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2007 | 55 | 4 |

Tytuł artykułu

Nutrients and conductivity in precipitation in the coast of King George Island [Antarctica] in relation to wind speed and penguin colony distance

Warianty tytułu

Języki publikacji

EN

Abstrakty

EN
The present paper reports on the year-long study of atmospheric precipitation (rain and snow) composition, including nitrogen, phosphorus and mineral matter as conductivity, in ice-free area of western coast of Admiralty Bay (King George Island). The effects of the local Adelie penguin colony on nitrogen and phosphorus concentrations in atmospheric precipitation, as well as the role of wind on nitrogen and phosphorus enrichment of ice-free areas uncovered by a progressing deglaciation of the Ecology Glacier (ASPA 128) were examined. The effect of marine influence on the mineral matter level (as conductivity) in atmospheric precipitation was examined too. The determination of conductivity, nitrogen and phosphorus were assayed according to standard methods. Conductivity, nitrogen and phosphorus concentrations in atmospheric precipitation differed depending on sampling sites location, precipitation type (rain or snow), season (summer or winter), and also distance from a penguin rookery. The mean conductivity of rain and snow amounted to 189 μS cm⁻¹ and was higher in rain (up to 290 μS cm⁻¹) than in snow samples (87 μS cm⁻¹). Mean total nitrogen and total phosphorus concentrations in precipitation amounted to 0.208 mg Ndm⁻³ and 0.028 mg P dm⁻³, respectively. A higher conductivity was recorded in the precipitation transported by NNW winds (200 μS cm⁻¹), and lower in the precipitation transported by SSE winds (80 μS cm⁻¹). The seasonal variability of conductivity was characterized by a higher values during summer (320 μS cm⁻¹) and lower – during winter (90 μS cm⁻¹). The most nutrientrich samples were those collected in the centre of the penguin rookery, average values of TN and TP concentrations were 0.450 mg N dm⁻³ and 0.090 mg P dm⁻³, respectively. At the other sites concentrations of TN and TP were lower. Seasonal variabilty of nitrogen and phosphorus concentrations were usually characterized by minimal concentrations during winter and maximal – during spring or summer. The concentrations of nitrogen and phosphorus were characterized by a statistically significant negative relation along the distance from the penguin rookery and along the altitude of sampling sites. The influence of the penguin rookery on the higher concentrations of biogenic compounds caused the high concentrations of ammonium nitrogen (averaging about 0.250 mg N dm⁻³) during summer at all sampling sites, even at those, located farthest away (about 2200 m) from the penguin colony. The annual nitrogen and phosphorus loads deposited by atmospheric precipitation onto the ice-free area were estimated at about 0.752 kg N ha⁻¹ and 0.061 kg P ha⁻¹, respectively.

Wydawca

-

Rocznik

Tom

55

Numer

4

Opis fizyczny

p.705-716,fig.,ref.

Twórcy

autor
  • Agricultural University of Szczecin, Kazimierza Krolewicza 4H, 71-550 Szczecin, Poland

Bibliografia

  • Abbott M., Einerson J., Schuster P., Susong D., Taylor H.E. 2004 – Trace elements and common ions in southeastern Idaho snow: regional air pollutant tracers for source area emissions – Fuel Proc. Technol., 85: 657–671.
  • Aristarain A.J., Delmas R.J. 2002 – Snow chemistry measurements on James Ross Island (Antarctic Peninsula) showing sea-salt aerosol modifications – Atmos. Environ., 36, 4: 765–772.
  • Battke Z., Marsz A., Pudełko R. 2001 – The Process of Deglaciation in the Region SSSI No. 8 and their Climatic and Hydrological Conditions (in polish with english summary) – Problemy Klimatologii Polarnej, 11: 121–135.
  • Bertler N. and 54 others. 2005 – Snow chemistry across Antarctica – Ann. Glaciol., 41: 167–1 79
  • Beyer L., Knicker K., Blume H.P., Bölter M., Vogt B., Schneider D. 1997 – Soil organic matter of suggested spodic horizons in relict ornithogenic soils of coastal Continental Antarctica (Casey Station, Wilkes Land) in comparison with that of spodic soil horizons in Germany – Soil Sci., 162: 518–527.
  • Björck S., Olsson S., Ellis-Evans C., Håkansson H., Humkum O., de Lirio J.M. 1996 – Late Holocene palaeoclimatic records from lake sediments on James Ross Island, Antarctica – Palaeogeography, Palaeoclimatology, Palaeoecology, 121: 195–220.
  • Braun M., Simoes J.C., Vogt S., Bremer U.F., Blindow N., Pfender M., Saurer H., Aquino F.E., Ferron F.A. 2001 – An improved topographic database for King George Island: compilation, application and outlook – Antarct. Sci., 13 (1): 41–52.
  • Claesson S., Steinneck S. 1996 – Plant nutrient management and the environment – Swedish University of Agricultural Sciences. Special Report, 41, Uppsala: pp. 69.
  • Fattori I., Becagli S., Bellandi S., Castellano E., Innocenti M., Mannini A., Severi M., Vitale V., Udisti R. 2005 – Cemical composition and physical futures of summer aerosol at Terra Nova Bay and Dome C, Antarctica – J. Environ. Monit., 7(12): 1256–1274.
  • Fahnestock J.T., Povirk K.L., Welker J.M. 2000 – Ecological significance of litter redistribution by wind and snow in arctic landscapes – Ecography, 23: 623–631.
  • Fisk M.C., Schmidt S.K., Seastedt T.R. 1996 – Topographic patterns of above- and belowground production and nitrogen cycling in alpine tundra – Ecology, 79: 2253–2266.
  • Gordon A.L., Molinelli E., Baker T. 1978 – Large-scale relative dynamic topography of the Southern Ocean – J. Geophys. Res., 83, 3023–3032.
  • Heywood R.B. 1968 – Ecology of fresh-water lakes of Signy Island, South Orkney Islands. 2, Physical and chemical properties of the lakes – Br. Antarct. Surv Bull., 18: 11–44.
  • Hiltbrunner E., Schwikowski M., Körner C. 2005 – Inorganic nitrogen storage in alpine snow pack in the Central Alps (Switzerland) – Atmos. Environ., 39: 2249–2259.
  • Jourdain B., Legrand M. 2002 – Year-round record of bulk and size-segregated aerosol composition and HCL and HNO₃ levels in the Dumont d´Urville (Coastal Antarctica) atmosphere – implication for sea-salt aerosol fractionation in the winter and summer – J. Geophys. Res., 107, D22, pp. 4645.
  • Juchnowicz-Bierbasz M. 1999 – Year-round changes of nutrients in fresh water bodies near Arctowski Station, South Shetland Islands, Antarctica – Pol. Polar Res., 20, 3: 243–258.
  • Juchnowicz-Bierbasz M., Rakusa-Suszczewski S. 2002 – Nutrients and cations in soil solution from the present and relict penguin colonies (Admiralty Bay, King George Island) – Pol. J. Ecol., 50: 79–91.
  • Kejna M., Láska K. 1999 – Weater conditions at H. Arctowski Station in 1996 – Pol. Polar Res. 20: 3, 203–220.
  • Kowalski D. 1985 – Wind structure at the Arctowski Station – Pol. Polar Res. 6, 3: 391–403.
  • Kowalski D., Wielbińska D. 1989 – Synoptic Features of the winter 1989 at Arctowski Station, King George Island, West Antarctica – Pol. Polar Res., 10: 57–71.
  • Legrand M., Ducroz F., Wagenbach D., Mulvaney R., Hall J. 1998 – Ammonium in coastal Antarctic aerosol and snow: Role of polar ocean and penguin emissions – J. Geophys. Res., 103 (D9): 11043–11056.
  • Marsz A.A. 2000 – Charakterystyka fizycznogeograficzna obszarów lądowych w otoczeniu Zatoki Admiralicji. [Physical and geographic characteristic of the land areas in the vicinity of the Admiralty Bay.] – WSM Gdynia, 125 pp. (in Polish)
  • Marsz A.A., Styszyńska A. 2000 – Główne cechy klimatu rejonu polskiej stacji antarktycznej im. H. Arctowskiego (Antarktyka Zachodnia, Szetlandy Południowe, Wyspa Króla Jerzego. [Main climate features of the area of H. Arctowski Antarctic Station (West Antarctica, South Shetlands)]. – WSM Gdynia, 264 pp. (in Polish)
  • Mishra V.K., Kim K., Hong S., Lee K. 2004 – Aerosol composition and its sources at the King Sejong Station, Antarctic peninsula – Atmos. Environ., 38, 24: 4069–4084.
  • Nędzarek A. 2006 – Annual raport of hydrochemical studies at H. Arctowski Station during 29th Expedition in 2005. (unpublished data, in Polish) 1–34.
  • Nędzarek A., Rakusa-Suszczewski S. 2004 – Decomposition of macroalgae and the release of nutrients in Admiralty Bay, King George Island, Antarctica – Polar Biosci., 17, 26–35.
  • Pietr J., Tatur A., Myrcha A. 1983 – Mineralization of penguin extrements in the Admiralty Bay region (King George Island, South Shetlands Islands, Antarctica) – Pol. Polar Res., 4: 97–112.
  • Rakusa-Suszczewski S., Nędzarek A. 2002 – Whale bones and macroalgae as source of nutrients and cations in the nearshore geoecosystem of Admiralty Bay (King George Island, Antarctica) – Pol. J. Ecol. 50, 3, 389–396.
  • Rakusa-Suszczewski S., Zieliński K. 1993 – Macrophytobenthos (In: The Maritime Antarctic Coastal Ekosystem of Admiralty Bay. Ed. S. Rakusa-Suszczewski) – Warsaw, Departament of Antarctic Biology, Polish Academy of Sciences, 57–60.
  • Reimann C., de Caritat P., Halleraker J.H., Volden T., Äyräs M., Niskavaara H., Chekushin V.A., Pavlov V.A. 1997 – Rainwater composition in eight arctic catchments in northern Europe (Finland, Norway and Russia) – Atmos. Environ., 31, 2: 159–170.
  • Rodrigo A., Àvila A., Rodà F. 2003 – The chemistry of precipitation, throughfall and stemflow in two holm oak (Quercus ilex L.) forests under a contrasted pollution environment in NE Spain – Sci. Total Environ., 305: 195–205.
  • Saxena A., Kulshrestha U.C., Kumar N., Kumari K.M., Srivastava S.S. 1996 – Characterization of precipitation at Agra – Atmos. Environ., 30, 20: 3405–3412.
  • Shaw G.E. 1988 – Antarctic aerosols – a review – Rev. Geophys., 28: 89–112.
  • Speir T.W., Cowling J.C. 1984 – Ornithogenic soils of the cape Bird adelie penguin rookeries, Antarctica – Polar Biol., 2 (4): 199–205.
  • Standard Methods for Examination of Water and Wastewater 19th Edition 1995 – Publ. Am. Health Ass., Washington.
  • StatSoft Inc. 2005. STATISTICA (data analysis software system), version 7.1. www.statsoft.com.
  • Suzuki T., Iizuka Y., Matsuoka K., Furukawa T., Kamiyama K., Watanabe O. 2002 – Distribution of sea salt components in snow cover along the traverse route from the coast to Dome Fuji station 1000 km inland at east Dronning Maud Land, Antarctica – Tellus B, 54 (4), 407 pp.
  • Tatur A. 2002 – Ornithogenic Ecosystems in the Maritime Antarctic. Formation, Development and Distination – (In: Geoecology of Antarctic Ice–Free Coastal Landscapes Eds: Beyer L., Bolter M.) – Springer–Verlag Berlin Heidelberg, pp. 161–184.
  • Tatur A., Myrcha A. 1988 – Soils and vegetation in abandoned penguin rookeries (Maritime Antarctic Zone) – Tenth Symposium on Polar Biology. 24–26 November 1987, Tokyo, National Institute of Polar Research – Proc. NIPR Symp. Polar Biology, 2: 181–189.
  • Zdanowski M.K., Żmuda M.J., Zwolska I. 2005 – Bacterial role in the decomposition of marine-derived material (penguin guano) in the terrestrial maritime Antarctic – Soil Biol. Biochem., 37: 581–595.

Typ dokumentu

Bibliografia

Identyfikatory

Identyfikator YADDA

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