Elementary applied mechanics, by T. Alexander (and A.W. Thomson). |
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Resultat 1-5 av 9
Side
... sloping plane being " trace " of spheroid - Other cases , as when wall runs up steepest declivity , and generally , when wall runs up at any slope less than that of greatest de- clivity , Ex . ( No. 88 ) . 95 103 106 112 ELEMENTARY ...
... sloping plane being " trace " of spheroid - Other cases , as when wall runs up steepest declivity , and generally , when wall runs up at any slope less than that of greatest de- clivity , Ex . ( No. 88 ) . 95 103 106 112 ELEMENTARY ...
Side 106
... sloping at the angle y , consider a small parallelopiped in the layer of depth D having vertical faces . At this depth , D , the intensity in lbs . per sq . ft . of the vertical pressure due to the weight of earth above , on a ...
... sloping at the angle y , consider a small parallelopiped in the layer of depth D having vertical faces . At this depth , D , the intensity in lbs . per sq . ft . of the vertical pressure due to the weight of earth above , on a ...
Side 107
... sloping layer , so that every point in that layer is in the same state of strain , and r ' is transmitted along the layer to act on the wall . To find out the ratio of the pair of conjugate stresses rand ' whose common obliquity is y ...
... sloping layer , so that every point in that layer is in the same state of strain , and r ' is transmitted along the layer to act on the wall . To find out the ratio of the pair of conjugate stresses rand ' whose common obliquity is y ...
Side 111
... sloping surface , WD cos y , = 130 × 9 × cos 20 ° 1099 lbs . per sq . in . is the conjugate thrust whose direction is parallel to sloping surface when earth is just about to spread . p cos y γ √ ( cos2y - cos2p ) cos y + √ ( cos2y ...
... sloping surface , WD cos y , = 130 × 9 × cos 20 ° 1099 lbs . per sq . in . is the conjugate thrust whose direction is parallel to sloping surface when earth is just about to spread . p cos y γ √ ( cos2y - cos2p ) cos y + √ ( cos2y ...
Side 114
... ( sloping layer ) plane upon which r acts and on the same side . Also cos 20 = 2r cos y - P - q . Case ( a ) page 85 . p - q Since the earth is upon the point of spreading , the princi- pal stress normal to the paper will be the least ...
... ( sloping layer ) plane upon which r acts and on the same side . Also cos 20 = 2r cos y - P - q . Case ( a ) page 85 . p - q Since the earth is upon the point of spreading , the princi- pal stress normal to the paper will be the least ...
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amount of resilience amount of stress angle of repose augmentation axis Cambridge chain component stresses cos² Crown 8vo dead load direction and intensity earth Edition ellipse elongation equal Equating equilibrium Eton College Extra fcap feet long find the intensity find the stress ft.-lbs greater greatest principal stress Hence Hooke's law horizontal inch in section instant internal stress J. P. MAHAFFY LATIN layer length live load modulus of elasticity normal component OM² Owens College pair of rectangular parallelopiped plane BB plane inclined plane of greatest planes of principal position of cc principal stresses Professor proof strain proof stress rectangular planes right angles School shearing shearing stress sin² sloping solid square inch stress on cc stretched surface tangential component tangential stress thrust total stress velocity wall weight
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