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Geohazards in the Rječina valley in the past and present
Rjecina je najznacajniji vodotok Hrvatskog primorja, duljine 18, 7 km. Izvor je krsko vrelo smjesteno u podnožju planina Gorskog kotara, koji drenira podzemnu vodu iz prostranog krskog zaleđa i vec
Fizikalni model formiranja graničnog sloja
U radu se razmatraju temeljna načela za formiranje graničnog sloja kod ravninskih (2D) i prostornih (3D) objekata te je dat opis načina njegova formiranja pomoću fizikalnih modela HM 133 i HM 152
The paper deals with the basic principles of forming the boundary layer in linear (2D) and spatial (3D) objects, along with the description and manner of their forming using * Građevinski fakultet
A model of mudflow propagation downstream from the Grohovo landslide near the city of Rijeka (Croatia)
Abstract. Mudflows regularly generate significant human and property losses. Analyzing mudflows is important to assess the risks and to delimit vulnerable areas where mitigation measures are
Wind action on bridges according to the European standard
U ovom radu je sažeto opisano djelovanje vjetra na konstrukcije prema europskoj normi EN 1991-1-4:2005, a posebno je obrađeno djelovanje vjetra na mostove. Opisane su pojave vrtložnog odvajanja i
Application of Snapback Chronometry Method in Calculation of Regulation
Study shows applied chronometry method in work of standard cyclic construction machine to accomplish regulation through measured time cycle and compare measured effects with effects obtained with standard methodology of calculating hydraulic excavator practical achievement for gaining regulation.
Methods of Roughness Coefficient Determination in Natural Riverbeds
The roughness coefficient determination in natural river beds is based on the analysis of boundary layer development along the canal walls. The structure of the open canal can be very complex and
Function of the drainage-retaining Botonega channel in the integrated management of the Botonega accumulation
The retaining Botonega channel represents one of the most significant water-managing facilities of the Istrian peninsula. Its purpose is related solely to protection against high waters and erosion,