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Abstract
Clinton and Vose measured seasonal fine root respiration rate in situ while controlling chamber temperature and [CO
2]. Atmospheric and [CO
2] ([CO
2]
a) and measured soil [CO
2] ([CO
2]
s) were alternately delivered to a cuvette containing intact fine roots of eastern white pine (
Pinus strobus L.). Respiration rates were consistently higher in [CO
2] [CO
2]
a than in [CO
2]
s, and were almost three times higher during midsummer. Respiration rates were immediately reversed after returning to the alternate [CO
2] (i.e., [CO
2]
a ® [CO
2]
s ® [CO
2]
a, and vice versa) suggesting a direct effect of elevated [CO
2] on apparent respiration. Soil[CO
2] -based respiration rates decreased with increasing [CO
2] on a dry mass and tissue [N] basis. The authors conclude that estimates of soil CO
2 flux and soil carbon budgets may be improved by more completely accounting for the rhizosphere microclimate (i.e., soil temperature and [CO
2]
s) during measurement of fine root respiration.
Citation
Clinton, Barton D.; Vose, James M. 1999. Fine root respiration in mature eastern white pine (
Pinus strobus) in situ: the importance of CO
2 in controlled environments. Tree Physiology. 19: 475-479.