Field identification procedures (excluding particles > 7.5cms & basic frictions on estimated weights |
Group symbol |
Typical names |
permeability if compacted |
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Coarse grain soils |
Gravels more than half of coarse friction |
clean gravel (little or no lines) |
wide range in grain size & substantial amounts of intermediate particle size |
CW |
well graded gravels,gravel sand mixtures, little or no line |
pervious |
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predominantly one size or a range of sizes with some intermediate size missing |
GP |
poorly graded gravels, gravel-sand mixtures, line or not |
very pervious |
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gravel with fines (lines) |
non plastic fines |
GM |
silty gravels poorl graded gravel-sand-salt mixtures |
semi pervious |
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plastic fines |
GC |
clayey gravels, poorly graded gravel sand clay mixtures |
impervious |
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Sands (more than half of coarse friction |
clean sands |
wider range in grain sizes and substantial amounts of all intermediate particle sizes |
SW |
well graded sands, gravelly sands, little or no lines |
pervious |
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predominantly one size or a range of sizes with some intermediate sizes missing |
SP |
poorly graded gravelly sands little or no lines |
pervious |
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non plastic fines |
SM |
silty sands poorly graded sand salt mixtures |
semipervious |
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sands with fines | |||||||||||||||||||||||
sands with fines |
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plastic fines |
SC |
claysands poorly graded sand-salt mixtures |
impervious |
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Fine grains soils
more than half is smaller than |
Identification procedures on fraction smaller than n°sieve size |
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dry strength (crushing characteristics) |
dilatancy (reaction to shaking |
Toughtness (consistency near plastici -ty limit |
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Silts and clays (liquid limit less than 50 |
none to slight |
quick to slow |
none |
ML |
inorganic silt and very fine sands, rocks, lime, silty or clayey fine sands with slight plasticity |
semiperviour |
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medium to high |
none to very slow |
medium |
CL |
inorganic clays of low to medium plasticity, gravelly clays, sandy clays, silty clays lean clays |
imp |
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slight to medium |
slow |
slight |
OL |
organic silts & organics silt-clay of low plasticity |
semiimpervious |
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Silts and Clays liquid limit greater than 50 |
slight to medium |
slow to none |
slight to medium |
MH |
inorganic silts, micaceous or diatomaceous fine sandy or silty soils,elastic silte |
semi -impervious |
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high to very high |
none |
high |
CH |
inorganic clays of high plasticity fat clays |
impervious |
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medium to high |
none to very slow |
slight to medium |
OH |
organic clays of medium to high plasticity |
imp |
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Highly organic soil |
Readily identified by color, odor, spongy feel and fibrous texture |
Pr |
pest ans other highly organic |
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Soils Hydrologic Properties |
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Soil Permeability |
Site Classification |
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coeffi- cient of permea- bility k |
relative permea- bility |
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Soil type |
site class |
general conditions required for such classification |
conditions found during site classification survey that are indicative of the class |
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cm/sec |
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field pum -ping test, relia -ble if well done |
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cons tant head perm- eame -ter liable |
com- puta- tion from grain size |
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relative to water table level |
relative to surface water accumulation |
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10 |
high |
clean gravel |
soil type |
ter- rain |
rain or irrigation |
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1 |
high |
coarse sand |
A- severe |
water table frequently above bottom of the system |
ground -water within 0.3 m of bottom of system |
any |
any |
any |
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0.1 |
medium |
rollig head permeameter |
reliable |
medium sands |
water table occasionally above bottom of the system and surface water accumulates & remains for long periods of soil surrounding the system |
ground -water within 0.3 m of bottom of system |
GC, SC, CL, CH, OH |
Any |
Any |
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0.01 |
medium |
fine sand, sands&gravels mixtures |
B - bad |
water table occasional above bottom of the system and surface water accumulates & remains for short periods |
ground -water within 1.5m of bottom of system |
GW, GP, SW, SP, GM, SM, ML, OL, MH |
any |
any |
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0.001 |
medium |
very fine sand |
water table never above the bottom of the system but surface water accumulates and remains for long periods in soil surrounding the system |
no ground water encoun -tered |
GC, SC, CI, CH, OH |
any |
7.6 cms or > / month or 50cms / year |
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0.0001 |
low |
un- relia- ble |
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silty sand, organic silt |
C - moderate |
water table never above the bottom of the system but surface water accumulates and remains for long periods in soil surrounding the system |
no ground water encountered |
GM, SM, ML, OL, MH |
any |
7.6 cms or > / month or 50cms / year |
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0.00001 |
low |
silt, glacial till |
GC, SC, CL, CH, OH |
any except low areas |
< 7.5cms / month or > 50cms/year |
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0.000001 |
low |
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silty clay |
D - mild |
water table never above the bottom of the system and surface water does not accumulate and remain in soil surrounding the system |
no ground water encountered |
GW, GP, SW, SP |
any |
any |
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0.0000001 0.00000001 0.000000001 |
practically impervious |
fairly relia- ble |
computation from test data (reliable) |
impervious soils e.g. homogeneous clays below some of weathering |
GM, SM, ML, OL, MH |
any except low areas |
<7.5cm /month or < 50cms/year |
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Suggested Boring Program for Various Engineering Structures |
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Structure |
Number of boring spacing |
Depth of borings |
Remarks |
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Rigid Frame structure |
1 boring per 230 m2 of ground floor area |
1.5 times the minimum dimension of footing below the base of the footing Pile footings 1.5 times the minimum dimension of animaginary footing located at 2/3 of the expected depth of piles |
cohesive soil: - continuous undisturbed samples for the first 3m - intermittent samplesat 1.5 to 3 m intervals thereafter - sample at every change of soil type cohesionless soils: - obtain undisturbed samples (if possible) or condutct in situ soundings such as SPT or CPT tests |
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Continuous truss (girder) type bridge |
minimum of 1 boring at every pier/footing |
1.5 times the minimum dimension of footing below the base of the footing Piles footings 1.5 times the minimum dimension of an imaginary footing located 2/3 of the expected depth of piles |
cohesive soils: pier size < 50m2 - continuous undisturbed samples at each pier pier size: 50 - 100m2 2 continuous undistubed samples at each pier pier size: 100- 250m2 4 continuous undistubed samples at each pier; more: minimum of 5 samples cohesionless soils: obtain undisturbed samples or soundings as for cohesive soils competent rock: trace formation at each pier, if in doubt of rock quality, drill at least 6 m into formation |
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Levees |
leeve high: 3 - 5m space boring at 300m intervals |
Depth of boring: 6m |
cohesive soils: continuous undisturbed samples cohesionless soils: continuous undisturbed sample or soundings locate borings along centerline of proposed structure |
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Levees |
leeve high: 6 - 12m space boring at 230m intervals |
Depth at least equal to height of leeve |
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Levees |
leeve high: 12 - 18m space boring at 150m intervals
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Depth at least equal to height of leeve |
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Earth dam preliminary investigation |
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depth at least equal to height of dam or twice the maximum head,whichever is greater. Trace the top of the impervious zone |
mximum stree occurs approximately at mid point of slope between the centerline and toe of proposed structure. Establish a square grid pattern of borings located upstream and downstream of dam centerline near midpoint of slope in a direction with respect to dam centerline |
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Earth dam primary investigation |
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trace the limits of various strata e.g. sand; - treat power plants, spillways and other control structures asrigid frame structures; - obtain adequate subsurface data to define the character of the abutments |
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Earth dams |
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Obtain in situ permeability and pore pressure measurments cohesive soils continuous undisturbed samples cohesionless soils: continuous undisturbed samples or soundings |
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borrow pit |
use a 60m grid spacing |
maximum depth to water table or sorking depth of equipment |
disturbed samples are satisfactory; may use augers to obtain samples |
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roads 2 lane highways |
1 boring / 150m along centerline and at each major change of soil profile |
For excavation and level terrain: 3 m below level finished grade. For compacted embankment: treat asfor leeves For rock extend 0.75m into rock |
cohesive soil: continuous undisturbed samples cohesionless soils: continuous undisturbed samples or soundings |
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roads: multilane highways |
1 boring /75m centerline, borings may be staggerred |
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airfield |
preliminary investigation |
place borings at 300m intervals in asquare grid patterns to a depth of 6m, sample may be disturbed, site facilities based upon preliminary investigation |
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airfield |
primary investigation |
runways |
2 lines in a square grid pattern of 30m on either side of runway centerline to a depth of 6m or 1.5m into rock |
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airfield |
primary investigation |
taxiway |
place borings at 60 - 75m intervals along centerline to depth of 6m |
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airfield |
primary investigation |
apron |
place borings in a 60 - 75m square grid to a depth of 6m |
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houses |
1 boring/ 750m2 in new subdivision |
to unweathered rock of 4.5m whichever is lesser |
obtain sample at 1.5m interval using undistributed sampling techniques for cohesive soils or undisturbed or sounding for cohesion less soils |