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Carbon and Nitrogen Pools in a Tallgrass Prairie Soil under Elevated Carbon Dioxide
Author(s) -
Williams M. A.,
Rice C. W.,
Omay A.,
Owensby C.
Publication year - 2004
Publication title -
soil science society of america journal
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.836
H-Index - 168
eISSN - 1435-0661
pISSN - 0361-5995
DOI - 10.2136/sssaj2004.1480
Subject(s) - carbon dioxide , mineralization (soil science) , soil water , nitrogen , soil carbon , chemistry , zoology , incubation , environmental chemistry , agronomy , environmental science , soil science , biology , biochemistry , organic chemistry
Soil is a potential C sink and could offset rising atmospheric CO 2 The capacity of soils to store and sequester C will depend on the rate of C inputs from plant productivity relative to C exports controlled by microbial decomposition. Our objective was to measure pools of soil C and N to assess the potential for C accrual and changes to N stocks as influenced by elevated atmospheric CO 2 Treatments (three replications, randomized complete block design) were ambient CO 2 —no chamber (NC), ambient CO 2 —chamber (AC), and two times ambient CO 2 —chamber (EC). Long‐term (290 d) incubations (35°C) were conducted to assess changes in the slow soil fractions of potentially mineralizable C (PMC) and potentially mineralizable N (PMN). Potentially mineralizable C was enhanced ( P < 0.1) by 19 and 24% in EC relative to AC and NC soil at the 0‐ to 5‐ and 5‐ to 15‐cm depths, respectively. Potentially mineralizable N was significantly greater by 14% at the 0‐ to 5‐cm depth in EC relative to AC, but decreased by 12% in EC relative to NC ( P < 0.1). Measurements of PMC indicate that increases in total soil C under elevated CO 2 in a previous study were a consequence of accrual into the slow pool. Relatively large amounts of new C deposited as a result of elevated CO 2 (C new ) remained in the soil after the 290‐d incubation. In contrast to accumulation of C into the slow fraction, C new was integrated into a passive fraction of soil organic matter (SOM). Accumulation of N was also detected in the whole soil, which cannot be explained by current estimates of ecosystem N flux.