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This study presents and discusses the result of research on the chemical composition of bottom sediments of throughflow lakes located in Drawieński National Park. Basic hydrochemical indicators of the studied sediments are discussed: total organic carbon (Corg), total nitrogen (Ntot), and the C_org/N_tot ratio, which shows the rate of organic matter mineralization. The research and the analysis of the results show that the quality of the studied sediments changed with their distribution in the lake basin. The highest C_org and N_tot values were noted in sediments accumulated in the maximum depth of each lake, and at the inflow and outflow from the first lake in the whole cascade of throughflow lakes. Low C_org/N_tot ratios indicate that most of the sedimentary organic matter in the throughflow lakes comes from aquatic organism production, but the small participation of land-plant organic matter delivered to the lakes is also shown.
Słowa kluczowe
Czasopismo
Rocznik
Tom
Strony
69--76
Opis fizyczny
bibliogr. 11 poz., tab., wykr.
Twórcy
autor
autor
autor
- West Pomeranian University in Szczecin, Department of Physics ul. Papieża Pawła VI 3, 71-459 Szczecin, Poland, lilla.mielnik@zut.edu.pl
Bibliografia
- 1.Kamaleldin M.H., Swinehart J.B., Spalding R.F., 1997, Evidence for Holocene environmental change from C/N ratios, and δ13C and δ15N values in Swan Lake sediments, western Sand Hills, Nebraska, Journal of Paleolimnology, 18: 121-30
- 2.Meyers P.A., Ishiwatari R., 1993, Lacustrine organic geochemistry - an overview of indicators of organic matter sources and diagenesis in lake sediments, Organic Geochemistry, 20: 867-00
- 3.Meyers P.A, 1997, Organic geochemical proxies of paleooceanographic, paleolimnologic, and paleoclimatic processes, Organic Geochemistry, 27(5): 213-50
- 4.Meyers P.A., Lallier-Vergès E., 1999, Lacustrine sedimentary organic matter records of Late Quaternary paleoclimates, Journal of Paleolimnology, 21: 345-72
- 5.Meyers P.A., 2003, Applications of organic geochemistry to paleolimnological reconstructions: a summary of examples from the Laurentian Great Lakes, Organic Geochemistry, 34: 261-89
- 6.Mielnik L., 2005, Influence of the drainage basin on physical and chemical properties of bottom sediments of lakes, Inżynieria Rolnicza 4(64), 31-36
- 7.L. Mielnik, R. Piotrowicz, P. Klimaszyk Piotrowicz R., Klimaszyk P., Kraska M, 1998, Results of the physico-chemical research on waters of lakes and rivers in Drawieński National Park on the basis of the analysis performed within spring and summer stagnation in 1997, pp. 189, Poznań, (in Polish)
- 8.Piotrowicz R., Kraska M., Klimaszyk P., Szyper H., Joniak T., 2006, Vegetation Richness and Nutrient Loads in 16 Lakes of Drawienski National Park (Northern Poland). Polish J. of Environ. Stud., 15(3): 467-78
- 9.Routh J., McDonald T.J., Grossman E.L., 1999, Sedimentary organic matter sources and depositional environment in the Yegua formation (Brazos County, Texas), Organic Geochemistry, 30: 1437-53
- 10.Szyper H., Kraska M., 1999, Assessment of interaction between the drainage basin and the resistance to degradation of 16 lakes in Drawieński National Park, Poznań, pp. 29, (in Polish)
- 11.Twichell S.C., Meyers P.A., 2002, Significance of high C/N ratios in organic-carbon-rich Neogene sediments under the Benguela Current upwelling system, Organic Geochemistry, 33: 715-22
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BUS8-0001-0024