Results 261 to 270 of about 22,008,466 (312)
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1991
In the previous chapter, we have derived the uncoupled differential equations (2.18) and (2.24) for the small deflection theory of plates. Through the first equation the membrane stress distribution for a plane stress problem can be obtained. In this chapter, a boundary integral formulation of this problem, based on the Rayleigh-Green theorem, will be ...
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In the previous chapter, we have derived the uncoupled differential equations (2.18) and (2.24) for the small deflection theory of plates. Through the first equation the membrane stress distribution for a plane stress problem can be obtained. In this chapter, a boundary integral formulation of this problem, based on the Rayleigh-Green theorem, will be ...
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1999
In this section we derive in the general form linearised relationships relevant to the description of the states of stress and strain, equations of motion and boundary conditions within the scope of the finite (large) initial deformations theory. After that a consistent transition to several variants of the small initial deformations theory will be ...
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In this section we derive in the general form linearised relationships relevant to the description of the states of stress and strain, equations of motion and boundary conditions within the scope of the finite (large) initial deformations theory. After that a consistent transition to several variants of the small initial deformations theory will be ...
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1989
The undisturbed in situ rock before an excavation is already under a certain stress. This stress-state is due to a variety of causes: gravity, stresses due to tectonic motions, the strata orientation, the creep and relaxation produced during geological periods, possible local unloading due to a relatively fast erosion, thermal contractions, etc.
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The undisturbed in situ rock before an excavation is already under a certain stress. This stress-state is due to a variety of causes: gravity, stresses due to tectonic motions, the strata orientation, the creep and relaxation produced during geological periods, possible local unloading due to a relatively fast erosion, thermal contractions, etc.
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The state op stress in a thick plate
Journal of Applied Mathematics and Mechanics, 1967Vorovich, I. I., Malkina, O. S.
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Epigenetics: Future Prospective in Human Disorders and Therapeutics
Medical Epigenetics, 2021Shriram N Rajpathak
exaly
2004
In applied mechanics and engineering, materials and structures are generally regarded as continua. This permits us to describe the behaviour and consequences of materials and structures by means of continuous functions. A material is a point (element), and a structure is a body.
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In applied mechanics and engineering, materials and structures are generally regarded as continua. This permits us to describe the behaviour and consequences of materials and structures by means of continuous functions. A material is a point (element), and a structure is a body.
openaire +1 more source
Disparities in Liver Cancer Occurrence in the United States by Race/Ethnicity and State
Ca-A Cancer Journal for Clinicians, 2017Rebecca L. Siegel +2 more
exaly
Method for detecting stressed state and stress detection apparatus
2021NISHIDA KOHJI +3 more
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A New Method of Predicting US and State-Level Cancer Mortality Counts for the Current Calendar Year
Ca-A Cancer Journal for Clinicians, 2004Ahmedin Jemal +2 more
exaly