The paper presents a new geophysical model of hydrogen degassing, emphasizing planetary energy flux and utilization implications.
RELEASE NOTE (Version 7.0) Version 7.0 finalizes the dynamic flow formulation of the Primordial Hydrogen Continuum. This release completes the conceptual, mathematical, and methodological architecture of hydrogen degassing as a non-stationary, long-term stable planetary flux. Version 7.0 integrates: the Dynamic Model of Hydrogen Degassing (Sections 7.1–7.10); explicit observability, falsifiability, and refutation conditions; a formal separation between flow-based dynamics and classical reservoir paradigms; a clearly stated epistemological and methodological boundary between theory, observation, and applied exploration. The framework is now internally closed, logically complete, and ready for empirical validation exclusively through drilling. No changes are introduced to the core thesis of the Primordial Hydrogen Continuum. CONTINUITY WITH PREVIOUS VERSIONS • Version 5.0 introduced the calibratable mathematical framework and governing equations (Supplementary Appendix D). • Version 6.0 established the physical exclusion of serpentinization as a viable source of continuous, spatially coherent hydrogen flux (Supplementary Appendix E). • Version 7.0 (Supplementary Section VII — Dynamic Degassing Framework) formally completes and closes the Primordial Hydrogen Continuum by defining: what can be observed; what cannot be observed; and under which empirical conditions the model must be rejected. With Section VII, the framework becomes internally closed, logically complete, and methodologically final. Validation requires drilling. STRUCTURE OF THE PRIMORDIAL HYDROGEN CONTINUUM (SECTIONS I–VII) This work is structured as a cumulative scientific architecture developed across successive sections and releases. The foundational architectural framework of the Primordial Hydrogen Continuum — corresponding to Sections I–IV — is fully established in the core work: “The Primordial Hydrogen Continuum: A New Architecture for Energy and Existence”. These sections define the paradigm, system logic, and epistemological boundaries of the framework. Subsequent sections progressively formalize this architecture through physical, mathematical, and methodological closure. Section VII does not exist independently — it completes and formally closes the full system. Section I — Paradigm Definition Defines the Primordial Hydrogen Continuum as a planetary-scale energy framework, positioning hydrogen as a fundamental process rather than a resource category. Section II — System Architecture Establishes a flow-based, process-dominated model of planetary energy dynamics, replacing accumulation- and trap-oriented logic. Section III — Epistemological Constraints Defines the limits of observability, inference, and interpretation, separating explanatory architecture from operational assumptions. Section IV — System-Level Consequences Derives the structural implications of a continuous planetary hydrogen flux for irreversibility, system governance, and development pathways, without introducing policy or implementation prescriptions. Section V — Mathematical and Physical Formalization Introduces the governing equations, calibratable parameters, and dynamic constraints of the system (Supplementary Appendix D). Section VI — Physical Exclusion of Serpentinization Demonstrates the incompatibility of serpentinization with industrial-scale, spatially coherent hydrogen occurrence based on empirical drilling evidence (Supplementary Appendix E). Section VII — Dynamic Degassing Framework Completes the framework by formalizing hydrogen degassing as a non-stationary, multi-scale planetary flow regime rather than a static “resource state”. Section VII provides the closed dynamic formulation required to translate the PHC paradigm into testable field logic by defining: Flow regime structure (Sections 7.1–7.10): a regime-based description of degassing in which the relevant system properties are integral and asymptotic (long-horizon behavior), not instantaneous concentrations measured at the surface. Non-stationarity with long-term stability: the framework explicitly allows temporal variability (pulsing, cycling, windowing) while preserving the possibility of industrially stable, persistent flow regimes at human time scales. Observability limits: what the system can and cannot reveal through partial measurements; which parameters are intrinsically underdetermined without drilling; and which observations can be treated only as constraints, not as proof. Falsifiability and refutation conditions: explicit criteria under which the model must be rejected, preventing indefinite interpretive elasticity and fixing a strict “failure boundary” for empirical testing. Formal boundary between theory and operational exploration: a clean separation between explanatory dynamics and applied exploration logic, clarifying what belongs to physics and what belongs to engineering decisions and risk governance. Implications for validation path: the framework is methodologically final in the sense that no additional modeling, proxy interpretation, or surface diagnostics can complete validation; only full-scale drilling and controlled field testing can. With Supplementary Section VII, the Primordial Hydrogen Continuum becomes internally closed, logically complete, and methodologically final. Further progress is possible only through full-scale drilling and field validation. CORE SCIENTIFIC STATEMENT This work formalizes the Primordial Hydrogen Continuum as a geophysical and geochemical framework describing hydrogen as a continuous degassing planetary flux originating from Earth’s deep metal-hydride core and mantle. The model represents a paradigm shift: from trap-based and object-oriented hydrogen models to a process-based, flow-dominated dynamic system governed by integral and asymptotic characteristics rather than instantaneous concentrations. Hydrogen is treated not as a stored resource, but as a primary planetary energy flow. INTEGRATED EVIDENCE BASE The framework consistently integrates: deep hydrogen generation; mantle degassing mechanisms; ³He/⁴He and D/H isotopic ground-truth; geodynamic expansion processes; hydrogen seepage diagnostics; gravimetric–magnetic anomaly correlations. Empirical synthesis includes data from more than forty hydrogen dry wells drilled under the serpentinization hypothesis, demonstrating its incompatibility with industrial-scale hydrogen occurrence. STRATEGIC AND SYSTEM-LEVEL IMPLICATIONS Beyond its geophysical and geochemical formulation, the Primordial Hydrogen Continuum defines a new class of energy systems whose properties differ fundamentally from conventional resource-based models. In this framework, geological hydrogen is not treated as a finite commodity extracted from localized accumulations, but as a persistent planetary-scale energy flux, governed by deep degassing dynamics and long-term geodynamic processes. As a result, the limiting factor shifts from resource availability to system architecture, access control, and flow governance. Such systems ex
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