hydraulic Conductivity

The auger-hole method is the most practical field test for K: bore a hole to below the water table, bail it out, and measure the recovery rate. The Bouwer-Rice method for slug tests gives K for the screened interval. Lab tests on core samples provide supplementary data.

Ekonomic Optimization of Spacing

Closer spacing costs more per acre but returns more yield on poorly drained soils. The economic optimum spacing is where the marginal cost of closer spacing equals the marginal yield benefit. This varies by corn/soybean price, tile cost, and soil drainage class.

Controlled Drainage

By placing adjustable outlet structures (risers) at field edges, the outlet level can be raised during non-critical periods to retain water and reduce nitrate leaching. The water table is lowered only before planting and during critical growth stages. This practice is compatible with any tile spacing.

Sources & Methodology

Last updated:

Frequently Asked Questions

  • K is the rate at which water moves through saturated soil, measured in inches per hour or feet per day. It depends on soil texture, structure, and macropores. Sandy soils: 1–10 in/hr; clays: 0.01–0.2 in/hr.