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Title: Radionuclide gas transport through nuclear explosion-generated fracture networks

Journal Article · · Scientific Reports
DOI:https://doi.org/10.1038/srep18383· OSTI ID:1259301
 [1];  [2];  [2];  [2];  [2]
  1. Los Alamos National Lab. (LANL), Los Alamos, NM (United States); Neptune and Company, Los Alamos, NM (United States)
  2. Los Alamos National Lab. (LANL), Los Alamos, NM (United States)

Underground nuclear weapon testing produces radionuclide gases which may seep to the surface. Barometric pumping of gas through explosion-fractured rock is investigated using a new sequentially-coupled hydrodynamic rock damage/gas transport model. Fracture networks are produced for two rock types (granite and tuff) and three depths of burial. The fracture networks are integrated into a flow and transport numerical model driven by surface pressure signals of differing amplitude and variability. There are major differences between predictions using a realistic fracture network and prior results that used a simplified geometry. Matrix porosity and maximum fracture aperture have the greatest impact on gas breakthrough time and window of opportunity for detection, with different effects between granite and tuff simulations highlighting the importance of accurately simulating the fracture network. In particular, maximum fracture aperture has an opposite effect on tuff and granite, due to different damage patterns and their effect on the barometric pumping process. From stochastic simulations using randomly generated hydrogeologic parameters, normalized detection curves are presented to show differences in optimal sampling time for granite and tuff simulations. As a result, seasonal and location-based effects on breakthrough, which occur due to differences in barometric forcing, are stronger where the barometric signal is highly variable.

Research Organization:
Los Alamos National Laboratory (LANL), Los Alamos, NM (United States)
Sponsoring Organization:
USDOE; Defense Threat Reduction Agency (DTRA)
Grant/Contract Number:
DTRA1-11-4539I/BRCALL08-Per5-I-2-0008; AC52-06NA25396
OSTI ID:
1259301
Alternate ID(s):
OSTI ID: 1321760
Report Number(s):
LA-UR-15-24015; srep18383
Journal Information:
Scientific Reports, Vol. 5; ISSN 2045-2322
Publisher:
Nature Publishing GroupCopyright Statement
Country of Publication:
United States
Language:
English
Citation Metrics:
Cited by: 34 works
Citation information provided by
Web of Science

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Cited By (5)

Flow-through compression cell for small-angle and ultra-small-angle neutron scattering measurements journal May 2018
Identification of dominant gas transport frequencies during barometric pumping of fractured rock journal July 2019
Surrogate Models for Estimating Failure in Brittle and Quasi-Brittle Materials journal July 2019
Delayed signatures of underground nuclear explosions journal March 2016
Upscaled discrete fracture matrix model (UDFM): an octree-refined continuum representation of fractured porous media journal December 2019