This study was designed to evaluate the crop water stress index (CWSI) for
low-energy precision application (LEPA) irrigated corn (Zen mays L.) grown
on slowly-permeable Pullman clay loam soil (fine, mixed, Torrertic Paleusto
ll) during the 1992 growing season at Bushland, Tex. The effects of six dif
ferent irrigation levels (100%, 80%, 60%, 40%, 20%, and 0% replenishment of
soil water depleted from the 1.5-m soil profile depth) on corn yields and
the resulting CWSI were investigated. Irrigations were applied in 25 mm inc
rements to maintain the soil water in the 100% treatment within 60-80% of t
he "plant extractable soil water" using LEPA technology, which wets alterna
te furrows only. The 1892 growing season was slightly wetter than normal. T
hus, irrigation water use was less than normal, but the corn dry matter and
grain yield were still significantly increased by irrigation. The yield, w
ater use, and water use efficiency of fully irrigated corn were 1.246 kg/m(
2), 786 mm, and 1.34 kg/m(3), respectively. CWSI was calculated from measur
ements of infrared canopy temperatures, ambient air temperatures, and vapor
pressure deficit values for the six irrigation levels. A "non-water-stress
ed baseline" equation for corn was developed using the diurnal infrared can
opy temperature measurements as T-c-T-a= 1.06-2.56 VPD, where T-c was the c
anopy temperature (degrees C), Ta was the air temperature (degrees C) and V
PD was the vapor pressure deficit (kPa). Trends in CWSI values were consist
ent with the soil water contents induced by the deficit irrigations. Both t
he dry matter and grain yields decreased with increased soil water deficit.
Minimal yield reductions were observed at a threshold CWSI value of 0.33 o
r less for corn. The CWSI was useful fur evaluating crop water stress in co
rn and should be a valuable tool to assist irrigation decision making toget
her with soil water measurements and/or evapotranspiration models.