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Journal of Environmental Quality 32:1365-1374 (2003)
© 2003 American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America

TECHNICAL REPORTS
Landscape and Watershed Processes

Dissolved Organic Carbon Dynamics in a Riparian Aquifer

Effects of Hydrology and Nitrate Enrichment

P.-A. Jacinthe*,a, P. M. Groffmanb and A. J. Goldc

a School of Natural Resources, 2021 Coffey Road, 210 Kottman Hall, Ohio State Univ., Columbus, OH 43210
b Inst. of Ecosystem Studies, Millbrook, NY 12545
c Dep. of Natural Resources Science, Univ. of Rhode Island, Kingston, RI 02881

* Corresponding author (jacinthe.1{at}osu.edu)

Received for publication May 10, 2002. The capacity of riparian soils to remove nitrate (NO-3) from ground water is well established, but the effects of ground water NO-3-enrichment on C dynamics are not well studied. We incubated horizontal cores of aquifer material extracted from beneath moderately well-drained (MWD) and poorly drained (PD) soils in a riparian forest in Rhode Island, USA for 132 d, and dosed (flow rate, 170 mL d-1; dissolved O2, 2 in PD and 5 mg L-1 in MWD cores) with ground water amended with either Br-, Br- + NO-3 (10 mg N L-1), or Br- + NO-3 + DOC (20 mg C L-1). The DOC was extracted from forest floor material and added during the first 56 d of the experiment. Addition of NO-3 had limited effect on CO2 production while DOC amendment had a significant effect in the PD but not in the MWD mesocosms. Total CO2 production (mg CO2–C kg-1 soil) was 6.3, 7.0, and 10.1 in the PD and 3.6, 4.0, and 4.5 in the MWD cores amended with Br-, Br- + NO-3, and Br- + NO-3 + DOC, respectively. Carbon balance (Cbal = DOCin - (DOCout + CO2–C) showed a net C retention of 8.0 mg C kg-1 soil in the DOC-amended MWD cores (equivalent to 50% of the DOC added), and a net C loss of 8.3 mg C kg-1 soil in similarly treated PD cores. The lack of C retention in the PD cores was ascribed to reductive dissolution of minerals implicated in DOC sorption. These findings underscore that there is marked variation in C dynamics in riparian aquifers that has the potential to influence the fate of NO3- and DOC in the landscape.

Abbreviations: DO, dissolved oxygen • DOC, dissolved organic carbon • DOCin, dissolved organic carbon in input solution • DOCout, dissolved organic carbon in core effluent • MBC, microbial biomass carbon • MWD, moderately well drained • PD, poorly drained • PDOM, patches of decomposed organic materials • SOC, soil organic carbon


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JEQ 2003 32: 1167-1172. [Full Text]  






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