کد مقاله | کد نشریه | سال انتشار | مقاله انگلیسی | نسخه تمام متن |
---|---|---|---|---|
5770474 | 1629411 | 2017 | 7 صفحه PDF | دانلود رایگان |
- Pyrogenic C stock in Amazon forest soils is estimated at 1.1 Pg (0.3Â m), 2.8 Pg (1Â m)
- Three samples per 1Â ha seem sufficient to capture spatial variability of pyrogenic C
- Pyrogenic C showed significant, large scale variability throughout the Amazon Basin
- Pyrogenic C represents up to on average 11% of total organic C
- Pyrogenic C is likely involved in millennial scale subsurface biogeochemical cycling
Amazon Basin forest soils contain considerable soil organic carbon stocks; however, the contribution of soil pyrogenic carbon (PyC) to the total is unknown. PyC is derived from local fires (historical and modern) and external inputs via aeolian deposition. To establish an initial estimate of PyC stocks in non-terra preta forest with no known history of fire, to assess site and vertical variability, as well as to determine optimal sampling design, we sampled 37 one hectare forest plots in the Amazon Basin and analysed PyC via hydrogen pyrolysis of three individual samples per plot and of bulked samples to 200Â cm depth. Using our data and published total organic carbon stocks, we present the first field-based estimate of total PyC stock for the Amazon Basin of 1.10 Pg over 0-30Â cm soil depth, and 2.76 Pg over 0-100Â cm soil depth. This is up to 20 times higher than previously assumed. Three individual samples per 1Â ha are sufficient to capture the site variability of PyC in our plots. PyC showed significant, large-scale variability among plots. To capture 50% of the PyC in 200Â cm soil profiles, soil must be sampled to a depth of at least 71Â cm. PyC represents a significant (11%) portion of total organic carbon in soil profiles 0-200Â cm depth. This finding highlights the potentially important role that historical fire has played in modifying soil C stocks. Our data suggest that PyC is an important carbon pool for long-term storage, involved in millennial scale biogeochemical cycling, particularly in the subsurface soil.
Journal: Geoderma - Volume 306, 15 November 2017, Pages 237-243