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Table of Contents

Self Purification of Stream - Environmental Engineering

Self Purification of Stream A polluted stream undergoes self-purification Zone A – Zone of clear water Zone B – Zone of Degradation Zone C –...

Self Purification of Stream


A polluted stream undergoes self-purification

  • Zone A – Zone of clear water
  • Zone B – Zone of Degradation
  • Zone C – Zone of Active decomposition
  • Zone D – Zone of Recovery
  • Zone E – Zone of recovery

Zone

Main Characteristics

Zone of Clear Water (1 & 5)

Clear water,  presence of fishes.

100% saturation

Zone of Degradation (2)

Dissolved oxygen level falls due to the decomposition of Organic Matter in this Zone.

Dark and turbid water.

Fishes may present

Algae are absent.

40% saturation

Zone of Active Decomposition (3)

Zone of heavy pollution.

Water is very dark and turbid

Dissolved oxygen level falls to Zero.

Critical Oxygen Deficient occurs.

Formation of the dirty scum layer.

Both fishes and algae absents

0% saturation

Zone of recovery (4)

Dissolved oxygen level increases and may reach to saturated value.

Decomposition of organic matter takes place up to the Nitrate level.

Both fishes and Algae reappear.

BOD falls down.

40% saturation




Purification of sewage in river

When sewage or sewage effluents are discharged into the river, river gets polluted temporary, but the conditions do not remain so forever, because the natural forces  of purification such as dilution, sedimentation, oxidation, reduction in sunlight go on acting upon the pollutants  and bring back the water into its original condition. This process known as self purification and various forces responsible for this are described briefly below:

1. Dilution and Dispersion: 

  • When sewage is discharged into large volume of river water, it gets rapidly dispersed and diluted. This results in reduction of concentration of organic matter in sewage.

2. Sedimentation: 

  • The suspended solids in sewage gets settle down into the river bed by the action of gravity.

3. Oxidation: 

  • The organic matter present in sewage gets oxidized by the microorganisms with the help of dissolved oxygen present in river and results in formation of stable products.

4. Reduction: 

  • It occurs due to hydrolysis of organic matter settles down at the bottom of river bed either chemically or biologically.

The above natural forces of purification depend on various factors which are:

  • 1. Temperature
  • 2. Turbulence
  • 3. Velocity of river stream
  • 4. Availability of dissolved oxygen
  • 5. Type and amount of organic matter present
  • 6. Rate of re-aeration.




Important Terms

Hydrolysis:

  • It is a chemical process in which a molecule is cleaved into two parts by the addition of a molecule of water. One fragment of the parent molecule gains a hydrogen ion (H+) from the additional water molecule. The other group collects the remaining hydroxyl group (OH-).

Pyrolysis

  •  It is the process in which the most of organic matter upon heating in an oxygen free atmosphere splits through a combination of thermal cracking and condensation reactions into gaseous, liquid and solid fractions.
  • The process typically occurs at temperatures above 430 °C (800 °F) and under pressure. It simultaneously involves the change of physical phase and chemical composition and is an irreversible process. So it is an endothermic process.

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Disposal of refuse and Sewage sickness of Land Method of disposal of refuse Landfill or Burying: Landfill refers to the disposal of waste ma...

Disposal of refuse and Sewage sickness of Land


Method of disposal of refuse


Landfill or Burying:

  • Landfill refers to the disposal of waste material by burying it.
  • It is an extended storage area for non-biodegradable waste.
  • Landfill is an area, which prevent contamination from the waste entering the area surrounding by soil and water and it also helps to reduce odor and pests

Incineration: 

  • This method involves burning of solid wastes in a furnace until the wastes are turned into ashes
  • In this process, the combustible portion of the waste is combined with oxygen forming carbon dioxide and water, which are released into the atmosphere
  • Incinerators are made in such a way that they do not give off extreme amounts of heat when burning solid wastes
  • Suitable temperature and operating conditions are required to achieve for incineration
  • It reduces the volume of waste up to 20 or 30% of the original volume
  • This method of solid waste management can be done by individuals, municipalities and even institutions
  • It involves of two stages involved such as drying and combustion. Drying and combustion may be accomplished either in separate units or successively in same units depending upon the temperature constraints or control parameter. It is an exothermic process.

Fluidized bed incineration:

  • It is a combustion technology used to burn solid fuels. 
  • In its most basic form, fuel particles are suspended in a hot, bubbling fluidity bed of ash and other particulate materials (sand, limestone etc.) through which jets of air are blown to provide the oxygen required for combustion or gasification. 
  • The resultant fast and intimate mixing of gas and solids promotes rapid heat transfer and chemical reactions within the bed

Pulverization 

  • It refers to the action of crushing and grinding heavier solids into the lighter solids.

Composting 

  • It is a natural biological process, carried out under controlled aerobic conditions (requires oxygen).
  • In this process, various microorganisms, including bacteria and fungi, break down organic matter into simpler substances.
  • The effectiveness of the composting process is dependent upon the environmental conditions present within the composting system i.e. oxygen, temperature, moisture, material disturbance, organic matter and the size and activity of microbial populations.


process of composting


Bangalore method

  • It is an anaerobic method conventionally carried out in pits. 
  • In the Bangalore method of composting, dry waste material of 25 cm thick is spread in a pit and a thick suspension of cow dung in water is sprinkled over for moistening.

Indore method

  • It is an aerobic method. 
  • The Indore method of composting in pits involves filling of alternate layers of similar thickness as in the Bangalore method.
  • However, to ensure aerobic condition the material is turned at specific intervals for which a 60 cm wide strip on the longitudinal side of the pit is kept vacant.

There are mainly two methods (Indore and Bangalore method) adopted in India for the decomposition of Solid wastes generated. 


The main difference between Indore Method and Bangalore Method for decomposition of MSW is given below:



Indore Method

Bangalore Method

Decomposition of MSW by composting is done aerobically.

Decomposition of MSW by composting is done an-aerobically.

Decomposition takes 2 - 3 Months

Decomposition takes 5 - 6 Months

Mixing is ensured either Mechanically or manually

 No mixing is done.





  • In Composting with a combination of proper environmental conditions and adequate time, microorganisms turn raw putrescible organic matter into a stabilized product.
  • Through composting, readily available nutrient and energy sources are transformed into carbon dioxide, water, and a complex form of organic matter compost. 
  • Process management can be optimized for a number of criteria, including the rate of decomposition (to reduce residence time in reactors and thus minimize facility size requirements), pathogen control, and odour management.
  • The key parameters are the available carbon to nitrogen (C: N) ratio, moisture, oxygen, and temperature.
  • Decomposition slows dramatically in mixtures under 40 to 45 percent moisture, which can lead facility operators to prematurely assume compost is stabilized and ready to sell.
  • A minimum moisture content of 50 to 55 percent is usually recommended for high rate composting of MSW.
  • During the active composting phase, additional water usually needs to be added to prevent premature drying and incomplete stabilization. MSW compost mixtures usually start at about 52 percent moisture and dry to about 37 percent moisture prior to final screening and marketing.



C/N ratio is an important factor in composting


  • since bacteria use nitrogen for their cell structure building and carbon for food.
  •  The optimum composting C/N ratio should be in range (30 - 50)
  •  So, If C/N ratio is more, Nitrogen is utilized prior to that of carbon, which results in incomplete digestion of organic matter.

gases produced from a land fill site


  • Sanitary landfill involves dumping the waste in layers and compacting them after each layer, hence tractor can be used very effectively for this purpose.It is simple and economical.

  • But there is continuous evolution of foul gases which may be explosive in nature. The major constituent gases produced from a land fill site are carbon dioxide and methane.

  • It also causes leachate in landfills which pollutes the nearby ground water thereby impacting the ecology of the area.



Sewage sickness of  Land: 

  • When sewage is applied continuously on a piece of land, the soil pores or voids may get filled up and clogged with sewage matter retained in them. This phenomenon of soil getting clogged is known as sewage sickness of the land.
The following preventive measures may be adopted to avoid sewage sickness:

Pre-treatment of sewage   

Sewage should be given some pre-treatment before it is applied on land.

Rotation of crops

It is desirable to grow different types of crops on a piece of land instead of one single crop. Rotation of crops minimizes the chances of sewage sickness.

Drainage of soil

Subsoil drain pipes should be laid in sufficient number to collect the percolated effluent.

Depth of sewage

The depth of sewage on land should be carefully decided by keeping in view the climatic conditions, drainage facilities, nature of crops, and characteristics of the soil.

Alternative arrangement

 There should be ample provision of extra land so that land with sewage sickness can be given the desired rest.

Intermittent application

Sewage should be applied on land at intervals. The period between successive applications depends on the general working of sewage farms and the permeability of the soil. Depending on the nature of the soil, this period between successive applications varies from few hours to few weeks.

Treatment to land

The land affected by sewage sickness should be properly treated before it is put up in use again. Clogged surfaces should be broken by suitable equipment.






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Environmental Engineering for Civil Engineers Water Supply and Sewage Treatment. Water Supply Sewage Treatment water Dis...

Environmental Engineering

for Civil Engineers



Water Supply and Sewage Treatment.

Latest Article

Types Treatment unit and its Mechanism

for example - trickling filter, Oxidation pond, Septic tank and its nature like aerobic or anaerobic process More

Disposal of refuse.

Method of disposal of refuse, process of composting, C/N ratio in composting Read More

Self Purification of Stream

A polluted stream undergoes self-purification, Purification of sewage in river Read More .

Sewage Sickness of Land

When sewage is applied continuously on a piece of land, the soil pores or voids may get filled up and clogged with sewage matter retained in them. This phenomenon of soil getting clogged is known as sewage sickness of the land. Read More

Important Content

The density in kg/cum (in situ) of municipal solid waste

The density of municipal solid waste for a typical Indian city is 400 kg/cum to 600 kg/cum with a calorific value of 5000 to 6000 kJ/kg.

The density of municipal solid waste for a typical city of the USA is 100 kg/cum to 600 kg/cum with a calorific value of 15000 kJ/kg approximately.

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Popular in Civil Engineering

Important Theories.

Types of Footing and Settlement

Types of shear failure:

IS code specification for permissible settlement of Foundation

more

Solid Waste

Important for Exams

  • Pyrolysis
  • Hydrolysis
  • Purification of sewage in river
  • Tunnels

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Important theories and its assumption on Soil Mechanics

Most Important theories used in soil mechanics as engineer Boussinesq Theory   Westergaard Theory   Coulombs Theory of Earth Pressure  Te...

Most Important theories

used in soil mechanics as engineer



Boussinesq Theory 


Boussinesq Theory: for stress strain relationship, due to a point load on surface:

  • The Boussinesq method on Soil Mechanics uses the theory of elasticity to calculate the vertical stress under a point load in a homogeneous, semi-infinite half space its assumptions is very important for civil engineers to remember for solving many important civil engineering problems
  • The stresses within a semi-infinite, homogeneous, isotropic mass, with a linear stress–
    strain relationship, due to a point load on the surface, were determined by Boussinesq
    in 1885

Assumptions consider on Boussinesq theory

  • Soil is Homogeneous and Isotropic, Semi-infinite and elastic.
  • Soil is Fully Saturated means Presence of zero air voids.
  • Soil is Initially unstressed.
  • Stress Distribution diagram about vertical axis is symmetrical.
  • Any Change in volume of Soil due to Load is Neglected.
  • Hooks law is Valid.
  • Self weight of soil is neglected.

Equations


`\sigma=\frac{3Q}{2\pi z^2}\left[\frac1{1+\left(\frac rz\right)^2}\right]^\frac{5}{2}` 
 
The vertical, radial, circumferential and shear stresses at a depth z and a horizontal distance r from the point of application of the load in boussinesq theory on soil mechanics

Kb is known as influence factor

Westergaard Theory

Assumptions of Westergaard Theory for soil mass in civil engineering

  • Soil is Homogeneous and Isotropic and Elastic.
  • Soil is consider as Cohesive like- clay.
  • Soil profile is Layered.
  • Here, μ= Poisson's Ratio. If Poisson's Ratio is considered zero for all practical purposes

Equations

  • `\sigma_z=\frac{Q}{\pi z^2}\left[\frac1{1+2\left(\frac rz\right)^2}\right]^\frac{3}{2}`
  • `\sigma_z=\frac Q{z^2}I_w`
  • Where,  Q is the point load and σz is the vertical stress due to the point load,
  • `I_w=\frac1\pi\left[\frac1{1+2\left(\frac rz\right)^2}\right]^\frac3{2}`


\sigma=\frac{Q}{\pi z^2}\left[\frac1{1+2\left(\frac rz\right)^2}\right]^\frac{3}{2}`




Coulomb's Theory of Earth Pressure on Retaining wall

  • Coulomb’s theory (1776) involves consideration of the stability, as a whole, of the wedge of soil between a retaining wall and a trial failure plane.
  • The force between the wedge and the wall surface is determined by considering the equilibrium of forces acting on the wedge when it is on the point of sliding either up or down the failure plane, i.e. when the wedge is in a condition of limiting equilibrium

Assumptions of Coulomb's Theory of Earth Pressure for determining

  • Soil mass is Homogeneous,Dry and Isotropic and ideally plastic.
  • Back-fill is ideally plastic material and dry.
  • Back-fill is cohesion-less like - Sand.
  • Back of the wall surface is rough means frictional retaining wall and inclined
  • The sliding Wedge itself act as a rigid body. i.e the equilibrium of the whole of the material.
  • The Coulomb's theory is now interpreted as an upper bound plasticity solution


Terzaghi Theory or Terzaghi’s Bearing Capacity Theory

Assumptions

  • Soil is Homogeneous and Isotropic.
  • Soil is fully Saturated.
  • Soil is considered as Hydrodynamic clay.
  • No soil consolidation.
  • Foundation is very Rigid.
  • No applied Moment present.
  • Soil is In-compressible.
  • One dimensional flow.
  • Darcy law is valid.
  • Strain is small.
  • No Sliding occur.

In other words of Terzaghi’s Bearing Capacity Theory

  • 1. Footing base is rough and is laid at a shallow depth (i.e., D f < B).
  • 2. The shear strength of soil above the base of footing is neglected. The soil above the base is replaced by a uniform surface,  g D f .
  • 3. The load on the footing is vertical and uniformly distributed.
  • 4. Footing is long, i.e., L/B ratio is infinite, where B is width and L is the length of the footing.
  • 5. Shear strength of soil is governed by Mohr–Coulomb equation.


Zones: Zone I is elastic zone, zone II is radial shear zone and zone III is passive zone.


Rankine's Theory of Earth Pressure

    Rankine’s theory (1857) considers the state of stress in a soil mass when the condition of plastic equilibrium has been reached.i.e. when shear failure is on the point of occurring throughout the mass.

Assumptions

  • Soil is Homogeneous and Isotropic and 
  • semi-infinite mass of soil with a horizontal surface
  • Consider Back of the wall is Friction-less or smooth.and vertical.
  • in other word having a vertical boundary formed by a smooth wall surface extending to semi-infinite depth.
  • Back-fill is dry and cohesion-less.
  • Critical Shear surface is Plane.
  • Back-plane is vertical and smooth like no friction.
  • Wall is Infinitely Long.
  • No strain condition occur.
  • Failure type sliding failure.
  • Resultant Force is not parallel to Back-fill Surface.
  • When the horizontal stress becomes equal to the passive pressure the soil is said to be inthe passive Rankine state
  • The Mohr circle representing the state of stress at failure in a two-dimensional element
  • The soil element is in state of plastic equilibrium. i.e in the verge of failure.
  •  The theory satisfies the conditions of a lower bound plasticity solution






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Foundation Quick revise your imp topics for exam  Ultimate bearing capacity: It is the minimum pressure at the base of the foundation soil f...

Foundation

Quick revise your imp topics for exam 



Ultimate bearing capacity: It is the minimum pressure at the base of the foundation soil fails in shear.

Safe bearing capacity: It is the maximum pressure at which soil can carry without shear failure.

Net load intensity: It is the minimum net load at which shear failure of soil can occur.

Allowable bearing capacity: The net intensity of loading which the foundation will carry without undergoing settlement in excess or the permissible value for the structure under consideration but not exceeding net safe bearing capacity is termed as allowable bearing capacity.




Sheet Piles:

Sheet piles are similar to retaining walls which are constructed to retain earth, water or any other filling materials. These walls are thinner in section compared to masonry walls.

Sheet pile walls are generally used for water front structures, i.e. in building wharfs, quays and piers, building diversion dams, such as cofferdams, river bank protection and retaining the sides of cuts made in earth.


Based on the Assumptions, Terzaghi Theory is applicable for shallow foundation because side shear resistance and stressing of soil above the foundation is ignored whereas,

Meyerhoff considered stress zone extended up to G.L. Hence Meyershoff's theory is applicable for deep footing also.


Types of Footing and Settlement


Type of Footing and Soil

Settlement and contact pressure

Rigid footing and sand

Settlement : Uniform

Contact Pressure:  Zero at edges and maximum at center

Rigid footing and Clay

Settlement : Uniform

Contact Pressure:  maximum at edges and minimum at center.

Flexible footing and sand

Settlement:  Maximum at edges and minimum at center.

Contact Pressure:   Uniform

Flexible footing and Clay

Settlement :  Minimum at edges and maximum at center

Contact Pressure:  Uniform




Pile Group


Settlement of a pile group is more than the settlement of a single pile, even when the load is the same. This is because the pressure bulb of the pile group is deeper than that of individual piles, causing the compression of a larger volume of soil by the pile group.

Important Points:

  • Pile group settlement for clayey soil can be computed from the principle of consolidation.
  • Pile group settlement for sandy soil can be computed from the formula below:
  • By Skempton’s Formula
  • By Meyerhof’s Formula for square pile group only
  • Where
  • Sg = group settlement of pile
  • Si = individual pile settlement
  • B = Width of pile group
  • r = number of rows in a pile group

The ultimate bearing capacity of a pile 

  • The ultimate bearing capacity of a pile is the maximum load which it can carry without failure or excessive settlement of the ground. The bearing capacity also depends upon the method of installation.

  • In Analytical method,
  • Qup = Qeb + Qsf
  • Qup = qb × Ab + qs × As
  • Where,
  • Qup = ultimate load on pile
  • Qeb = end bearing capacity
  • Qsf = skin friction
  • qb = End bearing resistance of unit area, Ab = bearing Area
  • qs = skin friction resistance of unit area, As = surface Area
  • For circular footing, ultimate bearing capacity

  • qu = 1.3 CNc + γDfNq + 0.3 γBNγ
  • For square footing, ultimate bearing capacity
  • qu = 1.3 CNc + γDfNq + 0.4 γBNγ



For clay soil

  • Qup = Nc × C × Ab + α c̅ As;
  • qb = Nc × C, qs = α c
  • Where, α = adhesion factor
  • c̅ = Average cohesion over depth of pile

‘Negative skin friction

  • ‘Negative skin friction’ or ‘downward drag’ is a phenomenon which occurs when a soil layer surrounding a portion of the pile settles more than the pile. Such relative motion may occur when the clay stratum undergoes consolidation due to
  • 1. A fill recently placed over the clay stratum.
  • 2. Lowering of the ground water table.
  • 3. Reconsolidation occurring due to disturbance caused by pile driving in sensitive clay stratum, etc.
  • The axial capacity of a pile is a summation of upward reaction due to bearing at the base and net upward skin frictional resistance. As the negative skin friction (acting downward) lowers the net skin resistance, it in turn reduces the axial capacity of piles.
  • Negative skin friction increases gradually as the consolidation of the clay layer proceeds since the effective overburden pressure gradually increases due to dissipation of excess pore pressure. 
According to IS 2911 : Part III 1973, the ratio of bearing resistance for double under- reamed pile to that of single under-reamed pile is 1.5 for sandy and clayey soils including black cotton soils.

Note:-

As per IS 2911: Part III (Some other recommendations)

  • 1. For deep deposits of expansive soils the minimum length of piles, irrespective of any other considerations shall be 3.5 m below the ground level. For recently filled up grounds or other strata or poor bearing, the piles should pass through them and rest in good bearing strata.
  • 2. The diameter of under-reamed piles may vary from 2 to 3 times the stem diameter depending upon the feasibility of construction. For Bored cast in situ under-reamed piles the bulb diameter normally be 2.5 times while for compaction piles it is 2 times.
  • 3. For piles up to 30 cm diameter, spacing of bulbs should not be greater than 1.5 times the diameter of bulb. For piles of diameter greater than 30 cm, spacing can be reduced to 1.25 times the stem diameter.
  • 4. The top most bulb should be at a minimum depth of 2 times the bulb diameter. In expansive soils, it should not be less than 1.75 m below ground level. The minimum clearance below underside of pile cap embedded in ground and the bulb should be a minimum 1.5 times the bulb diameter.
  • 5. Under reamed piles with more than two bulbs are not advisable without ensuring their feasibility in strata needing stabilisation of boreholes by drilling mud. The number of bulbs in case of bored compaction piles should not exceed tow in such strata.



Retaining Wall

  • Retaining wall is a structure that are designed and constructed to withstand lateral pressure of soil or hold back soil materials.
  • The lateral pressure could be also due to earth filling, liquid pressure, sand, and other granular materials behind the retaining wall structure.

The empirical formula for determining the depth (d) of retaining wall is given by:

Where, ka is the active earth pressure coefficient and it is given by:

News Record formula is used to determine the ultimate load carrying capacity (Qup) of a pile embedded in sand.  It is given by:

  {For Drop hammer and Single acting steam hammer}

 {For Double acting steam hammer}

Where,
W = Weight if hammer in KN
FOS is Factor of safety which is generally taken ‘6’ for all type of hammers.
H = Height of fall in cm.
S = penetration of pile per blow in cm.
C = Constant for accounting elastic compression of pile and pile cap.
A = area of piston in m2 and p is steam pressure in kN/m2.

The values of S, C and FOS for different type of hammers are given below in tabulated form:


Single acting Hammer

Double acting Hammer

Drop Hammer

S  = Average value for last 25 blows

S  = Average value for last 25 blows

S  = Average value for last 5 blows

C = 0.25 cm

No defined value but generally taken C = 0.25 cm.

C = 2.5 cm

FOS = 6

FOS = 6

FOS = 6






Local shear failure:

This type of failure is seen in relatively loose sand and soft clay.

Some characteristics of local shear failure are:

  • 1. Failure is not sudden and there is no tilting of footing.
  • 2. Failure surface does not reach the ground surface and slight bulging of soil around the footing is observed
  • 3. Failure surface is not well defined
  • 4. Failure is progressive
  • 5. In load-settlement curve, there is no well-defined peak
  • 6. Failure is characterized by considerable settlement directly beneath the foundation
  • 7. A significant compression of soil below the footing and partial development of plastic equilibrium is observed.
  • 8. Well-defined wedge and slip surfaces only beneath the foundation.
Load-settlement curve:-
Note: In general shear failure, failure plane circular for cohesive soils and log spiral for sand and silts.

Types of shear failure:

General shear failure:

  • It occurs in shallow foundations when placed on dense/stiff soil.
  • At the time of failure, the foundation will get tilted and heaving will occur at the side.
  • Before failure settlement will be small and negligible and the stress zone extends up to ground level. 

​Local shear failure:

  • It occurs in loose sand and soft clays in case of shallow foundation.
  • Before failure large settlement is recorded.
  • The stress zone does not extend up to the ground level hence there may e little or no heaving at the sides.

Punching shear failure:

  • It occurs in deep footing and pile which are placed on loose sand or soft clays.
  • In this failure soil below the foundation gets cut off from adjacent soil by shearing and large settlement is recorded in the small-time period.
  • The adjacent soil mass remains unstressed.

Foundtion Condition and Types of Failure


Foundation conditionTypes of shear failure
Footings on the surface or at shallow depths in very dense sandGeneral shear failure
Footing on saturated and normally consolidated clay under undrained loading

General shear failure

Footings at deeper depth in dense sandPunching shear failure
Footing on the surface or at shallow depths in loose sandPunching shear failure
Footing on very dense sand loaded by transient dynamic loadPunching shear failure
Footings on very dense sand underlain by loose sand or soft clayPunching shear failure
Footing on saturated and normally consolidated clay under drained loadingPunching/Local shear failure




Different IS codes and their use:

IS 456:2000 - Plain and reinforced concrete
IS 1080: 1985 - Design and construction of shallow foundation in soil (other than a raft, ring, and shell)
IS 1904:1986 - Design and construction of foundations in soils: General requirements
IS 2950: 1981 - Design and construction of raft foundation


IS code specification for permissible settlement:

(i) Total Permissible settlement:

  • For isolated footing on clay = 65 mm
  • For isolated footing on sand = 40 mm
  • For raft footing on clay = 65-100 mm
  • For raft footing on sand = 40-65 mm

(ii) Permissible Differential settlement:

  • For isolated footing on clay = 40 mm
  • For isolated footing on sand = 25 mm

(iii) Permissible angular settlement:

  • For high framed structure < 1/500
  • To prevent all type of minor damage < 1/1000

Note: 

For multi-storeyed buildings having isolated foundations on sand, the maximum permissible settlement is 60 mm 
[ For multistorey buildings having isolated foundations take the higher load as compare to single storey buildings having isolated foundations. So that deflection caused by multistorey building having isolated foundation higher than 40 mm (from the safer side)]

 

Foundtion and their Suitability

The different types of foundations and there suitability is specified in below in tabulated form:

Type of Foundation

Suitability

Spread footing foundation

 

This type of foundation can normally be used for three to four-storied buildings on common type of alluvial soils.

Stepped Foundation.

 

This type of foundation is provided on hilly places or in those situations where the ground is sloppy.

Pile Foundations

It is used in the following situations:

  1. When it is not economical to provide spread foundations and hard soil is at a greater depth.
  2. When it is very expensive to provide raft or grillage foundations.
  3. When heavy concentrated loads are to be taken up by the foundations.
  4. When the top soil is of compressible nature.
  5. When there is chances construction of irrigation canals in the near by area.
  6. In case of bridges when the scouring is more in the river bed.
  7. In marshy places.

Raft Foundations

This type of foundation is also recommended in such situations where the bearing capacity of the soil is very poor, the load of the structure is distributed over the whole floor area, or where a structure is subjected to constant shocks or jerks.

Well Foundations

This is generally provided for construction of bridge piers and the foundations are to be carried out in deep sandy soils of soft soils.








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