SM
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silty sand (symbol)
List different methods of natural transporting of soil.
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Glaciers, moving water, wind, settling out in salt water, settling out in fresh
water, due to gravity movement downslope
Consistency of Cohesive Soil depends on :
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Depends on the water content of the soil.
( At very low water contents, soil sample behaves like a solid )
( At very high water contents, may flow like a liquid)
Landslides are a
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type of slope failure or downward sediment
Soil is classified according to characteristic properties such as :
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Cohesion: non-cohesive soils ( gravel, sand ) and cohesive soils ( silt, clay )
Grain size: coarse-grained soils ( sand, gravel ) and fine-grained soils ( silt,
clay )
The three types of shear failure of soil are
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general shear failure (bulging / tilting)
local shear failure (slight bulging)
punching shear failure (little to no bulging)
,What are the characteristics of gravel, sands and silts
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cohesionless, non-plastic, and granular
Soil Shear Strength
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frictional resistance to sliding
interlocking between particles
cohesion between adjacent particles
Moisture content
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Mass of water / mass of solid
Classifications of soil by particle size
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Boulder
cobble
Gravel (G)
Sand (S)
, Clay (C)
Silt (M)
Unified Soil Classification System - Cohesionless
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cohesionless
1st Letter:
G = gravel
S = sand
2nd Letter:
W = well graded
P = poorly graded
M = >12% silt
C = >12% clay
Cohesive
1st Letter:
M = silt
C = clay
2nd Letter:
H = high (plasticity)
L = low (plasticity)
What are the characteristics of organic soils
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weak and deform excessively under load and should not be used as
foundations
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silty sand (symbol)
List different methods of natural transporting of soil.
Give this one a try later!
Glaciers, moving water, wind, settling out in salt water, settling out in fresh
water, due to gravity movement downslope
Consistency of Cohesive Soil depends on :
,Give this one a try later!
Depends on the water content of the soil.
( At very low water contents, soil sample behaves like a solid )
( At very high water contents, may flow like a liquid)
Landslides are a
Give this one a try later!
type of slope failure or downward sediment
Soil is classified according to characteristic properties such as :
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Cohesion: non-cohesive soils ( gravel, sand ) and cohesive soils ( silt, clay )
Grain size: coarse-grained soils ( sand, gravel ) and fine-grained soils ( silt,
clay )
The three types of shear failure of soil are
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general shear failure (bulging / tilting)
local shear failure (slight bulging)
punching shear failure (little to no bulging)
,What are the characteristics of gravel, sands and silts
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cohesionless, non-plastic, and granular
Soil Shear Strength
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frictional resistance to sliding
interlocking between particles
cohesion between adjacent particles
Moisture content
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Mass of water / mass of solid
Classifications of soil by particle size
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Boulder
cobble
Gravel (G)
Sand (S)
, Clay (C)
Silt (M)
Unified Soil Classification System - Cohesionless
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cohesionless
1st Letter:
G = gravel
S = sand
2nd Letter:
W = well graded
P = poorly graded
M = >12% silt
C = >12% clay
Cohesive
1st Letter:
M = silt
C = clay
2nd Letter:
H = high (plasticity)
L = low (plasticity)
What are the characteristics of organic soils
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weak and deform excessively under load and should not be used as
foundations