Soil structure — where it appears
Named by 3 essays across 2 fields — each of them below, with the objects they name alongside it.
The ground is a spring
Every dynamic result in this collection has assumed a structure rising from something that does not move. Nothing does. A foundation can slide and it can rock, both are flexibilities in series with the structure's own, and the rocking one carries a square of the height — so the period lengthens, the force falls, the drift rises, and the damping goes the wrong way.
The lining that is stronger for being weaker
A tunnel lining is not loaded. The ground arrives already stressed and the hole wants to squash into an ellipse; the lining's only job is to refuse, and how much moment it collects depends entirely on how hard it refuses. Make it stiffer and it takes more. Make it flexible — put joints in it, make it thin — and it takes almost none, while the hoop thrust it carries does not move at all.
The ground has a period of its own
An earthquake is measured on rock and felt on soil, and between the two is a layer that behaves exactly like a structure — a column fixed at bedrock, free at the surface, with a fundamental period of four times its depth over its shear wave velocity and a set of odd harmonics above it. The motion a building receives is the rock motion through that filter, and the filter is sharp.
Named alongside it
The objects these essays reach for when they reach for this one.
DampingImpedanceNatural periodResponse spectrumAmplificationBase isolationBase shearBedrockConstruction sequenceDriftDuctility demandEarth pressure