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Phosphorus in interstitial water: methods and dynamics
Interstitial (pore) water is important for phosphorus dynamics in limnic ecosystems. This review summarizes the most important processes influencing the generation and transport of pore-water P from, to and within the sediment. Sampling methodology is discussed thoroughly in combination with what li...
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Published in: | Hydrobiologia 1988-12, Vol.170 (1), p.103-132 |
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Main Authors: | , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
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Summary: | Interstitial (pore) water is important for phosphorus dynamics in limnic ecosystems. This review summarizes the most important processes influencing the generation and transport of pore-water P from, to and within the sediment. Sampling methodology is discussed thoroughly in combination with what little information is available on various P species in the pore water. Pore water P concentrations in various trophic systems and the spatial and temporal distributions are also described. The last sections of the article deal with diffusive P flux calculations and comparison with measured P fluxes. Factors influencing P fluxes, such as adsorption, possible precipitation mechanisms, advection and bioturbation, are discussed. The general conclusion drawn from this review is that pore-water P investigations (concentrations and gradients) are an underestimated ecological tool in studying and describing trophic status, redox conditions, spatial and temporal distribution of P-sediment release, potential precipitation mechanisms on a long-term basis and ground-water inflow areas, as well as lake-water seepage. (DBO) |
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ISSN: | 0018-8158 1573-5117 |
DOI: | 10.1007/BF00024901 |