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 "slug": "centrifuge-model-test",
 "title": "Centrifuge model test",
 "updated": "2026-10-15",
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 "excerpt": "A centrifuge model test, also called a centrifuge test, is a geotechnical modeling technique that spins scaled soil models at N times Earth's gravity, reproducing prototype stresses for foundations, slopes, tunnels, and earthquake studies.",
 "snippet": "A centrifuge model test, also called a centrifuge test, is a geotechnical modeling technique that spins scaled soil models at N times Earth's gravity, reproducing prototype stresses for foundations, slopes, tunnels, and earthquake studies.",
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 "markdown": "# Centrifuge model test\n\nA centrifuge model test is a physical modeling technique in geotechnical engineering in which a scaled soil–structure model is spun in a centrifuge so that it experiences N times Earth's gravity, reproducing the stress state of the full-scale prototype at 1/N linear scale.<sup>[1](https://geomechanics.org.au/wp-content/uploads/2025/11/AGJ19-4_Fahey.pdf)</sup><sup> • </sup><sup>[2](https://www.issmge.org/uploads/publications/53/115/P00293.pdf)</sup> The test produces stress, deformation, and failure-mechanism data at prototype stress levels, which is why roughly half of the physical modeling contributions to the journal [Géotechnique](https://www.edgepedia.org/geotechnique) use a centrifuge to make model stresses comparable to field scale.<sup>[3](https://eprints.soton.ac.uk/420591/1/Geotechnique_60th_physical_modelling_DJW.pdf)</sup> Typical problems include foundations, slopes, retaining structures, tunnels, piles, pipelines, offshore spud-cans and suction caissons, slope stability, and unsaturated soil behavior.<sup>[4](https://www.frontiersin.org/journals/built-environment/articles/10.3389/fbuil.2020.00121/full)</sup><sup> • </sup><sup>[5](https://www.tudelft.nl/citg/over-faculteit/afdelingen/geoscience-engineering/laboratory/facilities/geotechnical-centrifuges)</sup>\n\n| Key fact | Value |\n|---|---|\n| Scaling principle | All linear dimensions reduced by \\( 1/N \\), acceleration increased to N g; a 0.5 m layer at 200 g matches the stress profile of a 100 m field layer<sup>[1](https://geomechanics.org.au/wp-content/uploads/2025/11/AGJ19-4_Fahey.pdf)</sup> |\n| Stress and strain scale factors | 1, the main advantage over 1 g models<sup>[6](https://mostwiedzy.pl/pl/business/publication/download/1/derivation-of-the-scaling-laws-used-in-geotechnical-centrifuge-modelling-application-of-dimensional-_64995.pdf)</sup> |\n| Time scaling | Dynamic events \\( 1/N \\) (a 20 s earthquake at 50 g lasts 0.4 s); diffusion and consolidation \\( 1/N^{2} \\)<sup>[7](https://www.earthquakecountry.org/library/12481.pdf)</sup> |\n| Consolidation acceleration | A clay layer that takes 1 year to consolidate is modeled in about a 1-hour test at 100 g<sup>[8](https://onlinepubs.trb.org/Onlinepubs/trr/1992/1336/1336-004.pdf)</sup> |\n| Grain-size rule | No measurable scale effect when grain size is below about 3–5% of the smallest significant problem dimension<sup>[1](https://geomechanics.org.au/wp-content/uploads/2025/11/AGJ19-4_Fahey.pdf)</sup>; reasonable results with prototype soil where structural dimensions are at least 20 times the grain size<sup>[9](https://ascelibrary.org/doi/10.1061/%28ASCE%29GT.1943-5606.0000517)</sup> |\n| Facilities | Approximately 60 active geotechnical centrifuge facilities worldwide: 16 in Japan, 14 in the USA, 7 in China, 6 in the UK, 3 in Canada<sup>[10](https://scholarsmine.mst.edu/cgi/viewcontent.cgi?article=3261&context=icrageesd)</sup> |\n| Largest seismic-capable machines | UC Davis 9-m centrifuge: about 1,550 kg of soil at 75–80 g, representing roughly 50 m of prototype soil<sup>[11](https://www.frontiersin.org/journals/built-environment/articles/10.3389/fbuil.2025.1568832/full)</sup><sup> • </sup><sup>[4](https://www.frontiersin.org/journals/built-environment/articles/10.3389/fbuil.2020.00121/full)</sup> |\n\n## How it works\n\nSoil behavior depends on effective stress (soil stress carried by grain contacts, controlling soil strength), and self-weight stress in a 1 g model of scale \\( 1/N \\) is N times too small. Spinning the model to N g multiplies the body force by N, so the vertical overburden stress at depth \\( z/N \\) in the model equals that at depth z in the prototype; at 50 g, a 0.6 m soil layer reproduces the vertical effective stress profile of a 30 m layer at 1 g.<sup>[1](https://geomechanics.org.au/wp-content/uploads/2025/11/AGJ19-4_Fahey.pdf)</sup><sup> • </sup><sup>[4](https://www.frontiersin.org/journals/built-environment/articles/10.3389/fbuil.2020.00121/full)</sup> [Dimensional analysis](https://www.edgepedia.org/dimensional-analysis) via the Buckingham Π theorem confirms that stress and strain carry scaling factors of 1.<sup>[6](https://mostwiedzy.pl/pl/business/publication/download/1/derivation-of-the-scaling-laws-used-in-geotechnical-centrifuge-modelling-application-of-dimensional-_64995.pdf)</sup>\n\nTime does not scale uniformly. Dynamic events run N times faster in the model, while diffusion processes such as consolidation run \\( N^{2} \\) times faster.<sup>[7](https://www.earthquakecountry.org/library/12481.pdf)</sup><sup> • </sup><sup>[12](https://tc104-issmge.com/wp/wp-content/uploads/2023/07/Malcolm-Bolton-Schofield-Lecture.pdf)</sup> When shaking and pore-pressure diffusion are concurrent, as in liquefaction, the two scales conflict; the standard resolution is to increase the pore-fluid viscosity by a factor N, using silicone oil (preferred), glycerol–water, or cellulose-based mixtures, so that both the cyclic period and the diffusion time scale correctly.<sup>[7](https://www.earthquakecountry.org/library/12481.pdf)</sup><sup> • </sup><sup>[6](https://mostwiedzy.pl/pl/business/publication/download/1/derivation-of-the-scaling-laws-used-in-geotechnical-centrifuge-modelling-application-of-dimensional-_64995.pdf)</sup> For prototypes larger than a facility can accommodate at \\( 1/N \\), generalized (two-stage) scaling described in a 2005 Géotechnique paper by S. Iai, T. Tobita, and T. Nakahara divides the scaling factor into a 1 g stage μ and a centrifuge stage η.<sup>[13](https://doi.org/10.1680/geot.2005.55.5.355)</sup><sup> • </sup><sup>[14](https://www.sciencedirect.com/science/article/abs/pii/S0267726120311064)</sup>\n\n## How it is done\n\nThe practitioner first selects a container: plane-strain boxes with thick Perspex sides allow in-flight viewing and particle image velocimetry (PIV) of the model cross-section; at HKUST, model boxes reach 1.5 m × 1.5 m in plan and 1.0 m high.<sup>[15](https://gcf.hkust.edu.hk/sites/default/files/GCF%20manual.pdf)</sup>\n\n**Soil preparation** differs by material. Clay is usually consolidated at 1 g under a piston or dead load, then reconsolidated in flight to remove suction; a 400 mm kaolin layer may need 16 to 18 hours at 100 g to reach a normally consolidated state.<sup>[15](https://gcf.hkust.edu.hk/sites/default/files/GCF%20manual.pdf)</sup> Sand models are prepared by air pluviation, with nozzle size controlling flow rate and drop height controlling relative density.<sup>[15](https://gcf.hkust.edu.hk/sites/default/files/GCF%20manual.pdf)</sup>\n\n**Instrumentation** is saturated and calibrated before spinning: pore pressure transducers require vacuum saturation at about 100 kPa and linear voltage–pressure calibration. The total imbalance force at the test g-level must not exceed ±100 kN at HKUST. Measurement uses LVDTs, laser displacement sensors, and commercial load and pressure cells.<sup>[15](https://gcf.hkust.edu.hk/sites/default/files/GCF%20manual.pdf)</sup> Stopping the centrifuge to build an embankment in stages induces significant errors, so in-flight construction is preferred where possible.<sup>[1](https://geomechanics.org.au/wp-content/uploads/2025/11/AGJ19-4_Fahey.pdf)</sup>\n\n## Origin\n\nThe idea of using centrifugal acceleration to increase body forces on reduced-size models was published in the Mémoires of the Académie des Sciences, summarized in the Comptes Rendus, with examples including the [Britannia Bridge](https://www.edgepedia.org/britannia-bridge); its history is documented in a 1989 Géotechnique paper by W. H. Craig.<sup>[16](https://doi.org/10.1680/geot.1989.39.4.697)</sup><sup> • </sup><sup>[17](https://www.earthquakecountry.org/library/12480.pdf)</sup> An American mention was made at Columbia University, for mining problems, stating that model material weight must increase in the same ratio that model scale decreases; the same principle was published independently in the USSR in 1932 by N. N. Davidenkov and G. I. Pokrovsky.<sup>[17](https://www.earthquakecountry.org/library/12480.pdf)</sup>\n\nThe first Soviet centrifuge, built in 1932–3 at the VODGEO Institute in Moscow, was assembled from 1929 Ford automobile parts, with a 1 m effective radius arm rotating up to 280 rpm.<sup>[17](https://www.earthquakecountry.org/library/12480.pdf)</sup> The technique was used in Russia from the 1930s but not taken up in the west until the 1970s, when Andrew Schofield built one at UMIST; A. N. Schofield described the resulting Cambridge operations in his 1980 Géotechnique paper.<sup>[18](https://doi.org/10.1680/geot.1980.30.3.227)</sup><sup> • </sup><sup>[17](https://www.earthquakecountry.org/library/12480.pdf)</sup><sup> • </sup><sup>[19](https://geomechanics.org.au/wp-content/uploads/2017/07/AGS_Journal-Vol52-02_01.pdf)</sup> ISSMGE established an international technical committee on centrifuge modeling in 1981.<sup>[17](https://www.earthquakecountry.org/library/12480.pdf)</sup><sup> • </sup><sup>[4](https://www.frontiersin.org/journals/built-environment/articles/10.3389/fbuil.2020.00121/full)</sup>\n\n## Variants\n\n**Beam versus drum.** Beam centrifuges carry large payloads at radii up to 9 m; drum centrifuges reach up to 500 g but require small models and show higher distortions at small radius.<sup>[6](https://mostwiedzy.pl/pl/business/publication/download/1/derivation-of-the-scaling-laws-used-in-geotechnical-centrifuge-modelling-application-of-dimensional-_64995.pdf)</sup> The HKUST drum is an 850 g-ton, 250 g, 2.2 m diameter machine spinning a 3480 kg payload at up to about 450 rpm.<sup>[2](https://www.issmge.org/uploads/publications/53/115/P00293.pdf)</sup>\n\n**Dynamic variants.** Cambridge's bumpy road apparatus (two tracks, about 10 cycles at 1–2 Hz) and the stored angular momentum (SAM) actuator deliver sinusoidal base shaking in flight.<sup>[7](https://www.earthquakecountry.org/library/12481.pdf)</sup> Servo-hydraulic shakers reproduce recorded earthquake motions, including the 1989 Loma Prieta Corralitos record<sup>[8](https://onlinepubs.trb.org/Onlinepubs/trr/1992/1336/1336-004.pdf)</sup>, and the hammer-exciter plate method with absorptive-lined container walls lets a confined sample model a stratum of infinite lateral extent.<sup>[20](https://onlinelibrary.wiley.com/doi/10.1002/eqe.4290180806)</sup> KAIST pairs a 4-degree-of-freedom in-flight robot with an on-arm shaking table taking a 700 kg payload over 20–300 Hz.<sup>[21](https://hystec.koced.or.kr/en/sub32)</sup>\n\n**Major facilities.** Cambridge operates a 10 m rotor arm with a 4 m working radius reaching 155 g with a 900 kg model plus container. The UC Davis 9-m centrifuge is one of only two worldwide able to shake models with over 1,500 kg of soil.<sup>[4](https://www.frontiersin.org/journals/built-environment/articles/10.3389/fbuil.2020.00121/full)</sup><sup> • </sup><sup>[11](https://www.frontiersin.org/journals/built-environment/articles/10.3389/fbuil.2025.1568832/full)</sup> The Southampton UKCRIC facility commissioned in 2024 uses an Actidyn model C67 beam centrifuge with a 3 m platform radius, 130 g at 208 rpm, a two-step automatic in-flight balancing system, and the DigiDAQ system logging up to 1 MHz.<sup>[22](https://www.issmge.org/uploads/publications/53/125/ECPMG2024-34.pdf)</sup>\n\n## Applications\n\nCentrifuge tests quantify bearing capacity and settlement of foundations, tunnel and retaining-structure behavior, pile and pipeline response, offshore anchoring, and dike and embankment performance.<sup>[5](https://www.tudelft.nl/citg/over-faculteit/afdelingen/geoscience-engineering/laboratory/facilities/geotechnical-centrifuges)</sup><sup> • </sup><sup>[15](https://gcf.hkust.edu.hk/sites/default/files/GCF%20manual.pdf)</sup><sup> • </sup><sup>[23](https://plateformes.univ-gustave-eiffel.fr/en/detailed-view/centrifugeuse-geotechnique)</sup> In earthquake geotechnics, models of a silt layer over Nevada sand shaken at 0.65 g reproduced sand boils and water collection at the sloped silt–sand interface, and dynamic soil–structure interaction tests quantified radiation damping consistent with classical formulae.<sup>[8](https://onlinepubs.trb.org/Onlinepubs/trr/1992/1336/1336-004.pdf)</sup><sup> • </sup><sup>[20](https://onlinelibrary.wiley.com/doi/10.1002/eqe.4290180806)</sup> Drum centrifuges target long-distance landslides, debris flows, and hillslope erosion<sup>[2](https://www.issmge.org/uploads/publications/53/115/P00293.pdf)</sup>, and rainfall devices support studies of rainfall-induced slope failure.<sup>[24](https://www.mdpi.com/2076-3417/16/5/2442)</sup> A coordinated testing program across nine centrifuge centers benchmarked laterally loaded monopiles in sand and reproduced a similar prototype pile response across facilities despite differences in setups and pile geometries.<sup>[25](https://nottingham-repository.worktribe.com/index.php/output/57902268/centrifuge-modelling-considerations-of-laterally-loaded-monopiles-in-sand)</sup>\n\n## Limitations and alternatives\n\n**Particle-size effects.** [Grain size](https://www.edgepedia.org/grain-size) must stay below about 3–5% of the smallest significant problem dimension<sup>[1](https://geomechanics.org.au/wp-content/uploads/2025/11/AGJ19-4_Fahey.pdf)</sup>; Fuglsang and Ovesen suggested a model footing diameter of 30 times particle size.<sup>[10](https://scholarsmine.mst.edu/cgi/viewcontent.cgi?article=3261&context=icrageesd)</sup> Shear rupture bands about 10 particle diameters thick do not scale, so larger structures soften earlier at smaller proportional displacement.<sup>[12](https://tc104-issmge.com/wp/wp-content/uploads/2023/07/Malcolm-Bolton-Schofield-Lecture.pdf)</sup> A trapdoor-based modeling-of-models validation found reasonable results with prototype soil where structural dimensions are at least 20 times the grain size.<sup>[9](https://ascelibrary.org/doi/10.1061/%28ASCE%29GT.1943-5606.0000517)</sup>\n\n**Field curvature and boundaries.** The radial acceleration field varies across the model, promoting a more dilative response and lower excess porewater pressures than a uniform gravitational field; in the LEAP-2015/2017 exercise, a 5° sloping Ottawa F65 sand layer was repeated at six facilities at 23–50 g and radii 1.0–5.06 m, and displacement results varied with model scale, so numerical simulation should be performed at model scale.<sup>[26](https://www.mdpi.com/2673-7094/5/2/29)</sup> Modeling-of-models experiments generally support scaling-law validity but reveal variability across facilities due to sample preparation, base motion control, and acceleration-field differences<sup>[26](https://www.mdpi.com/2673-7094/5/2/29)</sup>; Ovesen's classic 1975 study showed consistent unit bearing capacity for 10 mm and 30 mm models of the same prototype footing.<sup>[3](https://eprints.soton.ac.uk/420591/1/Geotechnique_60th_physical_modelling_DJW.pdf)</sup>\n\n**Other limits.** Models use reconstituted soils with idealized stratigraphy and cannot reproduce complex construction processes.<sup>[4](https://www.frontiersin.org/journals/built-environment/articles/10.3389/fbuil.2020.00121/full)</sup> Compared with 1 g physical modeling, the centrifuge's stress and strain scale factors of 1 remove the self-weight stress deficit<sup>[6](https://mostwiedzy.pl/pl/business/publication/download/1/derivation-of-the-scaling-laws-used-in-geotechnical-centrifuge-modelling-application-of-dimensional-_64995.pdf)</sup>; rocking-foundation centrifuge tests have complemented 1 g shaking table tests of the same problems.<sup>[4](https://www.frontiersin.org/journals/built-environment/articles/10.3389/fbuil.2020.00121/full)</sup> The scaling laws and similitude questions underlying these comparisons were cataloged in a 2007 International Journal of Physical Modelling in Geotechnics paper by J. Garnier and colleagues.<sup>[27](https://doi.org/10.1680/ijpmg.2007.070301)</sup>\n\n## References\n\n1. [The geotechnical centrifuge facility at the University of Western Australia (Fahey et al., Australian Geomechanics, December 1990)](https://geomechanics.org.au/wp-content/uploads/2025/11/AGJ19-4_Fahey.pdf)\n2. [HKUST 850 g-ton drum centrifuge (ISSMGE paper)](https://www.issmge.org/uploads/publications/53/115/P00293.pdf)\n3. [Physical modelling in Géotechnique (D.J. White et al.)](https://eprints.soton.ac.uk/420591/1/Geotechnique_60th_physical_modelling_DJW.pdf)\n4. [NHERI Centrifuge Facility: Large-Scale Centrifuge Modeling in Geotechnical Research (Frontiers, 2020)](https://www.frontiersin.org/journals/built-environment/articles/10.3389/fbuil.2020.00121/full)\n5. [TU Delft Geotechnical Centrifuges facility page](https://www.tudelft.nl/citg/over-faculteit/afdelingen/geoscience-engineering/laboratory/facilities/geotechnical-centrifuges)\n6. [Derivation of the scaling laws used in geotechnical centrifuge modelling, application of dimensional analysis and Buckingham Π theorem (Konkol)](https://mostwiedzy.pl/pl/business/publication/download/1/derivation-of-the-scaling-laws-used-in-geotechnical-centrifuge-modelling-application-of-dimensional-_64995.pdf)\n7. [Centrifuge Modelling in Earthquake Geotechnical Engineering (V.S. Chandrasekaran)](https://www.earthquakecountry.org/library/12481.pdf)\n8. [Dynamic Centrifuge Modeling (Transportation Research Record 1336)](https://onlinepubs.trb.org/Onlinepubs/trr/1992/1336/1336-004.pdf)\n9. [Validation of Centrifuge Model Scaling for Soil Systems via Trapdoor Tests (J. Geotech. Geoenviron. Eng., 2011)](https://ascelibrary.org/doi/10.1061/%28ASCE%29GT.1943-5606.0000517)\n10. [Recent Advances in Centrifuge Modeling of Seismic Shaking (Kutter, State-of-the-Art)](https://scholarsmine.mst.edu/cgi/viewcontent.cgi?article=3261&context=icrageesd)\n11. [NHERI centrifuge facility: systems-scale hypergravity modeling (Frontiers, 2025)](https://www.frontiersin.org/journals/built-environment/articles/10.3389/fbuil.2025.1568832/full)\n12. [Bolton Schofield Lecture, 8th ICPMG (UWA)](https://tc104-issmge.com/wp/wp-content/uploads/2023/07/Malcolm-Bolton-Schofield-Lecture.pdf)\n13. [S. Iai, T. Tobita, T. Nakahara (2005). Generalised scaling relations for dynamic centrifuge tests. Géotechnique.](https://doi.org/10.1680/geot.2005.55.5.355)\n14. [Verification of generalized scaling laws: Two centrifuge tests of a liquefiable sloping deposit (Soil Dynamics and Earthquake Engineering)](https://www.sciencedirect.com/science/article/abs/pii/S0267726120311064)\n15. [HKUST Geotechnical Centrifuge Facility User Manual](https://gcf.hkust.edu.hk/sites/default/files/GCF%20manual.pdf)\n16. [W. H. Craig (1989). Édouard Phillips (1821–89)and the idea of centrifuge modelling. Géotechnique.](https://doi.org/10.1680/geot.1989.39.4.697)\n17. [The Seven Ages of Centrifuge Modelling (W.H. Craig)](https://www.earthquakecountry.org/library/12480.pdf)\n18. [A. N. Schofield (1980). Cambridge Geotechnical Centrifuge Operations. Géotechnique.](https://doi.org/10.1680/geot.1980.30.3.227)\n19. [Genesis of the National Geotechnical Centrifuge Facility – a 30 year perspective (Randolph et al., Australian Geomechanics)](https://geomechanics.org.au/wp-content/uploads/2017/07/AGS_Journal-Vol52-02_01.pdf)\n20. [Centrifugal modelling of dynamic soil-structure interaction (Weissman & Prevost, EESD 1989)](https://onlinelibrary.wiley.com/doi/10.1002/eqe.4290180806)\n21. [KAIST Geotechnical Centrifuge Testing Center (KOCED)](https://hystec.koced.or.kr/en/sub32)\n22. [The new geotechnical centrifuge facility in the UKCRIC (University of Southampton, 2024)](https://www.issmge.org/uploads/publications/53/125/ECPMG2024-34.pdf)\n23. [Université Gustave Eiffel Nantes Geotechnical Centrifuge](https://plateformes.univ-gustave-eiffel.fr/en/detailed-view/centrifugeuse-geotechnique)\n24. [Centrifuge Modeling of Failure Behaviors and Mechanical Response of Bridge Piers on High Expansive Soil Slopes (2026)](https://www.mdpi.com/2076-3417/16/5/2442)\n25. [Centrifuge modelling considerations of laterally loaded monopiles in sand (Int. J. Physical Modelling in Geotechnics 26(2), 93-104, DOI 10.1680/jphmg.25.00046, online December 2025)](https://nottingham-repository.worktribe.com/index.php/output/57902268/centrifuge-modelling-considerations-of-laterally-loaded-monopiles-in-sand)\n26. [Influence of Acceleration Field Curvature on Physical and Numerical Modeling of Liquefiable Slopes in Geotechnical Centrifuge Tests](https://www.mdpi.com/2673-7094/5/2/29)\n27. [J. Garnier and colleagues (2007). Catalogue of scaling laws and similitude questions in geotechnical centrifuge modelling. International Journal of Physical Modelling in Geotechnics.](https://doi.org/10.1680/ijpmg.2007.070301)\n\n---\n*Topic: Encyclopedia › Technology and the built world › Architecture, buildings, and civil works*\n\n*Initially written Sep 29, 2026 · Edited: Oct 15, 2026*\n\n*Copyright 2026 EdgeChat AI, a subsidiary of Biostate AI.*\n\nLicense: Edgepedia Community License 1.0, https://www.edgepedia.org/edgepedia/license\n",
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 "speakable": "A centrifuge model test, also called a centrifuge test, is a geotechnical modeling technique that spins scaled soil models at N times Earth's gravity, reproducing prototype stresses for foundations, slopes, tunnels, and earthquake studies."
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