Abstract
The soils formed on sandstones in sessile oak forests (Quercetum montanum typicum Cer. et Jov. 1953) were researched in the area of Fruska Gora. On permanent sample plots established in management units ?Cortanovacka Forest-Hopovo-Velika Remeta? and ?Beocin-Manastir-Katanske Livade-Osovlje?, in the are of NP ?Fruska Gora?, aiming at the monitoring of the effect of light regime on the development of sessile oak progeny in the given environmental conditions, based on the morphogenetic characteristics of the soil and analytic values of the soil properties, and based on the soil classification by Skoric et al. (1985), the following two soil types were defined: acid brown soil (dystric cambisol), and illimerised soil (luvisol). Acid brown soil belongs to the form of medium deep soils, and illimerised soil is classified as deep soil.
Highlights
SOIL PROPERTIES IN SESSILE OAK FORESTS (Quercetum montanum typicum Čer. et Jov. 1953) IN THE AREA OF FRUŠKA GORA Abstract: The soils formed on sandstones in sessile oak forests (Quercetum montanum typicum Čer. et Jov. 1953) were researched in the area of Fruška Gora
Summary The study results on the soils formed on sandstones in monodominant sessile oak forest (Quercetum montanum typicum Čer. et Jov. 1953) in the area of the National Park “Fruška Gora” are presented
The following two soil types were determined in the study of sessile oak stands, based on the Soil Classification of Yugoslavia (Škorić et al, 1985): dystric brown soil, and illimerised soil
Summary
Извод: У раду су приказани резултати проучавања земљишта образованих на пешчарима у шумама храста китњака Et Jov. 1953) IN THE AREA OF FRUŠKA GORA Abstract: The soils formed on sandstones in sessile oak forests На подручју Националног парка „Фрушка Гора“ шуме храста китњака заузимају површину од 4.660,80 hа што представља 4,79% од укупне повр шине китњака у Србији. У североисточној Србији KošaninиKnežević (2005) су проучили посмеђено дистрично хумусно-сили катно земљиште на гнајсу у шуми храста китњака са власуљом У истраживаним састојинама храста китњака, према Класификацији зем љишта Југославије (Škorić et al, 1985), детерминисана су два типа земљишта, и то: a) кисело смеђе земљиште (дистрични камбисол) и б) илимеризовано (лесивирано) земљиште (лувисол).
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