| Abstract: | Measurements of pore-fluid pressure and total bed-normal stress at the base of several ???10 m3 experimental debris flows provide new insight into the process of debris-flow deposition. Pore-fluid pressures nearly sufficient to cause liquefaction were developed and maintained during flow mobilization and acceleration, persisted in debris-flow interiors during flow deceleration and deposition, and dissipated significantly only during postdepositional sediment consolidation. In contrast, leading edges of debris flows exhibited little or no positive pore-fluid pressure. Deposition therefore resulted from grain-contact friction and bed friction concentrated at flow margins. This finding contradicts models that invoke widespread decay of excess pore-fluid pressure, uniform viscoplastic yield strength, or pervasive grain-collision stresses to explain debris-flow deposition. Furthermore, the finding demonstrates that deposit thickness cannot be used to infer the strength of flowing debris. |
| Genre: | Article |
| ProdID: | 70021283 |
| Citation Author: | Major, J. J.; Iverson, R. M. |
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| Citation End Page: | 1434 |
| Citation Issue: | 10 |
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| Citation Language: | English |
| Citation Larger Work Title: | Bulletin of the Geological Society of America |
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| Citation Number Of Pages: | 11 |
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| Citation Search Results Text: | Debris-flow deposition: Effects of pore-fluid pressure and friction concentrated at flow margins; 1999; Article; Journal; Bulletin of the Geological Society of America; Major, J. J.; Iverson, R. M. |
| Citation Start Page: | 1424 |
| Citation Volume: | 111 |
| Citation Year: | 1999 |
| Type: | citation/reference |
| Text: | Debris-flow deposition: Effects of pore-fluid pressure and friction concentrated at flow margins; 1999; Article; Journal; Bulletin of the Geological Society of America; Major, J. J.; Iverson, R. M. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| Date Other: | Fri, 1 Jan 1999 00:00 -0600 |
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