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Kryterium zrywności Hoek-Brown×Q-System×
DziedzinaInżynieria górniczaInżynieria górnicza
RodzinaProcess / pipelineProcess / pipeline
Rok powstania19801974
TwórcaEvert Hoek and E. T. BrownNick Barton (Norwegian Geotechnical Institute)
TypEmpirical criterion for rock mass strength predictionEmpirical index for tunnel support and stability prediction
Źródło pierwotneHoek, E., & Brown, E. T. (2002). The Hoek-Brown failure criterion and GSI: 2018 update. Journal of Rock Mechanics and Geotechnical Engineering, 10(2), 445-463. link ↗Barton, N., Lien, R., & Lunde, J. (1974). Engineering classification of rock masses for the design of tunnel support. Rock Mechanics, 6(4), 189-236. DOI ↗
Inne nazwyGeneralized Hoek-Brown Criterion, HB CriterionQ Index, Norwegian Geotechnical Institute Classification, Barton System
Pokrewne33
PodsumowanieThe Hoek-Brown Criterion, developed by Evert Hoek and E. T. Brown starting in 1980, is an empirical failure criterion that predicts the shear strength of rock masses as a function of confining pressure. It accounts for rock quality (via the Geological Strength Index, GSI) and thus bridges laboratory rock mechanics and field behavior. The criterion is widely used in mining for slope stability, pillar design, and stress analysis.The Q-System (NGI Index), introduced by Nick Barton and colleagues at the Norwegian Geotechnical Institute in 1974, is an alternative rock mass classification to RMR. It combines six parameters into a dimensionless index Q ranging from 0.001 to 1000, where higher Q values indicate better rock quality. The Q-System is particularly valued for tunnel and underground excavation design due to its explicit consideration of joint roughness and groundwater effects.
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ScholarGatePorównaj metody: Hoek-Brown Criterion · Q-System. Pobrano 2026-06-18 z https://scholargate.app/pl/compare