Above- and belowground ecosystem biomass and carbon pools in an age-sequence of temperate pine plantation forests

作者：Peichl Matthias; Arain A Altaf^*

来源：Agricultural and Forest Meteorology, 2006, 140(1-4): 51-63.

DOI：10.1016/j.agrformet.2006.08.004

• biomass
• carbon stock
• carbon sequestration
• afforestation
• plantation
• White pine
• chronosequence
• temperate conifer forest
• Great Lakes Region

We assessed the successional development of above- and belowground ecosystem biomass and carbon (C) pools in an age-sequence of four White pine (Pinus strobus L.) plantation stands (2-, 15-, 30-, and 65-years-old) in Southern Ontario, Canada. Biomass and C stocks of above- and belowground live and dead tree biomass, understorey and forest ground vegetation, forest floor C (LFH-layer), and woody debris were determined from plot-level inventories and destructive tree sampling. Small root biomass (< 5 mm) and mineral soil C stocks were estimated from soil cores. Aboveground tree biomass became the major ecosystem C pool with increasing age, reaching 0.5, 66, 92, and 176 t ha(-1) in the 2, 15-, 30, and 65-year-old stands, respectively. Tree root biomass increased from 0. 1 to 10, 18, 38 t ha(-1) in the 2-, 15, 30-, and 65-year-old stands, respectively, contributing considerably to the total ecosystem C in the three older stands. Forest floor C was 0.8, 7.5, 5.4, and 12.1 t C ha(-1) in the 2, 15-, 30-, and 65-year-old stands, respectively, indicating an increase during the first two decades, but no further age-effect during the later growth phase. Mineral soil C was age-independent with 37.2, 33.9, 39.1, and 36.7 t C ha(-1) in the 2-, 15-, 30-, and 65-year-old stands, respectively. Aboveground ecosystem C increased with age from 3 to 40, 52, and 100 t C ha(-1) in the 2-, 15-, 30-, and 65-year-old stands, respectively, due to an increase in aboveground tree biomass. Belowground ecosystem C remained similiar in the early decades after establishment with 37, 39, and 39 t C ha(-1) in the 2-, 15-, and 30-year-old stands, but increased to 56 t C ha(-1) in the 65-year-old stand due to an increase in root biomass. The difference in total ecosystem C between the 2- and 65-year-old stand was 116 t C ha(-1). Our results highlight the importance of considering the successional development of forest ecosystem C pools, when estimating C sink potentials over their complete life cycle.

• 出版日期2006-11-30