Cycling and retention of nitrogen and phosphorus in wetlands: a theoretical and applied perspective
- 1 August 1985
- journal article
- Published by Wiley in Freshwater Biology
- Vol. 15 (4) , 391-431
- https://doi.org/10.1111/j.1365-2427.1985.tb00212.x
Abstract
SUMMARY. This review considers the internal fluxes and transformations of nitrogen and phosphorus in wetland ecosystems. Emphasis is placed on the dynamic nature of nutrient cycling and the review is slanted towards an applied perspective, namely the possible use of wetlands as sinks for unwanted nutrients. A number of basic concepts pertaining to wetland ecosystems are first explained. These are: successional time scales, exchange equilibria and the concepts of storage and through flow, resource consumption and supply including the ideas of new and regenerated nutrients and the nutrient spiralling concept. Much of the following review material is referenced back to these concepts. Descriptions of the basic pathways of nutrients through different types of wetland systems are given with the emphasis placed on the movement into and out of the major storage compartments of wetland systems. The problems of conversion of qualitative information (or data in concentration units) on nutrient movements and transformations, into data on mass flows are then discussed. The importance of understanding groundwater, evapotranspiration processes and the effects of floods and seasonality on mass flow calculations can be significant. Unidentified groundwater sources can dilute nutrient concentrations, and evapotranspiration can increase concentrations. The pattern of through flow can also alter nutrient levels. Increasing residence time has the effect of decreasing nutrients in the wetland outflow. The review then considers the effects of adding nutrients to wetlands. The concept of the loading capacity is discussed in relation to the length of time a wetland can continue to remove nutrients from through flow. Sediment accumulation and degassing are seen as the major long‐term nutrient sinks. Nutrient enrichment results in biological changes to wetlands. These involve both changes in species composition and productivity. Not all are deleterious. The literature indicates that natural wetlands are not particularly effective as nutrient sinks when compared with conventional stripping plants but their value lies in removal of diffuse nutrient runoff at low concentrations. Dealing with this type of runoff by conventional means is not generally feasible. Recent studies show that artificially created wetlands can he effective systems for nutrient (particularly N) removal only if their internal removed mechanisms are understood and if these are optimized by management techniques.Keywords
This publication has 121 references indexed in Scilit:
- Tidal exchange of nitrogen and phosphorus between a mesohaline vegetated marsh and the surrounding estuary in the lower Chesapeake BayEstuarine, Coastal and Shelf Science, 1983
- Nitrogen Fixation Activity (Acetylene Reduction) in the Rhizosphere of Salt Marsh Angiosperms, Georgia, U.S.A.Botanica Marina, 1983
- Wastewater effects on a waterhyacinth marsh and adjacent impoundmentEnvironmental Management, 1981
- Effects of floods on nutrient and metal concentrations in a coastal plain streamWater Resources Research, 1981
- Impact of nutrient enrichment in a waterchestnut ecosystem at Takahama-iri Bay of Lake Kasumigaura, JapanWater, Air, & Soil Pollution, 1979
- Simulation of interrelations of the Everglades' marsh, peat, fire, water and phosphorusEcological Modelling, 1976
- The evaporation from a swampAgricultural Meteorology, 1970
- Input and Output of Minerals for a Small Watercress Bed Fed by Chalk WaterJournal of Applied Ecology, 1970
- Evaporation from a papyrus swampQuarterly Journal of the Royal Meteorological Society, 1969
- The Development of Peat LandsThe Quarterly Review of Biology, 1957