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Videos de Conceptos Relacionados

Temperature Dependent Deformation01:12

Temperature Dependent Deformation

In a nonhomogeneous rod made up of steel and brass, restrained at both ends and subjected to a temperature change, several steps are involved in calculating the stress and compressive load. Due to the problem's static indeterminacy, one end support is disconnected, allowing the rod to experience the temperature change freely. Next, an unknown force is applied at the free end, triggering deformations in the rod's steel and brass portions. These deformations are then calculated and added together...
Deformation of Member under Multiple Loadings01:11

Deformation of Member under Multiple Loadings

When a rod is made of different materials or has various cross-sections, it must be divided into parts that meet the necessary conditions for determining the deformation. These parts are each characterized by their internal force, cross-sectional area, length, and modulus of elasticity. These parameters are then used to compute the deformation of the entire rod.
In the case of a member with a variable cross-section, the strain is not constant but depends on the position. The deformation of an...
Dynamic Modulus of Elasticity of Concrete01:16

Dynamic Modulus of Elasticity of Concrete

The dynamic modulus of elasticity assesses how a concrete structure deforms under impact or dynamic loads. It is typically higher than the static modulus of elasticity, measured under slow, steady loading conditions.
The sonic test is a common method to determine the dynamic modulus. In this test, a concrete beam, sized either 6 x 6 x 30 inches or 4 x 4 x 20 inches, is clamped at its center. Vibrations are initiated at one end of the beam by an electromagnetic exciter unit powered by a...
Expansion and Contraction in Masonry Walls01:19

Expansion and Contraction in Masonry Walls

Masonry walls are subject to slight expansion and contraction due to variations in temperature and moisture. Thermal movement in masonry is relatively straightforward to measure and plan for. On the other hand, moisture movement poses more of a challenge. New clay masonry units typically absorb water and expand over time under normal environmental conditions. Conversely, new concrete masonry units tend to shrink as they lose the excess moisture acquired during their production process.
To...
Magnetostatic Boundary Conditions01:28

Magnetostatic Boundary Conditions

An electric field suffers a discontinuity at a surface charge. Similarly, a magnetic field is discontinuous at a surface current. The perpendicular component of a magnetic field is continuous across the interface of two magnetic mediums. In contrast, its parallel component, perpendicular to the current, is discontinuous by the amount equal to the product of the vacuum permeability and the surface current. Like the scalar potential in electrostatics, the vector potential is also continuous...
Deformation of a Beam under Transverse Loading01:15

Deformation of a Beam under Transverse Loading

Understanding beam deflection, particularly for indeterminate beams with overhanging segments and multiple concentrated loads, is crucial for ensuring structural integrity and functionality. The process begins with constructing an accurate free-body diagram, which helps identify the forces and moments acting on the beam. This diagram is vital for visualizing how bending moments vary along the beam's length, influencing its curvature.
The insights from the bending moment diagram extend to...

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Video Experimental Relacionado

Updated: Jun 24, 2026

Kinematic History of a Salient-recess Junction Explored through a Combined Approach of Field Data and Analog Sandbox Modeling
06:55

Kinematic History of a Salient-recess Junction Explored through a Combined Approach of Field Data and Analog Sandbox Modeling

Published on: August 5, 2016

Deformación variable en el tiempo en la zona sísmica de Nuevo Madrid.

Eric Calais1, Seth Stein

  • 1Department of Earth and Atmospheric Sciences, Purdue University, West Lafayette, IN 47906, USA.

Science (New York, N.Y.)
|March 17, 2009
PubMed
Resumen

Nuevos datos geodésicos sugieren que la zona sísmica de Nuevo Madrid se deforma demasiado lentamente para los terremotos recientes. Esto implica que las tasas de carga tectónica o las propiedades de las fallas cambian a lo largo de milenios, lo que afecta a las evaluaciones de riesgos sísmicos.

Videos de Experimentos Relacionados

Last Updated: Jun 24, 2026

Kinematic History of a Salient-recess Junction Explored through a Combined Approach of Field Data and Analog Sandbox Modeling
06:55

Kinematic History of a Salient-recess Junction Explored through a Combined Approach of Field Data and Analog Sandbox Modeling

Published on: August 5, 2016

Área de la Ciencia:

  • La geofísica es la geofísica.
  • Sismología Sismología Sismología.
  • La geodesia es una técnica de geodesia.

Sus antecedentes:

  • La zona sísmica de Nueva Madrid (NMSZ) es un importante peligro de terremotos intraplacas en el centro de los Estados Unidos.
  • Comprender la deformación y el potencial sísmico de la NMSZ es crucial para la evaluación del peligro.

Objetivo del estudio:

  • Evaluar las tasas actuales de deformación tectónica en la zona sísmica de Nuevo Madrid utilizando mediciones geodésicas.
  • Evaluar si la deformación observada puede explicar la ocurrencia de grandes terremotos en los últimos 5000 años.

Principales métodos:

  • Análisis de nuevos datos geodésicos (por ejemplo, GPS, InSAR) en toda la NMSZ.
  • Comparación de las tasas de deformación medidas con las requeridas para grandes terremotos prehistóricos.

Principales resultados:

  • Las mediciones geodésicas indican una deformación de corriente muy lenta o insignificante en la NMSZ.
  • La lenta deformación observada no puede explicar la frecuencia y la magnitud de los grandes terremotos pasados (los últimos 5000 años).

Conclusiones:

  • Las tasas actuales de carga tectónica o las propiedades de las fallas en la NMSZ pueden variar significativamente en escalas de tiempo milenarias.
  • Esta variabilidad desafía los modelos tradicionales de riesgo sísmico basados en supuestos de estado estacionario.