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Engg. Geology

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    St. Francis Dam, Ca. 1926.EngineeringGeology

    Concrete gravity dam constructed in 1926 inCalifornia collapsed 1928

    Rock was Schists and soft argillaceous conglomerateseparated by a distinct fault

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    Other dam failures

    Engineering GeologyIntelligent and useful application of geologicalknowled e to different branches of en ineerinconstitutes the subject matter ofENGINEERINGGEOLOGY

    Includes- Geological studies in the fieldand laboratory, Safety and economic

    p ann ng an execu on. s s anextensive field where the science of theearth and the art of engineering mergeinto each other

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    Condition required to successof dam.

    Water tight reservoir basin

    Low rate of accumulation of silt

    A narrow river channel

    Safe foundation

    Provision for disposal of surplus waterthrough suitable gateway

    Availability of the required material forconstruction nearby

    Geology of dam sites and reservoir

    Reservoir may fail due to excessiveleakage or as a result of rapidaccumulation of silt.

    Some rocks are porous and pervious and

    .Unconsolidated or partially consolidatedcourse sandstones are highly porous andpermeable.

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    Geology of dam sites and reservoircontd

    Massive igneous or metamorphic rocks.

    contain well developed joints and otherweakness planes, shear zones, faults

    the nature and position of water table

    and also the nature and structure of therocks forming the region

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    Geology of Bridge structure

    A railway bridge is being constructed at a height of 186m from bed level,

    between chainages 38.430 Km on left abutment to Katra side and chainage

    39.087 Km on right abutment to Reasi side.

    Chainage :38.430 Chainage :38.510

    P1

    River is flowing SW

    O = Center point of

    Katra Side

    Steel arch

    O

    Viaduct span

    Viaduct spans

    Chainage :39.087

    Chainage :38.775

    (P10)

    River

    bridge

    Lat 31o0445

    Long 74o5452

    Viaduct towards katra = 80 mSteel arch span = 265 mViaduct towards Reasi = 312 mTotal length of bridge80 + 265 +312 = 657 m

    E

    N

    Reasi Side

    Reasi sideKatra side

    740

    760

    780

    800

    Figure showing left abutment at Katra

    side with foundation locations of P1b and P1.

    -50

    0

    5038.46

    38.4838.5

    38.5238.54

    660

    680

    700

    720

    Figure showing right abutment on Reasi

    side with foundation locations of P10 to P21View of left and right abuttment

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    Sound rock profile underneath the floor

    Geology of Bridge structure

    and walls of natural depression

    Foundation and abutment should bestrong

    Geolo ical structure of the countr rockshouldnt create any stability problem

    Erosional action of the fast runningwater should be significant

    Geology of Bridge structure

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    Geology of tunnel site

    Governing Geological factors

    The nature of the country rock alongthe ali nment of the tunnel

    The geological structure of the region

    Position of the water table andprevailing ground water table

    condition along the length of thetunnel

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    Tunneling in rocks

    depends upon the nature of rock. Hardcrystalline rocks are very good but verydifficult to excavate

    Moreover they may also contain planes ofweakness. Proper profiling is difficult.

    Consolidated massive sandstones aregood but softer ones need some linings

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    Lining should varypoint to point

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    Nature of rock, orientation and spacing ofdiscontinuity, orientation of bedding planes with

    respect to the alignment

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    Overbreak

    overbreak than hard rock with welldefined and closely spaced discontinuityplanes

    In sedimentary rock more over breakoccurs along the strike than the dip

    Too much overbreak increases the costof tunnelling

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    Stability of Hill slopes

    The nature of the rocks occurring alongthe slope or cutting wall

    The geological structure of the countryrock

    The prevailing ground water conditions

    along the slope or cutting wall

    Stability of Hill slopes

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    Different kinds of U/gwater- a) soil water b)

    pellicular water in fracturedrock, c) pellicular water in

    sedimentary rocks d)Vadose water p) perchedwater WT-Water table E)

    Ground water e) Free

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    Building stonesStrength and durability mineralcom osition texture and structure

    Colour and beauty

    Cost

    ,mica are st carbonate rocks marble,limestone are relatively weak and wornout easily rong and durable where as

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    Building material(aggregates)road metals

    durable and there shouldnt betendency to react with cement

    For good road metals a) hard b) toughc) resistant to abrasion d) high

    cementing value


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