Relationships between cellulose decomposition, Jenny's k, forest-floor nitrogen, and soil temperature in Alaskan taiga forests

• Published in: Canadian Journal of Forest Research
• Main Authors: Fox, J.F., Van Cleve, K.
• Format: Text
• Language: unknown
• Published: Hosted by Utah State University Libraries 1983
• Subjects: Microorganisms; Tracheophyta: Plantae; Coniferopsida: Gymnospermae; Spermatophyta; Plantae; Betulaceae: Dicotyledones; Angiospermae; Salicaceae: Dicotyledones; Angiosperms; Dicots; Gymnosperms; Plants; Spermatophytes; Vascular Plants; Picea Glauca Picea Muriana Betula Papyrifera Populus Tremuloides Populus Balsamifera; Forest litter; decomposition; chemistry; Soil physics; temperature; Soil morphological features; soil temperature; Forest Sciences; taiga
• Online Access: https://digitalcommons.usu.edu/aspen_bib/4176; https://doi.org/10.1139/x83-109

Forest-floor decomposition is compared among 16 Alaskan taiga forest stands. These include black spruce (Piceamariana (Mill.) B.S.P.), white spruce (Piceaglauca (Moench) Voss), and birch (Betulapapyrifera Marsh.), aspen {Populustremuloides Michx.), and balsam poplar (Populusbalsamifera L.) types, spanning a wide range in decomposition rates, forest-floor microclimates, and litter quality. Jenny's index of decomposition rate, k, is reasonably well correlated with annual cellulose (filter-paper) decomposition differences among stands. Both estimates of decomposition rate are correlated with forest-floor heat sum and forest-floor nitrogen concentration. These between-site correlations support inferences based upon experimental work claiming that temperature and forest-floor chemical quality have a major influence upon the level of decomposition in a particular stand. Inferences about the factors regulating decomposition rate around an average level within one stand cannot legitimately be made from the same correlations. Moisture has not been considered in this analysis, but could also be important to between-stand differences in decomposition rate.