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美國巖土工程Research Proposal范文:Effect of clay property on landsli

時間:2019-04-10 14:41來源:未知 作者:anne 點擊:
導讀:本文是一篇關于粘土、導致、滑坡、擋土墻倒塌、基建失敗、等問題的介紹性Research Proposal。由粘土性質變化導致,比如由于水、溫度、受力因素,導致了一些自然災害和者事故。 目錄

導讀:本文是一篇關于粘土、導致、滑坡、擋土墻倒塌、基建失敗、等問題的介紹性Research Proposal。 由粘土性質變化導致,比如由于水、溫度、受力因素,導致了一些自然災害和者事故。

目錄
1.背景2
1.1滑坡分類2
1.2山體滑坡的原因5
2.粘土性質的影響6
2.1粘土中水含量的影響6
2.2施加力對粘土的影響8
3.擬議計劃9
參考10
1. Background 2
1.1 Classification of landslides 2
1.2 Causes of landslides 5
2. Effect of clay property 6
2.1 Effect of water content within clay 6
2.2 Effect of applied force on clay 8
3. Proposed plan 9
Reference 10
圖表
圖1泥石流示意圖2
圖2地球流動示意圖2
圖3碎片3的示意圖
圖4 sturzstrom 3的示意圖
圖5淺層滑坡的示意圖4
圖6深層滑坡的示意圖4
圖7滑坡頻率與年平均降雨量的關系7
圖8滑坡頻率與坡度角的關系8
圖9坡度分布與巖石類型9Table of Contents
Table of Figures
Figure 1 Schematic diagram for debris flow 2
Figure 2 Schematic diagram for earthflows 2
Figure 3 Schematic diagram for debris slide 3
Figure 4 Schematic diagram for sturzstrom 3
Figure 5 Schematic diagram for shallow landslide 4
Figure 6 Schematic diagram for deep-seated landslide 4
Figure 7 Frequency of landslide vs. mean annual rainfall 7
Figure 8 Landslide frequency vs. slope angle 8
Figure 9 Slope distribution vs. rock type 9
Effect of clay property on landslides粘土性質對滑坡的影響
Background背景
1.1 Classification of landslides滑坡分類
滑坡或山體滑坡被定義為地質時代的一種現象,包括各種地面運動,如淺層泥石流,斜坡深度破壞和落石等。山體滑坡在陸上,近海和沿海等地區很常見。重力是滑坡的主要原因,其他因素也影響原始坡度的穩定性。由于前置條件因素而形成的特定條件使得斜坡或區域容易發生故障,并且由于特定條件而觸發了實際滑坡的釋放。有不同類型的滑坡,深層滑坡,淺層滑坡,sturzstrom,碎片滑坡,地球流動和泥石流。
Landslide or landslip is defined as a phenomenon in geological era including various ground movements such as shallow debris flows, deep failure of slopes and rockfalls etc. Landslides are common in areas like onshore, offshore and coastal. Gravity is the main cause of landslide though, other contributing factors also affect the stability of original slope. Specific conditions built up because of pre-conditional factors make the slope or area prone to failure easily, and the releasing of actual landslide is triggered because of specific condition.There are different types of landslides, deep-seated landslide, shallow landslide, sturzstrom, debris landslide, earthflows and debris flow. 
當斜坡材料被水飽和時,泥漿流被釋放,汽車,房屋和樹木可能被所產生的泥漿吸收,因此支流和橋梁可能被引起的洪水阻擋。碎片很容易被誤認為是暴洪,而實際上卻完全不同。阿爾卑斯地區的基礎設施和建筑物受到嚴重破壞,因為泥濘的泥石流也造成了人類的生命。泥石流有時是開始與坡相關的因素造成的,并且可能阻塞河床,這可能會暫時造成水堵。與此同時,由于蓄水的失敗也產生了多米諾骨牌效應,并且流量的增加也體現了流量。固液混合物的密度可達2噸/立方米,速度可達14米/秒(Arattano和Franzi,2003年)。第一次嚴重的道路中斷是由于泥石流造成的,因為泥土碎片的影響被低估了。
Debris flow is released when the slope material is saturated with water, the cars, houses, and trees are possibly picked up by the resulting slurry, therefore the tributaries and bridges are possibly blocked by the caused flood. Debris is easily mistaken as flash flood, while they are totally different actually. Severe damage to infrastructure and structures in alpine areas are caused because of the muddy-debris flows, the human lives are claimed also. Debris flow is sometimes the result of starting slope-related factors, and possibly dam the stream beds, which may cause the water blockage temporarily. At the same time, domino effect is created also because of the failure of impoundments, and the increasing of flowing mass’ volume also attributes. Densities up to 2 tons/m3, velocities up to 14 m/s can be reached for the solid-liquid mixture (Arattano and Franzi, 2003). First severe interruption of road is caused for debris flow, and damage happens also because of underestimation of the influence of mud-debris.
Figure 1 Schematic diagram for debris flow
Earthflows move at speed ranges from slow to fast, which consist of viscous flow of fine-grained and saturated materials. Speed range from 0.17 to 20 km/h is typical. Earthflows are similar with the mudflow, while the speed is slower compared with mudflow, and more solid material is contained. They are more different from fluid flows, because of their higher speed. Pyroclastic, fine-grained, silt and fine sand, and clay are all susceptible to earthflows. The water content in the earthflow decides its velocity and higher water content causes higher velocity.
Figure 2Schematic diagram for earthflows
For debris landslide, it is chaotic movement of debris, soil and rocks mixed with ice and/or water. The incoherent mixture of smaller vegetation, broken timber and other debris caused by the saturation of thickly vegetated slopes triggers the debris landslide easily. It is different with debris avalanches, because it is slowerasless water content exists in debris landslide. Debris avalanches cause steep coastal cliffs easily, which happen normally on the oceans island volcanos’ submerged flanks, such as the Cape Verde Islands and Hawaiian Islands. Big rocks initiate the debris landslides firstly, which is the top part of slide and gradually break apart when they slide to the bottom. Thus the debris slides are slower than the debris avalanche, as latter has higher water content, and steeper slope. 
Figure 3 Schematic diagram for debris slide
Sturzstrom is a kind of rare landslide, which is not easy to be understood with long run-out. These slides are usually flowing slowly over low angle terrain, even slightly uphill. 
Figure 4 Schematic diagram for sturzstrom
Shallow landslide is defined as slide with superficial sliding surface from few decimeters to meters. Failures of road out-slopes, debris flow and debris slides are usually included in shallow landslide. The areas that have slopes with low permeable bottom soils under the high permeable soils are where the shallow landslides usually happen. The high permeable soils create high water pressure in the upper soils, as the bottom and low permeable soils trap the water in the shallower. Because of the filled water in the top soils, the slopes are unstable which are prone to slide over the bottom soils which are low permeable. 
Figure 5 Schematic diagram for shallow landslide
As for the deep-seated landslide, the sliding surface is located deeply below the depths of the roots of the trees, which are normally greater than ten meters. Weathered rocks, deep regolith are involved in the deep-seated landslides. This kind of landslide happens usually in the region which is tectonic active like Zagros Mountain in Iran. They move several meters per year, which are very slow. 
Figure 6 Schematic diagram for deep-seated landslide
1.2 Causes of landslides


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