Changes in petiole hydraulic properties and leaf water flow in birch and oak saplings in a CO2-enriched atmosphere.

Water relations in woody species are intimately related to xylem hydraulic properties. High CO(2) concentrations ([CO(2)]) generally decrease transpiration and stomatal conductance (g(s)), but there is little information about the effect of atmospheric [CO(2)] on xylem hydraulic properties. To determine the relationship between water flow and hydraulic structure at high [CO(2)], we investigated responses of sun and shade leaves of 4-year-old saplings of diffuse-porous Betula maximowicziana Regel and ring-porous Quercus mongolica Fisch. ex Ledeb. ssp. crispula (Blume) Menitsky grown on fertile brown forest soil or infertile volcanic ash soil and exposed to 500 micromol CO(2) mol(-1) for 3 years. Regardless of species and soil type, elevated [CO(2)] consistently decreased water flow (i.e., g(s) and leaf-specific hydraulic conductivity) and total vessel area of the petiole in sun leaves; however, it had no effect on these parameters in shade leaves, perhaps because g(s) of shade leaves was already low. Changes in water flow at elevated [CO(2)] were associated with changes in petiole hydraulic properties.

Accurate estimation of nitrogen concentration in deciduous tree leaves in a field study using a portable non-destructive nitrogen detector.

A non-destructive nitrogen (N) detector [Agriexpert PPW-3000 (PPW-3000)] is a useful device for rapid and non-destructive measurement of leaf N content. However, some studies find a poor correlation between the PPW-3000 reading and the actual leaf N content; the R2 value of the approximate equation was low. To improve the accuracy of N estimation, we determined the approximate equation taking into account the leaf development stage (maturing and mature leaves) and leaf flush type (early and late leaves). For the leaf development stage, we determined approximate equations for maturing leaves (Ya), mature leaves (Yb), and "maturing+mature" leaves (Yc) in species having simultaneous leaf emergence. The resulting accuracy of Ya, Yb, and Yc was quite high. For leaf flush species, we determined approximate equations for early leaves (Y1), late leaves (Y2), and "early+late" leaves (Y3) in species having heterophyllous leaf emergence. The accuracy of Y1 and Y2 was relatively high, but that of Y3 was low. We conclude that, when using a PPW-3000, we can determine an approximate equation for maturing and mature leaves jointly, but should treat early and late leaves separately.