Rocscience Coefficient of Restitution Table | ||||||||||
RN ( Normal ) | RT ( Tangential ) | Type | Verification | Location | ||||||
Min | Max | Mean | Standard | Min | Max | Mean | Standard | |||
Deviation | Deviation | |||||||||
0.370 | 0.420 | 0.870 | 0.920 | Hard surface paving | Tested using simulated | Glenwood Canyon, Colorado, USA | ||||
0.330 | 0.370 | 0.830 | 0.870 | Bedrock or boulders with little soil | rockfalls of similar size and shape of a previous rockfall. | |||||
or vegetation | ||||||||||
0.300 | 0.330 | 0.830 | 0.870 | Talus with little vegetation | ||||||
0.300 | 0.330 | 0.800 | 0.830 | Talus with some vegetation | ||||||
0.280 | 0.320 | 0.800 | 0.830 | Soft soil slope with little | ||||||
vegetation | ||||||||||
0.280 | 0.320 | 0.780 | 0.820 | Vegetated soil slope | ||||||
0.315 | 0.064 | 0.712 | 0.116 | Limestone face | Tested on restoration-blasting slopes made of four types of materials; blast-generated rock fragments, partially vegetated scree on berms, uncovered blast piles, and vegetated quarry waste. | Limestone quarry in England | ||||
0.303 | 0.080 | 0.615 | 0.170 | Partially vegetated limestone | ||||||
scree | ||||||||||
0.315 | 0.064 | 0.712 | 0.116 | Uncovered limestone blast pile | ||||||
0.251 | 0.029 | 0.489 | 0.141 | Vegetated covered limestone pile | ||||||
0.276 | 0.079 | 0.835 | 0.087 | Chalk face | Chalk quarry in England | |||||
0.271 | 0.018 | 0.596 | 0.085 | Vegetated chalk scree | ||||||
0.384 | 0.133 | 0.687 | 0.130 | Wood platform slope at 45 degrees was ud as a control for the field tests they did. | Tested as control parameters | Western North Carolina for | ||||
Interstate 40. | ||||||||||
0.200 | 0.530 | Dolomitic limestone boulders on rocky surfaces and on talus desposits | Consisted of hand made throws and free fall tests by fragmentation of rock using explosives, of dolomitic limestone boulders on rocky surfaces and on talus deposit of the landslide fans. Also ud back-analysis, and information from Urciuoli. | Atrani, Campania, Southern Italy | ||||||
0.100 | 0.200 | Remolded pyroclastic from the terraces situated at the ba of the cliff | ||||||||
0.000 | 0.240 | Impacts on detritus of the fans prent at the foot of a rock cliff | ||||||||
0.393 | 0.567 | Soil | Tested by dropping 3 to 5 cm cuboid and angular granite rock fragments onto slopes | Hong Kong | ||||||
0.453 | 0.737 | Shotcrete | ||||||||
0.487 | 0.910 | Rock slope | ||||||||
0.500 | 0.950 | Bedrock | Referenced from tests carried out by Barbieri et al. | Italcementi works at Castellammare di Stabia(northern slope of the Sorrentine Peninsula), and the area of Atrani. | ||||||
0.350 | 0.850 | Bedrock covered by large blocks | di Stabia(northern slope of the Sorrentine Peninsula), and the area of Atrani. | |||||||
0.300 | 0.700 | Debris formed by uniform | ||||||||
distributed elements | ||||||||||
0.250 | 0.550 | Soil covered by vegetation | ||||||||
0.530 | 0.990 | Clean hard bedrock | ||||||||
0.400 | 0.900 | Asphalt roadway | ||||||||
0.350 | 0.850 | Bedrock outcrops with hard surface, large boulders | ||||||||
0.320 | 0.820 | Talus cover | ||||||||
0.320 | 0.800 | Talus cover with vegetation | ||||||||
0.300 | 0.800 | Soft soil, some vegetation | ||||||||
0.370 | 0.420 | Smooth hard surfaces and paving | Developed by obrvation and literature review | Colordado, USA | ||||||
0.330 | 0.370 | Most bedrock and boulder fields | ||||||||
0.300 | 0.330 | Talus and firm soil slopes | ||||||||
0.280 | 0.300 | Soft soil slopes | ||||||||
0.870 | 0.920 | Smooth hard surfaces such as | ||||||||
pavement or smooth bedrock surfaces | ||||||||||
0.830 | 0.870 | Most bedrock surfaces and talus with no vegetation | ||||||||
0.820 | 0.850 | Most talus slopes with some low | ||||||||
vegetation | ||||||||||
0.800 | 0.830 | Vegetated talus slopes and soil slopes with spares vegetation | ||||||||
0.780 | 0.820 | Brush covered soil slope | ||||||||
0.530 | 0.040 | 0.990 | 0.040 | Clean Hard Bedrock | a) rolled many rocks down the slope to verify ud values b) comparison to historical rockfall events at site | Mountain road, near Bolzano, Sothtyrol, Italy | ||||
0.350 | 0.040 | 0.850 | 0.040 | Bedrock outkrop | ||||||
0.320 | 0.040 | 0.820 | 0.040 | Talus cover | ||||||
0.320 | 0.040 | 0.800 | 0.040 | Talus with vegetation | ||||||
0.400 | 0.040 | 0.900 | 0.040 | Asphalt paving | ||||||
0.530 | 0.040 | 0.990 | 0.040 | Clean Hard Bedrock | default program values ud | 170m deep open pit, Tasmania, Australia (overall pit angle between 55 and 65 degrees) | ||||
0.350 | 0.040 | 0.850 | 0.040 | Bedrock outcrop | ||||||
0.480 | 0.190 | 0.530 | 0.170 | Concrete | inver calculation of paths - standard deviations emed to large | Takamatsu, Japan | ||||
0.470 | 0.300 | 0.550 | 0.230 | Weathered Rock | ||||||
0.480 | 0.000 | 0.530 | 0.000 | Concrete | inver calculation of paths, roughness of 7.9 degrees for concrete, 9.3 for rock | |||||
0.470 | 0.000 | 0.550 | 0.000 | Weathered Rock | ||||||
0.850 | 0.000 | 0.530 | 0.000 | Concrete | inver calculation of paths | |||||
1.000 | 0.000 | 0.550 | 0.000 | Weathered Rock | ||||||
0.530 | 0.040 | 0.990 | 0.040 | Bedrock | Estimation, block diameters 10 to 30 cm | Fjord valley, State of Sogn og Fjordane, Norway | ||||
0.500 | 0.060 | 0.700 | 0.060 | Blockfield | ||||||
0.500 | 0.060 | 0.650 | 0.060 | Blockfield with bushes and small | ||||||
trees | ||||||||||
0.500 | 0.060 | 0.500 | 0.060 | Blockfield with forest | ||||||
0.300 | 0.060 | 0.800 | 0.060 | Top-soil with vegetation | ||||||
0.400 | 0.040 | 0.900 | 0.040 | Asphalt paving | ||||||
0.350 | 0.040 | 0.850 | 0.040 | Gravel road | ||||||
0.500 | 0.800 | Sparsley forested slope is covered by a veneer of very fine weathered talus derived from weak shisto units underlying the limestone cap. | Calculated from historic rockfall | Sunnybrae, (interior of )British Colombia, Canada | ||||||
0.500 | 0.800 | Limestone on bare uniform talus slope formed of basalt fragments with a modal size of 5 cm. | Calculated from historic rockfall | Hedley, (southern interior of ) British Colombia, Canada | ||||||
0.700 | 0.900 | rectangular bolder of metamorphod tuff on bare rock and a steep snow covered shelf. | Calculated from historic rockfall | Squamish Highway, north of Vancouver British Colombia, Canada | ||||||
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