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ŠUMARSKI LIST 11-12/2003 str. 68     <-- 68 -->        PDF

A. Tomašević. B. Kulić, Ž. Španjol, T. Kružić: RAZVOJ SASTOJINE I MELIORATIVNA ULOGA KULTURE ... Šumarski list br. II 12. CXXVII (2003). 579-596


8. LITERATURA - References


Bezak, K., 1992: Tablice drvnih masa cera, crnog Šume u Hrvatskoj (monografija), str. 33-77,


bora i običnog bora, Radovi br. 5 - izvanredno GZH, Zagreb.


izdanje, Šumarski institut Jastrebarsko, Zagreb. Seletković,Z. iZ. Katušin, 1992: Klima Hrvat-
Horvat, A., 1965: Melioracije degradiranih Šumskih ske. Šume u Hrvatskoj (monografija), str.


terena, svez. 2 - Krš, Zagreb. 13-18, GZH, Zagreb.


Klepac,D., 1963: Rast i prirast šumskih vrsta drveća Trijastić, I. 1998: Fitogeografsko raščlanjenje kli-


i sastojina, Zagreb. mazonalne šumske vegetacije Hrvatske. Šumar-


Klepac,D., 1965: Uređivanje šuma, Zagreb. ski list 122 (9 10): 407—421.


Matijević, B., 1994: Meliorativna uloga kulture xxx : Meteorološka podloga za potrebe prostornog


crnog bora na području šumskog predjela planiranja općine Rijeka, sažetak, Zagreb 1992.


"Lonja-Biljin" šumarije Rijeka, Diplomski rad, XXX : Program za gospodarenje borovim kulturama


Šumarski fakultet Sveučilišta u Zagrebu. 1977-1986.


Pranjić, A., N. Lukić, (1998): Izmjera šuma, Za- XXX : Program za gospodarenje šumama krša G.J.
greb. Oštrovica, 1988-1997.


Rauš, Đ., I. Trinajstić, J. Vukelić, J. Medve-
dović, 1992: Biljni svijet hrvatskih šuma.


SUMMARY: The climate of the Rijeka region has a maritime character.
According to Koppen ´s classification, parts of the Rijeka Commune along the
sea belong to class Cfax", with the mean annual air temperature of 13.6 "C
and the mean annual precipitation quantity of 1421.2 mm. Relative humidity
in this region ranges from the maximum, occurring in December (70 %), to
the minimum in July (52 %).


The geological substrate of this area is mainly made up of layered limestones,
and to a smaller degree of dolomites of different geological ages dating
from the Mesozoic period of Jurassic and cretaceous formations.
Depending on the geological substrate of either the limestone or the dolomite,
a large number of developmental stages and soil forms have developed in this
area, such as:


- brown red soil (terra rossa)


brown soil on limestone and dolomite (calcocambisol), supporting a
culture of black pine (Pinus nigra)


In the past, this area abounded in high forests of predominantly pubescent
oak (Quercus pubescens,) and Montpelier maple (Acer monspesulanum).
However, man s activities led to serious devastation of the forests, while many
were also burned in order to convert the soil into agricultural land and pastures.
At present, apart from agricultural land, bare rocky terrain and artificial
cultures of black pine, this area is covered with the vegetation of
xerothermal low forests and garrigues that represent degraded stages of the
former high oak forests.


Floristic and vegetational research has shown that the studied culture of
black pine was established in the climatozonal association of pubescent oak
fQuercus pubescens) at the transition between the Mediterranean-littoral vegetation
belt in the sub-Mediterranean vegetation zone with the association
Querco-Carpinetum orientalis H-ić 1939 and the Mediterranean-mountainous
vegetation zone with the epi-Mediterranean vegetation zone characterised by
the association Ostryo-Quercetum pubescentis /HtJ Trinajstić 1997. With
regard to abundant presence of hop hornbeam fOstryo carpinifolia,) and a
complete absence of oriental hornbeam fCarpinus orientalist it can be


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