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Title: Rate-weakening friction characterizes both slow sliding and catastrophic failure of landslides

Journal Article · · Proceedings of the National Academy of Sciences of the United States of America
 [1];  [1];  [1];  [1];  [2]
  1. Department of Geological Sciences, University of Oregon, Eugene, OR 97403,
  2. Department of Geological and Environmental Sciences, Stanford University, Stanford, CA 94305

Catastrophic landslides cause billions of dollars in damages and claim thousands of lives annually, whereas slow-moving landslides with negligible inertia dominate sediment transport on many weathered hillslopes. Surprisingly, both failure modes are displayed by nearby landslides (and individual landslides in different years) subjected to almost identical environmental conditions. Such observations have motivated the search for mechanisms that can cause slow-moving landslides to transition via runaway acceleration to catastrophic failure. A similarly diverse range of sliding behavior, including earthquakes and slow-slip events, occurs along tectonic faults. Our understanding of these phenomena has benefitted from mechanical treatments that rely upon key ingredients that are notably absent from previous landslide descriptions. Here, we describe landslide motion using a rate- and state-dependent frictional model that incorporates a nonlocal stress balance to account for the elastic response to gradients in slip. Our idealized, one-dimensional model reproduces both the displacement patterns observed in slow-moving landslides and the acceleration toward failure exhibited by catastrophic events. Catastrophic failure occurs only when the slip surface is characterized by rate-weakening friction and its lateral dimensions exceed a critical nucleation length h* that is shorter for higher effective stresses. However, landslides that are extensive enough to fall within this regime can nevertheless slide slowly for months or years before catastrophic failure. In conclusion, our results suggest that the diversity of slip behavior observed during landslides can be described with a single model adapted from standard fault mechanics treatments.

Research Organization:
Univ. of Oregon, Eugene, OR (United States)
Sponsoring Organization:
USDOE
Grant/Contract Number:
FE0013565
OSTI ID:
1312045
Alternate ID(s):
OSTI ID: 1469666
Journal Information:
Proceedings of the National Academy of Sciences of the United States of America, Journal Name: Proceedings of the National Academy of Sciences of the United States of America Vol. 113 Journal Issue: 37; ISSN 0027-8424
Publisher:
Proceedings of the National Academy of SciencesCopyright Statement
Country of Publication:
United States
Language:
English
Citation Metrics:
Cited by: 72 works
Citation information provided by
Web of Science

References (43)

Earthquake rupture propagation inferred from the spatial distribution of fault rock frictional properties journal June 2014
Comparison of smectite- and illite-rich gouge frictional properties: application to the updip limit of the seismogenic zone along subduction megathrusts journal October 2003
Stability of Steady Frictional Slipping journal June 1983
Rate and state dependent friction and the stability of sliding between elastically deformable solids journal September 2001
Landslide erosion controlled by hillslope material journal February 2010
Landslide triggering by rain infiltration journal July 2000
Earthflow sediment production and Holocene sediment record in a large Apennine catchment journal April 2013
A model of hydrological and mechanical feedbacks of preferential fissure flow in a slow-moving landslide journal January 2013
A visco-plastic model for slope analysis applied to a mudslide in Cortina d'Ampezzo, Italy journal August 1996
Residual strength of clays in landslides, folded strata and the laboratory journal March 1985
Geologic heterogeneity can produce aseismic slip transients: GEOLOGIC HETEROGENEITY AND ASEISMIC SLIP journal November 2012
Spatio-temporal complexity of slip on a fault journal January 1993
Coseismic and postseismic motion of a landslide: Observations, modeling, and analogy with tectonic faults journal October 2014
Regulation of landslide motion by dilatancy and pore pressure feedback journal January 2005
Mechanics of landslide initiation as a shear fracture phenomenon journal January 2004
Dynamics of Slow-Moving Landslides from Permanent Scatterer Analysis journal June 2004
Effects of variable normal stress on rock friction: Observations and constitutive equations journal January 1992
Observation and analysis of near-surface pore-pressure measurements in clay-shales slopes journal February 2011
A Scenario Study of Seismically Induced Landsliding in Seattle Using Broadband Synthetic Seismograms journal October 2013
Spontaneous and triggered aseismic deformation transients in a subduction fault model journal January 2007
Landslide mobility and hazards: implications of the 2014 Oso disaster journal February 2015
Landslides modeled as bifurcations of creeping slopes with nonlinear friction law journal December 1995
Rainfall, ground-water flow, and seasonal movement at Minor Creek landslide, northwestern California: Physical interpretation of empirical relations journal January 1987
A Pore-Pressure Diffusion Model for Estimating Landslide-Inducing Rainfall journal November 1994
Modeling of rock friction: 1. Experimental results and constitutive equations journal January 1979
Sediment yield, spatial characteristics, and the long-term evolution of active earthflows determined from airborne LiDAR and historical aerial photographs, Eel River, California journal June 2011
The use of Global Positioning System techniques for the continuous monitoring of landslides: application to the Super-Sauze earthflow (Alpes-de-Haute-Provence, France) journal February 2002
Earthquake nucleation on faults with rate-and state-dependent strength journal September 1992
Slip instability and state variable friction laws journal December 1983
Deep-seated downslope slip during strong seismic shaking: DEEP-SEATED DOWNSLOPE SLIP journal December 2011
Dilatancy, compaction, and slip instability of a fluid-infiltrated fault journal November 1995
Relations between hydrology and velocity of a continuously moving landslide—evidence of pore-pressure feedback regulating landslide motion? journal June 2009
Landslide subsurface slip geometry inferred from 3‐D surface displacement fields journal March 2015
Controls on the seasonal deformation of slow-moving landslides journal September 2013
Morphological and kinematic evolution of a large earthflow: The Montaguto landslide, southern Italy journal April 2013
Fault stability under conditions of variable normal stress journal August 1992
Acute Sensitivity of Landslide Rates to Initial Soil Porosity journal October 2000
The mobilization of debris flows from shallow landslides journal March 2006
Fast shearing of pre-existing shear zones in soil journal June 1996
Laboratory-Derived Friction laws and Their Application to Seismic Faulting journal May 1998
The contact between opposing fault surfaces at Dixie Valley, Nevada, and implications for fault mechanics journal January 1992
Landslide faults and tectonic faults, analogs?: The Slumgullion earthflow, Colorado journal January 1995
Kinematics of earthflows in the Northern California Coast Ranges using satellite interferometry journal October 2015