Construct · 3 fields · 4 citations
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In structural mechanics, buckling is a sudden sideways deflection of a slender member under compression: below a critical load the member stays straight, but once that load is reached it bows out abruptly and may collapse, failing by instability well before the material itself is crushed. Timoshenko and Gere's Theory of Elastic Stability develops the critical-load analysis that grew from Euler's eighteenth-century column formula. The referent is an elastic instability under compressive load, defined by a critical (buckling) load and a mode shape, the same mechanics that reshapes folded rock strata and growing tissue.[1]
In structural geology, buckling is how layered rock responds to compression along its bedding: a stiff layer embedded in weaker rock becomes unstable and folds at a preferred wavelength set by the layer's thickness and the stiffness contrast with its surroundings. Biot's 1961 Theory of folding of stratified viscoelastic media and its implications in tectonics and orogenesis gave the mechanical theory predicting that dominant wavelength. It is the same compressive instability as a buckling column, operating over geological time in viscoelastic strata and read out as fold wavelength and amplitude rather than a single critical load.[2]
In developmental biology, buckling explains how smooth tissues acquire folds: when a growing layer is constrained by a stiffer or slower-growing substrate, the resulting compression drives a mechanical instability that wrinkles the surface, as in the villi of the gut and the convolutions of the brain. Shyer and colleagues' 2013 Villification: How the Gut Gets Its Villi and Tallinen and colleagues' 2016 On the growth and form of cortical convolutions show these forms arising from growth-induced buckling. It is the same elastic instability as in a column or folded strata, here powered by differential growth and measured as the wavelength and pattern of the folds.[3][4]
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