|
|
||||||||
University of Florida, Inst. of Food and Agric. Sci., Soil and Water Sci. Dep., 106 Newell Hall, Gainesville, FL 32611.
* Corresponding author.
ABSTRACT
Constructed marshes are currently being used as a low-cost alternative for treatment of nutrient-enriched waters. These marshes may function as net sinks for nutrients, especially for particulate organic forms of N and P. However, decomposition of organic matter and nutrient release may influence the ability of the marsh to function for this purpose. One of the main factors affecting decomposition is the availability of inorganic electron acceptors (e.g., O2, NO–3, and SO2–4). The role of electron acceptor consumption on N and P regeneration and release was investigated using batch incubation experiments with recently deposited organic matter (floc sediment) and peat soils collected from the constructed marsh. In electron acceptor-amended soil cores, electron acceptor consumption proceeded rapidly in the order O2 > NO–3 > SO2–4. Mean oxygen reduction rate (OR) was 1.6 g O2 m–2 d–1 (2025 g O2 m–3 d–1), with corresponding values for NO–3 and SO2–4 of 0.23 g N m–2 d–1 (60 g N m–3 d–1) and 0.086 g S m–2 d–1 (5.4 g S m–3 d–1), respectively. If electron acceptor consumption was coupled to decomposition of organic matter in floc sediment with a C/N/P ratio of 190:14:1, aerobic catabolism accounted for 92% of NH+4, and soluble P regenerated in the soil, with anaerobic activity (NO–3- and SO2–4-reduction) accounting for the remaining 8%. In the constructed marsh receiving allochthonous inputs of labile organic matter, however, anaerobic decomposition was expected to be the dominant mechanism for nutrient regeneration. Under SO2–4-reducing conditions, net rates of organic N and P mineralization were 3.3 to 14 mg N L–1 sediment d–1 and 0.5 to 0.6 mg P L–1, respectively, and were highly correlated to production of dissolved inorganic C plus CH4-C. Once released to the soil porewater, nutrients were available for transport to the water column by diffusion and advection (e.g., gas ebullition), thus impacting water quality.
Florida Agric. Exp. Stn. Journal Ser. no. R-03655.
Received for publication July 13, 1993.
This article has been cited by other articles:
![]() |
R. Corstanje and K. R. Reddy Response of Biogeochemical Indicators to a Drawdown and Subsequent Reflood J. Environ. Qual., November 1, 2004; 33(6): 2357 - 2366. [Abstract] [Full Text] [PDF] |
||||
![]() |
J. P. Prenger and K. R. Reddy Microbial Enzyme Activities in a Freshwater Marsh after Cessation of Nutrient Loading Soil Sci. Soc. Am. J., September 1, 2004; 68(5): 1796 - 1804. [Abstract] [Full Text] [PDF] |
||||
![]() |
L. M. Malecki, J. R. White, and K. R. Reddy Nitrogen and Phosphorus Flux Rates from Sediment in the Lower St. Johns River Estuary J. Environ. Qual., July 1, 2004; 33(4): 1545 - 1555. [Abstract] [Full Text] [PDF] |
||||
![]() |
A. L. Wright and K. R. Reddy Heterotrophic Microbial Activity in Northern Everglades Wetland Soils Soil Sci. Soc. Am. J., November 1, 2001; 65(6): 1856 - 1864. [Abstract] [Full Text] [PDF] |
||||
![]() |
M.M. Fisher and K.R. Reddy Phosphorus Flux from Wetland Soils Affected by Long-Term Nutrient Loading J. Environ. Qual., January 1, 2001; 30(1): 261 - 271. [Abstract] [Full Text] |
||||
![]() |
T. E. Davidsson and M. Ståhl The Influence of Organic Carbon on Nitrogen Transformations in Five Wetland Soils Soil Sci. Soc. Am. J., May 1, 2000; 64(3): 1129 - 1136. [Abstract] [Full Text] |
||||
| HOME | HELP | FEEDBACK | SUBSCRIPTIONS | ARCHIVE | SEARCH | TABLE OF CONTENTS |
| The SCI Journals | Agronomy Journal | Crop Science | |||
| Vadose Zone Journal | Journal of Plant Registrations | ||||
| Journal of Natural Resources and Life Sciences Education |
Soil Science Society of America Journal |