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Tytuł:
Specjacja fosforu w leśnych glebach rdzawych na obszarach popożarowych
Phosphorus fractionation in forest Brunic Arenosols of post-fire areas
Autorzy:
Jonczak, J.
Olejarski, I.
Janek, M.
Powiązania:
https://bibliotekanauki.pl/articles/985713.pdf
Data publikacji:
2019
Wydawca:
Polskie Towarzystwo Leśne
Tematy:
lesnictwo
Nadlesnictwo Rudy Raciborskie
tereny popozarowe
gleby lesne
gleby rdzawe
gleby popozarowe
fosfor
specjacja chemiczna
phosphorus
sequential extraction
wildfire
brunic arenosols
leaching
Opis:
The studies on contents and profile distribution of total phosphorus and its fractions extracted according to the procedure of Hedley et al. [1982] in a modification of O’Halloran et al. [1987] in forest Brunic Arenosols of post−fire areas in the Rudy Raciborskie Forest District (S Poland) were undertaken. Five soil profiles developed from fluvioglacial sandy deposits of the Oder Glaciation were described and sampled 21 years after the fire occurrence and analyzed using standard procedures. Total content of the element was among typical for Brunic Arenosols of Poland, ranging from 683.1 to 880.4 mg/kg in Ofh horizons, from 154.2 to 566.5 mg/kg in mineral horizons affected by soil−forming processes and from 115.5 to 384.2 mg/kg in parent material. The content of distinguished phosphorus fractions varied, reflecting the effect of environmental factors and brunification soil−forming process. Residual fraction predominated in parent material, organic in O and most of A−horizons and bounded to sesquioxides in B−horizons. The observed proportions between residual fraction and sum of the remaining fractions were typical for soils of old−glacial areas, reflecting considerable degree of mineral substrate weathering. An effect of fire was not clear due to the lack of a reference soil. However, the studied soils showed some specific features, that can be explained by the influence of fire. Low content of fraction bounded to calcium and apatites is the first and elevated concentration of fraction bounded to sesquioxides in parent material is the other one. Profile distribution patterns of mentioned above fractions suggest leaching of phosphorus labile forms and their stabilization in deeper parts of the studied soils. This process could be initialized or accelerated by fire. Finally, it can be concluded, that studied properties of the contemporary soils are stronger influenced by pine forest vegetation than by fire before 21 years.
Źródło:
Sylwan; 2019, 163, 05; 396-406
0039-7660
Pojawia się w:
Sylwan
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Zawartość i profilowe rozmieszczenie frakcji fosforu w uprawnych i leśnych czarnoziemach z poziomem cambic
Content and profile distribution of phosphorus fractions in arable and forest Cambic Chernozems
Autorzy:
Jonczak, J.
Simansky, V.
Pollakova, N.
Powiązania:
https://bibliotekanauki.pl/articles/989926.pdf
Data publikacji:
2015
Wydawca:
Polskie Towarzystwo Leśne
Tematy:
gleboznawstwo
gleby uprawne
gleby lesne
czarnoziemy
fosfor
zawartosc fosforu
frakcje fosforu
specjacja chemiczna
rozmieszczenie profilowe
chernozems
arable soils
forest soils
phosphorus speciation
Opis:
Comparative studies on the content and profile distribution patterns of phosphorus fractions in arable and forest Cambic Chernozems were conducted near the village Báb (western Slovakia). Soil samples were collected from every 10 cm and analyzed using standard procedures in soil science. Long term differences in the type of the studied soils usage were reflected in their physical and chemical properties (bulk density, porosity, acidity, the total content of organic carbon and nitrogen), as well as in the content and profile distribution patterns of phosphorus fractions. Total phosphorus content ranged from 498.8 to 754.7 mg/kg in arable soil and from 480.4 to 835.9 mg/kg in forest soil. Residual fraction, which constituted 54.9−77.8% of total phosphorus in arable soil and 57.3−79.2% in forest soil, was a predominant fraction. Such large contribution of this fraction is typical for young soils, with weakly weathered mineral substrates. Exchangeable phosphorus in arable soil constituted 0.6−6.1%, while 0.5−3.0% in forest soil, showing decreasing trends with depth in both soils. Free iron oxides and carbonates were important factors influencing profile distribution of phosphorus in the investigated soils. Iron oxides bound the element mainly in acidified horizons, whereas carbonates in alakaline (Bw and C) horizons. Organic fraction significantly differed in the investigated soils. A much larger content and contribution of this fraction in total phosphorus was noticed in forest soil. The content of organic phosphorus was positively related to the content of organic carbon. Stable fraction of organic phosphorus predominated over labile one in both soils.
Źródło:
Sylwan; 2015, 159, 11; 931-939
0039-7660
Pojawia się w:
Sylwan
Dostawca treści:
Biblioteka Nauki
Artykuł
    Wyświetlanie 1-2 z 2

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