Temat: Vaccinio uliginosi-Betuletum - Katalog OPAC zbiorów

Skocz do pozycji: 1.

Tytuł:: Struktura i dynamika opadu organicznego w wybranych drzewostanach Slowinskiego Parku Narodowego w latach 2003-2005
The structure and dynamics of litterfall in forest stands in the Slowinski National Park in 2003-2005
Autorzy:: Parzych, A.
Trojanowski, J.
Powiązania:: https://bibliotekanauki.pl/articles/46069.pdf
Data publikacji:: 2009
Wydawca:: Instytut Badawczy Leśnictwa
Tematy:: Slowinski Park Narodowy
sklad frakcyjny
opad organiczny
bor sosnowy
drzewostany sosnowo-brzozowe
zespol Vaccinio uliginosi-Betuletum pubescentis
dynamika opadu
biomasa
struktura
zespoly roslinne
zespol Empetro nigri-Pinetum
Źródło:: Leśne Prace Badawcze; 2009, 70, 1; 41-48
1732-9442
2082-8926
Pojawia się w:: Leśne Prace Badawcze
Dostawca treści:: Biblioteka Nauki

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Tytuł:: Porównanie zasobów materii organicznej oraz wybranych wskaźników stanu ekochemicznego gleb w zespołach Empetro nigri-Pinetum i Vaccinio uliginosi-Betuletum pubescentis Słowińskiego Parku Narodowego
Comparing Empetro nigri-Pinetum and Vaccinio uliginosi-Betuletum pubescentis soils in terms of organic matter stocks and ecochemical indices in the Slowinski National Park
Autorzy:: Jonczak, J.
Parzych, A.
Powiązania:: https://bibliotekanauki.pl/articles/1311665.pdf
Data publikacji:: 2015
Wydawca:: Instytut Badawczy Leśnictwa
Tematy:: lesnictwo
ekosystemy lesne
zespoly roslinne
zespol Empetro nigri-Pinetum
zespol Vaccinio uliginosi-Betuletum pubescentis
gleby lesne
wlasciwosci fizyczne
wlasciwosci chemiczne
materia organiczna
zawartosc wegla organicznego
zawartosc azotu
stosunek wegla do azotu
odczyn gleby
wlasciwosci sorpcyjne
zawartosc metali
metale
formy biodostepne
Arenosols
soil organic matter
sorptive properties
nutrients
aluminium toxicity
Opis:: We conducted comparative studies on soil organic matter stocks and indices of the soil’s ecochemical state under Empetro nigri-Pinetum (En-P) and Vaccinio uliginosi-Betuletum pubescentis (Vu-Bp) in the Słowiński National Park. The investigated plant communities are associated with Arenosols that developed from eolian sands and are exposed to high groundwater levels. The presence of fossil Histosol at a depth of 75 cm in the Vu-Bp stand, which lies below the current groundwater level, is the factor that sets both stands apart. The fossil soil strongly differs from Arenosol in terms of its chemical composition. A high abundance of nutrients in bioavailable forms in the soil is one of the reasons for natural renewal of downy birch in the stand, which presence in turn affects the turnover of elements and the properties of Arenosol. The results of our studies confirm the existence of strong feedback between the soil and plant communities. Soils under the mixed pine-birch Vu-Bp stand are characterized by smaller stocks of organic matter and total organic carbon (TOC) contained in the ectohumus as compared to the soils under the pure pine En-P stand. The opposite is found in the humic horizon. Additionally, in the Vu-Bp stand we observed greater accumulation of total nitrogen (TN) in ectohumus, which is reflected in lower TOC:TN ratios. The contents of TN and TOC:TN ratios in humic horizons were similar in both stands. The soils under En-P were more strongly acidified, especially in O-horizons. Mineral horizons in both stands were characterized by a very small sorptive capacity, which increased in ectohumus and fossil soil. Significant differences between the stands were observed in the ionic composition of sorptive complexes. The soils under Vu-Bp stand were more strongly saturated with basic cations, predominantly calcium. In soil solums of both stands, we observed a deficit of bioavailable potassium and magnesium, which was partially compensated by significant amounts of these components in ectohumus and fossil soil in the Vu-Bp stand. Despite a strongly acidic pH, molar Ca:Al ratios suggest that there are no phytotoxic effects due to free aluminium in ectohumus, while they are unlikely in mineral horizons. The risk of phytotoxic effects is reduced by the influx of calcium from groundwater.
Źródło:: Leśne Prace Badawcze; 2015, 76, 4; 360-369
1732-9442
2082-8926
Pojawia się w:: Leśne Prace Badawcze
Dostawca treści:: Biblioteka Nauki

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