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Code: METH04V01 Date: July 27, 2014 Author: Emily Barasa STANDARD OPERATING PROCEDURES METHOD FOR DETERMINATION OF ATTERBERG LIMITS AND LINEAR SHRINKAGE IN SOILS Contact Details: Telephone: +254 (20) 7224000/4235/4279/4163 Email: [email protected] : Laboratory Manager, [email protected] Website: www. http://worldagroforestry.org/research/land-health Address Details: World Agroforestry Centre, Mailing: P.O Box 30677-00100 Nairobi, Kenya Physical address: United Nations Avenue Off Limuru Road, Gigiri, Nairobi, Kenya

STANDARD OPERATING PROCEDURES - | World Agroforestry · 2015. 8. 25. · STANDARD OPERATING PROCEDURE Date: July 27, 2014 Code: METH04V01 Title: Method for Determination of Atterberg

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  • Code: METH04V01

    Date: July 27, 2014

    Author: Emily Barasa

    STANDARD OPERATING PROCEDURES

    METHOD FOR DETERMINATION OF ATTERBERG LIMITS AND LINEAR SHRINKAGE IN SOILS

    Contact Details: Telephone: +254 (20) 7224000/4235/4279/4163 Email: [email protected] : Laboratory Manager, [email protected] Website: www. http://worldagroforestry.org/research/land-health

    Address Details: World Agroforestry Centre, Mailing: P.O Box 30677-00100 Nairobi, Kenya Physical address: United Nations Avenue Off Limuru Road, Gigiri, Nairobi, Kenya

    mailto:[email protected]:[email protected]

  • STANDARD OPERATING PROCEDURE Date: July 27, 2014 Code: METH04V01 Title: Method for Determination of Atterberg limits and linear shrinkage in soils

    Author: Emily Barasa

    2 | A t t e r b e r g S O P

    METHOD DOCUMENT CONTROL LOG

    Name and position Signature

    Author(s)

    Emily Mwake Barasa_Senior Laboratory Technician

    [signature for completeness and correctness of document]

    Verifiers Josephine Muteti_Laboratory Technician [signature for completeness and correctness of document]

    [signature for completeness and correctness of document]

    Authorizer Mercy Nyambura_Laboratory Manager Elvis Weullow_Deputy Laboratory Manager.

    [signature for completeness and correctness of document]

    Distribution of valid copies of this document: D102B

    In transition

    Revise before: [date]

    Historical data [dates of previous issues]

    Date retrieval: [to be filled in once the document has become obsolete and is archived]

    Changes in this version compared to previous version:

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  • STANDARD OPERATING PROCEDURE Date: July 27, 2014 Code: METH04V01 Title: Method for Determination of Atterberg limits and linear shrinkage in soils

    Author: Emily Barasa

    3 | A t t e r b e r g S O P

    SCOPE AND APPLICATION This procedure describes the determination of the bulk density, Atterberg limits (liquid and plastic

    limits) using cone penetrometer and linear shrinkage. The Atterberg limits are a basic measure of the

    nature of a fine-grained soil such as its shrinkage limit, plastic limit, and liquid limit. Depending on the

    water content, soil- may appear in four states; solid, semi-solid, plastic and liquid. In each state the

    consistency and behavior of the soil is different and thus so are its engineering properties. Therefore,

    the boundary in each state can be defined based on a change in the soil’s behavior. The Atterberg limits

    can be used to distinguish between silt and clay and it can distinguish between different types of silts

    and clay.

    PRINCIPLE Bulk density is a measure of the weight of the soil per unit volume (g/cc), usually given on an oven-dry

    (110° C) basis. Variation in bulk density is attributable to the relative proportion and specific gravity of

    solid organic and inorganic particles and to the porosity of the soil. Bulk density is important in

    quantitative soil studies and is generally used in calculating soil moisture movement within a profile and

    to compare soils qualitatively by converting percent to weight per unit volume. The determination

    usually consists of drying and weighing a soil sample, the volume of which is known. Liquid or plastic

    limit of soils is a measure of their consistency (compressibility, permeability, to compact, shrink-swell

    and shear strength). The method is based on the relationship between the moisture content and the

    penetration of a cone into the moist soil. The liquid limit (LL) is the moisture content at which the soil

    passes from the plastic, ductile behavior to the liquid, flowing behavior as determined by the liquid limit

    test. It is also defined as the water content at which the cone penetrates the moist soil to a depth of

    20mm when dropped from a standardized height. The plastic limit (PL) is the soil water content as the

    soil passes from the plastic, ductile behavior to the brittle, cracking behavior. Plasticity index (PI) is the

    range of the water content over which a soil behaves plastically. Soil shrinkage (LS) is the limit to which a

    soil material contracts as it loses water on drying.

    ABBREVIATIONS AND DEFINITIONS

    LL Liquid Limit

    PL Plastic Limit

    P10 Plasticity index

    LS Soil shrinkage

    L Length of the mound (mm)

    Ls Longitudinal length of the oven dry soil bar (mm)

  • STANDARD OPERATING PROCEDURE Date: July 27, 2014 Code: METH04V01 Title: Method for Determination of Atterberg limits and linear shrinkage in soils

    Author: Emily Barasa

    4 | A t t e r b e r g S O P

    RELATED DOCUMENT Method for operating penetrometer

    RELATED FORMS

    Logging form Recording form

    SAFETY AND ENVIRONMENT

    Personal protection:

    Heavy-duty gloves should always be used when removing samples from the oven to avoid burns. Care should be taken when handling the penetrometer to avoid injury.

    Electrical hazards:

    Electrical systems must conform to the ICRAF standards. Shock hazards exist inside the instruments. Only an authorized service representative or an individual with training in electronic repair should remove panels or circuit boards where voltages are greater than 20 V. The instruments require a third-wire protective grounding conductor. Three-to-two wire adapters are unsafe for these instruments.

    REQUIREMENTS

    Equipment a. Standard cone penetrometer

    b. Penetration cone assembly, a stainless steel cone with a cone angle of 30±1O and

    total moving mass of 80±0.1g, automatic zeroing device, displacement device

    c. Penetration container (cups) approximately 55mm in diameter and 40mm deep

    with a rim parallel to the flat base

    d. Balance of 2kg capacity and 0.001g accuracy

    e. Automatic controller with a built in 5±1 seconds timer: provides automatic

    control of the penetration period and also used as a timing device

    f. Oven capable of maintaining a temperatures of 1050C

    g. Vernier caliper graduated in millimeters

    h. Brass steel molds in the form of semi-cylindrical troughs; 140mm long and 21mm

    internal diameter

    i. Mixing bowl approximately 150mm diameter, with an air-tight lid

  • STANDARD OPERATING PROCEDURE Date: July 27, 2014 Code: METH04V01 Title: Method for Determination of Atterberg limits and linear shrinkage in soils

    Author: Emily Barasa

    5 | A t t e r b e r g S O P

    j. Two spatula or palette knives with blade approximately 100mm long and 20mm

    wide

    k. Test gauge: for checking the excessive wear to the point of the cone

    l. A flat glass plate

    m. Moisture boxes

    n. A metal straight edge

    o. Flat rubber mat

    p. Mortar and pestle

    q. Standard 425µm test sieve

    Materials & Supplies

    a. Petroleum jelly

    b. De-ionized water

    c. A damp cloth

    d. String 250mm long

    e. A scoop of 50 ml volume

    f. Wash bottle

    PROCEDURE

    Sample processing and preparation

    a. Air-dried Approximately 200g of soil grind and sieve through a 425µm sieve. NB: all

    portions of the sample must be ground with a pestle and motor to pass through the

    425µm sieve. The history of the sample should also be noted.

    b. Place 80% of the testing portion of the soil in a mixing bowl, wet the soil with an

    increment of de-ionized water and mix thoroughly with a palette knife. Continue

    adding increments of water until the test portion becomes a thick homogeneous

    paste. Add water such that the range of penetration values between approximately

    15mm to 25mm are obtained.

    c. After mixing the soil and before performing the test, the test portion should settle

    for an adequate period (As a preferred option the test portion can be cured at room

    temperature in an air tight container for at least 12 hours, and up to 24 hours for

    moist soils but the test can be done immediately after mixing for soils with low

    clay content.) to allow the water to permeate through the soil mass

  • STANDARD OPERATING PROCEDURE Date: July 27, 2014 Code: METH04V01 Title: Method for Determination of Atterberg limits and linear shrinkage in soils

    Author: Emily Barasa

    6 | A t t e r b e r g S O P

    d. Weigh 45mg of Soil sample into a 5ml centrifuge tube and add 2.5ml of an aqueous

    Triton X100 solution Add 40 µl of 1000 mg/l Se internal standard solution d into the

    suspension using a calibrated pipette. Mix the Suspension thoroughly and sonicate

    it. Transfer 10µl of the suspension into siliconized quartz disc and dry.

    e. In the case of Plants, the sample is dried and milled through a 1-mm sieve. Plant

    sample (45mg) is weighed into a 5ml centrifuge tube and 2.5ml of an aqueous Triton

    X100 solution is added. 40 µl of 1000 mg/l Sc internal standard solution and 10 µl of

    1000 mg/l Y are added into the suspension using calibrated pipettes. Suspension is

    mixed thoroughly and sonicated. 10µl of suspension is transferred onto a siliconized

    quartz disc and dried.

    f. Liquid samples are a diluted appropriately and the different dilutions are tested to

    find an optimal peak to scattering background ratio. The Liquid specimen (1000 µl) is

    then sampled into a labeled vial. For accurate determination of light elements only,

    add 40 µl of 100 mg/l Sc single element standard into the liquid sample and. For

    determination of heavier elements, transfer 50 µl of 100 mg/l Y single element

    internal standard using a calibrated pipette into the liquid sample. Note the 10 times

    dilution of the liquid standards as compared with the soil and plant methods.

    Liquid limit test a. After overnight curing, place the test portion on a flat glass plate and mix it with the

    palette knives for 10 to 40 minutes depending on the soil type. If necessary water or

    soil can be added so that the first cone penetration reading is approximately 16mm.

    b. Remove approximately 20g of the mixed soil with a palette knife and put aside for

    plastic limit determinations

    c. Place the mixed soil into the penetration cup palette knife and level it to a smooth

    top with the straight edge, taking care not to trap air. Tap the test cup on the rubber

    mat to remove air voids and refill it. Repeat this procedure until air voids are

    completely displaced and the cup is level filled.

    d. Assemble the drop cone apparatus and place the cone in the cone holder and raise

    the cone assembly to the highest position possible and level the penetrometer.

    Raise the penetration head as required.

    e. Place the cup on the base of the drop cone apparatus approximately central under

    the point of the penetration cone

    f. By adjusting, lower the penetration head until the tip of the cone makes contact

    with the surface of the soil such that a slight movement of the cup will just mark the

    surface of the soil.

  • STANDARD OPERATING PROCEDURE Date: July 27, 2014 Code: METH04V01 Title: Method for Determination of Atterberg limits and linear shrinkage in soils

    Author: Emily Barasa

    7 | A t t e r b e r g S O P

    g. Depress the indicator rod of the dial gauge until it lightly touches the top of the

    shaft. Note and record the reading taken on the dial gauge to the nearest 0.1mm

    h. Set the automatic controllers and release the penetrometer shaft and allow the

    cone to penetrate the soil for 5 seconds and then cramp or restrain the

    penetrometer shaft.

    i. Depress the indicator rod of the dial gauge until it lightly touches the top of the

    shaft. Note and record the reading taken on the dial gauge to the nearest 0.1mm

    j. Calculate the difference between the two dial gauge readings and record as the

    penetration value(depth)

    k. Raise the penetration head to remove the cone from the soil and clean the cone

    thoroughly with a damp cloth

    l. Remove approximately 10g, of the test soil portion with a palette knife, from near

    the area penetrated by the cone and determine the water content of the test

    sample by oven drying at 1050C.This is best facilitated by placing the penetration cup

    at a slight angle on the work bench and then drawing the palette knife in a

    downward and outward movement against the inside lip of the cup

    m. Remove the remaining soil from the cup and put it on the flat glass plate, remix it

    and if necessary (incase the first reading is not satisfactory) add water or soil and

    perform the next cone penetration.

    n. Repeat Procedures 3 to 12 is until three more determinations (18, 20 and 22) of soil

    water content and the penetration depth are obtained.

    Note: The test should always proceed from the drier to the wetter condition of the soil.

    Clean the cup and the cone thoroughly each time you remove the soil from th cup to

    add water.

    o. Reporting results

    Plot the moisture contents against the corresponding penetration depths for the

    four determinations on a linear graph with the percent moisture on the

    horizontal axis and the penetration depth on the vertical axis. Draw a straight

    line of best fit through the plotted points.

    Determine the moisture content corresponding to the intersection of the line of

    best fit and the 20mm penetration ordinate (interpolation). This moisture

    content is the liquid limit(LL)of the soil

    Linear Shrinkage test

    a. Clean and lightly grease the inner walls of the shrinkage mold to prevent the soil

    from adhering to the mold. Remove the wet soil from the cup after the

  • STANDARD OPERATING PROCEDURE Date: July 27, 2014 Code: METH04V01 Title: Method for Determination of Atterberg limits and linear shrinkage in soils

    Author: Emily Barasa

    8 | A t t e r b e r g S O P

    determination of penetration 20mm, and put in the greased mold with the

    palette knife. Remove Air bubbles or voids by lightly tapping the base of the

    mold on a flat rubber mat. Slightly overfill the mold and then level off the excess

    soil with a palette knife. Remove all soil adhering to the rim and edge of the

    mold by wiping with a damp cloth to stop friction between the soil in the mold

    and any adhering to the edges of the mold.

    b. Air dry The soil water mixture in the mold slowly at room temperature for 12 to

    24 hours and then transfer it to an oven and dry to constant weight at 105oC.

    c. Allow the mold and the dry soil to cool and measure the mean length of the soil

    bar to the nearest millimeter. If the soil bar has cracked into pieces during

    drying, carefully reposition the cracked edges together, then firmly hold the

    separate parts together and measure the bar’s length. If the soil bar curls or is

    curved, remove it carefully and measure the length of the top and bottom

    surfaces with a piece of string. The mean of the two lengths is the length of the

    soil bar.

    Note: Curling and curving can be prevented by slow drying of the mound and soil- water

    mixture. This can be done by air drying for periods of 48-72 hours the oven drying of

    60oC – 65oC until shrinkage has largely ceased, and then at 105oC to 110oC to complete

    the drying.

    d. Reporting results - The linear shrinkage of the soil is calculated as a percentage

    of the original length of the soil bar in the mound from the equation:

    Percentage of the linear shrinkage LS = (L-Ls/L) * 100 to the nearest 0.5%

    Plastic limit test

    a. Mold the 20g of cured soil put aside for plastic limits test into a ball and roll between

    the palms until the heat of the hands has dried the soil sufficiently for slight cracks

    to appear on its surface. Then divide sample into two subsamples for separate

    determination of each sub sample.

    b. Divide each subsample into four approximately equal parts and form each part into

    a thread of about 6 mm in diameter, between the first finger and thump of each

    hand. Roll the thread between the tips of the fingers of one hand and the surface of

    the glass plate. Apply sufficient pressure to reduce the diameter of the thread to

    about 3mm. Note: 5 to 15 complete forward and back movement of the hand is

    sufficient to reduce the thread to 3mm. Uniform rolling pressure should be

    maintained throughout the test.

  • STANDARD OPERATING PROCEDURE Date: July 27, 2014 Code: METH04V01 Title: Method for Determination of Atterberg limits and linear shrinkage in soils

    Author: Emily Barasa

    9 | A t t e r b e r g S O P

    c. Pick and mold the 3mm thread between the fingers to further dry the soil and then

    formed into a thread and rolled out again. This procedure is repeated until the

    thread shears both longitudinally and transversely. This first crumbling point is the

    plastic limit. The portions of the crumbled soil thread are gathered together and

    transferred to a moisture container. The other three parts of the subsample is

    treated similarly and placed in the same moisture container. The moisture content

    of the soil is determined by oven-drying at 1050C. This soil water content is the

    plastic limit.

    d. Reporting results; the average of the water contents obtained from the two plastic

    limit tests. The plastic limit (PL) is the average of the two water contents. If no

    shrinkage is observed on the sample the sample has no plastic limit and is reported

    as non-plastic. Note: If the two results of the moisture content differ by more than

    0.5% the test shall be repeated.

    Plasticity Index (PI)

    Plasticity index is calculated as follows:

    PI = LL – PL

    Soil water (moisture) Content determination

    a. Weigh and label a 50-mL beaker.is weighed and Record the weight.

    b. Collect subsamples of the wet soil and add to the beaker. Approximately 10g of wet

    should be sufficient

    c. Immediately weigh the beaker with wet soil and record the weight

    d. Dry soil in oven at 105C for at least 24 hours.

    e. Weigh beaker with dry soil and record the weight

    f. Report

    Sample identification and water content data information as follows:

    Water content data

    Sample No.

    Mass of cup (g0

    Mass of cup and wet soil (g)

    Mass of cup and dry soil

    mass of wet soil (g)

    mass of dry soil (g)

    % water content

  • STANDARD OPERATING PROCEDURE Date: July 27, 2014 Code: METH04V01 Title: Method for Determination of Atterberg limits and linear shrinkage in soils

    Author: Emily Barasa

    10 | A t t e r b e r g S O P

    Hence %Water content (W) = Mwet - Mdry /Mdry

    Report the liquid limit, plastic limit, and plasticity index to the nearest 0.1 percent or

    whole number

    Note: All forms of liquid and plastic test limits are subject to errors due to either

    operator error or variations in the equipment used. For the liquid limits the consistency

    of the test portion should be such that when tested, a penetration in the range of 9 to

    12 mm is obtained. The plastic limit in particular requires practice and cross-checking to

    identify the correct point, as it is easy to make the rolled thread crack and crumble

    prematurely

  • STANDARD OPERATING PROCEDURE Date: July 27, 2014 Code: METH04V01 Title: Method for Determination of Atterberg limits and linear shrinkage in soils

    Author: Emily Barasa

    11 | A t t e r b e r g S O P

    REFERENCES

    ASTM D4318 - 10 Standard Test Methods for Liquid Limit, Plastic Limit, and Plasticity Index of

    Soils.

  • STANDARD OPERATING PROCEDURE Date: July 27, 2014 Code: METH04V01 Title: Method for Determination of Atterberg limits and linear shrinkage in soils

    Author: Emily Barasa

    12 | A t t e r b e r g S O P

    ANNEX 1: Workflow

    Sample Grinding

    Sample Curing

    Plastic limit/Liquid limit/Linear shrinkage?

    Plastic Limit

    Sample Wetting

    Sample Penetration

    Oven Drying

    Roll the Threads

    · Mould the soil into a ball

    · Roll between your palms till

    it dries and cracks appear

    · Repeat the process of

    rolling until the thread

    crumbles

    · Divide the threads into two

    moisture beakers

    · Get the wet weight

    Record Results

    · Penetrate first at

    16mm then scoop the

    sample at the centre

    and get its wet weight

    · Repeat the process at

    18, 20 and 22mm and

    put in respective

    beakers

    · Transfer the scooped sample, the mould and the threads to the oven for 24hrs at 105

    oC

    · Get the dry weight

    · Soak samples overnight

    using de-ionized water

    · Mix using palette knife till soil

    is thoroughly mixed

    Plastic limit

    Linear Shrinkage

    Test

    Liquid Limit Test

    Shrinkage Mould Filling

    Linearshrinkage

    Liquid limit

    · Grease the

    shrinkage mould

    · Fill using pallette

    knife to level

    · Dry at room temp

    for 12-24hrs

    · Grind the sample to 425µm

    · Add soil or water to

    get the right

    thickness

    Action point

    Decision point

    Preparation

    Tape notes

    Process route

    From Soil Preparation Factory

    To Database

    Stored data

    ATTERBERG LIMITS WORKFLOW

    This section determines the atterberg limits (liquid and plastic limits) using cone penetrometer and linear shrinkage.

    Objective:This helps in determining compressibility, permeability, compatibility, shrink swell and shear strength of the soil

    LEGEND

  • STANDARD OPERATING PROCEDURE Date: July 27, 2014 Code: METH04V01 Title: Method for Determination of Atterberg limits and linear shrinkage in soils

    Author: Emily Barasa

    13 | A t t e r b e r g S O P

    Annex 2. QUALITY CONTROL

    Process Procedure

    Penetration Penetration range should be between 9-12 mm

    Identification Ensure you get the correct points

    Consistency Ensure consistency to avoid errors

    Report should include · Results of the determination of the limits

    · Possible deviations observed during analysis

    · Other operations that have affected the results