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elasticity friction drag and buoyancy models

Learning objectives

  • Outcome

    Calculate elastic force and deformation using Hooke's law within the elastic limit: F=−kxF=-kx and σ=Eε\sigma=E\varepsilon.

  • Outcome

    Distinguish static and kinetic friction and apply the conditions Ffr≤μsNF_{\text{fr}}\le\mu_s N and Ffr=μkNF_{\text{fr}}=\mu_k N in problem solving.

  • Outcome

    Compare linear and quadratic drag models and determine terminal speed from the force-balance condition.

  • Outcome

    Apply Archimedes' principle FA=ρfVdispgF_A=\rho_f V_{\text{disp}}g to determine floating and sinking conditions.

Understand the idea

Elasticity, friction, drag, and buoyancy models

Text

The mechanical models of elasticity, friction, drag, and buoyancy describe the forces that must be inserted into Newton's second law. For small deformations the elastic force is linear: F=−kxF=-kx, and stress is related to strain by Hooke's law σ=Eε\sigma=E\varepsilon; beyond the proportionality limit this model fails. Static dry friction takes values from zero up to Fmax⁡=μsNF_{\max}=\mu_s N, while kinetic friction is approximately constant, Fk=μkNF_k=\mu_k N, and opposes relative motion. Drag is modeled as linear, F=−bvF=-bv, at low speeds or quadratic, F=−12CDρAv2F=-\frac12 C_D\rho A v^2, at high speeds; terminal speed occurs when drag balances the driving force. Buoyancy is described by Archimedes' principle, FA=ρfVdispgF_A=\rho_f V_{\text{disp}}g; a body floats when FA=mgF_A=mg and sinks when its average density exceeds the fluid density. All these models are idealizations with limits of validity, and they are always used together with Newton's laws.

Worked examples

Direct

Problem

Direct. A spring of stiffness k=200 N/mk=200\ \mathrm{N/m} is stretched by x=4 cmx=4\ \mathrm{cm}. Find the magnitude and direction of the elastic force.

Solution

Convert the extension to SI: x=0.04 mx=0.04\ \mathrm{m}. By Hooke's law the force magnitude is F=kxF=kx. Substituting gives F=200⋅0.04=8 NF=200\cdot0.04=8\ \mathrm{N}. The elastic force is directed opposite to the extension, toward the equilibrium position: in vector form, F⃗=−kx⃗\vec F=-k\vec x.

Application

Problem

Application. A block of mass m=5 kgm=5\ \mathrm{kg} rests on a horizontal table. The friction coefficients are μs=0.5\mu_s=0.5 and μk=0.4\mu_k=0.4. A horizontal force F=30 NF=30\ \mathrm{N} is applied to the block. Will the block move, and if so, with what acceleration? Take g=9.8 m/s2g=9.8\ \mathrm{m/s^2}.

Solution

The normal reaction is N=mg=5⋅9.8=49 NN=mg=5\cdot9.8=49\ \mathrm{N}. The maximum static friction is Fmax⁡=μsN=0.5⋅49=24.5 NF_{\max}=\mu_s N=0.5\cdot49=24.5\ \mathrm{N}. Since F=30 N>24.5 NF=30\ \mathrm{N}>24.5\ \mathrm{N}, the block moves. Once motion starts, kinetic friction acts: Fk=μkN=0.4⋅49=19.6 NF_k=\mu_k N=0.4\cdot49=19.6\ \mathrm{N}. Newton's second law along the horizontal gives ma=F−Fkma=F-F_k, so a=(30−19.6)/5=2.08 m/s2a=(30-19.6)/5=2.08\ \mathrm{m/s^2}.

Transfer

Problem

Transfer. A wooden cube of side a=0.10 ma=0.10\ \mathrm{m} and density ρ=600 kg/m3\rho=600\ \mathrm{kg/m^3} floats in water (ρf=1000 kg/m3\rho_f=1000\ \mathrm{kg/m^3}). (a) What fraction of the cube's volume is submerged? (b) What minimum mass must be added to the cube so that its top face is level with the water surface? Take g=9.8 m/s2g=9.8\ \mathrm{m/s^2}.

Solution

The cube's volume is V=a3=1.0⋅10−3 m3V=a^3=1.0\cdot10^{-3}\ \mathrm{m^3}, and its mass is m=ρV=600⋅10−3=0.60 kgm=\rho V=600\cdot10^{-3}=0.60\ \mathrm{kg}. The floating condition is FA=mgF_A=mg, that is, ρfVdispg=mg\rho_f V_{\text{disp}}g=mg. Hence Vdisp=m/ρf=0.60/1000=6.0⋅10−4 m3V_{\text{disp}}=m/\rho_f=0.60/1000=6.0\cdot10^{-4}\ \mathrm{m^3}. The submerged fraction is Vdisp/V=0.60V_{\text{disp}}/V=0.60 (or 60%60\%). For the cube to be fully submerged, the displaced volume equals V=1.0⋅10−3 m3V=1.0\cdot10^{-3}\ \mathrm{m^3}, and the buoyant force is FA=ρfVg=1000⋅10−3⋅9.8=9.8 NF_A=\rho_f Vg=1000\cdot10^{-3}\cdot9.8=9.8\ \mathrm{N}. The cube's weight is mg=0.60⋅9.8=5.88 Nmg=0.60\cdot9.8=5.88\ \mathrm{N}. The added mass must supply the missing weight: Δm g=FA−mg\Delta m\,g=F_A-mg, so Δm=0.40 kg\Delta m=0.40\ \mathrm{kg}.

Practice

Text

Safe self-study activity: work in the PhET 'Buoyancy' simulation or an equivalent one, without heating or hazardous substances.

  1. Set the fluid density to 1000 kg/m31000\ \mathrm{kg/m^3} and vary the body density from 200200 to 1200 kg/m31200\ \mathrm{kg/m^3}.
  2. For each case, record whether the body floats or sinks, and measure the submerged volume fraction.
  3. Check Archimedes' principle: calculate FA=ρfVdispgF_A=\rho_f V_{\text{disp}}g and compare it with the body's weight mgmg.
  4. Plot the submerged fraction against the ratio ρ/ρf\rho/\rho_f and explain its shape.
  5. Optionally, if a drag simulation is available, compare the linear and quadratic models and determine the terminal speed.

Visual reference

Purpose

Show how elastic, friction, drag, and buoyancy forces enter the equations of motion and where the limits of validity of each model lie.

Representation

A combined three-part diagram: (1) a graph of Hooke's law F=−kxF=-kx with the proportionality limit marked; (2) a friction-force graph: as the external force increases, FfrF_{\text{fr}} rises up to μsN\mu_s N and then drops abruptly to μkN\mu_k N; (3) a force diagram for a body in a fluid — weight mgmg downward, buoyant force FAF_A upward, drag force FdF_d opposing velocity, plus a graph of Fd(v)F_d(v) with linear and quadratic regions.

Real-world examples

Cycling downhill: air drag and rolling friction

Scenario

A cyclist plus bicycle of total mass 80 kg80\ \mathrm{kg} rides down a straight 8%8\% descent (sin⁡θ≈0.08\sin\theta \approx 0.08). The drag area is CdA=0.40 m2C_d A = 0.40\ \mathrm{m^2}, air density ρ=1.2 kg/m3\rho = 1.2\ \mathrm{kg/m^3}, rolling resistance coefficient μr=0.005\mu_r = 0.005. At v=12 m/sv = 12\ \mathrm{m/s} the air drag is Fd=12ρCdAv2=0.5⋅1.2⋅0.40⋅144=34.6 NF_d = \frac{1}{2}\rho C_d A v^2 = 0.5 \cdot 1.2 \cdot 0.40 \cdot 144 = 34.6\ \mathrm{N}, rolling friction is Fr=μrmg=0.005⋅80⋅9.8=3.9 NF_r = \mu_r mg = 0.005 \cdot 80 \cdot 9.8 = 3.9\ \mathrm{N}, and the component of weight along the slope is mgsin⁡θ=80⋅9.8⋅0.08=62.7 Nmg\sin\theta = 80 \cdot 9.8 \cdot 0.08 = 62.7\ \mathrm{N}. The first two forces together give 38.5 N38.5\ \mathrm{N}, so the bicycle still speeds up. A steady speed is reached when 0.24 v2=62.7−3.90.24\,v^2 = 62.7 - 3.9, that is at v=15.6 m/s≈56 km/hv = 15.6\ \mathrm{m/s} \approx 56\ \mathrm{km/h}; at that speed the air already takes 58 N58\ \mathrm{N} out of the 62.7 N62.7\ \mathrm{N} supplied by the descent.

Connection

The scenario exercises the quadratic drag law Fd=12ρCdAv2F_d = \frac{1}{2}\rho C_d A v^2 with its coefficient CdC_d and the dry-friction model f=μNf = \mu N, where N=mgcos⁡θ≈mgN = mg\cos\theta \approx mg. Both forces enter the equation of motion along the incline, and the steady speed follows from the equilibrium condition mgsin⁡θ=Fr+Fdmg\sin\theta = F_r + F_d.

Suspension bridge: stretching a steel cable

Scenario

A steel hanger cable of a bridge, length L=12 mL = 12\ \mathrm{m} and cross-sectional area A=4.0 cm2=4.0×10−4 m2A = 4.0\ \mathrm{cm^2} = 4.0\times10^{-4}\ \mathrm{m^2}, is pulled with a force F=60 kNF = 60\ \mathrm{kN}; Young's modulus of steel is E=200 GPaE = 200\ \mathrm{GPa}. The stress is σ=F/A=6.0×104/4.0×10−4=1.5×108 Pa=150 MPa\sigma = F/A = 6.0\times10^{4} / 4.0\times10^{-4} = 1.5\times10^{8}\ \mathrm{Pa} = 150\ \mathrm{MPa}, below the yield strength of structural steel, so the deformation is elastic. The strain is ε=σ/E=7.5×10−4\varepsilon = \sigma/E = 7.5\times10^{-4} and the extension is ΔL=εL=9.0 mm\Delta L = \varepsilon L = 9.0\ \mathrm{mm}. The cable stiffness is k=EA/L=6.7×106 N/mk = EA/L = 6.7\times10^{6}\ \mathrm{N/m}, so an extra load of 1 kN1\ \mathrm{kN} stretches it by another 0.15 mm0.15\ \mathrm{mm} or so.

Connection

The scenario exercises linear elasticity: Hooke's law in the form σ=Eε\sigma = E\varepsilon and its equivalent for a whole body, F=kΔLF = k\Delta L with k=EA/Lk = EA/L. It is precisely this linear stress-strain relation (within the elastic limit) that turns the cable tension into an extension.

Ferry in harbour: the buoyancy force

Scenario

A ferry of mass m=480 t=4.8×105 kgm = 480\ \mathrm{t} = 4.8\times10^{5}\ \mathrm{kg} floats in sea water of density ρ=1025 kg/m3\rho = 1025\ \mathrm{kg/m^3}. Its weight is mg=4.8×105⋅9.8=4.70×106 Nmg = 4.8\times10^{5} \cdot 9.8 = 4.70\times10^{6}\ \mathrm{N}, so it displaces a volume V=m/ρ=4.8×105/1025=468 m3V = m/\rho = 4.8\times10^{5}/1025 = 468\ \mathrm{m^3} of water, and the buoyancy force Fb=ρVgF_b = \rho V g exactly balances that weight. When 40 t=4.0×104 kg40\ \mathrm{t} = 4.0\times10^{4}\ \mathrm{kg} of cargo is taken on board, an extra displaced volume of 4.0×104/1025=39 m34.0\times10^{4}/1025 = 39\ \mathrm{m^3} is needed; with a waterplane area of about 700 m2700\ \mathrm{m^2} the ferry settles roughly 39/700=0.056 m=5.6 cm39/700 = 0.056\ \mathrm{m} = 5.6\ \mathrm{cm} deeper.

Connection

The scenario exercises Archimedes' principle: the buoyant force Fb=ρfluidVdispgF_b = \rho_{fluid} V_{disp} g equals the weight of the displaced liquid, and the floating condition ρfluidVdispg=mg\rho_{fluid} V_{disp} g = mg links the mass of the vessel to the volume of its submerged part and to its draft.