© 1996 Heron Publishing—Victoria, Canada
Seasonal root distribution and soil surface carbon fluxes for one-year-old Pinus radiata trees growing at ambient and elevated carbon dioxide concentration
Stephen M. Thomas (1), David Whitehead (2, 3), John A. Adams (1), Jeff B. Reid (4), Robert R. Sherlock (1) and Alan C. Leckie (2)
1. Department of Soil Science, Lincoln University, P.O. Box 84, Canterbury, New Zealand / 2. New Zealand Forest Research Institute, University of Canterbury, Private Bag 4800, Christchurch, New Zealand / 3. Manaaki Whenua Landcare Research, P.O. Box 69, Lincoln 8152, New Zealand / 4. New Zealand Institute for Crop and Food Research Ltd., P.O. Box 85, Hastings, New Zealand / Received October 25, 1995
Summary
The increase in number of fine (< 0.5 mm diameter) roots of one-year-old clonal Pinus radiata D. Don trees grown in large open-top field chambers at ambient (362 µmol mol–1) or elevated (654 µmol mol–1) CO2 concentration was estimated using minirhizotron tubes placed horizontally at a depth of 0.3 m. The trees were well supplied
with water and nutrients. Destructive harvesting of roots along an additional tube showed that there was a linear relationship
between root number estimated from the minirhizotron and both root length density, Lv, and root carbon density, Cv, in the surrounding soil.
Root distribution decreased with horizontal distance from the tree. At a depth of 0.3 m, 88% of the total Cv was concentrated within a 0.15-m radius from tree stems in the elevated CO2 treatment, compared with 35% for trees in the ambient CO2 treatment. Mean Cv along the tubes ranged up to 5 × 10–2 µg mm–3 and tended to be greater for trees grown at elevated CO2 concentration, although the differences between CO2 treatments were not significant. Root growth started in spring and continued until late summer. There was no significant
difference in seasonal rates of increase in Cv between treatments, but roots were observed four weeks earlier in the elevated CO2 treatment. No root turnover occurred at a depth of 0.3 m during the first year after planting.
Mean values of carbon dioxide flux density at the soil surface, F, increased from 0.02 to 0.13 g m–2 h–1 during the year, and F was 30% greater for trees grown at elevated CO2 concentration than at ambient CO2. Diurnal changes in F were related to air temperature. The seasonal increase in F continued through the summer and early autumn, well after air temperature had begun to decline, suggesting that the increase
was partly caused by increase in Cv as the roots colonized the soil profile.
Keywords:
fine roots, minirhizotron, root carbon density, root length density.
