Je. Miller et al., ULTRAVIOLET-B RADIATION AND OZONE EFFECTS ON GROWTH, YIELD, AND PHOTOSYNTHESIS OF SOYBEAN, Journal of environmental quality, 23(1), 1994, pp. 83-91
The projected increase in solar ultraviolet-B (UV-B) radiation due to
depletion of stratospheric ozone (O-3) has caused concern regarding po
ssible UV-B damage to crops. At the same time, tropospheric O-3 is pro
jected to remain at concentrations that are known to damage crops. Sin
ce these two stressors may co-occur, experiments were performed to det
ermine their separate and joint effects on crop growth, yield, and pho
tosynthesis. Open-top chambers, equipped with filtered UV-B lamp syste
ms, were used in 3 yr of field studies to treat soybean [Glycine mau (
L.) Merr.; 'Coker 6955','Essex', and 'S 53-34'] with supplemental UV-B
radiation and/or O-3 from emergence through physiological maturity. T
reatment levels of biologically effective UV-B radiation (UV-B-BE) sim
ulated the increase in ground level W-B for stratospheric O-3 depletio
n up to 37% (approximately a doubling of ambient UV-B-BE). Ozone treat
ment concentrations ranged from 14 to 83 nL L(-1) (seasonal mean 12 h
d(-1) concentrations). Ultraviolet-B radiation did not affect soybean
seed yield in any of the 3 yr of the study. In 1 yr, UV-B affected pod
and seed number and pod weight, but the treatment means were not cons
istently related to the UV-B dose. No O-3 x UV-B interactions were fou
nd for any yield component at final harvest. Biweekly harvests of Esse
x during the growing season did not reveal any persistent effects of i
ncreased UV-B radiation on growth. Net carbon exchange rate (NCER), st
omatal conductance, and transpiration of Essex soybean leaves were not
suppressed by supplemental UV-B radiation. On the other hand, O-3 tre
atment consistently induced visible injury, suppressed NCER and water
use efficiency, accelerated reproductive development, and suppressed g
rowth and yield. It is concluded that tropospheric O-3 poses a greater
threat to soybean production than projected levels of UV-B radiation.