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Morphological and Physical Properties of Dehydrated Holocene Carbonate Limnic Deposits in Post-Bog Areas of NW Poland

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Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
Holocene limnic deposits characteristic of the average latitudes have partially outcropped as a result of young glacial sculpture aging. The change of the environment from limnic to telmatic and often the interference of a man associated with the regulation of water relations led to the emergence of limnic deposits that underwent the process of pedogenesis. In this work, 137 samples of carbonate deposits from 6 sites in NW Poland were analyzed in terms of their physical properties. Carbonate sediments were subject to determination of specific and bulk densities, total porosity and air porosity, current and capillary water capacity. On the basis of CaCO3 content, combustion loss, and non-lime mineral content, the studied sediments were classified into three groups: lacustrine chalk, calcareous gyttja, and clay-calcareous gyttja. Studies have shown that the sediments subject to pedogenesis in the top levels have characteristic morphological features in the form of cracks and numerous channels and iron fills in the form of spotted, streaked or marbled mosaic. The top levels of sediments, as a result of dehydration, clearly increase their bulk density. Properties of the lake chalk were formed mainly by the proportion of organic matter and CaCO3, while in the case of carbonate gyttja, the influence of mineral parts of the non-lime substances is also highlighted. In the top of carbonate sediments, there is a decrease in general and capillary porosity and an increase in the share of macropores.
Rocznik
Strony
136--142
Opis fizyczny
Bibliogr. 31 poz., rys., tab.
Twórcy
  • West Pomeranian University of Technology, Słowackiego 17 Str., 71-434 Szczecin, Poland
autor
  • West Pomeranian University of Technology, Słowackiego 17 Str., 71-434 Szczecin, Poland
Bibliografia
  • 1. Aleksander-Kwaterczak U., Kostka A. 2011. Lead in the environment of Lake Wigry (NE Poland). Limnological Review, 11(2): 59-68.
  • 2. Alonso_Zarza A.M., Wrigt V.P. 2010. Palustrine carbonates. In: Alonso-Zarza A.M., Tanner L.H. (eds): Carbonates in Continental Settings: Facies, Environments, and Processes. Elsevier, Developments in Sedimentology, 61: 103-132.
  • 3. Błaszkiewicz M. 2007. Origin and evolution of lake basins on early post-glacial landscape – selected issue. Studia Limnologica et Telmatologica 1: 5-16 (in Polish)
  • 4. Freytet P., Verrecchia E. 2002. Lacustrine and palustrine carbonate petrography: an overview. Journal of Paleolimnology, 27: 221-237.
  • 5. Gierlowski-Kordesch E.H. 2010. Lacustrine Carbonates. In: Alonso-Zarza A.M., Tanner L.H. (eds): Carbonates in Continental Settings: Facies, Environments, and Processes. Elsevier, Developments in Sedimentology, 61: 1-101.
  • 6. Glina B., Gajewski P., Kaczmarek Z., Rybczyński P. 2016. Current state of peatland soils as an effect of long-term drainage – preliminary results of peatland ecosystems investigation in the Grójecka Valley (central Poland). Soil Science Annual, 67(1): 3-9.
  • 7. Grzywna A. 2014. Evaluation of nutrient abundance in peat-muck soils of the Tyśmienica River Basin. Water-Envirinment-Rural Areas, 14(1): 19-26. (In Polish)
  • 8. IUSS Working Group WRB. 2015. World reference base for soil resources 2014. International soil classification system for naming soils and creating legends for soil maps. Update 2015. World Soil Resources Report 106, Food and Agriculture Organization of the United Nations, Rome: 188 pp.
  • 9. Jarnuszewski G. 2015. Chemical properties of organic soils developed from lacustrine chalk near the lakes Strzeszowskie, Sitno, and Sierakowo (Western Pomerania, north Poland). Soil Science Annual, 66(4): 168-179. (In Polish)
  • 10. Jones B.F., Bowser C.J. 1978. The mineralogy and related chemistry of lake sediments. In: Lerman A. (ed): Lakes Chemistry Geology Physics. Berlin, Heidelberg, New York, Springer-Verlag: 179-235.
  • 11. Karczewski A., Dmowska A., Stach A., Gudowicz J., Beszterda I., Łukaszczyk T., Smyk R., Uflik A. 2008. Geomorphology of the Myślibórz Lakeland and Szczecin Lowland. Numerical Geomorphological Map. AMU Institute of Paleogeography and Geoecology.
  • 12. Kechavarzi C., Dawson Q., Leeds-Harrison P.B. 2010. Physical properties of low-lying agricultural peat soils in England. Geoderma, 154: 196-202.
  • 13. Kelts K., Hsü K.J. 1978. Freshwater Carbonate Sedimentation. In: Lerman A. (ed): Lakes Chemistry Geology Physics. Berlin, Heidelberg, New York, Springer-Verlag: 295-323.
  • 14. Kiryluk A. 2009. Drying process in podt-bog meadow habitats. Water-Environment-Rural Areas, 9(4): 59-69. (In Polish)
  • 15. Koźmiński C., Michalska B., Czarnecka M. 2007. The climate of the West Pomeranian voivodeship. Akademia Rolnicza w Szczecinie, Uniwersytet Szczeciński: 1-147. (In Polish)
  • 16. Krzywonos K., 1993. Organogenic Carbonaceous Soils on Lacustrine Chalk. Characteristics and Classification Wiadomości IMUZ, 17(3): 37-55. (In Polish)
  • 17. Lemkowska B. 2013. “Quaternary rendzinas” in the Systematics of Polish Soil. Soil Science Annual, 64(4): 135-139. (In Polish)
  • 18. Lemkowska B., Sowiński P. 2008. Evolution of “post lake rendzinas” in the landscape of the Mazurian Lakeland. Soil Science Annual, 59(1): 134-140. (In Polish)
  • 19. Lewandowski J., Nita M. 2008. Evolution of the hydrographic system and vegetation in the drainage basin of the upper Piława and the upper Drawa Rivers (Pomorze Środkowe). Polish Geological Review, 56(5): 380-390. (In Polish)
  • 20. Markowski S. 1980. Structure and properties of peatlands’ bottom lake sediments of frequent occurrence in West Pomerania region as a basis for their identification and classification. In: Post conference materials Lake marl and gyttja, Gorzów Wielkopolski-Zielona Góra: 45-55. (In Polish)
  • 21. Okupny D., Rzepecki S., Borówka R. K., Forysiak J., Twardy J., Fortuniak A., Tomkowiak J. 2016. Factors influencing temporal changes in chemical composition of biogenic deposits in the middle Tążyna Ricer Valley (Kuyavian Lakeland, central Poland). Geologos, 22(2): 121-136.
  • 22. Pasierbski M. 1979. Remarks on the Genesis of Subglacial Channels in Northen Poland. Eiszeitalter u. Gegenwart, 29: 189-200.
  • 23. Piaścik H., Bieniek B. 2001. Changes in iron forms concentration as the result of the mucking process in different dehydration conditions. Soil Science Annual, 59: 119-125. (In Polish)
  • 24. Piaścik H., Gotkiewicz J. 2004. Transformation of dewatered peat soils as the cause of their. Soil Science Annual, 55(2): 331-338. (In Polish)
  • 25. Rutkowski J., Król K., Szczepańska J. 2007. Lithology of the profundal sediments in Słupiańska Bay (Wigry Lake, NE Poland)–introduction to interdisciplinary study. Geochronometria, 27: 47-52.
  • 26. Schnurrenberger D., Russel J., Kelts K. 2003. Classification of lacustrine sediments based on sedimentary components. Journal of Paleolimnology, 29: 141-154.
  • 27. Uggla H. 1976. Rendzinas in the Mazurian Lakeland. Soil Science Annual, 28(2): 113-125. (In Polish)
  • 28. Verrecchia E. 2007. Lacustrine and palustrine geochemical sediments. In: Nash D.J., McLaren S.J. (eds): Geochemical Sediments and Landscapes. Oxford, UK, Blackwell Publishing Ltd: 298-329.
  • 29. Wyrwicki R. 2001. Holocene carbonate sediments: properties and chemistry of gel, composition of liquid and solid components. Polish Geological Review, 49(6): 525-532. (In Polish)
  • 30. Wyrwicki R. 2003. Has lacustrine chalk originated in freshwater environment? Przegląd Geologiczny, 51(6): 483-488. (In Polish).
  • 31. Żurek-Pysz U. 1992. Strength and deformability of an organic-calcareous lacustrine deposit (gyttja) in relation to its water content and colloid content. Bulletin of the International Association of engineering geology, 45: 117-126.
Uwagi
Opracowanie rekordu w ramach umowy 509/P-DUN/2018 ze środków MNiSW przeznaczonych na działalność upowszechniającą naukę (2018).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-8ff676ca-2843-45d4-85a9-ee6cb7f35d40
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