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CIVL 392 - ddddd2 - Earthmoving Materials and Operations

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    EARTHMOVING MATERIALS

    AND OPERATIONS

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    Introduction to Earthmoving

    Earthmoving is the process of moving soil or

    rock from one location to another and

    processing it so that it meets construction

    requirements such as location, elevation,density, moisture content etc.

    Activities of earthmoving: Excavation, loading,

    hauling, damping, spreading, compacting,

    grading and finishing.

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    Equipment Selection

    The major criterion in selecting an equipmentis the ability of equipment to do the job. Thiscan be specified as:

    ability to maximise the profit

    possible future use

    availability of equipment, spare parts and

    services the effects of equipment down-time on other

    construction equipments

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    Production of Earthmoving

    Equipments

    Production= Volume per cycle x Cycles per hour

    Cost per unit of production =Equipment cost per hour

    Equipment production per hour

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    Production

    In calculating the job efficiency for cycles per hourthere are two methods:

    Using the number of effective working minutes in an

    hour to calculate the cycles per hour.

    To multiply the theoretical number of cycles per60 min (hour) by a numerical efficiency factor. The

    following Table shows job efficiency factors forearthmoving operations.

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    Job efficiency factors for

    earthmoving operations

    Job Conditions**

    Management Conditions*

    Excellent Good Fair Poor

    Excellent 0.84 0.81 0.76 0.70

    Good 0.78 0.75 0.71 0.65

    Fair 0.72 0.69 0.65 0.60

    Poor 0.63 0.61 0.57 0.52

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    Management conditions include

    Skill, training, and motivation of workers;

    Selection, operation, and maintenance ofequipment;

    Planning, job layout, supervision, andcoordination of work.

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    Job conditions

    Job conditions are the physical conditions of ajob that they affect production rate (notincluding the type of material involved). Theyinclude:

    Topography and work dimensions.

    Surface and weather conditions.

    Specification requirements for work methodsor Sequence

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    General Soil Characteristics

    Trafficability : The ability of a soil to support

    the weight of vehicles under repeated traffic.

    Trafficability is measured qualitatively. It is

    function of soil type and moisture.

    Loadability : is the measure of the difficulty in

    excavating and loading a soil. Loose granular

    soils are highly loadable, whereas compacted

    coehesive soils and rocks have low loadability.

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    General Soil Characteristics

    Unit weight : Soil unit weight is explained as kilogramper cubic meters. Unit weight depends on type of soil,moisture content and degree of compaction.

    Moisture Content: In their natural state, all soilscontain some moisture. The moisture content isexpressed as percentage.

    100Dry weight

    Dry weight-htMoist weig=(%)contentMoisture

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    Soil Volume Change Characteristics

    Soil Conditions

    There are three conditions that the soil may exist:

    Bank (in place or in situ): Material in its natural statebefore disturbance (Bm3).

    Loose : Material that has been excavated or loaded(Lm3).

    Compacted : Material state after compaction (Cm3).

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    Swell

    Soil volume increases after excavation since the soil

    grains are loosened during excavation and air fills the

    void spaces created. As a result one unit volume of

    soil in the bank condition will occupy more than one

    unit volume after excavation. This is called as Swell.Swell can be calculated as:

    100)1volumeseWeight/loo

    k volumeWeight/ban

    ((%)Swell

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    Shrinkage

    When a soil is compacted, some of the air inside of the

    soil is forced out. As a result the soil occupies less

    volume than it does either in bank or loose conditions.

    This is the reverse of swell and called as shrinkage.

    100)

    volumepactedWeight/Com

    k volumeWeight/ban-(1=(%)Shrinkage

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    Load and Shrinkage Factors

    In earthmoving contracts, it is important to convert all

    material volumes to a common unit of measure.

    Haul unit or spoil bank volumes are commonlyexpressed in loose measure. Conversion factor to

    convert from loose to bank volume is called as Load

    Factor. Loose volume is multiplied by load factor to

    find bank volume.

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    Load and Shrinkage Factors

    To convert a volume from bank volume to compacted volume,

    shrinkage factoris used.

    Load factor =Weight / loose unit volume

    Weight / bank unit volume

    Swell+1

    1=FactorLoad

    eunit volumpactedWeight/comeunit volumbankWeight/FactorShrinkage

    Shrinkage1FactorShrinkage

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    Example

    Problem:A Soil Weighs 1163kg/Lm3,

    1661kg/Bm3and 2077kg/Cm3,

    a) Find load factor and shrinkage factor.

    b) How many bank Bm3

    and compactedCm3are contained in 593,300 Lm3of

    this soil.

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    Solution

    a)

    b)

    Load Factor =1163

    1661= 0 70.

    Shrinkage Factor =

    1661

    2077=

    080.

    3Bm415,310=0.70593,300=VolumeBank

    Cm332,248=0.8415,310=VolumeCompacted 3

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    Example

    A soil weighs 1471 kg/m3loose, 1839 kg/m3in placeand 2090 kg/m3compacted.

    Find the swell and shrinkage.

    Find load factor and shrinkage factor.

    If an earth fill dam requires a compacted volume of

    4.6*106 m3of the above soil. How many loose cubicmeter of this soil must be hauled to construct thedam.

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    Solution

    a- 100)1volumeseWeight/loo

    k volumeWeight/ban((%)Swell

    25%100)11471

    1839((%)Swell

    100)volumepactedWeight/Com

    k volumeWeight/ban-(1=(%)Shrinkage

    12%100)20901839-(1=(%)Shrinkage

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    Solution

    Swell+1

    1=FactorLoad

    80.00.25+1

    1=FactorLoad

    Shrinkage1FactorShrinkage

    0.880.121FactorShrinkage

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    Solution

    Compacted volume = (bank volume x shrinkage factor)

    Bank Volume =

    36

    522727288.0

    10*6.4

    _

    _

    BmfactorShrinkage

    VolumeCompacted

    3

    653409180.0

    5227272_ LmLoadFactor

    BankVolume

    VolumeLosse

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    Triangular Spoil Bank

    Where:

    B: base width (m)

    H: pile height (m)

    L: pile length (m)R: angle of repose (deg)

    V: pile volume (m3)

    lengthareaSectionVolume

    2

    tanRB=H)

    tanRL

    4V(=B 1/2

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    Material Angle of Repose (degrees)

    Clay 35

    Common earth, dry 32

    Common earth, moist 37

    Gravel 35

    Sand, dry 25

    Sand, moist 37

    Typical Values of Angle of Repose

    of Excavated Soils

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    Example

    Problem:

    Find the base width and height of atriangular spoil bank containing 76.5 Bm3

    if the pile is 9.14m, the soils angle of

    repose is 37, and its swell is 25 %.

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    Solution

    Loose volume=76.5 x 1.25=95.6m3

    7.45m=)37tan9.14

    95.64(=widthBase 1/2

    2.80m=37tan2

    7.45=Height

    2

    tanRB=H)

    tanRL

    4V(=B 1/2

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    Example

    Problem:

    Find the base diameter and height of aconical spoil pile that will contain 76.5

    Bm3of excavation if the soils angle of

    repose is 32and its swell is 12%.

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    Example

    A rectangular ditch having a cross-sectional

    area of 2.4 m2is being excavated in a clay.

    The soils angle of repose is 35oand its swellis 30%. Find the height and base width of the

    triangular spoil bank that will result from the

    trench excavation.

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    Solution

    mB 22.435tan

    12.342/1

    2/12/12/1 )tan

    _sec4()

    tan

    _sec4()

    tan

    4(

    R

    areation

    RL

    Lareation

    RL

    VB

    Considering section area as loose measure = 2.4 x 1.3 = 3.12 m2

    mRB

    H 478.12

    )35(tan22.4

    2

    )(tan

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    Soil Identification and classification

    Fundamental Soil Types

    Soil is considered to be composed of five fundamental soil types: gravel,sand, silt, clay, and organic material.

    Gravel:is composed of individual particles larger than 6 mm but smaller

    than 76 mm.

    Sand: material smaller than gravel but larger than 0.07 mm (No. 200sieve).

    Silt: particles passing No. 200 sieve but larger than 0.002 mm.

    Clay: is composed of particles less than 0.002 mm in diameter.

    Organic soils: contain partially decomposed vegetable matters.

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    Soil Classification Systems

    Liquid Limit(LL)of a soil is the water content(expressed in percentage of dry weight) at which thesoil will just start to flow when subjected to a standardshaking test.

    Plastic limit(PL)of a soil is the moisture content inpercent at which the soil just begins to crumble whenrolled into a thread 0.3 cm in diameter.

    Plasticity index (PI)is the numerical differencebetween the liquid and plastic limits and representsthe range in moisture content over which the soilremains plastic.


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