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Geological Considerations in Civil Engineering

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    Geological Considerations In

    Civil Engineering

    Engineering Geology

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    Considerations for:

    Selection of site for dams

    Selection of site for reservoirs

    Construction of tunnels

    Construction of mountain roads

    2

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    Selection of site for dams

    3

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    Need for dams

    For hydroelectric power generation For irrigation purposes

    To obtain water for domestic and industrial

    purposes

    For fighting draughts and controlling floods

    For navigational facilitiesAdditional benefits include development of

    fisheries, tourism etc

    4

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    Types of Dams

    On the basis of design:

    o Gravity dams

    o Buttress dams

    o Arch dams

    o Earth dams

    5

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    1. Gravity dam

    A solid concrete or masonry structures, thatwithstands the water pressure, by virtue of its

    weight

    All forces acting on the dam are assumed to

    be directly transmitted to the foundation rocks

    They are generally of triangular profile andare among the safest

    6

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    Concrete GravityDam

    http://nptel.iitm.ac.in/courses/Webcourse-contents/IIT%20Kharagpur/Water%20Resource%20Engg/pdf/m4l04.pdf

    http://nptel.iitm.ac.in/courses/Webcourse-contents/IIT%20Kharagpur/Water%20Resource%20Engg/pdf/m4l04.pdfhttp://nptel.iitm.ac.in/courses/Webcourse-contents/IIT%20Kharagpur/Water%20Resource%20Engg/pdf/m4l04.pdfhttp://nptel.iitm.ac.in/courses/Webcourse-contents/IIT%20Kharagpur/Water%20Resource%20Engg/pdf/m4l04.pdfhttp://nptel.iitm.ac.in/courses/Webcourse-contents/IIT%20Kharagpur/Water%20Resource%20Engg/pdf/m4l04.pdf
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    8

    Grand Coulee Dam onColumbia river

    http://en.wikipedia.org/wiki/Grand_Coulee_Dam

    http://en.wikipedia.org/wiki/Grand_Coulee_Damhttp://en.wikipedia.org/wiki/Grand_Coulee_Damhttp://en.wikipedia.org/wiki/Grand_Coulee_Dam
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    2. Buttress dam

    They have a continuous upstream face,supported at regular intervals, by buttress

    walls on the downstream side

    They are lighter than solid dams

    Likely to induce greater stresses at the

    foundation, since most of the load passesthrough the buttress walls and is not spread

    uniformly over the foundation

    9

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    Buttress dam

    http://nptel.iitm.ac.in/courses/Webcourse-contents/IIT%20Kharagpur/Water%20Resource%20Engg/pdf/m4l04.pdf

    http://nptel.iitm.ac.in/courses/Webcourse-contents/IIT%20Kharagpur/Water%20Resource%20Engg/pdf/m4l04.pdfhttp://nptel.iitm.ac.in/courses/Webcourse-contents/IIT%20Kharagpur/Water%20Resource%20Engg/pdf/m4l04.pdfhttp://nptel.iitm.ac.in/courses/Webcourse-contents/IIT%20Kharagpur/Water%20Resource%20Engg/pdf/m4l04.pdfhttp://nptel.iitm.ac.in/courses/Webcourse-contents/IIT%20Kharagpur/Water%20Resource%20Engg/pdf/m4l04.pdf
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    Buttress Dam on Lower ColoradoRegion

    simscience.org

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    3. Arch dam

    Arch-shaped, convex at the upstream side

    Major portion of the thrust forces acting on

    the dam are transmitted by arch action, onto

    the abutment rocks

    Structural efficiency is higher than that of

    gravity dams, the presence of sound abutments

    is a prime necessity

    Uses less amount of concrete

    12

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    13

    Idukki Dam

    panoramio.com

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    4. Earth dam

    Non-rigid structures, built with naturally

    available materials such as earth and rock

    Ideal, where the dam site is weak to support

    concrete dams, or where competent rocks arefound at great depths

    14Homogenous, with toe drain Homogenous, with chimney drain

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    15

    Hirakud Dam, across the Mahanadi, Orissa

    panoramio.com

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    Forces acting on a dam

    Self weight

    Water pressure

    Uplift pressure

    Earthquake forces

    Other forces due to silt, wave and ice

    16

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    Geological considerations

    Narrow river valley

    Occurrence of bedrock at shallow depth

    Competent rocks to offer stable foundation

    Proper geologic structures

    17

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    1. Narrow river valley

    Narrow valley means smaller dam is required,

    and hence, lower costs

    Defective valleys include:

    o Deceptive narrowing due to thick superficial

    deposits

    o Narrowing due to rock outcrops

    o Presence of soluble material like gypsum,

    renders the rocks unsuitable

    18

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    Some defective narrow river valleys

    Chenna Kesavulu

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    2. Occurrence of bedrock at shallow depth

    The presence of strong bedrock near thesurface, reduces the cost of the foundation

    The site should be explore using electrical

    resistivity or seismic refraction methods, to

    assess the nature of the bedrock

    The presence of buried river valleys, huge

    boulders gives rise to problems, as they are

    composed of lose material

    20

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    3. Competent rocks for stable foundation

    Igneous rocks are safer than sedimentary ones

    Suitability of site depends on:

    The existing rock type

    The extent of weathering undergone

    The extent of fracturing

    The occurrence of geological structures

    The mode and number of rock types

    21

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    4. Proper geologic structures

    Undisturbed strata Disturbed strata

    Tilted beds

    Folded strata

    Faulted strata

    Jointed strata

    22

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    Undisturbed strata

    Chenna Kesavulu

    Gravity dam on horizontal beds

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    24Chenna Kesavulu

    Dam on beds inclined in the upstream direction

    Gentle inclination Steep inclination

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    25

    Dam on beds inclined in the downstream direction

    Gentle inclination Steep inclination

    Chenna Kesavulu

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    26Chenna Kesavulu

    Dam over vertical beds

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    27Chenna Kesavulu

    Dam over folded beds

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    28Chenna Kesavulu

    Dam over faulted beds

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    Selection of site for Reservoirs

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    Gibson Reservoir, Montana

    http://en.wikipedia.org/wiki/Gibson_Reservoir

    http://en.wikipedia.org/wiki/Gibson_Reservoirhttp://en.wikipedia.org/wiki/Gibson_Reservoirhttp://en.wikipedia.org/wiki/Gibson_Reservoir
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    Categorization of Reservoirs

    Storage and conservation reservoirs

    Flood control reservoirs

    Distribution reservoirs

    31

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    Storage Capacity of a Reservoir

    Storage capacity is expressed in terms of:

    o Useful storage

    o Dead storage

    o Surcharge storage

    32

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    http://nptel.iitm.ac.in/courses/Webcourse-contents/IIT%20Kharagpur/Water%20Resource%20Engg/pdf/m4l05.pdf

    Reservoir StorageCapacity

    http://nptel.iitm.ac.in/courses/Webcourse-contents/IIT%20Kharagpur/Water%20Resource%20Engg/pdf/m4l05.pdfhttp://nptel.iitm.ac.in/courses/Webcourse-contents/IIT%20Kharagpur/Water%20Resource%20Engg/pdf/m4l05.pdfhttp://nptel.iitm.ac.in/courses/Webcourse-contents/IIT%20Kharagpur/Water%20Resource%20Engg/pdf/m4l05.pdfhttp://nptel.iitm.ac.in/courses/Webcourse-contents/IIT%20Kharagpur/Water%20Resource%20Engg/pdf/m4l05.pdf
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    Influence of rock types

    Influence of geological structures

    Influence of water table

    Reservoir silting

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    Geological considerations

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    1. Influence of rock types

    Igneous rocks such as granites are less porous,

    hence will afford more stability

    Sedimentary rocks are often porous, but are

    more abundant than igneous ones

    Metamorphic rocks like gneisses behave like

    granites

    The nature of rocks are important, as theydetermine the leakage of water through the

    foundations

    35

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    2. Influence of geological structures

    Downstream dip of bedding planes, contribute

    to loss of water, development of uplift

    pressure

    Water can leak through a tilted permeablebed extending to a lower valley

    In certain cases, folding and faulting of the

    strata can prevent leakage of water

    36

    I li d b d d l k t i it

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    37Chenna Kesavulu

    Inclined beds and leakage at reservoir sites

    Leakage at reservoir sites due to geological structure

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    38Chenna Kesavulu

    Leakage at reservoir sites due to geological structure

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    3. Influence of water table

    Position of the water-table is the singlemost factor influencing the leakage of

    reservoir water. Rivers can be of:

    o Effluent nature

    o Influent nature

    39

    I fl f t t bl

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    Influence of water table

    Chenna Kesavulu

    l

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    Reservoir silting

    Deposition of sediments by rivers, gradually

    reduces the capacity of the reservoirs

    Silting can be controlled by:

    Growing vegetation on loose soil

    Covering weak zones with slabs

    Constructing retaining walls

    Diversion of sediment loaded waters

    Silt outlets

    Check dams and settling basins41

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    Construction of tunnels

    42

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    Purposes of Tunneling

    For facilitating rail and road traffic

    For public utilities

    For power generation

    For mining activities

    For diverting water during dam construction

    43

    T l b i hi

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    44

    Tunnel boring machine

    http://en.wikipedia.org/wiki/File:Tunnel_Boring_Machine_(Yucca_Mt).jpg

    http://en.wikipedia.org/wiki/File:Tunnel_Boring_Machine_(Yucca_Mt).jpghttp://en.wikipedia.org/wiki/File:Tunnel_Boring_Machine_(Yucca_Mt).jpg
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    Objects of Geological investigations

    Selection of tunnel alignment

    Selection of excavation method

    Selection of tunnel design

    Assessment of cost and stability

    Assessment of environmental hazards

    45

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    Geological profile along the tunnel axis

    Includes information regarding:

    o Location and depth of exploratory bore holes

    o Types of rocks and their characteristics

    o Structure of the rocks

    o Hydrological conditions

    o Ground temperature conditions

    46

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    47Parbin Singh

    Geological Profile

    F k i t ll ti f t l li i

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    48

    Formwork installation for tunnel lining

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    Geological considerations

    Types of rocks Geological structures

    Ground water conditions

    Overbreak

    49

    1 Types of rocks

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    1. Types of rocks

    Igneous rocks

    Competent, but difficult to work with

    Do not require lining

    Sedimentary rocks

    Less competent, compared to igneous

    Sandstones, shales etc are soft, easy to work

    Requires lining

    Metamorphic rocks

    Gneisses are similar to granites 50

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    2. Geological structures

    Effect of joints Effect of faults

    Effect of folds

    Effect of undisturbed or tilted strata

    51

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    52Chenna Kesavulu

    Tunnels in relation to joints, faults and shear zones

    Joints parallel to tunnel axis Joints perpendicular to tunnel axis

    T l ll l h i f f ld

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    53Chenna Kesavulu

    Tunnels parallel to the axis of fold

    T l di l t th i f f ld

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    54Chenna Kesavulu

    Tunnels perpendicular to the axis of fold

    T l thi k i li d h i t l b d

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    55Chenna Kesavulu

    Tunnels on thick, inclined or horizontal beds

    T l l i li d b d

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    Tunnels along inclined beds

    Tunnel along strike ofinclined bed

    Tunnel along dip of inclinedbed

    Chenna Kesavulu

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    3. Ground water conditions

    Tunnel axis passing entirely through imperviousformations

    Tunnel axis mostly above the water table

    Tunnel axis below the water table

    57

    4 Overbreak

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    4. Overbreak

    Tunneling through hard rocks requires the removal

    of some rocks outside the proposed perimeter

    This excess quantity of rock removed, is called

    the overbreak

    Geological factors governing the amount of

    overbreak are:

    The nature of the rocks

    Orientation of the joints

    Orientation of bedding planes58

    Overbreak

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    Overbreak

    Cases where overbreak is lessChenna Kesavulu

    O b k ( td)

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    Overbreak (contd)

    Cases where overbreak is more

    Chenna Kesavulu

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    Construction of roads

    61

    A road in Vietnam, 1900m above msl

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    62rickmann-uk.com

    ,

    I fl f G l i l f

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    Influence of Geological factors

    Topography Lithological characters

    Consolidated hard rock

    Unconsolidated material

    Geological structures

    Weathering

    Groundwater conditions

    63

    Geological structures

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    g

    Road cut parallel to dip Road cut parallel to strike

    Beds dip into the hill - safe

    Chenna Kesavulu

    Geological structures & weathering

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    Joint sets inclined towardsfree face

    g g

    Unequal weathering causingrock fall

    Chenna Kesavulu

    C li d i f d i

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    Complicated regions for road construction

    Hilly areas - meandering

    Marshy regions - subsidence

    Waterlogged areas capillary action

    Permafrost regions blanket action

    66

    Geological problems after road

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    Geological problems after roadconstruction

    Frost action

    Replacing the porous soil

    Lowering the water table Erosion problems

    Provision of interception ditches

    67

    R f

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    Parbin Singh, Engineering and General Geology, S KKataria & Sons

    Chenna Kesavulu, N, Textbook of Engineering Geology,

    MacMillan India

    Thompson, G R and J Turk, Introduction to Physical

    Geology, Thomson Brooks/Cole

    Reference