broj: 5-6/2024
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| RIJEČ UREDNIŠTVA | ||
| Uredništvo HŠD-a | ||
| The scientific and professional character of Forestry Journal pdf HR EN | 217 | |
| IZVORNI ZNANSTVENI ČLANCI | ||
| Igor Poljak, Zlatko Šatović, Antonio Vidaković, Katarina Tumpa, Marilena Idžojtić | UDKps://doi.org/10.31298/sl.148.5-6.1 | |
| Population variability of rosemary willow (Salix eleagnos Scop.) based on leaf morphometry: evidence of small and large-leaf morphotypes pdf HR EN | 219 | |
| Ivan Perković, David Počekal, Vibor Roje, Darko Bakšić, Nikola Pernar | UDKps://doi.org/10.31298/sl.148.5-6.2 | |
| Influence of the parent material on calcocambisol in the area of the Plitvice lakes national park pdf HR EN | 237 | |
| Summary Calcocambisol (brown soil on limestone and dolomite) is one of the most common soil types in Croatia, and it is the dominant soil type developed on karst, as well as in the area of the Plitvice Lakes National Park, which is located in the karst area. As its name suggests, calcocambisol is developed on different carbonate substrates, which are different in terms of chemical composition as well as in terms of rock erosion. In the area of the National Park, 30 pedological profiles have been opened, 18 of which were on limestone and 12 on dolomite. In the field, ectomorphological and endomorphological soil parameters were determined. The following parameters were determined on the collected soil samples in the humus-accumulative (A) and cambic (B) horizons: particle size distribution of the soil, soil reaction, i.e. pH-value in water and CaCl2 solution, carbonate content, and total carbon and total nitrogen content using the dry burning method. The highest differences in ectomorphological parameters between limestone and dolomite were found in the classification of rockiness and stoneness, where they ranged from very low to very high on limestone, while they were absent on dolomite. On the profiles of calcocambisol on top of dolomite, a higher proportion of sand fractions and less clay than on calcocambisol on top of limestones was found. The dominant soil textural class of calcocambisol on top of limestone was silty clay, while in calcocambisol on top of dolomite it was silty clay loam. The pH-values of the soil and the proportion of CaCO3 on calcocambisol on top of dolomite were statistically significantly higher than on calcocambisol on top of limestone. Since there was no great difference in the fractions of organic carbon and total nitrogen between calcocambisol on top of limestones and dolomites, there was also no great difference in the C/N ratio. The average C/N ratio along the entire profile of calcocambisol on top of limestone and dolomite was 14, i.e. decomposition continued undisturbed and there was no accumulation of raw humus. The hypotheses in this paper were confirmed, and clear differences in the investigated ectomorphological (rockiness and stoniness) and endomorphological (particle size distribution, pH-values and CaCO3 content) properties between calcocambisol on top of limestone and dolomite were observed. Keywords: calcocambisol, limestone, dolomite, Plitvice Lakes National Park | ||
| Mirzeta Memišević Hodžić, Dalibor Ballian | UDKps://doi.org/10.31298/sl.148.5-6.3 | |
| Phenological traits of leafing and leaf retention of black poplar (Populus nigra L.) in the clonal archive in Žepče, Bosnia and Herzegovina pdf HR EN | 249 | |
| Ahmet Acarer | UDKps://doi.org/10.31298/sl.148.5-6.4 | |
| Brown bear (Ursus Arctos L.) distribution model in Europe: Current situation and the potential role of climate change pdf HR EN | 261 | |
| Mevlüt Zenbilci, Serkan Özdemir, Alican Çivg˘a, Yasin Ünal, Idris Og˘urlu | UDKps://doi.org/10.31298/sl.148.5-6.5 | |
| Habitat suitability modeling of wild goat (Capra aegagrus Erxleben, 1777) in different periods pdf HR EN | 273 | |
| Gizem Misirliog˘lu, Selçuk Gümüş | UDKps://doi.org/10.31298/sl.148.5-6.6 | |
| Time-dependent change of natural vegetation on forest road fill slopes and its effects on erosion decrease pdf HR EN | 285 | |