Pregled bibliografske jedinice broj: 645184
Development of Hydro-Debris 2D and 3D applicable for stony debris flow
Development of Hydro-Debris 2D and 3D applicable for stony debris flow // Landslide and flood hazard assessment, Abstract Proceedings / Arbanas, Mihalić, S. ; Arbanas, Ž. (ur.).
Zagreb: Grad Zagreb ; Ured za upravljanje u hitnim situacijama, 2013. str. 32-32 (predavanje, međunarodna recenzija, sažetak, ostalo)
CROSBI ID: 645184 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Development of Hydro-Debris 2D and 3D applicable for stony debris flow
Autori
Yamashiki, Yosuke ; Kurokawa, Shota ; Žic, Elvis ; Takahashi, Tamotsu ; M. Ramy Rozainy, M. A. Z. ; Sušanj, Ivana ; Fujiki, Shigeo
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, ostalo
Izvornik
Landslide and flood hazard assessment, Abstract Proceedings
/ Arbanas, Mihalić, S. ; Arbanas, Ž. - Zagreb : Grad Zagreb ; Ured za upravljanje u hitnim situacijama, 2013, 32-32
ISBN
978-953-7479-28-2
Skup
1st Regional Symposium on Landslides in the Adriatic-Balkan Region (ReSyLAB), 3rd Workshop of the Japanese-Croatian Project "Risk Identification and Land-Use Planning for Disaster Mitigation of Landslides and Floods in Croatia"
Mjesto i datum
Zagreb, Hrvatska, Zagreb, Croatia
Vrsta sudjelovanja
Predavanje
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
Hydro-Debris 2D ; Hydro-Debris 3D ; Euler-Lagrangian Coupling method ; debris flow ; Grohovo landslide ; experimental and numerical studies
Sažetak
The aim of this survey is to develop numerical prediction method "Hydro-Debris 2D" and "Hydro-Debris 3D" applicable for Croatian catchment. They are Euler-Lagrangian Coupling method for stony debris flow with particle sizes, applicable both for experimental field and estimation of real rock movement. We investigate velocity of each sediment movement through steep-slope channel experimental study, and then compared with numerical simulation results using Hydro-Debris 2D. We employed three different slope angles (15, 20, and 25 degrees) both for experimental and numerical studies. The average velocity values are well simulated in numerical study within 10% difference, in most cases, while some specific case differs much, especially at the last part of debris flow. Based on these results, Hydro-Debris 3D model has also developed and applied for Grohovo Landslide zone. Although there is no "experimental" study for the landslide zone, our model may predict movement of individual particles, as we assumed that the grain sizes are uniform.
Izvorni jezik
Engleski
Znanstvena područja
Građevinarstvo
POVEZANOST RADA
Projekti:
114-0982709-2549 - HIDROLOGIJA OSJETLJIVIH VODNIH RESURSA U KRŠU (Ožanić, Nevenka, MZOS ) ( CroRIS)
Ustanove:
Građevinski fakultet, Rijeka