Jack R. Mauney
Agricultural Research Service
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Agricultural and Forest Meteorology | 1994
Jack R. Mauney; Bruce A. Kimball; Paul J. Pinter; Robert L. LaMorte; Keith F. Lewin; John Nagy; George R. Hendrey
To quantify the growth and yield responses to CO2 enrichment in an open field setting, freeair CO2 enrichment (FACE) technology was used to expose a cotton (Gossypium hirsutum L.) crop to 550 γmol mol−2 CO2 throughout the growing seasons of 1989, 1990 and 1991 in fields near Maricopa, Arizona. In 1990 and 1991 a water stress treatment was also imposed. Response data for all years were consistent, and the data for 1991 were the least compromised by unusual weather or equipment failures. In that season the biomass was increased 37% by the 48% increase in CO2 concentration. Harvestable yield was increased 43%. The increase in biomass and yield was attributed to increased early leaf area, more profuse flowering and a longer period of fruit retention. The FACE treatment increased water-use efficiency (WUE) to the same amount in the well-irrigated plots as in the water-stressed plots. The increase in WUE was due to the increase in biomass production rather than a reduction of consumptive use.
Agricultural and Forest Meteorology | 1994
Bruce A. Kimball; Robert L. LaMorte; R.S. Seay; Paul J. Pinter; R.R. Rokey; D.J. Hunsaker; William A. Dugas; M.L. Heuer; Jack R. Mauney; George R. Hendrey; Keith F. Lewin; John Nagy
Abstract The effects of free-air CO2 enrichment (FACE) at 550 μmol mol−1 on the energy balance and evapotranspiration, ET, of cotton (Gossypium hirsutum L.) were investigated. Latent heat flux, λET was calculated as the residual in an energy balance approach from determinations of net radiation, Rn minus surface soil heat flux, G0, minus sensible heat flux, H. Rn was directly measured. G0 was determined from measurements with soil heat flux plates at 10 mm depth, corrected for temperature changes in the soil above. H was determined from measurements of air temperature with aspirated psychrometers, of foliage temperature with IR thermometers, and of wind speed with cup anemometers. Under ambient CO2 (control) conditions (about 370 μmol mol−1), the λET from the energy balance approach agreed fairly well with values from several other methods, including the Bowen ratio method, lending credence to the technique. However, the results had an uncertainty of the order of 20% associated with the Rn measurements. Therefore, an apparent increase in ET of about 13% in the FACE plots was judged insignificant. The conclusion that any effects of CO2 enrichment to 550 μmol mol−1 on the ET of cotton were too small to be detected was consistent with the results of other investigators who determined ET in the same experiment using stem flow gauges and the soil water balance.
Agricultural and Forest Meteorology | 1994
Steven W. Leavitt; Eldor A. Paul; Bruce A. Kimball; George R. Hendrey; Jack R. Mauney; Roy Rauschkolb; Hugo H. Rogers; Keith F. Lewin; John Nagy; Paul J. Pinter; Hyrum B. Johnson
A role for soils as global carbon sink or source under increasing atmospheric CO2 concentrations has been speculative. Free-air carbon dioxide enrichment (FACE) experiments with cotton, conducted from 1989 to 1991 at the Maricopa Agricultural Center in Arizona, maintained circular plots at 550 μmol mol−1 CO2 with tank CO2 while adjacent ambient control plots averaged about 370 μmol mol−1 CO2. This provided an exceptional test for entry of carbon into soils because the petrochemically derived tank CO2 used to enrich the air above the FACE plots was depleted in both radiocarbon (14C content was 0% modern carbon (pmC)) and 13C (δ13C≈ −36‰) relative to background air, thus serving as a potent isotopic tracer. Flask air samples, and plant and soil samples were collected in conjunction with the 1991 experiment. Most of the isotopic analyses on the plants were performed on the holocellulose component. Soil organic carbon was obtained by first removing carbonate with HCl, floating off plant fragments with a NaCl solution, and picking out remaining plant fragments under magnification. The δ13C of the air above the FACE plots was approximately −15 to −19‰, i.e. much more 13C depleted than the background air of approximately −7.5‰. The δ13C values of plants and soils in the FACE plots were 10–12‰ and 2‰13C-depleted, respectively, compared with their control counterparts. The 14C content of the FACE cotton plants was approximately 40 pmC lower than tha tof the control cotton, but the 14C results from soils were conflicting and therefore not as revealing as the δ13C of soils. Soil stable-carbon isotope patterns were consistent, and mass balance calculations indicate that about 10% of the present organic carbon content in the FACE soil derived from the 3 year FACE experiment. At a minimum, this is an important quantitative measure of carbon turnover, but the presence of 13C-depleted carbon, even in the recalcitrant 6 N HCl resistant soil organic fraction (average age 2200 years before present (BP)), suggests that at least some portion of this 10% is an actual increase in carbon accumulation. Similar isotopic studies on FACE experiments in different ecosystems could permit more definitive assessment of carbon turnover rates and perhaps provide insight into the extent to which soil organic matter can accommodate the ‘missing’ carbon in the global carbon cycle.
Agricultural and Forest Meteorology | 1994
D.J. Hunsaker; George R. Hendrey; Bruce A. Kimball; Keith F. Lewin; Jack R. Mauney; John Nagy
The CO2 concentration of the atmosphere is predicted to double by the next century, and this is expected to increase significantly the growth and yield of many important agricultural crops. One consequence of larger and more vigorous plants may be increased crop evapotranspiration (ET) and irrigation water requirements. The objective of this work was to determine ET of cotton (Gossypium hirsutum L. cv. ‘Deltapine 77’) grown under ambient (about 370 μmol mol−1) and enriched (550 μmol mol−1) CO2 concentrations for both well-watered and water-stress irrigation managements. Studies were conducted in 1990 and 1991 within a large, drip-irrigated cotton field in central Arizona. Cotton ET was measured during the growing seasons using a soil water balance, based on neutron gauge soil water measurements. ET, for periods from 7 to 14 days, was not significantly different between ambient and enriched CO2 treatments at the 0.05 probability level, and the total seasonal ET for the CO2 treatments varied by 2% or less in either year. However, water-stress treatments, which were initiated on 3 July (day of year (DOY) 184) in 1990 and on 20 May (DOY 128) in 1991, had significantly lower (P < 0.05) ET than well-watered treatments starting at the end of July in 1990 and in early July in 1991 when the plants were about 75–90 days old. The result that CO2 enrichment to 550 μmol mol−1 did not significantly change the ET of cotton was consistent with the results of co-investigators who measured ET in the same experiments using stem flow gauges and an energy balance. This result implies that irrigation water use would not have to be increased to produce cotton in a future high-CO2 world. However, if a concomitant change in climate occurs, such as global warming, cotton evapotranspiration may change in response to the changed weather condition.
Agricultural and Forest Meteorology | 1994
D.L. Hendrix; Jack R. Mauney; Bruce A. Kimball; Keith F. Lewin; John Nagy; George R. Hendrey
Root, stem and leaf tissues, from cotton plants exposed to CO2 at ambient (370 μmol mol−1 (control)) or elevated (550 μmol mol−1 (FACE; free-air carbon dioxide enrichment)) levels in the field during the 1990 and 1991 growing seasons, were analyzed for nonstructural carbohydrates (glucose, fructose, sucrose and starch). Besides the FACE treatment, these plants were also exposed to two irrigation levels: 100% and 67% replacement of evapotranspiration. FACE had a greater effect upon cotton plant nonstructural carbohydrates than did irrigation treatments. Leaf carbohydrate content was increased by FACE, but this increase was much more pronounced in the stems and roots. Starch and soluble sugars in leaves in FACE plots tended to be consistently greater than in control leaves, without much change in carbohydrate content during the growing season. In contrast, root and stem, starch and soluble sugar pools were strongly increased by FACE and fluctuated strongly during the growing season. In both seasons, stem and taproot nonstructural carbohydrate content passed through a minimum during periods of heavy boll set. The fluctuations in stem and root carbohydrate content were therefore probably caused by the varying metabolic demands of the developing plant. These results suggest that a significant effect of CO2 enrichment on starch-accumulating plants is an increase of nonstructural carbohydrate, especially starch, in nonleaf storage pools. This buildup occurs somewhat independently of the water status of the plant, and these enlarged pools can be drawn upon by the growing plant to maintain growth during periods of high metabolic demand.
Agricultural and Forest Meteorology | 1994
N.C. Bhattacharya; J.W. Radin; Bruce A. Kimball; Jack R. Mauney; George R. Hendrey; John Nagy; Keith F. Lewin; D.C. Ponce
As part of an intensive study of crop response to CO2 enrichment in a free-air CO2 enrichment (FACE) experiment in the field, we determined aspects of the water relations of a cotton crop on selected dates in 1991. The atmosphere was enriched from 370 μmol CO2 mol−1 (control) to about 550 μmol mol−1 in free air during daylight hours. Under full irrigation, CO2 enrichment decreased stomatal conductance and single-leaf transpiration only toward the end of the season, and these changes led to increased leaf water potentials only at that time of year. Under water-stressed (deficit irrigation) conditions, CO2 enrichment decreased conductance throughout the season but there was no corresponding consistent effect on leaf water potentials. As with the fully irrigated controls, CO2 enrichment increased leaf water potentials only at the end of the season. CO2 enrichment increased season-long biomass accumulation 39% under full irrigation and 34% under deficit irrigation. These results are consistent with previous studies of cotton in open-top chambers that found only small effects of CO2 enrichment on internal water relations of cotton, and no water stress-induced increase in crop responsiveness to elevated CO2.
Critical Reviews in Plant Sciences | 1992
Jack R. Mauney; Keith F. Lewin; George R. Hendrey; Bruce A. Kimball
Most crops respond positively to an increase in CO{sub 2} concentration, based on experiments in glasshouses, growth chambers and open-topped CO{sub 2} enrichment enclosures. For example, from examining 480 citations an average response of 30% increase in yield with doubling of CO{sub 2} was found. Such previous experiments with cotton (Gossypium hirsutum L.) have shown it to be one of the most responsive species observed, with yield increases of 60 to 100% when CO{sub 2} is doubled. 12 refs., 8 figs., 5 tabs.
Critical Reviews in Plant Sciences | 1992
Bruce A. Kimball; Paul J. Pinter; Jack R. Mauney
Other chapters have described the 1989 Free-Air CO{sub 2} Enrichment (FACE) experiment, which involved enriching the atmosphere to 550 {mu}mol mol{sup {minus}1} of CO{sub 2} over cotton in an open field at the University of Arizona Maricopa Agricultural Center (MAC). Prior work showed that such enrichment in open-top chambers elevated the foliage temperatures of well-watered cotton by about 0.6{degrees}C (with a 95% confidence interval of about {+-} 0.3{degrees}C). Thus, one objective of the 1989 FACE experiment was to determine experimentally under open-field conditions how CO{sub 2} concentrations like those expected in the future would affect cotton foliage temperatures. 10 refs., 8 figs., 2 tabs.
Agricultural and Forest Meteorology | 1994
Paul J. Pinter; S.B. Idso; D.L. Hendrix; R.R. Rokey; R.S. Rauschkolb; Jack R. Mauney; Bruce A. Kimball; George R. Hendrey; Keith F. Lewin; John Nagy
Abstract In vivo chlorophyll concentrations were estimated using a Minolta SPAD 502 meter on upper-canopy leaves of cotton plants exposed to air enriched to an atmospheric CO 2 concentration of approximately 550 μmol mol −1 in a free-air CO 2 enrichment (FACE) study. Measurements were made on 27 days during the final 90 days of the 1991 growing season. In both well-watered and moderately water-stressed plants, leaves in the FACE plots had greater chlorophyll a concentrations than leaves in the ambient air control plots (about 370 μmol CO 2 mol −1 ): season-long chlorophyll a averages were 7.1% greater in the ‘wet’ treatment and 8.2% greater in the ‘dry’ treatment. This finding differs from what has been observed in a number of studies where experimental plants were grown in small pots. It is, however, typical of what has been observed in studies employing larger pots and open fields, and is a compelling rationale for conducting additional studies of this nature in FACE projects.
Agricultural and Forest Meteorology | 1994
Sherwood B. Idso; Bruce A. Kimball; G. W. Wall; R. L. Garcia; Robert L. LaMorte; Paul J. Pinter; Jack R. Mauney; George R. Hendrey; Keith F. Lewin; John Nagy
Daytime measurements of leaf CO2 exchange rates in a free-air CO2 enrichment (FACE) experiment reveal that at photosynthetically active radiation (PAR) flux rates in excess of 1000 μmol m−2 s−1, cotton leaves exposed to an atmospheric CO2 concentration of approximately 500 μmol mol−1 exhibit net photosynthetic rates about 30% greater than those for leaves of similar plants growing in ambient air. As PAR flux rates drop below this value, the stimulatory effect of elevated CO2 rises, suggesting that the relative benefits of atmospheric CO2 enrichment will be greater for shaded cotton leaves that for those exposed to full sunlight.