Pressure, Resistance, and Stability of Earth - American Society of Civil Engineers: Transactions, Paper No. 1174, - Volume LXX, December 1910 by J. C. Meem
page 5 of 92 (05%)
page 5 of 92 (05%)
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Referring again to the area, _A N_{1} V J N A_, Fig. 2, it is probable that, while self-sustaining, some at least of the lower portion must derive its initial support from the "centering" below, and the writer has made the arbitrary assumption that the lower half of it is carried by the structure while the upper half is entirely independent of it, and, in making this assumption, he believes he is adding a factor of safety thereto. The area, then, which is assumed to be carried by an underground structure the depth of which is sufficient to allow the lines, _V A_ and _J A_, to intersect below the surface, is the lower half of _A N_{1} V E J N A_, or its equivalent, _A V E J A_, plus the area, _V E J_, or _A V J A_, the angle, _A V J_, being 1 [phi] [alpha] = --- ( 90° - [phi] ) + [phi] = 45° + -------. 2 2 It is not probable that these lines of thrust or pressure transmission, _A N_, _D K_, etc., will be straight, but, for purposes of calculation, they will be assumed to be so; also, that they will act along and parallel to the lines of repose of their natural slope, and that the thrust of the earth will therefore be measured by the relation between the radius and the tangent of this angle multiplied by the weight of material affected. The dead weight on a plane, _V J_, due to the material above, is, therefore, where _l_ = span or extreme width of opening = _V J_, _W_ = weight per cubic foot of material, and _W_{1}_ = weight per linear foot. |
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