Cultivating Flora

When to Start and Stop Irrigation in Kansas Growing Seasons

Kansas spans a wide gradient of climate, soils, and cropping systems. Deciding when to start and stop irrigation depends on region, crop, soil water holding capacity, current weather and forecast, and long-term water supply considerations. This article synthesizes principles and provides concrete, actionable guidance for Kansas producers and managers so irrigation timing maximizes yield, conserves water, and reduces risk.

Kansas climate and soil context

Kansas climate ranges from humid continental in the east to semi-arid in the west. Annual precipitation can exceed 35 inches in the far east but commonly falls to 15 inches or less in western counties. Growing season rainfall distribution is highly variable year to year, and June through August are the months of highest crop water demand.
Soils influence how frequently and how much you must irrigate. Typical root zone effective water holding capacity (plant available water, PAW) varies by texture:

Rooting depth differs by crop and management: corn commonly explores 36 inches or more, soybeans 24-36 inches, winter wheat 18-30 inches. Effective water available to the crop is PAW times root zone depth.

Regional differences and practical consequences

Western Kansas: limited rainfall and more evaporative demand mean irrigation often begins earlier in the season and is the dominant source of crop water. Start planning irrigation at planting or soon after if soil moisture is shallow.
Central Kansas: variable — some seasons natural rainfall meets early needs while mid-season irrigations are needed during hot dry periods.
Eastern Kansas: more rain, fewer irrigations in average years. Irrigation often is used to supplement during extended dry spells or to protect sensitive reproductive stages.

Principles of irrigation timing

Irrigation timing is best driven by two complementary approaches: soil moisture status and crop water demand (ET). Use both together for robust decisions.

Soil moisture thresholds and allowable depletion

Irrigate to refill the root zone before crop stress causes irreversible yield loss. The most common operational rule is to apply water when root-zone depletion reaches a crop- and soil-specific allowable depletion fraction of total available water (TAW).
Key guidance:

Example: Corn with 36 in root zone and loam PAW 0.14 in/in -> TAW = 36 x 0.14 = 5.0 inches. If AD = 0.50, irrigate when 2.5 inches are depleted; refill to near field capacity (apply ~2.5 inches plus some allowance for system inefficiencies).
During critical reproductive periods (corn tassel-silk, soybean R1-R4, wheat heading and grain fill), reduce AD (refill earlier) because yield response per unit water is high.

Using ET and weather forecasts

Reference evapotranspiration (ETo) combined with crop coefficients (Kc) gives crop evapotranspiration (ETc = ETo x Kc). In Kansas, mid-summer daily ETc often ranges from roughly 0.15 to 0.35 inches per day depending on region and heat. Use local ETo estimates, adjust for effective rainfall, and schedule irrigations to replace the accumulated ET losses up to the allowable depletion.
Practical tips:

Crop-specific timing guidance for Kansas

Different crops have different critical periods and rooting behavior. Below are practical, field-ready timing rules.

Corn (grain)

Soybean

Grain Sorghum (milo)

Winter Wheat

Alfalfa and forage crops

Vegetables and high-value horticulture

Scheduling and practical management

Tools and monitoring

Irrigation depth and frequency

Conservation, risk management, and the Ogallala Aquifer

Water resource limits define long-term viability in western Kansas. Consider:

Practical takeaways and a simple decision checklist

Closing summary

Irrigation timing in Kansas requires a balance of soil moisture monitoring, crop growth stage awareness, and regional climate realities. Start irrigation when depletion of plant available water reaches a crop-specific allowable level, and stop when additional water no longer increases yield or when physiological maturity is reached. Protect critical reproductive windows by maintaining higher soil moisture. Combining soil sensors, ET tracking, and practical field checks will produce the best results: higher yields with smarter, more sustainable water use.