Field Study: Determining Actual ET of Various Grasses
The study location has a high-desert climate characterized by hot, dry summers and cold winters, with average annual precipitation of about 8 inches. This is a transition zone where both cool- and warm-season turfgrasses can be grown. Cool-season grasses included in the study were Kentucky bluegrass (‘Adelphi’ and ‘Park’), turf-type tall fescue (‘Shenandoah’) and perennial ryegrass (‘Seville’). Warm-season grasses included seeded varieties of bermudagrass (‘Guymon’), buffalograss (‘Bison’) and blue grama (‘Lovington’). Nutrients were applied as needed to prevent stress and all grasses were mown at 2.75 inches except for blue grama, which was raised to 4 inches due to poor initial quality at the lower height.
Researchers used a line-source sprinkler (LSS) system that delivered a gradient of water across test plots, ranging from full replacement of ETos (near 100%) close to the sprinkler line to less than 10% replacement farther away. Catch cans recorded irrigation amounts and soil moisture was monitored with neutron probes down to 54 inches. Then, ETa was calculated using a “water-balance” approach that considered irrigation, rainfall, changes in soil water, and gravitational drainage. Turf quality was rated visually on a 1-9 scale, where 6 represented the minimum acceptable level for golf course play. Importantly, the study determined ETa at the point along the irrigation gradient where turf maintained its minimum acceptable quality – providing a realistic basis for irrigation scheduling in water-limited conditions for each of the different grasses in the study. It’s important to note that this amount varies by grass type and is something superintendents managing different species should consider. Irrigation began in March or April and was performed two or three times per week to maintain 100% replacement of ETos in the plot nearest the water source. A weather station recorded data to calculate ET. The full details of the study materials and methods, as well as the statistical analysis and Kc modeling, can be found here in the peer-reviewed scientific article.
Developing Variable Kc Models Using Actual ET Rates and GDD
Rather than estimating Kc based on the calendar (which likely would not provide year-to-year consistency), the researchers normalized Kc values using GDD, a measure of accumulated heat units. This approach accounts for differences in growing season onset, duration and year-to-year temperature variability. The researchers also validated their models with independent data collected during a second field study in New Mexico from 2003 to 2005, which included different grasses, ensuring the findings were robust and applicable across seasons and for different grass varieties.
This is the first study to develop crop coefficient models adjusted for GDD specifically for turfgrass, and unlike prior research, it emphasizes minimum water requirements for acceptable quality rather than optimal quality for near perfect conditions. Its validation with independent data collected several years later demonstrates the reliability of the models across varying conditions.
Key Results: Turfgrass Water Use Patterns and Variable Kc Models
Measured ETa varied by grass type and year. At peak water use, cool-season grasses used between 0.21 and 0.26 inch of water per day, while warm-season grasses required between 0.18 and 0.20 inch per day. For cool-season grasses, year-to-year variability was more pronounced than differences among cultivars, indicating that weather conditions had a stronger influence on water use than genetic variation. Warm-season grasses, on the other hand, exhibited greater within-year variability, reflecting their sensitivity to seasonal heat patterns. When data were averaged across years and cultivars, daily cool-season predicted water use ranged from 0.04 to 0.24 inch and warm-season predicted water use ranged from 0.04 to 0.19 inch.
Kc values also displayed seasonal patterns. When averaged across years and cultivars, peak cool-season grass Kc values ranged from about 0.76 to 0.95, while warm-season grass peak Kc values ranged from about 0.66 to 0.76. But when Kc values were looked at over the course of a growing season, predicted cool-season Kc ranged from 0.44 to 0.90 and predicted warm-season Kc ranged from 0.36 to 0.69. These lower values indicate that at certain times of the year observed ET was much lower than constant reference ET, and irrigation can be reduced during these periods (Figure 1).