Scour Project

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    EXPERIMENTAL STUDY TO OBSERVE SCOUR

    AROUND A BRIDGE PIER

    MAJOR PROJECT

    SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE

    AWARD OF THE DEGREE OF

    B.TECH

    IN

    CIVIL ENGINEERING

    BYA GROUP OF FINAL YEAR STUDENTS

    UNDER THE GUIDANCE OF

    DR. N.K.TIWARI

    DEPARTMENT OF CIVIL ENGINEERING

    NATIONAL INSTITUTE OF TECHNOLOGY

    KURUKSHETRA-136119

    MAY 2013

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    CONTENTS

    i. CERTIFICATE

    ii. ACKNOWLEDGEMENT

    ii. ABSTRACT

    CHAPTERS

    1.INTRODUCTION

    Areas affected by Scour.Causes of Scouring.

    2.REVIEW AND LITERATURE

    Factors affecting scouring

    Effect of Velocity of approach.Effect of depth of flow.

    Effect of sediment size.

    Effect of sediment grading.

    Effect of pier shape.

    Effect of pier size.

    Theoretical Scouring.

    Mechanism of Scouring.

    3.EXPERIMENTAL STUDIES

    4.CONCLUSION

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    CERTIFICATE

    Certified that the major project entitled EXPERIMENTAL STUDY TO OBSERVESCOUR AROUND A BRIDGE PIER which is being submitted in partial fulfilment

    of the requirement of the degree of bachelor of technology in civil engineering

    of National Institute of Technology, Kurukshetra is a record of the work carried

    out by a group of 12 students:

    1. Ajay Dev 109102

    2. Abhimanyu Rana 109136

    3. Anshul Sheokand 109383

    4. Himanshu Grover 109509

    5. Varun Bhagi 109512

    6. Puneet Mehta 109513

    7. Shubham Singhal 109536

    8. Anurag Malik 109711

    9. Akhilesh Dahiya 109712

    10.Balvindra Singh 109729

    11.Rahul Sharma 10973412.Arushi Jain 109825

    DR. N.K. TIWARI

    ASTT. PROFESSOR

    CIVIL ENGG. DEPTT.

    NIT KURUKSHETRA

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    Acknowledgement

    We express our sincere gratitude and indebtedness to our respected

    guide Dr. N.K. Tiwari, Astt. Professor, Civil Engineering Department,NIT Kurukshetra for providing constant inspiration, co-operation and

    encouragement throughout the study.

    We are also thankful to the staff of fluid mechanics lab and Mr. Kewal

    Singh of soil mechanics lab of NIT Kurukshetra for their co-operation

    and help during the experiment.

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    ABSTRACT

    The most common cause of bridge failures is floods with the scouring of

    bridge foundations being the most common cause of flood damage to

    bridges.

    The present study attempts to study the scour around a bridge pier

    which is seated in soil containing a particular percentage of clay, and

    produce an equation to determine the relationship between the velocity

    of flow and the scour depth. As clay has adhesive and cohesive

    properties, it is quite logical to expect clay to produce greater forces ofattraction between the particles of silt and decrease the extent of

    scouring around a bridge pier.

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    1. INTRODUCTION

    Bridge scour is the removal ofsediment such assand androcks from

    aroundbridge abutments orpiers. Scour, caused by swiftly movingwater, can scoop out scour holes, compromising the integrity of a

    structure.

    Bridge scour is one of the three main causes ofbridge failure (the others

    being collision and overloading). It has been estimated that 60% of all

    bridge failures result from scour and other hydraulic-related causes.

    Areas affected by Scour:

    Water normally flows faster around piers and abutments making themsusceptible to local scour. At bridge openings, contraction scour canoccur when water accelerates as it flows through an opening that isnarrower than the channel upstream from the bridge. Degradation scouroccurs both upstream and downstream from a bridge over large areas.Over long periods of time, this can result in lowering of the stream bed.

    Causes:

    Stream channel instability resulting in river erosion and changing angles-of-attack can contribute to bridge scour. Debris can also have asubstantial impact on bridge scour in several ways. A build-up ofmaterial can reduce the size of the waterway under a bridgecausing contraction scourin the channel. A build-up of debris on theabutment can increase the obstruction area and increase local scour.Debris can deflect the water flow, changing the angle of attack,increasing local scour. Debris might also shift the entire channel aroundthe bridge causing increased water flow and scour in another location.

    During flooding, although the foundations of a bridge might not sufferdamage, the fill behind abutments may scour. This type of damagetypically occurs with single-span bridges with vertical wall abutments.

    An important consideration in designing the pier is to predict themaximum depth of scour hole so that the foundation of the structure canbe sited deep enough to avoid the possibility of undermining.

    http://en.wikipedia.org/wiki/Sedimenthttp://en.wikipedia.org/wiki/Sandhttp://en.wikipedia.org/wiki/Rockshttp://en.wikipedia.org/wiki/Bridgehttp://en.wikipedia.org/wiki/Abutmenthttp://en.wikipedia.org/wiki/Pier_(architecture)http://en.wikipedia.org/wiki/Bridge_failurehttp://en.wikipedia.org/wiki/Bridge_failurehttp://en.wikipedia.org/wiki/Pier_(architecture)http://en.wikipedia.org/wiki/Abutmenthttp://en.wikipedia.org/wiki/Bridgehttp://en.wikipedia.org/wiki/Rockshttp://en.wikipedia.org/wiki/Sandhttp://en.wikipedia.org/wiki/Sediment
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    2. REVIEW AND LITERATURE

    FACTORS AFFECTING THE SCOUR DEPTH

    a)Effect of velocity of approach:Undisturbed approach flow velocity U, definitely influences the local

    scour depth around bridge piers. As approach velocity increases, there

    is a linear increase in the scour depth till clear water flow condition

    exists. Maximum scour depth is attained at the critical velocity. Chabert

    and Engeldinger (1956) and Laursen (1963) inferred that local live bed

    scour depth is 10% less than the clear water scour depth irrespective of

    the approach velocity of flow. However recent studies have shown that

    when the approach velocity exceeds the threshold velocity. The scour

    depth first decreases and then increases again (Melville, 1988).

    b)Effect of depth of flow:

    For shallow depth of flow local scour depth increases with increases in

    depth of flow. But further increase in depth of flow for a deep flow, the

    scour depth becomes independent of depth of flow. Many researchers

    such as Laursen (1963), Breusers (1977), Ettema (1980) and Chiew

    (1982) have observed the same trend in their experiments. Due to

    obstruction caused by pier, two rollers having opposite direction of

    rotation are created. One is surface roller created around pier near the

    water surface and the other is horse shoe vortex roller created around

    pier near alluvial bed of the channel. As per Melville (1988);

    In principle, as so long (two rollers) do not interfere with each other, the

    local scour depth is independent of floor depth.However following the regime theory, some researchers such as

    Laursen (1963) etc. suggested that depth of local scour increases.

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    c)Effect of sediment size:

    Relatively recent studies have shown that sediment size has a definite

    influence on the local scour, (Nicollet, 1971; Ettema, 1980) Ettema

    (1980) inferred from the laboratory data in clear water, non ripple

    forming sediments that local scour is independent of sediment size so

    long as size of obstruction is greater than or equal to 50 times the size of

    the sediments (D/d5050). Breuseres et al. (1977) argue that effect ofgrain size, d50is limited to a single particle size sediment.

    d)Effect of sediment grading:

    Ettema (1980) and Grade (1989) observed that increase in the standard

    deviation of the particle size distribution of sediments; causing formation

    of armour layer at the base of scour whole decreases both, rate of scour

    and the equilibrium scour depth.

    e)Effect of pier shape:

    Most of the researchers agree on the influence of pier shape on local

    scour depth. It is accepted that blunter the pier facing, the area facingthe flow increases, thereby reversing the flow direction and creating

    more turbulence than a streamlined shape. Melville suggested a shape

    factor to account for the effect of pier shape.

    f)Effect of pier size:

    Interferences made by the researchers regarding the influences of pier

    size on the equilibrium scour depth are not quite debatable. It is directly

    concluded that larger is the size of pier, more is the equilibrium scour

    depth. For all other factors being constant the scour depth varies as D

    where D is width or dia of pier & Toch(1956) design curve corresponds

    to =0.7 (Hsm=1.35D0.7

    h0.3), Larras(1963) suggests =0.75

    (Hsm=1.05D0.75

    ).

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    Theoretical Scouring:

    On the basis of laboratory and some field data, a number of equations

    have been developed. In India, Lacey-Inglis method to estimate scour

    depth DSEis related to Laceys depth as:

    DL= 0.47(Q/f)1/3

    DSE= 2DL

    Here Q is designed flood discharge in cm3/sec, f is Laceys Silt Factor, aconstant of proportionality was obtained from the analysis of scour data

    on 17 bridges in indo- gangetic plains and its value varied from 1.76 to

    2.59 with an average of 2.09 in its basic form with slight variation lacey.

    Inglis method is recommended for D SE by Indian railways and Indian

    road congress . This method is purely empirical in nature and gives

    combined scour caused due to flow modifications by introduction of pier,

    flow construction due to guide bunds and flow concentration due to non

    uniform distribution of flow.

    Mechanism of Scouring

    A bridge pier is spur like obstruction which causes flow acceleration and

    separation at the upstream face of the pier. As the flow moves pass the

    obstacle creating a vortex trial that moves downstream in a direction

    approximately perpendicular to the structure. This results in scouring of

    the bed around the structure locally, Lim(1998). Once a scour hole is

    formed, the scouring mechanism is dominated by the vortex system and

    an associate downfall cause by the stagnation pressure gradient, which

    developed ahead of the structure. The downfall acts like a vertical jet

    impinging and eroding sediment from the bed. The vortex system and

    the down flow, along with cone around the trip of the structure. Melville

    (1992) reported that out of 108 bridges failures recorded in Newzealand

    between the years,1960-1984,29 attributed to fail scour.

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    According to Liu et al (1957) at an pier the approach flow is considered

    to consists of an upper hand lower layer which separates into an upflow

    and downfall on hitting the pier.

    The flow from a surface roller, while the down flow rolls up to form thebottom vortex called the principle vortex . On approaching the pier upper

    layer tends to divide ,part of the flow accelerates along the upstream

    corner of the pier and the remaining flow slowly circulates in the near

    segment pool .

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    3. EXPERIMENTAL STUDIES

    Properties of Soil Used in the Experimental

    Studies

    Sieve size inmicron

    Mass ofparticles

    retained

    Mass ofparticles finer

    Percentagefiner

    4750 0 1000 100

    2360 20 980 98

    1180 15 965 96.5

    600 20 945 94.5

    300 545 400 40

    150 317.5 82.5 8.25

    75 57.5 25 2.5

    Retained on

    pan

    25 1000

    Total 1000

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    10098

    96.594.5

    40

    8.25

    2.50

    10

    20

    30

    40

    50

    60

    70

    80

    90

    100

    0 0.5 1 1.5 2 2.5 3 3.5 4 4.5 5

    %

    Retained

    SIZE(mm)

    Sieve Analysis

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    SEDIMENTS SOURCE AND PROPERTIES

    The sediment was collected from Samani village, Karnal from a lake bed

    to be used in the flume having the following properties.

    Type of sediment = Fine sand

    Medium size of sediments, d50 = 0.45 mm

    D84 = 0.51mm

    D60 = 0.42mm

    D10 = 0.18mm

    D30 = 0.28mm

    Co-efficient of uniformity = d60/d10= 2.33 < 3

    Co-efficient of Curvature = (d30)2/d10.d60 =1.034

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    Properties of Clay Used:

    35.5

    36

    36.5

    37

    37.5

    38

    38.5

    39

    39.5

    40

    40.5

    3.688 3.583 3.258 2.944

    Watercontent

    (W%)

    No. of blows (N)

    Flow Curve

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    S.No. Weight of

    empty

    container(gm)

    W1

    Wt. of

    container +

    wet soil(gm)

    W2

    Wt. of

    container

    +dry soil(gm)

    W3

    Water content

    (%)

    (W2 -W3)*100/(W3W1)

    No. of

    blows

    1. 26.79 52.63 45.64 37.08 40

    2. 25.36 43.78 38.72 37.87 36

    3. 26.26 57.52 48.76 38.9 26

    4. 27.23 55.88 47.76 40.14 19

    Liquid Limit (L.L.) = 39%

    Ip = 0.73( L.L. -20) = 14%

    Plastic Limit = L.L. - Ip = 25%

    Specific Gravity = 1.658

    So, clay is Medium plastic clay.

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    Experimental Setup

    Flume: A flumeis man-madechannel for water, in the form of anopen inclinedgravity chute whose walls are raised above the

    surrounding terrain, in contrast to atrench orditch.Flumes

    leadwater from adiversion dam orweir to their desired location.

    The experiment was conducted in a 12m long, 40cm wide and 60cm

    deep tilting bed flume in a fluid mechanics laboratory of NIT kurukshetra.

    There were 2 panels of glass for visual observation and rest of panels

    were made of steel plates on both sides. It was supported on a steel

    truss with a jack for the adjustment of bed slope. The water pumped

    from a sump channel with the help of 15 hp centrifugal pump which is

    discharging into a stilling tank upstream of the flume. The pump was

    drawing water from the sump 2.75 x 1.75 m in a plane and 1.75 m deep

    and delivering water at the upstream channel. Channel bed was levelled.

    Further, a tailgate was provided at the flume to control the flow of water

    after passing through the flume goes to a rectangular tank. The outlet

    channel from the concrete tank passes the flow over the sharp crested

    weir of height 40 cm provided in a 60 cm wide channel to measure the

    discharge downstream before entering to the sump channel. The pier is

    a placed at a distance of 3 m diameter and is fitted in a prepared bed of

    soil length 40 cm consisting of 30% clay and 70% sand by weight the

    detail of experimental setup is given in the diagram.

    http://en.wikipedia.org/wiki/Watercoursehttp://en.wikipedia.org/wiki/Chute_(gravity)http://en.wikipedia.org/wiki/Trenchhttp://en.wikipedia.org/wiki/Ditchhttp://en.wikipedia.org/wiki/Waterhttp://en.wikipedia.org/wiki/Diversion_damhttp://en.wikipedia.org/wiki/Weirhttp://en.wikipedia.org/wiki/Weirhttp://en.wikipedia.org/wiki/Diversion_damhttp://en.wikipedia.org/wiki/Waterhttp://en.wikipedia.org/wiki/Ditchhttp://en.wikipedia.org/wiki/Trenchhttp://en.wikipedia.org/wiki/Chute_(gravity)http://en.wikipedia.org/wiki/Watercourse
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    Model setup and Experimental procedure

    The pier models are used in experiments in circular pier of a diameter 4cm and length 100 cm. A uniform flow of a certain known velocity is set

    in the flume. Care is taken to ensure the height of water flow is atleast

    2.15 times the diameter of the pier and also there is no disturbance in

    the soil bed profile .The flow goes on for 3 hours and then the maximum

    scour depth around the pier is noted down by using a bent point gauge

    so that the scour depth can be taken more accurately and efficiently.

    The height of water over the rectangular sharp crested weir installed at

    the end of the flume is also noted down .And the discharge of water is

    calculated in the flume using the following formulae:

    1. Rehbocks formula is usedto calculate the coefficient of dischargeof the sharp crested weir

    Cd= 0.611 + 0.08 Hw/ P

    Where, Hw= head over weir

    P = height of weir

    2. Discharge is calculated using the following equation

    Q = 2/3 Cd 2 g X L X Hw3/2

    Where, Q = discharge

    L= Width of channel where weir is provided

    Velocity of flow V = Q/(H X W)

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    FLOW CONDITIONS

    Uniform Flow ConditionsStudies on sediment bed were conducted under conditions of uniformflow. Turbulence is diminished using honeycombing at the head of thejet.

    Velocity of Flow

    After a few initial trails by regulating tail control gate & regulating valveand varying the velocities varying from 10cm/sec to 21cm/sec, a criticalvelocity equal to 19.32cm/sec was established just below the incipientmotion of the sediment where the particle just started moving under theinfluence of flow without formation of bed features. This is the velocityjust below the incipient motion of the sediment and which wasmaintained throughout for most of the experiment. Discharge wasmeasured with the help of an already calibrated orifice meter fitted in thedelivery outlet

    Depth of Flow

    In order to minimize the effect of flow depth on the flume was kept equalto or greater than 2.5 x diameter of the pier. Scour depth becomesalmost independent of flow depth.

    Duration of Test Run

    Duration of test run was taken as 3 hours.

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    Scour Measurements

    Initially the sediment bed mixed with 30% of clay and labelled acrossand along the flow direction. The pier model was fixed with the glasspanel section of the flume. The critical velocity of the Ucwas determinedto be 19.32cm/sec .

    The flow was started and water was allowed to accumulate in thechannel by closing the gate. Then water head maintained to avoid themovement of particles with water by adjusting the gate. Then theparticular required head is maintained in the manometer for the

    experiment. This is done by varying the discharge in the jet by the helpof valve. Then the required water depth of upstream of the pier hasmaintained by varying the tailgate opening. After this, labelling in thechannel around the pier model was done. This instant markedcommencement of the test run.

    Reading for the scour depth was taken at the upstream of the outer edgeof the pier and also at the locations where the scour depth could bemaximum. Scour depth measurement were taken with the help of

    improvised Z shaped point gauge . After 3 hours stopping the flow thestatic scour profile of the sediment was recorded by taking scour depthof the pier. critical velocity was calculated by taking the observations ofthe sediments at the various discharge .Scour depth for various velocities and flow depths were observed .

    Criteria For Analysis

    The maximum scour depth at a point the periphery of the pier observedis used for the particular experiment at the end of experiment was takenas the criteria for the analysis of the study.

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    OBSERVATIONS

    EXPERIMENTAL DATA

    S. No. Hw

    (cm)

    Cd Q(cm3/s) H

    (cm)

    Velocity

    of flow

    (cm/s)

    Time

    (hours)

    Scour

    depth (cm)

    1. 5.0 0.621 12300 22.20 14.0266

    1 0.800

    2 1.175

    3 1.325

    2. 5.0 0.621 12300 18.30 17.0159

    1 0.950

    2 1.550

    3 1.900

    3. 5.0 0.621 12300 15.60 19.9610

    1 1.125

    2 1.800

    3 2.250

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    As it can be observed, the results point closely to the equation

    SD = 0.1558V-0.8613

    Where SD= Scour Depth (cm)

    V= Velocity of Flow (cm/s)

    0

    0.5

    1

    1.5

    2

    2.5

    14.0266 17.0159 19.961

    Scourdepth(cm)

    Velocity(cm/s)

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    CONCLUSIONS

    1.Local scouring phenomenon was studied for a

    circular pier resting in a prepared bed consisting

    of 30% clay & 70% sand.

    2.Relationship was established between velocity of

    flow and scour depth