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Unified Soil Classification System Training Part C - USCS using Field Tools.

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Unified Soil Classification Unified Soil Classification System Training System Training Part C - USCS using Field Part C - USCS using Field Tools Tools
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Unified Soil Classification Unified Soil Classification System TrainingSystem Training

Part C - USCS using Field ToolsPart C - USCS using Field Tools

Flow Chart for Coarse-GrainedFlow Chart for Coarse-Grained

Flow Chart for Fine-GrainedFlow Chart for Fine-Grained

USCS Flow Chart - Activity 3USCS Flow Chart - Activity 3

Flow Chart OverviewFlow Chart Overview

Two Broad CategoriesTwo Broad Categories– Fine-Grained - 50% or more finer than the Fine-Grained - 50% or more finer than the

# 200 sieve# 200 sieve

– Coarse-Grained - Less than 50% finer than Coarse-Grained - Less than 50% finer than the # 200 sievethe # 200 sieve

Remember system uses minus 3”Remember system uses minus 3”

Visual DeterminationVisual Determination

Visual DeterminationVisual Determination

Visual DeterminationVisual DeterminationRemember that percent is

by dry weight. Gravel Particles overpower

gradation

Visual DeterminationVisual Determination

A sand size particle is the smallest that can be seen

without magnifier

Textural DeterminationTextural Determination

When wetted thoroughly, coarse-grained soils have a distinct grittiness. Practice on known samples

Tests to Characterize FinesTests to Characterize Fines

Liquid Limit EvaluationLiquid Limit Evaluation– High - Greater than 50High - Greater than 50

– Low - Less than 50Low - Less than 50

Begin with standard amount of minus Begin with standard amount of minus

# 40 soil - begin adding water with wash # 40 soil - begin adding water with wash

bottlebottle

Activity 4 -Activity 4 - Liquid Limit Evaluation Liquid Limit Evaluation

•Low LL soils

water penetrates quickly

Activity 4 -Activity 4 - Liquid Limit Evaluation Liquid Limit Evaluation

Activity 4 -Activity 4 - Liquid Limit Evaluation Liquid Limit Evaluation

•High LL soils

water penetrates slowly - check for heat of hydration in CH soils

Activity 4 -Activity 4 - Liquid Limit Evaluation Liquid Limit Evaluation

•High LL soils -

requires more than 50 drops per tablespoon of soil - calibrate with known samples data

•When shocked, dilatent soil releases free water and becomes “livery”in appearance

Activity 5 -Activity 5 - Dilatency Evaluation Dilatency Evaluation

•When squeezed, dilatent soil becomes dull

Activity 5 -Activity 5 - Dilatency Evaluation Dilatency Evaluation

Activity 6 -Activity 6 - Toughness Evaluation Toughness Evaluation

•Reaching plastic limit requires adding considerable dry soil.

•Thread can be re-rolled several times after reaching plastic limit.

•Thread requires pressure to form.

• Thread can be rolled out to lengths > 2”

Activity 7 -Activity 7 - Ribbon Evaluation Ribbon Evaluation

•Length of Ribbon

•Strength

•Related to Clay Content

•See Module 3

•Ribbon more than 2 inches long indicates clay content is > 40 %

Activity 8Activity 8 - - Shine Evaluation Shine Evaluation

Activity 8Activity 8 - - Dry Strength Evaluation Dry Strength Evaluation

•Very High - cube cannot be crushed even on hard surface

•High - Can be crushed only against hard surface

•Medium - Can be crushed with considerable pressure

•Low - crumbles with some pressure

Typical Behavior CH soilTypical Behavior CH soil

High High

Liquid Liquid

LimitLimit

High toughness - easily roll out High toughness - easily roll out thread to 1/8 inch diameter to thread to 1/8 inch diameter to length of several incheslength of several inches

Zero dilatencyZero dilatency Ribbons to more than 1-1/2 inchRibbons to more than 1-1/2 inch High dry strengthHigh dry strength High ShineHigh Shine

Typical CH soilTypical CH soil

Slickensides

Typical CH soilTypical CH soil

Typical Behavior ML soilTypical Behavior ML soil

Low Low

Liquid Liquid

LimitLimit

Slight to no toughness - If a thread Slight to no toughness - If a thread can be formed to 1/8 inch diameter can be formed to 1/8 inch diameter it can’t be reformedit can’t be reformed

Medium to high dilatencyMedium to high dilatency Ribbons only slightly if anyRibbons only slightly if any Low to very low dry strengthLow to very low dry strength No Shine (watch out for mica)No Shine (watch out for mica)

Typical Behavior MH soilTypical Behavior MH soil

High High

Liquid Liquid

LimitLimit

Medium toughness - If a thread can Medium toughness - If a thread can be formed to 1/8 inch diameter it be formed to 1/8 inch diameter it has low strengthhas low strength

Low dilatencyLow dilatency Ribbons slightly to moderatelyRibbons slightly to moderately Low to Medium dry strengthLow to Medium dry strength Low Shine (watch out for mica)Low Shine (watch out for mica)

Typical Behavior CL soilTypical Behavior CL soil

Low Low

Liquid Liquid

LimitLimit

Medium to high toughness - A Medium to high toughness - A thread can be formed to 1/8 inch thread can be formed to 1/8 inch diameter with medium toughnessdiameter with medium toughness

Low to none dilatencyLow to none dilatency Ribbons slightly to moderatelyRibbons slightly to moderately Medium dry strengthMedium dry strength Low to Medium Shine (watch out Low to Medium Shine (watch out

for mica)for mica)

Distinguishing between CL Distinguishing between CL and MH difficultand MH difficult

MH

CH

CL

MLPI is the same -

Only difference is in LL

50

A-Line

Coarse-Grained ClassesCoarse-Grained Classes

Visual ExaminationVisual Examination– Determine whether G or S is predominantDetermine whether G or S is predominant– Determine if Clean or DirtyDetermine if Clean or Dirty

If CleanIf Clean– Determine if Poorly or Well GradedDetermine if Poorly or Well Graded

If DirtyIf Dirty– Determine if Fines are Plastic or NotDetermine if Fines are Plastic or Not

Clean or Dirty ?Clean or Dirty ?

When wetted a clean coarse-grained soil will not leave a stain on your palm. A dirty soil will leave a stain

Clean or Dirty ?Clean or Dirty ?

If a soil sample is dropped in a beaker of water, a cloud remaining after about 30 seconds indicates more than 12 % fines

Visual Determination Visual Determination Well or Poorly GradedWell or Poorly Graded

A well graded sample has a wide range of particle sizes that are about equally distributed by weight

Visual Determination Visual Determination Well or Poorly GradedWell or Poorly Graded

A gap-graded sample

has a range of

particle sizes

missing. This

sample has coarse

and fine but no

medium size particles

Visual Determination Visual Determination Well or Poorly GradedWell or Poorly Graded

A well-graded

sample has a

wide range of

particle sizes that

are about equally

distributed.

Visual Determination Visual Determination Well or Poorly GradedWell or Poorly Graded

A poorly graded sample is predominately one size of particle

Poorly Graded SandPoorly Graded Sand

Well Graded SandWell Graded Sand

Evaluation of Plasticity of Evaluation of Plasticity of FinesFines The Most Useful

Field Tests are Toughness and

Dilatency

Typical GC soil - glacial tillTypical GC soil - glacial till

Gravel with matrix of clay

Typical GM soil - AlluviumTypical GM soil - Alluvium

Gravel with matrix of

silt


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