PL EN


Preferencje help
Widoczny [Schowaj] Abstrakt
Liczba wyników
Powiadomienia systemowe
  • Sesja wygasła!
Tytuł artykułu

Fluxes of biogenic substances in precipitation and throughfall in woodland ecosystems of Słowiński National Park

Identyfikatory
Warianty tytułu
PL
Przepływ substancji biogenicznych wraz z opadami atmosferycznymi i podkoronowymi w wybranych ekosystemach leśnych Słowińskiego Parku Narodowego
Języki publikacji
EN
Abstrakty
EN
In the study the dynamics of concentration level changes was analyzed in the period between 2002 and 2005 concerning N-NH_4, N-NO_3, P-PO_4 and pH in bulk precipitation and throughfall in two different woodland ecosystems of Słowiński National Park. Both woodland ecosystems were influenced by the same weather conditions. On the basis of obtained results it was found that chemical variability of throughfall waters is mainly determined by both species composition and the kind of forest stand, as well as its trophic conditions Comparing to bulk precipitation (collected at an open area) throughfall samples collected at the Vaccinio uligi-nosi -Beluletumpubescenlis ecosystem were poor in N-NH_4 and P-PO_4 enriched in N-NO_3, and slightly more acidic (by 3.9%), while at the Empelro nigri - Pinetum ecosystem were poor in N-NH_4 enriched in P-PO_4 and N-NO_3 and more acidic (by 4.4%).
PL
W pracy przeanalizowano dynamikę zmian poziomów stężeń N-NH_4, N-NO_3, P-PO_4 oraz pH w opadach na otwartej przestrzeni i opadach podkoronowyeh w dwóch różnych ekosystemach leśnych Słowińskiego Parku Narodowego w okresie 2002-2005. Badane ekosystemy leśne znajdowały się pod wpływem takich samych warunków meteorologicznych. Na podstawie uzyskanych wyników stwierdzono, że o zmianie jakości wód podkoronowyeh decydują przede wszystkim rodzaj i gatunek drzewostanu, a także stan troficzny ekosystemu leśnego. Opady podkoronowe w porównaniu do opadów na otwartej przestrzeni w zespole Vaccinio uliginosi - Betuletum pubescentis były uboższe w N-NH_4 i P-PO_4 wzbogacone w N-NO_3,oraz nieco bardziej kwaśne (o 3,9%), a w zespole Empetro nigri - Pine tum uboższe w N-NH_4 wzbogacone w P-PO_4, i N-NO_3 oraz bardziej kwaśne (o 4,4%).
Rocznik
Strony
13--24
Opis fizyczny
bibliogr. 46 poz., tab., wykr.
Twórcy
autor
autor
  • Pomeranian Academy, Institute of Biology and Environmental Protection, Environmental Chemistry Research Unit ul. Arciszewskiego 22, 76-200 Słupsk, Poland
Bibliografia
  • [1] Bednorz J.: Animal world, [in:] H. Piotrovvska (eds), Nature of Słowiński National Park, Bogucki, Poznań-Gdańsk 1997
  • [2] Blond E.R., W.T. Swank, T. Williams: Precipitation, throughfall. and stem flow chemistry in a Coastal Loblolly Pine Stand, Freshwater Wetlands and Wiltwife, 61-78 (1986).
  • [3] Bochenek W.: Influence of atmospheric circulation on electrolytic conductivity of precipitation water solutions in the Bystrzanka catchment in the period between 1995-2004, Nature Environment Monitoring KTN. Kielce 2005, 6, 49-58.
  • [4] Bormann F.H., G.E. Likens: Pattern and Process in a Forested Ecosystem, Springer Verlag, Berlin, New York 1979.
  • [5] Butler T.J., G.E. Likens: A direct comparison of throughfall plus stem flow to estimates of dry and total deposition for sulfur and nitrogen, Atmos. Environ., 29, 1253-1265 (1995).
  • [6] Carleton T.J., T. Kavanagh: Influence of stand age and spatial location on throughfall chemistry beneath Black spruce. Can. J. Forest Res., 20, 1917-1925 (1990).
  • [7] Charron A , H Plaisance, S. Saurage. P. Coddeville, I.C. Galloo, R. Guillermo: A study of the source -receptor relationships influencing the acidity of precipitation collected at a rural site in France, Atmos. Environ., 34, 3665-3674 (2000).
  • [8] Chiwa M, D.H. Kim, H. Sakugawa: Rainfall, stem flow and throughfall chemistry at urban- and mountain-facing sites at Ml. Gokurakuj, Hiroshima, Western Japan, Water, Air, Soil Pollut., 146, 93-109 (2003).
  • [9] Foster N.W., I.K. Morrison: Distribution and cycling of nutrients in a natural Pinus Banksiana ecosystem. Ecology, 57, 110-120(1976).
  • [10] Hansen K : Throughfall and canopy interaction in spruce forest, Forskningsserien 8, Danish Forest and Landscape Research Inst., Lyngby 1994.
  • [11] Hansen K.: In-conopy throughfall measurements of ion fluxes in Norway spruce, Atmos. Environ.. 30.4065-1076(1996).
  • [12] Hermanowicz W., J. Dojlido, W. Dożańska, B. Kosiorowski, .1. Zerbe: Physico-chemical measurements of water and waste-waters, Arkady Press, Warsaw 1999.
  • [13] Janek M.: Influence of coniferous forest stands on bulk precipitation quality. Works of Institute of Forest Research, 4, 73-87 (2000)
  • [14] Janek M.: Influence of coniferous forest stands on bulk precipitation quality. Part II. Seasonal changes in quantity and chemical profile of precipitation in coniferous forest stands of Augustowska Forest, Works of Institute of Forest Research, 3, 73-86 (2002).
  • [151 Jansen W.,A. Block, J. Knack: Acid rain History, genesis, effects, Aura 4 (1998).
  • [16] Jóżwiak M., R. Kozlowski: Transformation of bulk precipitation in chosen ecosystems of Świętokrzyskie Mis., Regional Monitoring of Natural Environment, KTN Kielce 2004, 5, 199-217.
  • [17] Konieczka P., J. Namieśnik, B.Zygmunt, E. Bulska, A. Świtaj-Zawadka.A. Naganowska, E. Kremer, M. Rompa' Qualify assessment and quality control of analytical results - OA/QC. Centre of Excellence in Environment Analysis and Monitoring, Gdańsk (in Polish) 2004.
  • [18] Kowalkowski A.. M. Jóźwiak: Chemical composition of bulk precipitation. Świętokrzyski National Park-Nature, Economy, Culture, Bodzentyn - Krakow 2000.
  • [19] Kowalkowski A., M. Jóźwiak, R. Kozlowski: Versauerung der Niederschldge und Bodenzustand im Świętokrzyski National Park, DBG, Mittcilungen, Band 98, 49-50 (2002).
  • [20] Kowalkowski A.M. Jóźwiak. R. Kozlowski: Changes in qualify of bulk precipitation in the Świętokrzyski National Parkforest ecosystem. Environ. Engin. Tech. .1., 5, 97-110 (2002).
  • [21] Kozlowski R.: An inflow of mineral compounds together with bulk precipitation to the forest bottom layer in the Base Station of Integrated Monitoring of Natural Integrated Monitoring of Natural Environment. An action and monitoring of geoecosystems considering atmospheric pollution. Environmental Monito ring Library, Kielce 2001, 207-218.
  • [22] Kozlowski R.: Quantitative and qualitative variability of throughfall stem flow in chosenforesl ecosystems of Świętokrzyskie Mis., Regional Monitoring of Natural Environment. KTN Kielce 2002, 3, 95-102.
  • [23] Kozlowski R.: Spatial variability of throughfall waters in mixed fir-pine forest stand in the central part of Świętokrzyskie Mts., Regional Monitoring of Natural Environment, KTN Kielce 2003, 4, 99-106.
  • [24] Kram K.J.: Bulk deposition and aerosol-gaseous input of elements in the forested area of Coastal Region (Pomerania. North Poland), Pol. J. Ecol., 53, 261-268 (2005).
  • [25] Krzysztofiak L.: A report of Base Station of Integrated Monitoring of Natural Environment (Krzywe) for the hydrologie period between 1994 and 1997, [in:] Kostrzewski A. (eds.) Integrated Monitoring of Natural Environment. Geoecosystems condition in the period between 1994 and 1997, Environmental Monitoring Library'. PIOŚ, Warsaw 1998, 103-122.
  • [26] Likens G.E., ELF. Bormann: Biogeochemistry of a Forested ecosystem. Springer- Verlag, New York. Berlin, Heidelberg, London, Paris. Tokyo, Hong Kong, Barcelona, Budapest 1995, 1-159.
  • [27] Lovett G.M., S.E. Lindberg: Atmospheric deposition and canopy interactions of nitrogen of forest. Can J. For. Res, 23, 1603-1616(1993).
  • [28] Malzahn E.: Monitoring of hazards and pollutions of forest ecosystem of Białowieska Forest, Cosmos. 51. 435-441,(2002).
  • [29] Matuszkiewicz J. M.: Polish woodland ecosystems, PWN, Warszawa 2002.
  • [30] Mazurek M., Z. Zwoliński: An activity of chosen polish geoecosystems in the framework of monitoring measurements in hydrologie year 1999, http://main.amu.edu.pl/~-zmsp/stan99/stan99.html. Institute of Quaternary Research and Geoecology UAM, Poznań 2000.
  • [31] Słowiński National Park protection plan. Forest ecosystems protection procedures for the period between 2002 and 2021. Vol. 7 General description. Vol. 9.1 Taxonomical forest description - Land Compound. Units 1-63, Jelenia Mt. Office of planning and designing 2003
  • [32] Polkowska Ż., A. Astel, M. Grynkiewicz. T. Górecki. J. Namieśnik: Studies on intercorrelation between ions co-occuring in precipitation in the Gdańsk -Sopot - Gdynia Tricity (Poland), J. Atmos. Chem., 41. 239-264 (2002).
  • [33] Polkowska Ż.. A. Astel, B Walna. S. Malek, K. Mądrzycka. T. Górecki., .1. Siepak, J. Namieśnik: Chemometric analysis of rainwater and throughfall at several sites in Poland, Atmos. Environ., 39. 837-855 (2005).
  • [34] Pryor S.C., R..I. Barthelmie: Nutrient fluxes in precipitation, throughfall and stem flow: observations from the deciduous forest, Geophysic. Res. Abstr, 5, 1911 (2003).
  • [35] Pryor S.C., R.J. Barthelmie: Liquid and chemical fluxes in precipitation, throughfall and stemflow: Observations from a deciduous forest and a red pine plantation in the Midwestern U.S.A., Water, Air, Soil Pollut., 163, 203-227, (2005).
  • [36] Rabski K.: Mezoclimatic background of Słowiński National Park, National Parks and Nature Reservoirs. 11,37-54(1992).
  • [37] Shubzda J., S.E. Lindberg, C.T. Garten. S.C. Nodvin: Elevation trends in the fluxes of sulphur and nitrogen in throughfall in the southern Appalachian Mountains: some surprising result. Water. Air, Soil Pollut., 85, 2265-2270 (1995).
  • [38] Stachurski A.: Nutrient control in through/all waters of forest ecosystems, Pol. Ecol., 35, 3-69 (1987).
  • [39] Stachurski A., J.R. Zimka: The budget of nitrogen dissolved in rainfall during its passing through the crown canopy in forest ecosystems, Pol. Ecol., 32, 191-218 (1984).
  • [40] Stachurski A., J.R. Zimka: Radicals cycle in land ecosystems. Cosmos, 54, 391-400 (2004).
  • [41] SzarekG.: Sulphur and nitrogen input to the Ratanica forested catchment (Carpathian foothills, Southern Poland), Water, Air, Soil Poll., 85, 1765-1770 (1995).
  • [42] Tyszka .1., T. Wawrzyniak, M. Janek: Ion fluxes through spruce and pine forest ecosystems in various environmental pollution conditions, Works of Institute of Forest Research, 864, 35-56 (1998).
  • [43] Van Dobeen H.F., J. Mulder, H. van Dam, H. llouweling: Impact of acid atmospheric deposition on the biogeochemistry of moorland pools and surrounding terrestrial environment, Agricultural Research Reports 931, Pudoc Scientific Publishers. Wageningen 1992, 1-199.
  • [44] Walna B., Ż. Polkowska. S. Malek, K. Medrzycka, J. Namieśnik, J. Siepak: Tendencies of Change in the Chemistry of Precipitation at Three Monitoring Stations 1996-1999, Pol. J. Environ. Stud.. 12, 467-472 (2003).
  • [45] Zimka J.R., A. Stachurski: Forest decline in Karkonosze Mis. (Poland), Part II, An analysis of acidity and chemistry of atmospheric precipitation, throughfall and forest stream waters, Pol. Ecol., 44, 153-177 (1996).
  • [46] Żelazny M.: Physical conditions of atmospheric precipitations, [in:] M. Żelazny (cds). Dynamics of nutrients in bulk precipitation, surface and underground waters in the catchments characterized by various utilization in the Wiśnickie foothills, Institute of Geography and Space Economy, UJ, Krakow 2005
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BUS5-0013-0010
JavaScript jest wyłączony w Twojej przeglądarce internetowej. Włącz go, a następnie odśwież stronę, aby móc w pełni z niej korzystać.