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Surface forces
Caused by direct contact of one body with the surface of another.
Body force
Developed when one body exerts a force on another without direct physical contact.
Prismatic
Cross sections are the same throughout its length.
Homogeneous material
Has the same properties throughout its volume.
Isotropic material
Has the same properties in all directions.
Load Factors
Reflect the probability of total loading occurrence.
Yielding
Occurs when stress exceeds the elastic limit, causing permanent deformation.
Yield stress
Stress causing yielding and plastic deformation.
Strain Hardening
Material can support increased load after yielding.
Ductile Materials
Can undergo large strains before fracturing.
Brittle Materials
Exhibit little or no yielding before failure.
Strain energy
Work stored in a material due to external load.
Modulus of Resilience
Strain-energy density at the proportional limit.
Modulus of Toughness
Represents the area under the stress-strain diagram.
Ductility Factor
Ratio of toughness to resilience modulus.
Creep
Continuous deformation under sustained load.
Fatigue
Breakdown due to repeated stress or strain cycles.
Plasticity
Material deforms permanently above elastic limit.
Residual Stress
Stress remaining after plastic deformation.
Beams
Slender members supporting perpendicular loads.
Dilatation
Change in volume per unit volume.
Resonance
Building period coincides with earthquake period.
Torsional Shear Stress
Occurs when mass center differs from rigidity center.
Ground Displacement
Measured by a seismometer.
Rigidity of a Structure
Reciprocal of deflection.
Story
Space between two adjacent floors.
Diaphragms
Transfer lateral forces to vertical elements.
Shear wall
Resists lateral forces on its plane.
Center of Gravity
Point with no torque from gravitational force.
Center of Rigidity
Point where lateral force resistance acts.
Center of Mass
Point where seismic force acts.
Eccentricity
Distance between rigidity and mass centers.
Design seismic base shear
Total lateral force.
Flexibility of a structure
Inverse of stiffness.
Story drift
Displacement between levels.
Story displacement
Lateral displacement of a story.
Damping
Rate of absorbing natural vibration.
Seismometer
Measures peak ground acceleration.
Magnetometer
Measures rock strain under pressure.
Focus (Hypocenter)
Origin of earthquake waves.
Epicenter
Point above the earthquake focus.
Story drift ratio
Drift divided by story height.
Intensity
Measure of earthquake shaking strength.
Magnitude
Measure of energy released in an earthquake.
Liquefaction
Soil loses shear strength during shaking.
Earthquake
Violent ground movement due to energy release.
Shear Drift
Building sideways deflection from lateral loads.
Chord Drift
Vertical load sideways deflection.
Resultant
Force determining equilibrium or motion.
Hooke’s Law
Principle for axially loaded material deformation.