Interdependence between phosphorus forms in sediments and iron in interstitial waters in the Gulf of Gdańsk

• Autorzy: Matuszewska K. , Białkowska I. , Bolałek J.
• Języki publikacji: EN

Abstrakty

EN

The content of various phosphorus forms in sediments and the content of iron in interstitial waters were measured in sediment samples collected in the Gulf of Gdańsk in March 2001. The studies showed that the greatest amounts of the total phosphorus and total dissolved iron were present in the uppermost sediment layer, and their respective concentrations ranged from 203.99 žmol g-1 d.w. to 1894.02 μmol g-1 d.w., and from 0.02 μmol dm-3 to 4.68 μmol dm-3. The contents of these parameters were directly connected with the type of sediment – the greatest concentrations were measured in fine sediments. The analysis of multiple correlation coefficients demonstrated that in over 90% of cases the concentration of phosphorus bound with iron depended on: the sediment type and its humidity, the content of organic matter, and the concentration of the total iron dissolved in the interstitial waters.

Słowa kluczowe

EN

phosphorus forms; iron; sediment type

• Wydawca: Institute of Oceanography University of Gdańsk
• Czasopismo: Oceanological and Hydrobiological Studies
• Rocznik: 2003
• Tom: Vol. 32, No. 1
• Strony: 5--14
• Opis fizyczny: Bibliogr. 27 poz., tab., wykr.

Twórcy

autor

Matuszewska K.

• University of Gdańsk, Instituteof Oceanography, Al. Marszałka Piłsudskiego 46, 81-378 Gdynia

autor

Białkowska I.

• University of Gdańsk, Instituteof Oceanography, Al. Marszałka Piłsudskiego 46, 81-378 Gdynia

autor

Bolałek J.

• University of Gdańsk, Instituteof Oceanography, Al. Marszałka Piłsudskiego 46, 81-378 Gdynia

Bibliografia

• [1]. Andrieux-Loyer F. and Aminot A., 2001, Phosphorus forms releated to sediment grain size and geochemical characteristics in French coastal areas, Estuarine, Coastal and Shelf Science, 52, 617-629.
• [2]. Andrulewicz E. and Witek Z., 2002, Anthropogenic pressure and environmemal effects on the Gulf of Gdansk: Recent Managment Efforts, [In]: G. Schernewski, U. Schiewer (eds.), Baltic Coastal Ecosystem, Springer, 119-139.
• [3]. Anshutz P., Zhong S. and Sundby B.,1998, Burial efficiency of phosphorus wid the geochemistry of iron in continental margin sediments, Limnol. Oceanogr., 43, 53-64.
• [4]. Białkowska I. and Bolałek J., 2000, Distribution of the Fe (II) and Fe (III) dissolved in the interstitial water of the Gulf of Gdańsk, Oceanological Studies, 29, 43-54.
• [5]. Chapelle F.H. and Lovley D.R., 1992, Competitive Exclusion of Sulfałe Reduction by Fe (III)-Reducting Bacteria, Ground Water, 30, 29-36.
• [6]. Coleman M.L., Hedrick D.B., Lovley D.R., White D.C. and Pye K., 1993. Reduction of Fe (III) in sediments by sulphate reducing bacteria, Nature, 361. 436-438.
• [7]. Falkowska L., Bolałek J. and Łysiak-Pastuszak E., 1999, Analiza chemiczna wody morskiej 2, Wydawnictwo Uniwersytetu Gdańskiego, 82p.
• [8]. Fleischer S., Bengtsson M. and Johansson G., 1988, Mechanism of the aerobic Fe(III) P solubilization at the sediment-water interface, Theoretical Applied Limnology, 23, 1825-1829.
• [9]. Gobler Ch. J., Donat J. R., Consolvo III J. A. and Safiudo-Wilhelmy S. A., 2002, Physicochemical speciation of iron during coastal algal blooms, Marine Chemistry, 77, 71-89.
• [10]. Golterman H.L., 1995, Theoretical aspects of the adsorption of ortho-phosphate onto iron-hydroxide, Hydrobiologia, 315, 59-68.
• [11]. Graca B. and Bolałek J., 2000, Temporal variations in phosphorus species in the surface layer of bottom sediments from the Gulf of Gdańsk - preliminary research, Oceanological Studies, 29, 55-66.
• [12]. Hay R.W., 1990, Chemia bio-nieorganiczna, Warszawa, Państwowe Wydawnictwo Naukowe, 256p.
• [13]. Jansson M., 1987, Anaerobie dissolution of iron-phosphorus complexes in sediment due to the activity of nitrate-reducnig bacteria, Microb. Ecol, 14, 81-89.
• [14]. Jensen H., S., Mortensen P., B., Andersen F., O., Rasmussen E. and Jensen A., 1995, Phosphorus cycling in a coastal marine sediment, Aarhus Bay, Denmark, Limnol. Oceanogr., 40, 908-917.
• [15]. Jensen H., S. and Thamdrup B., 1993, Iron-bound phosphorus in marine sediments as measured by bicarbonate-dithionite extraction, Hydrobiologia, 253, 47-59.
• [16]. Koch M., S., Benz R., E. and Rudnick D., T., 2001, Solid-phase phosphorus pools in highly organic carbonate sediments of northeastern Florida Bay, Estuarine, Coastal and Shelf Science, 52, 279-291.
• [17]. Koroleff F., 1976, Deterrnination of phosphorus, [In]: K. Grasshoff (red), Methods of seawater analysis, Verlag-Chimie, 117-122 .
• [18]. Lewin R., 1984, How microorganisms transport iron, Science 225, 401-402.
• [19]. Liu X. and Millero F. J., 2002, The solubiliry of iron in seawater, Marine Chemistry, 77, 43-54.
• [20]. Lovley D.R., Phillips E.J. and Lonergan D.J., 1991, Enzymatic versus Nonenzymatic Mechanisms for Fe (III) Reduction in Aquaqtic Sediments, Environ. Sci. Tech., 25, 1062-1067.
• [21]. Racinkowski R., 1973, Badanie współczesnych osadów morskich, [In]: E. Riihle (ed.), Metodyka badań osadów czwartorzędowych, 459-475, Wydawnictwa Geologiczne, Warszawa.
• [22]. Santana-Casiano J. M., Gonzffiez-Wvila M., Jesus-Rodriguez M. and Millero F. J., 2000, The effeet of organic compounds in the oxidation kinetics of Marine Chemistry, 70, 211-222.
• [23]. Slomp C. P., Van der Gaast S. J. and Van Raphorst W., 1995, Phosphorus Binding by Poorly Crystaline Iron Oxides in North Sea, Mar. Chem., 52. 55-73.
• [24]. Sundareshwar P., V. and Morris J., T., 1999, Phosphorus sorption characteristics of intertidal sediments along estuarine salinity gradient. Limnol. Oceanogr., 44, 1693-1701.
• [25]. Sundby B., Gobeil Ch., Silverberg N. and Mucci A., i in., 1992, The phosphorus tytle in coastal marine sediments, Limnol. Oceanogr., 37, 1129-1145.
• [26]. Williams J., D., H., Jaquet J-M. and Thomas R., L., 1976, Forms of phosphorus in the surficial sediments of Lake Erie, J. Fish. Res. Board Can., 33, 413.
• [27]. Yao W. and Millero J., 1995, Oxidation of Hydrogen Sulfide by Hydrous Fe(III) Oxides in Seawater, Mar. Chem., 52, 1-16.