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Local variability of soil properties of forest stands along the North-South climatic transect in Europe

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Języki publikacji
EN
Abstrakty
EN
The differentiation of the properties of soils at the level of pedons constitutes one of the most essential elements of the functional-structural analysis of the ecosystems. The purpose of the studies presented in this paper was to assess the spatial variability of the soil cover as conditioned by the micro-habitat differentiation and expressed through the variability of thickness of the genetic horizons for individual pedons, as well as spatial differences in acidity, moisture, conductivity, and organic carbon content. The studies were conducted on podzolic soils covered with forest vegetation. The results of studies carried out and described here indicate an influence of the local topo-habitat conditions on the spatial variability of soil properties. the following results can be drawn on the basis of the results obtained: 1) within the organic horizon the highest spatial differentiation of the properties considered was observed in the soils of Finland and Norway, while within the humus and enrichment horizons it was greater in the soils of the Polish part of the study area; 2) an exception to the above regularity is constituted by moisture; the highest spatial differentiation at this factor within all the genetic horizons was always observed in the soils characterised by its highest values; 3) spatial differentiation of the properties analysed is greater within the organic and humus horizons than in the enrichment horizon; 4) the biggest differences between the particular variants of the experiment, implemented during the four years of study, were displayed by: a) within the organic layer - the pedons of the northern and central parts of the study area, fromm Norway to Latvia, b) within the humus layer - the marginal pedons of FN1 and PL3 as well as the pedons of the central part of the study area - from Lithuania and Latvia, c) within the enrichment layer - the pedons of the Polish part of the study area; 5)interdependence was observed between the length of the micro-transects and the variability of the soil properties analysed; and 6) the strongest interrelation between the analysed properties were registered for the moisture - organic carbon content and moisture - conductivity.
Słowa kluczowe
Rocznik
Strony
461--469
Opis fizyczny
Bibliogr. 20 poz., tab., wykr.
Twórcy
autor
  • Institute of Geography and Spatial Organisation, Polish Academy of Sciences, Twarda 51/55, 00-818 Warsaw, Poland
Bibliografia
  • [1] Breymeyer A. 2003 - Pine ecosystem response to warming along North-South climatic transect in Europe: presentation of research project - Pol. J. Ecol. 51, 4:403-411.
  • [2] Brown I. 1979 - Etude systematique de la variable d’um soil podzoliąue, le long d’une tranchee duns une erabliere a Boulea Jaune - Can. Jour. Soil Sc. 59, 131-146. (inFrench).
  • [3] Brown I., Thorp J. 1942 - Morphology and composition of some soils of the Miami family and the Miami catena - U.S. Dept. Agric. Tech. Buli. 834, 1-55.
  • [4] Degórski M. 1990 - Warunki siedliskowe kateny ekosystemów leśnych na Wysoczyźnie Rawskiej, ze szczególnym uwzględnieniem dynamiki wodno-troficznych właściwości gleb. [Habitat conditions of the forest ecosystems in the catena situated on the Rawa Plateau with particular regard to dynamie of hydro-trophic soil properties] - Dokum Geogr. 5-6, Warszawa, 240 pp. (in Polish).
  • [5] Degórski M. 1995 - Analysis of a catenary complex of soils and forest plant communities in the South Mazovia Uplands (Central Poland) - Ekol. Pol. 42 (3-4), 265-289.
  • [6] Degórski M. 1998 - Sezonowa dynamika wybranych gleb siedlisk borów i borów mieszanych na transektach badawczych: klimatycznym (wzdłuż 52°N, od 12° do 32°E) i „śląskim” [Sezonal dynamics to selected properties of the soils of pine and mixed pine forest habitat along a climatic transect (52°N, 12°-32°E ) and „silesian” transect], (In: Bory sosnowe w gradiencie kontynentalizmu i zanieczyszczeń w Europie Środkowej - badania geoekologiczne. [Pine forest in Central European gradient of continentality and pollution - geoecological study]. Eds: A. Breymeyer, E. Roo-Zielińska) - Dokumentacja Geograficzna 13, 55-62. (in Polish).
  • [7] Degórski M., 2000 - Is a geodiversity a part of landscape diversity. (In: Multifunctional Landscapes, interdisciplinary approaches to landscape research and management. Eds: Brandt J., Tress B., Tress G.) - Pablished by the Centre for Landscape Research, Roskilde, 215-216.
  • [8] Degórski M. 2001 - Pedosfera - element środowiska łączący abiotyczną i biotyczną różnorodność. [Pedosphere - environmental element connecting geo- and biodiversity] (In: Między geografią i biologią - badania nad przemianami środowiska przyrodniczego, Ed: E. Roo-Zielińska, J. Solon). - Prace Geogr. 179, 227-238. (in Polish)
  • [9] Degórski M. 2002 - Przestrzenna zmienność właściwości gleb bielicoziemnych środkowej i północnej Europy a geograficzne zróżnicowanie czynników pedogenicznych. [The spatial variability to the properties of podzolic soils in central and northem Europe and the geographical differentiation of pedogenic factors] - Prace Geogr. 182, Warszawa, 189 pp. (in Polish).
  • [10] Degórski M. 2003a - Pedodiversity as a part of geodiversity in creation of landscape structure. (In: Multifunctional Landscape Vol 2: Monitoring, Diversity & Management. Ed. J. Brandt) - Advances in Ecological Sciences Vol 15, Wit Press. 105-121.
  • [11] Degórski M. 2003b - Morpholitological genesis and soil properties of pine forest ecosystems in relation to the north-south transect in Europe - Pol. J. Ecol. 51,4:441-459.
  • [12] Dziadowiec H., Gonet S. 1999 - Przewodnik metodyczny do badań materii organicznej gleb. [Guide-book for the methodology in soil organic matter research] - Prace Kom. Nauk. PTGleb. 120, Warszawa, 89 pp. (in Polish).
  • [13] Głazowska M. A. 1981 - Gleby kuli ziemskiej. [Soil of the Earth]. - PWN, 435 pp. (in Polish).
  • [14] FAO/UNESCO 1990 - Soil Map of the World. Revised legend - Soils Bulletin, FAO, Rome.
  • [15] Prusinkiewicz Z. 1999 - Środowisko i gleby w definicjach. [Environment and soils in definition] - Oficyna Wyd. TURPRESS, Toruń, 477 pp. (in Polish)
  • [16] Mokma D. 1983 - New Chemical criteria for defining the spodic horizon. - Soil Sci. of American Jour. 47(5), 972-976.
  • [17] Solon J., 2003 - Scots pine forests of the Vaccinio-Piceetea class in Europe: forest sites studied-Pol. J. Ecol. 51, 4:421-439.
  • [18] Steila D. 1976 - The geography of soils. Formation, distribution and management - Prentice Hall, Inc., Englewood Cliffs, New Jersey, 1- 222.
  • [19] Systematyka Gleb Polski, 1989 - Polish soil taxonomy - PTG, Roczn. Gleb., 40 (3/4), 150 pp. (in Polish)
  • [20] WRB (World Reference Base for Soil Resources) 1998 - World Soil resources Reports 84 - FAO, ISRIC and ISSS.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BGPK-0638-2918
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