|Title||Fine root respiration in northern hardwood forests in relation to temperature and nitrogen availability|
|Publication Type||Journal Article|
|Year of Publication||1996|
|Authors||Zogg GP, Zak DR, Burton AJames, Pregitzer KS|
We examined fine-root (< 2.0 mm diameter) respiration throughout one growing season in four northern hardwood stands dominated by sugar maple (Acer saccharum Marsh.), located along soil temperature and nitrogen (N) availability gradients. In each stand, we fertilized three 50x50 m plots with 30 kg NO3-N/ha/yr and an additional three plots received no N and served as controls. We predicted that root respiration rates would increase with increasing soil temperature and N availability. We reasoned that respiration would be greater for trees using NO3- as an N source than for trees using NH4+ as a N source because of the greater carbon (C) costs assocaited with NO3- versus NH4+ uptake and assimilation. Within stands, seasonal patterns of fine-root respiration rates followed temporal changes in soil temperature, ranging from a low of 2.1 umol O2/kg/s at 6C to a high of 7.0 umol O2 /kg/s at 18C. Differences in respiration rates among stands at a given soil temperature were related to variability in total net N mineralized (48-90 ug N/g) throughout the growing season and associated changes in mean root tissue N concentration (1.18-1.36 mol N/kg). The hypothesized increases in respiration in response to NO3- fertilization were not observed. The best-fit model describing patterns within and among stands had root respiration rates increasing exponentially with soil temperature and increasing linearly with increasing tissue N concentration: R= 1.347Ne0.072t (r2=0.63, P<0.01), where R is root respiration rate (umol O2/kg/s), N is root tissue N concentration (mol N/kg), and T is soil temperature (C). We conclude that, in northern hardwood forests domianted by sugar maple, root respiration is responsive to changes in both soil temperature and N availability, and that both factors should be considered in models of forest C dynamics.