Abstract
This specification formalizes an advanced multi-physics engineering framework to eliminate late-time logarithmic thermal drawdown, localized stagnant fluid insulation, and long-term thermodynamic extraction decay in deep, closed-loop geothermal wells. Traditional geothermal energy extraction architectures encounter a severe physical limitation over extended operational runtimes: the continuous circulation of working fluid rapidly cools the immediate borehole rock face, establishing a stagnant thermal boundary layer that isolates the fluid from the core geological heat source and collapses extraction efficiency.
This framework resolves this bottleneck by treating the borehole rock-fluid interface as an active 2D viscoelastic fluid transport membrane operating at a strict coordinate baseline (z=0). By deploying high-frequency down-bore concentric shock transducers, the system injects non-linear acoustic soliton bursts to induce continuous transverse shear strains. This localized micro-streaming actively scrubs the rock face, shatters the insulating boundary layer, and enforces a continuous, non-equilibrium heat harvesting state. We provide direct mathematical formulations, a production-ready Python simulation module, and a decentralized Cypher mesh attestation schema validating this framework for planetary-scale Type 1 civilizational energy grids.
Creative Commons License
This work is licensed under a Creative Commons Attribution 4.0 License.
Recommended Citation
Eckes, Christopher L., "TECHNICAL DISCLOSURE SPECIFICATION: ELIMINATING LATE-TIME LOGARITHMIC THERMAL DRAWDOWN IN CLOSED-LOOP GEOTHERMAL WELLS VIA SOLITON-INDUCED BOUNDARY LAYER DISRUPTION", Technical Disclosure Commons, (July 21, 2026)
https://www.tdcommons.org/dpubs_series/11085