1. How Much Soil Carbon is Derived from Woody Detritus? A Ten-Year Study of 13C Incorporation into Soil Organic Matter.
- Author
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Fahey, Timothy J., Heinz, Alexis K., Mathisson, Rachel, Fahey, Catherine, and Yavitt, Joseph B.
- Subjects
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SOIL structure , *FOREST soils , *TEMPERATE forests , *SUGAR maple , *CARBON in soils - Abstract
The importance of woody detritus as a source of soil organic matter is not well constrained. We quantified the recovery of 13C derived from isotopic-enriched sugar maple wood in various C fractions of two temperate forest soils in central New York, USA. Decay rates of small woody debris were quite rapid (k = 0.362 to 0.477 per year) and after 10 years less than 1% of the original wood mass remained in incubation bags. After six years we recovered only 0.26% (± 0.025) of the added 13C in the upper 5 cm of underlying soil. After 10 years this recovery declined to 0.11% (± 0.020) indicating substantial lability of retained SOC; most of this decline occurred from year 6 to 8 in the 1–5 cm depth increment, suggesting that the residue was quite stable at 10 years. The largest fraction of 13C was recovered in microaggregates (45%), especially those occluded within macroaggregates (30%), with a smaller proportion associated with the silt + clay fraction (20%). These proportions did not change significantly from year 6 to 10. Faster decay and higher 13C recovery were coincident with abundant saproxylic invertebrates from Scarabaeidae at one of the sites. We conclude that small woody debris is a minor source of stable SOC in these temperate forests (that is, less than 1% of annual SOC accumulation). [ABSTRACT FROM AUTHOR]
- Published
- 2024
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