Skip to main content
U.S. Department of Energy
Office of Scientific and Technical Information

Transport of radionuclides released from a multiple-patch source into a planar fracture with transverse hydrodynamic dispersion

Conference · · Trans. Am. Nucl. Soc.; (United States)
OSTI ID:5459007
Fractures are considered a main path for hydrological transport of radionuclides released in a geologic repository. Although actual fractures form a complex network, single-fracture transport models are useful in predicting travel time and concentrations of released nuclides. Analytical solutions for one-dimensional transport in a single fracture with molecular diffusion in the surrounding rock matrix have been shown for the cases with and without longitudinal hydrodynamic dispersion in the fracture for a source of infinite width. In reality, however, when multiple waste packages of finite size are exposed to a fracture, the released radionuclides will spread due to hydrodynamic dispersion transverse to the flow direction. To show these effects, the authors present analytical solutions and numerical illustrations for the space-time-dependent concentrations of radionuclides released from finite patch sources into a planar fracture with transverse dispersion and matrix diffusion.
Research Organization:
Univ. of California, Berkeley
OSTI ID:
5459007
Report Number(s):
CONF-870601-Summs.
Conference Information:
Journal Name: Trans. Am. Nucl. Soc.; (United States) Journal Volume: 54
Country of Publication:
United States
Language:
English