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dc.contributor.authorMałek, Stanisław
dc.contributor.authorJanuszek, Kazimierz
dc.contributor.authorBarszcz, Józef
dc.contributor.authorBłońska, Ewa
dc.contributor.authorWanic, Tomasz
dc.contributor.authorGąsienica-Fronek, Wojciech
dc.contributor.authorKroczek, Marek
dc.date.accessioned2014-10-07T12:02:10Z
dc.date.available2014-10-07T12:02:10Z
dc.date.issued2011
dc.identifier.issn0071-6677
dc.identifier.urihttps://depot.ceon.pl/handle/123456789/5383
dc.description.abstractThe experimental plots were located in the middle forest zone (900– 950 m) on two nappes of the flysch Carpathians Magura (the Ujsoły Forest District) and Silesian (the Wisła Forest District) in the spruce stands of age class 21– 40 years. Serpentinite was introduced in the autumn of 2008 on all plots while other fertilizers (N, P, NP and NPK) in the spring of 2009. Based on the chemical composition of soil solutions collected in lysimeters placed at the depth of 20 cm in the autumn 2008 and the spring and autumn 2009, ecochemical parameters were calculated: acid neutralization capacity (ANCaq), alkalinity (ALK), the degree of soil acidity (Ma%), acidic cations (Ma), saturation of the exchangeable complex of the soil solid phase (Mb) with alkalis, saturation with alkalis (BS), molar relations Ca/Al, Mb/Al, BC/Al. After the winter, soil solutions became acidic, especially in the Wisła Forest District. The saturation of the studied soils demonstrates moderate flexibility of soils in the Wisła Forest District in relation to acid load, and high flexibility of the Ujsoły soils. The opposite trend was observed for the degree of acidity of soils. Acid neutralization capacity and alkalinity of the waters showed significant variations in soil pH even in the case of small variations in the composition of the solution, if they were caused by the inflow of the anions of NO3 - and SO42-. After application of the fertilizers, an increase of Mg, Ca and Mb was noted in the soil solution, determined in the overlaying highly acidic organic horizons trough the ion-exchange buffering mechanism of highly protonated functional groups with high buffering capacity. Highly improved content of Mg in a soil, and in some cases – also the content of N, P and K, present potential improvement of forest growth capacity without the hazard of adverse side-effects of liming. Aluminum stress in the spruce is unlikely, while trees in the control plots in the Wisła Forest District may already be sensitive.pl_PL
dc.language.isoenpl_PL
dc.publisherInstytut Badawczy Leśnictwa (Forest Research Institute), Komitet Nauk Leśnych PAN (The Committee on Forestry Sciences of the Polish Academy of Sciences)pl_PL
dc.rightsCreative Commons Uznanie autorstwa na tych samych warunkach 3.0 Polska
dc.rights.urihttp://creativecommons.org/licenses/by-sa/3.0/pl/legalcode
dc.subjectmountainspl_PL
dc.subjectPicea abies standspl_PL
dc.subjectslow-realease fertilizerspl_PL
dc.subjectecochemical indicatorspl_PL
dc.titlePreliminary assessment of the ecochemical condition of soils after fertilization of younger spruce Picea abies (L.) H. Karst. stands in the Beskid Śląski and Żywiecki Mts.pl_PL
dc.typeinfo:eu-repo/semantics/articlepl_PL
dc.contributor.organizationForest Research Institute, Sękocin Starypl_PL
dc.contributor.organizationCommittee on Forestry Sciences, Polish Academy of Sciences
dc.description.epersonPrzemysław Szmit
dc.rights.DELETETHISFIELDinfo:eu-repo/semantics/openAccess


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