4.5 Article

Field and monitoring data of debris-flow events in the Swiss Alps

期刊

CANADIAN GEOTECHNICAL JOURNAL
卷 40, 期 1, 页码 161-175

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CANADIAN SCIENCE PUBLISHING
DOI: 10.1139/T02-087

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debris flow; Swiss Alps; monitoring; dynamic analysis

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Debris flow is a common process in the Swiss Alps and in other mountainous parts of the world. The understanding of debris-flow behaviour is essential to assess the hazards they present. An important approach towards improving the knowledge of debris-flow processes is the gathering of real-time data by debris-flow observation stations. Observation stations were established in three Swiss debris flow prone watersheds and equipped with video cameras, ultrasonic devices, a radar device, geophones, and rain gauges. In 2000, four significant debris flows were observed. The data provided useful information on the mechanics of debris flows and on the efficiency of the measuring devices. The observed debris flows are characterized by volumes between 5 000 and 35 000 m(3), front velocities ranging from 2 to 5 m/s, and peak discharges between 20 and 125 m(3)/s. The analysis of the monitoring data revealed that ultrasonic and radar devices are very helpful tools, whereas the quality of the geophone signal strongly depends on the substrate on which the instrument is installed (i.e., bedrock versus unconsolidated material). Video images are useful to verify the data obtained by the other devices. A dynamic analysis of one debris flow was carried out and the simulated results are in fair agreement with the observed data.

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