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Irrigation Scheduling Calculator

Calculate irrigation intervals, soil water depletion thresholds, and cycle application volume using FAO-56 agronomic water balance equations.

Method reviewed by Plant Calculator Team·Updated August 2026

Agronomic Soil-Water Parameters

Configure soil physical characteristics, crop root zone, and atmospheric water loss.

in
%
in/day
sq ft

Enter your parameters above and click "Calculate Results" to view recommendations.

How this is worked out

TAW = AWC × R_d · RAW = TAW × MAD · Interval (Days) = ⌊RAW / ET<sub>c</sub>⌋ · Gross Depth = RAW / E_i

Where AWC is Available Water Capacity (in/ft), R_d is effective root zone depth (ft), MAD is Management Allowed Depletion fraction, ET<sub>c</sub> is daily crop evapotranspiration (in/day), and E_i is application efficiency.

Assumptions

  • TAW represents the maximum plant-available soil moisture between Field Capacity (FC) and Permanent Wilting Point (PWP).
  • MAD is set according to crop sensitivity (typically 40% for shallow vegetables, 50% for standard crops, 60% for deep turf/trees).
  • Irrigation is triggered precisely when cumulative daily ETc depletion equals Readily Available Water (RAW).
  • Gross application depth accounts for distribution uniformity and wind drift losses.

Principles of agronomic irrigation scheduling: FAO-56 water balance

Scientific irrigation scheduling is the process of determining exact watering intervals and application depths to sustain maximum crop transpiration without causing water stress, nutrient leaching, or anaerobic root conditions. Rather than watering on a static weekly timer, precision scheduling utilizes the soil reservoir as a biological sponge that stores precipitation and irrigation water for root extraction.

Soil Available Water Capacity (AWC) by Texture

The physical capacity of a soil profile to hold water available for plant uptake is bounded by Field Capacity (FC) (the moisture content after gravitational drainage has ceased, ~-33 kPa) and the Permanent Wilting Point (PWP) (the moisture level where plants irreversibly wilt, ~-1500 kPa).

Soil Texture Available Water Capacity Reference Values
Soil Texture AWC (Inches / Foot) AWC (mm / Meter) Irrigation Characteristic
Coarse Sand0.50 – 0.7540 – 60Rapid drainage, requires daily or 2-day micro-cycles
Sandy Loam1.20 – 1.50100 – 125Moderate retention, highly responsive to drip pulses
Medium Loam1.70 – 2.00140 – 170Ideal agricultural balance of aeration and storage
Silt Loam2.00 – 2.30165 – 190Highest plant-available moisture capacity
Clay Loam1.80 – 2.10150 – 175High water retention; slow infiltration requires soak stages
Heavy Clay1.50 – 1.80125 – 150Tightly bound hygroscopic water limits usable fraction

The FAO-56 Soil Water Balance Equations

1. Total Available Water: TAW = AWC × R_d
2. Readily Available Water: RAW = TAW × MAD
3. Irrigation Interval (Days): Interval = FLOOR(RAW / ETc)
4. Gross Application Depth: d_gross = RAW / E_a
5. Total Cycle Volume: Volume (gal) = Area (sq ft) × d_gross (in) × 0.6233

Three Worked Scheduling Examples

1. Drip-Irrigated Beefsteak Tomatoes in Silt Loam Soil

Root depth = 24 inches (2.0 ft). AWC = 2.1 in/ft → TAW = 4.20 inches. For tomatoes at fruit sizing, allowable depletion (MAD) is 45% → RAW = 4.20 × 0.45 = 1.89 inches. At peak summer daily ETc of 0.27 in/day: Interval = 1.89 ÷ 0.27 = 7.0 Days. Drip efficiency = 90% → Gross depth = 1.89 ÷ 0.90 = 2.10 inches per cycle.

2. Overhead Sprinkler Bibb Lettuce in Sandy Loam

Shallow root depth = 10 inches (0.83 ft). AWC = 1.4 in/ft → TAW = 1.17 inches. Lettuce is sensitive to moisture fluctuations (MAD = 35%) → RAW = 1.17 × 0.35 = 0.41 inches. With daily ETc = 0.20 in/day: Interval = 0.41 ÷ 0.20 = 2 Days. Sprinkler efficiency = 65% → Gross application = 0.41 ÷ 0.65 = 0.63 inches every 48 hours.

3. Micro-Sprinkler Apple Orchard in Clay Loam

Root depth = 48 inches (4.0 ft). AWC = 2.0 in/ft → TAW = 8.00 inches. Deciduous fruit trees tolerate 55% MAD → RAW = 8.00 × 0.55 = 4.40 inches. Daily ETc = 0.32 in/day: Interval = 4.40 ÷ 0.32 = 13 Days. Micro-sprinkler efficiency = 80% → Gross application = 4.40 ÷ 0.80 = 5.50 inches per cycle.

Common Irrigation Scheduling Mistakes

  • Frequent shallow watering on deep-rooted crops: Daily 10-minute sprinkler cycles wet only the top 2 inches of soil, encouraging weak, superficial root mats that succumb to heat stress within hours of sun exposure.
  • Ignoring system application efficiency: Supplying only the net crop water demand without adjusting for 25% to 35% sprinkler evaporation and wind drift leads to cumulative root zone moisture deficit.
  • Applying water faster than soil infiltration rate: Heavy clay soils have intake rates below 0.20 in/hr. Applying 1.0 inch in 30 minutes creates surface runoff and puddling rather than root recharge.

Coordinate system flow and emitter layout with our Drip Irrigation Planner, Drip Flow Rate Calculator, and Watering Schedule Calculator.

Common questions

What is Management Allowed Depletion (MAD)?

Management Allowed Depletion (MAD) is the maximum percentage of Total Available Water (TAW) that a crop can extract from the root zone before experiencing water stress and yield decline. For shallow-rooted vegetables like lettuce and onions, MAD is typically set between 30% and 40%, while drought-hardy crops and mature fruit trees tolerate 50% to 60% depletion.

How does soil texture influence irrigation interval?

Coarse sandy soils hold very little water (0.5 to 1.0 inches per foot of depth), necessitating frequent, shallow waterings every 2 to 3 days. Heavy clay and silt loam soils store significantly more water (1.8 to 2.4 inches per foot), allowing extended irrigation intervals of 6 to 10 days between cycles.

What is the difference between Net and Gross Irrigation Depth?

Net Irrigation Depth (d_net) is the exact volume of water needed to refill the root zone depletion back to field capacity. Gross Irrigation Depth (d_gross) accounts for system distribution inefficiencies, wind drift, and evaporation by dividing net depth by the irrigation system efficiency (e.g. 90% for drip, 70% for overhead rotors).

How do I determine Daily Crop Evapotranspiration (ETc)?

Daily ETc is calculated by multiplying local Reference Evapotranspiration (ET0 from weather stations) by the specific Crop Coefficient (Kc) for the current growth stage (ETc = ET0 × Kc). Peak summer mid-season vegetable ETc typically ranges between 0.20 and 0.35 inches per day.

Method reviewed by

Plant Calculator Team

Editorial Team

The Plant Calculator team is a group of gardening enthusiasts, horticulturists, and landscaping professionals dedicated to helping you grow your best garden.

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