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Geological factors influencing retaining wall performance
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Retaining walls failures by earthquakes fall into two main categories. The first failure mode is by the wall itself sliding away from the back fill. The second failure consists of more than one action, or combined action, by sliding and rocking displacements or during an earthquake. During an earthquake, soil is displaced vertically and laterally due to a sudden release of energy, the cause of earthquakes. In area where seismic activity is readily occurring, the retaining wall must account for these displacements, in addition with the typical requirements. These requirements consist of a factory of safety against failure in bearing, sliding, and overturning.
In geologic terms, secondary effects from earthquakes refer shaking that occur from
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The Ji-Ji (or Chi- Chi) Earthquake was an earthquake that occurred along the Chelungpu Fault in central Taiwan. The earthquake recorded a magnitude of 7.3 on the Richter scale which classifies the event as a major earthquake. The earthquake caused 2,415 casualties and injured over 11,000 people. It also caused significant damage to the area amounting to over 10 billion U.S. dollars. The aftermath included the destruction of major building, schools, and even affects soil reinforced soils. Among the damages caused by the earthquakes were many reinforced retaining walls. Everything was destroyed. A group of civil engineers took advantage if this disaster to investigate the geosynethic retaining walls used in Taiwan. The investigation included a total of 6 retaining structures, four modular-block reinforced soil retaining walls two rein enforced slopes that were relatively close to the fault like and received great damage (Linga. and Leshchinsky …show more content…
This wall failed in a different, more conventional way. Two cracks were formed at the crest of the wall, 0.5 meters from the block and two meters form the blocks. This caused the blocks to move roughly 30 centimeters from the backfill. This caused a failure in the bottom corner of the wall and eventually backfill went through the wall. Geogrids and pins were used to connect the modular blocks. The first crack corresponds to length of the geo soil (Linga et al. 2007).
After reviewing the earthquake that occurred in Taiwan and a few of the failing retaining walls, a few questions can be asked about the failure modes. Were there any repetitions in failure modes? Was each retaining wall designed to withstand a seismic event? Finally, did the geosyenthic or pin connections cause any failures? If so, could a different connection or type of synthetic be used instead? From these questions, the engineers at Stratton Oakmont are working on new retaining walls to withstand earthquakes of all
This rock type could prove dangerous, being soft and with little solidness in its structure. Therefore placing the protection over the rock cliffs was a very well thought and planned engineering
Earthquakes play a major role into understanding the composition and materials that exist within the Earth (Merali and Skinner, 2009, p.252). Earthquakes are the main source of insight into the inner workings of the earth, due to the nature of the seismic waves they produce. P and S waves are reflected and refracted at different boundaries within the earth, and this enables seismologists to make inferences about the internal composition and structural of planet Earth. (Merali and Skinner, 2009, p.252).
Tsunamis caused by the Earthquake leads to flooding along the coastal environment. This damages any homes. Flooding caused new lakes or sag ponds on the land. Increasing groundwater flow from springs and displacing stream channel. ("Flood Consequences")
An earthquake felt throughout the Midwest on June 18 was a shaky reminder that earthquakes can occur anywhere.
Massive Mega-Quakes happen at regular intervals in the Pacific Northwest. There have been mega-quakes in the beginning of time. In Japan, a mega-quake send a 600-foot wave of water.
At 5:12 a.m. on April 18th, 1906, the California city of San Francisco was awoken by a 7.8 magnitude earthquake. Chaos erupted with the earthquake leading to fire break outs throughout San Francisco (Cameron and Gordon. Pgs 69-73).The earthquake and the resulting fires caused destruction to majority of the city with buildings crumbling and igniting into flames. Many people died along with thousands and thousands of people being left homeless. This devastating earthquake left the city and United States in a financial crisis. Although the 1906 earthquake was one of the worst natural disasters in U.S. history, the city of San Francisco was able to overcome these substantial physical, social and economic impacts it had.
Before the San Francisco earthquake, not much was understood about earthquakes like how and where they occurred, or the destruction that could occur and the theory of plate tectonics was over a half-century away. Now scientists can answer the following questions: where a strong quake will likely happen, how probable it is, how intense it will be, how will the infrastructure fare, where to avoid building critical structures, and how do we design and build earthquake resistant structures. Scientists that flourished after this earthquake were Lawson, Reid and Gilbert but the most significant discovery is credited to Henry Fielding Reid, Professor of Geology at John Hopkins University. Most of the building structures that were destroyed or damaged were made out of wood. About 24,500 buildings out of the 28,000 buildings were built with wood structures and the other 3,500 buildings structures were made out of brick. With almost 90 percent of the structures being wood, fires and gas caused most of the
The San Francisco earthquake that took place in 1906 is fairly well-known because of its damage and intensity that would affect many lives. The online exhibit of The 1906 San Francisco Earthquake and Fire shows how much was lost during this natural disaster, and how the city was before. Many would wonder what is the purpose of documenting how it was before, and after the earthquake, but the fact that no one was expecting one so big impacted countless lives. Also, at the time San Francisco was becoming the most popular city, therefore it would appear in the headlines how a well-known place that most people loved would become damaged (The Bancroft Library, 2006). Overall, this virtual field trip shows the cause and effect of the earthquake that would change San Francisco in numerous ways.
On February 1, 2003, the Space Shuttle Columbia was lost due to structural failure in the left wing. On take-off, it was reported that a piece of foam insulation surrounding the shuttle fleet's 15-story external fuel tanks fell off of Columbia's tank and struck the shuttle's left wing. Extremely hot gas entered the front of Columbia's left wing just 16 seconds after the orbiter penetrated the hottest part of Earth's atmosphere on re-entry. The shuttle was equipped with hundreds of temperature sensors positioned at strategic locations. The salvaged flight recorded revealed that temperatures started to rise in the left wing leading edge a full minute before any trouble on the shuttle was noted. With a damaged left wing, Columbia started to drag left. The ships' flight control computers fought a losing battle trying to keep Columbia's nose pointed forward.
benchmark for the future, and integrated investigation into the effects of earthquakes in the U.S.
A safe and stable wall(pit) is of importance and vital to all aspects of mining operations especially blasting. Ensuring a stable pit wall requires a fair knowledge of geology, ground water conditions, slope and blast design. The strength of the rock mass under tensile, shear and compressional loading will determine the overall stability of a pit wall.
... although we may never be able to understand exactly what soil failures can occur when a natural disasters take place, as time goes on and testing instruments and materials advance we will hopefully have a better understanding of what we can do to avoid soil failures and come up with a better and more sufficient method of improving the soils structure and strength permanently. While researching the information for this report I feel I have a much better understanding for construction geo-technics and foundations especially regarding the deformation, liquefaction and pile information related to this specific event. I hope to carry the information I have learned from this event into the construction field and apply them towards an authentic project that’s taking place and know that the information, regarding soils, I have given input on will be precise and accurate.
Earthquakes are vibrations felt at the surface of the earth which are caused by disturbances of the energy in the earth's interior. These vibrations are known as seismic waves. (Skinner Robinson McVerry 1) There are different type sof seisimc waves such as Primary (P) waves, whcih travel the fastest, Secondary (S) waves which cause the earth to vibrate vertically, Surface (L) waves. P and S waves are "affected by changes in the density and the rigidity of the materials through which they pass." (Columbia Encyclopedia) Earthquakes vary in their intensity and duration. Often times they are strong enough to cause massive destriction. Tall buildings often suffer as a result of these natural disasters. In recent years this has become a larger and larger threat with both the number of large buildings, and their number of occupants increasing. In an effort to try to minimize the damage caused by earthquakes many some engineers focus primarily on designing and constructing earthquake resistant buildings. Earthquake engineers have gathered much of their information from analyzing past earthquakes, and learning which buildings can and can't withstand the tremors. The goals of these engineers is to design buildings that can withstand moderate earthquakes and obtain minimal damage, and that the buildings will not collapse lowering the probability of human deaths.
Earthquakes belong to the class of most disastrous natural hazards. They result in unexpected and tremendous earth movements. These movements results from dissemination of an enormous amount of intense energy in form of seismic waves which are detected by use of seismograms. The impact of earthquakes leaves behind several landmarks including: destruction of property, extensive disruption of services like sewer and water lines, loss of life, and causes instability in both economic and social components of the affected nation (Webcache 2).
Taher, R. (2011). General recommendations for improved building practices in earthquake and hurricane prone areas. San Francisco, CA: Architecture for Humanity Retrieved from