Elsevier

Advances in Agronomy

Volume 77, 2002, Pages 293-368
Advances in Agronomy

Responses of Agricultural Crops to Free-Air CO2 Enrichment

https://doi.org/10.1016/S0065-2113(02)77017-XGet rights and content

Over the past decade, free-air CO2 enrichment (FACE) experiments have been conducted on wheat, perennial ryegrass, and rice, which are C3 grasses; sorghum, a C4 grass; white clover, a C3 legume; potato, a C3 forb with tuber storage; and cotton and grape, which are C3 woody perennials. Elevated CO2 increased photosynthesis, biomass, and yield substantially in C3 species, but little in C4. It decreased stomatal conductance in both C3 and C4 species and greatly improved water-use efficiency in all crops. Growth stimulations were as large or larger under water stress compared to well-watered conditions. At low soil N, stimulations of nonlegumes were reduced, whereas elevated CO2 strongly stimulated the growth of the clover legume at both ample and low N conditions. Roots were generally stimulated more than shoots. Woody perennials had larger growth responses to elevated CO2, but their reductions in stomatal conductance were smaller. Tissue N concentrations went down, while carbohydrate and some other carbon-based compounds went up, with leaves being the organs affected most. Phenology was accelerated slightly in most but not all species. Elevated CO2 affected some soil microbes greatly but not others, yet overall activity was stimulated. Detection of statistically significant changes in soil organic carbon in any one study was nearly impossible, yet combining results from several sites and years, it appeared that elevated CO2 did increase sequestration of soil carbon. Comparisons of the FACE results with those from earlier chamber-based results were consistent, which gives confidence that conclusions drawn from both types of data are accurate.

Introduction

The increasing CO2 concentration of Earth's atmosphere and associated predictions of global warming (IPCC, 1996) have stimulated research programs to determine the likely effects of the future elevated CO2 levels on agricultural productivity and on the functioning of natural ecosystems (e.g., Dahlman et al., 1985). However, even predating the global change concerns, the effects of atmospheric CO2 enrichment have been studied for more than a century in greenhouses, controlled-environment chambers, open-top chambers, and other enclosures to confine the CO2 gas around the experimental plants (e.g., Drake et al., 1985; Enoch and Kimball, 1986; Schulze and Mooney, 1993). The results of these many chamber-based experiments have been reviewed by Kimball (1983, 1986, 1993), Morison (1985), Cure (1985), Cure and Acock (1986), Kimball and Idso (1983), Poorter (1993), Idso and Idso (1994), Ceulemans and Mousseau (1994), Wullschleger et al. (1997), Cotrufo et al. (1998), Norby et al. (1999), Nakagawa and Horie (2000), Curtis and Wang (1998), and Wand et al. (1999) (although the latter two also included a few observations from recent nonchamber open-field experiments).

However, the environment inside enclosures is not generally like that outside (e.g., Kimball et al., 1997; McLeod and Long, 1999); thus, there have been many concerns that the results from such enclosure-based CO2-enrichment experiments might not be representative of future open fields and forests. Therefore, various attempts were made to develop techniques which could maintain the CO2 concentrations over open-field plots at elevated levels despite the challenges imposed by open-field winds causing rapid dispersal of the CO2 (Allen, 1992; Norby et al., 2001). Eventually, engineers from Brookhaven National Laboratory (Upton, New York) working cooperatively with scientists from the U.S. Department of Agriculture, Agricultural Research Service, and from Tuskegee University, as well as others, were able to adapt a “vertical vent pipe” technology that could adequately maintain the desired high levels of CO2 over open-field plots all growing-season long (Hendrey, 1993; Norby et al., 2001). The first such experiment with publishable biological data was conducted on cotton in 1989 at Maricopa, Arizona. After success with cotton, the Brookhaven group moved their engineering efforts to the forest, and they were able to increase the scale of the apparatus to accommodate 14-m-tall trees (e.g., Delucia et al., 1999). Once it was demonstrated that such free-air CO2 enrichment (FACE) experiments were feasible, several other research groups also initiated similar experiments in both managed and natural ecosystems. To date, there are about 30 active or planned FACE sites (http://cdiac.esd.ornl.gov/programs/FACE/face.html; http://www.face.bnl.gov/; http://gcte-focus1.org/co2.html).

The purposes of this paper are (i) to compile the available data from the FACE experiments on agricultural crops; (ii) to determine the relative responses of the several crops to elevated CO2 with regard to their physiology, growth, yield, water relations, and soil processes; (iii) to search for similarities and differences among species and plant functional types; and (iv) to compare these FACE results with those from prior chamber-based studies.

Section snippets

Methodology

We have extracted data from papers and manuscripts generated by our agricultural-crop-oriented free-air CO2 enrichment (FACE) projects at Maricopa, Arizona; Shizukuishi, Iwate, Japan; and Rapolano, Terme, Italy, as well as from the grassland project at Eschikon, Switzerland. The experimental protocols and site characteristics for the several experiments are listed in Table I. From the absolute crop response values, we computed the relative increases (or decreases, which are listed as negative

Photosynthesis

It is well known that elevated CO2 stimulates photosynthesis. The main uncertainties regard the degrees of stimulation for each species and environmental condition. Also important is whether or not the plants acclimate to the higher CO2 by altering the biochemical makeup of the their photosynthetic apparatus so that the photosynthetic rate at high CO2 decreases to become closer to that at today's ambient CO2. The biochemical and molecular bases for such photosynthetic acclimation have been

Compendium and Conclusions

The quantitative relative changes due to elevated CO2 (550 or about 190 μmol mol−1 above ambient) in the several crop growth and other parameters as determined from the FACE experiments are summarized in Table III. Except as noted, the responses agree with prior chamber-based results. Obviously, the FACE experiments on agricultural crops during this past decade have produced a vast amount of information about the responses of several species to elevated CO2. The selected species were

Summary

Over the past decade, free-air CO2-enrichment (FACE) experiments have been conducted on several agricultural crops: wheat (Triticum aestivum L.), perennial ryegrass (Lolium perenne), and rice (Oryza sativa L.) which are C3 grasses; sorghum (Sorghum bicolor (L.) Möench), a C4 grass; white clover (Trifolium repens), a C3 legume; potato (Solanum tuberosum L.), a C3 forb with tuber storage; and cotton (Gossypium hirsutum L.) and grape (Vitis vinifera L.) which are C3 woody perennials. Using reports

Acknowledgments

The senior author greatly appreciates the Science and Technology Agency (STA) Fellowship (ID 300005), which enabled him to work on this paper at the National Institute of Agro-Environmental Science, Tsukuba, Japan, for 3 months. We also appreciate the cooperation of Drs. Josef Noesberger and Herbert Blum, Institute of Plant Sciences, ETH, Zurich, Switzerland, who furnished preprint copies of several papers with data from the Swiss FACE Project and provided helpful comments.

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