Equilibrium

The angle that saves the most concrete

Cut an arch dam into horizontal rings and each ring is a curved surface with water on one side. The projection rule gives the water's whole push on it without an integral — the pressure times the chord — and the two abutments, pushing back along the ring, turn that into a thrust equal to the pressure times the radius, the hoop formula of a pipe arrived at without a pipe. From there one line of calculus says that the ring using least concrete has a central angle of 133.6°, whatever the canyon, the depth or the concrete. That number explains why arch dams in narrowing canyons are drawn at a constant angle rather than a constant radius, and why the angle that suits the concrete is not the one that suits the rock.

Assumes Every pressure points at the pin, A basement is a boat and The hinge put in on purpose.

Every pressure points at the pin. On a curved surface every element of a fluid’s pressure pushes in a different direction, so no multiplication gives the resultant, but two free bodies do: the horizontal component is the force on the surface’s vertical projection, and the vertical component is the weight of the fluid above it. On a radial gate, every element’s line of action passes through the trunnion as well, and the hoist that lifts it sees none of the water’s moment.

That essay worked in section, with the radial gate curved in a vertical plane. An arch dam is the same argument turned through ninety degrees. Its curvature is in plan: seen from above, the dam bows upstream into the reservoir, and each horizontal slice of it is a ring of concrete with water pressing on its convex face and rock at its two ends. The projection rule applies to each ring exactly as it applied to the radial gate, and it gives the whole design of the ring in two lines.

The water pushes on the chord

Take one ring, a metre high, 50 m below the water surface, spanning a 100 m gap between the canyon walls. The water presses on it at γwy\gamma_w y = 491 kPa, normal to its face everywhere.

The water pushes on the chord, and the abutments push back along the arch. One horizontal ring of an arch dam, one metre high, 50 m below the water, spanning a 100 m gap with a central angle of 133.6°, drawn in plan with the water on the convex side. The water presses 491 kPa normal to the face everywhere (arrows); by the projection rule its resultant is that pressure times the chord, 49,050 kN per metre of height, pointing straight downstream. Each abutment pushes back along the ring's tangent, at 66.8° to the chord, so the two thrusts are N = pw/2sin(θ/2) = 26,686 kN — the pressure times the ring's radius, 54.4 m, which is the hoop formula of a pipe, arrived at without a pipe.
Fig. 1 One ring of an arch dam, a metre high and 50 m below the water, spanning a 100 m gap with a central angle of 133.6°, in plan with the water on the convex side. The water’s push on it is the pressure times the chord, 49,050 kN per metre of height, pointing downstream; each abutment pushes back along the ring’s tangent with N = 26,686 kN, the pressure times the ring’s 54.4 m radius.

The resultant of that pressure, by the projection rule, is the pressure times the ring’s projection on a plane normal to the stream: the chord across the canyon, 100 m. So the water pushes the ring downstream with 49,050 kN for every metre of its height, and nothing about the ring’s curvature enters. A flat wall across the gap would receive the same push; a deeply curved one would receive the same push. The curvature does not change the load. It changes where the load goes.

A flat wall would have to carry it by bending, spanning 100 m across the canyon as a beam. A curved ring carries it by compression along its own length, and the compression arrives at the abutments along the ring’s tangent. With a central angle θ\theta the tangent at each end makes θ/2\theta/2 with the chord, so the two abutment thrusts NN balance the water when

2Nsin⁡(θ/2)=p w.2N\sin(\theta/2) = p\,w.

The chord is w=2Rsin⁡(θ/2)w = 2R\sin(\theta/2), so this is N=pRN = pR — the hoop tension of a pipe under internal pressure, with the sign reversed because the water is outside the ring. The formula usually derived by cutting a cylinder in half has been reached here without any cylinder, by the projection rule and two forces. A shell carries its load by being curved in exactly this sense: the load is the same as on a flat plate, and the curvature turns it into membrane force.

A ring as thick as its thrust

A ring of concrete allowed a compressive stress σ\sigma needs a thickness t=pR/σt = pR/\sigma. At 5 N/mm² — a working stress of the kind used to proportion arch dams by this method — the 50 m ring with a 54.4 m radius is 5.34 m thick. The choice is the radius, or equivalently the central angle, and the gap is fixed by the canyon.

Three arches across one gap. Rings of an arch dam 50 m below the water across a 100 m gap, in plan, at central angles of 60°, 133.6° and 180°, each drawn to scale with its thickness, pR/σ at 5.0 N/mm². 60.0°: radius 100.0 m, 9.81 m thick, 105 m long, 1,027 m³ per metre of height; 133.6°: radius 54.4 m, 5.34 m thick, 127 m long, 677 m³ per metre of height; 180.0°: radius 50.0 m, 4.91 m thick, 157 m long, 770 m³ per metre of height. The flat arch is short and thick, the semicircle thin and long; between them lies the ring that uses least concrete.
Fig. 2 Rings 50 m below the water across a 100 m gap, at central angles of 60°, 133.6° and 180°, drawn to scale with their thickness at 5 N/mm². At 60°, radius 100 m, 9.81 m thick, 105 m long, 1,027 m³ per metre of height; at 133.6°, 54.4 m, 5.34 m, 127 m long, 677 m³; at 180°, 50 m, 4.91 m, 157 m long, 770 m³.

The three rings show the trade. The 60° ring is nearly flat: short, but with a radius of 100 m it carries a large thrust and is nearly 10 m thick. The semicircle has the smallest radius any ring across a 100 m gap can have, 50 m, so its thrust and its thickness are least, 4.91 m; but it is half again as long. Concrete is thickness times length, and between those two extremes is a ring that uses less than either.

One line of calculus

The volume of a ring per metre of height is its thickness times its length:

V=pRσ⋅Rθ=pσ(w2)2θsin⁡2(θ/2).V = \frac{pR}{\sigma}\cdot R\theta = \frac{p}{\sigma}\left(\frac{w}{2}\right)^2 \frac{\theta}{\sin^2(\theta/2)}.

Everything outside the last fraction is fixed by the water, the concrete and the canyon. The last fraction depends on the angle alone, and setting its derivative to zero gives

tan⁡θ2=θ,θ=133.56°.\tan\frac{\theta}{2} = \theta, \qquad \theta = 133.56°.

The thrust is least at a semicircle, the concrete at 133.6°. For a ring of an arch dam across a fixed gap, against its central angle: the thrust in it (which sets its thickness) as a multiple of its least, at 180°; its length, as a multiple of the gap, least at 0°; and its volume, thickness times length, as a multiple of its least. The volume is least at 133.56°, where tan(θ/2) = θ, and is within 2 per cent of that from 118° to 150°; at 90° it is 14 per cent more, at 180° 14 per cent more. The width of the canyon, the depth of water and the strength of the concrete all scale the ring and none of them moves the angle.
Fig. 3 For a ring across a fixed gap, against its central angle: the thrust, and so the thickness, as a multiple of its least, at 180°; the length as a multiple of the gap; and the volume as a multiple of its least, at 133.56°. The volume is within 2 per cent of its least from 118° to 150°, and 14 per cent more at 90° and at 180°.

Whatever the canyon, the depth or the concrete, the ring that uses least concrete has a central angle of 133.6°. The thrust is least at 180°; the length is least for a flat ring; their product has a minimum between them, at an angle that is a property of the geometry of circles and nothing else. The minimum is also flat: anywhere from 118° to 150° costs within 2 per cent of the least, which is why real arch dams are drawn at angles in that range rather than at one exact figure, and why the abutments, not the concrete, usually decide where in the range.

This is an unusual kind of result for this subject. Most optimal forms depend on the loading — the line of thrust follows the load and changes when it does — but the water pressure here enters only as a scale, and so does everything else. The optimum is pure shape.

Where the thrust goes into the rock

The abutment thrust leaves the ring along its tangent, at θ/2\theta/2 to the chord. Part of it pushes straight into the canyon wall, across the valley; the rest pushes along the valley, downstream, and has to be resisted by the rock’s strength in shear.

The flatter the arch, the more of its thrust goes into the rock. How an abutment's thrust divides between a push across the valley, into the rock of the canyon wall (solid), and a push along the valley, downstream (dashed), as fractions of the thrust, against the ring's central angle. At 60° 87 per cent of it pushes into the rock; at 133.6°, 39 per cent; at 180°, none — a semicircular ring pushes its abutments straight downstream, along the canyon walls, and relies on the rock's shear to hold it. The angle that saves concrete is not the angle that suits the abutments, and in a canyon of weak or jointed rock it is the abutments that decide.
Fig. 4 How an abutment’s thrust divides between a push across the valley into the rock (solid) and a push along the valley, downstream (dashed), against the ring’s central angle. At 60°, 87 per cent pushes into the rock; at 133.6°, 39 per cent; at 180°, none.

A flat ring pushes mostly into the rock: at 60°, 87 per cent of its thrust is directed across the valley, into the canyon wall, where rock is strongest. At the economical 133.6° only 39 per cent is, and 92 per cent of the thrust’s magnitude — sin⁡66.8°\sin 66.8° — is directed along the valley. A semicircle pushes its abutments straight downstream, parallel to the canyon walls, and holds on only by the rock’s shear and friction along the contact — the question of whether it slides, asked of a mountain.

The angle that suits the concrete is not the angle that suits the rock. In a canyon of sound rock the concrete wins and the dam is drawn near 133.6°. In a canyon whose walls are jointed parallel to the river, or weathered at the surface, the abutment governs and the rings are drawn flatter, with more concrete, so that more of their thrust goes into the rock rather than along it. Many of the historic failures of arch dams were failures of an abutment rather than of the arch, which is this division of the thrust being decided in the wrong direction.

Constant angle, or constant radius

A dam is many rings stacked, and the canyon gets narrower with depth. That raises a question the single ring did not: as the gap shrinks towards the foot, what should the rings do?

The first arch dams kept a constant radius — every ring an arc of the same circle, the upstream face a vertical cylinder — because that is simple to set out and to build. As the canyon narrows, a ring of fixed radius spans a shorter chord, which means a smaller central angle, which means a flatter ring: the expensive end of the volume curve. And its thickness, pR/σpR/\sigma with RR fixed, grows in proportion to the depth all the way to the foot.

In a V-shaped canyon the cheapest dam is thickest half-way down. Ring thickness against depth for an arch dam in a V-shaped canyon 200 m wide at the crest and 100 m deep, with concrete stressed to 5.0 N/mm²: rings kept at 133.6° all the way down (solid), so that their radius shrinks with the canyon, and rings kept at the crest's radius of 108.8 m (dashed), so that their angle closes as the canyon narrows. The constant-radius dam thickens steadily with the water, to 10.7 m half-way down and 21.3 m at the foot; the constant-angle dam's thickness is the pressure times a shrinking radius, greatest at 50 m, 5.3 m, and thinning below. In all it needs 60 per cent of the constant-radius dam's concrete.
Fig. 5 Ring thickness against depth for an arch dam in a V-shaped canyon 200 m wide at the crest and 100 m deep, at 5 N/mm²: rings kept at 133.6° (solid), so that their radius shrinks with the canyon, and rings kept at the crest’s radius of 108.8 m (dashed). The constant-radius dam is 10.7 m thick half-way down and 21.3 m at its foot; the constant-angle dam is thickest at 50 m, 5.3 m, and needs 60 per cent of the other’s concrete.

The constant-angle dam keeps every ring at 133.6°, so each ring’s radius shrinks with its chord. Its thickness is then the pressure, which grows with depth, times a radius that shrinks with depth; in a V-shaped canyon the product is greatest half-way down and falls to nothing at the foot, where the gap closes. The cheapest dam in a V-shaped canyon is thickest half-way down, not at its foot, which is the opposite of every gravity structure and of every intuition about water pressure. Over the whole dam it needs 60 per cent of the constant-radius dam’s concrete.

The reason is visible ring by ring. At the crest the two dams are the same ring, 200 m across at 133.6°, with a radius of 108.8 m. Half-way down the V has narrowed to 100 m. The constant-angle ring there is the 54.4 m ring of the free-body figure; the constant-radius ring keeps its 108.8 m radius, so across a 100 m chord its central angle has closed to 54.7°, and by the volume curve a ring at 54.7° uses 64 per cent more concrete than one at 133.6° across the same chord. Lower still the constant-radius rings are flatter yet, while carrying the deepest water. The constant-radius dam is paying the steep side of the volume curve exactly where the pressure is greatest.

The constant-angle form is old: it is credited to Lars Jorgensen, whose Salmon Creek Dam in Alaska, finished in 1914, was the first built on the principle. Its upstream face is not a cylinder but a twisted surface, every ring centred on a different point, and its overhang near the crest — where the rings are largest and the dam leans upstream — is the visible signature of the arithmetic.

The narrower the canyon gets, the more a constant angle saves. The concrete in a constant-angle arch dam as a share of a constant-radius one's, against how the canyon narrows with depth — its width as (1 − depth/height) to the power drawn: nought is a rectangular canyon, one a V, two a V that pinches at its foot. In a rectangular canyon the two are one dam; at 0.5 the constant-angle dam needs 73 per cent of the concrete, in a V 60 per cent, at 2 49 per cent. A constant radius suits a canyon whose width does not change; every canyon that narrows with depth leaves the constant-radius dam's lower rings at ever smaller angles, which is the expensive end of the volume curve.
Fig. 6 The concrete in a constant-angle dam as a share of a constant-radius one’s, against how the canyon narrows with depth: width as (1 − depth/height) raised to the power drawn. In a rectangular canyon the two are one dam; at a power of 0.5, 73 per cent; in a V, 60 per cent; at 2, a canyon that pinches at its foot, 49 per cent.

The saving depends on how fast the canyon narrows. In a canyon with vertical walls the gap is the same at every depth, the two forms are the same dam, and nothing is saved. In a U-shaped canyon that narrows slowly at first the constant-angle dam saves about a quarter; in a V, two-fifths; in a canyon that pinches towards a narrow gorge at its foot, half. A constant radius suits a canyon that does not narrow, and canyons that do not narrow are rare.

A pipe that is open on one side

The hoop formula is usually met in a pipe or a tank, where a closed ring holds a pressure on its inside and the force in the wall is the pressure times the radius whatever the ring is made of. The arch dam’s ring is the same ring cut open and turned round: the pressure is outside, the force is compression rather than tension, and the two cut ends are held by rock instead of by the rest of the ring.

Cutting the ring open is what creates the optimum. A closed pipe has no choice of angle — it is 360° — and its only free variable is its radius, which is set by how much it has to carry. An open ring across a gap has a free angle, because the gap fixes the chord and not the radius, and the angle trades thrust against length. The pipe and the dam share the formula and differ in what is fixed.

The same open ring appears wherever pressure meets a curve that ends on supports. A curved retaining wall in plan, a cofferdam of sheet piles bowed against the water, a vault seen in section carrying its own weight — each is a ring of some angle spanning a fixed gap, and each has the same trade between a tight curve that is thin but long and a flat one that is short but thick. The number 133.6° is exact only for a circle under uniform pressure, but the shape of the trade is general, and so is the flatness of its minimum: a curve somewhat flatter or tighter than the optimum costs almost nothing, which leaves the designer free to let something else decide.

What the projection rule does here

The two derivations in this essay — the push on the chord and the thrust in the ring — both come from the rule that the resultant of pressure on any curved surface equals the pressure on its projection. The rule works because pressure has no preferred direction: it pushes equally on every face of a fluid element, so any closed free body of water is in equilibrium under its own weight and the pressures on its faces, and the curved surface can be replaced by a flat one without changing the force.

That is also why the dam’s shape cannot reduce the water’s push. Every arch dam across a 100 m gap, at every angle, receives exactly 49,050 kN per metre of height at a depth of 50 m. What the shape chooses is the path: through bending of a flat wall, through compression of a curved ring, or — in a gravity dam — through the weight of a block of concrete large enough to resist the push by friction on its base. The arch dam is the cheapest of the three in a narrow canyon of good rock because compression is the most efficient way concrete can carry anything, and it can only use compression because the rock at its ends can push back.

One ring, by hand

Fifty metres down, the water pressure is 9.81×50=4919.81 \times 50 = 491 kPa. Across a 100 m chord the push is 491×100=49,050491 \times 100 = 49{,}050 kN per metre of height.

At the optimum, tan⁡(θ/2)=θ\tan(\theta/2) = \theta; writing ϕ=θ/2\phi = \theta/2, tan⁡ϕ=2ϕ\tan\phi = 2\phi, which a few trials settle at ϕ\phi = 1.1656 rad = 66.78°. The radius is R=50/sin⁡66.78°=54.4R = 50/\sin 66.78° = 54.4 m and the thrust N=pR=491×54.4=26,690N = pR = 491 \times 54.4 = 26{,}690 kN; check: 2×26,690×sin⁡66.78°=49,0602 \times 26{,}690 \times \sin 66.78° = 49{,}060 kN, the push on the chord. At 5,000 kPa the thickness is 26,690/5,000=5.3426{,}690/5{,}000 = 5.34 m, and the length 54.4×2.331=12754.4 \times 2.331 = 127 m, so the ring holds 5.34×127=677 m35.34 \times 127 = 677\ \text{m}^3 for each metre of its height.

For the semicircle, RR = 50 m, tt = 4.91 m, length 157 m, 770 m³ — 14 per cent more concrete for a ring 8 per cent thinner.

Rings, and nothing else

The calculation rests on choices that limit it.

The dam is a stack of independent rings. A real arch dam is also a set of vertical cantilevers fixed into the valley floor, and the water’s load divides between ring action and cantilever action by their relative stiffness — the stiffer path taking more. Near the foot the cantilevers are short and stiff and carry most of the load, which is why a real dam is not thin there even in a V-shaped canyon; the ring calculation is the preliminary method, and the division between the two was the subject of the trial-load analyses of the 1930s.

The ring is thin. The hoop formula takes the thrust on a single radius; a ring whose thickness is a tenth of its radius has a few per cent more stress on its upstream face, and the abutments’ fixity puts bending into rings that the thin-ring model treats as hinged.

The stress is a single allowable number. A real design checks the arch’s own buckling, temperature changes that shorten and lengthen the rings, and the uplift of water in the foundation, which a basement under water shows can be the governing load of a structure that sits in it.

The reservoir is full and still. A dam spends its life at many levels, and the rings near the crest are lightly loaded for most of it; an earthquake adds a hydrodynamic pressure that is greatest part-way down and acts in both directions, so that a ring designed only to be pushed must also survive being pulled, which a thin compression ring cannot. The ring calculation sizes the dam for the one load it carries every day.

The abutments do not move. Rock deforms under 27 MN per metre of height, and an abutment that gives lets the ring flatten and bend; the stiffness of the rock is as much a part of an arch dam as the concrete.

Still open: the ring that is not circular

Every ring here is an arc of a circle, because the hoop formula is simplest for a circle and because a circle under uniform pressure carries it in pure compression. But the water pressure on a ring is uniform only in magnitude: on a ring whose ends are fixed into rock that gives, or one loaded by silt on its lower part, it is not the circle that carries the load in pure compression but some other curve, flatter at the crown or steeper at the ends. Whether a ring shaped to the funicular of its real loading — elliptical or parabolic arches are used in some dams for this reason — saves more than the 2 per cent margin around 133.6°, or whether the circle’s simplicity is worth more than whatever the funicular ring saves, is the question of what the optimal angle becomes once the ring is allowed a shape as well as an angle.

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AbutmentArchCurved surface pressureHoop stressHydrostatic pressureOptimisationThrust