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Znanstveno-stručno i staleško glasilo
Hrvatskoga šumarskoga društva
Journal of Forestry Society of Croatia
      Prvi puta izašao 1877. godine i neprekidno izlazi do današnjeg dana
   ISSN No.: 0373-1332              UDC 630*
upute autorima

select * from clancislEN where brojid=200405 and arb=1 order by id

Pernar, N., Vukelić, J., Bakšić, D., Baričević, D. UDK 630* 114.4 + 188
An Insight Into Genesis and Properties of Soil in the Riparian Region of North-Eastern Baranja     pdf     HR     EN 223
Summary: Pedological and vegetational research into riparian forests of north-eastern Baranja was conducted during the summer of 2002. In each of the 12 locations defined by micro-relief and flora a pedological profile was opened in order to do morphological research and soil sampling for physical-chemical analyses.A total of six forest communities were identified in the study area: the purple willow thicket (Salicetum purpureae Wend.-Zel. 1952), the forest of almond willow (Salicetum triandrae Malc. 1929), the forest of white willow with bedstraw (Galio-Salicetum albae Rauš 1973), the forest of white willow and black poplar (Salici albae-Populetum nigrae Tx. 1931), the forest of white and black poplar (Populetum nigro-albae Slavn. 1952) and the forest of spreading elm and narrow-leaved ash (Fraxino-Ulmetum laevis Slav. 1952).
The pedogenesis of the study area is characterised by distinct effects of the Danube hydrological regime. As a rule, the soil texture is of loamy to sandy character. Only in micro-relief depressions away from the riverbed (mostly in the surface part) may the texture be somewhat heavier (clayey loam to light clay). A characteristic feature of the soil in this region is a prominent texture stratigraphy. Apart from alluviation as a geological and pedogenetic process, these forest ecosystems are characterised by high organic production, which is sporadically significantly manifested in pedosphere humisation. The dominant soil type was found to be fluvisol, regularly carbonate, while gleysol and humofluvisol are represented to a much lesser degree.
All these three soil types differ from one another in terms of ecological production. It should be pointed out that ecological-productive differences within one type are in some cases much larger than among the types, which is closely connected to the features of the water regime properties and the texture.
From the aspect of pedotaxonomic nomenclature, in our view it is not necessary to classify some soils from the alluvial plain into a separate type. This refers to humofluvisols with a shallow A-horizon. An approach to the WRB classification seems to be a better solution, according to which the majority of such soils are classified into a group of fluvisols (except those with the A-horizon thicker than 25 cm).

Key words: Baranja riparian forests; fluvisol; humofluvisol; pedophysiographic features
Krpan, A. P. B., Poršinsky, T. UDK 630* 363
Efficiency of Mechanical Felling and Processing in Soft and Hardwood broadleaved stands – Part 2: Efficiency of harvesters in the culture of soft broadleaf trees     pdf     HR     EN 233
Zečić, Ž., Krpan, A. P. B., Poršinsky, T., Šušnjar, M. UDK 630* 375
Efficiency of tractors 8090 and 9078 in shelterwood fellings of stands in Požega mountains     pdf     HR     EN 245
Pilaš, I., Potočić, N. UDK 630* 561 + 116
Depedence of intraseasonal variations of tree stem diameter changes, electrical resistanee of cambial zone and groundwater in common oak stand (Q. robur L.)     pdf     HR     EN 255
Popijač, M., Seletković, I., Volner, M., Lovrenčić, I., Barišić, D., Kezić, N. UDK 630* 160 + 161
Dynamics of 137Cs and 40K Movement in Silver fir Trees on Sljeme Mountain     pdf     HR     EN 269
Posavec, S. UDK 630* 652
Specificy of Bussines Analyses Entities in Managing with Forest and Forest Land     pdf     HR     EN 279
Štorga, D. UDK 630* 582 + 525
Application of GIS in Stand Extraction According to Dendrometric Parameters     pdf     HR     EN 287

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