Consistence of the Soil GES 394 Revised by Mr. Brian Oram

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Presentation transcript:

Consistence of the Soil GES 394 Revised by Mr. Brian Oram

WHAT IS Consistency ? Soil consistence provides a means of describing the degree and kind of cohesion and adhesion between the soil particles as related to the resistance of the soil to deform or rupture. Soil consistence provides a means of describing the degree and kind of cohesion and adhesion between the soil particles as related to the resistance of the soil to deform or rupture. Since the consistence varies with moisture content, the consistence can be described as dry consistence, moist consistence, and wet consistence. Since the consistence varies with moisture content, the consistence can be described as dry consistence, moist consistence, and wet consistence. Consistence that is evaluated includes rupture resistance and stickiness. Consistence that is evaluated includes rupture resistance and stickiness. The rupture resistance is a field measure of the ability of the soil to withstand an applied stress or pressure as applied using the thumb and forefinger. The rupture resistance is a field measure of the ability of the soil to withstand an applied stress or pressure as applied using the thumb and forefinger.

Quick Review Cohesion is the attraction of one water molecule to another resulting from hydrogen bonding. Cohesion is the attraction of one water molecule to another resulting from hydrogen bonding. Adhesion is similar to cohesion except with adhesion involves the attraction of a water molecule to a non-water molecule. Adhesion is similar to cohesion except with adhesion involves the attraction of a water molecule to a non-water molecule.

When We Describe Consistency – We Attempt to Describe the Following Environmental Applications (our focus) Environmental Applications (our focus) –Rupture Resistance – Moist and Dry Consistency –Stickiness – Wet Consistency –Plasticity- Wet Consistency Geophysical / Engineering Geophysical / Engineering –Manner and Type of Failure –Penetration Resistance

Rupture Resistance A measure of the strength of the soil to withstand an applied stress A measure of the strength of the soil to withstand an applied stress Moisture content is also considered Moisture content is also considered –Dry –Moist (field capacity)

Dry Consistency ClassDescription LooseNoncoherent Symbol L or LO or lo Soft (<8 N)Soil crushes under very low pressure Slightly Hard (8 to < 20 N)Soil material crushes- low pressure - little resistance Mod Hard (20 to < 40 N)Soil material crushes- moderate pressure -resistance Hard (40 to < 80 N)Soil material crushes under strong pressure Very Hard (80 to < 160 N)Can not be crushed between thumb and forefinger. Extremely HardPressure applied by foot with full body 1 Newton (N) = lb/ft

Dry and Moist Consistency MoistDryStressSpecimenFails LooseLoose0 Very Friable Soft < 8 N Friable Slightly Hard 8 to < 20 N Firm Moderately Hard 20 to < 40 N Very Firm Hard 40 to < 80 N Extremely Firm Very Hard 80 to < 160 N 1 Newton (N) = lb/ft

Wet Consistency Describe Stickiness- Describe Stickiness- –The capacity of soil to adhere to other objects –Estimated at moisture content that displays maximum adherence between thumb and fore finger Describe Plasticity Describe Plasticity –Degree a soil can be molded or reworked causing permanent deformation without rupturing.

Stickiness Classes Non-Sticky – little or no soil adheres to fingers after release of pressure Non-Sticky – little or no soil adheres to fingers after release of pressure Slightly Sticky – soil adheres to both fingers after release of pressure with little stretching on separation of fingers Slightly Sticky – soil adheres to both fingers after release of pressure with little stretching on separation of fingers Moderately Sticky – soil adheres to both fingers after release of pressure with some stretching on separation of fingers Moderately Sticky – soil adheres to both fingers after release of pressure with some stretching on separation of fingers Very Sticky - soil adheres firmly to both fingers after release of pressure with stretches greatly on separation of fingers Very Sticky - soil adheres firmly to both fingers after release of pressure with stretches greatly on separation of fingers

Non-Sticky Very Sticky Slightly- Sticky

Plasticity The degree to which puddled or reworked soil can be permanently deformed without rupturing The degree to which puddled or reworked soil can be permanently deformed without rupturing Evaluation done by forming a 4 cm long wire of soil at a water content where maximum plasticity is expressed Evaluation done by forming a 4 cm long wire of soil at a water content where maximum plasticity is expressed

Plasticity Class Non-Plastic – will not form a 6 mm dia, 4 cm long wire, or if formed, can not support itself if held on end Non-Plastic – will not form a 6 mm dia, 4 cm long wire, or if formed, can not support itself if held on end Slightly Plastic – 6 mm dia, 4 cm long wire wire supports itself, 4 mm dia, 4 cm long wire wire does not Slightly Plastic – 6 mm dia, 4 cm long wire wire supports itself, 4 mm dia, 4 cm long wire wire does not Moderately Plastic – 4 mm dia, 4 cm long wire wire supports itself, 2 mm dia, 4 cm long wire wire does not Moderately Plastic – 4 mm dia, 4 cm long wire wire supports itself, 2 mm dia, 4 cm long wire wire does not Very Plastic – 2 mm dia, 4 cm long wire wire supports itself Very Plastic – 2 mm dia, 4 cm long wire wire supports itself

Estimating Clay Mineralogy Using Consistence and Color

2:1 Clay- Montmorillonite High Shrink and Swell Potential

1:1 Clay- Kaolinite

Consistence of the Soil GES 394 Revised by Mr. Brian Oram