Equilibrium

The pressure that stops growing

A tank of liquid presses harder the deeper it gets, without limit. A silo of grain does not. Wall friction carries part of the weight, the pressure that generates the friction is proportional to the pressure being carried, and the equation that follows is the one that describes a rope round a bollard.

Assumes The load that depends on what carries it, The force that is whatever it needs to be and Weight is the only thing resisting it.

Water in a tank presses on the wall with γh\gamma h. Nothing stops it: go deeper and the pressure grows, in exact proportion, forever.

Grain in a silo does not do that, and the difference is one property that water does not have. Grain has shear strength. It can transmit a shear stress to the wall it is resting against, and once it does, part of its own weight is being carried by the wall rather than by whatever is underneath.

That is not a small correction. At the base of a 30 m fill in an 8 m silo the vertical pressure is 85 kN/m² against a liquid’s 270, and the wall is carrying 69% of the stored weight.

A tank grows without limit; a silo stops. Vertical pressure against depth in a 8 m silo of a solid weighing 9 kN/m³, beside the straight line a liquid of the same weight would have produced. The free body is a slice: its own weight in, the wall friction out, and the friction is μK times the vertical pressure that generates it. The result saturates at γR/μK = 89 kN/m² and reaches 63% of it at one characteristic depth, R/μK = 9.9 m. At the base the pressure is 85 kN/m² against a liquid's 270 — 69% less — and the wall has taken 69% of the stored weight down with it. The exponent is the capstan's, and for the same reason.
Fig. 1 The whole argument in two curves. Vertical pressure against depth in an 8 m silo of a solid weighing 9 kN/m³, beside the straight line a liquid of the same weight would have drawn: the liquid has no ceiling and the solid saturates at γR/μK\gamma R/\mu K = 89 kN/m², reaching 63% of it at one characteristic depth of 9.9 m. The third curve is the horizontal pressure, which is KK times the vertical and therefore saturates with it. At the base the solid reads 85 kN/m² against the liquid’s 270, and the wall has taken 69% of the stored weight down with it.

Which free body produced the number

A horizontal slice of the stored solid, of thickness dzdz, across the whole cross-section.

Four things act on it. Its own weight, γA dz\gamma A\,dz, downward. The vertical pressure from the slice above, pvAp_v A, downward. The vertical pressure from the slice below, (pv+dpv)A(p_v + dp_v)A, upward. And the friction on the wall around its perimeter, μphUdz\mu p_h U dz, upward, where php_h is the horizontal pressure pushing the solid against the wall.

Sum them:

A dpv=γA dz−μphU dzA\,dp_v = \gamma A\,dz - \mu p_h U\,dz

Now the closure that makes it solvable. The horizontal pressure is taken as a fixed fraction of the vertical one, ph=Kpvp_h = K p_v — the same assumption every earth-pressure argument on this site makes, and just as much an assumption here. Substituting and writing R=A/UR = A/U for the hydraulic radius:

dpvdz=γ−μKRpv\frac{dp_v}{dz} = \gamma - \frac{\mu K}{R}p_v

which is a first-order linear equation whose solution is

pv(z)=γRμK(1−e−μKz/R)p_v(z) = \frac{\gamma R}{\mu K}\left(1 - e^{-\mu K z/R}\right)

The derivative goes to zero. As pvp_v grows, the friction it generates grows with it, and at pv=γR/μKp_v = \gamma R/\mu K the friction is carrying the whole of each new slice’s weight and the pressure stops rising.

One term in that slice is not a force the material supplies willingly, and the solution has already decided what it is.

The reaction lies inside the cone, so the block stands. A block of 100 on a plane at 15°, against a coefficient of friction of 0.45. Resolving across and along the plane gives a normal force of 96.6 and a friction demand of 25.9, against a capacity of μN = 43.5 — a ratio of 0.60. Added together the two make one contact reaction leaning 15.0° from the normal, and the admissible reactions fill a cone of half-angle arctan μ = 24.2°. Equilibrium is possible exactly when the demanded reaction lies inside that cone, which here it does. The weight enters neither the cone nor the lean: a block of any weight on this slope leans its reaction by the same 15.0°, which is why the angle of repose is a material property and the size of a heap of sand is not.
Fig. 2 Friction as a cone rather than a force. The wall shear in the slice above is written at its limit — τ=μph\tau = \mu p_h — which is the assumption that the solid is settling relative to the wall everywhere. If it is not, the friction is whatever it needs to be, it is less than that, and every pressure on this page is an underestimate.

The three numbers in it, and what they do

R=A/UR = A/U, the hydraulic radius. For a circle it is D/4D/4 — 2.0 m for the 8 m silo here. It is the only geometry in the answer, and it is the ratio of what is being carried to what is available to carry it by friction. A wide silo has a large RR, a high ceiling and behaves nearly like a tank; a narrow one has a small RR and saturates almost at once.

μ\mu, the friction between the solid and the wall. Not the internal friction of the material — that is a different number and it is KK’s business. This is a contact property, and it depends as much on the wall as on the contents: a smooth-lined steel silo has half the wall friction of a concrete one, which halves the saturation depth’s denominator and doubles the ceiling.

KK, the ratio of horizontal to vertical pressure. Between about 0.4 and 0.6 for granular solids at rest, and the least well known of the three. It is the same KK that appears in earth pressure and it carries the same caveat: it depends on the state of the material rather than on the material.

All three appear only in the products γR/μK\gamma R/\mu K and R/μKR/\mu K. The problem has two parameters, not four.

A tank grows without limit; a silo stops. Vertical pressure against depth in a 4 m silo of a solid weighing 9 kN/m³, beside the straight line a liquid of the same weight would have produced. The free body is a slice: its own weight in, the wall friction out, and the friction is μK times the vertical pressure that generates it. The result saturates at γR/μK = 44 kN/m² and reaches 63% of it at one characteristic depth, R/μK = 4.9 m. At the base the pressure is 44 kN/m² against a liquid's 270 — 84% less — and the wall has taken 84% of the stored weight down with it. The exponent is the capstan's, and for the same reason.
Fig. 3 The first of those two, halved. The same solid against the same wall in a 4 m silo instead of an 8 m one: the hydraulic radius halves, so the ceiling halves to 44 kN/m² and the characteristic depth halves to 4.9 m. The base pressure is 44 kN/m² against the liquid’s 270 — 84% less, where the wider silo was 69% less — and the wall is carrying 84% of the stored weight. A narrow silo has saturated before it is properly deep.

The exponent is the capstan’s

The equation dpv/dz=γ−(μK/R)pvdp_v/dz = \gamma - (\mu K/R)p_v has a first cousin on this site, and the relationship is exact rather than poetic.

A rope wrapped round a bollard obeys dT/dθ=μTdT/d\theta = \mu T, giving T=T0eμθT = T_0 e^{\mu\theta} — the capstan equation, and the reason a sailor holds a hawser under tons of load with one hand. The mechanism there is: friction is proportional to the normal force, the normal force is proportional to the tension, so the tension grows exponentially in the wrapped angle.

The mechanism here is: friction is proportional to the horizontal pressure, the horizontal pressure is proportional to the vertical pressure, so the vertical pressure approaches its ceiling exponentially in the depth.

Same statement, same equation, different variable. Feeding this silo’s μK\mu K and its depth-to-radius ratio into the capstan routine gives e3.038=20.85e^{3.038} = 20.85, which is exactly the exponential factor in the silo solution.

The two problems even share their surprise. In both, the exponential means the answer is dominated by a ratio — wrapped angle for the rope, depth over hydraulic radius for the silo — and both saturate so fast that the practical question becomes “how many turns” or “how many diameters” rather than anything about magnitude.

The same rope, two bollards, one answer. A rope wrapped 180° round two bollards of different size, held at 200 N, with μ = 0.25 at the contact. Both hold 439 N at the far end, because T₂/T₁ = e^(μβ) and the radius is not in it: a smaller bollard squeezes the rope harder over a shorter length of contact and the two cancel exactly. What the radius does change is the squeeze. The contact pressure runs to 2.9 kN per metre of contact on the 0.15 m bollard and 8.8 kN/m on the 0.05 m one, in the ratio of the radii — which is why a rope burns at the far end of a wrap on a thin pin and not on a fat one. The rope is drawn thickening with its tension and the inward arrows are the local pressure, both to scale.
Fig. 4 The rope round the bollard, which is this differential equation in its other setting. Three turns multiply the holdable load by 43 for a friction coefficient of 0.2; three diameters of depth take a silo to half its ceiling.

How much the wall carries, and why slenderness decides

The base takes pv(H)×Ap_v(H) \times A and the wall takes the rest, so the wall’s share is

1−pv(H)γH1 - \frac{p_v(H)}{\gamma H}

which depends on nothing but the ratio H/DH/D once the material and the wall are fixed:

depth ÷ diameter wall’s share base pressure
0.5 18% 30 kN/m²
1 31% 49
2 50% 71
4 70% 85
8 85% 89
16 92% 89

Past about four diameters the base pressure has stopped changing altogether — it is at the ceiling — so everything added above that point goes into the wall and nothing goes into the floor.

That single row is the whole reason silos are structurally different from tanks. A tall silo’s wall is a vertical load-carrying element, carrying tens of thousands of kilonewtons of stored material by friction, on top of resisting the horizontal pressure. The failure that follows is a vertical buckle of the wall rather than a burst — which is not what anybody expects a silo to do.

Past a certain slenderness the wall is carrying the silo. The share of the stored weight taken by wall friction rather than by the base, against how many diameters deep the silo is. The vertical pressure saturates at γR/μK = 89 kN/m² and the base can never take more than that times its area, so everything added above simply goes into the wall: at one diameter the wall has 31% of it, at four 70%, and at sixteen 92%. A tall silo is a structure whose contents hang from its sides, which is why silo walls fail vertically and why they are designed for a load that a tank of the same fluid does not have.
Fig. 5 The same table as a curve. The transition is at about two diameters and the asymptote is approached fast; a “squat” silo and a “slender” one are two different structures with two different failure modes, and the boundary between them is a number on this axis.

That makes the wall a surface that carries by being curved in two directions at once: a thin cylinder in hoop tension from the horizontal pressure, and in vertical compression from the friction. The friction hands it 371 kN per metre of perimeter at the base here — a membrane force that nothing about the stored material’s weight suggests would be there, and the one that decides the wall’s thickness against buckling.

The same equation with a different name

Silos are not the only place a saturating pressure appears, and the family is worth naming because the mechanism transfers exactly.

A trench. The soil in a narrow trench arches across it and hands part of its weight to the sides, so the vertical stress on a pipe at the bottom is far less than γH\gamma H — which is the trench condition every buried pipe is designed for, and it is Janssen with the trench walls in place of the silo’s.

A tunnel. The ground above a tunnel arches over it for the same reason, and the load the lining is designed for is a fraction of the overburden. The fraction is set by a hydraulic radius that here is the tunnel’s own width.

A pile. A pile in sand carries load by shaft friction, and the shaft friction depends on the horizontal stress against the pile, which depends on the vertical stress in the ground — and the vertical stress stops growing with depth once the pile’s own zone of influence starts arching. The observation that shaft friction reaches a “critical depth” and then stops increasing is the same saturation in the same equation.

What the three share is the ingredient water does not have: a material that can transmit shear to a boundary, and a boundary close enough that the shear matters. The hydraulic radius is the measure of “close enough”, and everything else follows.

Five loads behind one wall, and the water is the biggest. The horizontal pressure on a 6 m wall retaining soil at 18 kN/m³ with a friction angle of 30°, a surcharge of 10 kPa and the water table 2 m down, drawn once as the profile the wall feels and then once per term. The terms are surcharge 20.0 kN/m at 3.00 m, soil above water 12.0 kN/m at 4.67 m, soil at the water table 48.0 kN/m at 2.00 m, submerged soil 27.2 kN/m at 1.33 m, water 78.5 kN/m at 1.33 m, and they sum to 185.7 kN/m — matched to 7e-8 by integrating the drawn profile numerically. The largest single term is the water, at 78.5 kN/m: water has no shear strength, so its coefficient is exactly one where the soil's is 0.333, and it acts on top of the soil's effective stress rather than instead of it. The combined resultant sits at 1.90 m above the base, 0.317 of the height rather than the third point at 2.00 m that a pure triangle would give.
Fig. 6 The retained-soil version, which is Janssen’s problem with the friction left out because a retaining wall’s soil is not confined on two sides. The moment it is — a basement between two walls, a narrow trench — the arching starts and the pressure falls below the triangular one.

What the material is doing in every one of them is forming an arch nobody drew. Arching in a granular solid is a thrust line finding its way to two supports, the same object a three-pinned arch has its hinges put in on purpose to make determinate; the silo’s supports happen to be its own walls, and the thrust delivered to them is the friction this page is about.

Two identical pipes, and one carries three times the other. Load per metre on a buried conduit against the depth of cover, in trench widths, with the weight of the prism of soil directly above it drawn between them. A conduit laid in a narrow trench is stiffer than nothing and softer than the sides: the backfill settles relative to the undisturbed ground, the friction on the trench walls acts upward, and the conduit gets 64% of the prism. Lay the same conduit on the ground and build an embankment over it and it is now stiffer than the fill beside it, the interior prism settles less, the friction acts downward, and it gets 172% — a factor of 2.71 between two pipes with nothing different but which way the ground moved. The equation is Janssen's, the same one a silo wall obeys, with a trench for a silo; both curves start on the prism line, because with no depth there is no shear to redistribute anything. This is why a flexible pipe is buried rather than a rigid one: making the conduit weaker moves it down the page.
Fig. 7 Janssen’s equation with a trench for a silo, and the reversal that comes with it. Load per metre on a buried conduit against the depth of cover in trench widths, with the weight of the prism of soil directly above it drawn between the two curves. In a narrow trench the backfill settles relative to the undisturbed ground, the friction on the trench walls acts upward, and the conduit gets 64% of the prism. Lay the same conduit on the ground and build an embankment over it and the interior prism settles less than the fill beside it, the friction reverses, and it gets 172% — a factor of 2.71 between two pipes with nothing different about them but which way the ground moved.

The horizontal pressure, which is what bursts it

ph=Kpvp_h = Kp_v saturates too, at γR/μ\gamma R/\mu — 38 kN/m² at the base of the silo drawn.

For a circular silo that produces a hoop tension of phD/2=152p_h D/2 = 152 kN per metre of height, which is the number the wall’s horizontal reinforcement or its plate thickness is sized on. It is constant over the lower part of a tall silo, because the pressure has saturated — so a tall silo’s hoop reinforcement is uniform below a few diameters and graded above, which is the opposite arrangement to a tank’s.

For a rectangular silo it is much worse. A flat wall has to span between corners in bending rather than carry the pressure as a hoop tension, so the same 38 kN/m² produces a moment rather than a membrane force, and rectangular silos are correspondingly heavier for the same capacity. The hydraulic radius does not care about the shape — a square silo of 8 m side has exactly the same R=2R = 2 m and the same pressures — so the difference is entirely in what the wall does with them.

One consequence of the saturation is easy to get wrong on the way out. A load spread over a surface has a resultant, and where that resultant acts is decided by the shape of the distribution rather than by its total: a liquid’s triangle puts it at H/3H/3, while the silo’s profile is very nearly uniform over the lower part of a tall wall and puts it much higher. Any overturning or foundation calculation on the wall needs the right one, and the two differ by a sixth of the height.

One length, and why a tabletop model predicted full-size silos

Write the solution with the characteristic depth in it and something becomes visible that the four parameters conceal:

pv(z)=γz0(1−e−z/z0),z0=RμKp_v(z) = \gamma z_0\left(1 - e^{-z/z_0}\right), \qquad z_0 = \frac{R}{\mu K}

There is one length in the problem, and the depth enters only as the ratio z/z0z/z_0. Everything else — the friction coefficient, the pressure ratio, the diameter — has been absorbed into it, and the unit weight sets the scale of the pressures without affecting their shape at all.

The consequence is that all silos are the same silo. Two of them holding the same material against the same wall, one 8 m across and one 16 m, have identical curves once depth is measured in units of z0z_0; the second simply has a z0z_0 twice as large, so it reaches the same fraction of its ceiling at twice the depth. A silo is “slender” or “squat” according to H/z0H/z_0, and that ratio is what the table two sections up is really tabulating — H/DH/D stands in for it only because the material and the wall were held fixed.

A tank grows without limit; a silo stops. Vertical pressure against depth in a 16 m silo of a solid weighing 9 kN/m³, beside the straight line a liquid of the same weight would have produced. The free body is a slice: its own weight in, the wall friction out, and the friction is μK times the vertical pressure that generates it. The result saturates at γR/μK = 178 kN/m² and reaches 63% of it at one characteristic depth, R/μK = 19.8 m. At the base the pressure is 139 kN/m² against a liquid's 270 — 49% less — and the wall has taken 49% of the stored weight down with it. The exponent is the capstan's, and for the same reason.
Fig. 8 The other end of that comparison: 16 m across, holding the same solid against the same wall. Every pressure has doubled with the diameter — the ceiling is 178 kN/m² where the 8 m silo’s was 89 — and the characteristic depth has doubled with it, from 9.9 m to 19.8, so the curve reaches the same fraction of its own ceiling at twice the depth. At the base it reads 139 kN/m² against the liquid’s 270, and the wall has taken 49% rather than 69%. Measured in units of z0z_0 this is the first figure on the page, unchanged.

This is why Janssen’s tabletop experiment settled the question for structures a hundred times its size. He was not measuring silos; he was measuring the shape of a dimensionless curve, and the shape does not know how big the apparatus is. It is the same argument that makes any model test worth doing, and it is unusually clean here because the problem has exactly one dimensionless group in it.

Two design consequences fall straight out, and they are worth stating because they cut against instinct.

Every pressure scales with the diameter and none of them with the height. The ceiling is γz0=γR/μK\gamma z_0 = \gamma R/\mu K, so doubling the diameter doubles the vertical pressure at the base, doubles the horizontal pressure, and doubles the hoop tension per metre — while quadrupling the stored volume. Capacity bought by widening is paid for at the full rate. Capacity bought by heightening a silo that is already several z0z_0 deep costs nothing in pressure at all, because the pressure stopped rising; it costs only more wall, carrying more accumulated friction.

And the ceiling contains no reference to how much is stored. A silo filled to four diameters and a silo filled to forty put the same horizontal pressure on their walls at the base and the same vertical pressure on their floors. That is the property this collection has met once before, in a substructure whose uplift does not grow when the building does — an action with a ceiling set by geometry rather than by quantity — and it is rare enough in structures to be worth recognising when it appears.

The number a designer actually needs

Three quantities come out of the solution and each sizes a different part of the structure.

The horizontal pressure sizes the wall’s hoop reinforcement, and it saturates — so on a tall silo it is a constant below a few diameters, at γR/μ\gamma R/\mu.

The wall friction sizes the wall’s vertical reinforcement or its plate thickness against buckling, and it accumulates — 371 kN per metre of perimeter at the base here, growing all the way down.

The base pressure sizes the floor and the foundation, and it saturates too, at a value that on a slender silo is a small fraction of the stored weight divided by the area.

The uncomfortable part is that the three are not conservative in the same direction. A low estimate of μ\mu gives a high base pressure and a low wall friction; a high one gives the opposite. So there is no single conservative choice of the friction coefficient, and a silo has to be checked with a high value for the wall and a low value for the floor — two calculations with two different numbers for the same physical property.

That is a shape worth carrying past this page. A parameter that appears on both sides of a load path has no conservative value, and the honest response is two load cases rather than a cautious number.

The floor is the plainest instance of it. What it is designed for is a pressure whose whole uncertainty sits in the load and none of it in a resistance — the character it shares with the class of checks where weight is the only thing resisting, and the reason a silo floor is sized by a number nobody can measure to better than a factor of two.

Where the model stops

Everything is at rest. The Janssen solution is the filling case, and silos fail while emptying. When the solid starts to flow, the material at the wall moves down relative to the material at the centre, the principal stress directions rotate, and KK jumps — sometimes by a factor of two or three, in a band that travels up the silo as a “switch”. The pressure spike that follows is the single commonest cause of silo failure and this equation does not contain it.

KK is a constant. It is not: it depends on the stress state, on whether the material is being loaded or unloaded, and on how the silo was filled. The whole solution is an envelope around a number nobody can measure well.

And the pressure is uniform across the section. It is not — the vertical stress is higher at the centre than at the wall — so pvp_v here is a mean, and the friction is computed from a php_h derived from that mean rather than from the pressure actually at the wall.

Nor is the filling symmetric. Eccentric filling or eccentric discharge produces a pressure distribution that is not axisymmetric, which puts bending into a wall designed for hoop tension, and is the second commonest cause of failure.

What the pictures cannot show

The curves are drawn for a silo that has been filled and left. A real one is filled, emptied, and filled again, dozens of times a year, and the pressures are different every time depending on how fast and from where.

Nor can they show the material. Grain, cement, coal and wood chips have wall friction coefficients spanning a factor of three and KK values spanning a factor of two, so the same silo behaves quite differently depending on what is in it — and a silo designed for one product and later used for another is a structure being asked a question it was not designed for.

The assumption the figure rests on

ph=Kpvp_h = Kp_v, with KK constant and known. Everything downstream — the saturation, the depth, the wall’s share, the hoop tension, the exponent — is that one closure. It is the same closure earth-pressure theory makes, it is unavoidable if a one-dimensional equation is wanted, and it is the reason silo design codes wrap the elegant result above in a set of multipliers whose job is to cover the range KK actually takes.

There is a second assumption of the same kind sitting beside it, and it is the one the first figure of the free-body section drew. The friction is at its limit everywhere. Janssen’s solution assumes full mobilisation over the whole height, which requires the solid to be settling relative to the wall all the way down — true while a silo is being filled, and not true afterwards. A silo standing full and undisturbed has less friction on its walls than the equation credits it with, and correspondingly more pressure on its floor.

The history, and the year it was measured

Janssen published this in 1895, and what makes the paper worth remembering is not the derivation — the differential equation is a page — but that he measured it first.

He built a model silo with a floor that could be weighed independently of the walls, filled it with grain, and read off how much of the fill the floor was carrying as the depth grew. The measurement showed the floor’s share falling toward an asymptote; the equation came afterwards, to explain a curve that was already on paper.

That order matters because the closure ph=Kpvp_h = Kp_v is not derivable from anything. It is a modelling choice, and the only reason to believe it is that the solution it produces has the shape the measurements have. A century and a quarter of silo design rests on a fitted constant in a one-dimensional model — which is a fair description of a great deal of this subject, stated plainly for once.

The ladder from here

Later rungs on this anchor: the discharge case and the switch pressure, where KK changes and a travelling band of high pressure runs up the wall. Mass flow against funnel flow, and how the hopper geometry decides which one happens. Eccentric discharge, which is the load case that turns a hoop-tension problem into a bending one. The hopper itself, where the wall is inclined and the friction has a vertical and a horizontal component. Silo quaking, a self-excited oscillation driven by stick-slip at the wall. And the measurement problem underneath all of it: why μ\mu and KK are quoted as ranges, and what a designer does with a load that has a factor of two of genuine uncertainty in it.

What this makes readable

Essays that name this one as a prerequisite.

Named alongside this one

Essays reaching for the same objects. Nobody chose these; they are what the concept index makes visible.

What links here

Every essay whose body links to this one.

The objects this essay names

Each one links to every other essay that touches it.

CapstanCharacteristic depthDischargeFree bodyFrictionHydraulic radiusHydrostatic pressureJanssenLateral pressure ratioSaturationSiloStored solidWall friction