Factors of safety represent reserve capacity
which a foundation or structure has against collapse for a given set of loads
and design conditions. Uncertain design parameters and loads, require a
higher factor of safety than required when the design parameters are well
known. For most hydraulic structures, designers should have a high level of
confidence in the soil and pile parameters and the analysis. Therefore,
uncertainty in the analysis and design parameters should be minimized rather
than requiring a high factor of safety. For less significant structures, it
is permissible to use larger factors of safety if it is not economical to
reduce the uncertainty in the analysis and design by performing additional
studies, testing, etc. Also, factors of safety must be selected to assure
satisfactory performance for service conditions. Failure of critical components
to perform as expected can be as detrimental as an actual collapse.
Therefore, it is imperative that in choosing a design approach, the designer
consider the functional significance of the project, the degree of uncertainty
in the design parameters and the analytical approach, and the probability of failure due to both collapse and functional inadequacy.
Foundation, Concrete and Earthquake Engineering
1964 Alaska Earthquake: Lateral Spreads Damaged 200 Bridges
During the 1964 Alaska earthquake, more than 200 bridges were damaged or destroyed by spreading of floodplain deposits toward river channels. The spreading compressed the superstructures, buckled decks, thrust stringers over abutments, and shifted and tilled abutments and piers.
This news are known to all but do we know what is lateral spreading or what is the relation between earthquake and lateral spreading. Let us try to find out the answer of above questions.
In Alaska Earthquake March 27, 1964, Twentymile River Bridge fell into
the river, and some of the wood piles were driven through the reinforced
concrete deck.
|
Lateral spreads involve lateral displacement of large, surficial blocks of soil as a result of liquefaction of a subsurface layer. Displacement occurs in response to combination of gravitational forces and inertial forces generated by an earthquake. Lateral spreads generally develop on gentle slopes (most commonly less than 3 degrees) and move toward a free face such as an incised river channel. Horizontal displacements commonly range up to several meters, but where slopes are particularly favorable and ground shaking durations are long, displacements may range up to several tens of meters. The displaced ground usually breaks up internally, causing fissures, scarps, horsts, and grabens to form on the failure surface.
Failure of Million Dollar Bridge on the Copper River Highway in 1964 Alaska
Earthquake
|
LIQUEFACTION AND GROUND FAILURE
In liquefaction process soil deposits behave as a viscous liquid rather than as a solid temporarily losing strength. Cohesionless soil deposits primarily sands and silts under seismic waves, primarily shear waves that pass through saturated granular layers, distort the granular structure, and cause loosely packed groups of particles to collapse. Disruptions to the particulate structure generated by these collapses cause transfer of load from grain-to-grain contacts in the soil to the interstitial pore water. This transfer of load increases pressure, in the pore water, causing drainage to occur. If drainage is restricted, a transient build up of pore-water pressure will occur. If the pore-water pressure rises to a level approaching the overburden pressure grain-to-grain contact stresses approach zero and the granular layer temporarily behaves as a viscous liquid rather than as a solid and liquefaction has occurred. In the liquefied condition, soil deformation: may occur with little shear resistance. Deformations large enough to cause damage to constructed works (usually more than 0.1 m) are called ground failure.
Looseness of the soil, the packing arrangement of soil grains, the amount of cementing between particles, and the amount of drainage restriction are factors that control the degree of liquefaction.
The amount of soil deformation following liquefaction depends on the looseness of the material, the thickness and areal extent of the liquefied layer, the ground slope, and the distribution of loads applied by buildings and other structures on the ground surface.
Determination Difficulties of Cyclic Strains of Soil During Earthquake
Estimation of the seismic response of shallow foundations during a strong earthquake has been proven a difficult task throughout the years. The main cause of this difficulty arises from the fact that soil behaves in a highly non-linear manner when subjected to large cyclic strains.
It can deform substantially and, when saturated, can develop high pore pressures and finally liquefy. Liquefaction consequently leads to severe loss of bearing capacity, which damages seriously the superstructure. Extensive damage to shallow foundations due to liquefaction has been reported in numerous cases in the past, from Niigata (1964) earthquake to the more recent 1999 M 7.4 Kocaeli earthquake.
It can deform substantially and, when saturated, can develop high pore pressures and finally liquefy. Liquefaction consequently leads to severe loss of bearing capacity, which damages seriously the superstructure. Extensive damage to shallow foundations due to liquefaction has been reported in numerous cases in the past, from Niigata (1964) earthquake to the more recent 1999 M 7.4 Kocaeli earthquake.
| Liquefaction Impact |
Kaptai Dam of Bangladesh
Kaptai dam is the one and only dam of Bangladesh that is used to generate hydro-electric power. This dam was constructed across Karnaphuli River at Kaptai in Rangamati district, 65 km upstream of Chittagong. It is an earthfill embankment dam which reservoir is called Kaptai Lake. The water storage capacity of the Kaptai dam is 11000 km2. The construction of the dam was started in 1957 and was completed in 1962.
Under the guidance of then Chief Engineer (Irrigation) Khwaja Azimuddin, the construction site was chosen at present location of the dam in 1951. The International Engineering Co. Inc. (IECO) was engaged for a study on the project. Utah International Inc. was selected as construction contractor.
| The 16 gated (each 12.2 m X 11.3 m size) spillway of Kaptai Dam have discharge capacity of 625000 cusec. |
| Kaptai Dam with spillway and Power Plant |
Kaptai dam can reduce the downstream flood peak in the Karnafuli river by 50% by storing water in the reservoir. Kaptai dam is 670.56m long and 45.7m high. The width at the foundation level is 45.7m and at crest level 7.6m. The crest level is 36m above mean sea level (MSL).
India Have Got Third Position in Dam Building
Before independence i.e. 1947, there were fewer than 300 large dams in India and by the year 2000 the number had grown to over 4000, more than half of them built between 1971 and 1989. India is declared to be the third in the world in dam building, after US and China.
Dams in India have been built across many perennial rivers. These dams are a part of the several multi-purpose projects launched by India to serve a variety of needs. In a multi-purpose project, a river forms a unit and a river valley is developed, by exploiting all the resources of the river.
| Durgapur Barrage across the Damodar River at Durgapur in Bardhaman district in the Indian state of West Bengal. |
Dams are built to harness the river water so that it can be utilised according to needs. A multipurpose project is launched often for storing water for irrigation purposes, generating hydro-electricity by utilising the water stored by the dams, preventing floods and facilitating afforestation in the catchment areas of the reservoirs. However, the dams also provide drinking water, using the canals for navigation in some areas and also facilitating pisciculture and recreational activities. The main multipurpose projects constituting the major Indian dams are the Hirakud Project in Orissa, the Bhakra Nangal inPunjab, the Damodar Valley Project in Bihar and Bengal, the Tungabhadra Project in Andhra Pradesh and Karnataka, the Rihand Project in Uttar Pradesh.
| Hirakud Dam across the Mahanadi River, about 15 km from Sambalpur in the state of Orissa in India. |
Some of the Indian dams were built primarily for flood control, water supply, and hydroelectric power generation, the primary purpose of most Indian dams (96 percent) remains irrigation. In fact, large dam construction in India has been the main form of investment in irrigation undertaken by the Indian government. But, starting in the 1980s, public investment in large dams in India has been the subject of a sustained controversy that was epitomized by the Sardar Sarovar Project, based on the balance between the social, environmental, and economic costs of dams and their benefits.
| Bhakra Nangal Dam is situated across the river Sutlej that falls under the region of Bilaspur in Himachal Pradesh |
Tourist Spot near Dams is very much popular and good sources for attracting tourists. There are all the states in India where dams have been established but Karnataka is very rich in having most of dams and Reservoirs. Dams in Karnataka is very popular serving the purpose of people of Karnataka and Bangalore. Karnataka is much enriched in terms Dams in South India.
1. Almatti Dam
|
2. Gajanur Dam
|
3. Gundal Reservoir
|
4. Harangi Dam
|
5. Hidkal Dam
|
6. Kadra Dam
|
7. Kanakanala Dam
|
8. Kanva reservoir
|
9. Kodasalli Dam
|
10. Krishna Raja Sagara Dam
|
11. Lakkavalli Dam
|
12. Linganamakki Dam
|
13. Marconahally Dam
|
14. Mari Kanive Dam
|
15. Narihalla Dam
|
16. Nugu Reservoir
|
17. Sathanur Dam
|
18. Supa Dam
|
19. Suvarnavathi Reservoir
|
20. Thippagondanahalli Reservoir
|
21. Tunga Anicut Dam
|
22. Tungabhadra Dam
|
23. Vani Vilas Sagar Reservoir
|
Subscribe to:
Posts (Atom)