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2012 | 60 | 4 |
Tytuł artykułu

Dynamics of phosphorus in lacustrine sediments: the process of uptake-release of dissolved phosphorus by sediments in different habitats and lakes

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Lake eutrophication and its consequences is still an important water quality problem being an effect of nutrient input to surface waters. In most lakes of the temperate zone, phosphorus is the nutrient responsible for eutrophication. Bottom sediments are the main pool involved in the retention and cycling of this element. Bottom sediments, depending on their chemical composition and aeration of the overlying water, may take up or release dissolved phosphorus i.e. the form easy utilizable by the plants. This study was aimed at comparing the exchange (uptake/release) of dissolved reactive phosphorus (DRP) in experiments that simulated natural conditions in various types of bottom sediments originating from different river-lake habitats typical of Masurian Lakeland (north-east Poland). Several river-lake systems typical for postglacial landscape were selected like river Jorka (15 km long, 5 lakes in cascade) and river Krutynia (~100 km long flowing through 17 lakes). Sediments used in experiments were taken from the littoral and profundal zones of four lakes (meso- meso-eu-, eutrophic and hypertrophic), from a humic lake and from ecotone zones at the land-water border and at the border between lake and river (from through-flow lakes). In total, 154 experiments were performed to assess the intensity of P exchange at a high (> 8 mg O2 L-1) and low (<2 mg O2 L-1) concentration of oxygen in water overlying undisturbed sediment cores. The following P fractions were isolated using the sequential extraction method and their importance was further analysed: easily exchangeable P (NH4Cl-RP – loosely bound, most available P; BD-RP – redox-dependent P associated with metal (Fe, Mn) hydroxides; NaOH-RP – phosphorus adsorbed mainly on metal (Fe, Al) oxides), hardly exchangeable P (BD-NRP – mainly organic P, whose stability depends on redox potential; NaOH-NRP – phosphorus in microorganisms, polyphosphates and part of organic P bound to detritus and humic substances) and non-exchangeable P (Hcl-P – phosphorus bound to carbonates, apatite-P and phosphorus released during total dissolution of metal oxides; P-residual – non-exchangeable P together with part of organic P). The effect of various factors (i.e. Fe, Mn, Mg, Al, Ca, organic matter, total P content and its fractions) on the intensity of DRP uptake/release was analysed with Pearson correlation and multiple regression. In sediments (both littoral and profundal) from lakes of the Jorka River trophic gradient, high oxygen conditions were always accompanied by P uptake (from –0.9 to –2.8 mg P m-2 d-1) while reduced oxygen concentrations were followed by DRP release (from 2.3 to 18.6 mg P m-2 d-1). These values were several dozen times higher than those noted for sediments from humic lake. Profundal sediments released more P than the littoral ones. In profundal sediments of all lakes of the Jorka River, the intensity of DRP release tooverlying water under reduced O2 concentrations was higher than the uptake rate under aerobic conditions. It means that DRP release prevailed over its uptake. Release rate of DRP tended to be higher from sediments of eutrophic and hypertrophic lakes than from those of meso- and mesoeutrophic lakes both in the two studied habitats (littoral, profundal) and seasons (spring and summer). Sediments of humic lake (from both littoral and profundal zones) showed a low dynamics of DRP uptake/release with a small prevalence of the latter (0.02 to 0.08 mg P m-2 d-1). River-lake-river sediments (from the inflows and outflows of the Krutynia River to a lake) were different in comparison with typical lake sediments – they released DRP to aerated overlying water in both meso- and meso-eutrophic lake. Phosphorus was released from in-shore bog sediments at reduced oxygen concentration in overlying water in both seasons (spring and summer) while under aerobic conditions DRP was weakly taken up and/or released. Fe, Mn, Mg, total P content and redox-dependent easily exchangeable BD-RP fraction had a significant effect on the intensity of P uptake at high concentration of oxygen and P release under reduced oxygen concentration (Pearson correlation, P <0.01). Factor analysis showed that at a high O2 concentration the intensity of DRP uptake by sediments was determined by redoxdependent fraction of P bound to Fe and Mn hydroxides (BD-RP) and the P fraction bound to carbonates and apatite (HCl-P) (r2 = 0.48). At reduced O2 concentration in overlying water the intensity of DRP release was affected by redox-dependent fraction of P associated with Fe and Mn hydroxides (BD-RP), P fraction bound to metal oxides (NaOH-RP), organic P in detritus, P in microorganisms and combined in humic substances (NaOH-NRP) and P fraction bound to carbonates and apatites (HCl-P) (r2 = 0.63). Sediments from eutrophic and hypertrophic lakes in the lower course of the Jorka River are most intensively eutrophicated. They showed the highest values of DRP release and the predominance of P release over P uptake was the highest (up to seven fold). Sediments of these lakes contained the highest amounts of redox-dependent elements – Fe and Mn. Hence, these lakes easily accumulate phosphorus at high concentrations of oxygen but equally easily release it when oxygen in water is depleted. More stable are meso- and meso-eutrophic lakes situated higher in the Jorka River system. Sediments of these lakes released smaller amounts of DRP than eutrophic and hypertrophic lakes and the prevalence of DRP release over uptake was threefold. In-shore bog sediments form a stable system when overlying waters are rich in oxygen. Under reduced oxygen concentrations, however, these habitats become an important P source (comparable with profun dal sediments) for lake littoral zone in case of theirclose contact with lake waters. A system able to bind phosphorus stronger and faster will hamper the delivery of available P to lake water and thus will delay lake eutrophication; that able to release P will accelerate eutrophication. In this case, internal loading may have a decisive effect on the lake trophic status. Profundal mid-lake sites, in-shore bogs and to a smaller extent littoral sediments (gyttja type) are the systems accelerating eutrophication. Humic lake sediments (dy type) are more equilibrated among the studied systems – the differences between uptake and release are small there.
Opis fizyczny
  • Centre for Ecological Research Polish Academy of Sciences, Dziekanow Lesny, Konopnickiej 1, 05–092 Lomianki, Poland
  • Andersen F.O. 1997 – Importance of benthic oxygen metabolism for the exchange of phosphatebetween sediment and water in the littoral zone of eutrophic lake – Verh. Internat. Verein. Limnol. 26: 289–293.
  • Andersen F.O., Ring P. 1999 – Comparison of phosphorus release from littoral and profundal sediments in a shallow, eutrophic lake – Hydrobiologia, 408/409: 175–183.
  • Arenas V., De La Lanza G. 1981 – The effect of dried and cracked sediment on availability of phosphorus in a coastal lagoon – Estuaries, 4: 206–212.
  • Bajkiewicz-Grabowska E., 1996 – Struktura fizycznogeograficzna obszaru drenowanego przez system rzeczno-jeziorny Krutyni (Pojezierze Mazurskie) [The physicogeographical structure of the area drained by the Krutynia river-lake system, Masurian Lakeland] (In: Funkcjonowanie systemow rzecznojeziornych w krajobrazie pojeziernym: rzeka Krutynia (Pojezierze Mazurskie) [Functioning of river-lake systems in a lakeland landscape: Krutynia River (Masurian Lakeland)], Eds: A. Hillbricht-Ilkowska, R.J. Wiśniewski) Zesz. Nauk. Kom. PAN, „Człowiek i Środowisko” 13: 21–34 (in Polish).
  • Borling K. 2003 – Phosphorus sorption, accumulation and leaching. Effects of long-term inorganic fertilization of cultivated soils – Ph.D. thesis, Swedish University of Agricultural Sciences, Uppsala, 39 pp.
  • Bostrom B. 1984 – Potential mobility of phosphorus in different types of lake sediments – Int. Rev. ges. Hydrobiol. 69: 457–474.
  • Caraco N.F., Cole J.J., Likens G.E. 1989 – Evidence for sulphate-controlled phosphorus release from sediments of aquatic systems – Nature, 341: 316–318.
  • Caraco N.F., Cole J.J., Likens G.E. 1992 – New and recycled primary production in an oligotrophic lake: Insights for summer phosphorus dynamics – Limnol. Oceanogr. 37: 590–602.
  • Carlyle G.C., Hill A.R. 2001 – Groundwater phosphate dynamics in a river riparian zone: effects of hydrologic flowpaths, lithology and redox chemistry – J. Hydrol. 247: 151–168.
  • Chapin III F.S., Barsdate R.J., Barel D. 1978 – Phosphorus cycling in Alaskan coastal tundra: a hypothesis for the regulation of nutrient cycling – Oikos, 31: 189–199.
  • Choiński A. 1991 – Katalog jezior Polski. Część pierwsza: Pojezierze Pomorskie [Polish lakes catalog. Part one: Pomeranian Lake District] – Wydawnictwo Naukowe UAM, 221 pp. (in Polish).
  • Christensen K.K. 1997 – Differences in iron, manganese, and phosphorus binding in fresh-water sediment vegetated with Littorella uniflora and bentic microalgae – Water, Air and Soil Pollution, 99: 265–273.
  • Clark M.W., Reddy K.R. 2002 – Contribution of internal phosphorus loads in south Florida water conservation area canal sediments – Wetland Biogeochemistry Laboratory, Soil and Water Science Department, Final Report. Attachment 2A, 135 pp.
  • Correll D.L. 1998 – The role of phosphorus in the eutrophication of receiving waters: A review – J. Environ. Qual. 27: 261–266.
  • D’Angelo E.M., Reddy K.R. 1994 – Diagenesis of organic matter in a wetland receiving hypereutrophic lake water: I. Distribution of dissolved nutrients in the soil and water column – J. Environ. Qual. 23: 928–936.
  • De Groot C.J., Golterman H.L. 1993 – On the presence of organic phosphatein some Camargue sediments: evidence for the importance of phytate – Hydrobiologia, 252: 105–116.
  • De Groot C.J., Van Wijck C. 1993 – The impact of desiccation of a freshwater marsh (Garines Nord, Camargue, France) on sedimentwater-vegetation interactions, Part 1 Sediment chemistry – Hydrobiologia, 252: 83–94.
  • de Haan H., Salonen K. 1990 – Abiotic transformations of iron and phosphate in humic lake water revealed by double-isotope labeling and gel filtration – Limnol. Oceanogr. 35: 491–497.
  • Evans D.J., Johnes P.J., Lawrence D.S. 2004 – Physico-chemical controls on phosphorus cycling in two lowland streams. Part 2 - The sediment phase – Science of the Total Environment, 329: 165–182.
  • Gachter R., Meyer S., Mares A. 1988 – Contribution of bacteria to release and fixation of phosphorus in lake sediments – Limnol. Oceanogr. 33: 1542–1558.
  • Gardolinski P.C.F.C., Worsfold P.J., McKelvie I.D. 2004 – Seawater induced release and transformation of organic and inorganic phosphorus from river sediments – Water Research, 38: 688–692.
  • Goedkoop W., Pettersson K. 2000 – Seasonal changes in sediment phosphorus forms in relation to sedimentation and benthic bacterial biomass in Lake Erken – Hydrobiologia, 431: 41–50.
  • Golterman H.L. 1997 – The distribution of phosphate over iron-bound and calciumbound phosphate in stratified sediments – Hydrobiologia, 364: 75–81.
  • Golterman H.L. 2001 – Phosphate release from anoxic sediments or ‘What did Mortimer really write?’ – Hydrobiologia, 450: 99–106.Golterman H.L. 2004 – The chemistry of phosphate and nitrogen compounds in sediments – Kluwer Academic Publisher, Dordecht, Boston, London, 251 pp.
  • Golterman H.L., Clymo R.S. 1978 – Methods for physical, chemical analysis of fresh waters. IBP Handbook No 8. – Blackwell Scientific Publications, Oxford, Edinburgh, London, Melbourne, 214 pp.
  • Golterman H.L., Paing J., Serrano L., Gomez E. 1998 – Presence of and phosphate release from polyphosphates or phytate phosphate in lake sediments – Hydrobiologia, 364: 99–104.
  • Gopal B., Hillbricht-Ilkowska A., Wetzel R.G. 1993 – Wetlands and ecotones. Studies on land-water interactions – National Institute of Ecology, New Delhi International scientific publications, New Delhi, 301 pp.
  • Gude H., Gries T. 1998 – Phosphorus fluxes in Lake Constance – Arch. Hydrobiol. Spec. Issues Advanc. Limnol. 53: 505–544.
  • Hadwen W.L., Arthington A.H., Mosisch T.D. 2003 – The impact of tourism on dune lakes on Fraser Island, Australia – Lakes & Reservoirs: Research and Management, 8: 15–26.
  • Haycock N.E., Burt T., Goulding K.W.T., Pinay G. 1996 – Buffer zones: their processes and potential in water protection. The proceedings of the internal conference on buffer zones – The proceedings of the International Conference on buffer zones, Quest Environmental, 326 pp.
  • Heidenreich M., Kleeberg A. 2003 – Phosphorus-binding in iron-rich sediments of a shallow Reservoir: spatial characterization based on sonar data – Hydrobiologia, 506/509: 147–153.
  • Hillbricht-Ilkowska A., Dusoge K., Ejsmont-Karabin J., Jasser I., Kufel I., Ozimek T., Rybak J.I., Rzepecki M., Węgleńska T. 1998 – Long term effects of liming in a humic lake – Pol. J. Ecol. 46: 347–415.
  • Hillbricht-Ilkowska A., Ryszkowski L.A., Sharpley A.N. 1995 – Phosphorus transfers and landscape structure: riparian sites and diversified land use patterns (In: Phosphorus in the global environment: transfer, cycles and management, Ed: H. Tiessen) – John Wiley and Sons Chichester, New York, Brisbane, Toronto, Singapore, pp. 202–229.
  • Hilbricht-Ilkowska A., Wiśniewski R.J. 1996 – Funkcjonowanie systemow rzecznojeziornych w krajobrazie pojeziernym: rzeka Krutynia (Pojezierze Mazurskie) [Functioning of river-lake systems in a lakeland land-scape: Krutynia River (Masurian Lakeland)] – Zeszyty Naukowe Komitetu „Człowiek i Środowisko” PAN, 13: 461 pp. (in Polish).
  • Horppila J., Nurminen L. 2001 – The effect of an emergent macrophyte (Typha angustifolia) on sediment resuspension in a shallow north temperate lake – Freshwater Biol. 46: 1447–1455.
  • House W.A., Denison F.H. 2002 – Total phosphorus content of river sediments in relationship to calcium, iron and organic matter concentrations – The Science of the Total Environment, 282/283: 341–351.
  • Hupfer M., Gachter R., Meyer J.S. 1995 – Poly-P in lake sediments, 31P NMR spectrometry as a tool for its identification – Limnol. Oceanogr. 40: 610–617.
  • Jensen H.S., Andersen F.O. 1992 – Importance of temperature, nitrate, and pH for phosphate release from aerobic sediments of four shallow, eutrophic lakes – Limnol. Oceanogr. 37: 577–589.
  • Jeppesen E., Jensen J.P., Sondergaard M., Mortensen E., Sortkjar O., Orlik K. 1990 – Fish manipulation as a lake restoration tool in shallow, eutrophic, temperate lakes 2: threshold levels, long-term stability and conclusions – Hydrobiologia, 200/201: 219–227.
  • Jeppesen E., Sondergaard M., Kronvang B., Jensen J.P., Svendsen L.M., Lauridsen T. 1999 – Lake and catchment management in Denmark – Hydrobiologia, 395/396: 419–432.
  • Jin X., Wang S., Pang Y., Zhao H., Zhou X. 2005 – The adsorption of phosphate on different trophic lake sediments – Colloids and Surfaces A: Physicochem. Eng. Aspects, 254: 241–248.
  • Kadlec R.H., Knight R.L. 1996 – Treatment Wetlands – CRC Press, Inc., Lewis Publishers: Boca Raton, New York, London, Tokyo. 893 pp.
  • Kairesalo T., Matilainen T. 1994 – Phosphorus fluctuation in water and deposition into sediment within an emergent macrophyte stand – Hydrobiologia, 275/276: 285–292.
  • Kaiserli A., Voutsa D., Samara C. 2002 – Phosphorus fractionation in lake sediments - Lakes Volvi and Koronia, N. Greece – Chemosphere, 46: 1147–1155.
  • Kankaala P., Ojala A., Tulonen T., Arvola L. 2002 – Changes in nutrient retention capacity of boreal aquatic ecosystems under climate warming: a simulation study – Hydrobiologia, 469: 67–76.
  • Kassila J., Hasnaoui M., Droussi M., Loudiki M., Yahyaoui A. 2001 – Relation between phosphate and organic matter in fish-pond sediments of the Deroua fish farm (Beni-Mellal, Morocco): implications for pond management – Hydrobiologia, 450: 57–70.
  • Khoshmanesh A., Hart B.T., Duncan A., Beckett R. 2002 – Luxury uptake of phosphorus by sediment bacteria – Water Research, 36: 774–778.
  • Kleeberg A., Jendritzki D., Nixdorf B. 1999 – Surficial sediment composition as a record of environmental changes in the catchment of shallow Lake Petersdorf, Brandenburg, Germany – Hydrobiologia, 408/409: 185–192.
  • Kloss M., Wilpiszewska I. 1985 – Vegetation of hollows without runoff in the Jorka river watershed – Pol. Ecol. Stud. 11: 209–214.
  • Kłosowski S., Tomaszewicz H. 1996 – Zbiorowiska roślinności brzegowej systemu rzeczno- jeziornego Krutyni [Communities of the shore vegetation of the Krutynia river-lake system] (In: Funkcjonowanie systemow rzecznojeziornych w krajobrazie pojeziernym: rzeka Krutynia (Pojezierze Mazurskie) [Functioning of river-lake systems in a lakeland landscape: Krutynia River (Masurian Lakeland)], Eds: A. Hillbricht-Ilkowska, R.J. Wiśniewski) – Zeszyty Naukowe Komitetu „Człowiek i Środowisko” PAN, 13: 346–376 (in Polish).
  • Lamers L.P.M., Tomassen H.B.M., Roelofs J.G.M. 1998a – Sulphate-induced eutrophication and phytotoxicity in freshwater wetlands – Environ. Sci. Technol. 32: 199–205.
  • Lamers L.P.M., Van Roozendaal S.M.E., Roelofs J.G.M. 1998b – Acidification of freshwater wetlands: combined effects of nonairborne sulfur pollution and desiccation – Water, Air and Soil Pollution, 105: 95–106.
  • Lewandowski K.B., 1996 – Bentos rzeczno-jeziorny stref przejściowych systemu rzeki Krutyni, Pojezierze Mazurskie [Benthos of river-lake transitional zones of the Krutynia River system, Masurian Lakeland] (In: Funkcjonowanie systemow rzeczno-jeziornych w krajobrazie pojeziernym: rzeka Krutynia (Pojezierze Mazurskie) [Functioning of river-lake systems in a lakeland landscape: Krutynia River (Masurian Lakeland)], Eds: A. Hillbricht-Ilkowska, R.J. Wiśniewski) – Zeszyty Naukowe Komitetu „Człowiek i Środowisko”PAN, 13: 303–312 (in Polish).
  • McDowell R.W., Sharpley A.N. 2003 – The uptake and release of phosphorus from overland low in a stream environment – J. Environ. Qual. 32: 937–948.
  • McDowell R.W., Sharpley A.N., Folmar G. 2003 – Modification of phosphorus exportfrom an eastern USA catchment by fluvial sediment and phosphorus inputs – Agriculture, Ecosystems and Environment, 99: 187–199.
  • Mitsch W.J. 1992 – Landscape design and the role created, restored, and natural riparian wetlands in controlling nonpoint source pollution – Ecological Engineering, 1: 27–47.
  • Moore B.C., Lafer J.E., Funk W.H. 1994 – Influence of aquatic macrophytes on phosphorus and sediment pore-water chemistry in a freshwater wetland – Aquat. Bot. 49: 137–148.
  • Mulholland P.J., Yarbro L.A., Sniffen R.P., Kuenzler E.J. 1981 – Effects of floods on nutrient and metal concentrations in a coastal plain stream – Wat. Res. Res. 17: 758–764.
  • Mulqueen J., Rodgers M., Scally P. 2004 – Phosphorus transfer from soil to surface waters – Agricultural Water Management, 68: 91–105.
  • Naiman R.J., Decamps H. 1990 – The ecology and management of aquatic-terrestrial ecotones – Man and The Biosphere Series, 4, 316 pp.
  • Nguyen L., Sukias J. 2002 – Phosphorus fractions and retention in drainage ditch sediments receiving surface runoff and subsurface drainage from agricultural catchments in the North Island, New Zealand – Agriculture, Ecosystems and Environment, 92: 49–69.
  • Nurnberg G.K. 1988 – Prediction of phosphorus release rates from total and reductant-soluble phosphorus in anoxic lake sediments – Can. J. Fisheries Aquat. Sci. 45: 453–462.
  • Nurnberg G.K., Dillon P.J., McQeen D.J. 1986 – Internal phosphorus load in an oligotrophic Precamrian Shield lake with an anoxic hypolimnion – Can. J. Fish. Aq. Sci. 43 (3): 574–580.
  • Nurnberg G.K., Peters R.H. 1984 – The importance of internal phosphorus load to eutrophication of lakes with anoxic hypolimnia – Ver. Internat. Verein. Limnol. 22: 190–194.
  • Ohle W. 1964 – Kolloidkomplexe als Kationenund Anionenaustauscher in Binnengewassern – Vom Wasser, 30: 50–64.
  • Ostrofsky M.L., Osborne D.A., Zebulske T.J. 1989 – Relationship between anaerobic sediment phosphorus release rates and sedimentary phosphorus species – Can. J. Fisheries Aquat. Sci. 46: 416–419.
  • Panigatti M.C., Maine M.A. 2002 – Phosphate dynamics in the Middle Paran´a wetlands using 32P isotopic technique – Hydrobiologia, 472: 45–51.
  • Petticrew E.L., Arocena J.M. 2001 – Evaluation of iron-phosphate as a source of internallake phosphorus loadings – The Science of the Total Environment, 266: 87–93.
  • Picard Ch.R., Fraser L.H., Steer D. 2005 – The interacting effects of temperature and plant community type on nutrient removal in wetland microcosms – Bioresource Technology, 96: 1039–1047.
  • Planter M., Wiśniewski R.J. 1985 – Factors affecting nutrient budget in lakes of the r. Jorka watershed (Masurian Lakeland, Poland). IX. The exchange of phosphorus between sediments and water – Ekol. Pol. 33: 329–344.
  • Psenner R. 1984 – Phosphorus release patterns from sediments of a meromictic mesotrophic lake (Piburger See, Austria) – Ver. Internat. Verein. Limnol. 22: 219–228.
  • Qiu S., McComb A.J. 1995 – The planktonic and microbial contributions to phosphorus release from fresh and air-dried sediments – Aust. J. Mar. Freshwat. Res. 46: 1039–1045.
  • Qiu S., McComb A.J. 2002 – Interrelations between iron extractability and phosphate sorption in reflooded air-dried sediments – Hydrobiologia, 472: 39–44.
  • Reddy K.R., D’Angelo E.M. 1994 – Soil processes regulating water quality in wetlands (In: Global Wetlands: Old World and New, Ed: W.J. Mitsch) – Elsevier, Amsterdam, Lausanne, New York, Oxford Shannon, Tokyo, 309–325.
  • Reynolds C.S., Davies P.S. 2001 – Sources and bioavailability of phosphorus fractions in freshwaters: a British perspective – Biol. Rev. 76: 27–64.
  • Roelofs J.G.M. 1991 – Inlet of alkaline river water into peaty lowlands: effects on water quality and Stratiotes aloides L. stands – Aquat. Bot. 39: 267–293.
  • Rzepecki M. 1997 – Sediments in a humic lake with artificially increased calcium content: sink or source for phosphorus? – Water, Air and Soil Pollution, 99: 457–464.
  • Rzepecki M. 2000 – Wetlands in lakes protection: nutrient dynamics and removal in ecotones of river-lake system (Masurian Lakeland, Poland) – Verh. Internat. Verein. Limnol. 27: 1685–1689.
  • Rzepecki M. 2002 – Wetland zones along lake shores as barrier systems: field and experimental research on nutrient retention and dynamics – Pol. J. Ecol. 50: 527–541.
  • Rzepecki M. 2010 – Dynamics of phosphorus in lacustrine sediments: contents and fractions in relation to lake trophic state and chemical composition of bottom deposits – Pol. J. Ecol. 58: 529–548.
  • Scheffer M., Hospper S.H., Meijer M.L., Moss B., Jeppesen E. 1993 – Alternativeequilibria in shallow lakes – Trends in Ecology and Evolution, 8: 275–279.
  • Schindler D.W. 1977 – Evolution of phosphorus limitation in lakes – Science, 195: 260–262.
  • Schindler D.W., Hesslein R., Kipphur G. 1977 – Interactions between sediments and overlying waters in an experimentally eutrophied Precambian Shield Lake (In: Interactions between sediments and freshwater, Ed: H.L. Golterman) – Dr. W. Junk, The Hague, pp. 235–243.
  • Seling U. 2003 – Particle size-related phosphate binding and P-release at the sediment–water interface in a shallow German lake – Hydrobiologia, 492: 107–118.
  • Seling U., Schlungbaum G. 2003 – Characterization and quantification of phosphorus release from profundal bottom sediments in two dimictic lakes during summer stratification – J. Limnol. 62: 151–162.
  • Sharpley A.N., Hedley M.J., Sibbesen E., Hillbricht-Ilkowska A., House W.A., Ryszkowski L. 1995 – Phosphorus transfer from terrestrial to aquatic ecosystems (In: Phosphorus in the global environment, transfers, cycles and management, Ed: H. Tiessen) – J. Wiley & Sons, pp. 171–199.
  • Sinke A., Cornelese A.A., Keizer P., Van Tongeren O.F.R., Cappenberg T.E. 1990 – Mineralization, pore water chemistry and phosphorus release from peaty sediments in the eutrophic Loosdrecht lakes, Netherlands – Freshwat. Biol. 23: 587–599.
  • Smith D.R., Haggard B.E., Warnemuende E.A., Huang C. 2005 – Sediment phosphorus dynamics for three tile fed drainage ditches in Northeast Indiana – Agricultural Water Management, 71: 19–32.
  • Sommers L.E., Harris R.F., Williams J.D.H., Armstrong D.E., Syers J.K. 1972 – Fractionation of organic phosphorus in lake sediment – Soil Sci. Soc. Am. Proc. 36: 51–54.
  • Sondergaard M., Jensen J.P., Jeppesen E. 2003 – Role of sediment and internal loading of phosphorus in shallow lakes – Hydrobiologia, 506/509: 135–145.
  • Suplee M.W., Cotner J.B. 2002 – An evaluation of the importance of sulfate reduction and temperature to P fluxes from aerobic-surfaced, lacustrine sediments – Biogeochemistry, 61: 199–228.
  • Turner B.L., Haygarth P. M. 2000 – Phosphorus Forms and Concentrations in Leachate under Four Grassland Soil Types – Soil Sci. Soc. Am. J. 64: 1090–1099.
  • Venterink H., Olde T., Davidsson E., Kiehl K., Leonardson L. 2002 – Impact of drying and re-wetting on N, P and K dynamics in a wetland – Plant & Soil, 243: 119–130.
  • Vought L.B.M., Dahl J., Pedersen L.C., Lacoursiere J.O. 1994 – Nutrient retention in riparian ecotones – Ambio, 23: 342–348.
  • Walbridge M.R. 1991 – Phosphorus availability in acid organic soils of the lower North Carolina coastal plain – Ecology, 72: 2083–2100.
  • Watts C.J. 2000a – Seasonal phosphorus release from exposed, re-inundated littoral sediments of two Australian reservoirs – Hydrobiologia, 431: 27–39.
  • Watts C.J. 2000b – The effect of organic matter on sedimentary phosphorus release in an Australian reservoir – Hydrobiologia, 431: 13–25.
  • Wauer G., Gonsiorczyk T., Kretschmer K., Casper P., Koschel R. 2005 – Sediment treatment with a nitrate-storing compound to reduce phosphorus release – Water Research, 39: 494–500.
  • Wetzel R.G. 2001 – Limnology. Lake and rivers ecosystems – Academic Press, San Diego, San Francisco, New York, Boston, London, Sydney, Tokio, Saunders College Publishing, 1006 pp.
  • Wiśniewski R.J., Rzepecki M. 1996 – Osady denne stref przejściowych rzeka-jezioro i jezioro-rzeka w systemie rzeczno-jeziornym Krutyni(Pojezierze Mazurskie); rola w krążeniu fosforu [Bottom sediments of the river-lake and lake river transition zones in the Krutynia fluvio-lacustrine system (Masurian Lakeland); the role in the phosphorus cycling] (In: Funkcjonowanie systemow rzeczno-jeziornych w krajobrazie pojeziernym: rzeka Krutynia (Pojezierze Mazurskie) [Functioning of river-lake systems in a lakeland landscape: Krutynia River (Masurian Lakeland)], Eds: A. Hillbricht-Ilkowska, R.J. Wiśniewski) – ZeszytyNaukowe Komitetu „Człowiek i Środowisko” PAN, 13: 313–345 (in Polish).
  • Zhou Q., Gibson C.E., Zhu Y. 2001 – Evaluation of phosphorus bioavailability in sediments of three contrasting lakes in China and the UK – Chemosphere, 42: 221–225.
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