Flume Experiments for Investigation of Rainfall-Induced Slope Failure

Article Preview

Abstract:

The rainfall-induced slope failure is the major geo-hazard all over the world including Malaysia. Number of studies done already to investigate the process of slope failure, however the parameters that control the initiation of flowslide type of failure is still lacking. In tropical areas different mass movements occur from erosion to flow type of failure, in order to understand the mechanism will help to mitigate the posed risk. The flowslide is also type of slope failure that mostly occur in granular type soils, when initiated attain the higher velocity and fluid like motion, and it is dangerous than other types of landslides. The flowslide type of slope failure mainly due to rainfall. Field studies are timing consuming and expensive, while numerical studies requires lot of characteristics related to geology of the materials. Therefore laboratory flume experiments used in order to understand the mechanism and behavior of slope failure by changing different parameters such as density, rainfall intensity, thickness and initial moisture condition. The model slope prepared by sandy type of the soil and failure induced by artificial rainfall by installing the sprinklers above the model flume. During the experiments the pore pressure and moisture content were measured. From the detailed experimental study it was observed density of soil slope controls the initiation of the flowslide type failure. Small density of the soil slope suffers from flowslide type of the failure at smaller rainfall intensity. However in case of higher density even higher rainfall intensity accompanied with significant initial moisture conditions did not trigger the flowslide. The erosion gullies formed from toe to crest of the slope in the case of dense slope. The measurements of moisture content at the lower parts of the slope can be used as early warning of slope failure, however piezometers less reliable for prediction of slope failure in advance. Before large failure the settlement occur at the crest of the slope.

You might also be interested in these eBooks

Info:

Pages:

49-56

Citation:

Online since:

June 2015

Export:

Price:

Permissions CCC:

Permissions PLS:

Сopyright:

© 2015 Trans Tech Publications Ltd. All Rights Reserved

Share:

Citation:

* - Corresponding Author

[1] C. -C. Hunag and C. -L. Lo, Simulation of subsurface flows associated with rainfall-induced shallow slope failures , GeoEngineering, vol. 8, pp.101-111, (2013).

Google Scholar

[2] G. Acharya Analysing the interactions between waterinduced soil erosion and shallow landslides , Doctor of Philosophy, Civil and Natural Resources Engineering, University of Canterbury Canterbury, (2011).

Google Scholar

[3] G. Crosta, Rainfall threshold regionalization: an aid for landslide susceptibility zonation, Environmental Geology, vol. 35, pp.131-245, (1998).

DOI: 10.1007/s002540050300

Google Scholar

[4] G. -r. Zhang, Y. -j. Qian, Z. -c. Wang, and B. Zhao, Analysis of rainfall infiltration law in unsaturated soil slope, The Scientific World Journal, vol. 2014, p.7, (2014).

DOI: 10.1155/2014/567250

Google Scholar

[5] M. T. J. Terlien, The determination of statistical and deterministic hydrological landslide-triggering thresholds, Environmental Geology, vol. 35, pp.124-130, 1998/08/01 (1998).

DOI: 10.1007/s002540050299

Google Scholar

[6] B. Collins and D. Znidarcic, Stability analyses of rainfall induced landslides, Journal of Geotechnical and Geoenvironmental Engineering, vol. 130, pp.362-372, (2004).

DOI: 10.1061/(asce)1090-0241(2004)130:4(362)

Google Scholar

[7] Y. Sahin, Laboratory tests to study stability mechanism of rainfall infiltrated unsaturated fine-grained soil slopes developing into shallow landslides and their hydraulic properties, Civil Engineering, İzmir Institute of Technology, (2013).

Google Scholar

[8] D. G. Fredlund and N. R. Morgenstern, Stress state variables for unsaturated soils, Journal of the Geotechnical Engineering Division, vol. 103, pp.447-466, (1977).

DOI: 10.1061/ajgeb6.0000423

Google Scholar

[9] N. Lu and W. J. Likos, Unsaturated Soil Mechanics: Wiley, (2004).

Google Scholar

[10] K. A. Johnson and N. Sitar, Hydrologic conditions leading to debris-flow initiation, Canadian Geotechnical Journal, vol. 27, pp.789-801, 1990/12/01 (1990).

DOI: 10.1139/t90-092

Google Scholar

[11] Wolle C.M. and W. Hachichi, Rain-induced landslides in southeastern Brazil, in 12th International Conf. on Soil mechanics and Foundation Engineering, Rio de janeiro, 1989, pp.1639-1642.

Google Scholar

[12] R. -H. Chen, K. -J. Kuo , and W. -N. Chien Failure mechanism of granular soil slopes under high intensity rainfalls , Journal of GeoEngineering, vol. 7, pp.21-31, (2012).

Google Scholar

[13] D. Eckersley. (1990, Instrumented Laboratory Flowslides. Geotechnique 40, 489-502. Available: http: /www. icevirtuallibrary. com/content/article/10. 1680/geot. 1990. 40. 3. 489.

DOI: 10.1680/geot.1990.40.3.489

Google Scholar

[14] G. Wang and K. Sassa, Pore-pressure generation and movement of rainfall-induced landslides: Effects of grain size and fine-particle content, Engineering Geology, vol. 69, pp.109-125, (2003).

DOI: 10.1016/s0013-7952(02)00268-5

Google Scholar

[15] K. Sako, R. Kitamura, and R. Fukagawa, Study of slope failure due to rainfall: A comparison between experiment and simulation, in Unsaturated Soils ed: ASCE, 2006, pp.2324-2325.

DOI: 10.1061/40802(189)197

Google Scholar

[16] G. Acharya, T. A. Cochrane, T. Davies, and E. Bowman, The influence of shallow landslides on sediment supply; a flume-based investigation using sandy soil, presented at the International Association for Computer Methods and Advances in Geomechanics (IACMAG), (2009).

DOI: 10.1016/j.enggeo.2009.06.008

Google Scholar

[17] Orense Rolando. P, Slope failures triggered by heavy rainfall, Philippine Engineering Journal, vol. 25, p.73–90, (2005).

Google Scholar

[18] H. Rahardjo, T. T. Lee, E. C. Leong, and R. B. Rezaur, Response of a residual soil slope to rainfall, Candian Geotechnical Journal, vol. 42, pp.340-351, 2005/04/01 (2005).

DOI: 10.1139/t04-101

Google Scholar

[19] L. M. Lee, A. Kassim, and N. Gofar, Performances of two instrumented laboratory models for the study of rainfall infiltration into unsaturated soils, Engineering Geology, vol. 117, pp.78-89, (2011).

DOI: 10.1016/j.enggeo.2010.10.007

Google Scholar

[20] S. M. Springman, C. Jommi, and P. Teysseire, Instabilities on moraine slopes induced by loss of suction: A case history, Geotechnique, vol. 53, pp.3-10, (2003).

DOI: 10.1680/geot.2003.53.1.3

Google Scholar

[21] J. A. Blatz, N. J. Ferreira, and J. Graham, Effects of near-surface environmental conditions on instability of an unsaturated soil slope, Canadian Geotechnical Journal, vol. 41, pp.1111-1126, 2004/12/01 (2004).

DOI: 10.1139/t04-058

Google Scholar

[22] F. Cai and K. Ugai, Numerical analysis of rainfall effects on slope stability, International Journal of Geomechanics, vol. 4, pp.69-78, (2004).

DOI: 10.1061/(asce)1532-3641(2004)4:2(69)

Google Scholar

[23] Y. Okura, H. Kitahara, H. Ochiai, T. Sammori, and A. Kawanami, Landslide fluidization process by flume experiments, Engineering Geology, vol. 66, pp.65-78, (2002).

DOI: 10.1016/s0013-7952(02)00032-7

Google Scholar

[24] G. Wang and K. Sassa, An experimental study on the rainfall-induced-flowslides, in Environmental Forest Science. vol. 54, K. Sassa, Ed., ed: Springer Netherlands, 1998, pp.591-598.

DOI: 10.1007/978-94-011-5324-9_62

Google Scholar

[25] R. P. Orense, S. Shimoma, K. Maeda, and I. Towhata, Instrumented model slope failure due to water seepage, Journal of Natural Disaster Science, vol. 26, pp.15-26, (2004).

DOI: 10.2328/jnds.26.15

Google Scholar

[26] A. Tohari, M. Nishigak, and M. Komatsu, Laboratory rainfall-induced slope failure with moisture content measurement, Journal of Geotechnical and Geoenvironmental Engineering Geology, vol. 133, pp.575-587, (2007).

DOI: 10.1061/(asce)1090-0241(2007)133:5(575)

Google Scholar

[27] L. Picarelli and L. Olivares, Modelling of flowslides behaviour for risk mitigation, in Physical Modelling in Geotechnics, ed: Taylor & Francis, (2006).

DOI: 10.1201/noe0415415866.ch8

Google Scholar

[28] R. M. Iverson and R. G. Lahusen, Dynamic pore-pressure fuctuations in rapidly shearing granular materials, Science, vol. 246, pp.796-799, (1989).

DOI: 10.1126/science.246.4931.796

Google Scholar

[29] H. Moriwaki, T. Inokuchi, T. Hattanji, K. Sassa, H. Ochiai, and G. Wang, Failure processes in a full-scale landslide experiment using a rainfall simulator, Landslides, vol. 1, pp.277-288, 2004/12/01 (2004).

DOI: 10.1007/s10346-004-0034-0

Google Scholar

[30] S. G. Catane, M. A. H. Zarco, C. J. N. Cordero, R. A. N. Kaimo, and J. Ricarido M. Saturay, Laboratory Experiments on Steady State Seepage-Induced Landslides Using Slope Models and Sensors, (2011).

Google Scholar