Bulk fluid flow → Electrical work
Bulk fluid flowOcean wave motionPressure gradientElastic deformationMechanical stress or strainDirect piezoelectric effectSeparated surface chargeElectrical work
Epistemic state of the route
- known constituent relations
- 7 / 7 established or replicated · weakest constituent established
- constituent maturity floor
- K4 · experimentally observed
- search for this exact route
- Not assessed — complete composition not searched.
- recorded-pathway overlap
- shares relations, in order, with Wave-impact piezoelectric harvester · 3/7 relations shared
- route-level evidence
- 0 sources for the complete composition · 6 cited by the constituent steps
- boundaries and interfaces
- BOUNDARY compatible · no region transition
Explorematrix context · physics checks · steps · route evidence · constituent evidence · cite
Matrix context
D = disequilibrium row · C = coupling family column. A cell reads the state of the atlas for that pair.
D.10 × C.24 · Bulk fluid flow × Turbomachineryfamily: TurbomachineryD.10 × C.10 · Bulk fluid flow × Piezoelectricfamily: Piezoelectric
Typed bounds on this route
Every limit the atlas holds for this route, as constraint records: reached through bounded_by claims on the route's own entities. Hard bounds (an upper bound or a formula) decide the thermodynamic-bound check above; benchmarks, constitutive relations and resource limits are listed and never decisive. No prose limit exists anywhere (pass 42).
- Electromechanical coupling factor · formula-bound · hard, applies to this routeconverted fraction per cycle ≤ k² = d²/(s·ε)
Steps
- 01kinetic → mechanical · loss to thermal
- wind fetch over open water
liquidrefs [1] [2] - 02mechanical → mechanicalrefs [1] [2]
- 03mechanical → mechanical
- pressure acting on a diaphragm or shell
solidrefs [3] - 04mechanical → mechanical
- the deformed member carries a cyclic stress or strain state that can drive a stress-driven conversion (flexoelectric
- elastocaloric
- piezoelectric)
refs [3] [4] - 05mechanical → electrical · loss to thermalD = d · σ · piezoelectric charge coefficient d [C/N]
- a non-centrosymmetric crystal or a poled ferroelectric ceramic or polymer
- stress below the depoling and fracture limits
solid · non-centrosymmetric crystal requiredrefs [5] [3] [4] - 06electrical → electricalrefs [3]
- 07electrical → electrical · loss to thermal
- electrodes on the charged surfaces connected through a load
refs [6]
Evidence for the complete composition · 0
No source on record for this exact composition. The sources below support the individual steps, not the route as a whole.
Evidence for the constituent relations · 6
- [1]S. H. Salter. Wave power (1974)
- [2]J. Falnes. Ocean Waves and Oscillating Systems: Linear Interactions Including Wave-Energy Extraction (2002)
- [3]J. F. Nye. Physical Properties of Crystals: Their Representation by Tensors and Matrices (1985)
- [4]A. Erturk, D. J. Inman. Piezoelectric Energy Harvesting (2011)
- [5]J. Curie, P. Curie. Développement par compression de l'électricité polaire dans les cristaux hémièdres à faces inclinées (1880)
- [6]H. B. Radousky, H. Liang. Energy harvesting: an integrated view of materials, devices and applications (2012)
Cite this route
Physical Transformation Atlas (2026). route p-9f8d05e0b5: Bulk fluid flow → Ocean wave motion → Pressure gradient → Elastic deformation → Mechanical stress or strain → Direct piezoelectric effect → Separated surface charge → Electrical work. Dataset revision rbfbfcbb70e57 (hash of the canonical data). https://physical-transformation-atlas.wldud5192.workers.dev/path/9f8d05e0b5
Ids and matrix addresses are stable across revisions; the revision hash identifies the exact canonical files the record was compiled from and is meta.data_hash in every /api export. Reuse terms: see the license field in any export.