Abstract
Forest floor CO2 efflux (FFcer) is an important component of global carbon budgets. FFcer exhibited a distinct seasonal trend following patterns of soil temperature, but soil water content and the volume percent of the soil's coarse fraction were also correlated with observed rates. Over the entire measurement period, FFcer ranged from a typical minimum of 0.8 μmol m-2 s-1 to an average maximum near 5.7 μmol m-2 s-1. No significant differences in FFcer were observed among the ridge-top and slope positions, but FFcer in the valley-bottom locations was lower on several occasions. An empirical model of FFcer based on these observations is suggested for application to whole-stand estimates of forest carbon sequestration. -from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 1-15 |
| Number of pages | 15 |
| Journal | Tree Physiology |
| Volume | 13 |
| Issue number | 1 |
| DOIs | |
| State | Published - 1993 |