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1

Sklad frakcyjny zwiazkow prochnicznych organicznych gleb popozarowych w nadlesnictwie Chocianow

100%
Bogacz A.
Roczniki Gleboznawcze
|
2009
|
tom 60
|
nr 3
27-36
2

Morfologia profili oraz wlasciwosci chemiczne i zasoby materii organicznej w glebach po pozarze w borze sosnowym

100%
Gonet S. S., Dziadowiec H., Bucko M.
Roczniki Gleboznawcze
|
2009
|
tom 60
|
nr 2
32-38
3
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Specjacja fosforu w leśnych glebach rdzawych na obszarach popożarowych

100%
Jonczak J., Olejarski I., Janek M.
Sylwan
|
2019
|
tom 163
|
nr 05
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.
4
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Wpływ sposobu rewitalizacji pożarzyska na stan mikrobiologiczny gleb 20 lat po całkowitym pożarze lasu

100%
Mocek-Płociniak A., Bielinska E. J., Wolna-Maruwka A., Futa B.
Sylwan
|
2016
|
tom 160
|
nr 03
The article assesses the influence of method of revitalisation of the forest fire site in Potrzebowice Forest District (western Poland) on basic parameters of the microbial activity in soils. We investigated study plots established in 1994, two years after the forest had burnt down completely. We applied three different methods of soil preparation and planted either Scots pines (Pinus sylvestris L.) or grey alders (Alnus incana (L.) Moench.). For comparisons an area of natural succession and untreated control plot, which was located beyond the range of the fire, were taken. 18 years after the application of the methods of renewal of the fire site, the soils have not undergone full microbiological regeneration. The soils at the fire site were mainly colonised by heterotrophic eubacteria. The population of these microorganisms, which were usually found in fresh litter and in the strict rhizosphere, was greater than in the soil of the control plot. On the other hand, there were low populations of actinobacteria, which regenerated poorly, especially at the accumulation and humus levels of the post−fire soils. The population of fungi was also lower than in the control soil. The applied methods of the fire site renewal have not had significant influence on the microbiological state of the soils under investigation. However, the rate of regeneration of the microbiocenosis after the fire in the forest soils was much faster in the case of artificial renewal than in natural succession.
5

Wpływ sposobu przygotowania gleby oraz nasadzeń sosną zwyczajną i olszą szarą na właściwości gleb zdegradowanych przez pożar

80%
Kaczmarek Z., Gajewski P., Mocek A.
Roczniki Gleboznawcze
|
2011
|
tom 62
|
nr 2
6

Właściwości silnie przesuszonych organicznych gleb popożarowych obiektu Sobin-Jędrzychów

80%
Bogacz A., Jedo M., Wozniczka P.
Woda - Środowisko - Obszary Wiejskie
|
2011
|
tom 11
|
nr 4[36]
7

Wlasciwosci fizyczno-chemiczne i biochemiczne gleb bielicowych szesc lat po pozarze calkowitym lasu

71%
Januszek K., Lasota J., Gruba P., Domicz G.
Acta Agraria et Silvestria. Series Silvestris
|
2001
|
tom 39
47-61
After a total forest fire the litter and mor horizons have been transformed into a mineral-humus horizons. Higher dehydrogenase and protease but lower phosphatase activities in mineral-humus horizons of post-fire soils as compared to mor humus of control soils were observed. In post-fire soils, lower exchangeable potassium and higher available phosphorus amounts were noted. In mineral-humus horizons of post-fire soils higher values of pH and higher amounts of iron, lead, cadmium and zinc but lower amounts of copper, extracted in 1M HCl, were determined.
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