A density- and composition-aware model for detonation propagation in the TATB-based explosive PBX 9502
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The ability to accurately model the subsurface transport of radionuclides is fundamental to the remote detection and characterization of underground nuclear explosion (UNE) events. Developing more sophisticated transport models presents a significant opportunity to enhance monitoring capabilities, particularly in the reliable prediction of signature migration. Experimentally determined characterization of geologic materials associated with transport properties is the pertinent base information for such robust model development and calibration. Here, we report results from an unprecedented study demonstrating changes to the pore and fracture network structures in geological materials in response to UNEs over nanometer to micrometer length scales. Volcanic tuffs of five different lithological formations from pre- and post-UNE environments were collected from the Nevada National Security Site. Combined ultra-small and small-angle neutron scattering techniques were used to characterize the tuff pore structure. The results demonstrate measurable differences in the specific surface area and porosity of samples pre- and post-shot from texturally similar lithological formations, indicating that pore properties can serve as a direct physical signature of a UNE. The results also provide experimentally determined transport parameters in support of advanced model development through the integration of gas migration, hydrodynamic simulations, and geologic framework models.
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Documents a study to examine model behavior as compared to open literature data on overdriven states in explosives
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Presentation at APS DFD 2024, SLC, Utah.
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This report describes an improvement to the XDDT code previously described in SAND2026-19856. The improvements include a conversion from CGS units to SI units, a simplified mesh refinement capability, and the addition of tabular gas-phase equation of state (EOS) tables.
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