Ozone stress, carbon dioxide enrichment, and nitrogen fertility interactions in cotton

Citation
As. Heagle et al., Ozone stress, carbon dioxide enrichment, and nitrogen fertility interactions in cotton, CROP SCI, 39(3), 1999, pp. 731-741
Citations number
39
Categorie Soggetti
Agriculture/Agronomy
Journal title
CROP SCIENCE
ISSN journal
0011183X → ACNP
Volume
39
Issue
3
Year of publication
1999
Pages
731 - 741
Database
ISI
SICI code
0011-183X(199905/06)39:3<731:OSCDEA>2.0.ZU;2-W
Abstract
Ozone (O-3) in the troposphere can cause plant stress leading to foliar inj ury and suppressed growth and yield, whereas elevated CO2 generally enhance s growth and yield. Numerous studies have been performed to determine effec ts of O-3 and CO2 separately, but relatively few have been performed to det ermine if O-3 can affect plant response to CO2 or vice versa. Open-top fiel d chambers were used to determine if such interactions occur for cotton (Go ssypium hirsutum L.), which is relatively sensitive to O-3. Nitrogen nutrit ion is especially important in cotton production so N nutrition was include d as an experimental factor. Plants were grown in 14-L pots at low, medium, and high soil N levels and exposed to three CO2 and two or three O-3 treat ments in all combinations during two seasons. The CO2 treatments were ambie nt (370 mu L L-1) and two treatments with CO2 added for 24 h d(-1) at appro ximately 1.5 and 2.0 Limes ambient. In 1995, the O-3 treatments were charco al filtered air (CP), and nonfiltered air (NF) with O-3 added for 12 h d(-1 ) (NF+). In 1996, a NF treatment was also included to represent ambient O-3 conditions. The CF, NF, and NF+ treatments resulted in seasonal O-3 concen trations of approximately 23, 51, and 75 nL L-1. Carbon dioxide enrichment generally stimulated growth and yield whereas O-3 exposure suppressed growt h. and yield. Stimulation induced by CO2 increased as O-3 stress increased. For example, in 1995 at medium N, the percentage increase in yield caused by doubling CO2 in CF air was 0%, but was 52% in NF+ air. Comparable values for 1996 were 23% in CF air and 140% in NF+ air. These interactions occurr ed for a range of soil N levels, and were probably caused by CO2-induced pr evention of O-3 stress. The results emphasize the need to consider O-3 x CO 2 interactions to ensure correct interpretation of cause-effect relationshi ps in CO2 enrichment studies with crops that are sensitive to O-3.