rockfall参数选取参考

更新时间:2023-05-12 05:51:21 阅读: 评论:0

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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