Review banner (jpeg, 45K)

bulletORNL Review Home Page
bulletFeatured in This Edition
bulletLast Article
bulletNext Article
bulletSearch the ORNL Review Site
bulletComment on this article

The high growth rate of an Oak Ridge tree plantation exposed to carbon dioxide–enriched air declined significantly in the FACE experiment's second year.

High-Carbon Tree Growth Rate Falls

In 1998, an experimental 10-year-old sweetgum plantation in Oak Ridge National Laboratory's Environmental Research Park showed a 35% increase in growth over a nearby control stand of trees. More wood was produced in the test forest's tree trunks and more fine roots grew in the soil. The 15-m-tall sweetgum trees in the plantation's 25-m-diameter plots grew more because they were being exposed to air containing 50% more carbon dioxide (CO2) than is in the atmosphere, thanks to free-air CO2 enrichment (FACE) technology.

High-carbon sweetgum forest (jpg, 114K)
Standing in a hydraulic lift, Rich Norby collects leaves in the high-carbon sweetgum forest for measurements of leaf mass, nitrogen concentrations, and rates of photosynthesis.

In 1999, the second year of the FACE experiment funded by the Department of Energy, some of the data surprised Richard Norby and his ORNL collaborators Stan Wullschleger, Carla Gunderson, Gerry O'Neill, Paul Hanson, Nelson Edwards, Tim Tschaplinski, Mac Post, Don Todd, and Tony King. The growth rate increase of the experimental plantation was reduced to 15% over that of the control stand. These results differ from those at a Duke University plantation dominated by loblolly pine trees with sweetgum trees in the understory. In the past three years, Duke researchers have observed a sustained growth rate increase of 25% per year in the trunks of high-CO2 pine trees over that of control trees in a normal atmosphere.

"The dramatic growth response we saw in the first year in Oak Ridge disappeared in the second," says Norby, leader of the collaboration at the FACE facility and a researcher in ORNL's Environmental Sciences Division (ESD). "It could be year-to-year variability or a blip in the first year's data because of the sudden increase in CO2 concentration. It could be a short-term response that is not indicative of the long-term response. Some of our data indicate that the growth increase was actually maintained but the extra carbon was not stored in the tree trunks."

Many of the physiological responses observed in the second year were similar to those in the first year of the FACE experiment. "We observed that photosynthesis remained enhanced," Norby says, referring to the process by which plants use the energy from sunlight to convert CO2 and water into sugars needed for growth. "The leaf area stayed the same, and the trees conserved water just as well in the second year as the first."

In both years, ORNL scientists observed that the tree leaf pores (stomata), which allow CO2 to enter and water vapor to escape, were not open as wide in plots receiving the extra CO2. "Trees use more water on sunny days and less on overcast or rainy days," says Norby. "Because of high CO2 in air, they can close their stomata a little on days of high water use and get the CO2 they need while letting out less water. Thus, they draw less water from the ground, allowing soil moisture levels to be higher. Higher soil moisture could result in more activity by microbes that may make more nitrogen available to plants, fertilizing them and promoting their growth."

In addition to the tree growth rate difference in 1998 and 1999 at the FACE facility, ORNL scientists also observed that the leaves of the high-CO2 trees became heavier in 1999, probably because more of the extra carbon was used to produce leaves than increase trunk growth. They also found that the nitrogen concentration of leaves and litter (fallen leaves on the forest floor) was lower, which could retard the cycling of nitrogen and carbon in the ecosystem.

ORNL researchers also observed an increase in production and mortality of fine roots in the second year, resulting in a change in the belowground allocation of carbon. "We saw an increase in carbon cycling because of high root turnover," Norby says. "The fine roots took in more carbon and then rapidly died, releasing more carbon to the soil than usual."

Because ORNL and Duke scientists are doing similar experiments on plantations of equivalent size and age in the same climate zone, they propose to collaborate on a study of nutrient cycling and carbon sequestration in these test forests if DOE funding is available. They will also try to help each other understand the variability in the results from the Oak Ridge and Duke experiments.

Beginning of Article

Related Web sites

ORNL's Environmental Sciences Division
National Environmental Research Park

Building Energy Use and Carbon Management Table of Contents Search the ORNL Review Site Comments to Editor ORNL Review Home Page ORNL Home Page