Willowmere Lock
Stone chamber · Upper reach · North bank
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Close the lower gate, balance the chamber to the upper reach, then release the boat safely.
03 / Lockmaster controls
When the gust arrives, choose how to spend pump energy. Boost closes the time gap; conserve favours efficiency.
Chamber level · m
vs. timeFlow rate · m³/s
in / out04 / Field notes
THE SCIENCE / EQUATIONS, ASSUMPTIONS & MODEL LIMITS
Hydraulic flow
Q = Cᵈ · A · a · √(2g · |Δh|) · sign(Δh)Q is volumetric flow (m³/s), Cᵈ is a discharge coefficient, A is the gate aperture area (m²), a is the opening fraction, and Δh is the water-head difference (m).
dh/dt = (Qᵢₙ + Qₚᵤₘₚ − Qₗₑₐₖ) / Aₗₒ꜀ₖThe chamber level is integrated by a fixed-step solver at 120 Hz. The dashed graph is an analytic, idealised fill curve for a constant upstream head and gate opening.
h(t) = H − [√(H − h₀) − (k·t/2)]²Buoyancy & pressure
Fᵦ = ρ · g · VᵈᶦˢᵖˡᵃᶜᵉᵈArchimedes' principle: a floating hull displaces a volume of water whose weight balances the vessel mass. The displayed draft uses a vertical-sided waterplane approximation:
draft ≈ mᵥₑₛₛₑₗ / (ρ · Aʷᵃᵗₑᵣₚˡᵃⁿᵉ)p = ρ · g · dGauge pressure increases with depth below the free surface. Fresh water density is treated as 1000 kg/m³ and g as 9.81 m/s².
Assumptions & simplifications
Water is incompressible and treated as fresh water of uniform density. The gate law is an approximate orifice equation; real lock hydraulics include submerged jets, changing discharge coefficients, turbulence, wall friction and complex transients.
The boat is a simplified box-hull with constant waterplane area. Mooring is a one-dimensional spring-damper approximation; wind loading is approximate. Pump efficiency is assumed to be 70% for the energy KPI.
Visual water waves are decorative and do not feed back into the hydraulic solver. No claim is made that this is a design or navigation tool.