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Soil Dynamics

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Critical State Soil Mechanics

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Critical state soil mechanics is a framework used to describe the behavior of soil under shearing conditions. It posits that soil behavior can be predicted based on critical state lines in stress space. Factors are void ratio, soil composition, and confining pressure.

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Resilient Modulus

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Resilient modulus (MRM_R) is a measure of soil's elastic response under repeated loading, such as traffic loads. It's important for pavement design and depends on factors like soil type, moisture content, and the magnitude of the applied load.

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Dynamic Soil Properties

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Dynamic soil properties include parameters such as shear modulus and damping ratio, which define the soil's response to dynamic loading. Influencing factors are soil type, void ratio, effective stress, and strain amplitude.

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Seismic Site Response Analysis

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Seismic site response analysis is the evaluation of soil response to earthquake ground motion. The analysis can predict amplification of seismic waves and site-specific ground motion. Influencing factors include soil stratigraphy, bedrock depth, and seismic wave characteristics.

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Cyclic Stress Ratio (CSR)

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CSR=τcyclicσvertical\text{CSR} = \frac{\tau_{cyclic}}{\sigma'_{vertical}}
, where τcyclic\tau_{cyclic} is cyclic shear stress and σvertical\sigma'_{vertical} is effective vertical stress. CSR is used to evaluate the potential for soil liquefaction during earthquakes. Factors affecting CSR include earthquake magnitude, depth of water table, and soil density.

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Atterberg Limits

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Atterberg limits are a basic measure of the critical water contents of fine-grained soils. These limits define the boundaries between different soil states: liquid, plastic, and solid. The limits are influenced by mineral composition, temperature, and organic content.

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Liquefaction Potential

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Liquefaction potential refers to the likelihood that a saturated soil will lose strength and stiffness under an applied stress, often due to earthquake shaking, causing it to behave like a liquid. Factors affecting liquefaction include soil composition, level of saturation, confining pressure, and seismic intensity.

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Soil Amplification

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Soil amplification is the increase in seismic wave amplitude as waves move from bedrock to softer soil layers. Factors that affect it include soil type, depth to bedrock, and the frequency of the incoming seismic waves.

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Shear Wave Velocity (Vs)

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Shear wave velocity is the speed at which a shear wave travels through a medium, and it's used to gauge the stiffness of that medium, in this case, soil. Higher Vs indicates stiffer soil. It's affected by soil density, elasticity, and confining pressure.

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Pore Water Pressure

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Pore water pressure refers to the pressure of groundwater held within a soil void. An increase in pore water pressure can lead to a decrease in soil strength. Factors affecting it include soil permeability, drainage conditions, and external loading.

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