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ŠUMARSKI LIST 1-2/1974 str. 33     <-- 33 -->        PDF

13.
Muc k enha u s en, E. (1962): Entstehung, Eingenschaften und Systematik
der Bodentypen und Bodensystematik. Handbuch der Pflanzenernahrung und
Diingung. Wien — New York.
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M ii c k e n h a us e n, E. (1966): Bodentypen und Bodensystematik. Handbuch
der Pflanzenernahrung und Diingung. Wien — New York.
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N e u g e b a u e r, V., Ć i r i ć, M., et al. (1963): Klasifikacija zemljišta Jugoslavije.
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16.
* * * Soil Survey Manual by Soil Survey Staff. USD of Agricult., Washington,
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škorić, A., Filipovski, Gj., Ćirić, M. (1972): Klasifikacija tala Jugoslavije,
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Summary


CLASSIFICATION OF SOILS
OF THE CENTRAL MOUNTAIN REGION OF SLAVONIA


In pedogenetic investigations and the classification of the soils of the
central mountains in Slavonia (Psunj, Papuk, Krndija, Požeška gora, Dilj gora)
the division of soils into two basic highest categories, order and class, was
accepted (E. Miickenhausen, 1962, 1966, 1970). The »uniform criterion of soil
classification from soil type to lower systematic categories« was applied, as
it was done in our pedogenetic and cartographic work in the Sava River Valley


(P. Kovačević, M. Kalinić, et al., 1967, 1972). This paper presents the following
classificational soil units: Soil type, soil subtype, soil variety, soil genus, soil
species and soil phase. (Table I — IV).
A) Terrestrial Soils of Mountainous Relief (over approx. 230—250 m. a. s. 1.)
Sierozems (Rhegosols) on clastic rocks, the structural composition of the profile:
(A)-C or (A)-C-R;
Sierozems (Lithosols) on hard rocks, the structural composition of the profile:
(A)-C or (A)-R;
Colluvial (Deluvial) soils, poorly developed with (A)- or A-horizonts, formed by
recent diluvion of eroded material. Subtypes: calcareous and dystric
siliceous colluvium;
Rendzinas and Pararendzinas, with the structural composition of the profile:
A-AC-R and A-AC-CR, etc.
Rankers (Humous-Siliceous Soils) of predominantly A-AC-CR composition, and
on hard rocks of A-R structural composition of the profile;


Eutric Brown Soils (Eutric Cambisols) developed on limy marls, limestones,
calcarenites, and in places also on non-calcareous loams, clayey loams or
solifluctional sediments which may cover the mentioned rocks. The structural
composition of the profile: A-(B)-C or A-(B)-CR. In the central mountains,
the subtypes eutric brown soils were determined;


Ilimerized Soils (Luvisols) have the ArA;rB-C profile structure. They are developed
on pleistocene loams and clays, loesslike sediments, sandy-loamy
substrata or loamy sands of the mountainous region of the Dilj, Krndija,
Požeška Gora mountains. They are frequently stands of Sessile Oak and
Common Hornbeam, Sessile Oak and Turkey Oak or Sessile Oak and
Hungarian Oak forests;


Dystric Brown Soils (Dystric Cambisols, Acid Brown Soils) are developed on
intrusive, metamorphic and sediment siliceous rocks and are of A-(B)-C
profile structure. In the central mountain region they are characteristic
of the Beech and Fir forests, in particular. A discription is given of typical
acid brown soils, humous-dystric acid brown soils, brown acid ilimerized
soils an the soil stage related to humous-dystric brown soil and brown
podsolic soil;


Pseudogleys (Planosols). Mainly slighty expressed pseudogleys were determined,
as well as short wet phases, and more often lessive-pseudogleys. The soils