TY - JOUR
T1 - Soil carbon and nitrogen cycling and storage throughout the soil profile in a sweetgum plantation after 11 years of CO 2-enrichment
AU - Iversen, Colleen M.
AU - Keller, Jason K.
AU - Garten, Charles T.
AU - Norby, Richard J.
PY - 2012/5
Y1 - 2012/5
N2 - Increased partitioning of carbon (C) to fine roots under elevated [CO 2], especially deep in the soil profile, could alter soil C and nitrogen (N) cycling in forests. After more than 11 years of free-air CO 2 enrichment in a Liquidambar styraciflua L. (sweetgum) plantation in Oak Ridge, TN, USA, greater inputs of fine roots resulted in the incorporation of new C (i.e., C with a depleted δ 13C) into root-derived particulate organic matter (POM) pools to 90-cm depth. Even though production in the sweetgum stand was limited by soil N availability, soil C and N contents were greater throughout the soil profile under elevated [CO 2] at the conclusion of the experiment. Greater C inputs from fine-root detritus under elevated [CO 2] did not result in increased net N immobilization or C mineralization rates in long-term laboratory incubations, possibly because microbial biomass was lower in the CO 2-enriched plots. Furthermore, the δ 13CO 2 of the C mineralized from the incubated soil closely tracked the δ 13C of the labile POM pool in the elevated [CO 2] treatment, especially in shallower soil, and did not indicate significant priming of the decomposition of pre-experiment soil organic matter (SOM). Although potential C mineralization rates were positively and linearly related to total SOM C content in the top 30 cm of soil, this relationship did not hold in deeper soil. Taken together with an increased mean residence time of C in deeper soil pools, these findings indicate that C inputs from relatively deep roots under elevated [CO 2] may increase the potential for long-term soil C storage. However, C in deeper soil is likely to take many years to accrue to a significant fraction of total soil C given relatively smaller root inputs at depth. Expanded representation of biogeochemical cycling throughout the soil profile may improve model projections of future forest responses to rising atmospheric [CO 2]. Published 2012 This article is a U.S. Government work and is in the public domain in the USA.
AB - Increased partitioning of carbon (C) to fine roots under elevated [CO 2], especially deep in the soil profile, could alter soil C and nitrogen (N) cycling in forests. After more than 11 years of free-air CO 2 enrichment in a Liquidambar styraciflua L. (sweetgum) plantation in Oak Ridge, TN, USA, greater inputs of fine roots resulted in the incorporation of new C (i.e., C with a depleted δ 13C) into root-derived particulate organic matter (POM) pools to 90-cm depth. Even though production in the sweetgum stand was limited by soil N availability, soil C and N contents were greater throughout the soil profile under elevated [CO 2] at the conclusion of the experiment. Greater C inputs from fine-root detritus under elevated [CO 2] did not result in increased net N immobilization or C mineralization rates in long-term laboratory incubations, possibly because microbial biomass was lower in the CO 2-enriched plots. Furthermore, the δ 13CO 2 of the C mineralized from the incubated soil closely tracked the δ 13C of the labile POM pool in the elevated [CO 2] treatment, especially in shallower soil, and did not indicate significant priming of the decomposition of pre-experiment soil organic matter (SOM). Although potential C mineralization rates were positively and linearly related to total SOM C content in the top 30 cm of soil, this relationship did not hold in deeper soil. Taken together with an increased mean residence time of C in deeper soil pools, these findings indicate that C inputs from relatively deep roots under elevated [CO 2] may increase the potential for long-term soil C storage. However, C in deeper soil is likely to take many years to accrue to a significant fraction of total soil C given relatively smaller root inputs at depth. Expanded representation of biogeochemical cycling throughout the soil profile may improve model projections of future forest responses to rising atmospheric [CO 2]. Published 2012 This article is a U.S. Government work and is in the public domain in the USA.
KW - C
KW - Carbon mineralization
KW - Elevated [CO ]
KW - Fine roots
KW - Liquidambar styraciflua
KW - Mineral-associated organic matter
KW - Net nitrogen mineralization
KW - Particulate organic matter
KW - Soil carbon
KW - Soil depth
UR - http://www.scopus.com/inward/record.url?scp=84859485210&partnerID=8YFLogxK
U2 - 10.1111/j.1365-2486.2012.02643.x
DO - 10.1111/j.1365-2486.2012.02643.x
M3 - Article
AN - SCOPUS:84859485210
SN - 1354-1013
VL - 18
SP - 1684
EP - 1697
JO - Global Change Biology
JF - Global Change Biology
IS - 5
ER -